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Actinocamax Stock Photos and Images
. Actinocamax spec 6 Actinocamax spec. - - Print - Iconographia Zoologica - Special Collections University of Amsterdam - UBAINV0274 090 08 0023 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/actinocamax-spec-6-actinocamax-spec-print-iconographia-zoologica-special-collections-university-of-amsterdam-ubainv0274-090-08-0023-image207862953.htmlRMP24Y8W–. Actinocamax spec 6 Actinocamax spec. - - Print - Iconographia Zoologica - Special Collections University of Amsterdam - UBAINV0274 090 08 0023
Fossils of extinct marine cephalopods, ancestors to the squid and cuttlefish, from the Jurassic period. Belemnites paxillosus, B. digitalis, B. canaliculatus, B. acuminatus, B. pistilliformis and Actinocamax. 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/image-license-details/?v=1https://www.alamy.com/fossils-of-extinct-marine-cephalopods-ancestors-to-the-squid-and-cuttlefish-from-the-jurassic-period-belemnites-paxillosus-b-digitalis-b-canaliculatus-b-acuminatus-b-pistilliformis-and-actinocamax-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-image209713847.htmlRMP55847–Fossils of extinct marine cephalopods, ancestors to the squid and cuttlefish, from the Jurassic period. Belemnites paxillosus, B. digitalis, B. canaliculatus, B. acuminatus, B. pistilliformis and Actinocamax. 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.
Actinocamax, vintage engraved illustration. Earth before man – 1886. Stock Vectorhttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-actinocamax-vintage-engraved-illustration-earth-before-man-1886-84300940.htmlRFEW46KT–Actinocamax, vintage engraved illustration. Earth before man – 1886.
Archive image from page 353 of Cuvier's animal kingdom arranged. Cuvier's animal kingdom : arranged according to its organization cuviersanimalkin00cuvi Year: 1840 342 MOLLUSCA. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Sna Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/archive-image-from-page-353-of-cuviers-animal-kingdom-arranged-cuviers-animal-kingdom-arranged-according-to-its-organization-cuviersanimalkin00cuvi-year-1840-342-mollusca-fissure-from-the-exterior-surface-being-marked-witii-a-longitudinal-gutter-on-one-side-or-with-two-or-several-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-hke-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basis-form-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-the-ammonites-brug-or-sna-image259563216.htmlRMW283ET–Archive image from page 353 of Cuvier's animal kingdom arranged. Cuvier's animal kingdom : arranged according to its organization cuviersanimalkin00cuvi Year: 1840 342 MOLLUSCA. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Sna
The animal kingdom, arranged after its organization : forming a natural history of animals, and an introduction to comparative anatomy . to mention thatutantous appendages ofchins, (KcAinus).—Eu. 342 MOLLUSCA.. fissure; from the exterior surface being marl<ed with a longitudinal gutter on one side, or with two orseveral gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis,form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of t Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-animal-kingdom-arranged-after-its-organization-forming-a-natural-history-of-animals-and-an-introduction-to-comparative-anatomy-to-mention-thatutantous-appendages-ofchins-kcainuseu-342-mollusca-fissure-from-the-exterior-surface-being-marllted-with-a-longitudinal-gutter-on-one-side-or-with-two-orseveral-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-hke-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basisform-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-t-image338306928.htmlRM2AJB5X8–The animal kingdom, arranged after its organization : forming a natural history of animals, and an introduction to comparative anatomy . to mention thatutantous appendages ofchins, (KcAinus).—Eu. 342 MOLLUSCA.. fissure; from the exterior surface being marl<ed with a longitudinal gutter on one side, or with two orseveral gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis,form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of t
. Cuvier's animal kingdom : arranged according to its organization. Animals. 342 MOLLUSCA.. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is founded, for they, also, are only found in a fossil state. They are distingui Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/cuviers-animal-kingdom-arranged-according-to-its-organization-animals-342-mollusca-fissure-from-the-exterior-surface-being-marked-witii-a-longitudinal-gutter-on-one-side-or-with-two-or-several-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-hke-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basis-form-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-the-ammonites-brug-or-snake-stones-is-founded-for-they-also-are-only-found-in-a-fossil-state-they-are-distingui-image216323651.htmlRMPFXB0K–. Cuvier's animal kingdom : arranged according to its organization. Animals. 342 MOLLUSCA.. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is founded, for they, also, are only found in a fossil state. They are distingui
. Die Leitfossilien, ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen . 1 Belemnitenthier und Bcleninitenschale, ideale Reconstruction. 3 Reconstruction der Beloranitenschale; das Rostniin längsgespalten, um den tütcnföriiiigen Phragiuokon zu zeigen. 2 Kostrum am einen Ende verwittert und zugespitzt; Actinocamax-Stadium. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/die-leitfossilien-ein-handbuch-fr-den-unterricht-und-fr-das-bestimmen-von-versteinerungen-1-belemnitenthier-und-bcleninitenschale-ideale-reconstruction-3-reconstruction-der-beloranitenschale-das-rostniin-lngsgespalten-um-den-ttcnfriiiigen-phragiuokon-zu-zeigen-2-kostrum-am-einen-ende-verwittert-und-zugespitzt-actinocamax-stadium-image180884653.htmlRMME8065–. Die Leitfossilien, ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen . 1 Belemnitenthier und Bcleninitenschale, ideale Reconstruction. 3 Reconstruction der Beloranitenschale; das Rostniin längsgespalten, um den tütcnföriiiigen Phragiuokon zu zeigen. 2 Kostrum am einen Ende verwittert und zugespitzt; Actinocamax-Stadium.
