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    Birthplace of Georges Cuvier, born and died in Montbéliard 1769-1832, rue Cuvier, Montbéliard, Doubs, France

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    Birthplace of Georges Cuvier, born and died in Montbéliard

    © Denis Bringard / Biosphoto

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    © Denis Bringard / Biosphoto

    Birthplace of Georges Cuvier, born and died in Montbéliard 1769-1832, rue Cuvier, Montbéliard, Doubs, France

    Empreintes fossilisées de mammifères de l'époque Oligocene dans le Luberon (dalle de Saignon). Empreinte à 3 doigts de Ronzotherium (Rhinoceros), et à 2 doigts d'Entélodon (Phacochère). Ancien rivage boueux d'un lac, la dalle à empreintes fossiles de Saignon est un site exceptionnel où sont conservées des centaines de traces de pas de mammifères (des parents du rhinocéros, du chevrotain ou du phacochère) et des empreintes d’oiseaux, animaux qui peuplaient le Luberon il y a 33 millions d’années. Les sites à empreintes de pas fossiles de mammifères sont très rares à l’échelle de la planète. Le Luberon en présente plusieurs, dont la dalle de Carlet à Saignon. Geoparc du Luberon. France

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    Empreintes fossilisées de mammifères de l'époque Oligocene dans le Luberon (dalle de Saignon). Empreinte à 3 doigts de Ronzotherium (Rhinoceros), et

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Empreintes fossilisées de mammifères de l'époque Oligocene dans le Luberon (dalle de Saignon). Empreinte à 3 doigts de Ronzotherium (Rhinoceros), et à 2 doigts d'Entélodon (Phacochère). Ancien rivage boueux d'un lac, la dalle à empreintes fossiles de Saignon est un site exceptionnel où sont conservées des centaines de traces de pas de mammifères (des parents du rhinocéros, du chevrotain ou du phacochère) et des empreintes d’oiseaux, animaux qui peuplaient le Luberon il y a 33 millions d’années. Les sites à empreintes de pas fossiles de mammifères sont très rares à l’échelle de la planète. Le Luberon en présente plusieurs, dont la dalle de Carlet à Saignon. Geoparc du Luberon. France

    Fossilized mammal footprints from the Oligocene period in the Luberon (Saignon slab). Footprint of Ronzotherium (Rhinoceros) and Entelodon (Warthog). A former muddy lake shore, the Saignon fossil footprint slab is an exceptional site where hundreds of mammal footprints (relatives of the rhinoceros, chevrotain and warthog) and bird prints are preserved, animals that populated the Luberon 33 million years ago. Fossilized mammal footprint sites are extremely rare worldwide. The Luberon has several, including the Carlet slab in Saignon. Geoparc du Luberon. France

    RM2596302JPG

    Fossilized mammal footprints from the Oligocene period in the Luberon (Saignon slab). Footprint of Ronzotherium (Rhinoceros) and Entelodon (Warthog).

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Fossilized mammal footprints from the Oligocene period in the Luberon (Saignon slab). Footprint of Ronzotherium (Rhinoceros) and Entelodon (Warthog). A former muddy lake shore, the Saignon fossil footprint slab is an exceptional site where hundreds of mammal footprints (relatives of the rhinoceros, chevrotain and warthog) and bird prints are preserved, animals that populated the Luberon 33 million years ago. Fossilized mammal footprint sites are extremely rare worldwide. The Luberon has several, including the Carlet slab in Saignon. Geoparc du Luberon. France

    Fossilized footprints of mammals from the Oligocene da period. A former muddy lakeshore, the Saignon fossil footprint slab is an exceptional site containing hundreds of mammal footprints (relatives of the rhinoceros, chevrotain and warthog) and bird prints, animals that populated the Luberon 33 million years ago. Fossilized mammal footprint sites are extremely rare worldwide. The Luberon has several, including the Carlet slab in Saignon. Geoparc du Luberon. France

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    Fossilized footprints of mammals from the Oligocene da period. A

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Fossilized footprints of mammals from the Oligocene da period. A former muddy lakeshore, the Saignon fossil footprint slab is an exceptional site containing hundreds of mammal footprints (relatives of the rhinoceros, chevrotain and warthog) and bird prints, animals that populated the Luberon 33 million years ago. Fossilized mammal footprint sites are extremely rare worldwide. The Luberon has several, including the Carlet slab in Saignon. Geoparc du Luberon. France

