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Fossil remains sections Stock Photos and Images
Logs and cross sections of the fossil remains of fallen trees dating from the Late Trassic era of 225 million years ago, The Cr Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-logs-and-cross-sections-of-the-fossil-remains-of-fallen-trees-dating-87990472.htmlRFF348MT–Logs and cross sections of the fossil remains of fallen trees dating from the Late Trassic era of 225 million years ago, The Cr
Psaronius asterolithus, fossil seed fern, trunk, Roliegend, Germany, Saxony Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-psaronius-asterolithus-fossil-seed-fern-trunk-roliegend-germany-saxony-76030379.htmlRMEBKDEK–Psaronius asterolithus, fossil seed fern, trunk, Roliegend, Germany, Saxony
Section through fossil ammonite (Hildoceras bifons) in Jurassic Upper Lias, Whitby, North Yorkshire, England, UK. Diameter 60mm Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-section-through-fossil-ammonite-hildoceras-bifons-in-jurassic-upper-24335037.htmlRFBBGFGD–Section through fossil ammonite (Hildoceras bifons) in Jurassic Upper Lias, Whitby, North Yorkshire, England, UK. Diameter 60mm
CONSTRUCTING AN EXTINCT MONSTER FROM FOSSIL REMAINS SECTIONS OF THE BACKBONE. The Artesian Well Water Supply of Australia. MODEL OF TRICERATOPS EXHIBITED AT THE PAN-AMERICAN EXPOSITION. FRILL HORNS AND JAWS., scientific american, 1902-01-18 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/constructing-an-extinct-monster-from-fossil-remains-sections-of-the-backbone-the-artesian-well-water-supply-of-australia-model-of-triceratops-exhibited-at-the-pan-american-exposition-frill-horns-and-jaws-scientific-american-1902-01-18-image334346153.htmlRM2ABXNX1–CONSTRUCTING AN EXTINCT MONSTER FROM FOSSIL REMAINS SECTIONS OF THE BACKBONE. The Artesian Well Water Supply of Australia. MODEL OF TRICERATOPS EXHIBITED AT THE PAN-AMERICAN EXPOSITION. FRILL HORNS AND JAWS., scientific american, 1902-01-18
Archive image from page 180 of Dawn of life being the. Dawn of life: being the history of the oldest known fossil remains, and their relation to geological time and to the development of the animal kingdom dawnoflifebeingh00daws Year: 1875 Fig. 40. Archceocy'athus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.) Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/archive-image-from-page-180-of-dawn-of-life-being-the-dawn-of-life-being-the-history-of-the-oldest-known-fossil-remains-and-their-relation-to-geological-time-and-to-the-development-of-the-animal-kingdom-dawnoflifebeingh00daws-year-1875-fig-40-archceocyathus-atlanticusshowing-outer-surface-and-longitudinal-and-transverse-sections-after-billings-image259469157.htmlRMW23RFH–Archive image from page 180 of Dawn of life being the. Dawn of life: being the history of the oldest known fossil remains, and their relation to geological time and to the development of the animal kingdom dawnoflifebeingh00daws Year: 1875 Fig. 40. Archceocy'athus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.)
Mookaite, a brecciated radiolarite, composed of fossil radiolarians, Western Australia, Cretaceous period. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/mookaite-a-brecciated-radiolarite-composed-of-fossil-radiolarians-western-australia-cretaceous-period-image357423271.htmlRM2BNE10R–Mookaite, a brecciated radiolarite, composed of fossil radiolarians, Western Australia, Cretaceous period.