Fossils of extinct marine cephalopods Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-fossils-of-extinct-marine-cephalopods-38109050.htmlRMC600DE–Fossils of extinct marine cephalopods
Belemnites of the Cretaceous, vintage engraved illustration. Earth before man – 1886. Stock Vectorhttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-belemnites-of-the-cretaceous-vintage-engraved-illustration-earth-before-84300939.htmlRFEW46KR–Belemnites of the Cretaceous, vintage engraved illustration. Earth before man – 1886.
Archive image from page 353 of Cuvier's animal kingdom arranged. Cuvier's animal kingdom : arranged according to its organization cuviersanimalkin00cuvi Year: 1840 fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is fo Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/archive-image-from-page-353-of-cuviers-animal-kingdom-arranged-cuviers-animal-kingdom-arranged-according-to-its-organization-cuviersanimalkin00cuvi-year-1840-fissure-from-the-exterior-surface-being-marked-witii-a-longitudinal-gutter-on-one-side-or-with-two-or-several-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-hke-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basis-form-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-the-ammonites-brug-or-snake-stones-is-fo-image259563187.htmlRMW283DR–Archive image from page 353 of Cuvier's animal kingdom arranged. Cuvier's animal kingdom : arranged according to its organization cuviersanimalkin00cuvi Year: 1840 fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is fo
. The animal kingdom, arranged after its organization, forming a natural history of animals, and an introduction to comparative anatomy. Zoology. fissure ; from the exterior surface being marked with a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much like the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stoxes,— Is founded, for they, also Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-animal-kingdom-arranged-after-its-organization-forming-a-natural-history-of-animals-and-an-introduction-to-comparative-anatomy-zoology-fissure-from-the-exterior-surface-being-marked-with-a-longitudinal-gutter-on-one-side-or-with-two-or-several-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-like-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basis-form-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-the-ammonites-brug-or-snake-stoxes-is-founded-for-they-also-image236750315.htmlRMRN4WCB–. The animal kingdom, arranged after its organization, forming a natural history of animals, and an introduction to comparative anatomy. Zoology. fissure ; from the exterior surface being marked with a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much like the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stoxes,— Is founded, for they, also
. Cuvier's animal kingdom : arranged according to its organization. Animals. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is founded, for they, also, are only found in a fossil state. They are distinguished, in genera Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/cuviers-animal-kingdom-arranged-according-to-its-organization-animals-fissure-from-the-exterior-surface-being-marked-witii-a-longitudinal-gutter-on-one-side-or-with-two-or-several-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-hke-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basis-form-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-the-ammonites-brug-or-snake-stones-is-founded-for-they-also-are-only-found-in-a-fossil-state-they-are-distinguished-in-genera-image216323247.htmlRMPFXAE7–. Cuvier's animal kingdom : arranged according to its organization. Animals. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is founded, for they, also, are only found in a fossil state. They are distinguished, in genera
. Die Leitfossilien, ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen . sind relativ schlanker als die ausgewachsener. Zuweilen wurde das Bilduugsgewebe nicht ganz durch Kalkspat erfüllt; die Scheiden bleiben dann locker und sind an der Spitze oft gerunzelt oder verdrückt (Fig. 67). Auch die Umgebung der Alveole ist oft leichter zerstörbar als der übrige Teil des Rostrums; durch Yerwitterung und Abrollung resultieren dann zweiseitig zugespitzte Rostra, die man früher als besondere Gattung, Actinocamax, auffasste (Fig. 66, 2). Alle Prismen stehen, wie gesagt, senk- rech Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/die-leitfossilien-ein-handbuch-fr-den-unterricht-und-fr-das-bestimmen-von-versteinerungen-sind-relativ-schlanker-als-die-ausgewachsener-zuweilen-wurde-das-bilduugsgewebe-nicht-ganz-durch-kalkspat-erfllt-die-scheiden-bleiben-dann-locker-und-sind-an-der-spitze-oft-gerunzelt-oder-verdrckt-fig-67-auch-die-umgebung-der-alveole-ist-oft-leichter-zerstrbar-als-der-brige-teil-des-rostrums-durch-yerwitterung-und-abrollung-resultieren-dann-zweiseitig-zugespitzte-rostra-die-man-frher-als-besondere-gattung-actinocamax-auffasste-fig-66-2-alle-prismen-stehen-wie-gesagt-senk-rech-image180884565.htmlRMME8031–. Die Leitfossilien, ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen . sind relativ schlanker als die ausgewachsener. Zuweilen wurde das Bilduugsgewebe nicht ganz durch Kalkspat erfüllt; die Scheiden bleiben dann locker und sind an der Spitze oft gerunzelt oder verdrückt (Fig. 67). Auch die Umgebung der Alveole ist oft leichter zerstörbar als der übrige Teil des Rostrums; durch Yerwitterung und Abrollung resultieren dann zweiseitig zugespitzte Rostra, die man früher als besondere Gattung, Actinocamax, auffasste (Fig. 66, 2). Alle Prismen stehen, wie gesagt, senk- rech
