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    584 pictures found

    Scyphocrinus elegans. Upper Silurian (420 million years). Morocco. Plate 60 cm in diameter. - Blouet brothers collection

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    Scyphocrinus elegans. Upper Silurian (420 million years). Morocco. Plate 60 cm in diameter. - Blouet brothers

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Scyphocrinus elegans. Upper Silurian (420 million years). Morocco. Plate 60 cm in diameter. - Blouet brothers collection

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    Trilobite seen from below, with legs (390 million years). Germany. Bundenbach, Germany. - Blouet brothers collection

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    Trilobite seen from below, with legs (390 million years). Germany. Bundenbach, Germany. - Blouet

    © Pascal Goetgheluck / Biosphoto

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    © Pascal Goetgheluck / Biosphoto

    Trilobite seen from below, with legs (390 million years). Germany. Bundenbach, Germany. - Blouet brothers collection

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    The Gardon de Sainte Croix in the Cevennes, Very old Cambrian/Ordovician micaschists deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    RM2551286JPG

    The Gardon de Sainte Croix in the Cevennes, Very old Cambrian/Ordovician micaschists deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cevennes, Very old Cambrian/Ordovician micaschists deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    The Gardon de Sainte Croix in the Cevennes, Very old Cambrian/Ordovician micaschists deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

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    The Gardon de Sainte Croix in the Cevennes, Very old

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cevennes, Very old Cambrian/Ordovician micaschists deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    From the Peña Foratata, view of the Permian red sandstone from the Peña Collarada to the Anayet (ancient volcano), Aragonese Pyrenees, Spain

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    From the Peña Foratata, view of the Permian red sandstone from the Peña Collarada to the Anayet (ancient volcano), Aragonese Pyrenees, Spain

    © Georges Lopez / Biosphoto

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    © Georges Lopez / Biosphoto

    From the Peña Foratata, view of the Permian red sandstone from the Peña Collarada to the Anayet (ancient volcano), Aragonese Pyrenees, Spain

    Trunk of tree horsetail (Calamites) fossilised in Carboniferous sandstone, planted with maritime pine. Diameter 30 cm - length 3 metres - Calamites is a genus of fossil plants of the Sphenophyta group, close to horsetails. Like horsetails, Calamites has articulated stems and sometimes reduced, whorled leaves. The genus lived in the Carboniferous period between 360 and 300 Ma (millions of years ago), Grand Combe, Gard, France

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    Trunk of tree horsetail (Calamites) fossilised in Carboniferous sandstone, planted with maritime pine. Diameter 30 cm - length 3 metres - Calamites

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Trunk of tree horsetail (Calamites) fossilised in Carboniferous sandstone, planted with maritime pine. Diameter 30 cm - length 3 metres - Calamites is a genus of fossil plants of the Sphenophyta group, close to horsetails. Like horsetails, Calamites has articulated stems and sometimes reduced, whorled leaves. The genus lived in the Carboniferous period between 360 and 300 Ma (millions of years ago), Grand Combe, Gard, France

    Foliose lichens (Xanthoparmelia stenophylla) on red pelites, Gorges de Daluis, Southern Alps, France

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    Foliose lichens (Xanthoparmelia stenophylla) on red pelites, Gorges de Daluis, Southern Alps, France

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Foliose lichens (Xanthoparmelia stenophylla) on red pelites, Gorges de Daluis, Southern Alps, France

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

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    The Gardon de Sainte Croix in the Cévennes, very ancient

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    RM2496044JPG

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    RM2496043JPG

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

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    The Gardon de Sainte Croix in the Cévennes, very ancient

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The Gardon de Sainte Croix in the Cévennes, very ancient micaschists of Cambrian/Ordovician age deformed by Hercynian tectonics, Le Martinet, St Etienne Vallée Française, Cévennes, France

    Permian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du Barrot

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    Permian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Permian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du Barrot

    Permian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du Barrot

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    Permian pelites in the Daluis Gorges, Alpes Maritimes, France.

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Permian pelites in the Daluis Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Daluis Gorges, Dôme du Barrot

    Snails (Solatopupa cianensis) on Permian pelites of the Gorges du Cians, Alpes Maritimes, France. Endemic species of the Gorges du Cians and Daluis, Dôme du Barrot

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    Snails (Solatopupa cianensis) on Permian pelites of the Gorges du Cians, Alpes Maritimes, France. Endemic species of the Gorges du Cians and Daluis,

    © Jean-Philippe Delobelle / Biosphoto

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    Snails (Solatopupa cianensis) on Permian pelites of the Gorges du Cians, Alpes Maritimes, France. Endemic species of the Gorges du Cians and Daluis, Dôme du Barrot

    Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du Barrot

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    Permian pelites of the Cians Gorges, Alpes Maritimes, France.

