RMRR855K–. Abbildungen und Beschreibungen fossiler Pflanzen-Reste der palaeozoischen und mesozoischen Formationen. Paleobotany; Paleobotany. . 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.. Potonié, H. (Henry), 1857-1913; Preussische Geologische Landesanstalt. Berlin : In vertrieb bei der K. Geologischen Landesanstalt
RMMCR9JH–. Europäisch gebliebene Typen oligocener Gewächse. 1. Betula pulchella, Sap. — 2 bis 5. Carpmus cuspidata, Sap.: 2 bis 3, Blätter; 4 bis 5, Früchte. Fig. 67.
RMRHYG5Y–. Beitrag zur Paläontologie des Thüringer Waldes : Die Grauwacke des Bohlens und des Pfaffenberges bei Saalfeld, I. Fauna. Paleobotany. I â s =5 I $1 V », »^ *v '^1 ^ N "o «s % ^ 5; 55. 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.. Richter, Reinhard, 1813-1884. Dresden : Arnold
RMMCR9KM–. Verschiedene Formen oligo-cener Comptonien. 1 bis 5. Comptonia dryandraefolia, Brongn. — 6. C. obtusiloba, Hr. (Saint-Jean de Garguier). — 7. C. dryandroules, Ung. (Sotzka). — 8. C. Matlieroniana, Sap. (Armissan). ceen die Gattung Comptonia (Fig. 57) und einige Myrica, mit breitlinienförmigen, an den Rändern gezahnten Blättern. Einige wenig zahlreiche Eichen mit eckig gelappten, oben in eine Spitze auslaufenden Blättern, beginnen sich zu verbreiten. Die Ahorne werden weniger selten, manche Wasserpflanzen und namentlich die Wasserlilien und Nelumbos gewinnen an Mächtigkeit und Mannigfaltigkei
RMMCR9B3–. Homologe Formen miocener und oligocener Eichen. (Typen mit gezahnten Blättern). 1. Quercus cuneifolia, Sap. (Unteres Oligocen, Gargas). — 2. Q. armata, Sap. (Un- teres Aquitan, Armissan). — 3. (I. au/ecedens, Sap. (Oberes Eocen, Gypse von Aix).— 4. Q. mediterranen, Ung. (Unteres Miocen, Cuuii). — 5. Q. praecursor, Sap. (Unte- res l'lioeen, Meximieux). Klimas entstand in Europa durch die Verminderung der Dimen- sionen der Blattfläche die Section der Hex oder Chlorobalanus, die sich bis heute fortgepflanzt hat, freilich mit Veränderung ihrer Charaktere, indem sie je nach den Abwechslungen mehr
RMRR8555–. Abbildungen und Beschreibungen fossiler Pflanzen-Reste der palaeozoischen und mesozoischen Formationen. Paleobotany; Paleobotany. H. Potonek, Abbildungen u. Beschreibungen foss. Pflanzen. Lief. VI (1909). — 111. Lepidopteris stuttgardiensis. ? ?? " "?'??????'?""? ?? ??. '",,."; :V.i;-?x..'. '"'.•;?' T"'"' ;' ?VvSy^rÄ/iv f*% Ä., Gez. C. Tob kicke. A 2 5 ß M Fig. 1. Lepidopteris stuttgardiensis (Jaeg.) Schimp. « Keupersandstein: Stuttgart. A. Spindel mit Scheinfelderung und Resten diaphragma-artiger Fächerimg; F. 1. 0. ebenfalls mit Felderung. (Verg
RMPF6PNR–. Diatomées fossiles du Japon. Espèces marines & nouvelles des calcaires argileux de Sendaï & Yedo. Paleobotany. Diatomées Fossiles PI V.. ffiotoh,. 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.. Brun, Jacques, 1826-1908; Tempère, Joannes Albert, 1847-1926. Leipzig, Theodor Oswald Wigel, Leipzig
RMMEFEB8–. Die fossile Flora der Permischen Formation . 1—6. Nöggerathia Göpperti Eichw. — 7. Typba latifolia. - 8. Musa sapientou. — 8*. M. rosacea. — 9. Amomum granum Paradisi. — 10. Schizopteris neuropteroides Sepp-
RMRJ66FP–. The geological history of plants [microform]. Paleobotany; Paléobotanique. FiQ. b2.—Alethopteri8 grandis (Dawson). Middle coal-formation of Nova Scotia.. 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.. Dawson, J. W. (John William), Sir, 1820-1899. New York : D. Appleton
RMMCR9K2–. Oligocene Fächerpalme; mittlerer Theil eines Blattwedels. (Sehr verkleinert.) Sabal major, Ung. massiger Grösse, aber zwischen ihnen erhebt sein majestätisches Haupt Sabal major, dessen Blätter an Grösse und Schönheit den- jenigen der Schirmpalmen der Antillen (Sabal umbraculifera)
RMRJ66W7–. The geological history of plants [microform]. Paleobotany; Paléobotanique. THE ERIAN OR DEVONIAN FORESTS. 65. Fio. 20. — Sphe- iiophyllum nn- tiguHin (Erian, Is'ew BniiiBwiek), See pp. 61, C7. dichotomously, and covered with interrupted ridges. Leavoo rudimentary, or short, rigid, and pointed ; in barren stems, numerous and spirally arranged • in fertile stems and brauchlets, sparsely scattered or absent; in decorticated specimens, represented by a minute punctate scars. Young branch- es circinate ; rhizomata cylindrical, cov- ered with hairs or ramenta, and having circular areoles irregular
RMPF6PPC–. Diatomées fossiles du Japon. Espèces marines & nouvelles des calcaires argileux de Sendaï & Yedo. Paleobotany. Diatomées Fossiles PI. I.. hototypie F.TAcpoi À ( '". i-'.-'fs-.. 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.. Brun, Jacques, 1826-1908; Tempère, Joannes Albert, 1847-1926. Leipzig, Theodor Oswald Wigel, Leipzig
RMMCR9PM–. Palaeocenes Farnkraut des Waldes von Baumfarn von Sezanne (Stück eines Gelinden (Spitze eines Blattwedels). Blattwedels). Osmunda eocenica, Sap. und Mar. Alsophila thelypteroides, Sap.