. Cuvier's animal kingdom : arranged according to its organization. Animals. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is founded, for they, also, are only found in a fossil state. They are distinguished, in genera Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/cuviers-animal-kingdom-arranged-according-to-its-organization-animals-fissure-from-the-exterior-surface-being-marked-witii-a-longitudinal-gutter-on-one-side-or-with-two-or-several-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-hke-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basis-form-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-the-ammonites-brug-or-snake-stones-is-founded-for-they-also-are-only-found-in-a-fossil-state-they-are-distinguished-in-genera-image231852441.htmlRMRD5P49–. Cuvier's animal kingdom : arranged according to its organization. Animals. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is founded, for they, also, are only found in a fossil state. They are distinguished, in genera
. Description of the fossil remains of Mollusca found in the chalk of England. Cephalopoda. Cephalopoda, Fossil; Paleontology. Fig. A Fig.B 1. Belemnitella mucronata, Schlotheim, Sp. Plate I, figs. 1, 2, and 3. Belemnites, 1° species : Breyn, de Belemnitis, figs. 1—6. Belemnites mucronatus, Schlotheim. Petref., p. 47, No. 4. — — Mantell. Sussex, t. xvi, fig. 1. — — Nilsson. Petrif. Saec, t. ii, fig. 1. — — Sowerby. Min. Conch., t. 600, figs. 2 and 4. Belemnites electrikus. Miller. Geol. Tr., 2d series, vol. ii, t. viii, figs. 18—21. AcTiNOCAMAX VEKUS? Miller. Loc. cit., t. ix, figs. 17 and 18. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/description-of-the-fossil-remains-of-mollusca-found-in-the-chalk-of-england-cephalopoda-cephalopoda-fossil-paleontology-fig-a-figb-1-belemnitella-mucronata-schlotheim-sp-plate-i-figs-1-2-and-3-belemnites-1-species-breyn-de-belemnitis-figs-16-belemnites-mucronatus-schlotheim-petref-p-47-no-4-mantell-sussex-t-xvi-fig-1-nilsson-petrif-saec-t-ii-fig-1-sowerby-min-conch-t-600-figs-2-and-4-belemnites-electrikus-miller-geol-tr-2d-series-vol-ii-t-viii-figs-1821-actinocamax-vekus-miller-loc-cit-t-ix-figs-17-and-18-image215994940.htmlRMPFBBN0–. Description of the fossil remains of Mollusca found in the chalk of England. Cephalopoda. Cephalopoda, Fossil; Paleontology. Fig. A Fig.B 1. Belemnitella mucronata, Schlotheim, Sp. Plate I, figs. 1, 2, and 3. Belemnites, 1° species : Breyn, de Belemnitis, figs. 1—6. Belemnites mucronatus, Schlotheim. Petref., p. 47, No. 4. — — Mantell. Sussex, t. xvi, fig. 1. — — Nilsson. Petrif. Saec, t. ii, fig. 1. — — Sowerby. Min. Conch., t. 600, figs. 2 and 4. Belemnites electrikus. Miller. Geol. Tr., 2d series, vol. ii, t. viii, figs. 18—21. AcTiNOCAMAX VEKUS? Miller. Loc. cit., t. ix, figs. 17 and 18.
. The animal kingdom, arranged after its organization, forming a natural history of animals, and an introduction to comparative anatomy. Zoology. 342 MOLLUSCA.. fissure ; from the exterior surface being marked with a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much like the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stoxes,— Is founded, Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-animal-kingdom-arranged-after-its-organization-forming-a-natural-history-of-animals-and-an-introduction-to-comparative-anatomy-zoology-342-mollusca-fissure-from-the-exterior-surface-being-marked-with-a-longitudinal-gutter-on-one-side-or-with-two-or-several-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-like-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basis-form-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-the-ammonites-brug-or-snake-stoxes-is-founded-image236750331.htmlRMRN4WCY–. The animal kingdom, arranged after its organization, forming a natural history of animals, and an introduction to comparative anatomy. Zoology. 342 MOLLUSCA.. fissure ; from the exterior surface being marked with a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much like the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stoxes,— Is founded,
