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Pholadomya Stock Photos and Images
Pholadomya lirata (J. Sowerby) a bivalve that burrowed into soft sea-bed deposits Middle Jurassic, Callovian Stage; Lower Oxford Clay, Weymouth, Dorset. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/stock-photo-pholadomya-lirata-j-sowerby-a-bivalve-that-burrowed-into-soft-sea-76387513.htmlRMEC7N1D–Pholadomya lirata (J. Sowerby) a bivalve that burrowed into soft sea-bed deposits Middle Jurassic, Callovian Stage; Lower Oxford Clay, Weymouth, Dorset.
White Pholadomya Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/stock-photo-white-pholadomya-77315317.htmlRMEDP0D9–White Pholadomya
white pholadomya Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/stock-photo-white-pholadomya-25375824.htmlRMBD7Y3C–white pholadomya
Pholadomya, Print, Pholadomya is a genus of fossil saltwater clams, marine bivalve molluscs in the family Pholadomyidae Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-print-pholadomya-is-a-genus-of-fossil-saltwater-clams-marine-bivalve-molluscs-in-the-family-pholadomyidae-image328696371.htmlRM2A2NBG3–Pholadomya, Print, Pholadomya is a genus of fossil saltwater clams, marine bivalve molluscs in the family Pholadomyidae
Extinct bivalve mollusks: Pholadomya Murchisoni, Terebratula omalogogastyr, T. resupinata, T. perovalis and T. Theodori. Handcoloured lithograph by an unknown artist from Dr. F.A. Schmidt's 'Petrefactenbuch,' published in Stuttgart, Germany, 1855 by Verlag von Krais & Hoffmann. Dr. Schmidt's 'Book of Petrification' introduced fossils and palaeontology to both the specialist and general reader. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/extinct-bivalve-mollusks-pholadomya-murchisoni-terebratula-omalogogastyr-t-resupinata-t-perovalis-and-t-theodori-handcoloured-lithograph-by-an-unknown-artist-from-dr-fa-schmidts-petrefactenbuch-published-in-stuttgart-germany-1855-by-verlag-von-krais-hoffmann-dr-schmidts-book-of-petrification-introduced-fossils-and-palaeontology-to-both-the-specialist-and-general-reader-image209725603.htmlRMP55R43–Extinct bivalve mollusks: Pholadomya Murchisoni, Terebratula omalogogastyr, T. resupinata, T. perovalis and T. Theodori. Handcoloured lithograph by an unknown artist from Dr. F.A. Schmidt's 'Petrefactenbuch,' published in Stuttgart, Germany, 1855 by Verlag von Krais & Hoffmann. Dr. Schmidt's 'Book of Petrification' introduced fossils and palaeontology to both the specialist and general reader.
. Pholadomya 222 Pholadomya - Print - Iconographia Zoologica - Special Collections University of Amsterdam - UBAINV0274 005 06 0035 Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-222-pholadomya-print-iconographia-zoologica-special-collections-university-of-amsterdam-ubainv0274-005-06-0035-image207824718.htmlRMP236FA–. Pholadomya 222 Pholadomya - Print - Iconographia Zoologica - Special Collections University of Amsterdam - UBAINV0274 005 06 0035
Pholadomya loveni. 2 Jun 20161 Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-loveni-2-jun-20161-image353453068.htmlRM2BF14YT–Pholadomya loveni. 2 Jun 20161
Pholadomya (Procardia) sp. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-procardia-sp-image473725108.htmlRM2JEM15T–Pholadomya (Procardia) sp.
Pholadomya adelaidis. 16 Jan 20134182 Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-adelaidis-16-jan-20134182-image353531822.htmlRM2BF4NCE–Pholadomya adelaidis. 16 Jan 20134182
White Pholadomya. Reimagined by Gibon. Classic art with a modern twist reimagined Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/white-pholadomya-reimagined-by-gibon-classic-art-with-a-modern-twist-reimagined-image230418771.htmlRFRATDDR–White Pholadomya. Reimagined by Gibon. Classic art with a modern twist reimagined
Fossils of extinct bivalve mollusks Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/stock-photo-fossils-of-extinct-bivalve-mollusks-38109170.htmlRMC600HP–Fossils of extinct bivalve mollusks
A monograph of the Mollusca from the Great Oolite chiefly from Minchinhampton and the coast of Yorkshire . TAB. XI. Fig. 1. Pholadomya solitaria, p. 123. 2. Myacites calceiformis, p. 113. 3. Goniomya literata, p. 119. 4. Anatina undulata, p. 188. 5. 5a. Myacites Vezelayi, p. 111. 6. 6a. Anatina plicatella, p. 118. 7. la. Pholadomya socialis, p. 122. .vTVvc Tab. XT. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-monograph-of-the-mollusca-from-the-great-oolite-chiefly-from-minchinhampton-and-the-coast-of-yorkshire-tab-xi-fig-1-pholadomya-solitaria-p-123-2-myacites-calceiformis-p-113-3-goniomya-literata-p-119-4-anatina-undulata-p-188-5-5a-myacites-vezelayi-p-111-6-6a-anatina-plicatella-p-118-7-la-pholadomya-socialis-p-122-vtvvc-tab-xt-image338917824.htmlRM2AKB140–A monograph of the Mollusca from the Great Oolite chiefly from Minchinhampton and the coast of Yorkshire . TAB. XI. Fig. 1. Pholadomya solitaria, p. 123. 2. Myacites calceiformis, p. 113. 3. Goniomya literata, p. 119. 4. Anatina undulata, p. 188. 5. 5a. Myacites Vezelayi, p. 111. 6. 6a. Anatina plicatella, p. 118. 7. la. Pholadomya socialis, p. 122. .vTVvc Tab. XT.
Ancient mollusk shell fossilized in clay. Mollusk fossil. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/ancient-mollusk-shell-fossilized-in-clay-mollusk-fossil-image221616633.htmlRFPTFE7N–Ancient mollusk shell fossilized in clay. Mollusk fossil.
. Die Leitfossilien : ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen . 1,, 2. Glycimeris Heberti Bosqu. Oligocän. 3. Pliol.adomya Royaiia D'Urb. Cenoman. 4., 5. Pholadomya Candida Lam. Receut. Mantellinie vielfach unterbrochen. Schlossrand zahnlos. Hinterseite kürzer. Cyrtodaria Daudin. Jungtertiär — Jetzt. Pholadomyidae. L Schale gleichklappig. 2. Schale ungleichklappig, die rechte Schale höher gerückt als die linke. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/die-leitfossilien-ein-handbuch-fr-den-unterricht-und-fr-das-bestimmen-von-versteinerungen-1-2-glycimeris-heberti-bosqu-oligocn-3-plioladomya-royaiia-durb-cenoman-4-5-pholadomya-candida-lam-receut-mantellinie-vielfach-unterbrochen-schlossrand-zahnlos-hinterseite-krzer-cyrtodaria-daudin-jungtertir-jetzt-pholadomyidae-l-schale-gleichklappig-2-schale-ungleichklappig-die-rechte-schale-hher-gerckt-als-die-linke-image180883825.htmlRMME7Y4H–. Die Leitfossilien : ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen . 1,, 2. Glycimeris Heberti Bosqu. Oligocän. 3. Pliol.adomya Royaiia D'Urb. Cenoman. 4., 5. Pholadomya Candida Lam. Receut. Mantellinie vielfach unterbrochen. Schlossrand zahnlos. Hinterseite kürzer. Cyrtodaria Daudin. Jungtertiär — Jetzt. Pholadomyidae. L Schale gleichklappig. 2. Schale ungleichklappig, die rechte Schale höher gerückt als die linke.
![Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Oh. XX.] OOLITIC STKATA. 413 in their turn, repose upon the lias in the south and west of England. Among the characteristic shells of the Inferior Oolite, I may instance Terebratula fimbria (fig. 425), Rhynchonella spinosa (fig. 426), and Pholadomya fidicula (fig. 427). The extinct genus Pleurotomaria is also a form very common in this division as well as in the Oolitic sys- tem generally^ It resembles the Trochus i Stock Photo](https://c8.alamy.com/comp/RWTH1K/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-oh-xx-oolitic-stkata-413-in-their-turn-repose-upon-the-lias-in-the-south-and-west-of-england-among-the-characteristic-shells-of-the-inferior-oolite-i-may-instance-terebratula-fimbria-fig-425-rhynchonella-spinosa-fig-426-and-pholadomya-fidicula-fig-427-the-extinct-genus-pleurotomaria-is-also-a-form-very-common-in-this-division-as-well-as-in-the-oolitic-sys-tem-generally-it-resembles-the-trochus-i-RWTH1K.jpg "Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Oh. XX.] OOLITIC STKATA. 413 in their turn, repose upon the lias in the south and west of England. Among the characteristic shells of the Inferior Oolite, I may instance Terebratula fimbria (fig. 425), Rhynchonella spinosa (fig. 426), and Pholadomya fidicula (fig. 427). The extinct genus Pleurotomaria is also a form very common in this division as well as in the Oolitic sys- tem generally^ It resembles the Trochus i Stock Photo")
Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Oh. XX.] OOLITIC STKATA. 413 in their turn, repose upon the lias in the south and west of England. Among the characteristic shells of the Inferior Oolite, I may instance Terebratula fimbria (fig. 425), Rhynchonella spinosa (fig. 426), and Pholadomya fidicula (fig. 427). The extinct genus Pleurotomaria is also a form very common in this division as well as in the Oolitic sys- tem generally^ It resembles the Trochus i Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-oh-xx-oolitic-stkata-413-in-their-turn-repose-upon-the-lias-in-the-south-and-west-of-england-among-the-characteristic-shells-of-the-inferior-oolite-i-may-instance-terebratula-fimbria-fig-425-rhynchonella-spinosa-fig-426-and-pholadomya-fidicula-fig-427-the-extinct-genus-pleurotomaria-is-also-a-form-very-common-in-this-division-as-well-as-in-the-oolitic-sys-tem-generally-it-resembles-the-trochus-i-image239641407.htmlRMRWTH1K–Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Oh. XX.] OOLITIC STKATA. 413 in their turn, repose upon the lias in the south and west of England. Among the characteristic shells of the Inferior Oolite, I may instance Terebratula fimbria (fig. 425), Rhynchonella spinosa (fig. 426), and Pholadomya fidicula (fig. 427). The extinct genus Pleurotomaria is also a form very common in this division as well as in the Oolitic sys- tem generally^ It resembles the Trochus i
Bivalve shell fossil from mining industry. Ancient mollusk shell fossilized in clay. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bivalve-shell-fossil-from-mining-industry-ancient-mollusk-shell-fossilized-in-clay-image223299270.htmlRFPY84DX–Bivalve shell fossil from mining industry. Ancient mollusk shell fossilized in clay.
Pholadomya (Procardia) sp. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-procardia-sp-image473759990.htmlRM2JENHKJ–Pholadomya (Procardia) sp.
Pholadomya, Print, Pholadomya is a genus of fossil saltwater clams, marine bivalve molluscs in the family Pholadomyidae., Reimagined by Gibon, design of warm cheerful glowing of brightness and light rays radiance. Classic art reinvented with a modern twist. Photography inspired by futurism, embracing dynamic energy of modern technology, movement, speed and revolutionize culture. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-print-pholadomya-is-a-genus-of-fossil-saltwater-clams-marine-bivalve-molluscs-in-the-family-pholadomyidae-reimagined-by-gibon-design-of-warm-cheerful-glowing-of-brightness-and-light-rays-radiance-classic-art-reinvented-with-a-modern-twist-photography-inspired-by-futurism-embracing-dynamic-energy-of-modern-technology-movement-speed-and-revolutionize-culture-image349776983.htmlRF2B91M33–Pholadomya, Print, Pholadomya is a genus of fossil saltwater clams, marine bivalve molluscs in the family Pholadomyidae., Reimagined by Gibon, design of warm cheerful glowing of brightness and light rays radiance. Classic art reinvented with a modern twist. Photography inspired by futurism, embracing dynamic energy of modern technology, movement, speed and revolutionize culture.
A monograph of the Mollusca from the Great Oolite chiefly from Minchinhampton and the coast of Yorkshire . TAB. XI. Fig. 1. Pholadomya solitaria, p. 123. 2. Myacites calceiformis, p. 113. 3. Goniomya literata, p. 119. 4. Anatina undulata, p. 188. 5. 5a. Myacites Vezelayi, p. 111. 6. 6a. Anatina plicatella, p. 118. 7. la. Pholadomya socialis, p. 122. .vTVvc Tab. XT.. S..& :r2?*qk iV*** Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-monograph-of-the-mollusca-from-the-great-oolite-chiefly-from-minchinhampton-and-the-coast-of-yorkshire-tab-xi-fig-1-pholadomya-solitaria-p-123-2-myacites-calceiformis-p-113-3-goniomya-literata-p-119-4-anatina-undulata-p-188-5-5a-myacites-vezelayi-p-111-6-6a-anatina-plicatella-p-118-7-la-pholadomya-socialis-p-122-vtvvc-tab-xt-s-r2qk-iv-image338917271.htmlRM2AKB0C7–A monograph of the Mollusca from the Great Oolite chiefly from Minchinhampton and the coast of Yorkshire . TAB. XI. Fig. 1. Pholadomya solitaria, p. 123. 2. Myacites calceiformis, p. 113. 3. Goniomya literata, p. 119. 4. Anatina undulata, p. 188. 5. 5a. Myacites Vezelayi, p. 111. 6. 6a. Anatina plicatella, p. 118. 7. la. Pholadomya socialis, p. 122. .vTVvc Tab. XT.. S..& :r2?*qk iV***
. Die Leitfossilien, ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen . 1., L'. Glycimeris Heberti Bosqu. Oligocän. 3. Pholadomya Royana D'Ürb. Ceuoman. 4., 5. Pholadomya Candida Lam. Recent. Mantellinie vielfach unterbrochen. Schlössrand zahnlos. Hinterseite kürzer. Cyrtodaria Daudin. Jungtertiär — Jetzt. Pholadomyidae. 1. Schale gleichklappig. 2. Schale ungleichklappig, die rechte Schale höher gerückt als die linke. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/die-leitfossilien-ein-handbuch-fr-den-unterricht-und-fr-das-bestimmen-von-versteinerungen-1-l-glycimeris-heberti-bosqu-oligocn-3-pholadomya-royana-drb-ceuoman-4-5-pholadomya-candida-lam-recent-mantellinie-vielfach-unterbrochen-schlssrand-zahnlos-hinterseite-krzer-cyrtodaria-daudin-jungtertir-jetzt-pholadomyidae-1-schale-gleichklappig-2-schale-ungleichklappig-die-rechte-schale-hher-gerckt-als-die-linke-image180883693.htmlRMME7XYW–. Die Leitfossilien, ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen . 1., L'. Glycimeris Heberti Bosqu. Oligocän. 3. Pholadomya Royana D'Ürb. Ceuoman. 4., 5. Pholadomya Candida Lam. Recent. Mantellinie vielfach unterbrochen. Schlössrand zahnlos. Hinterseite kürzer. Cyrtodaria Daudin. Jungtertiär — Jetzt. Pholadomyidae. 1. Schale gleichklappig. 2. Schale ungleichklappig, die rechte Schale höher gerückt als die linke.