    Fossilized footprints of mammals from the Oligocene da period. A former muddy lakeshore, the Saignon fossil footprint slab is an exceptional site containing hundreds of mammal footprints (relatives of the rhinoceros, chevrotain and warthog) and bird prints, animals that populated the Luberon 33 million years ago. Fossilized mammal footprint sites are extremely rare worldwide. The Luberon has several, including the Carlet slab in Saignon. Geoparc du Luberon. France

    RM2596300JPG

    Fossilized footprints of mammals from the Oligocene da period. A former muddy lakeshore, the Saignon fossil footprint slab is an exceptional site

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Fossilized footprints of mammals from the Oligocene da period. A former muddy lakeshore, the Saignon fossil footprint slab is an exceptional site containing hundreds of mammal footprints (relatives of the rhinoceros, chevrotain and warthog) and bird prints, animals that populated the Luberon 33 million years ago. Fossilized mammal footprint sites are extremely rare worldwide. The Luberon has several, including the Carlet slab in Saignon. Geoparc du Luberon. France

    Fossilized footprints of mammals from the Oligocene da period. A former muddy lakeshore, the Saignon fossil footprint slab is an exceptional site containing hundreds of mammal footprints (relatives of the rhinoceros, chevrotain and warthog) and bird prints, animals that populated the Luberon 33 million years ago. Fossilized mammal footprint sites are extremely rare worldwide. The Luberon has several, including the Carlet slab in Saignon. Geoparc du Luberon. France

    RM2596299JPG

    Fossilized footprints of mammals from the Oligocene da period. A former muddy lakeshore, the Saignon fossil footprint slab is an exceptional site

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Fossilized footprints of mammals from the Oligocene da period. A former muddy lakeshore, the Saignon fossil footprint slab is an exceptional site containing hundreds of mammal footprints (relatives of the rhinoceros, chevrotain and warthog) and bird prints, animals that populated the Luberon 33 million years ago. Fossilized mammal footprint sites are extremely rare worldwide. The Luberon has several, including the Carlet slab in Saignon. Geoparc du Luberon. France

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for their rich paleontological content. Some thirty different species of ammonites have been recorded in the Tuilière sections, and belemnite rostrums are abundant in certain levels, as are gastropods and lamellibranchs (oysters and plicatula). These marls also yield corals, sea urchins, brachiopods and shark teeth. The Aptian is the penultimate stratigraphic stage of the Lower Cretaceous. It extends from ≃ -121.4 to ≃ -113.0 Ma, succeeding the Barremian and preceding the Albian (Secondary or Mesozoic Era). France

    RM2596282JPG

    Small pyrite ammonites in Aptian grey marls. The gray marls

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for their rich paleontological content. Some thirty different species of ammonites have been recorded in the Tuilière sections, and belemnite rostrums are abundant in certain levels, as are gastropods and lamellibranchs (oysters and plicatula). These marls also yield corals, sea urchins, brachiopods and shark teeth. The Aptian is the penultimate stratigraphic stage of the Lower Cretaceous. It extends from ≃ -121.4 to ≃ -113.0 Ma, succeeding the Barremian and preceding the Albian (Secondary or Mesozoic Era). France

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for their rich paleontological content. Some thirty different species of ammonites have been recorded in the Tuilière sections, and belemnite rostrums are abundant in certain levels, as are gastropods and lamellibranchs (oysters and plicatula). These marls also yield corals, sea urchins, brachiopods and shark teeth. The Aptian is the penultimate stratigraphic stage of the Lower Cretaceous. It extends from ≃ -121.4 to ≃ -113.0 Ma, succeeding the Barremian and preceding the Albian (Secondary or Mesozoic Era). France

    RM2596281JPG

    Small pyrite ammonites in Aptian grey marls. The gray marls

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for their rich paleontological content. Some thirty different species of ammonites have been recorded in the Tuilière sections, and belemnite rostrums are abundant in certain levels, as are gastropods and lamellibranchs (oysters and plicatula). These marls also yield corals, sea urchins, brachiopods and shark teeth. The Aptian is the penultimate stratigraphic stage of the Lower Cretaceous. It extends from ≃ -121.4 to ≃ -113.0 Ma, succeeding the Barremian and preceding the Albian (Secondary or Mesozoic Era). France