RMRJ4KGC–. On new plants from the Erian and Carboniferous [microform] : and on the characters and affinities of paleozoic gymnosperms. Paleobotany; Paléobotanique. .1 i. PsTSft Bedpath Musbuh, MoGtll Uniybesitt, Montbkal, NoTBs ON Speoimbns, 1890. On New Plants from the Ebian and Oabbonif- EBOus, and on the Chabaotebs and Affinities of PAKfflozoio Gymnospebms.' By Sib J. Wiluam Dawbon, L.L.D., F.R.8. In Palffio-botany it often happens that some specimen recently discovered opens up a multitude of new questions respecting former acquisitions. A noteworthy instance of this in my recent experience, has be
RMPF6PN9–. Diatomées fossiles du Japon. Espèces marines & nouvelles des calcaires argileux de Sendaï & Yedo. Paleobotany. imées fossiles PI VI iel. 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.. Brun, Jacques, 1826-1908; Tempère, Joannes Albert, 1847-1926. Leipzig, Theodor Oswald Wigel, Leipzig
RMMCR9TB–. Charakteristische Pflanzen der Cenoman-Kreide Amerikas (Dakotagruppe): — Primi- tive Dicotyledonen. 1. Fagus polyclada, Lqx., Blatt. — 2. Platanus primaeva, Lqx., Blatt. — 3. Quer- cus (Caslanea?) primordiales, Lqx., Blatt. bemerkt in dieser Flora, deren Kenntniss wir''[den gelehrten Forschungen von Lesquereux verdanken, die Gegenwart der Platane, der Buche, einer Eiche oder eines Kastanienbaums, eines Epheu's u. s. w., und wenn man keine Crednerien findet, wie in Europa, so trifft man an deren Platz zwei Typen an, Protophyllum und Aspidiophyllum, welche ihre charakteristischen Züge zeigen u
RMRJ6653–. The geological history of plants [microform]. Paleobotany; Paléobotanique. LATER CRETACEOUS AND KAINOZOIC. 195 ami leaves of carices and grasses, so that these i)lants, now so importiint to the nourishment of man and his com- panion animals, were already rei)resented.. Fio. 70.—Vegetation of Later Cretnceoua. Exogens and palms. (Atlor Saporta.) But the great feature of the time was its dicotyle- donous forests, and I have only to enumerate the genera supposed to be represented in order to show the richness of the time in plants of this type. It may be necessary to explain here that th generi
RMPF6PMT–. Diatomées fossiles du Japon. Espèces marines & nouvelles des calcaires argileux de Sendaï & Yedo. Paleobotany. Diatomées foss les PI.VTttK. Pkolotypie F. 'f/teees âr. 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.. Brun, Jacques, 1826-1908; Tempère, Joannes Albert, 1847-1926. Leipzig, Theodor Oswald Wigel, Leipzig
RMMCR9K6–. Charakteristische Typen verschiedener oligocener Gewächse. 1 bis 2. Myrsine celastroides, EU. — 3. 31. euneata, Sap. — 4. Celastrus splendidus, Sap. — 5. C. Zachariensis, Sap. — 6. Hex celastrina, Sap. — 7. Andromeda neglecta, Sap. — 8. Diospyros varians, Sap. — 9. Zizyphus Ungeri, Ett. — 10. il/?/r- iws rectinervis, Sap. — 11. üf. caryopihylloides, Sap. Mar. (Fig. 65) und Acacien (A. Bousqueti, Sap., A sotzläana, Ung.). Alle diese Arten leiten die Analogie in diesem Labyrinth von Formen, die zugleich sehr mannigfaltig und doch nach einem gemeinschaftlichen Modelle hergestellt erscheinen, so
RMREWP3B–. On the genus Lepidophloios [microform] : as illustrated by specimens from the coal formation of Nova Scotia and New Brunswick. Paleobotany; Paleobotany; Paléobotanique; Paléobotanique. ay thus Ihj e loaf-base, 0 former is r condition OS of Corda. will appear V) ,AR()KI>. fforded to me I described in re since been Iness of Prof iparently of a • flattened, its id with clay- rkings of the is scarcely an ire preserved, Y occupied by last is a ring Bsue, about a g to what has [UH J. w. DAWiON] ON THE GENUd LEP1D0PHL0I08 61 in similar stems been regarded as an equivalent of corky bark. This tis
RMPF6PN7–. Diatomées fossiles du Japon. Espèces marines & nouvelles des calcaires argileux de Sendaï & Yedo. Paleobotany. Dialomées fo ssifes ^1 }. j |. 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.. Brun, Jacques, 1826-1908; Tempère, Joannes Albert, 1847-1926. Leipzig, Theodor Oswald Wigel, Leipzig
RMMCR9RH–. Palaeocene Helleboree (?) des Waldes von Gelinden. Dewalquea Gelindenensis, Sap. und Mar. Fig. 39. Fig. 40.