. Cuvier's animal kingdom : arranged according to its organization. Animals. 342 MOLLUSCA.. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is founded, for they, also, are only found in a fossil state. They are distingui Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/cuviers-animal-kingdom-arranged-according-to-its-organization-animals-342-mollusca-fissure-from-the-exterior-surface-being-marked-witii-a-longitudinal-gutter-on-one-side-or-with-two-or-several-gutters-towards-the-summit-or-as-that-surface-is-smooth-and-without-gutters-some-fossils-very-much-hke-the-belemnites-but-without-a-cavity-and-even-with-a-protruding-basis-form-the-genus-actinocamax-of-miller-it-is-upon-similar-conjectures-that-the-classification-of-the-ammonites-brug-or-snake-stones-is-founded-for-they-also-are-only-found-in-a-fossil-state-they-are-distingui-image231852444.htmlRMRD5P4C–. Cuvier's animal kingdom : arranged according to its organization. Animals. 342 MOLLUSCA.. fissure ; from the exterior surface being marked witii a longitudinal gutter on one side, or with two or several gutters towards the summit ; or as that surface is smooth and without gutters. Some fossils, very much hke the Belemnites, but without a cavity, and even with a protruding basis, form the genus Actinocamax of Miller. It is upon similar conjectures that the classification of the Ammonites, Brug., or Snake-stones,— Is founded, for they, also, are only found in a fossil state. They are distingui
. Bulletin of the British Museum (Natural History), Geology. . .v|^ xC^ >»1 D Scale 1:2,000,000 'trough' 'shelf' 'swell' Fig. 16 Location of the major 'axes' affecting Lower Chalk sedimentation in England, and their relationship to the thickness of the Actinocamax plenus Marls. Isopachytes (in feet) based on the work of Jefferies (1963) and the present authors. These axes are also used in the delimitation of the provinces discussed in the stratigraphic account. 68. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - c Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-of-the-british-museum-natural-history-geology-v-xc-gt1-d-scale-12000000-trough-shelf-swell-fig-16-location-of-the-major-axes-affecting-lower-chalk-sedimentation-in-england-and-their-relationship-to-the-thickness-of-the-actinocamax-plenus-marls-isopachytes-in-feet-based-on-the-work-of-jefferies-1963-and-the-present-authors-these-axes-are-also-used-in-the-delimitation-of-the-provinces-discussed-in-the-stratigraphic-account-68-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-c-image233961578.htmlRMRGHTAJ–. Bulletin of the British Museum (Natural History), Geology. . .v|^ xC^ >»1 D Scale 1:2,000,000 'trough' 'shelf' 'swell' Fig. 16 Location of the major 'axes' affecting Lower Chalk sedimentation in England, and their relationship to the thickness of the Actinocamax plenus Marls. Isopachytes (in feet) based on the work of Jefferies (1963) and the present authors. These axes are also used in the delimitation of the provinces discussed in the stratigraphic account. 68. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - c
. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Fig. 69. BacuUtes sulcatus Baily, 1855. Typical form. Suture lines. A. SAM-PCP8152. B. SAM-PCP8153. C. SAM-PCP8661. Scale bar for size. Kennedy (1984: 146). Unfortunately, neither the lectotype nor any of the other paralectotypes could be traced by us in the collections in Bonn, and we have to assume that they are lost. Subsequent records of B. brevicosta all have to viewed with caution. The specimens from the Lower Senonian of Sweden (with Actinocamax quadrata) from Eriksdal, Sweden, described and f Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annals-of-the-south-african-museum-=-annale-van-die-suid-afrikaanse-museum-natural-history-fig-69-bacuutes-sulcatus-baily-1855-typical-form-suture-lines-a-sam-pcp8152-b-sam-pcp8153-c-sam-pcp8661-scale-bar-for-size-kennedy-1984-146-unfortunately-neither-the-lectotype-nor-any-of-the-other-paralectotypes-could-be-traced-by-us-in-the-collections-in-bonn-and-we-have-to-assume-that-they-are-lost-subsequent-records-of-b-brevicosta-all-have-to-viewed-with-caution-the-specimens-from-the-lower-senonian-of-sweden-with-actinocamax-quadrata-from-eriksdal-sweden-described-and-f-image236410182.htmlRMRMHBGP–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Fig. 69. BacuUtes sulcatus Baily, 1855. Typical form. Suture lines. A. SAM-PCP8152. B. SAM-PCP8153. C. SAM-PCP8661. Scale bar for size. Kennedy (1984: 146). Unfortunately, neither the lectotype nor any of the other paralectotypes could be traced by us in the collections in Bonn, and we have to assume that they are lost. Subsequent records of B. brevicosta all have to viewed with caution. The specimens from the Lower Senonian of Sweden (with Actinocamax quadrata) from Eriksdal, Sweden, described and f
