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Trias jurassic Black & White Stock Photos
Historische, zeichnerische Darstellung, Versteinerungen aus dem Jura, Juraformation, früher Oolithformation, Sedimentärgebilde zwischen Trias und Kreide, 19. Jahrhundert, aus Meyers Konversations-Lexikon, 1889 Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/historische-zeichnerische-darstellung-versteinerungen-aus-dem-jura-juraformation-frher-oolithformation-sedimentrgebilde-zwischen-trias-und-kreide-19-jahrhundert-aus-meyers-konversations-lexikon-1889-image247767572.htmlRMTB2P1T–Historische, zeichnerische Darstellung, Versteinerungen aus dem Jura, Juraformation, früher Oolithformation, Sedimentärgebilde zwischen Trias und Kreide, 19. Jahrhundert, aus Meyers Konversations-Lexikon, 1889
. The geological history of plants. Paleobotany; 1888. THE FLORi OF THE EARLY MESOZOIO. 177 As we ascend, however, 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 the presence of the endogens, in species allied to. Fig. 64.—Jurassic vegetation. Cyeads 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 higher plants come in abund- an Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-geological-history-of-plants-paleobotany-1888-the-flori-of-the-early-mesozoio-177-as-we-ascend-however-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-the-presence-of-the-endogens-in-species-allied-to-fig-64jurassic-vegetation-cyeads-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-higher-plants-come-in-abund-an-image232064401.htmlRMRDFCE9–. The geological history of plants. Paleobotany; 1888. THE FLORi OF THE EARLY MESOZOIO. 177 As we ascend, however, 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 the presence of the endogens, in species allied to. Fig. 64.—Jurassic vegetation. Cyeads 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 higher plants come in abund- an
. The geological history of plants. Paleobotany; 1888. THE FLORi OF THE EARLY MESOZOIO. 177 As we ascend, however, 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 the presence of the endogens, in species allied to. Fig. 64.—Jurassic vegetation. Cyeads 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 higher plants come in abund- an Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-geological-history-of-plants-paleobotany-1888-the-flori-of-the-early-mesozoio-177-as-we-ascend-however-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-the-presence-of-the-endogens-in-species-allied-to-fig-64jurassic-vegetation-cyeads-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-higher-plants-come-in-abund-an-image216413016.htmlRMPG2D08–. The geological history of plants. Paleobotany; 1888. THE FLORi OF THE EARLY MESOZOIO. 177 As we ascend, however, 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 the presence of the endogens, in species allied to. Fig. 64.—Jurassic vegetation. Cyeads 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 higher plants come in abund- an
Fossils of the Jurassic period Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/fossils-of-the-jurassic-period-image247767641.htmlRMTB2P49–Fossils of the Jurassic period
![. 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 Stock Photo](https://c8.alamy.com/comp/RJ66AT/the-geological-history-of-plants-microform-paleobotany-palobotanique-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-ijurassic-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-RJ66AT.jpg ". 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 Stock Photo")
. 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 Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-geological-history-of-plants-microform-paleobotany-palobotanique-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-ijurassic-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-image234935312.htmlRMRJ66AT–. 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