![Elemente der paläontologie bearbeitet (1890) Elemente der paläontologie bearbeitet elementederpal00stei Year: 1890 I. Thierreich. —VII. Mollusca. — ».Klasse: Lamellibranchiata. Desraodonta. 241 A. Ligament Uusserlich. Schale dünn. Schlossrand ohne Zähne oder deutlich entwickelten Ligamentlöffel. Pholadomya Sow. (Fig. 234 A, B). Die dünnschalige, gleichklappige Muschel zeigt einen querovalen oder fast dreiseitigen Umriss. Die Wirbel der vorn und hinten klaffenden Sehale meist stark nach vorn gerückt und gegen einander gebogen [B]. Schlossrand gerade, zahnlos oder mit schwach ent- wickeltem Vor Stock Photo](https://c8.alamy.com/comp/RWTB1P/elemente-der-palontologie-bearbeitet-1890-elemente-der-palontologie-bearbeitet-elementederpal00stei-year-1890-i-thierreich-vii-mollusca-klasse-lamellibranchiata-desraodonta-241-a-ligament-uusserlich-schale-dnn-schlossrand-ohne-zhne-oder-deutlich-entwickelten-ligamentlffel-pholadomya-sow-fig-234-a-b-die-dnnschalige-gleichklappige-muschel-zeigt-einen-querovalen-oder-fast-dreiseitigen-umriss-die-wirbel-der-vorn-und-hinten-klaffenden-sehale-meist-stark-nach-vorn-gerckt-und-gegen-einander-gebogen-b-schlossrand-gerade-zahnlos-oder-mit-schwach-ent-wickeltem-vor-RWTB1P.jpg "Elemente der paläontologie bearbeitet (1890) Elemente der paläontologie bearbeitet elementederpal00stei Year: 1890 I. Thierreich. —VII. Mollusca. — ».Klasse: Lamellibranchiata. Desraodonta. 241 A. Ligament Uusserlich. Schale dünn. Schlossrand ohne Zähne oder deutlich entwickelten Ligamentlöffel. Pholadomya Sow. (Fig. 234 A, B). Die dünnschalige, gleichklappige Muschel zeigt einen querovalen oder fast dreiseitigen Umriss. Die Wirbel der vorn und hinten klaffenden Sehale meist stark nach vorn gerückt und gegen einander gebogen [B]. Schlossrand gerade, zahnlos oder mit schwach ent- wickeltem Vor Stock Photo")
Elemente der paläontologie bearbeitet (1890) Elemente der paläontologie bearbeitet elementederpal00stei Year: 1890 I. Thierreich. —VII. Mollusca. — ».Klasse: Lamellibranchiata. Desraodonta. 241 A. Ligament Uusserlich. Schale dünn. Schlossrand ohne Zähne oder deutlich entwickelten Ligamentlöffel. Pholadomya Sow. (Fig. 234 A, B). Die dünnschalige, gleichklappige Muschel zeigt einen querovalen oder fast dreiseitigen Umriss. Die Wirbel der vorn und hinten klaffenden Sehale meist stark nach vorn gerückt und gegen einander gebogen [B]. Schlossrand gerade, zahnlos oder mit schwach ent- wickeltem Vor Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/elemente-der-palontologie-bearbeitet-1890-elemente-der-palontologie-bearbeitet-elementederpal00stei-year-1890-i-thierreich-vii-mollusca-klasse-lamellibranchiata-desraodonta-241-a-ligament-uusserlich-schale-dnn-schlossrand-ohne-zhne-oder-deutlich-entwickelten-ligamentlffel-pholadomya-sow-fig-234-a-b-die-dnnschalige-gleichklappige-muschel-zeigt-einen-querovalen-oder-fast-dreiseitigen-umriss-die-wirbel-der-vorn-und-hinten-klaffenden-sehale-meist-stark-nach-vorn-gerckt-und-gegen-einander-gebogen-b-schlossrand-gerade-zahnlos-oder-mit-schwach-ent-wickeltem-vor-image239636706.htmlRMRWTB1P–Elemente der paläontologie bearbeitet (1890) Elemente der paläontologie bearbeitet elementederpal00stei Year: 1890 I. Thierreich. —VII. Mollusca. — ».Klasse: Lamellibranchiata. Desraodonta. 241 A. Ligament Uusserlich. Schale dünn. Schlossrand ohne Zähne oder deutlich entwickelten Ligamentlöffel. Pholadomya Sow. (Fig. 234 A, B). Die dünnschalige, gleichklappige Muschel zeigt einen querovalen oder fast dreiseitigen Umriss. Die Wirbel der vorn und hinten klaffenden Sehale meist stark nach vorn gerückt und gegen einander gebogen [B]. Schlossrand gerade, zahnlos oder mit schwach ent- wickeltem Vor
Pholadomya (Procardia) sp. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-procardia-sp-image473711337.htmlRM2JEKBJ1–Pholadomya (Procardia) sp.
A guide to the fossil invertebrate animals in the Department of geology and palaeontology in the British museum (Natural history) . rge Tricliites with its thickshell, a favourite haunt of Lithodoimts, as various specimensshow. Another specimen shows a Litliodomns burrow in thefloor of the Oolitic sea, here formed of black CarboniferousLimestone. Then follow many species of Trigonia, Astarte,Pholadomya, Ceromya and other genera. Among all thesespecimens may be noticed others from the Ironstone ofDuston, Northamptonshire, and from the Collyweston Slate.In Yorkshire the Bajocian series includes Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-guide-to-the-fossil-invertebrate-animals-in-the-department-of-geology-and-palaeontology-in-the-british-museum-natural-history-rge-tricliites-with-its-thickshell-a-favourite-haunt-of-lithodoimts-as-various-specimensshow-another-specimen-shows-a-litliodomns-burrow-in-thefloor-of-the-oolitic-sea-here-formed-of-black-carboniferouslimestone-then-follow-many-species-of-trigonia-astartepholadomya-ceromya-and-other-genera-among-all-thesespecimens-may-be-noticed-others-from-the-ironstone-ofduston-northamptonshire-and-from-the-collyweston-slatein-yorkshire-the-bajocian-series-includes-image342705207.htmlRM2AWFFYK–A guide to the fossil invertebrate animals in the Department of geology and palaeontology in the British museum (Natural history) . rge Tricliites with its thickshell, a favourite haunt of Lithodoimts, as various specimensshow. Another specimen shows a Litliodomns burrow in thefloor of the Oolitic sea, here formed of black CarboniferousLimestone. Then follow many species of Trigonia, Astarte,Pholadomya, Ceromya and other genera. Among all thesespecimens may be noticed others from the Ironstone ofDuston, Northamptonshire, and from the Collyweston Slate.In Yorkshire the Bajocian series includes
![. Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen . Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten flaffeiib; ©djiofj mit flcinem 3^1^)"^; 2)?antelbud)t mäÃig tief; ©ip^onen long, ga Stock Photo](https://c8.alamy.com/comp/MAB7PT/dr-johannes-leunis-synopsis-der-thierkunde-ein-handbuch-fr-hhere-lehranstalten-und-fr-alle-welche-sich-wissenschaftlich-mit-der-naturgeschichte-der-thiere-beschftigen-wollen-pholadomya-candida-eben-bic-hufe-lajipe-ticit-innen-unten-tic-vecte-lape-von-anfjcn-in-13-ber-natvl-@rije-9-pliolailoiiiya-sow-siien-tttudcl-@cloc-glcicltappig-bnn-mit-uon-bcn-aitvbclit-ausftvqfilcnbcn-9itppcn-unglcicl-=-feitig-qiiev-ouai-ober-rautenfrmig-aufijebltt-rillten-flaffeiib-djiofj-mit-flcinem-31quot-2antelbudt-mig-tief-iponen-long-ga-MAB7PT.jpg ". Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen . Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten flaffeiib; ©djiofj mit flcinem 3^1^)"^; 2)?antelbud)t mäÃig tief; ©ip^onen long, ga Stock Photo")
. Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen . Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten flaffeiib; ©djiofj mit flcinem 3^1^)"^; 2)?antelbud)t mäÃig tief; ©ip^onen long, ga Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/dr-johannes-leunis-synopsis-der-thierkunde-ein-handbuch-fr-hhere-lehranstalten-und-fr-alle-welche-sich-wissenschaftlich-mit-der-naturgeschichte-der-thiere-beschftigen-wollen-pholadomya-candida-eben-bic-hufe-lajipe-ticit-innen-unten-tic-vecte-lape-von-anfjcn-in-13-ber-natvl-@rije-9-pliolailoiiiya-sow-siien-tttudcl-@cloc-glcicltappig-bnn-mit-uon-bcn-aitvbclit-ausftvqfilcnbcn-9itppcn-unglcicl-=-feitig-qiiev-ouai-ober-rautenfrmig-aufijebltt-rillten-flaffeiib-djiofj-mit-flcinem-31quot-2antelbudt-mig-tief-iponen-long-ga-image178497840.htmlRMMAB7PT–. Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen . Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten flaffeiib; ©djiofj mit flcinem 3^1^)"^; 2)?antelbud)t mäÃig tief; ©ip^onen long, ga
Dr Johannes Leunis Synopsis der Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen drjohannesleun01leun Year: 1883-86 I. Siphoniata. 1009 Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten fla Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/dr-johannes-leunis-synopsis-der-dr-johannes-leunis-synopsis-der-thierkunde-ein-handbuch-fr-hhere-lehranstalten-und-fr-alle-welche-sich-wissenschaftlich-mit-der-naturgeschichte-der-thiere-beschftigen-wollen-drjohannesleun01leun-year-1883-86-i-siphoniata-1009-pholadomya-candida-eben-bic-hufe-lajipe-ticit-innen-unten-tic-vecte-lape-von-anfjcn-in-13-ber-natvl-@rije-9-pliolailoiiiya-sow-siien-tttudcl-@cloc-glcicltappig-bnn-mit-uon-bcn-aitvbclit-ausftvqfilcnbcn-9itppcn-unglcicl-=-feitig-qiiev-ouai-ober-rautenfrmig-aufijebltt-rillten-fla-image241518464.htmlRMT0X37C–Dr Johannes Leunis Synopsis der Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen drjohannesleun01leun Year: 1883-86 I. Siphoniata. 1009 Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten fla
Pholadomya (Procardia) sp. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-procardia-sp-image473725767.htmlRM2JEM21B–Pholadomya (Procardia) sp.
Memoirs of the Geological Survey of India . y similar to the above; fossils being tolerably abimdant,and including many of the Garoodamungalum species, with others, such as Cyjirina, Opis,&c., which do not occur lower down, but which pass up into the Arrialoor group. Eetuming to the lower beds at Kolokaunuttom; on the camping ground to the West andSouth of this vUlage three bands of conglomerate limestone cropout prominently in parallel ridges, marking the bottom of thegroup. The included pebbles are chiefly of gneiss, and their fossil contents consist of CardiumSillanum, a Pholadomya, A.start Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/memoirs-of-the-geological-survey-of-india-y-similar-to-the-above-fossils-being-tolerably-abimdantand-including-many-of-the-garoodamungalum-species-with-others-such-as-cyjirina-opisc-which-do-not-occur-lower-down-but-which-pass-up-into-the-arrialoor-group-eetuming-to-the-lower-beds-at-kolokaunuttom-on-the-camping-ground-to-the-west-andsouth-of-this-vulage-three-bands-of-conglomerate-limestone-cropout-prominently-in-parallel-ridges-marking-the-bottom-of-thegroup-the-included-pebbles-are-chiefly-of-gneiss-and-their-fossil-contents-consist-of-cardiumsillanum-a-pholadomya-astart-image338229443.htmlRM2AJ7K2Y–Memoirs of the Geological Survey of India . y similar to the above; fossils being tolerably abimdant,and including many of the Garoodamungalum species, with others, such as Cyjirina, Opis,&c., which do not occur lower down, but which pass up into the Arrialoor group. Eetuming to the lower beds at Kolokaunuttom; on the camping ground to the West andSouth of this vUlage three bands of conglomerate limestone cropout prominently in parallel ridges, marking the bottom of thegroup. The included pebbles are chiefly of gneiss, and their fossil contents consist of CardiumSillanum, a Pholadomya, A.start
Pholadomya (Procardia) sp. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-procardia-sp-image473728522.htmlRM2JEM5FP–Pholadomya (Procardia) sp.
. The Quarterly journal of the Geological Society of London. fewshells,—a very small Corhula often occurs in great abundance; bsmall calcareous concretions, in which the Pholadomya Koninckii is notuncommon; c, large concretionary blocks, often very argillaceous;their lower surface frequently presents masses of shells, especially theCyprina Morrisii. Traces of Plants occur both in ** b and c. 16 3. Grey clayey sands, rather dark when wet, but lighter-coloured when diy (the upper part especially looking at a distance almost like chalk),—thelower part is more argillaceous and darker; d* a seam of Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-quarterly-journal-of-the-geological-society-of-london-fewshellsa-very-small-corhula-often-occurs-in-great-abundance-bsmall-calcareous-concretions-in-which-the-pholadomya-koninckii-is-notuncommon-c-large-concretionary-blocks-often-very-argillaceoustheir-lower-surface-frequently-presents-masses-of-shells-especially-thecyprina-morrisii-traces-of-plants-occur-both-in-b-and-c-16-3-grey-clayey-sands-rather-dark-when-wet-but-lighter-coloured-when-diy-the-upper-part-especially-looking-at-a-distance-almost-like-chalkthelower-part-is-more-argillaceous-and-darker-d-a-seam-of-image337118844.htmlRM2AGD2EM–. The Quarterly journal of the Geological Society of London. fewshells,—a very small Corhula often occurs in great abundance; bsmall calcareous concretions, in which the Pholadomya Koninckii is notuncommon; c, large concretionary blocks, often very argillaceous;their lower surface frequently presents masses of shells, especially theCyprina Morrisii. Traces of Plants occur both in ** b and c. 16 3. Grey clayey sands, rather dark when wet, but lighter-coloured when diy (the upper part especially looking at a distance almost like chalk),—thelower part is more argillaceous and darker; d* a seam of
Pholadomya (Procardia) sp. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-procardia-sp-image473729162.htmlRM2JEM6AJ–Pholadomya (Procardia) sp.
Memoires de la Société de physique et d'histoire naturelle de Genève . Tig 1. Panopœa acutisulcaia. K.g. 2. P. plicata. Fi^. 4P. Sataudiana. Fig 3 P. Ehodani . PI. 29.. Elrin^rr ad nn/ de/* et J^th Fi^. 1 Pholadomya Favrina Fié. S. P Genevensis. Fi6.3. Macfra ôaultina. Fié 4 Anatina RhodanJ.—Fi6.5. Periploma Sabaudiana Fiô. 6. Thracia lotimda. Fid. 7. T. alpina . Fi^. S. Petricola Rhodaiii PI.30. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/memoires-de-la-socit-de-physique-et-dhistoire-naturelle-de-genve-tig-1-panopa-acutisulcaia-kg-2-p-plicata-fi-4p-sataudiana-fig-3-p-ehodani-pi-29-elrinrr-ad-nn-de-et-jth-fi-1-pholadomya-favrina-fi-s-p-genevensis-fi63-macfra-aultina-fi-4-anatina-rhodanjfi65-periploma-sabaudiana-fi-6-thracia-lotimda-fid-7-t-alpina-fi-s-petricola-rhodaiii-pi30-image339998969.htmlRM2AN4849–Memoires de la Société de physique et d'histoire naturelle de Genève . Tig 1. Panopœa acutisulcaia. K.g. 2. P. plicata. Fi^. 4P. Sataudiana. Fig 3 P. Ehodani . PI. 29.. Elrin^rr ad nn/ de/* et J^th Fi^. 1 Pholadomya Favrina Fié. S. P Genevensis. Fi6.3. Macfra ôaultina. Fié 4 Anatina RhodanJ.—Fi6.5. Periploma Sabaudiana Fiô. 6. Thracia lotimda. Fid. 7. T. alpina . Fi^. S. Petricola Rhodaiii PI.30.