. Bulletin de la Société géologique de France. Geology. 1891 CH. JANET. â NOUVELLES BELEMNITES SENONIENNES 719 Les figures ci-contre donnent la coupe transversale de Y Actinoca- max Grossouvrei et de V Actinocamax Toucasi que nous décrivons plus loin. Fig. 1.. Actinocamax Toucasi Ch. Janet. Section transversale dans la partie la plus renflée. Individu figuré PI. XIV, Fig. 4 a.b.c. 3° Le rostre, au moins chez les individus qui n'ont pas atteint leur entier développement, s'amincit beaucoup plus rapidement vers sa partie antérieure que celui d'A. subventricosus, dont la forme reste touj Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-1891-ch-janet-nouvelles-belemnites-senoniennes-719-les-figures-ci-contre-donnent-la-coupe-transversale-de-y-actinoca-max-grossouvrei-et-de-v-actinocamax-toucasi-que-nous-dcrivons-plus-loin-fig-1-actinocamax-toucasi-ch-janet-section-transversale-dans-la-partie-la-plus-renfle-individu-figur-pi-xiv-fig-4-abc-3-le-rostre-au-moins-chez-les-individus-qui-nont-pas-atteint-leur-entier-dveloppement-samincit-beaucoup-plus-rapidement-vers-sa-partie-antrieure-que-celui-da-subventricosus-dont-la-forme-reste-touj-image234091415.htmlRMRGRNYK–. Bulletin de la Société géologique de France. Geology. 1891 CH. JANET. â NOUVELLES BELEMNITES SENONIENNES 719 Les figures ci-contre donnent la coupe transversale de Y Actinoca- max Grossouvrei et de V Actinocamax Toucasi que nous décrivons plus loin. Fig. 1.. Actinocamax Toucasi Ch. Janet. Section transversale dans la partie la plus renflée. Individu figuré PI. XIV, Fig. 4 a.b.c. 3° Le rostre, au moins chez les individus qui n'ont pas atteint leur entier développement, s'amincit beaucoup plus rapidement vers sa partie antérieure que celui d'A. subventricosus, dont la forme reste touj
. Bulletin de la Société géologique de France. Geology. EXC. A CHAILVET, LAON, ETC. 739 le sentier s'encaisse entre deux talus formés par l'assise à Ditrupa strangulata doiomitisée*. Il court ensuite, jusqu'à MontbavinS sur un plateau aride, formé par le Calcaire grossier marin. Après avoir marché, pendant quelques instants, à la surface de ce plateau, on descend vers Ghaillevois, et l'on reprend à Ghailvet- Urcel le train pour Laon. Après le déjeuner, les voitures nous conduisent à Molinchart. La route se déroule, en grande partie, sur la craie sénonienne, à Actinocamax qaadratus, Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-exc-a-chailvet-laon-etc-739-le-sentier-sencaisse-entre-deux-talus-forms-par-lassise-ditrupa-strangulata-doiomitise-il-court-ensuite-jusqu-montbavins-sur-un-plateau-aride-form-par-le-calcaire-grossier-marin-aprs-avoir-march-pendant-quelques-instants-la-surface-de-ce-plateau-on-descend-vers-ghaillevois-et-lon-reprend-ghailvet-urcel-le-train-pour-laon-aprs-le-djeuner-les-voitures-nous-conduisent-molinchart-la-route-se-droule-en-grande-partie-sur-la-craie-snonienne-actinocamax-qaadratus-image234053870.htmlRMRGP22P–. Bulletin de la Société géologique de France. Geology. EXC. A CHAILVET, LAON, ETC. 739 le sentier s'encaisse entre deux talus formés par l'assise à Ditrupa strangulata doiomitisée*. Il court ensuite, jusqu'à MontbavinS sur un plateau aride, formé par le Calcaire grossier marin. Après avoir marché, pendant quelques instants, à la surface de ce plateau, on descend vers Ghaillevois, et l'on reprend à Ghailvet- Urcel le train pour Laon. Après le déjeuner, les voitures nous conduisent à Molinchart. La route se déroule, en grande partie, sur la craie sénonienne, à Actinocamax qaadratus,
. Annales des sciences naturelles. TIBLE DES PLANCHES REIATIVES AUX MEMOIllES CONTENUS DANS CE VOLDME. P1.ANCHS I. A. Conlracdon musculaire. — B. Termes fossile. 2. Méliponidcs. 3. Métamorphose des Diptères. 4. Anatomie des Arachnides. 5. Anatomie de la Pyrochroa coccinea. 6. A. Anatomie de la Pyrochroa coccinea. - A. Psychoda nerrosa. — C. Actinocamax. Artemia salina. f Corps de Wolf. 7- 8. 9- 10. II. Architecture des Abeilles. FIN DE LA TABLE DU TREIZIÈME VOLUME. Ekhata de lu Note sur l'architecture des Abeilles. Moraldi, /ûe2;MaraIdi, aux pages 358 , ligne 4 , et 36^ clignes 3 w i3 , ç/i Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annales-des-sciences-naturelles-tible-des-planches-reiatives-aux-memoilles-contenus-dans-ce-voldme-p1anchs-i-a-conlracdon-musculaire-b-termes-fossile-2-mliponidcs-3-mtamorphose-des-diptres-4-anatomie-des-arachnides-5-anatomie-de-la-pyrochroa-coccinea-6-a-anatomie-de-la-pyrochroa-coccinea-a-psychoda-nerrosa-c-actinocamax-artemia-salina-f-corps-de-wolf-7-8-9-10-ii-architecture-des-abeilles-fin-de-la-table-du-treizime-volume-ekhata-de-lu-note-sur-larchitecture-des-abeilles-moraldi-e2maraidi-aux-pages-358-ligne-4-et-36-clignes-3-w-i3-i-image236612834.htmlRMRMXJ2A–. Annales des sciences naturelles. TIBLE DES PLANCHES REIATIVES AUX MEMOIllES CONTENUS DANS CE VOLDME. P1.ANCHS I. A. Conlracdon musculaire. — B. Termes fossile. 2. Méliponidcs. 3. Métamorphose des Diptères. 4. Anatomie des Arachnides. 5. Anatomie de la Pyrochroa coccinea. 6. A. Anatomie de la Pyrochroa coccinea. - A. Psychoda nerrosa. — C. Actinocamax. Artemia salina. f Corps de Wolf. 7- 8. 9- 10. II. Architecture des Abeilles. FIN DE LA TABLE DU TREIZIÈME VOLUME. Ekhata de lu Note sur l'architecture des Abeilles. Moraldi, /ûe2;MaraIdi, aux pages 358 , ligne 4 , et 36^ clignes 3 w i3 , ç/i