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for their rich paleontological content. Some thirty different species of ammonites have been recorded in the Tuilière sections, and belemnite rostrums are abundant in certain levels, as are gastropods and lamellibranchs (oysters and plicatula). These marls also yield corals, sea urchins, brachiopods and shark teeth. The Aptian is the penultimate stratigraphic stage of the Lower Cretaceous. It extends from ≃ -121.4 to ≃ -113.0 Ma, succeeding the Barremian and preceding the Albian (Secondary or Mesozoic Era). France

    RM2596280JPG

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for their rich paleontological content. Some thirty different species of ammonites have been recorded in the Tuilière sections, and belemnite rostrums are abundant in certain levels, as are gastropods and lamellibranchs (oysters and plicatula). These marls also yield corals, sea urchins, brachiopods and shark teeth. The Aptian is the penultimate stratigraphic stage of the Lower Cretaceous. It extends from ≃ -121.4 to ≃ -113.0 Ma, succeeding the Barremian and preceding the Albian (Secondary or Mesozoic Era). France

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for their rich paleontological content. Some thirty different species of ammonites have been recorded in the Tuilière sections, and belemnite rostrums are abundant in certain levels, as are gastropods and lamellibranchs (oysters and plicatula). These marls also yield corals, sea urchins, brachiopods and shark teeth. The Aptian is the penultimate stratigraphic stage of the Lower Cretaceous. It extends from ≃ -121.4 to ≃ -113.0 Ma, succeeding the Barremian and preceding the Albian (Secondary or Mesozoic Era). France

    RM2596279JPG

    Small pyrite ammonites in Aptian grey marls. The gray marls

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Small pyrite ammonites in Aptian grey marls. The gray marls around Apt were proposed by Alcide d'Orbigny as a reference for the Aptian stage, for their rich paleontological content. Some thirty different species of ammonites have been recorded in the Tuilière sections, and belemnite rostrums are abundant in certain levels, as are gastropods and lamellibranchs (oysters and plicatula). These marls also yield corals, sea urchins, brachiopods and shark teeth. The Aptian is the penultimate stratigraphic stage of the Lower Cretaceous. It extends from ≃ -121.4 to ≃ -113.0 Ma, succeeding the Barremian and preceding the Albian (Secondary or Mesozoic Era). France

    Dry algae on paramoudras (sandstone ball) hollows. Jaizkibel coastal massif - Basque Country - Spain

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    Dry algae on paramoudras (sandstone ball) hollows. Jaizkibel

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Dry algae on paramoudras (sandstone ball) hollows. Jaizkibel coastal massif - Basque Country - Spain

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

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    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    RM2595757JPG

    The paramoudras of Jaizkibel, on Spain's Basque Coast.

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    RM2595756JPG

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    RM2595755JPG

    The paramoudras of Jaizkibel, on Spain's Basque Coast.

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The paramoudras of Jaizkibel, on Spain's Basque Coast. Spectacular sandstone fossil concretions formed around the burrows of marine worms living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes are 20 to 40 cm in diameter and were originally flexible - The holes are the worms' galleries - Jaizkibel coastal massif - Basque Country - Spain

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin (fossilized biological activity) and uncovered by erosion - the yellow discs are "paramoudras", concretions around the burrows of deep-sea marine worms - Jaizkibel coastal massif - Spain

    RM2595750JPG

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin (fossilized biological activity) and uncovered by erosion - the yellow discs are "paramoudras", concretions around the burrows of deep-sea marine worms - Jaizkibel coastal massif - Spain

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin (fossilized biological activity) and uncovered by erosion - the yellow discs are "paramoudras", concretions around the burrows of deep-sea marine worms - Jaizkibel coastal massif - Spain

    RM2595749JPG

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Polychrome graphics in the Jaizkibel sandstone on Spain's Basque Coast. Remarkable Eocene sandstone structures (geoforms) of partly biological origin (fossilized biological activity) and uncovered by erosion - the yellow discs are "paramoudras", concretions around the burrows of deep-sea marine worms - Jaizkibel coastal massif - Spain

    Natural honeycomb lace (Geoforms) in sandstone from Jaizkibel (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological origin (fossil biological activities called Paramoudra, concretions around marine worm burrows) and uncovered then sculpted into honeycomb shapes by erosion - Jaizkibel coastal massif - Spain