A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . FOSSIL FAUNA. 117 PLATE XLIX. Remains of Encrinites. Fig. 1. A polislied slab of limestone formed of portions of the stems of encrinites; the whitefigures are produced by sections of the calcareous spar into which the ossicula ar®transmuted. The dark spots are the cavities of the entrochites^ filled with mineralmatter of a different colour. Fig. 2, is the pentagonal base of the receptacle of the Derbyshire Encrinite. Fi Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-pictorial-atlas-of-fossil-remains-consisting-of-coloured-illustrations-selected-from-parkinsons-organic-remains-of-a-former-world-and-artiss-antediluvian-phytology-fossil-fauna-117-plate-xlix-remains-of-encrinites-fig-1-a-polislied-slab-of-limestone-formed-of-portions-of-the-stems-of-encrinites-the-whitefigures-are-produced-by-sections-of-the-calcareous-spar-into-which-the-ossicula-artransmuted-the-dark-spots-are-the-cavities-of-the-entrochites-filled-with-mineralmatter-of-a-different-colour-fig-2-is-the-pentagonal-base-of-the-receptacle-of-the-derbyshire-encrinite-fi-image342696506.htmlRM2AWF4TX–A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . FOSSIL FAUNA. 117 PLATE XLIX. Remains of Encrinites. Fig. 1. A polislied slab of limestone formed of portions of the stems of encrinites; the whitefigures are produced by sections of the calcareous spar into which the ossicula ar®transmuted. The dark spots are the cavities of the entrochites^ filled with mineralmatter of a different colour. Fig. 2, is the pentagonal base of the receptacle of the Derbyshire Encrinite. Fi
. Dawn of life: being the history of the oldest known fossil remains, and their relation to geological time and to the development of the animal kingdom. Paleontology; Eozoon; Life. Fig. 40. Archceocy'athus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.). 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, John William, Sir, 1820-1899. London, Hodder & Stoughton Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/dawn-of-life-being-the-history-of-the-oldest-known-fossil-remains-and-their-relation-to-geological-time-and-to-the-development-of-the-animal-kingdom-paleontology-eozoon-life-fig-40-archceocyathus-atlanticusshowing-outer-surface-and-longitudinal-and-transverse-sections-after-billings-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-john-william-sir-1820-1899-london-hodder-amp-stoughton-image216098606.htmlRMPFG3YA–. Dawn of life: being the history of the oldest known fossil remains, and their relation to geological time and to the development of the animal kingdom. Paleontology; Eozoon; Life. Fig. 40. Archceocy'athus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.). 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, John William, Sir, 1820-1899. London, Hodder & Stoughton
Psaronius scolecolithus, fossil seed fern, trunk, Roliegend, Germany, Saxony Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-psaronius-scolecolithus-fossil-seed-fern-trunk-roliegend-germany-saxony-76030380.htmlRMEBKDEM–Psaronius scolecolithus, fossil seed fern, trunk, Roliegend, Germany, Saxony
Close up of a polished cross section of Kambaba Jasper, fossil Stromatolite, Madagascar. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/close-up-of-a-polished-cross-section-of-kambaba-jasper-fossil-stromatolite-madagascar-image357423274.htmlRM2BNE10X–Close up of a polished cross section of Kambaba Jasper, fossil Stromatolite, Madagascar.
A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . tholithes; figs. 3, 6, P. asteroUthes; figs. 5, 6, 7, are enlarged figuresof the transverse sections of some of the vessels forming the vascular tissue. From the stellular figure produced by transverse sections of the vessels, this fossil wood hasreceived the name of ^ Staarenstein, or Starry-stone. In the time of Mr. Parkinson, thetubes now known to be the vessels of the vascular tissue, were supposed to have beenprodu Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-pictorial-atlas-of-fossil-remains-consisting-of-coloured-illustrations-selected-from-parkinsons-organic-remains-of-a-former-world-and-artiss-antediluvian-phytology-tholithes-figs-3-6-p-asterouthes-figs-5-6-7-are-enlarged-figuresof-the-transverse-sections-of-some-of-the-vessels-forming-the-vascular-tissue-from-the-stellular-figure-produced-by-transverse-sections-of-the-vessels-this-fossil-wood-hasreceived-the-name-of-staarenstein-or-starry-stone-in-the-time-of-mr-parkinson-thetubes-now-known-to-be-the-vessels-of-the-vascular-tissue-were-supposed-to-have-beenprodu-image342724136.htmlRM2AWGC3M–A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . tholithes; figs. 3, 6, P. asteroUthes; figs. 5, 6, 7, are enlarged figuresof the transverse sections of some of the vessels forming the vascular tissue. From the stellular figure produced by transverse sections of the vessels, this fossil wood hasreceived the name of ^ Staarenstein, or Starry-stone. In the time of Mr. Parkinson, thetubes now known to be the vessels of the vascular tissue, were supposed to have beenprodu
Ammonite, cross section. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/ammonite-cross-section-image263049191.htmlRMW7XWWY–Ammonite, cross section.
Close up of a polished cross section of Kambaba Jasper, fossilised Stromatolite, Madagascar. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/close-up-of-a-polished-cross-section-of-kambaba-jasper-fossilised-stromatolite-madagascar-image357423259.htmlRM2BNE10B–Close up of a polished cross section of Kambaba Jasper, fossilised Stromatolite, Madagascar.