Pholadomya (Procardia) sp. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-procardia-sp-image473697956.htmlRM2JEJPG4–Pholadomya (Procardia) sp.
The ore deposits of Utah . 18 CHARACTERISTIC FOSSILS OF JURASSIC AGE. 19 2, Pholadomya kingii Meek; 3, Pseudomonotis (Eumicrolis) curta (Hall); 4, 5, Astarle packardi White; 6, 7, Cryphaeacalceola var. nebrascensis Meek and Hayden; 8, 9, Ostrea strigilecula White; 10, 11, Pentacrinus whilei Clark; 12, 13,Cuciillaoa haguci Meek; 14, 15, Pleuromya subrompressa Meek; 16; Lima occidentalis Hall and Whitfield; 17, Rhyu-clioiiella myrina Hall and Whitfield; 18, Trigonia quadrangularis Hall and Whitfield ; 19, Camptonectes stygius White. GEOLOGY. 7y Ophir ill the Oquirrh Range; in the MountNebo Range Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-ore-deposits-of-utah-18-characteristic-fossils-of-jurassic-age-19-2-pholadomya-kingii-meek-3-pseudomonotis-eumicrolis-curta-hall-4-5-astarle-packardi-white-6-7-cryphaeacalceola-var-nebrascensis-meek-and-hayden-8-9-ostrea-strigilecula-white-10-11-pentacrinus-whilei-clark-12-13cuciillaoa-haguci-meek-14-15-pleuromya-subrompressa-meek-16-lima-occidentalis-hall-and-whitfield-17-rhyu-clioiiella-myrina-hall-and-whitfield-18-trigonia-quadrangularis-hall-and-whitfield-19-camptonectes-stygius-white-geology-7y-ophir-ill-the-oquirrh-range-in-the-mountnebo-range-image338095362.htmlRM2AJ1G2A–The ore deposits of Utah . 18 CHARACTERISTIC FOSSILS OF JURASSIC AGE. 19 2, Pholadomya kingii Meek; 3, Pseudomonotis (Eumicrolis) curta (Hall); 4, 5, Astarle packardi White; 6, 7, Cryphaeacalceola var. nebrascensis Meek and Hayden; 8, 9, Ostrea strigilecula White; 10, 11, Pentacrinus whilei Clark; 12, 13,Cuciillaoa haguci Meek; 14, 15, Pleuromya subrompressa Meek; 16; Lima occidentalis Hall and Whitfield; 17, Rhyu-clioiiella myrina Hall and Whitfield; 18, Trigonia quadrangularis Hall and Whitfield ; 19, Camptonectes stygius White. GEOLOGY. 7y Ophir ill the Oquirrh Range; in the MountNebo Range
Pholadomya (Procardia) sp. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-procardia-sp-image473760031.htmlRM2JENHN3–Pholadomya (Procardia) sp.
. The American journal of science and arts. iae, and a longitudinal groove.—Found in Mon-mouth county, N. J. PHOLADOMYA. p. ocddentalis. (S. G. M.) PI. VIII, fig. 3. Oblong-angular, ven-tricose near the beaks; with twenty five or thirty narrow, elevated,subtortuous costae, having broad, slightly concave intervening spaces.Length two inches, breadth three inches. An extremely variablespecies: I possess five specimens, (all more or less broken,) in all ofwhich there is a difference in the number and relative position of theribs. CTTIIEREA. C excavata. (S. G. M.) PI. V, fig. 1. Suborbicular, comp Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-american-journal-of-science-and-arts-iae-and-a-longitudinal-groovefound-in-mon-mouth-county-n-j-pholadomya-p-ocddentalis-s-g-m-pi-viii-fig-3-oblong-angular-ven-tricose-near-the-beaks-with-twenty-five-or-thirty-narrow-elevatedsubtortuous-costae-having-broad-slightly-concave-intervening-spaceslength-two-inches-breadth-three-inches-an-extremely-variablespecies-i-possess-five-specimens-all-more-or-less-broken-in-all-ofwhich-there-is-a-difference-in-the-number-and-relative-position-of-theribs-cttiierea-c-excavata-s-g-m-pi-v-fig-1-suborbicular-comp-image336924207.htmlRM2AG467B–. The American journal of science and arts. iae, and a longitudinal groove.—Found in Mon-mouth county, N. J. PHOLADOMYA. p. ocddentalis. (S. G. M.) PI. VIII, fig. 3. Oblong-angular, ven-tricose near the beaks; with twenty five or thirty narrow, elevated,subtortuous costae, having broad, slightly concave intervening spaces.Length two inches, breadth three inches. An extremely variablespecies: I possess five specimens, (all more or less broken,) in all ofwhich there is a difference in the number and relative position of theribs. CTTIIEREA. C excavata. (S. G. M.) PI. V, fig. 1. Suborbicular, comp
Pholadomya pedernalis Roemer, 1849. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-pedernalis-roemer-1849-image473712647.htmlRM2JEKD8R–Pholadomya pedernalis Roemer, 1849.
A treatise on malacology; or, Shells and shell fish . shell, which iselongated, solen-shaped, gaping widely at the basalmargin, and united by a ligament, i^fig. 114. w.) F. clava. Sow. Gen. f. 1—4. Gastrochixa Lam. Animal perforating or parasitic ;tube calcareous, clavate, nearly divided longitudinallyfor half its length by an internal ridge, which formsa double aperture; the other or thick extremity en-closes an ovate bivalve shell, gaping very wide ante-riorly ; hinge linear and marginal; teeth none. {^fig.114. 6, c,d) G. modiolina. Sow. Gen. f. 1.* Pholadomya Sow. Shell 115 not tubular, pho Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-treatise-on-malacology-or-shells-and-shell-fish-shell-which-iselongated-solen-shaped-gaping-widely-at-the-basalmargin-and-united-by-a-ligament-ifig-114-w-f-clava-sow-gen-f-14-gastrochixa-lam-animal-perforating-or-parasitic-tube-calcareous-clavate-nearly-divided-longitudinallyfor-half-its-length-by-an-internal-ridge-which-formsa-double-aperture-the-other-or-thick-extremity-en-closes-an-ovate-bivalve-shell-gaping-very-wide-ante-riorly-hinge-linear-and-marginal-teeth-none-fig114-6-cd-g-modiolina-sow-gen-f-1-pholadomya-sow-shell-115-not-tubular-pho-image339101465.htmlRM2AKKBAH–A treatise on malacology; or, Shells and shell fish . shell, which iselongated, solen-shaped, gaping widely at the basalmargin, and united by a ligament, i^fig. 114. w.) F. clava. Sow. Gen. f. 1—4. Gastrochixa Lam. Animal perforating or parasitic ;tube calcareous, clavate, nearly divided longitudinallyfor half its length by an internal ridge, which formsa double aperture; the other or thick extremity en-closes an ovate bivalve shell, gaping very wide ante-riorly ; hinge linear and marginal; teeth none. {^fig.114. 6, c,d) G. modiolina. Sow. Gen. f. 1.* Pholadomya Sow. Shell 115 not tubular, pho
Pholadomya subventricosa Meek & Hayden. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-subventricosa-meek-hayden-image473725982.htmlRM2JEM292–Pholadomya subventricosa Meek & Hayden.
. Palæontology ... rfitliffrmi ll (Cretaceous) HLjASPB ;;-.. WM CJabtJ, del Bowen& C° lith. Fhiladf PLATE XXXVI Fig. 11. Fig- 12. Fig. 13. Fig. 14. Fig. 15. Fig. 16. Fig. 17. 17 a. Fig. 18. 18 a. Fig. 19. 19 a. Undetermined. 276 Pholadomya Sonorensis. Slightly magnified. 265 Tapes Hiluardi. Natural size. 265 Cardium (Granocardium) sabulosum. Natural size. 267 Cardium (Protocardium) granuliferum. Natural size. 267 i. Cardita alticosta. Magnified. 268 Eemondia furcata. Natural size. 270 Hinge of left valve. Cuculuea inermis. Natural size. 271End view of same. Exogyra plicata. Natural size. 275Ed Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/palontology-rfitliffrmi-ll-cretaceous-hljaspb-wm-cjabtj-del-bowen-c-lith-fhiladf-plate-xxxvi-fig-11-fig-12-fig-13-fig-14-fig-15-fig-16-fig-17-17-a-fig-18-18-a-fig-19-19-a-undetermined-276-pholadomya-sonorensis-slightly-magnified-265-tapes-hiluardi-natural-size-265-cardium-granocardium-sabulosum-natural-size-267-cardium-protocardium-granuliferum-natural-size-267-i-cardita-alticosta-magnified-268-eemondia-furcata-natural-size-270-hinge-of-left-valve-cuculuea-inermis-natural-size-271end-view-of-same-exogyra-plicata-natural-size-275ed-image336843362.htmlRM2AG0F42–. Palæontology ... rfitliffrmi ll (Cretaceous) HLjASPB ;;-.. WM CJabtJ, del Bowen& C° lith. Fhiladf PLATE XXXVI Fig. 11. Fig- 12. Fig. 13. Fig. 14. Fig. 15. Fig. 16. Fig. 17. 17 a. Fig. 18. 18 a. Fig. 19. 19 a. Undetermined. 276 Pholadomya Sonorensis. Slightly magnified. 265 Tapes Hiluardi. Natural size. 265 Cardium (Granocardium) sabulosum. Natural size. 267 Cardium (Protocardium) granuliferum. Natural size. 267 i. Cardita alticosta. Magnified. 268 Eemondia furcata. Natural size. 270 Hinge of left valve. Cuculuea inermis. Natural size. 271End view of same. Exogyra plicata. Natural size. 275Ed
Pholadomya subventricosa Meek & Hayden. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-subventricosa-meek-hayden-image473728485.htmlRM2JEM5ED–Pholadomya subventricosa Meek & Hayden.
![Memoires de la Société de physique et d'histoire naturelle de Genève . Elrin^rr ad nn/ de/* et J^th Fi^. 1 Pholadomya Favrina Fié. S. P Genevensis. Fi6.3. Macfra ôaultina. Fié 4 Anatina RhodanJ.—Fi6.5. Periploma Sabaudiana Fiô. 6. Thracia lotimda. Fid. 7. T. alpina . Fi^. S. Petricola Rhodaiii PI.30.. •lerri^t^ a</ ^ra/ ./r/.rf/i/li ^t/À.e&S^Ajti^à^neve^i F]6. 4 Venus Vihrayeana. l^^^é^ Thetis Genevensis. Fig. 3 Cardium Neckenanini. Fio. A C.Dupiiiiaiium. PI. 31 Stock Photo](https://c8.alamy.com/comp/2AN47FX/memoires-de-la-socit-de-physique-et-dhistoire-naturelle-de-genve-elrinrr-ad-nn-de-et-jth-fi-1-pholadomya-favrina-fi-s-p-genevensis-fi63-macfra-aultina-fi-4-anatina-rhodanjfi65-periploma-sabaudiana-fi-6-thracia-lotimda-fid-7-t-alpina-fi-s-petricola-rhodaiii-pi30-lerrit-alt-ra-rrfili-tesajtinevei-f-6-4-venus-vihrayeana-l-thetis-genevensis-fig-3-cardium-neckenanini-fio-a-cdupiiiiaiium-pi-31-2AN47FX.jpg "Memoires de la Société de physique et d'histoire naturelle de Genève . Elrin^rr ad nn/ de/* et J^th Fi^. 1 Pholadomya Favrina Fié. S. P Genevensis. Fi6.3. Macfra ôaultina. Fié 4 Anatina RhodanJ.—Fi6.5. Periploma Sabaudiana Fiô. 6. Thracia lotimda. Fid. 7. T. alpina . Fi^. S. Petricola Rhodaiii PI.30.. •lerri^t^ a</ ^ra/ ./r/.rf/i/li ^t/À.e&S^Ajti^à^neve^i F]6. 4 Venus Vihrayeana. l^^^é^ Thetis Genevensis. Fig. 3 Cardium Neckenanini. Fio. A C.Dupiiiiaiium. PI. 31 Stock Photo")
Memoires de la Société de physique et d'histoire naturelle de Genève . Elrin^rr ad nn/ de/* et J^th Fi^. 1 Pholadomya Favrina Fié. S. P Genevensis. Fi6.3. Macfra ôaultina. Fié 4 Anatina RhodanJ.—Fi6.5. Periploma Sabaudiana Fiô. 6. Thracia lotimda. Fid. 7. T. alpina . Fi^. S. Petricola Rhodaiii PI.30.. •lerri^t^ a</ ^ra/ ./r/.rf/i/li ^t/À.e&S^Ajti^à^neve^i F]6. 4 Venus Vihrayeana. l^^^é^ Thetis Genevensis. Fig. 3 Cardium Neckenanini. Fio. A C.Dupiiiiaiium. PI. 31 Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/memoires-de-la-socit-de-physique-et-dhistoire-naturelle-de-genve-elrinrr-ad-nn-de-et-jth-fi-1-pholadomya-favrina-fi-s-p-genevensis-fi63-macfra-aultina-fi-4-anatina-rhodanjfi65-periploma-sabaudiana-fi-6-thracia-lotimda-fid-7-t-alpina-fi-s-petricola-rhodaiii-pi30-lerrit-alt-ra-rrfili-tesajtinevei-f-6-4-venus-vihrayeana-l-thetis-genevensis-fig-3-cardium-neckenanini-fio-a-cdupiiiiaiium-pi-31-image339998510.htmlRM2AN47FX–Memoires de la Société de physique et d'histoire naturelle de Genève . Elrin^rr ad nn/ de/* et J^th Fi^. 1 Pholadomya Favrina Fié. S. P Genevensis. Fi6.3. Macfra ôaultina. Fié 4 Anatina RhodanJ.—Fi6.5. Periploma Sabaudiana Fiô. 6. Thracia lotimda. Fid. 7. T. alpina . Fi^. S. Petricola Rhodaiii PI.30.. •lerri^t^ a</ ^ra/ ./r/.rf/i/li ^t/À.e&S^Ajti^à^neve^i F]6. 4 Venus Vihrayeana. l^^^é^ Thetis Genevensis. Fig. 3 Cardium Neckenanini. Fio. A C.Dupiiiiaiium. PI. 31
Pholadomya sancti-sabae Roemer, 1849. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/pholadomya-sancti-sabae-roemer-1849-image473737838.htmlRM2JEMHCE–Pholadomya sancti-sabae Roemer, 1849.