. Bulletin de la Société géologique de France. Geology. 116 AUGUSïA HURE conséquence de provoquer, près Saint-Martin-du-Tertre, l'appa- rition de la zone à Galeola papillosa, caractérisant les couches supérieures de l'assise k Actinocamax quadratus. Dans le pointe- ment de craie sur lequel s'appuie la tombelle la plus au N., et même un peu plus bas, nous avons recueilli plusieurs de ces Echinides, ainsi qu'un fragment de Micraster que, malgré son mauvais état, nous considérons comme Micr. Schroderi Stolley (ancien M. pseudoglyphus de Grossouvre), et assez particulier à ce niveau. D Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-116-augusa-hure-consquence-de-provoquer-prs-saint-martin-du-tertre-lappa-rition-de-la-zone-galeola-papillosa-caractrisant-les-couches-suprieures-de-lassise-k-actinocamax-quadratus-dans-le-pointe-ment-de-craie-sur-lequel-sappuie-la-tombelle-la-plus-au-n-et-mme-un-peu-plus-bas-nous-avons-recueilli-plusieurs-de-ces-echinides-ainsi-quun-fragment-de-micraster-que-malgr-son-mauvais-tat-nous-considrons-comme-micr-schroderi-stolley-ancien-m-pseudoglyphus-de-grossouvre-et-assez-particulier-ce-niveau-d-image234057528.htmlRMRGP6NC–. Bulletin de la Société géologique de France. Geology. 116 AUGUSïA HURE conséquence de provoquer, près Saint-Martin-du-Tertre, l'appa- rition de la zone à Galeola papillosa, caractérisant les couches supérieures de l'assise k Actinocamax quadratus. Dans le pointe- ment de craie sur lequel s'appuie la tombelle la plus au N., et même un peu plus bas, nous avons recueilli plusieurs de ces Echinides, ainsi qu'un fragment de Micraster que, malgré son mauvais état, nous considérons comme Micr. Schroderi Stolley (ancien M. pseudoglyphus de Grossouvre), et assez particulier à ce niveau. D
. Bulletin de la Société belge de géologie, de paléontologie et d'hydrologie. Geology; Paleontology. 14 A. RUTOT. â NOTE SUR LA FAUNE DES COUCHES 25 B. mucronata et à B. quadrata, dans la Craie de Trivières, près de Mons ; et pour mieux confirmer le fait de l'association des trois formes au même niveau, je viens de découvrir la présence de nombreux Actinocamax verus à la base du Hervien, aux environs de Visé. GASTROPODES. Dentalium alternans, Mùll. Parmi les espèces recueillies dans les concrétions gréseuses gros- sières, glauconifères de la partie inférieure du Crétacé de S Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-de-la-socit-belge-de-gologie-de-palontologie-et-dhydrologie-geology-paleontology-14-a-rutot-note-sur-la-faune-des-couches-25-b-mucronata-et-b-quadrata-dans-la-craie-de-trivires-prs-de-mons-et-pour-mieux-confirmer-le-fait-de-lassociation-des-trois-formes-au-mme-niveau-je-viens-de-dcouvrir-la-prsence-de-nombreux-actinocamax-verus-la-base-du-hervien-aux-environs-de-vis-gastropodes-dentalium-alternans-mll-parmi-les-espces-recueillies-dans-les-concrtions-grseuses-gros-sires-glauconifres-de-la-partie-infrieure-du-crtac-de-s-image234094669.htmlRMRGRX3W–. Bulletin de la Société belge de géologie, de paléontologie et d'hydrologie. Geology; Paleontology. 14 A. RUTOT. â NOTE SUR LA FAUNE DES COUCHES 25 B. mucronata et à B. quadrata, dans la Craie de Trivières, près de Mons ; et pour mieux confirmer le fait de l'association des trois formes au même niveau, je viens de découvrir la présence de nombreux Actinocamax verus à la base du Hervien, aux environs de Visé. GASTROPODES. Dentalium alternans, Mùll. Parmi les espèces recueillies dans les concrétions gréseuses gros- sières, glauconifères de la partie inférieure du Crétacé de S
. Bulletin de la Société géologique de France. Geology. Actinocamax Toucasi Ch. Janet. Section transversale dans la partie la plus renflée. Individu figuré PI. XIV, Fig. 4 a.b.c. 3° Le rostre, au moins chez les individus qui n'ont pas atteint leur entier développement, s'amincit beaucoup plus rapidement vers sa partie antérieure que celui d'A. subventricosus, dont la forme reste toujours beaucoup plus cylindrique. 4° Il y a, un peu au-dessous des bords de l'alvéole, à peu près au niveau de l'ovisac, un léger rétrécissement qui n'existe guère chez A. subventricosus. 5° La fente Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-actinocamax-toucasi-ch-janet-section-transversale-dans-la-partie-la-plus-renfle-individu-figur-pi-xiv-fig-4-abc-3-le-rostre-au-moins-chez-les-individus-qui-nont-pas-atteint-leur-entier-dveloppement-samincit-beaucoup-plus-rapidement-vers-sa-partie-antrieure-que-celui-da-subventricosus-dont-la-forme-reste-toujours-beaucoup-plus-cylindrique-4-il-y-a-un-peu-au-dessous-des-bords-de-lalvole-peu-prs-au-niveau-de-lovisac-un-lger-rtrcissement-qui-nexiste-gure-chez-a-subventricosus-5-la-fente-image234091405.htmlRMRGRNY9–. Bulletin de la Société géologique de France. Geology. Actinocamax Toucasi Ch. Janet. Section transversale dans la partie la plus renflée. Individu figuré PI. XIV, Fig. 4 a.b.c. 3° Le rostre, au moins chez les individus qui n'ont pas atteint leur entier développement, s'amincit beaucoup plus rapidement vers sa partie antérieure que celui d'A. subventricosus, dont la forme reste toujours beaucoup plus cylindrique. 4° Il y a, un peu au-dessous des bords de l'alvéole, à peu près au niveau de l'ovisac, un léger rétrécissement qui n'existe guère chez A. subventricosus. 5° La fente
. 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/image-license-details/?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