Petrified wood segment Blue Mesa Badlands Petrified Forest National Park Arizona USA December 2012. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-petrified-wood-segment-blue-mesa-badlands-petrified-forest-national-78772669.htmlRMEG4B9H–Petrified wood segment Blue Mesa Badlands Petrified Forest National Park Arizona USA December 2012.
Ammonite, cross section on black background, Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-ammonite-cross-section-on-black-background-86765785.htmlRMF14EJ1–Ammonite, cross section on black background,
Psaronius asterolithus, fossil seed fern, trunk, vascular tissue, Roliegend, Germany, Saxony Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-psaronius-asterolithus-fossil-seed-fern-trunk-vascular-tissue-roliegend-76030378.htmlRMEBKDEJ–Psaronius asterolithus, fossil seed fern, trunk, vascular tissue, Roliegend, Germany, Saxony
A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . ded by a whiteband, which is probably the remains of the cortical or external tissue of the originalzoophyte. I have seen many transverse sections in which the central mass waseither of a pink or purple colour, and encircled by a white zone, in the squared flintsof the walls of churches and other ancient edifices in Sussex. Medals of Creation, p. 237. 2 Polished specimens of the pebbles of the Isle of Wight, exhibiting Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-pictorial-atlas-of-fossil-remains-consisting-of-coloured-illustrations-selected-from-parkinsons-organic-remains-of-a-former-world-and-artiss-antediluvian-phytology-ded-by-a-whiteband-which-is-probably-the-remains-of-the-cortical-or-external-tissue-of-the-originalzoophyte-i-have-seen-many-transverse-sections-in-which-the-central-mass-waseither-of-a-pink-or-purple-colour-and-encircled-by-a-white-zone-in-the-squared-flintsof-the-walls-of-churches-and-other-ancient-edifices-in-sussex-medals-of-creation-p-237-2-polished-specimens-of-the-pebbles-of-the-isle-of-wight-exhibiting-image342704309.htmlRM2AWFERH–A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . ded by a whiteband, which is probably the remains of the cortical or external tissue of the originalzoophyte. I have seen many transverse sections in which the central mass waseither of a pink or purple colour, and encircled by a white zone, in the squared flintsof the walls of churches and other ancient edifices in Sussex. Medals of Creation, p. 237. 2 Polished specimens of the pebbles of the Isle of Wight, exhibiting
A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . of the enclosed corals {Astrea undulata, of Dr. Fleming); from Switzerland: probably from the Oolitic or Jurassic formation. Fig. 11. Vertical section of a fossil coral, showing the transverse arrangement of the internal cells. Fig. 12 & 13. These specimens are polished sections of a very beautiful compound coral {AstreaTisburiensis, of Miss Benett), which occurs in a sUicified state in the Portland bedsthat are quarrie Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-pictorial-atlas-of-fossil-remains-consisting-of-coloured-illustrations-selected-from-parkinsons-organic-remains-of-a-former-world-and-artiss-antediluvian-phytology-of-the-enclosed-corals-astrea-undulata-of-dr-fleming-from-switzerland-probably-from-the-oolitic-or-jurassic-formation-fig-11-vertical-section-of-a-fossil-coral-showing-the-transverse-arrangement-of-the-internal-cells-fig-12-13-these-specimens-are-polished-sections-of-a-very-beautiful-compound-coral-astreatisburiensis-of-miss-benett-which-occurs-in-a-suicified-state-in-the-portland-bedsthat-are-quarrie-image342708295.htmlRM2AWFKWY–A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . of the enclosed corals {Astrea undulata, of Dr. Fleming); from Switzerland: probably from the Oolitic or Jurassic formation. Fig. 11. Vertical section of a fossil coral, showing the transverse arrangement of the internal cells. Fig. 12 & 13. These specimens are polished sections of a very beautiful compound coral {AstreaTisburiensis, of Miss Benett), which occurs in a sUicified state in the Portland bedsthat are quarrie