Report of the United States Geological Survey of the territories . cimen, left side. 5^%. The larger imperfect type-specimen, same view. 5, c. Right view of a small specimen. Fig. 6. Thracia gracilis 224 6, a. A left-side view of one of the smaller specimens.6, b. A right-side view of the larger type-specimen. Fig. 7. Mactra (Ctmbophora ?) Formosa 207 A right-side view of an entire specimen.Fig. 8. Pholadomya subventhicosa 217 8, a. A left-side view of an imperfect cast, which is the type-specimen.6, /». A dorsal view of same. Fig. 9. Glycimehis occidentalis 2i>0 9, a. A side view of I he t Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/report-of-the-united-states-geological-survey-of-the-territories-cimen-left-side-5-the-larger-imperfect-type-specimen-same-view-5-c-right-view-of-a-small-specimen-fig-6-thracia-gracilis-224-6-a-a-left-side-view-of-one-of-the-smaller-specimens6-b-a-right-side-view-of-the-larger-type-specimen-fig-7-mactra-ctmbophora-formosa-207-a-right-side-view-of-an-entire-specimenfig-8-pholadomya-subventhicosa-217-8-a-a-left-side-view-of-an-imperfect-cast-which-is-the-type-specimen6-a-dorsal-view-of-same-fig-9-glycimehis-occidentalis-2igt0-9-a-a-side-view-of-i-he-t-image338072642.htmlRM2AJ0F2X–Report of the United States Geological Survey of the territories . cimen, left side. 5^%. The larger imperfect type-specimen, same view. 5, c. Right view of a small specimen. Fig. 6. Thracia gracilis 224 6, a. A left-side view of one of the smaller specimens.6, b. A right-side view of the larger type-specimen. Fig. 7. Mactra (Ctmbophora ?) Formosa 207 A right-side view of an entire specimen.Fig. 8. Pholadomya subventhicosa 217 8, a. A left-side view of an imperfect cast, which is the type-specimen.6, /». A dorsal view of same. Fig. 9. Glycimehis occidentalis 2i>0 9, a. A side view of I he t
. Palæontology ... WM CJabtJ, del Bowen& C° lith. Fhiladf PLATE XXXVI Fig. 11. Fig- 12. Fig. 13. Fig. 14. Fig. 15. Fig. 16. Fig. 17. 17 a. Fig. 18. 18 a. Fig. 19. 19 a. Undetermined. 276 Pholadomya Sonorensis. Slightly magnified. 265 Tapes Hiluardi. Natural size. 265 Cardium (Granocardium) sabulosum. Natural size. 267 Cardium (Protocardium) granuliferum. Natural size. 267 i. Cardita alticosta. Magnified. 268 Eemondia furcata. Natural size. 270 Hinge of left valve. Cuculuea inermis. Natural size. 271End view of same. Exogyra plicata. Natural size. 275Edge view of same. 32AJLJE QETDA IJ FS;V(DIi Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/palontology-wm-cjabtj-del-bowen-c-lith-fhiladf-plate-xxxvi-fig-11-fig-12-fig-13-fig-14-fig-15-fig-16-fig-17-17-a-fig-18-18-a-fig-19-19-a-undetermined-276-pholadomya-sonorensis-slightly-magnified-265-tapes-hiluardi-natural-size-265-cardium-granocardium-sabulosum-natural-size-267-cardium-protocardium-granuliferum-natural-size-267-i-cardita-alticosta-magnified-268-eemondia-furcata-natural-size-270-hinge-of-left-valve-cuculuea-inermis-natural-size-271end-view-of-same-exogyra-plicata-natural-size-275edge-view-of-same-32ajlje-qetda-ij-fsvdii-image336843179.htmlRM2AG0EWF–. Palæontology ... WM CJabtJ, del Bowen& C° lith. Fhiladf PLATE XXXVI Fig. 11. Fig- 12. Fig. 13. Fig. 14. Fig. 15. Fig. 16. Fig. 17. 17 a. Fig. 18. 18 a. Fig. 19. 19 a. Undetermined. 276 Pholadomya Sonorensis. Slightly magnified. 265 Tapes Hiluardi. Natural size. 265 Cardium (Granocardium) sabulosum. Natural size. 267 Cardium (Protocardium) granuliferum. Natural size. 267 i. Cardita alticosta. Magnified. 268 Eemondia furcata. Natural size. 270 Hinge of left valve. Cuculuea inermis. Natural size. 271End view of same. Exogyra plicata. Natural size. 275Edge view of same. 32AJLJE QETDA IJ FS;V(DIi
. Palæontology ... rf fcftfrwWo (Cretaceous). // IL >d.Vb, del Bowen& C° Tith. Philada On StonetyAJ.Ibootson. PLATE XXIX. PAGE Fig. 61. Solbn (Hypogella) cuneatus. Natural size. 175 Fig. 02. Corbula Hoitxn. Natural size. 176 62. Left valve. 62 a. Right valve. 62 b. Anterior end. Fig. 63. C. ALEFOKMIS. Natural size. 177 Fig. 61. Anatina quaduata. Natural size. 177 Fig. 65. Pholadomya Okegonensis. Natural size. 178 Fig. 66. Pleuromya papyhacea. Natural size. 178 Fig. 67. Ap.comya uxdulata. Natural size. 179 Fig. 68. ? Mactra texuissima. Natural size. 179 Fig. 69. 69 a. Hinge of Cymbophoka Ash Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/palontology-rf-fcftfrwwo-cretaceous-il-gtdvb-del-bowen-c-tith-philada-on-stonetyajibootson-plate-xxix-page-fig-61-solbn-hypogella-cuneatus-natural-size-175-fig-02-corbula-hoitxn-natural-size-176-62-left-valve-62-a-right-valve-62-b-anterior-end-fig-63-c-alefokmis-natural-size-177-fig-61-anatina-quaduata-natural-size-177-fig-65-pholadomya-okegonensis-natural-size-178-fig-66-pleuromya-papyhacea-natural-size-178-fig-67-apcomya-uxdulata-natural-size-179-fig-68-mactra-texuissima-natural-size-179-fig-69-69-a-hinge-of-cymbophoka-ash-image336850090.htmlRM2AG0RMA–. Palæontology ... rf fcftfrwWo (Cretaceous). // IL >d.Vb, del Bowen& C° Tith. Philada On StonetyAJ.Ibootson. PLATE XXIX. PAGE Fig. 61. Solbn (Hypogella) cuneatus. Natural size. 175 Fig. 02. Corbula Hoitxn. Natural size. 176 62. Left valve. 62 a. Right valve. 62 b. Anterior end. Fig. 63. C. ALEFOKMIS. Natural size. 177 Fig. 61. Anatina quaduata. Natural size. 177 Fig. 65. Pholadomya Okegonensis. Natural size. 178 Fig. 66. Pleuromya papyhacea. Natural size. 178 Fig. 67. Ap.comya uxdulata. Natural size. 179 Fig. 68. ? Mactra texuissima. Natural size. 179 Fig. 69. 69 a. Hinge of Cymbophoka Ash
. God's two books; or, Plain facts about evolution, geology, and the Bible . m. Mastodon 1. Univalve (Cerithtum) 2. Conifer (Sequoia) NummuliteUnivalve (Natica) 1. Pearl Mussel (Inoceramtis) 2. Ammonite, new form {Turrilites) 3. Bivalve (Pecten)Ammonite, new form {Hamitcs) Bivalve (Pholadomya)Bivalve (Trigonia) Cycad (Maiitcllla)Univalve (Nerinaa) Fish-lizard (Iclitliyosaur)Ammonite.Sea-lily (Encrinits)Footprints of Labyrinthodon. 1. Bivalve (Bakeziellia) 2. Lampshell (Productus)Ganoid {Palcconiscus)Precursors of Ammonites (Gonialite)2. CluTj-moss (Lepidodendron)Horsetail Plants (Calamite) Gan Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/gods-two-books-or-plain-facts-about-evolution-geology-and-the-bible-m-mastodon-1-univalve-cerithtum-2-conifer-sequoia-nummuliteunivalve-natica-1-pearl-mussel-inoceramtis-2-ammonite-new-form-turrilites-3-bivalve-pectenammonite-new-form-hamitcs-bivalve-pholadomyabivalve-trigonia-cycad-maiitclllaunivalve-nerinaa-fish-lizard-iclitliyosaurammonitesea-lily-encrinitsfootprints-of-labyrinthodon-1-bivalve-bakeziellia-2-lampshell-productusganoid-palcconiscusprecursors-of-ammonites-gonialite2-clutj-moss-lepidodendronhorsetail-plants-calamite-gan-image369991591.htmlRM2CDXG1B–. God's two books; or, Plain facts about evolution, geology, and the Bible . m. Mastodon 1. Univalve (Cerithtum) 2. Conifer (Sequoia) NummuliteUnivalve (Natica) 1. Pearl Mussel (Inoceramtis) 2. Ammonite, new form {Turrilites) 3. Bivalve (Pecten)Ammonite, new form {Hamitcs) Bivalve (Pholadomya)Bivalve (Trigonia) Cycad (Maiitcllla)Univalve (Nerinaa) Fish-lizard (Iclitliyosaur)Ammonite.Sea-lily (Encrinits)Footprints of Labyrinthodon. 1. Bivalve (Bakeziellia) 2. Lampshell (Productus)Ganoid {Palcconiscus)Precursors of Ammonites (Gonialite)2. CluTj-moss (Lepidodendron)Horsetail Plants (Calamite) Gan
. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Photo : J. V. L. R. JVeill & Co., Ltd. »LAMELLIBRANCHIA FROM NORTHERN ZULULAND. 1-3. Trigonia hennigi. 4. Pholadomya luynesi.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. South African Museum. Cape Town : The Museum Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/annals-of-the-south-african-museum-=-annale-van-die-suid-afrikaanse-museum-natural-history-photo-j-v-l-r-jveill-amp-co-ltd-lamellibranchia-from-northern-zululand-1-3-trigonia-hennigi-4-pholadomya-luynesi-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-south-african-museum-cape-town-the-museum-image236439402.htmlRMRMJMTA–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Photo : J. V. L. R. JVeill & Co., Ltd. »LAMELLIBRANCHIA FROM NORTHERN ZULULAND. 1-3. Trigonia hennigi. 4. Pholadomya luynesi.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. South African Museum. Cape Town : The Museum
. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Lower Cretaceous Lemellibranchia from Northern Zululand. 291 Dipoloceras quadratum, Deiradoceras spp., Pervinquieria spp., Gervillia dentata, Inoceramus concentricus, Scabrotrigonia spp., Pholadomya vignesi, Goniomya sp., Veniella etheridgei, Exogyra conica, Ostrea sp., and Turritella manuanensis. The beds Z17 are less fossiliferous, but carry Adkinsites umsinenense,. Gssferopoc/ /.//7?esfo/7e. Fig. 3. Pervinquieria, Hysteroceras chojfati, Dipoloceras cristatum, and Phylloceras velledae. North of the Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/annals-of-the-south-african-museum-=-annale-van-die-suid-afrikaanse-museum-natural-history-lower-cretaceous-lemellibranchia-from-northern-zululand-291-dipoloceras-quadratum-deiradoceras-spp-pervinquieria-spp-gervillia-dentata-inoceramus-concentricus-scabrotrigonia-spp-pholadomya-vignesi-goniomya-sp-veniella-etheridgei-exogyra-conica-ostrea-sp-and-turritella-manuanensis-the-beds-z17-are-less-fossiliferous-but-carry-adkinsites-umsinenense-gssferopoc-7esfo7e-fig-3-pervinquieria-hysteroceras-chojfati-dipoloceras-cristatum-and-phylloceras-velledae-north-of-the-image236439961.htmlRMRMJNG9–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Lower Cretaceous Lemellibranchia from Northern Zululand. 291 Dipoloceras quadratum, Deiradoceras spp., Pervinquieria spp., Gervillia dentata, Inoceramus concentricus, Scabrotrigonia spp., Pholadomya vignesi, Goniomya sp., Veniella etheridgei, Exogyra conica, Ostrea sp., and Turritella manuanensis. The beds Z17 are less fossiliferous, but carry Adkinsites umsinenense,. Gssferopoc/ /.//7?esfo/7e. Fig. 3. Pervinquieria, Hysteroceras chojfati, Dipoloceras cristatum, and Phylloceras velledae. North of the
![. Bulletin of the British Museum (Natural History) Geology Supplement. ss JURASSIC RHYNCHONELLIDS Distribution. The distribution of the species is very uncertain and the only definite records are from the " Terrain a Chailles ", of northern France and the Swiss Jura around Basel. Occurrence. The specimens collected by the author at Pagny were from sandy limestones containing cherty bands and nodules. The large associated fauna con- sisted of ammonites, lamellibranchs, mainly Pholadomya and Lima types, and Thurmannella obtrita. T. obtrita was the most abundant element and tended to. 3 Stock Photo](https://c8.alamy.com/comp/RGHB1A/bulletin-of-the-british-museum-natural-history-geology-supplement-ss-jurassic-rhynchonellids-distribution-the-distribution-of-the-species-is-very-uncertain-and-the-only-definite-records-are-from-the-quot-terrain-a-chailles-quot-of-northern-france-and-the-swiss-jura-around-basel-occurrence-the-specimens-collected-by-the-author-at-pagny-were-from-sandy-limestones-containing-cherty-bands-and-nodules-the-large-associated-fauna-con-sisted-of-ammonites-lamellibranchs-mainly-pholadomya-and-lima-types-and-thurmannella-obtrita-t-obtrita-was-the-most-abundant-element-and-tended-to-3-RGHB1A.jpg ". Bulletin of the British Museum (Natural History) Geology Supplement. ss JURASSIC RHYNCHONELLIDS Distribution. The distribution of the species is very uncertain and the only definite records are from the " Terrain a Chailles ", of northern France and the Swiss Jura around Basel. Occurrence. The specimens collected by the author at Pagny were from sandy limestones containing cherty bands and nodules. The large associated fauna con- sisted of ammonites, lamellibranchs, mainly Pholadomya and Lima types, and Thurmannella obtrita. T. obtrita was the most abundant element and tended to. 3 Stock Photo")