    RM2595748JPG

    Natural honeycomb lace (Geoforms) in sandstone from Jaizkibel (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Natural honeycomb lace (Geoforms) in sandstone from Jaizkibel (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological origin (fossil biological activities called Paramoudra, concretions around marine worm burrows) and uncovered then sculpted into honeycomb shapes by erosion - Jaizkibel coastal massif - Spain

    Natural lacework (geoforms) in Jaizkibel sandstone (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological origin (fossilized biological activities known as Paramoudra, concretions around marine worm burrows) uncovered and sculpted into honeycomb shapes by erosion - Jaizkibel coastal massif - Spain

    RM2595747JPG

    Natural lacework (geoforms) in Jaizkibel sandstone (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Natural lacework (geoforms) in Jaizkibel sandstone (Spanish Basque Country). Remarkable Eocene sandstone sculptures (geoforms) of partly biological origin (fossilized biological activities known as Paramoudra, concretions around marine worm burrows) uncovered and sculpted into honeycomb shapes by erosion - Jaizkibel coastal massif - Spain

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en partie biologique (activités biologiques fossiles appelées Paramoudra, concrétions autour des terriers de vers marins) et mises à jour puis sculptées en nid d'abeille par l'érosion - Massif côtier de Jaizkibel - Espagne

    RM2595746JPG

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en partie biologique (activités biologiques fossiles appelées Paramoudra, concrétions autour des terriers de vers marins) et mises à jour puis sculptées en nid d'abeille par l'érosion - Massif côtier de Jaizkibel - Espagne

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en partie biologique (activités biologiques fossiles appelées Paramoudra, concrétions autour des terriers de vers marins) et mises à jour puis sculptées en nid d'abeille par l'érosion - Massif côtier de Jaizkibel - Espagne

    RM2595745JPG

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Dentelles naturelles (Géoformes) dans les grès de Jaizkibel (Pays Basque espagnol). Remarquables sculptures de grès éocènes (géoformes) d'origine en partie biologique (activités biologiques fossiles appelées Paramoudra, concrétions autour des terriers de vers marins) et mises à jour puis sculptées en nid d'abeille par l'érosion - Massif côtier de Jaizkibel - Espagne

    Broken fossils of rudists in a limestone rock in Biscay. Bivalve from the Secondary Era, with very uneven, rough valves, one horn-shaped and attached to the rocks, the other flat and serving as a lid. (The accumulation of rudists has formed veritable reefs ["rudist limestones"] where all the usual fauna of reef facies can be found. Basque Country, Spain

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    Broken fossils of rudists in a limestone rock in Biscay. Bivalve from the Secondary Era, with very uneven, rough valves, one horn-shaped and attached

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Broken fossils of rudists in a limestone rock in Biscay. Bivalve from the Secondary Era, with very uneven, rough valves, one horn-shaped and attached to the rocks, the other flat and serving as a lid. (The accumulation of rudists has formed veritable reefs ["rudist limestones"] where all the usual fauna of reef facies can be found. Basque Country, Spain

    Petrified trees in the Namib Desert, Sossusvlei-Deadvlei-Sesriem, Namibia

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    Petrified trees in the Namib Desert, Sossusvlei-Deadvlei-Sesriem, Namibia

    © Christophe Ravier / Biosphoto

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    © Christophe Ravier / Biosphoto

    Petrified trees in the Namib Desert, Sossusvlei-Deadvlei-Sesriem, Namibia

    Petrified trees in the Namib Desert, Sossusvlei-Deadvlei-Sesriem, Namibia

    RM2593369JPG

    Petrified trees in the Namib Desert, Sossusvlei-Deadvlei-Sesriem, Namibia

    © Christophe Ravier / Biosphoto

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    © Christophe Ravier / Biosphoto

    Petrified trees in the Namib Desert, Sossusvlei-Deadvlei-Sesriem, Namibia

    Ammonite fossil and chocolate slug (Arion rufus), Vosges du Nord Regional Nature Park, France

    RM2574812JPG

    Ammonite fossil and chocolate slug (Arion rufus), Vosges du

    © Michel Rauch / Biosphoto

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    © Michel Rauch / Biosphoto