RMRJ66WP–. The geological history of plants [microform]. Paleobotany; Paléobotanique. Fio. 17.—I^tilophijton jtiumoaum (Lower Carboniferous, Nova Scotia). ^Natural size and muguiiied. A second type of plant, which may have been Rhizo- carpean in its affinities, is that to which I have given the name Ptilopliyton. It consists of beautiful feathery * "Journal of the Geological Society," 1865. f Flumalina of Hall. ifi. 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
RMPF6PP4–. Diatomées fossiles du Japon. Espèces marines & nouvelles des calcaires argileux de Sendaï & Yedo. Paleobotany. Diatomées fossiles. r//.'/,>tr/nir I. 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.. Brun, Jacques, 1826-1908; Tempère, Joannes Albert, 1847-1926. Leipzig, Theodor Oswald Wigel, Leipzig
RMMCR9NN–. Ollelia paridensis, Sap.
RMRHY8CN–. On the genus Lepidophloios [microform] : as illustrated by specimens from the coal formation of Nova Scotia and New Brunswick. Paleobotany; Paleobotany; Paléobotanique; Paléobotanique. -SMa{^%av'„..ii«*'i,. 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.. Dawson, J. W. (John William), Sir, 1820-1899; Royal Society of Canada. Montreal : [s. n. ]
RMPF6PMG–. Diatomées fossiles du Japon. Espèces marines & nouvelles des calcaires argileux de Sendaï & Yedo. Paleobotany. . 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.. Brun, Jacques, 1826-1908; Tempère, Joannes Albert, 1847-1926. Leipzig, Theodor Oswald Wigel, Leipzig
RMMEFEK8–. Die fossile Flora der Permischen Formation . 1—4. Dictyothalamus Schrollianus Göpp.
RMRJ4KFB–. On new plants from the Erian and Carboniferous [microform] : and on the characters and affinities of paleozoic gymnosperms. Paleobotany; Paléobotanique. DfWalchia, also with eriarium.) the paper nade addi- ?ecially on places on ai-d Island, ent to the »wa, and vith draw- Mr. Bain's 1 show the and woody le external >s indicate with the fy branch- rm which, irds as be- erences in in greater f the long, furrowed md in the jed nodes es. This and ap- lin diflfer- ood. esent the )ecimens kS in the kings Of r surface e medul- )rse dia- 11 phragms characteristic of Sternbergia. In other examples
RMPF6PN3–. Diatomées fossiles du Japon. Espèces marines & nouvelles des calcaires argileux de Sendaï & Yedo. Paleobotany. Diatomées fossiles PI.VII / /. i .. 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.. Brun, Jacques, 1826-1908; Tempère, Joannes Albert, 1847-1926. Leipzig, Theodor Oswald Wigel, Leipzig
RMMCR9D5–. Charakteristische mio-pliocene Arten von Senigaglia. 1. bis 2. Salisburiu adiantoides, Ung. — 3. bis 4. Sassafras Ferretianum, Massal. — o. Acer Curnaliae, Massal, duiße Arten und viele andere, die man aufzählen könnte, lebten nicht nur in Europa über die Mioeenperiode hinaus fort, in welcher *) Man beachte unter den Fig. 101 abgebildeten Arten von Senigaglia die beiden Eichen, Querem Fallopiana und Cornaliae. Die erstere Art gehört zum Typus unserer Steineiche, Qu. robur; Qu. Cornaliae dagegen schliesst sich sehr nahe der Qu. infectoria an. Acer Cornaliae (Fig. 100, 5) gehört ohne Zweifel z
RMRR8547–. Abbildungen und Beschreibungen fossiler Pflanzen-Reste der palaeozoischen und mesozoischen Formationen. Paleobotany; Paleobotany. 4 T Ge& G. Jonrs.. Gez. C. TÖBEICKE. Fig. 2. Lonchopteris Bricei. Vorkommen wie Fig. 1. S. B.1.. 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.. Potonié, H. (Henry), 1857-1913; Preussische Geologische Landesanstalt. Berlin : In vertrieb bei der K. Geologischen Landesanstalt
RMMCRA22–. Primordiale Landpflanzen, von Lesquereux im Obersilur Amerikas beobachtet. 1. Psilophyton cornutum, Lqx. — 2. bis 4. Sphenopliyllum primaevum, Lqx. — 5. An- nularia Romingeri, Lqx. — 6. I'rotostigma sigillaroides, Lqx. unbestimmte Charaktere zu besitzen und sich durch die Hymeno- phylleen den Farnen, durch Psilotum den Bärlappen und durch Pilularia den Rhizocarpeen zu nähern. Die beinahe nackten und durch successive Gabeltheilung verästelten Stämme von Psilo- phyton, die bei ihrer Entwicklung wie ein Bischofstab eingerollt waren, Hessen dünne, mit kleinen einfachen, mehr oder minder lederart