. Bulletin of the British Museum (Natural History) Geology Supplement. ss JURASSIC RHYNCHONELLIDS Distribution. The distribution of the species is very uncertain and the only definite records are from the " Terrain a Chailles ", of northern France and the Swiss Jura around Basel. Occurrence. The specimens collected by the author at Pagny were from sandy limestones containing cherty bands and nodules. The large associated fauna con- sisted of ammonites, lamellibranchs, mainly Pholadomya and Lima types, and Thurmannella obtrita. T. obtrita was the most abundant element and tended to. 3 Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-british-museum-natural-history-geology-supplement-ss-jurassic-rhynchonellids-distribution-the-distribution-of-the-species-is-very-uncertain-and-the-only-definite-records-are-from-the-quot-terrain-a-chailles-quot-of-northern-france-and-the-swiss-jura-around-basel-occurrence-the-specimens-collected-by-the-author-at-pagny-were-from-sandy-limestones-containing-cherty-bands-and-nodules-the-large-associated-fauna-con-sisted-of-ammonites-lamellibranchs-mainly-pholadomya-and-lima-types-and-thurmannella-obtrita-t-obtrita-was-the-most-abundant-element-and-tended-to-3-image233951126.htmlRMRGHB1A–. Bulletin of the British Museum (Natural History) Geology Supplement. ss JURASSIC RHYNCHONELLIDS Distribution. The distribution of the species is very uncertain and the only definite records are from the " Terrain a Chailles ", of northern France and the Swiss Jura around Basel. Occurrence. The specimens collected by the author at Pagny were from sandy limestones containing cherty bands and nodules. The large associated fauna con- sisted of ammonites, lamellibranchs, mainly Pholadomya and Lima types, and Thurmannella obtrita. T. obtrita was the most abundant element and tended to. 3
. Bulletin de la Société géologique de France. Geology. Bull. Soc. (féal, de Fr NOTE DE, M. LERICHE I BARTONIEN (Sables de Wemmel et Argiles d'Assche; Marnes à Pholadomya ludensis). carte paléogéogrtjft,^^ ^^ ^^^^^^^^. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Société géologique de France. Paris : La Société Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-bull-soc-fal-de-fr-note-de-m-leriche-i-bartonien-sables-de-wemmel-et-argiles-dassche-marnes-pholadomya-ludensis-carte-palogogrtjft-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-socit-gologique-de-france-paris-la-socit-image234053483.htmlRMRGP1GY–. Bulletin de la Société géologique de France. Geology. Bull. Soc. (féal, de Fr NOTE DE, M. LERICHE I BARTONIEN (Sables de Wemmel et Argiles d'Assche; Marnes à Pholadomya ludensis). carte paléogéogrtjft,^^ ^^ ^^^^^^^^. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Société géologique de France. Paris : La Société
. Bulletin of the British Museum (Natural History) Geology Supplement. INDEX 213 quadrata, Mactromya, 97 quennelli, Ampullospira, 165 quennelli, Fimbria, 99 quennelli, Myophorella, 79 quenstedti, Hippopodium, 82 Quenstedtia, 119 radiata, Meleagrinella, 48 Radulopecten, 57 rahmuensis, Homomya, 128 rahmuensis, Lima (Plagiostoma), 61 rahmuensis, Protocardia, 104 recki, Astarte, 91 reticulata, Pholadomya, 125 Rhabdocolpus, 156 Rhabdoconcha, 151 rhomboidalis, Praeconia, 94 rollandi, Eligmus, 47 Rollieria, 29 Rutitrigonia, 81 Ryderia, 27 saemanni, Bourguetia, 152 saggersoni, Gervillia, 45 saggersoni Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-british-museum-natural-history-geology-supplement-index-213-quadrata-mactromya-97-quennelli-ampullospira-165-quennelli-fimbria-99-quennelli-myophorella-79-quenstedti-hippopodium-82-quenstedtia-119-radiata-meleagrinella-48-radulopecten-57-rahmuensis-homomya-128-rahmuensis-lima-plagiostoma-61-rahmuensis-protocardia-104-recki-astarte-91-reticulata-pholadomya-125-rhabdocolpus-156-rhabdoconcha-151-rhomboidalis-praeconia-94-rollandi-eligmus-47-rollieria-29-rutitrigonia-81-ryderia-27-saemanni-bourguetia-152-saggersoni-gervillia-45-saggersoni-image233978031.htmlRMRGJHA7–. Bulletin of the British Museum (Natural History) Geology Supplement. INDEX 213 quadrata, Mactromya, 97 quennelli, Ampullospira, 165 quennelli, Fimbria, 99 quennelli, Myophorella, 79 quenstedti, Hippopodium, 82 Quenstedtia, 119 radiata, Meleagrinella, 48 Radulopecten, 57 rahmuensis, Homomya, 128 rahmuensis, Lima (Plagiostoma), 61 rahmuensis, Protocardia, 104 recki, Astarte, 91 reticulata, Pholadomya, 125 Rhabdocolpus, 156 Rhabdoconcha, 151 rhomboidalis, Praeconia, 94 rollandi, Eligmus, 47 Rollieria, 29 Rutitrigonia, 81 Ryderia, 27 saemanni, Bourguetia, 152 saggersoni, Gervillia, 45 saggersoni
. Bulletin of the British Museum (Natural History), Geology. 70 specimens and is in this way similar to the anterior flank of Pentagrammysia. Genus SIPHOGRAMMYSIA Chernychev, 1950 Type species. Pholadomya kasanensis Geinitz 1880. Permian. ?Kazanian, Kazan, U.S.S.R. Discussion. Siphogrammysia resembles some other sanguino- litids in shape and has divergent ribs forming Vs in a similar way to Cosmomya and Pentagrammysia (Chernychev 1950; l=Manankovia Astafieva-Urbaitis, 1983), but the discordant ribs are much bolder in design and more prominent. They are convergent in pattern with ribs of the tr Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-of-the-british-museum-natural-history-geology-70-specimens-and-is-in-this-way-similar-to-the-anterior-flank-of-pentagrammysia-genus-siphogrammysia-chernychev-1950-type-species-pholadomya-kasanensis-geinitz-1880-permian-kazanian-kazan-ussr-discussion-siphogrammysia-resembles-some-other-sanguino-litids-in-shape-and-has-divergent-ribs-forming-vs-in-a-similar-way-to-cosmomya-and-pentagrammysia-chernychev-1950-l=manankovia-astafieva-urbaitis-1983-but-the-discordant-ribs-are-much-bolder-in-design-and-more-prominent-they-are-convergent-in-pattern-with-ribs-of-the-tr-image233951580.htmlRMRGHBHG–. Bulletin of the British Museum (Natural History), Geology. 70 specimens and is in this way similar to the anterior flank of Pentagrammysia. Genus SIPHOGRAMMYSIA Chernychev, 1950 Type species. Pholadomya kasanensis Geinitz 1880. Permian. ?Kazanian, Kazan, U.S.S.R. Discussion. Siphogrammysia resembles some other sanguino- litids in shape and has divergent ribs forming Vs in a similar way to Cosmomya and Pentagrammysia (Chernychev 1950; l=Manankovia Astafieva-Urbaitis, 1983), but the discordant ribs are much bolder in design and more prominent. They are convergent in pattern with ribs of the tr
. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. 268 ANNALS OF THE SOUTH AFRICAN MUSEUM. Fig. 2. A-B. Puzosia bistricta (White). SAM-PCA2649. x 1. C-F. Undetermined bivalves from the 'Couches a Pholadomya, Reinecke Collection, South African Museum, x 1,5.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. South African Museum. Cape Town : The Museum Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/annals-of-the-south-african-museum-=-annale-van-die-suid-afrikaanse-museum-natural-history-268-annals-of-the-south-african-museum-fig-2-a-b-puzosia-bistricta-white-sam-pca2649-x-1-c-f-undetermined-bivalves-from-the-couches-a-pholadomya-reinecke-collection-south-african-museum-x-15-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-south-african-museum-cape-town-the-museum-image236456898.htmlRMRMKF56–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. 268 ANNALS OF THE SOUTH AFRICAN MUSEUM. Fig. 2. A-B. Puzosia bistricta (White). SAM-PCA2649. x 1. C-F. Undetermined bivalves from the 'Couches a Pholadomya, Reinecke Collection, South African Museum, x 1,5.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. South African Museum. Cape Town : The Museum
. Bulletin de la Société géologique de France. Geology. Bull. Soc. gèol. de Fr. NOl. LEGENDE IbARTONIEN (Sables de Wemmel et Argiles d'Assche; Marnes à Pholadomya ludensis). â -.Limite probable de l'extension de la mer barbonienne Les sédiments post-bartoniens sont Supposés enlevés. Carte paléogc. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Société géologique de France. Paris : La Société Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-bull-soc-gol-de-fr-nol-legende-ibartonien-sables-de-wemmel-et-argiles-dassche-marnes-pholadomya-ludensis-limite-probable-de-lextension-de-la-mer-barbonienne-les-sdiments-post-bartoniens-sont-supposs-enlevs-carte-palogc-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-socit-gologique-de-france-paris-la-socit-image234053517.htmlRMRGP1J5–. Bulletin de la Société géologique de France. Geology. Bull. Soc. gèol. de Fr. NOl. LEGENDE IbARTONIEN (Sables de Wemmel et Argiles d'Assche; Marnes à Pholadomya ludensis). â -.Limite probable de l'extension de la mer barbonienne Les sédiments post-bartoniens sont Supposés enlevés. Carte paléogc. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Société géologique de France. Paris : La Société
![. North American geology and palaeontology for the use of amateurs, students, and scientists [microform]. Paleontology; Paleontology; Geology; Paléontologie; Paléontologie; Géologie. Fia. 891.—Pliolauella newberryi. omata, Hall, 1870, Prelim. Notice Lam. Shells, p. 64, syn. for P. radiata. parallela. Hall, 1883, Pal. N. Y., vol. 5, pi. 78, figs. 22-24, Ham. Gr. radiata, Conrad, 1842, (Nuculitesradiatus,) Jour. Acad. Nat. Sci., vol. 8, p. 248, and Pal. N. Y., vol. 5, pi. 78, figs. 15-21, Ham. Gr. truncata, Hall, 1870, Prelim. Notice Lam. Shells, p. 64, syn. for P. radiata. Pholadomya elongata, Stock Photo](https://c8.alamy.com/comp/RJ12DX/north-american-geology-and-palaeontology-for-the-use-of-amateurs-students-and-scientists-microform-paleontology-paleontology-geology-palontologie-palontologie-gologie-fia-891pliolauella-newberryi-omata-hall-1870-prelim-notice-lam-shells-p-64-syn-for-p-radiata-parallela-hall-1883-pal-n-y-vol-5-pi-78-figs-22-24-ham-gr-radiata-conrad-1842-nuculitesradiatus-jour-acad-nat-sci-vol-8-p-248-and-pal-n-y-vol-5-pi-78-figs-15-21-ham-gr-truncata-hall-1870-prelim-notice-lam-shells-p-64-syn-for-p-radiata-pholadomya-elongata-RJ12DX.jpg ". North American geology and palaeontology for the use of amateurs, students, and scientists [microform]. Paleontology; Paleontology; Geology; Paléontologie; Paléontologie; Géologie. Fia. 891.—Pliolauella newberryi. omata, Hall, 1870, Prelim. Notice Lam. Shells, p. 64, syn. for P. radiata. parallela. Hall, 1883, Pal. N. Y., vol. 5, pi. 78, figs. 22-24, Ham. Gr. radiata, Conrad, 1842, (Nuculitesradiatus,) Jour. Acad. Nat. Sci., vol. 8, p. 248, and Pal. N. Y., vol. 5, pi. 78, figs. 15-21, Ham. Gr. truncata, Hall, 1870, Prelim. Notice Lam. Shells, p. 64, syn. for P. radiata. Pholadomya elongata, Stock Photo")
. North American geology and palaeontology for the use of amateurs, students, and scientists [microform]. Paleontology; Paleontology; Geology; Paléontologie; Paléontologie; Géologie. Fia. 891.—Pliolauella newberryi. omata, Hall, 1870, Prelim. Notice Lam. Shells, p. 64, syn. for P. radiata. parallela. Hall, 1883, Pal. N. Y., vol. 5, pi. 78, figs. 22-24, Ham. Gr. radiata, Conrad, 1842, (Nuculitesradiatus,) Jour. Acad. Nat. Sci., vol. 8, p. 248, and Pal. N. Y., vol. 5, pi. 78, figs. 15-21, Ham. Gr. truncata, Hall, 1870, Prelim. Notice Lam. Shells, p. 64, syn. for P. radiata. Pholadomya elongata, Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/north-american-geology-and-palaeontology-for-the-use-of-amateurs-students-and-scientists-microform-paleontology-paleontology-geology-palontologie-palontologie-gologie-fia-891pliolauella-newberryi-omata-hall-1870-prelim-notice-lam-shells-p-64-syn-for-p-radiata-parallela-hall-1883-pal-n-y-vol-5-pi-78-figs-22-24-ham-gr-radiata-conrad-1842-nuculitesradiatus-jour-acad-nat-sci-vol-8-p-248-and-pal-n-y-vol-5-pi-78-figs-15-21-ham-gr-truncata-hall-1870-prelim-notice-lam-shells-p-64-syn-for-p-radiata-pholadomya-elongata-image234822502.htmlRMRJ12DX–. North American geology and palaeontology for the use of amateurs, students, and scientists [microform]. Paleontology; Paleontology; Geology; Paléontologie; Paléontologie; Géologie. Fia. 891.—Pliolauella newberryi. omata, Hall, 1870, Prelim. Notice Lam. Shells, p. 64, syn. for P. radiata. parallela. Hall, 1883, Pal. N. Y., vol. 5, pi. 78, figs. 22-24, Ham. Gr. radiata, Conrad, 1842, (Nuculitesradiatus,) Jour. Acad. Nat. Sci., vol. 8, p. 248, and Pal. N. Y., vol. 5, pi. 78, figs. 15-21, Ham. Gr. truncata, Hall, 1870, Prelim. Notice Lam. Shells, p. 64, syn. for P. radiata. Pholadomya elongata,
. Bulletin de la Société géologique de Normandie.. Geology. 14. PHOTOCO LLOGRAPH1E I.ECEKF, ROUEN FOSSILES DE L'ASSISE DES CARREAUX 1 Ammonites bipartitus Ziet., fragment, 2 Ammonites? sp. ind. 3 Lima gibbosa Soie. 4 Pholadomya?... 5 Mytilus solenoïcles d'Orb. 6 Pholadomya clytia d'Orb. 7 Lima?..., stries fines sur les deux calt?es. 8 Pecten fibrosus Soie. 9 Isocardia tener Soio. 10, 13 Ostrea dilatata, jeune, De<h. 11 Mytilus gibbosns d'Orb 12 Plicatula catyloides Deslong. 14 Ammonites plicatilis Soio., fragment.. Please note that these images are extracted from scanned page images that ma Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-normandie-geology-14-photoco-llograph1e-iecekf-rouen-fossiles-de-lassise-des-carreaux-1-ammonites-bipartitus-ziet-fragment-2-ammonites-sp-ind-3-lima-gibbosa-soie-4-pholadomya-5-mytilus-solenocles-dorb-6-pholadomya-clytia-dorb-7-lima-stries-fines-sur-les-deux-caltes-8-pecten-fibrosus-soie-9-isocardia-tener-soio-10-13-ostrea-dilatata-jeune-delth-11-mytilus-gibbosns-dorb-12-plicatula-catyloides-deslong-14-ammonites-plicatilis-soio-fragment-please-note-that-these-images-are-extracted-from-scanned-page-images-that-ma-image234068909.htmlRMRGPN7W–. Bulletin de la Société géologique de Normandie.. Geology. 14. PHOTOCO LLOGRAPH1E I.ECEKF, ROUEN FOSSILES DE L'ASSISE DES CARREAUX 1 Ammonites bipartitus Ziet., fragment, 2 Ammonites? sp. ind. 3 Lima gibbosa Soie. 4 Pholadomya?... 5 Mytilus solenoïcles d'Orb. 6 Pholadomya clytia d'Orb. 7 Lima?..., stries fines sur les deux calt?es. 8 Pecten fibrosus Soie. 9 Isocardia tener Soio. 10, 13 Ostrea dilatata, jeune, De<h. 11 Mytilus gibbosns d'Orb 12 Plicatula catyloides Deslong. 14 Ammonites plicatilis Soio., fragment.. Please note that these images are extracted from scanned page images that ma