    Ammonite fossil and chocolate slug (Arion rufus), Vosges du Nord Regional Nature Park, France

    Rio Martin Nature Reserve: Archosaur footprints from the Triassic period, Teruel Province, Spain

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    Rio Martin Nature Reserve: Archosaur footprints from the Triassic period, Teruel Province, Spain

    © Georges Lopez / Biosphoto

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    © Georges Lopez / Biosphoto

    Rio Martin Nature Reserve: Archosaur footprints from the Triassic period, Teruel Province, Spain

    Rio Martin Natural Park: Archosaur footprints from the Triassic period, Teruel Province, Spain

    RM2574617JPG

    Rio Martin Natural Park: Archosaur footprints from the Triassic period, Teruel Province, Spain

    © Georges Lopez / Biosphoto

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    © Georges Lopez / Biosphoto

    Rio Martin Natural Park: Archosaur footprints from the Triassic period, Teruel Province, Spain

    Dinosaur (Aragosaurus) footprints from the Cretaceous period 120 million years ago, located at the entrance to the village of Ariño, Teruel province, Spain.

    RM2574607JPG

    Dinosaur (Aragosaurus) footprints from the Cretaceous period 120

    © Georges Lopez / Biosphoto

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    © Georges Lopez / Biosphoto

    Dinosaur (Aragosaurus) footprints from the Cretaceous period 120 million years ago, located at the entrance to the village of Ariño, Teruel province, Spain.

    Dinosaur (Aragosaurus) footprints from the Cretaceous period 120 million years ago, located at the entrance to the village of Ariño, Teruel province, Spain.

    RM2574606JPG

    Dinosaur (Aragosaurus) footprints from the Cretaceous period 120 million years ago, located at the entrance to the village of Ariño, Teruel province,

    © Georges Lopez / Biosphoto

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    © Georges Lopez / Biosphoto

    Dinosaur (Aragosaurus) footprints from the Cretaceous period 120 million years ago, located at the entrance to the village of Ariño, Teruel province, Spain.

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    RM2572025JPG

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    © Antoine Lorgnier / Biosphoto

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    © Antoine Lorgnier / Biosphoto

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    RM2572024JPG

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    © Antoine Lorgnier / Biosphoto

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    © Antoine Lorgnier / Biosphoto

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    Fossilized tree trunk approximately 200 million years old (Triassic period). Petrified Forest National Park. Arizona. USA.

    RM2572023JPG

    Fossilized tree trunk approximately 200 million years old

    © Antoine Lorgnier / Biosphoto

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    © Antoine Lorgnier / Biosphoto

    Fossilized tree trunk approximately 200 million years old (Triassic period). Petrified Forest National Park. Arizona. USA.

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    RM2572022JPG

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    © Antoine Lorgnier / Biosphoto

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    © Antoine Lorgnier / Biosphoto

    The Petrified Forest National Park is home to thousands of fossilized tree trunks approximately 200 million years old (Triassic period). Arizona. USA.

    Fossils in marl, Saint-Saturnin-lès-Apt, Luberon Regional Nature Park, France

    RM2561691JPG

    Fossils in marl, Saint-Saturnin-lès-Apt, Luberon Regional Nature Park, France

    © David Tatin / Biosphoto

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    © David Tatin / Biosphoto

    Fossils in marl, Saint-Saturnin-lès-Apt, Luberon Regional Nature Park, France

    Ichthyosaur (Platypteryginae). Luc Ebbo and his large specimen of an Ichthyosaur (Platypteryginae) from the Albian of Provence, certainly one of the most complete ever discovered during the Cretaceous. 5m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552468JPG

    Ichthyosaur (Platypteryginae). Luc Ebbo and his large specimen of an Ichthyosaur (Platypteryginae) from the Albian of Provence, certainly one of the most complete ever discovered

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Ichthyosaur (Platypteryginae). Luc Ebbo and his large specimen of an Ichthyosaur (Platypteryginae) from the Albian of Provence, certainly one of the most complete ever discovered during the Cretaceous. 5m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Hoplites dentatus. Albian of Troy. 15cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552467JPG

    Hoplites dentatus. Albian of Troy. 15cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Hoplites dentatus. Albian of Troy. 15cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Tooth from an indeterminate Pliosaur specimen from the Aptian of Provence. 25cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552466JPG