Text-book of structural and physiological botany . FiG. 545. —Stem of Cycadoidea 77ze^alophylla(Cycadeae), from Portland Isle.. Fig. 546. — Branch ofPresleamnn (Cycadeae). 428 Structural and Physiological Botany, The uniformity of vegetation characteristic of the Carbo-niferous is still more marked in the Triassic system. Next in succession above the Trias is the Jurassic sys-tem^ which again is divided into three sections, the Lias^ andthe Lowei: and Upper Oolite. The fossil remains found in thisformation lead to the conclusion that the marine plants ofthe Lias did not differ essentially from Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/text-book-of-structural-and-physiological-botany-fig-545-stem-of-cycadoidea-77zealophyllacycadeae-from-portland-isle-fig-546-branch-ofpresleamnn-cycadeae-428-structural-and-physiological-botany-the-uniformity-of-vegetation-characteristic-of-the-carbo-niferous-is-still-more-marked-in-the-triassic-system-next-in-succession-above-the-trias-is-the-jurassic-sys-tem-which-again-is-divided-into-three-sections-the-lias-andthe-lowei-and-upper-oolite-the-fossil-remains-found-in-thisformation-lead-to-the-conclusion-that-the-marine-plants-ofthe-lias-did-not-differ-essentially-from-image343262774.htmlRM2AXCY4P–Text-book of structural and physiological botany . FiG. 545. —Stem of Cycadoidea 77ze^alophylla(Cycadeae), from Portland Isle.. Fig. 546. — Branch ofPresleamnn (Cycadeae). 428 Structural and Physiological Botany, The uniformity of vegetation characteristic of the Carbo-niferous is still more marked in the Triassic system. Next in succession above the Trias is the Jurassic sys-tem^ which again is divided into three sections, the Lias^ andthe Lowei: and Upper Oolite. The fossil remains found in thisformation lead to the conclusion that the marine plants ofthe Lias did not differ essentially from
A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . er.A gioove visible on the external surface indicates the inner axis, which by compression hasbeen pressed from its natural central position; see fig. 2, a, b, c, d : figs. 6, 7, 8, 9, show in thecorresponding transverse sections the position of this body. The mode of attachment of the rootlets to the tubercle on the main root, is representedfig. 5. Fig. 3, exhibits the characters of the two kinds of variolse, or tuberc Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-pictorial-atlas-of-fossil-remains-consisting-of-coloured-illustrations-selected-from-parkinsons-organic-remains-of-a-former-world-and-artiss-antediluvian-phytology-era-gioove-visible-on-the-external-surface-indicates-the-inner-axis-which-by-compression-hasbeen-pressed-from-its-natural-central-position-see-fig-2-a-b-c-d-figs-6-7-8-9-show-in-thecorresponding-transverse-sections-the-position-of-this-body-the-mode-of-attachment-of-the-rootlets-to-the-tubercle-on-the-main-root-is-representedfig-5-fig-3-exhibits-the-characters-of-the-two-kinds-of-variolse-or-tuberc-image342717088.htmlRM2AWG340–A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . er.A gioove visible on the external surface indicates the inner axis, which by compression hasbeen pressed from its natural central position; see fig. 2, a, b, c, d : figs. 6, 7, 8, 9, show in thecorresponding transverse sections the position of this body. The mode of attachment of the rootlets to the tubercle on the main root, is representedfig. 5. Fig. 3, exhibits the characters of the two kinds of variolse, or tuberc
A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . la from Saumur. Fig. 6. A Ventriculite from a gravel-pit; the markings are produced by the exposed andpartially abraded outer integument, which in perfect examples consists of a regularnet-work of subcylindrical fibres. Fig. 7, is a transverse section of a Siphonia {Siphotiia pyriformis of Goldfuss). Fig. 8. A nearly perfect specimen of a similar fossil. In fig. 7, are shown sections of tubespassing from the periphery t Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-pictorial-atlas-of-fossil-remains-consisting-of-coloured-illustrations-selected-from-parkinsons-organic-remains-of-a-former-world-and-artiss-antediluvian-phytology-la-from-saumur-fig-6-a-ventriculite-from-a-gravel-pit-the-markings-are-produced-by-the-exposed-andpartially-abraded-outer-integument-which-in-perfect-examples-consists-of-a-regularnet-work-of-subcylindrical-fibres-fig-7-is-a-transverse-section-of-a-siphonia-siphotiia-pyriformis-of-goldfuss-fig-8-a-nearly-perfect-specimen-of-a-similar-fossil-in-fig-7-are-shown-sections-of-tubespassing-from-the-periphery-t-image342706018.htmlRM2AWFH0J–A pictorial atlas of fossil remains, consisting of coloured illustrations selected from Parkinson's 'Organic remains of a former world,' and Artis's 'Antediluvian phytology.' . la from Saumur. Fig. 6. A Ventriculite from a gravel-pit; the markings are produced by the exposed andpartially abraded outer integument, which in perfect examples consists of a regularnet-work of subcylindrical fibres. Fig. 7, is a transverse section of a Siphonia {Siphotiia pyriformis of Goldfuss). Fig. 8. A nearly perfect specimen of a similar fossil. In fig. 7, are shown sections of tubespassing from the periphery t