![. The chain of life in geological time [microform] : a sketch of the origin and succession of animals and plants. Paleontology; Paleobotany; Paléontologie; Paléobotanique. Fir,. 145.—A Theriodont Rei)tileof the Trias (Z. j'r<Jjfl!wr/«). —After Owen. Reduced.. Fig. 146.—Skeleton of Pterodochyhis crassirostris. Jurassic of Solenhofen. Reduced.. 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), S Stock Photo](https://c8.alamy.com/comp/RJ6TNB/the-chain-of-life-in-geological-time-microform-a-sketch-of-the-origin-and-succession-of-animals-and-plants-paleontology-paleobotany-palontologie-palobotanique-fir-145a-theriodont-reitileof-the-trias-z-jrltjjfl!wr-after-owen-reduced-fig-146skeleton-of-pterodochyhis-crassirostris-jurassic-of-solenhofen-reduced-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-s-RJ6TNB.jpg ". The chain of life in geological time [microform] : a sketch of the origin and succession of animals and plants. Paleontology; Paleobotany; Paléontologie; Paléobotanique. Fir,. 145.—A Theriodont Rei)tileof the Trias (Z. j'r<Jjfl!wr/«). —After Owen. Reduced.. Fig. 146.—Skeleton of Pterodochyhis crassirostris. Jurassic of Solenhofen. Reduced.. 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), S Stock Photo")
. The chain of life in geological time [microform] : a sketch of the origin and succession of animals and plants. Paleontology; Paleobotany; Paléontologie; Paléobotanique. Fir,. 145.—A Theriodont Rei)tileof the Trias (Z. j'r<Jjfl!wr/«). —After Owen. Reduced.. Fig. 146.—Skeleton of Pterodochyhis crassirostris. Jurassic of Solenhofen. Reduced.. 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), S Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-chain-of-life-in-geological-time-microform-a-sketch-of-the-origin-and-succession-of-animals-and-plants-paleontology-paleobotany-palontologie-palobotanique-fir-145a-theriodont-reitileof-the-trias-z-jrltjjfl!wr-after-owen-reduced-fig-146skeleton-of-pterodochyhis-crassirostris-jurassic-of-solenhofen-reduced-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-s-image234949719.htmlRMRJ6TNB–. The chain of life in geological time [microform] : a sketch of the origin and succession of animals and plants. Paleontology; Paleobotany; Paléontologie; Paléobotanique. Fir,. 145.—A Theriodont Rei)tileof the Trias (Z. j'r<Jjfl!wr/«). —After Owen. Reduced.. Fig. 146.—Skeleton of Pterodochyhis crassirostris. Jurassic of Solenhofen. Reduced.. 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), S
. The Cambridge natural history. Zoology. 498 FISHES CHAP. bodied Holosteans with rhombic scales, rarely, as in Aeiheolepis, cycloid in the caudal region. All the fins possess fulcra. Teeth more or less conical, with a tendency to become tritoral in certain genera. Jugular plate present or absent. Acentro23Jiorus (Upper Permian); Semionotus (Trias of England, Germany, S. Africa, and N. America); Lepidotus (Fig. 292) (Trias of G-ermany, Jurassic of Europe and India, Cretaceous of Brazil); the deep- bodied Dapcdius (Lias of Dorset, Fig. 293), and Aetheolepis (Jurassic of New South Wales) are cha Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-cambridge-natural-history-zoology-498-fishes-chap-bodied-holosteans-with-rhombic-scales-rarely-as-in-aeiheolepis-cycloid-in-the-caudal-region-all-the-fins-possess-fulcra-teeth-more-or-less-conical-with-a-tendency-to-become-tritoral-in-certain-genera-jugular-plate-present-or-absent-acentro23jiorus-upper-permian-semionotus-trias-of-england-germany-s-africa-and-n-america-lepidotus-fig-292-trias-of-g-ermany-jurassic-of-europe-and-india-cretaceous-of-brazil-the-deep-bodied-dapcdius-lias-of-dorset-fig-293-and-aetheolepis-jurassic-of-new-south-wales-are-cha-image232154416.htmlRMRDKF94–. The Cambridge natural history. Zoology. 498 FISHES CHAP. bodied Holosteans with rhombic scales, rarely, as in Aeiheolepis, cycloid in the caudal region. All the fins possess fulcra. Teeth more or less conical, with a tendency to become tritoral in certain genera. Jugular plate present or absent. Acentro23Jiorus (Upper Permian); Semionotus (Trias of England, Germany, S. Africa, and N. America); Lepidotus (Fig. 292) (Trias of G-ermany, Jurassic of Europe and India, Cretaceous of Brazil); the deep- bodied Dapcdius (Lias of Dorset, Fig. 293), and Aetheolepis (Jurassic of New South Wales) are cha
Search Results for Trias jurassic Black & White Stock Photos and Images (7)
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