. Bulletin de la Société géologique de France. Geology. 404 F. PRIEM 16 Dec. supérieur, depuis le Génomanien jusque dans le Sénonien supé- rieur (craie à Actinocamax quadratus). On peut citer aussi du même gisement (coll. du Muséum) un fragment dune grande vertèbre de Squale. SÃNONIEN Scapanorhynchus subulatus Ag. sp. â Cette espèce a été recueillie à l'état de dents incomplètes par M. Paul Lemoine dans le Sénonien d'Antsirane et d'une localité désignée sous le nom de col de l'Embrasure. Je rapporte avec doute à cette espèce un frag- ment de dent antérieure (coll. Paul Lem Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-404-f-priem-16-dec-suprieur-depuis-le-gnomanien-jusque-dans-le-snonien-sup-rieur-craie-actinocamax-quadratus-on-peut-citer-aussi-du-mme-gisement-coll-du-musum-un-fragment-dune-grande-vertbre-de-squale-snonien-scapanorhynchus-subulatus-ag-sp-cette-espce-a-t-recueillie-ltat-de-dents-incompltes-par-m-paul-lemoine-dans-le-snonien-dantsirane-et-dune-localit-dsigne-sous-le-nom-de-col-de-lembrasure-je-rapporte-avec-doute-cette-espce-un-frag-ment-de-dent-antrieure-coll-paul-lem-image234059619.htmlRMRGP9C3–. Bulletin de la Société géologique de France. Geology. 404 F. PRIEM 16 Dec. supérieur, depuis le Génomanien jusque dans le Sénonien supé- rieur (craie à Actinocamax quadratus). On peut citer aussi du même gisement (coll. du Muséum) un fragment dune grande vertèbre de Squale. SÃNONIEN Scapanorhynchus subulatus Ag. sp. â Cette espèce a été recueillie à l'état de dents incomplètes par M. Paul Lemoine dans le Sénonien d'Antsirane et d'une localité désignée sous le nom de col de l'Embrasure. Je rapporte avec doute à cette espèce un frag- ment de dent antérieure (coll. Paul Lem
. Bulletin de la Société géologique de France. Geology. Corax falcatus Ag. â La collection du Muséum renferme aussi une dent de Corax falcatus (fig. 6), provenant du Sénonien de la Montagne des Français (M. Schneebli, Muséum 1900-12). Elle est ici figurée. Notidanus microdon Ag. â Cette espèce se trouve depuis le Céno- manien jusque dans le Sénonien supérieur (craie à Actinocamax quadratus). Elle est représentée dans le Sénonien de la Montagne des Français (Muséum, M. Schnee- bli, 1900-12) par une dent incom- plète ici figurée (fig. 7). Fig. G. â Corax falcatus Ag. Dent vue Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-corax-falcatus-ag-la-collection-du-musum-renferme-aussi-une-dent-de-corax-falcatus-fig-6-provenant-du-snonien-de-la-montagne-des-franais-m-schneebli-musum-1900-12-elle-est-ici-figure-notidanus-microdon-ag-cette-espce-se-trouve-depuis-le-cno-manien-jusque-dans-le-snonien-suprieur-craie-actinocamax-quadratus-elle-est-reprsente-dans-le-snonien-de-la-montagne-des-franais-musum-m-schnee-bli-1900-12-par-une-dent-incom-plte-ici-figure-fig-7-fig-g-corax-falcatus-ag-dent-vue-image234059579.htmlRMRGP9AK–. Bulletin de la Société géologique de France. Geology. Corax falcatus Ag. â La collection du Muséum renferme aussi une dent de Corax falcatus (fig. 6), provenant du Sénonien de la Montagne des Français (M. Schneebli, Muséum 1900-12). Elle est ici figurée. Notidanus microdon Ag. â Cette espèce se trouve depuis le Céno- manien jusque dans le Sénonien supérieur (craie à Actinocamax quadratus). Elle est représentée dans le Sénonien de la Montagne des Français (Muséum, M. Schnee- bli, 1900-12) par une dent incom- plète ici figurée (fig. 7). Fig. G. â Corax falcatus Ag. Dent vue
. Bulletin de la Société géologique de France. Geology. *9°J POISSONS FOSSILES DE MADAGASCAR 465. Corax falcatus Ag. â La collection du Muséum renferme aussi une dent de Corax falcatus (fig. 6), provenant du Sénonien de la Montagne des Français (M. Schneebli, Muséum 1900-12). Elle est ici figurée. Notidanus microdon Ag. â Cette espèce se trouve depuis le Céno- manien jusque dans le Sénonien supérieur (craie à Actinocamax quadratus). Elle est représentée dans le Sénonien de la Montagne des Français (Muséum, M. Schnee- bli, 1900-12) par une dent incom- plète ici figurée (fig. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-de-la-socit-gologique-de-france-geology-9j-poissons-fossiles-de-madagascar-465-corax-falcatus-ag-la-collection-du-musum-renferme-aussi-une-dent-de-corax-falcatus-fig-6-provenant-du-snonien-de-la-montagne-des-franais-m-schneebli-musum-1900-12-elle-est-ici-figure-notidanus-microdon-ag-cette-espce-se-trouve-depuis-le-cno-manien-jusque-dans-le-snonien-suprieur-craie-actinocamax-quadratus-elle-est-reprsente-dans-le-snonien-de-la-montagne-des-franais-musum-m-schnee-bli-1900-12-par-une-dent-incom-plte-ici-figure-fig-image234059597.htmlRMRGP9B9–. Bulletin de la Société géologique de France. Geology. *9°J POISSONS FOSSILES DE MADAGASCAR 465. Corax falcatus Ag. â La collection du Muséum renferme aussi une dent de Corax falcatus (fig. 6), provenant du Sénonien de la Montagne des Français (M. Schneebli, Muséum 1900-12). Elle est ici figurée. Notidanus microdon Ag. â Cette espèce se trouve depuis le Céno- manien jusque dans le Sénonien supérieur (craie à Actinocamax quadratus). Elle est représentée dans le Sénonien de la Montagne des Français (Muséum, M. Schnee- bli, 1900-12) par une dent incom- plète ici figurée (fig.