RMRJ66AT–. The geological history of plants [microform]. Paleobotany; Paléobotanique. TliE FLORA. OF THE EARLY MESOZOIC. 177 As we ascend, Jiowever, in the Mesozoic, we find new and higher types. Even within the Jurassic epoch, the next in succession to the Trias, there are clear indica- tions of tlie presence of the cndogens, in species allied to. Fia. 6-i.—Jurassic vegetation. Cycads and pines. (After Saporta.) the screw-pines and grasses ; and the palms appear a little later, while a few exogenous trees have left their remains in the Lower Cretaceous, and in the Middle and Upper Cretaceous these hig
RMMEFEHF–. Die fossile Flora der Permischen Formation .
RMRJ68KJ–. Notes on the North American species of dadoxylon [microform] : with special reference to type material in the collections of the Peter Redpath Museum, McGill University. Paleobotany; Paléobotanique. [r^KMiAiinu 1 Noirni .Mi;i;ic.. si'i;(ii;s oi- l^l'(l.^•|,(l^• S9. I'K:. !I. —fiiHHAtlCS I'liA.Mil.lM.M X ISII.. 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.. Penhallow, D. P. (David Pearce), 1854-1910; Royal Society of
RMMCR9M8–. Charakteristische Arten aus den Gypsen von Aix. 1 bis 2. Cards antiqua, Sap.; Eocener Judasbaum (l, Blatt; 2, Schote). Schoten verschiedener Arten von Gummibäumen (Acacia). 3 bis 7. Bei weiterem Vordringen in das Innere des Landes würde man sich in Waldgegenden gefunden haben, welche durch ihr An- sehen und die Vergesellschaftung der Pflanzenformen den Gehöl- zen ähnlich gesehen hätten, die heute in Innerafrika existiren. Die Gummibäume (Acacia) herrschen augenscheinlich vor. Man hat etwa ein Dutzend Arten entdeckt, die an ihren Früchten und Blättchen leicht erkennlich sind. Unsere Abbildung
RMRJ66G4–. The geological history of plants [microform]. Paleobotany; Paléobotanique. 1; i! I |i i II 12G TUE GEOLOGICAL HISTORY OF PLANTS. of fossil ferns, in wliich the fructification is for the most part wanting, it is still more so, depending in great part on the form and venation of the divisions of the fronds.. Fio. 51.—Group of coal-formation ferns, a, Odontopteris suhcuneata (Bnu- bury). B, Neuropteria cordata (Brongniart). c, Alethopteris lonc/dtica (Brongrniart). d, Dicti/opteris obiiqud I Hunhury), e, Phyllopteris an- tiqua (Dawson), magnified; e>, Natural size, f, H'europteris cyclopte-
RMMCR9BX–. Charakteristische Arten der plioeenen Tuffe von Meximieux. 1. Adiantum reniforme, L. — 2 bis 4. Bambusa lugdunensis, Sap.: 2, ausgewachse- nes Rohrstück; 3, 4 Blätter. — 5, 6. Quercus p>raecursor, Sap.: 5, Blatt; 6, Eichel ohne Hülle. doch mit unterscheidenden Nuancen, die um so merkwürdiger er- scheinen, da sie ebenso erkenntlich, als wenig auffallend sind. Die Schlingpflanzen zeigten eine Waldrebe (CJemat/s) und eine Menispermee (Cocciilus) mit nordamerikanischer Verwandtschaft. Ein dem heutigen fast gleicher Oleander und ein dem plio- eenen Europa eigenthümlicher Granatbaum (Punicü Pla
RMMCR9B8–. AiUmi aus dem Forest-bed. (Oberes Pliocen.) 1 bi> 2. Pinus montana, Mitt., Zapfen. — 3 bis 4. Abies pectinata, D. C., abge- löste Zapfen-Schuppen. einigt war. Professor Heer, der in London dieselben Pflanzen- reste untersucht hat, erwähnt noch die Bergfichte (Pinus mon- tana, MilL, Fig. 112, Ibis 2), den gemeinen Eibenbaum, den Hasel- nussstrauch, die Eiche und mehrere Wasserpflanzen, darunter die
RMRHYDTY–. Beiträge zur Kenntniss der Kreideflora Australiens. Paleobotany -- Tertiary; Paleobotany -- Australia. e.V. Ettingshausen: Beiträge zur Kreidefloia Australiens. Taf. DI.. „ilh uIp:.!^ i?i .r. :>u-.:e;:;ersWe-4P«Svi}u3.Gra2 Denkschriftend.k.Akadd.VV.math.naturw. Classe Bd. LXIE.. 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.. Ettingshausen, Constantin, Freiherr von, 1826-1897. Wien, Staatsdruckerei
RMMCR9WM–.