. Bulletin de la Société des sciences naturelles de l'Ouest de la France. Natural history -- France. 5'2 SOCIETE DES SCIENCES NATURELLES J>E L OUEST coiitiennent : Bel. tripartitus Blainv., Am. fGrammatocerasJ sparsicosta Haug., Lima electra d'Orb., Serpula segmentata E. Dumort., Pentacrinus Jurensis Quenst. Au-dessus vient la zone à Ostrea Beaumonti avec Bel. tripartitus Schloth., Bel. breviformis Voltz., Am. fLudwigiaJ Maclra Dumort., Pholadomya Zieteni Ag. Puis la zone à 7?/i. cynocephala avec Terebratula infra-ooiithica Desl., Gresslya pinguis Ag., Lima punctata Sow. sp. TRANCHÃE N' 3 Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-des-sciences-naturelles-de-louest-de-la-france-natural-history-france-52-societe-des-sciences-naturelles-jgte-l-ouest-coiitiennent-bel-tripartitus-blainv-am-fgrammatocerasj-sparsicosta-haug-lima-electra-dorb-serpula-segmentata-e-dumort-pentacrinus-jurensis-quenst-au-dessus-vient-la-zone-ostrea-beaumonti-avec-bel-tripartitus-schloth-bel-breviformis-voltz-am-fludwigiaj-maclra-dumort-pholadomya-zieteni-ag-puis-la-zone-7i-cynocephala-avec-terebratula-infra-ooiithica-desl-gresslya-pinguis-ag-lima-punctata-sow-sp-tranche-n-3-image234054155.htmlRMRGP2CY–. Bulletin de la Société des sciences naturelles de l'Ouest de la France. Natural history -- France. 5'2 SOCIETE DES SCIENCES NATURELLES J>E L OUEST coiitiennent : Bel. tripartitus Blainv., Am. fGrammatocerasJ sparsicosta Haug., Lima electra d'Orb., Serpula segmentata E. Dumort., Pentacrinus Jurensis Quenst. Au-dessus vient la zone à Ostrea Beaumonti avec Bel. tripartitus Schloth., Bel. breviformis Voltz., Am. fLudwigiaJ Maclra Dumort., Pholadomya Zieteni Ag. Puis la zone à 7?/i. cynocephala avec Terebratula infra-ooiithica Desl., Gresslya pinguis Ag., Lima punctata Sow. sp. TRANCHÃE N' 3
. Bulletin de la Société des sciences naturelles de l'Ouest de la France. Natural history -- France. 54 SOCIÃTà DES SCIENCES NATURELLES DE l'OUEST La zone à Am. radians (zone n° H), contient : Am. sparsicosta Haug. Avicula Milnsteri Goldf. Lima punctata Sow. Serpula segmentata Dumort. Les lits à Ostrea Beaumonti fournissent : Am. opalinus Reink. Trifjonia pulchella ? Ag. â aalensis Zieten. Ostrea sportella Dumort. Les calcaires à Rh, cynocephala contiennent : Am. opalinus Reink. Terebratula infra-oolithica E. Desl. Gresslya pinguis Ag. â conglobata E. Desl., à Pholadomya Hausmanni Goldf. la Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-des-sciences-naturelles-de-louest-de-la-france-natural-history-france-54-socit-des-sciences-naturelles-de-louest-la-zone-am-radians-zone-n-h-contient-am-sparsicosta-haug-avicula-milnsteri-goldf-lima-punctata-sow-serpula-segmentata-dumort-les-lits-ostrea-beaumonti-fournissent-am-opalinus-reink-trifjonia-pulchella-ag-aalensis-zieten-ostrea-sportella-dumort-les-calcaires-rh-cynocephala-contiennent-am-opalinus-reink-terebratula-infra-oolithica-e-desl-gresslya-pinguis-ag-conglobata-e-desl-pholadomya-hausmanni-goldf-la-image234054127.htmlRMRGP2BY–. Bulletin de la Société des sciences naturelles de l'Ouest de la France. Natural history -- France. 54 SOCIÃTà DES SCIENCES NATURELLES DE l'OUEST La zone à Am. radians (zone n° H), contient : Am. sparsicosta Haug. Avicula Milnsteri Goldf. Lima punctata Sow. Serpula segmentata Dumort. Les lits à Ostrea Beaumonti fournissent : Am. opalinus Reink. Trifjonia pulchella ? Ag. â aalensis Zieten. Ostrea sportella Dumort. Les calcaires à Rh, cynocephala contiennent : Am. opalinus Reink. Terebratula infra-oolithica E. Desl. Gresslya pinguis Ag. â conglobata E. Desl., à Pholadomya Hausmanni Goldf. la
. Bullettino. Mollusks; Mollusks; Mollusks, Fossil. — 292 — GENERI. Numero delle specie citate conservate Viventi nel Mediter- raneo Nello .... Neithea . . Nucinella . Nucula . . Nuculina. . Ostrea. . Pandora . . Panopoea. Pecchiolia . *. Pecten. . Pectunculus. Perna .... Petricola. . Pharus . Pholadidea . Pholadomya. Pholas. . Pinna.... Pisidium. . Placunanomia . Pleuronectia. Plicatula. . Polla .... Poronia , . , 149 91 139 139 139 55 37*9 345 3SO 94 138 104 316 330 349 383 349 105 319 74 93 •78 330 166 3 1 1 27 3 46 6 10 4 67 27 2 7 1 3 10 6 9 9 8 4 7 1 2. Please note that these images are Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bullettino-mollusks-mollusks-mollusks-fossil-292-generi-numero-delle-specie-citate-conservate-viventi-nel-mediter-raneo-nello-neithea-nucinella-nucula-nuculina-ostrea-pandora-panopoea-pecchiolia-pecten-pectunculus-perna-petricola-pharus-pholadidea-pholadomya-pholas-pinna-pisidium-placunanomia-pleuronectia-plicatula-polla-poronia-149-91-139-139-139-55-379-345-3so-94-138-104-316-330-349-383-349-105-319-74-93-78-330-166-3-1-1-27-3-46-6-10-4-67-27-2-7-1-3-10-6-9-9-8-4-7-1-2-please-note-that-these-images-are-image233724075.htmlRMRG71CB–. Bullettino. Mollusks; Mollusks; Mollusks, Fossil. — 292 — GENERI. Numero delle specie citate conservate Viventi nel Mediter- raneo Nello .... Neithea . . Nucinella . Nucula . . Nuculina. . Ostrea. . Pandora . . Panopoea. Pecchiolia . *. Pecten. . Pectunculus. Perna .... Petricola. . Pharus . Pholadidea . Pholadomya. Pholas. . Pinna.... Pisidium. . Placunanomia . Pleuronectia. Plicatula. . Polla .... Poronia , . , 149 91 139 139 139 55 37*9 345 3SO 94 138 104 316 330 349 383 349 105 319 74 93 •78 330 166 3 1 1 27 3 46 6 10 4 67 27 2 7 1 3 10 6 9 9 8 4 7 1 2. Please note that these images are
. Bulletin de la Socit des sciences naturelles de Sane-et-Loire. Natural history; Natural history -- France. â 46 III Sur la montagne de Beaune, au lieudit « en Pierre- Blanche », autour d'une fontaine, une couche marneuse blanc grisâtre rattachable à Toxfordien (zone à Cardioceras cordatum), et dans laquelle on trouve : Ostrea; Pholadomya exaltata; des Tiigonia plus ou moins fragmentés ; Perna mytiloïde^; Cidaris Jlorigemma et autres; Millericrinus, en fragments très nombreux; Belemnites hastaius, dont quelques fort beaux échantillons; des Polypiers, et notamment des ThamnastrÅa sur le Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-des-sciences-naturelles-de-sane-et-loire-natural-history-natural-history-france-46-iii-sur-la-montagne-de-beaune-au-lieudit-en-pierre-blanche-autour-dune-fontaine-une-couche-marneuse-blanc-gristre-rattachable-toxfordien-zone-cardioceras-cordatum-et-dans-laquelle-on-trouve-ostrea-pholadomya-exaltata-des-tiigonia-plus-ou-moins-fragments-perna-mytilode-cidaris-jlorigemma-et-autres-millericrinus-en-fragments-trs-nombreux-belemnites-hastaius-dont-quelques-fort-beaux-chantillons-des-polypiers-et-notamment-des-thamnastra-sur-le-image233797674.htmlRMRGAB8X–. Bulletin de la Socit des sciences naturelles de Sane-et-Loire. Natural history; Natural history -- France. â 46 III Sur la montagne de Beaune, au lieudit « en Pierre- Blanche », autour d'une fontaine, une couche marneuse blanc grisâtre rattachable à Toxfordien (zone à Cardioceras cordatum), et dans laquelle on trouve : Ostrea; Pholadomya exaltata; des Tiigonia plus ou moins fragmentés ; Perna mytiloïde^; Cidaris Jlorigemma et autres; Millericrinus, en fragments très nombreux; Belemnites hastaius, dont quelques fort beaux échantillons; des Polypiers, et notamment des ThamnastrÅa sur le
. Abhandlungen u. Bericht des Vereins für Naturkunde zu Kassel .... Verein für Naturkunde zu Kassel; Natural history. Tafel 1.. Fig. 1a, b. c. Pholadomya cf. Hausmanni 6oldF. Seiten-, Wirbel- und Hinteransicht. Arietenschichten. l/olkmarsen. S. iZ2. Fig. 2. Pinna sp. Stück eines Steini<erns i/on den l^irbeln gesehen. Lias y. Welda bei l^olkmansen. S.1Ze. Fig.3a,b. ? Anoplophora sp. Stein kern. Natürliche Grösse und eti^3 Znnal nat.Gr. Mittleren Keuper. Berge bei Hombeng a. £. S. 1Z3.. Please note that these images are extracted from scanned page images that may have been digitally enhanced Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/abhandlungen-u-bericht-des-vereins-fr-naturkunde-zu-kassel-verein-fr-naturkunde-zu-kassel-natural-history-tafel-1-fig-1a-b-c-pholadomya-cf-hausmanni-6oldf-seiten-wirbel-und-hinteransicht-arietenschichten-lolkmarsen-s-iz2-fig-2-pinna-sp-stck-eines-steinilterns-ion-den-lirbeln-gesehen-lias-y-welda-bei-lolkmansen-s1ze-fig3ab-anoplophora-sp-stein-kern-natrliche-grsse-und-eti3-znnal-natgr-mittleren-keuper-berge-bei-hombeng-a-s-1z3-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-image238050143.htmlRMRR83AR–. Abhandlungen u. Bericht des Vereins für Naturkunde zu Kassel .... Verein für Naturkunde zu Kassel; Natural history. Tafel 1.. Fig. 1a, b. c. Pholadomya cf. Hausmanni 6oldF. Seiten-, Wirbel- und Hinteransicht. Arietenschichten. l/olkmarsen. S. iZ2. Fig. 2. Pinna sp. Stück eines Steini<erns i/on den l^irbeln gesehen. Lias y. Welda bei l^olkmansen. S.1Ze. Fig.3a,b. ? Anoplophora sp. Stein kern. Natürliche Grösse und eti^3 Znnal nat.Gr. Mittleren Keuper. Berge bei Hombeng a. £. S. 1Z3.. Please note that these images are extracted from scanned page images that may have been digitally enhanced
![. Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen. Zoology. I. Siphoniata. 1009. Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten flaffeiib; ©djiofj mit flcinem 3^1^)"^; 2)?antelbud)t mà Stock Photo](https://c8.alamy.com/comp/REKWKF/dr-johannes-leunis-synopsis-der-thierkunde-ein-handbuch-fr-hhere-lehranstalten-und-fr-alle-welche-sich-wissenschaftlich-mit-der-naturgeschichte-der-thiere-beschftigen-wollen-zoology-i-siphoniata-1009-pholadomya-candida-eben-bic-hufe-lajipe-ticit-innen-unten-tic-vecte-lape-von-anfjcn-in-13-ber-natvl-@rije-9-pliolailoiiiya-sow-siien-tttudcl-@cloc-glcicltappig-bnn-mit-uon-bcn-aitvbclit-ausftvqfilcnbcn-9itppcn-unglcicl-=-feitig-qiiev-ouai-ober-rautenfrmig-aufijebltt-rillten-flaffeiib-djiofj-mit-flcinem-31quot-2antelbudt-m-REKWKF.jpg ". Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen. Zoology. I. Siphoniata. 1009. Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten flaffeiib; ©djiofj mit flcinem 3^1^)"^; 2)?antelbud)t mà Stock Photo")
. Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen. Zoology. I. Siphoniata. 1009. Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten flaffeiib; ©djiofj mit flcinem 3^1^)"^; 2)?antelbud)t mà Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/dr-johannes-leunis-synopsis-der-thierkunde-ein-handbuch-fr-hhere-lehranstalten-und-fr-alle-welche-sich-wissenschaftlich-mit-der-naturgeschichte-der-thiere-beschftigen-wollen-zoology-i-siphoniata-1009-pholadomya-candida-eben-bic-hufe-lajipe-ticit-innen-unten-tic-vecte-lape-von-anfjcn-in-13-ber-natvl-@rije-9-pliolailoiiiya-sow-siien-tttudcl-@cloc-glcicltappig-bnn-mit-uon-bcn-aitvbclit-ausftvqfilcnbcn-9itppcn-unglcicl-=-feitig-qiiev-ouai-ober-rautenfrmig-aufijebltt-rillten-flaffeiib-djiofj-mit-flcinem-31quot-2antelbudt-m-image232777203.htmlRMREKWKF–. Dr. Johannes Leunis Synopsis der thierkunde. Ein handbuch für höhere lehranstalten und für alle, welche sich wissenschaftlich mit der naturgeschichte der thiere beschäftigen wollen. Zoology. I. Siphoniata. 1009. Pholadomya Candida; eben bic Hufe Ãla^Jipe ticit innen; unten tic vec^te Ãlap^e Von anfjcn; in 1/3 ber natüvL @röije. 9. Pliolailoiiiya'^ Sow. Sii^^en- tttU)'d)Cl. @cl)o(c glcicl)t(appig, bünn, mit Uon bcn ai'tvbclit auSftvQfilcnbcn 9itppcn, unglcicl) = feitig, qiiev--ouaI ober rautenförmig, aufijeblät)t, Rillten flaffeiib; ©djiofj mit flcinem 3^1^)"^; 2)?antelbud)t mÃ