. Die Leitfossilien, ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen. Paleontology, Stratigraphic; Paleontology. sind relativ schlanker als die ausgewachsener. Zuweilen wurde das Bilduugsgewebe nicht ganz durch Kalkspat erfüllt; die Scheiden bleiben dann locker und sind an der Spitze oft gerunzelt oder verdrückt (Fig. 67). Auch die Umgebung der Alveole ist oft leichter zerstörbar als der übrige Teil des Rostrums; durch Yerwitterung und Abrollung resultieren dann zweiseitig zugespitzte Rostra, die man früher als besondere Gattung, Actinocamax, auffasste (Fig. 66, 2). A Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/die-leitfossilien-ein-handbuch-fr-den-unterricht-und-fr-das-bestimmen-von-versteinerungen-paleontology-stratigraphic-paleontology-sind-relativ-schlanker-als-die-ausgewachsener-zuweilen-wurde-das-bilduugsgewebe-nicht-ganz-durch-kalkspat-erfllt-die-scheiden-bleiben-dann-locker-und-sind-an-der-spitze-oft-gerunzelt-oder-verdrckt-fig-67-auch-die-umgebung-der-alveole-ist-oft-leichter-zerstrbar-als-der-brige-teil-des-rostrums-durch-yerwitterung-und-abrollung-resultieren-dann-zweiseitig-zugespitzte-rostra-die-man-frher-als-besondere-gattung-actinocamax-auffasste-fig-66-2-a-image231521014.htmlRMRCJKBJ–. Die Leitfossilien, ein Handbuch für den Unterricht und für das Bestimmen von Versteinerungen. Paleontology, Stratigraphic; Paleontology. sind relativ schlanker als die ausgewachsener. Zuweilen wurde das Bilduugsgewebe nicht ganz durch Kalkspat erfüllt; die Scheiden bleiben dann locker und sind an der Spitze oft gerunzelt oder verdrückt (Fig. 67). Auch die Umgebung der Alveole ist oft leichter zerstörbar als der übrige Teil des Rostrums; durch Yerwitterung und Abrollung resultieren dann zweiseitig zugespitzte Rostra, die man früher als besondere Gattung, Actinocamax, auffasste (Fig. 66, 2). A
. Description of the fossil remains of Mollusca found in the chalk of England. Cephalopoda. Cephalopoda, Fossil; Paleontology. Fig. A Fig.B 1. Belemnitella mucronata, Schlotheim, Sp. Plate I, figs. 1, 2, and 3. Belemnites, 1° species : Breyn, de Belemnitis, figs. 1—6. Belemnites mucronatus, Schlotheim. Petref., p. 47, No. 4. — — Mantell. Sussex, t. xvi, fig. 1. — — Nilsson. Petrif. Saec, t. ii, fig. 1. — — Sowerby. Min. Conch., t. 600, figs. 2 and 4. Belemnites electrikus. Miller. Geol. Tr., 2d series, vol. ii, t. viii, figs. 18—21. AcTiNOCAMAX VEKUS? Miller. Loc. cit., t. ix, figs. 17 and 18. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/description-of-the-fossil-remains-of-mollusca-found-in-the-chalk-of-england-cephalopoda-cephalopoda-fossil-paleontology-fig-a-figb-1-belemnitella-mucronata-schlotheim-sp-plate-i-figs-1-2-and-3-belemnites-1-species-breyn-de-belemnitis-figs-16-belemnites-mucronatus-schlotheim-petref-p-47-no-4-mantell-sussex-t-xvi-fig-1-nilsson-petrif-saec-t-ii-fig-1-sowerby-min-conch-t-600-figs-2-and-4-belemnites-electrikus-miller-geol-tr-2d-series-vol-ii-t-viii-figs-1821-actinocamax-vekus-miller-loc-cit-t-ix-figs-17-and-18-image231677420.htmlRMRCWPWG–. Description of the fossil remains of Mollusca found in the chalk of England. Cephalopoda. Cephalopoda, Fossil; Paleontology. Fig. A Fig.B 1. Belemnitella mucronata, Schlotheim, Sp. Plate I, figs. 1, 2, and 3. Belemnites, 1° species : Breyn, de Belemnitis, figs. 1—6. Belemnites mucronatus, Schlotheim. Petref., p. 47, No. 4. — — Mantell. Sussex, t. xvi, fig. 1. — — Nilsson. Petrif. Saec, t. ii, fig. 1. — — Sowerby. Min. Conch., t. 600, figs. 2 and 4. Belemnites electrikus. Miller. Geol. Tr., 2d series, vol. ii, t. viii, figs. 18—21. AcTiNOCAMAX VEKUS? Miller. Loc. cit., t. ix, figs. 17 and 18.