RMRJ6629–. The geological history of plants [microform]. Paleobotany; Paléobotanique. THE TERTIARY TO THE MODERN PERIOD. 229 abundant on the shores of the Great Slave Lake and on tlie McKenzie River, and according to Richardson con- stitutes much of the drift timber of the Arctic coast (Fig. 78). 6. Thuja occidentalis, Linn. Trunks and branches in the Leda clay at Montreal. This tree occurs in New England and Canada, and extends northward into the. Fig. 78.—Populus balsami/era. Pleistocene, Canada. Hudson Bay territories. It is a northern though not arctic species in its geogra})hical range. According
RMMEJXW7–. Die alttertiäre Flora von Messel bei Darmstadt .
RMRR858B–. Abbildungen und Beschreibungen fossiler Pflanzen-Reste der palaeozoischen und mesozoischen Formationen. Paleobotany; Paleobotany. 2 — Filicites frogills Schlotheim zum Teil, Petrefactenkünde 1820, S. 408. Abbildung in »Flora der Vorwelt« 1804, Taf. X, Fig. 17. (Hier ohne wissensch. Namen.) Sphenopteris fragilis Brongniart, Prodrome 1828, p. 51. » Gravenhorstii Brongniart, 1. c, p. 51 und Histoire 1829, p. 191, Taf. LV, Fig. 3. Gleiehenites Linkii Göppert, foss. Farne 1836, p. 182, Taf. 2, Fig. 1. Calymmotheca Linkii Stur zum Teil, Culmflora II, 1877, p. 267 (161), Taf. XII (XXIX), Fig. 1-4.
RMMCR9CA–.
RMRHY8BF–. On the genus Lepidophloios [microform] : as illustrated by specimens from the coal formation of Nova Scotia and New Brunswick. Paleobotany; Paleobotany; Paléobotanique; Paléobotanique. . 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.. Dawson, J. W. (John William), Sir, 1820-1899; Royal Society of Canada. Montreal : [s. n. ]
RMMCRA2A–. ^® Charakteristische devonische Pflanzen aus Canada. 1. Calamodendron ieiiuistriatttm, Dn., Stück eines Stammes. — 2. ßornia transitionis, Goepp., Stamm mit Blättern. — 3. Aslerophyllites latifoUa, Dn. — 4. bis 5. Annu- laria laxa, Dn. Blättern besetzt, die wie Tannennadeln schmal, aber durch Dicho- tomie in mehrere Segmente getheilt waren. Dem Ansehen nach waren es riesige Schafthalme; aber ihre höhere innere Organisation
RMMCR9B7–. Charakteristische Arten des jüngeren Pliocen der Auvergne und Italiens. 1. Quercus Mirbechii antiqua, Sap. (Auvergne). — 2, Quercus Lamoltü, Sap., (Auv.). — 3. Quercus roburoides, Gaud. (Massa-Maritima). — 4. Quercus Hex, L. (Lipari). — 5. Fagus sylvatica, L. (Oberes Arnothal). — 6. Vibumum tinus, L. (Toscanische Travertine). — 7. Vitis vinlfera L. (Travertine von Era). — 8. Mespilus pyracantha L. (Travertine von Toscana).
RMRHYDWF–. Beiträge zur Kenntniss der Kreideflora Australiens. Paleobotany -- Tertiary; Paleobotany -- Australia. e.V. EUingshauseit: Beiträge zur Ivj-eideflora Australiens. Tai: ü.. Denkschriften d k.Akad.d.W. math.natunv. Classe Bd. LXII. Tiier'EWe sPresuhii.O.-A::. 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.. Ettingshausen, Constantin, Freiherr von, 1826-1897. Wien, Staatsdruckerei
RMMCR9TE–. Charakteristische Pflanzen der Senon-Kreide des Harzes: — Primitive Dicotyledonen. 1. Credneria triucumiuata, Hampe, Blatt. — 2. Abieütes curvifolius, Dkr., Zweig. — 3. Dryophyllum Hausmanni, Dkr., f'euille. gehen. Die Blätter dieser seltsamen Gattung sind häufig zusam- mengerollt, wie wenn sie sich von selbst von dem Stengel losgelöst hätten, der sie trug, und dann in den Sand oder Schlamm fort- geschwemmt worden wären; man hat sie nicht nur in Böhmen und Sachsen, sondern auch bei Blankenburg im Harz, in Westphalen, Aachen und bis nach Nordgrönland gefunden. Die Gattung, der diese Blätter a
RMRJ66G9–. The geological history of plants [microform]. Paleobotany; Paléobotanique. Fio. 50.—Stems of CalamoJendron and tissues magnified (Nova Scotia), a, 6, Casts of axis in sandstone, with woody envelope (reduced). c, d, Woody tissue (highly magnified). their affinities with modern forms ; but the knowledge of this subject has been constantly extending, and a suffi- cient amount of information has been obtained to enable us to say something as to their probable relationships. (Figs. 51 to 55.) The families into which modern ferns are divided are, it must be confessed, somewhat artificial, and in t
RMMCR9XC–.