. Bulletin de la Société belge de géologie, de paléontologie et d'hydrologie. Geology; Paleontology. ET TRIASIQUE DES ENVIRONS D'ARLON ET DE FLORENVILLE i i3 vons dans le grès de Virton sous son faciès argileux. Il y est constitué par des marnes sableuses alternant avec des calcaires sablo-argileux, bleuâtres et grisâtres par altération. Les fossiles y sont nombreux : Belemnites clavatus* de Bl. Ammonites planicosta, Sow. Ammonites armatus, Sow. Pholadomya Hausmanni, Gold. GryphÅa cymbium, Lm. Nous sommes ici dans la zone à A. armatus ou à la base du Char- mouthien (voir tableau des Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-belge-de-gologie-de-palontologie-et-dhydrologie-geology-paleontology-et-triasique-des-environs-darlon-et-de-florenville-i-i3-vons-dans-le-grs-de-virton-sous-son-facis-argileux-il-y-est-constitu-par-des-marnes-sableuses-alternant-avec-des-calcaires-sablo-argileux-bleutres-et-gristres-par-altration-les-fossiles-y-sont-nombreux-belemnites-clavatus-de-bl-ammonites-planicosta-sow-ammonites-armatus-sow-pholadomya-hausmanni-gold-grypha-cymbium-lm-nous-sommes-ici-dans-la-zone-a-armatus-ou-la-base-du-char-mouthien-voir-tableau-des-image234062945.htmlRMRGPDJW–. Bulletin de la Société belge de géologie, de paléontologie et d'hydrologie. Geology; Paleontology. ET TRIASIQUE DES ENVIRONS D'ARLON ET DE FLORENVILLE i i3 vons dans le grès de Virton sous son faciès argileux. Il y est constitué par des marnes sableuses alternant avec des calcaires sablo-argileux, bleuâtres et grisâtres par altération. Les fossiles y sont nombreux : Belemnites clavatus* de Bl. Ammonites planicosta, Sow. Ammonites armatus, Sow. Pholadomya Hausmanni, Gold. GryphÅa cymbium, Lm. Nous sommes ici dans la zone à A. armatus ou à la base du Char- mouthien (voir tableau des
. Bulletin de la Société géologique de France. Geology. TERRAINS DU SEUIL DU POITOU 83l Lioceras (Graphoceras) V-scrip- Pholadomya lyrata Sow. tnin S. S. Buck. Ressopygiis Constantini Gott. Pygaster semisulcatus Ag. Trigonia sp. Lima Etheridgi Wright. Mytilus Sowerbyanus d'Orb. Modiota plicata Sow. Gryphsea sublobata Dehh. Terebratula sp. â sp. je citerai comme un point intéressant à visiter, montrant le passage du Toarcien au Bajocien la coupe de la Fontaine de Gabouret ' au nord-est de Lusignan. Le fond du vallon montre les marnes bleues du Lias supérieur, dont la teinte se prolonge jus Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-terrains-du-seuil-du-poitou-83l-lioceras-graphoceras-v-scrip-pholadomya-lyrata-sow-tnin-s-s-buck-ressopygiis-constantini-gott-pygaster-semisulcatus-ag-trigonia-sp-lima-etheridgi-wright-mytilus-sowerbyanus-dorb-modiota-plicata-sow-gryphsea-sublobata-dehh-terebratula-sp-sp-je-citerai-comme-un-point-intressant-visiter-montrant-le-passage-du-toarcien-au-bajocien-la-coupe-de-la-fontaine-de-gabouret-au-nord-est-de-lusignan-le-fond-du-vallon-montre-les-marnes-bleues-du-lias-suprieur-dont-la-teinte-se-prolonge-jus-image234059814.htmlRMRGP9K2–. Bulletin de la Société géologique de France. Geology. TERRAINS DU SEUIL DU POITOU 83l Lioceras (Graphoceras) V-scrip- Pholadomya lyrata Sow. tnin S. S. Buck. Ressopygiis Constantini Gott. Pygaster semisulcatus Ag. Trigonia sp. Lima Etheridgi Wright. Mytilus Sowerbyanus d'Orb. Modiota plicata Sow. Gryphsea sublobata Dehh. Terebratula sp. â sp. je citerai comme un point intéressant à visiter, montrant le passage du Toarcien au Bajocien la coupe de la Fontaine de Gabouret ' au nord-est de Lusignan. Le fond du vallon montre les marnes bleues du Lias supérieur, dont la teinte se prolonge jus
. Boletn de la Real Sociedad Espaola de Historia Natural. Real Sociedad Espaola de Historia Natural; Natural history; Natural history -- Spain. DE HISTORIA NATURAL. 213 dose, hasta desaparecer casi. Otro ejemplar de pequeño tama- ño, con una valva muy conVexa y de 15 costillas, ig-noro á qué especie pueda referirse; no falta tampoco un pequeño Chlamys en las capas superiores. El Sr. Nicklés cita la Ostrea Offreti Kil. como característica de las Atalayas, pero sin duda se encuentran además otras es- pecies. Los g-éneros Cardiiim, Venus, Pholadomya (una especie de g-ran tamaño), Lima, Spo7idyIns Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/boletn-de-la-real-sociedad-espaola-de-historia-natural-real-sociedad-espaola-de-historia-natural-natural-history-natural-history-spain-de-historia-natural-213-dose-hasta-desaparecer-casi-otro-ejemplar-de-pequeo-tama-o-con-una-valva-muy-convexa-y-de-15-costillas-ig-noro-qu-especie-pueda-referirse-no-falta-tampoco-un-pequeo-chlamys-en-las-capas-superiores-el-sr-nickls-cita-la-ostrea-offreti-kil-como-caracterstica-de-las-atalayas-pero-sin-duda-se-encuentran-adems-otras-es-pecies-los-g-neros-cardiiim-venus-pholadomya-una-especie-de-g-ran-tamao-lima-spo7idyins-image234545181.htmlRMRHGCNH–. Boletn de la Real Sociedad Espaola de Historia Natural. Real Sociedad Espaola de Historia Natural; Natural history; Natural history -- Spain. DE HISTORIA NATURAL. 213 dose, hasta desaparecer casi. Otro ejemplar de pequeño tama- ño, con una valva muy conVexa y de 15 costillas, ig-noro á qué especie pueda referirse; no falta tampoco un pequeño Chlamys en las capas superiores. El Sr. Nicklés cita la Ostrea Offreti Kil. como característica de las Atalayas, pero sin duda se encuentran además otras es- pecies. Los g-éneros Cardiiim, Venus, Pholadomya (una especie de g-ran tamaño), Lima, Spo7idyIns
![. Bulletin de la Société géologique de France. Geology. in MAURICE LKRrCHE PQ / pj i Bartonien sup. continkntal ^ (S' masse du Gypse). 1 H ] BaRTONIEI^I SUP. MARIN 1 s ] 5 / {Marnes « | 4- S y W l Pholadomya ludensis). i: ] (J / Bartonien inf. continental X^ 1 ^ {Calcaire de Noisy-le-Sec). « ^ ] Bartonien inf. marin â < 1 (Sables de Marines ^ et de Cresne). + l Ledien continental g {Marnes de Saint-Oiien). ^ ^ ^ 1 Leihen makin I ^ L ^ [ {Sables de Beauchamp). | « -[- « g; [ Lutétien continental I ^ ^ r. , S {Calcaire grossier supérieur). | g i Lutétien marin j =Y Stock Photo](https://c8.alamy.com/comp/RGMY9F/bulletin-de-la-socit-gologique-de-france-geology-in-maurice-lkrrche-pq-pj-i-bartonien-sup-continkntal-s-masse-du-gypse-1-h-bartonieii-sup-marin-1-s-5-marnes-4-s-y-w-l-pholadomya-ludensis-i-j-bartonien-inf-continental-x-1-calcaire-de-noisy-le-sec-bartonien-inf-marin-lt-1-sables-de-marines-et-de-cresne-l-ledien-continental-g-marnes-de-saint-oiien-1-leihen-makin-i-l-sables-de-beauchamp-g-luttien-continental-i-r-s-calcaire-grossier-suprieur-g-i-luttien-marin-j-=y-RGMY9F.jpg ". Bulletin de la Société géologique de France. Geology. in MAURICE LKRrCHE PQ / pj i Bartonien sup. continkntal ^ (S' masse du Gypse). 1 H ] BaRTONIEI^I SUP. MARIN 1 s ] 5 / {Marnes « | 4- S y W l Pholadomya ludensis). i: ] (J / Bartonien inf. continental X^ 1 ^ {Calcaire de Noisy-le-Sec). « ^ ] Bartonien inf. marin â < 1 (Sables de Marines ^ et de Cresne). + l Ledien continental g {Marnes de Saint-Oiien). ^ ^ ^ 1 Leihen makin I ^ L ^ [ {Sables de Beauchamp). | « -[- « g; [ Lutétien continental I ^ ^ r. , S {Calcaire grossier supérieur). | g i Lutétien marin j =Y Stock Photo")
. Bulletin de la Société géologique de France. Geology. in MAURICE LKRrCHE PQ / pj i Bartonien sup. continkntal ^ (S' masse du Gypse). 1 H ] BaRTONIEI^I SUP. MARIN 1 s ] 5 / {Marnes « | 4- S y W l Pholadomya ludensis). i: ] (J / Bartonien inf. continental X^ 1 ^ {Calcaire de Noisy-le-Sec). « ^ ] Bartonien inf. marin â < 1 (Sables de Marines ^ et de Cresne). + l Ledien continental g {Marnes de Saint-Oiien). ^ ^ ^ 1 Leihen makin I ^ L ^ [ {Sables de Beauchamp). | « -[- « g; [ Lutétien continental I ^ ^ r. , S {Calcaire grossier supérieur). | g i Lutétien marin j =Y Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-in-maurice-lkrrche-pq-pj-i-bartonien-sup-continkntal-s-masse-du-gypse-1-h-bartonieii-sup-marin-1-s-5-marnes-4-s-y-w-l-pholadomya-ludensis-i-j-bartonien-inf-continental-x-1-calcaire-de-noisy-le-sec-bartonien-inf-marin-lt-1-sables-de-marines-et-de-cresne-l-ledien-continental-g-marnes-de-saint-oiien-1-leihen-makin-i-l-sables-de-beauchamp-g-luttien-continental-i-r-s-calcaire-grossier-suprieur-g-i-luttien-marin-j-=y-image234029755.htmlRMRGMY9F–. Bulletin de la Société géologique de France. Geology. in MAURICE LKRrCHE PQ / pj i Bartonien sup. continkntal ^ (S' masse du Gypse). 1 H ] BaRTONIEI^I SUP. MARIN 1 s ] 5 / {Marnes « | 4- S y W l Pholadomya ludensis). i: ] (J / Bartonien inf. continental X^ 1 ^ {Calcaire de Noisy-le-Sec). « ^ ] Bartonien inf. marin â < 1 (Sables de Marines ^ et de Cresne). + l Ledien continental g {Marnes de Saint-Oiien). ^ ^ ^ 1 Leihen makin I ^ L ^ [ {Sables de Beauchamp). | « -[- « g; [ Lutétien continental I ^ ^ r. , S {Calcaire grossier supérieur). | g i Lutétien marin j =Y
![. Bulletin de la Société linnéenne de Normandie. Natural history; Natural history. Coupe géologique des carrières du four à chaux de Vimoutiers ( Orne) 1 m". Calcaire oolithique fragmenté en plaquettes jau- nâtres. ... 1"' ., » Calcaire gréseux ferrugineux jaune caverneux spa- th'que, corrodé par des émanations acides, avec polypiers, etc i"' 50 Gros bancs de calcaire oolithique blanc fissuré, avec nérinées, cidaris, etc., (pierre h chaux) 2°' 50 Gros bauc du calcaire oolithique blanc très-fissuré avec pholadomya, etc., (pierre à chaux) 2"' » â > Les fi Stock Photo](https://c8.alamy.com/comp/RGN2YH/bulletin-de-la-socit-linnenne-de-normandie-natural-history-natural-history-coupe-gologique-des-carrires-du-four-chaux-de-vimoutiers-orne-1-mquot-calcaire-oolithique-fragment-en-plaquettes-jau-ntres-1quot-calcaire-grseux-ferrugineux-jaune-caverneux-spa-thque-corrod-par-des-manations-acides-avec-polypiers-etc-iquot-50-gros-bancs-de-calcaire-oolithique-blanc-fissur-avec-nrines-cidaris-etc-pierre-h-chaux-2-50-gros-bauc-du-calcaire-oolithique-blanc-trs-fissur-avec-pholadomya-etc-pierre-chaux-2quot-gt-les-fi-RGN2YH.jpg ". Bulletin de la Société linnéenne de Normandie. Natural history; Natural history. Coupe géologique des carrières du four à chaux de Vimoutiers ( Orne) 1 m". Calcaire oolithique fragmenté en plaquettes jau- nâtres. ... 1"' ., » Calcaire gréseux ferrugineux jaune caverneux spa- th'que, corrodé par des émanations acides, avec polypiers, etc i"' 50 Gros bancs de calcaire oolithique blanc fissuré, avec nérinées, cidaris, etc., (pierre h chaux) 2°' 50 Gros bauc du calcaire oolithique blanc très-fissuré avec pholadomya, etc., (pierre à chaux) 2"' » â > Les fi Stock Photo")
. Bulletin de la Société linnéenne de Normandie. Natural history; Natural history. Coupe géologique des carrières du four à chaux de Vimoutiers ( Orne) 1 m". Calcaire oolithique fragmenté en plaquettes jau- nâtres. ... 1"' ., » Calcaire gréseux ferrugineux jaune caverneux spa- th'que, corrodé par des émanations acides, avec polypiers, etc i"' 50 Gros bancs de calcaire oolithique blanc fissuré, avec nérinées, cidaris, etc., (pierre h chaux) 2°' 50 Gros bauc du calcaire oolithique blanc très-fissuré avec pholadomya, etc., (pierre à chaux) 2"' » â > Les fi Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-linnenne-de-normandie-natural-history-natural-history-coupe-gologique-des-carrires-du-four-chaux-de-vimoutiers-orne-1-mquot-calcaire-oolithique-fragment-en-plaquettes-jau-ntres-1quot-calcaire-grseux-ferrugineux-jaune-caverneux-spa-thque-corrod-par-des-manations-acides-avec-polypiers-etc-iquot-50-gros-bancs-de-calcaire-oolithique-blanc-fissur-avec-nrines-cidaris-etc-pierre-h-chaux-2-50-gros-bauc-du-calcaire-oolithique-blanc-trs-fissur-avec-pholadomya-etc-pierre-chaux-2quot-gt-les-fi-image234032613.htmlRMRGN2YH–. Bulletin de la Société linnéenne de Normandie. Natural history; Natural history. Coupe géologique des carrières du four à chaux de Vimoutiers ( Orne) 1 m". Calcaire oolithique fragmenté en plaquettes jau- nâtres. ... 1"' ., » Calcaire gréseux ferrugineux jaune caverneux spa- th'que, corrodé par des émanations acides, avec polypiers, etc i"' 50 Gros bancs de calcaire oolithique blanc fissuré, avec nérinées, cidaris, etc., (pierre h chaux) 2°' 50 Gros bauc du calcaire oolithique blanc très-fissuré avec pholadomya, etc., (pierre à chaux) 2"' » â > Les fi
. Bulletin de la Société géologique de France. Geology. 1909 FAILLE DE TROIS-CHATELS 3o5 â 3. Des calcaires coralligènes blancs, près de la petite maisonnette qui est au bas du chemin de Croix ; a. Des marnes à Ostrea virgala; 5. Des calcaires blanchâtres compacts ; 6. Des marnes à Ptérocères, Pholadomya Protêt, Ceromya, Ostrea Briiatrutana ; 7. Des calcaires compacts; 8 Des marnes à Ostrea virgula; 9. Des calcaires compacts plus ou moins lâchetés; 10. T)çs mà Tues k Ostrea virgula qui sont vi>ibles avant d'arriver au fossé du fort, qui est à gauche du chemin; 11. Des calcaires Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-1909-faille-de-trois-chatels-3o5-3-des-calcaires-corallignes-blancs-prs-de-la-petite-maisonnette-qui-est-au-bas-du-chemin-de-croix-a-des-marnes-ostrea-virgala-5-des-calcaires-blanchtres-compacts-6-des-marnes-ptrocres-pholadomya-prott-ceromya-ostrea-briiatrutana-7-des-calcaires-compacts-8-des-marnes-ostrea-virgula-9-des-calcaires-compacts-plus-ou-moins-lchets-10-ts-m-tues-k-ostrea-virgula-qui-sont-vigtibles-avant-darriver-au-foss-du-fort-qui-est-gauche-du-chemin-11-des-calcaires-image234060586.htmlRMRGPAJJ–. Bulletin de la Société géologique de France. Geology. 1909 FAILLE DE TROIS-CHATELS 3o5 â 3. Des calcaires coralligènes blancs, près de la petite maisonnette qui est au bas du chemin de Croix ; a. Des marnes à Ostrea virgala; 5. Des calcaires blanchâtres compacts ; 6. Des marnes à Ptérocères, Pholadomya Protêt, Ceromya, Ostrea Briiatrutana ; 7. Des calcaires compacts; 8 Des marnes à Ostrea virgula; 9. Des calcaires compacts plus ou moins lâchetés; 10. T)çs mà Tues k Ostrea virgula qui sont vi>ibles avant d'arriver au fossé du fort, qui est à gauche du chemin; 11. Des calcaires