    Tooth from an indeterminate Pliosaur specimen from the Aptian of Provence. 25cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Tooth from an indeterminate Pliosaur specimen from the Aptian of Provence. 25cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Workshop. Work on the release of fossils with rotary precision tools. Ebbo collection

    RM2552465JPG

    Workshop. Work on the release of fossils with rotary precision tools. Ebbo collection

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Workshop. Work on the release of fossils with rotary precision tools. Ebbo collection

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    Workshop. Work on the release of fossils with rotary precision tools. Ebbo collection

    RM2552464JPG

    Workshop. Work on the release of fossils with rotary precision

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Workshop. Work on the release of fossils with rotary precision tools. Ebbo collection

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    Workshop. Work on the release of fossils with rotary precision tools. Ebbo collection

    RM2552463JPG

    Workshop. Work on the release of fossils with rotary precision tools. Ebbo collection

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Workshop. Work on the release of fossils with rotary precision tools. Ebbo collection

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    Luc Ebbo's collection. Undetermined fish from the Alpine Oligocene. 45cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552462JPG

    Luc Ebbo's collection. Undetermined fish from the Alpine Oligocene. 45cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Luc Ebbo's collection. Undetermined fish from the Alpine Oligocene. 45cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Large specimen of Paleorhynchus glarisianus from the Alpine Oligocene. 1.30m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552461JPG

    Large specimen of Paleorhynchus glarisianus from the Alpine Oligocene. 1.30m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Large specimen of Paleorhynchus glarisianus from the Alpine Oligocene. 1.30m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Large specimen of Paleorhynchus glarisianus from the Alpine Oligocene. 1.30m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552460JPG

    Large specimen of Paleorhynchus glarisianus from the Alpine Oligocene. 1.30m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Large specimen of Paleorhynchus glarisianus from the Alpine Oligocene. 1.30m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Plate of Betelgeusia orientalis starfish from the Barremian of Tamanar (Morocco). 35cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552459JPG

    Plate of Betelgeusia orientalis starfish from the Barremian of Tamanar (Morocco).

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Plate of Betelgeusia orientalis starfish from the Barremian of Tamanar (Morocco). 35cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Tumidocarcinus giganteus. Crab from the Miocene of New Zealand. 30cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552458JPG

    Tumidocarcinus giganteus. Crab from the Miocene of New Zealand. 30cm. Luc

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Tumidocarcinus giganteus. Crab from the Miocene of New Zealand. 30cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Austrian Triassic (Norian) fish cemetery in the Salzburg region resulting from the drying up of a lagoon. Heterolepidotus ornatus. 1m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552457JPG

    Austrian Triassic (Norian) fish cemetery in the Salzburg region resulting from the

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Austrian Triassic (Norian) fish cemetery in the Salzburg region resulting from the drying up of a lagoon. Heterolepidotus ornatus. 1m. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Heterolepidotus ornatus. Triassic ( Norien) from the Salzburg region of Austria. 80cm. Luc Ebbo collection. Paleogalerie, Salignac.Ebbo collection

    RM2552456JPG

    Heterolepidotus ornatus. Triassic ( Norien) from the Salzburg

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Heterolepidotus ornatus. Triassic ( Norien) from the Salzburg region of Austria. 80cm. Luc Ebbo collection. Paleogalerie, Salignac.Ebbo collection

    Restrictions:
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    Nodule of amber from the Albian of Provence (exterior and interior). 20cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552455JPG

    Nodule of amber from the Albian of Provence (exterior and interior). 20cm. Luc Ebbo

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Nodule of amber from the Albian of Provence (exterior and interior). 20cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    Restrictions:
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    Turrilites sp with preservation of Albian spines from Provence. 25cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552454JPG

    Turrilites sp with preservation of Albian spines from Provence.

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Turrilites sp with preservation of Albian spines from Provence. 25cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

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    Turtle shell (Glarichelys sp) from the Alpine Oligocene associated with the disarticulated remains of a large fish. 50cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    RM2552453JPG

    Turtle shell (Glarichelys sp) from the Alpine Oligocene associated with the

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Turtle shell (Glarichelys sp) from the Alpine Oligocene associated with the disarticulated remains of a large fish. 50cm. Luc Ebbo collection. Paleogalerie, Salignac. Ebbo collection

    Restrictions:
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