RMRJ66PD–. The geological history of plants [microform]. Paleobotany; Paléobotanique. THE BRIAN OR DEVONIAN FORESTS. 79 folk Island pine, than that of the modern yews. These trees are chiefly known to us by their mineralised trunks, which are often found like drift-wood on modern sand- banks embedded in the Erian sandstones or limestones. It often shows its structure in the most perfect man- ner in specimens penetrated by calcite or silica, or by pyrite, and in which the original woody matter has. Please note that these images are extracted from scanned page images that may have been digitally enhanced
RMMEFERY–. Die fossile Flora der Permischen Formation . I. Calamites leioderma Gutb. â 2. 'â '>. Asterophyllites clatior Göpp. â 4. Huttonia huricnta Göpp. â â¢">. <'. Huttonia eqnisetiformis Göpp. 'Lithogr. ii. Druck r JA, Fischer in lasse/.
RMRHYDRT–. Beiträge zur Kenntniss der Kreideflora Australiens. Paleobotany -- Tertiary; Paleobotany -- Australia. e.V. Ktlingshaiison; Hoiträge zur Kreideflora .Aiistrnlions Taf.I-.. Ijüi.ü.Druck bei Th,Schneiders We SPresuhr..Gras Denkschriften dk.Akad.d.Vmath.naturw. Classe Bd. LXIT.. 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.. Ettingshausen, Constantin, Freiherr von, 1826-1897. Wien, Staatsdruckerei
RMMCR9BA–. Charakteristische Arten des südlichen Frankreichs aus der Zeit des Elephas meridio- nalis. 1. Pinus caroliniana, Carr. , Zapfen (Saint-Martial). — 2 bis 3. Quercus Farnetto, Ten. — 4 bis 5. Quercus lusitanica, Webb. — 6. Parrotia pristina, Ett. Spanien und Portugal identisch gefunden. Die in Südfrankreich damals herrschenden Formen sind also seitdem ausgewandert; sie Saporta, die Pflanzenwelt,. 22
RMRJ0J6G–. Flora fossilis Alaskana [microform] = Fossile Flora von Alaska. Paleobotany; Paléobotanique. ||J tf.i i;l.l ^ilrlil Sll.il.,1' r MII N " '? iK» ii..r liuiM .ii.iA r.ii> y. Imu- 1 l'linils |)llinilfIAi;l '1 ri.llicr;! Timm 11 - 7 lioliil;! ii|i,>..i ft lirliiLi ^-JMJHliruh.l !' .li'.iis KVli r-,lnini v.ii' III llmirii^ Kiiiiili|i>|jiii.. 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.. Heer, Oswald, 1809-18
RMMEFEPE–. Die fossile Flora der Permischen Formation . At Assmann 7^* I. 2. Xouropteris imbricata Gripp. — 3. i. F'phenopteiis integra Göpp. Lilhoyr
RMRJ66YH–. The geological history of plants [microform]. Paleobotany; Paléobotanique. I H I. U^ T 34 THE GEOLOGICAL HISTORY OF PLANTS. and which sometimes communicates to them a marvellous resemblance to the netted under surface of an exogenous leaf. Flattened stems of plants and layers of cortical matter, when carbonised, shrink in such a manner as to produce minute reticulated cracks. These become filled with mineral matter before the coaly substance has been completely consolidated. A further compression occurs, causing the coaly substance to collapse, leaving the little veins of harder mineral matt
RMMCR9J1–. "t" Anaectomeria Broiujniartü, Sap. (Armis- san). Reife Fracht im Augenblicke des Autplatzens.
RMRHY89D–. On the genus Lepidophloios [microform] : as illustrated by specimens from the coal formation of Nova Scotia and New Brunswick. Paleobotany; Paleobotany; Paléobotanique; Paléobotanique. [wp J. w. DAWMON) Thanh. 18117. Sec. IV.—I'iatb VII. ON TUK (iKNUS I.EI'IDOI'IILOIOS. ffip-v*-. i. 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.. Dawson, J. W. (John William), Sir, 1820-1899; Royal Society of Canada. Montreal : [s. n. ]
RMMCR9JC–.