. Natal province : descriptive guide and official hand-book . ls from all parts of the world, and following these a collection of localminerals. A collection representing the action of geological agencies, such as weathering, earth-movements, volcanic action, etc., has been arranged. The walls of this hall are provided with some impressive photographic enlargementsof typical Natal scenery, also maps and sections dealing with the geology of Zululand andNatal. The Colony is very poor in fossil-remains, but some specimens of fossils from theCretaceous beds of the coast, and plant-remains from the Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/natal-province-descriptive-guide-and-official-hand-book-ls-from-all-parts-of-the-world-and-following-these-a-collection-of-localminerals-a-collection-representing-the-action-of-geological-agencies-such-as-weathering-earth-movements-volcanic-action-etc-has-been-arranged-the-walls-of-this-hall-are-provided-with-some-impressive-photographic-enlargementsof-typical-natal-scenery-also-maps-and-sections-dealing-with-the-geology-of-zululand-andnatal-the-colony-is-very-poor-in-fossil-remains-but-some-specimens-of-fossils-from-thecretaceous-beds-of-the-coast-and-plant-remains-from-the-image376073098.htmlRM2CRRH22–. Natal province : descriptive guide and official hand-book . ls from all parts of the world, and following these a collection of localminerals. A collection representing the action of geological agencies, such as weathering, earth-movements, volcanic action, etc., has been arranged. The walls of this hall are provided with some impressive photographic enlargementsof typical Natal scenery, also maps and sections dealing with the geology of Zululand andNatal. The Colony is very poor in fossil-remains, but some specimens of fossils from theCretaceous beds of the coast, and plant-remains from the
![. The dawn of life [microform] : being the history of the oldest known fossil remains, and their relations to geological time, and to the development of the animal kingdom. Paleontology; Life; Paléontologie; Vie. mmi^ (; ^'C^^. Fig. 40. Archccocyathus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.). 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 Stock Photo](https://c8.alamy.com/comp/RJ5H18/the-dawn-of-life-microform-being-the-history-of-the-oldest-known-fossil-remains-and-their-relations-to-geological-time-and-to-the-development-of-the-animal-kingdom-paleontology-life-palontologie-vie-mmi-c-fig-40-archccocyathus-atlanticusshowing-outer-surface-and-longitudinal-and-transverse-sections-after-billings-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-RJ5H18.jpg ". The dawn of life [microform] : being the history of the oldest known fossil remains, and their relations to geological time, and to the development of the animal kingdom. Paleontology; Life; Paléontologie; Vie. mmi^ (; ^'C^^. Fig. 40. Archccocyathus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.). 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 Stock Photo")
. The dawn of life [microform] : being the history of the oldest known fossil remains, and their relations to geological time, and to the development of the animal kingdom. Paleontology; Life; Paléontologie; Vie. mmi^ (; ^'C^^. Fig. 40. Archccocyathus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.). 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 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-dawn-of-life-microform-being-the-history-of-the-oldest-known-fossil-remains-and-their-relations-to-geological-time-and-to-the-development-of-the-animal-kingdom-paleontology-life-palontologie-vie-mmi-c-fig-40-archccocyathus-atlanticusshowing-outer-surface-and-longitudinal-and-transverse-sections-after-billings-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-image234921716.htmlRMRJ5H18–. The dawn of life [microform] : being the history of the oldest known fossil remains, and their relations to geological time, and to the development of the animal kingdom. Paleontology; Life; Paléontologie; Vie. mmi^ (; ^'C^^. Fig. 40. Archccocyathus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.). 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