. Bulletin de la Société géologique de France. Geology. Ami. Soc. géol. du Nord, t. XXXVI, 1907, p. 370. FiG. 25. â La crayère de Chalons-sur-Vesle (Marne). Contact de la Craie et du Landénien. C, Craie de Reims, à Actinocamax quadratus ; M, Marne blanche, landénienne, à Ostrea eversa ; T, Tuffeau, à Ostrea eversa. et Pholadomya Konincki, avec, en a, banc de tuffeau compactât très dur. Descendue à Muizon, la Société traverse la Vesle, pviis gagne la crayère de Chà lons-sur-Vesle, qui montre la Craie de Reims,. Please note that these images are extracted from scanned page images tha Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-ami-soc-gol-du-nord-t-xxxvi-1907-p-370-fig-25-la-crayre-de-chalons-sur-vesle-marne-contact-de-la-craie-et-du-landnien-c-craie-de-reims-actinocamax-quadratus-m-marne-blanche-landnienne-ostrea-eversa-t-tuffeau-ostrea-eversa-et-pholadomya-konincki-avec-en-a-banc-de-tuffeau-compactt-trs-dur-descendue-muizon-la-socit-traverse-la-vesle-pviis-gagne-la-crayre-de-ch-lons-sur-vesle-qui-montre-la-craie-de-reims-please-note-that-these-images-are-extracted-from-scanned-page-images-tha-image234053783.htmlRMRGP1YK–. Bulletin de la Société géologique de France. Geology. Ami. Soc. géol. du Nord, t. XXXVI, 1907, p. 370. FiG. 25. â La crayère de Chalons-sur-Vesle (Marne). Contact de la Craie et du Landénien. C, Craie de Reims, à Actinocamax quadratus ; M, Marne blanche, landénienne, à Ostrea eversa ; T, Tuffeau, à Ostrea eversa. et Pholadomya Konincki, avec, en a, banc de tuffeau compactât très dur. Descendue à Muizon, la Société traverse la Vesle, pviis gagne la crayère de Chà lons-sur-Vesle, qui montre la Craie de Reims,. Please note that these images are extracted from scanned page images tha
![. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. Oh. XX.] OOLITIC STKATA. 413 in their turn, repose upon the lias in the south and west of England. Among the characteristic shells of the Inferior Oolite, I may instance Terebratula fimbria (fig. 425), Rhynchonella spinosa (fig. 426), and Pholadomya fidicula (fig. 427). The extinct genus Pleurotomaria is also a form very common in this division as well as in the Oolitic sys- tem generally^ It resembles the Trochus in form, but is marked by a deep cleft (a, fig. 428 a Stock Photo](https://c8.alamy.com/comp/RCHT8K/elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-geology-oh-xx-oolitic-stkata-413-in-their-turn-repose-upon-the-lias-in-the-south-and-west-of-england-among-the-characteristic-shells-of-the-inferior-oolite-i-may-instance-terebratula-fimbria-fig-425-rhynchonella-spinosa-fig-426-and-pholadomya-fidicula-fig-427-the-extinct-genus-pleurotomaria-is-also-a-form-very-common-in-this-division-as-well-as-in-the-oolitic-sys-tem-generally-it-resembles-the-trochus-in-form-but-is-marked-by-a-deep-cleft-a-fig-428-a-RCHT8K.jpg ". Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. Oh. XX.] OOLITIC STKATA. 413 in their turn, repose upon the lias in the south and west of England. Among the characteristic shells of the Inferior Oolite, I may instance Terebratula fimbria (fig. 425), Rhynchonella spinosa (fig. 426), and Pholadomya fidicula (fig. 427). The extinct genus Pleurotomaria is also a form very common in this division as well as in the Oolitic sys- tem generally^ It resembles the Trochus in form, but is marked by a deep cleft (a, fig. 428 a Stock Photo")
. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. Oh. XX.] OOLITIC STKATA. 413 in their turn, repose upon the lias in the south and west of England. Among the characteristic shells of the Inferior Oolite, I may instance Terebratula fimbria (fig. 425), Rhynchonella spinosa (fig. 426), and Pholadomya fidicula (fig. 427). The extinct genus Pleurotomaria is also a form very common in this division as well as in the Oolitic sys- tem generally^ It resembles the Trochus in form, but is marked by a deep cleft (a, fig. 428 a Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-geology-oh-xx-oolitic-stkata-413-in-their-turn-repose-upon-the-lias-in-the-south-and-west-of-england-among-the-characteristic-shells-of-the-inferior-oolite-i-may-instance-terebratula-fimbria-fig-425-rhynchonella-spinosa-fig-426-and-pholadomya-fidicula-fig-427-the-extinct-genus-pleurotomaria-is-also-a-form-very-common-in-this-division-as-well-as-in-the-oolitic-sys-tem-generally-it-resembles-the-trochus-in-form-but-is-marked-by-a-deep-cleft-a-fig-428-a-image231502899.htmlRMRCHT8K–. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. Oh. XX.] OOLITIC STKATA. 413 in their turn, repose upon the lias in the south and west of England. Among the characteristic shells of the Inferior Oolite, I may instance Terebratula fimbria (fig. 425), Rhynchonella spinosa (fig. 426), and Pholadomya fidicula (fig. 427). The extinct genus Pleurotomaria is also a form very common in this division as well as in the Oolitic sys- tem generally^ It resembles the Trochus in form, but is marked by a deep cleft (a, fig. 428 a
. Elements of geology. Geology. Fig. 212.. Terehratula spinosa. Inferior Oolite. a Pholadomya fidicula. Inferior Oolite. b Heart-shaped anterior termination of the same. * Fitton, Geol. Trans., Second Series, vol. iv. pi. 23, fig. 12.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lyell, Charles, Sir, 1797-1875; Gibbes, Lewis Reeve, 1810-1894, former owner. DSI; Merrill, George P. (George Perkins), 1854-1929, former owner Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/elements-of-geology-geology-fig-212-terehratula-spinosa-inferior-oolite-a-pholadomya-fidicula-inferior-oolite-b-heart-shaped-anterior-termination-of-the-same-fitton-geol-trans-second-series-vol-iv-pi-23-fig-12-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-lyell-charles-sir-1797-1875-gibbes-lewis-reeve-1810-1894-former-owner-dsi-merrill-george-p-george-perkins-1854-1929-former-owner-image231525094.htmlRMRCJTHA–. Elements of geology. Geology. Fig. 212.. Terehratula spinosa. Inferior Oolite. a Pholadomya fidicula. Inferior Oolite. b Heart-shaped anterior termination of the same. * Fitton, Geol. Trans., Second Series, vol. iv. pi. 23, fig. 12.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Lyell, Charles, Sir, 1797-1875; Gibbes, Lewis Reeve, 1810-1894, former owner. DSI; Merrill, George P. (George Perkins), 1854-1929, former owner
![. Elemente der paläontologie bearbeitet. Paleontology. I. Thierreich. —VII. Mollusca. — ».Klasse: Lamellibranchiata. Desraodonta. 241 A. Ligament Uusserlich. Schale dünn. Schlossrand ohne Zähne oder deutlich entwickelten Ligamentlöffel. Pholadomya Sow. (Fig. 234 A, B). Die dünnschalige, gleichklappige Muschel zeigt einen querovalen oder fast dreiseitigen Umriss. Die Wirbel der vorn und hinten klaffenden Sehale meist stark nach vorn gerückt und gegen einander gebogen [B]. Schlossrand gerade, zahnlos oder mit schwach ent- wickeltem Vorsprunge. Das Ligament liegt äusserlich. Häufig tren- nen 2 vo Stock Photo](https://c8.alamy.com/comp/RCXCKY/elemente-der-palontologie-bearbeitet-paleontology-i-thierreich-vii-mollusca-klasse-lamellibranchiata-desraodonta-241-a-ligament-uusserlich-schale-dnn-schlossrand-ohne-zhne-oder-deutlich-entwickelten-ligamentlffel-pholadomya-sow-fig-234-a-b-die-dnnschalige-gleichklappige-muschel-zeigt-einen-querovalen-oder-fast-dreiseitigen-umriss-die-wirbel-der-vorn-und-hinten-klaffenden-sehale-meist-stark-nach-vorn-gerckt-und-gegen-einander-gebogen-b-schlossrand-gerade-zahnlos-oder-mit-schwach-ent-wickeltem-vorsprunge-das-ligament-liegt-usserlich-hufig-tren-nen-2-vo-RCXCKY.jpg ". Elemente der paläontologie bearbeitet. Paleontology. I. Thierreich. —VII. Mollusca. — ».Klasse: Lamellibranchiata. Desraodonta. 241 A. Ligament Uusserlich. Schale dünn. Schlossrand ohne Zähne oder deutlich entwickelten Ligamentlöffel. Pholadomya Sow. (Fig. 234 A, B). Die dünnschalige, gleichklappige Muschel zeigt einen querovalen oder fast dreiseitigen Umriss. Die Wirbel der vorn und hinten klaffenden Sehale meist stark nach vorn gerückt und gegen einander gebogen [B]. Schlossrand gerade, zahnlos oder mit schwach ent- wickeltem Vorsprunge. Das Ligament liegt äusserlich. Häufig tren- nen 2 vo Stock Photo")
. Elemente der paläontologie bearbeitet. Paleontology. I. Thierreich. —VII. Mollusca. — ».Klasse: Lamellibranchiata. Desraodonta. 241 A. Ligament Uusserlich. Schale dünn. Schlossrand ohne Zähne oder deutlich entwickelten Ligamentlöffel. Pholadomya Sow. (Fig. 234 A, B). Die dünnschalige, gleichklappige Muschel zeigt einen querovalen oder fast dreiseitigen Umriss. Die Wirbel der vorn und hinten klaffenden Sehale meist stark nach vorn gerückt und gegen einander gebogen [B]. Schlossrand gerade, zahnlos oder mit schwach ent- wickeltem Vorsprunge. Das Ligament liegt äusserlich. Häufig tren- nen 2 vo Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/elemente-der-palontologie-bearbeitet-paleontology-i-thierreich-vii-mollusca-klasse-lamellibranchiata-desraodonta-241-a-ligament-uusserlich-schale-dnn-schlossrand-ohne-zhne-oder-deutlich-entwickelten-ligamentlffel-pholadomya-sow-fig-234-a-b-die-dnnschalige-gleichklappige-muschel-zeigt-einen-querovalen-oder-fast-dreiseitigen-umriss-die-wirbel-der-vorn-und-hinten-klaffenden-sehale-meist-stark-nach-vorn-gerckt-und-gegen-einander-gebogen-b-schlossrand-gerade-zahnlos-oder-mit-schwach-ent-wickeltem-vorsprunge-das-ligament-liegt-usserlich-hufig-tren-nen-2-vo-image231691375.htmlRMRCXCKY–. Elemente der paläontologie bearbeitet. Paleontology. I. Thierreich. —VII. Mollusca. — ».Klasse: Lamellibranchiata. Desraodonta. 241 A. Ligament Uusserlich. Schale dünn. Schlossrand ohne Zähne oder deutlich entwickelten Ligamentlöffel. Pholadomya Sow. (Fig. 234 A, B). Die dünnschalige, gleichklappige Muschel zeigt einen querovalen oder fast dreiseitigen Umriss. Die Wirbel der vorn und hinten klaffenden Sehale meist stark nach vorn gerückt und gegen einander gebogen [B]. Schlossrand gerade, zahnlos oder mit schwach ent- wickeltem Vorsprunge. Das Ligament liegt äusserlich. Häufig tren- nen 2 vo
. Elemente der paläontologie bearbeitet. Paleontology. Fig. 233. Ligamentstützen einer desmodonten Mu- schel {iltja), A Oberrand der linken Klappe (rechts = vorn) mit dem nach innen gelichteten Löfi'el, welcher das Ligament trägt, ly = Vorderrand, inj. = Mittelleisteu, //(â = Hinterrand des Löffels. li Querschnitt durch die Wirbelgegend der beiden Klappen. U = Ligamentlöffel der linken Klappe; W = zurncltgebogener, fast ganz mit der Schale verwachsener Ligamentträger der rechten Klappe. Zwischen beiden das Ligament il). Fig. 234. Ã, B Pholadomya paucicosta Rö. Oxford (T. ä chailles). Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/elemente-der-palontologie-bearbeitet-paleontology-fig-233-ligamentsttzen-einer-desmodonten-mu-schel-iltja-a-oberrand-der-linken-klappe-rechts-=-vorn-mit-dem-nach-innen-gelichteten-lfiel-welcher-das-ligament-trgt-ly-=-vorderrand-inj-=-mittelleisteu-=-hinterrand-des-lffels-li-querschnitt-durch-die-wirbelgegend-der-beiden-klappen-u-=-ligamentlffel-der-linken-klappe-w-=-zurncltgebogener-fast-ganz-mit-der-schale-verwachsener-ligamenttrger-der-rechten-klappe-zwischen-beiden-das-ligament-il-fig-234-b-pholadomya-paucicosta-r-oxford-t-chailles-image231691374.htmlRMRCXCKX–. Elemente der paläontologie bearbeitet. Paleontology. Fig. 233. Ligamentstützen einer desmodonten Mu- schel {iltja), A Oberrand der linken Klappe (rechts = vorn) mit dem nach innen gelichteten Löfi'el, welcher das Ligament trägt, ly = Vorderrand, inj. = Mittelleisteu, //(â = Hinterrand des Löffels. li Querschnitt durch die Wirbelgegend der beiden Klappen. U = Ligamentlöffel der linken Klappe; W = zurncltgebogener, fast ganz mit der Schale verwachsener Ligamentträger der rechten Klappe. Zwischen beiden das Ligament il). Fig. 234. Ã, B Pholadomya paucicosta Rö. Oxford (T. ä chailles).
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