RMRR854A–. Abbildungen und Beschreibungen fossiler Pflanzen-Reste der palaeozoischen und mesozoischen Formationen. Paleobotany; Paleobotany. lonchopteris und Lonchoptendium; diese Zweiteilung, die wir oben auf Grund der Aderungseigentümlichkeiten vorgenommen hatten, erweist sich auch hinsichtlich der Verbreitung fruchtbar, und auch im geologischen Vorkommen scheinen die beiden Gruppen Eigen- tümlichkeiten zu bieten, insbesondere insofern, als Angehörige der Lonchopteridtum sich z. T. in tieferen Schichten finden als die Eulonchopteris, eine Tatsache, die phylogenetische Bedeutung hat. Wie sich aus dies
RMMCRA2N–. Marine Urpflanzen. 1. BilSbites rugosa (Cruzmna rugosa d'Orb.). Unterer Theil oder Sockel eines Blatt- standes (Silurschichten der Sierra von Algarre). — 2. Harlania Hallii, Goepp. (Obersilur), Theil eines Blattstandes mit Verästelungen. und in derselben Ebene liegen, in eine wellige Ausbreitung über- geht, die am Rande nur undeutlich begrenzt, aber von bedeuten- der Grösse ist. Auf dem Blatte der Bilobiten, dessen Durch- messer in der Gegend seiner grössten Breite gewiss mehrere Fuss betrug, zeigen sich viele wellige, schief gerichtete Rinnen, welche die ganze Oberfläche des Phylloms bede
RMRR853R–. Abbildungen und Beschreibungen fossiler Pflanzen-Reste der palaeozoischen und mesozoischen Formationen. Paleobotany; Paleobotany. A. 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.. Potonié, H. (Henry), 1857-1913; Preussische Geologische Landesanstalt. Berlin : In vertrieb bei der K. Geologischen Landesanstalt
RMMEFEJ4–. Die fossile Flora der Permischen Formation . l—3. Calamortendron striatum Brongn.
RMRJ670F–. The geological history of plants [microform]. Paleobotany; Paléobotanique. LAURENTIAN AND EARLY PALEOZOIC. 29 ClimacticJiniteSy from the same beds which afford Pro- ticlinites. The principal difference between Protichnites and their modern representatives is that the latter have two lateral furrows produced by the sides of the cara- pace, which are wanting in the for- mer. I subsequently applied the same explanation to sev- eral other ancient forms now known under the gener- al name Bilobites (Figs. 6 and 7).* The tubercu- lated impressions known as Phyma- toderma and Caul- erpites may, as Z
RMMCR9XE–. Charakteristische Jurapflanzen: — Fruchtorgane der C)-cadeen. 1. Cycadospadix Hennoquei (Pom.); Schimp., Fruchtblatt (Infralias). — 2. Steno- rhachis Ponceleti (Nath.), Sap., Fruchtorgan von Podozamites (Infralias). — 3. Beania (jracilis, Carr. (Oolith). — 4. Zamiostrobus incrassalus, L. et H. (Oolith).
RMREWNWM–. On the genus Lepidophloios [microform] : as illustrated by specimens from the coal formation of Nova Scotia and New Brunswick. Paleobotany; Paleobotany; Paléobotanique; Paléobotanique. [sir J. w. DAWSON] Trans. 1897. Sec. IV.—Plate VIH. ON THE GENUS LEPIDOPHLOIOS. 93. 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.. Dawson, J. W. (John William), Sir, 1820-1899; Royal Society of Canada. Montreal : [s. n. ]
RMMCR9F5–. Charakteristische Pappeln aus dem Miocen. 1. Populus mutubilis, AI. Br.; Zweig mit Früchten. — 2. bis 4. Populus latior, Hr.; 2, Zweig; 3, Blatt; 4, Früchte. wie so viele andere tertiäre Arten, welche die Zunahme der Er- kältung gegen Süden hin vertrieben hat, lebt sie fast ohne Ver- änderung in der heutigen homologen Art des nördlichen Afrikas und westlichen Asiens fort. Sehr viele europäische Formen des Miocen sind in der That durch alle ersichtliche Charaktere mit noch lebenden, in der heutigen warrn-gemässigten Zone zerstreuten Arten zu sehr verwandt, als dass man nicht ein Band der Ab-
RMMEJXWX–. Die alttertiäre Flora von Messel bei Darmstadt .
RMRJ66KP–. The geological history of plants [microform]. Paleobotany; Paléobotanique. THE CAIIBONIFEUOUS FLORA. 115 their roots are properly roots at all, and not stems of some aquatic i)lant. Thou tlio structure of their. Flo. 88.—atigmaria root, seen i om almvc, nhowing its regular divisions. From "Acadiun Geolof^y." stems its most puzzlin*^, and their fruit is an cni<^ma, for while some have found connected with them cones supposed to resemble those of lycopods, others attribute to them fruits like those of vew- trees. For years I have been myself gathering materials from the rich coal-
RMMCR9NB–. Charakteristische Pflanzen vom Trocadero (Paris). 1 bis 2. Euphorbiophyllum retus, Sap. Eoeene Wolfsmilchart. — 3 bis 5. Zizyphus pseudo-ühgeri, Sap., Eocener Judendorn. Fio-. 49.