. Dawn of life: being the history of the oldest known fossil remains, and their relation to geological time and to the development of the animal kingdom. Paleontology; Eozoon; Life. Fig. 40. Archceocy'athus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.). 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, John William, Sir, 1820-1899. London, Hodder & Stoughton Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/dawn-of-life-being-the-history-of-the-oldest-known-fossil-remains-and-their-relation-to-geological-time-and-to-the-development-of-the-animal-kingdom-paleontology-eozoon-life-fig-40-archceocyathus-atlanticusshowing-outer-surface-and-longitudinal-and-transverse-sections-after-billings-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-john-william-sir-1820-1899-london-hodder-amp-stoughton-image231804751.htmlRMRD3H93–. Dawn of life: being the history of the oldest known fossil remains, and their relation to geological time and to the development of the animal kingdom. Paleontology; Eozoon; Life. Fig. 40. Archceocy'athus Atlanticus—showing outer surface and longitudinal and transverse sections. {After Billings.). 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, John William, Sir, 1820-1899. London, Hodder & Stoughton
![. Second contribution to the studies on the Cambrian faunas of North America [microform]. Paleontology; Arthropoda, Fossil; Arthropoda, Fossil; Paléontologie; Arthropodes fossiles; Arthropodes fossiles. m â â â * f" 60 CAMBRIAN ?AUNAS OF NORTH AMERICJ*. (buli,. :to. «11 the foiiriations from the Laurentiau ui)wards, often with character istic fossils. I liave also made sections of many of the tossiliferous pebbles in tliese conglomerates without finding any certain remains of such organisms, though the fragments of the crusts of some of the Primordial trilobites, when their tubuli are i Stock Photo](https://c8.alamy.com/comp/RJ4P1K/second-contribution-to-the-studies-on-the-cambrian-faunas-of-north-america-microform-paleontology-arthropoda-fossil-arthropoda-fossil-palontologie-arthropodes-fossiles-arthropodes-fossiles-m-fquot-60-cambrian-aunas-of-north-americj-buli-to-11-the-foiiriations-from-the-laurentiau-uiwards-often-with-character-istic-fossils-i-liave-also-made-sections-of-many-of-the-tossiliferous-pebbles-in-tliese-conglomerates-without-finding-any-certain-remains-of-such-organisms-though-the-fragments-of-the-crusts-of-some-of-the-primordial-trilobites-when-their-tubuli-are-i-RJ4P1K.jpg ". Second contribution to the studies on the Cambrian faunas of North America [microform]. Paleontology; Arthropoda, Fossil; Arthropoda, Fossil; Paléontologie; Arthropodes fossiles; Arthropodes fossiles. m â â â * f" 60 CAMBRIAN ?AUNAS OF NORTH AMERICJ*. (buli,. :to. «11 the foiiriations from the Laurentiau ui)wards, often with character istic fossils. I liave also made sections of many of the tossiliferous pebbles in tliese conglomerates without finding any certain remains of such organisms, though the fragments of the crusts of some of the Primordial trilobites, when their tubuli are i Stock Photo")
. Second contribution to the studies on the Cambrian faunas of North America [microform]. Paleontology; Arthropoda, Fossil; Arthropoda, Fossil; Paléontologie; Arthropodes fossiles; Arthropodes fossiles. m â â â * f" 60 CAMBRIAN ?AUNAS OF NORTH AMERICJ*. (buli,. :to. «11 the foiiriations from the Laurentiau ui)wards, often with character istic fossils. I liave also made sections of many of the tossiliferous pebbles in tliese conglomerates without finding any certain remains of such organisms, though the fragments of the crusts of some of the Primordial trilobites, when their tubuli are i Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/second-contribution-to-the-studies-on-the-cambrian-faunas-of-north-america-microform-paleontology-arthropoda-fossil-arthropoda-fossil-palontologie-arthropodes-fossiles-arthropodes-fossiles-m-fquot-60-cambrian-aunas-of-north-americj-buli-to-11-the-foiiriations-from-the-laurentiau-uiwards-often-with-character-istic-fossils-i-liave-also-made-sections-of-many-of-the-tossiliferous-pebbles-in-tliese-conglomerates-without-finding-any-certain-remains-of-such-organisms-though-the-fragments-of-the-crusts-of-some-of-the-primordial-trilobites-when-their-tubuli-are-i-image234903695.htmlRMRJ4P1K–. Second contribution to the studies on the Cambrian faunas of North America [microform]. Paleontology; Arthropoda, Fossil; Arthropoda, Fossil; Paléontologie; Arthropodes fossiles; Arthropodes fossiles. m â â â * f" 60 CAMBRIAN ?AUNAS OF NORTH AMERICJ*. (buli,. :to. «11 the foiiriations from the Laurentiau ui)wards, often with character istic fossils. I liave also made sections of many of the tossiliferous pebbles in tliese conglomerates without finding any certain remains of such organisms, though the fragments of the crusts of some of the Primordial trilobites, when their tubuli are i