RMRR855F–. Abbildungen und Beschreibungen fossiler Pflanzen-Reste der palaeozoischen und mesozoischen Formationen. Paleobotany; Paleobotany. I : ???-?': ': ' '? ?, warn ^Y4 r o1 %;.^;. 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.. Potonié, H. (Henry), 1857-1913; Preussische Geologische Landesanstalt. Berlin : In vertrieb bei der K. Geologischen Landesanstalt
RMMCR9HA–. Aquitanische Hainbuchen und Buchen. 1. bis 4. Carpinus Ungeri, Ett. (Manosque). — 5. bis 7. Fagus pristina, Sap. (Manosque). gegen eine andere Erlenform, A. phocaeensis, Sap. (Fig. 79, 5), der vorigen zwar sehr nahe verwandt, die sich aber mehr der syrischen als der kaukasischen Erle nähert. Es sind das kleine Schwankungen, die nur den Einfiuss der zahllosen Wechselfälle bezeugen, welchen die Arten bei ihrer Fortpflanzung bis in unsere Zeiten unterworfen waren. Der charakteristische Ahorn des Miocen, Acer trüobaUim (Fig. 80, 2 bis 3), welcher jetzt auftritt, hat nach Heer unver- 18*
RMRHY87G–. On the genus Lepidophloios [microform] : as illustrated by specimens from the coal formation of Nova Scotia and New Brunswick. Paleobotany; Paleobotany; Paléobotanique; Paléobotanique. {8IR I. W. DAWHON] TllANS. 1807. 8kC. IV.—I'lATH XIIl ON THK (iKNlJS LEriDOI'lILOIOS. 103. 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.. Dawson, J. W. (John William), Sir, 1820-1899; Royal Society of Canada. Montreal : [s. n. ]
RMMCR9BE–. Fig. 117. Successive Aenderungen des Typhus Epheu (Hedera) im Laufe der Ter- tiärzeiten« 1. Hedera prcsca, Sap. (Palaeocen von Sezanne). — 2. //. Philiberti, Sap. (Oberes Eocen, Gypse von Aix). — 3. //. Kargii, Br. (Oberes Miocen, Oeningen). — 4. II. acutelobata, Sap. (Unteres Plioeen, Dernbaeh). — 5. //. Mac-Clur!, Hr. (Unteres Mioeen, Grönland). — 6. H. Strozzi, Gaud. (Unteres Plioeen, Toscana). 24*
RMRJ66NA–. The geological history of plants [microform]. Paleobotany; Paléobotanique. 82 THE GEOLOGICAL HISTORY OF PLANTS, Erian and the Permian. They culminated, however, in the Carboniferous period, and the coal-fields of southern France have proved so far the richest in their remains. Lastly, a single specimen, collected by Prof. James Hall, of Albany, at Eighteen-mile Creek, Lake Erie, has the structure of an ordinary angiospermous exogen, and has been described by me as Syringoxylon mirahile*. Fio. 81.—Erian fruits, &c., some wymnospcnnous, and probably of Cordaites and Taxine trees (St. John,
RMMEFEJB–. Die fossile Flora der Permischen Formation .
RMMEFERT–. Die fossile Flora der Permischen Formation . G. Stenzel ye*. 1 — 4. Diplazium giganteum. — 5. Pteris aquilina. Ltthogr. u. Druck Th, Fischer in Cassel.
RMRHY886–. On the genus Lepidophloios [microform] : as illustrated by specimens from the coal formation of Nova Scotia and New Brunswick. Paleobotany; Paleobotany; Paléobotanique; Paléobotanique. 97. 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.. Dawson, J. W. (John William), Sir, 1820-1899; Royal Society of Canada. Montreal : [s. n. ]
RMMCRA20–.
RMRJ66PJ–. The geological history of plants [microform]. Paleobotany; Paléobotanique. I' 1 lii i li! ti 78 THE GEOLOGICAL HISTORY OF PLANTS. latter have long ago descended from their pristine emi- nence to a very humble place in nature, the former still, in the southern hemisphere at least, retain their arboreal dimensions and an- B ^1^ cient dominance. Cil!k. The family of the Equisetacem, or mare's-tails, was also represented by large species of Calamites and by Asterophyl- lites in the Erian; but, as its headquar- ters are in the Car- boniferous, we may defer its considera- tion till the next chapte
RMMEFET6–. Die fossile Flora der Permischen Formation .
RMRHY8E4–. On the genus Lepidophloios [microform] : as illustrated by specimens from the coal formation of Nova Scotia and New Brunswick. Paleobotany; Paleobotany; Paléobotanique; Paléobotanique. ay thus Ihj e loaf-base, 0 former is r condition OS of Corda. will appear V) ,AR()KI>. fforded to me I described in re since been Iness of Prof iparently of a • flattened, its id with clay- rkings of the is scarcely an ire preserved, Y occupied by last is a ring Bsue, about a g to what has [UH J. w. DAWiON] ON THE GENUd LEP1D0PHL0I08 61 in similar stems been regarded as an equivalent of corky bark. This tis
RMMEJXWY–. Die alttertiäre Flora von Messel bei Darmstadt . / / /â ///// ^ m 'Ihn m
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