    © Jean-Philippe Delobelle / Biosphoto

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    Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du Barrot

    Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du Barrot

    RM2495063JPG

    Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du Barrot

    Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du Barrot

    RM2495062JPG

    Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Gorges du Cians, Dôme du Barrot

    Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du Barrot

    RM2495061JPG

    Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dôme du Barrot

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

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    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez,

    © Jean-Philippe Delobelle / Biosphoto

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    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

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    Graphics in grey-blue shales from the Brioverian period in

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

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    Graphics in grey-blue shales from the Brioverian period in

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    RM2489740JPG

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez,

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Graphics in grey-blue shales from the Brioverian period in Brittany. Brioverian shale in the cove of Ty Marc, Saint Nic, Bay of Douarnenez, Finistère, Brittany, France

    Quarry for the extraction of porphyry wheels in the Esterel Massif. Site exploited until the 18th century - Protected massif of volcanic origin dating from the Permian (primary era) and formed of rhyolites (porphyry) with brilliant colours under the setting sun. Var, France

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    Quarry for the extraction of porphyry wheels in the Esterel Massif. Site exploited until the 18th century - Protected massif of volcanic origin

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    Quarry for the extraction of porphyry wheels in the Esterel Massif. Site exploited until the 18th century - Protected massif of volcanic origin dating from the Permian (primary era) and formed of rhyolites (porphyry) with brilliant colours under the setting sun. Var, France

    The Blavet gorges, a famous site in the Esterel Massif. A protected massif of volcanic origin dating from the Permian period (primary era) and formed of rhyolites (porphyry) with brilliant colours under the setting sun. Var, France

    RM2466983JPG

    The Blavet gorges, a famous site in the Esterel Massif. A protected massif of volcanic origin dating from the Permian period (primary era) and formed

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The Blavet gorges, a famous site in the Esterel Massif. A protected massif of volcanic origin dating from the Permian period (primary era) and formed of rhyolites (porphyry) with brilliant colours under the setting sun. Var, France

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by rhyolites (porphyries) with brilliant colours under the setting sun. Var, France

    RM2466982JPG

    The creeks of Cap Dramont, in the Esterel Massif. A small

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by rhyolites (porphyries) with brilliant colours under the setting sun. Var, France

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by rhyolites (porphyries) with brilliant colours under the setting sun. Var, France

    RM2466981JPG

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by rhyolites (porphyries) with brilliant colours under the setting sun. Var, France

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by rhyolites (porphyries) with brilliant colours under the setting sun. Var, France

    RM2466980JPG

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by rhyolites (porphyries) with brilliant colours under the setting sun. Var, France

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by rhyolites (porphyries) with brilliant colours under the setting sun. Var, France

    RM2466979JPG

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian

    © Jean-Philippe Delobelle / Biosphoto

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    © Jean-Philippe Delobelle / Biosphoto

    The creeks of Cap Dramont, in the Esterel Massif. A small classified and protected massif created by a volcanic activity dating from the Permian (primary era) and formed by rhyolites (porphyries) with brilliant colours under the setting sun. Var, France

    The Var river in the Gorges de Daluis, Mercantour National Park, Alps, France

    RM2459111JPG

    The Var river in the Gorges de Daluis, Mercantour National Park, Alps, France

    © Michel Rauch / Biosphoto

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    © Michel Rauch / Biosphoto

    The Var river in the Gorges de Daluis, Mercantour National Park, Alps, France

    Dalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, France

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    Dalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures

    © Georges Lopez / Biosphoto

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    Dalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, France

    Dalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, France

    RM2452353JPG

    Dalle aux Arenaygues = stone flowers witnessing the Devonian

    © Georges Lopez / Biosphoto

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    © Georges Lopez / Biosphoto

    Dalle aux Arenaygues = stone flowers witnessing the Devonian 360million years ago. Jean Pierre Dugène discovered it in 2010. Rare circular structures with a radiating shape reminiscent of a cartwheel. In the center of the structure is the opening of a chimney for the escape of water and sand, fossilized. These structures were created during an earthquake in sediments of detrital origin deposited in the shallow sea. These 'Arenaygues' are considered to be the most characteristic and best preserved specimens in the world. Ossau Valley, Pyrenees, France

    Trilobite fossil. Karoo, Western Cape, South Africa

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    Trilobite fossil. Karoo, Western Cape, South Africa

    © Roger de La Harpe / Biosphoto

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    © Roger de La Harpe / Biosphoto

    Trilobite fossil. Karoo, Western Cape, South Africa

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    Fossilised (fossilized) shells, plants and crinoids. Karoo, Western Cape, South Africa.

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    Fossilised (fossilized) shells, plants and crinoids. Karoo, Western Cape, South Africa.

    © Roger de La Harpe / Biosphoto

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    © Roger de La Harpe / Biosphoto

    Fossilised (fossilized) shells, plants and crinoids. Karoo, Western Cape, South Africa.

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    Fossil Fern (Neuropteris sp), Carboniferous, Germany

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    Fossil Fern (Neuropteris sp), Carboniferous, Germany

    © John Cancalosi / Biosphoto

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    Fossil Fern (Neuropteris sp), Carboniferous, Germany

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    Fossil Fern (Neurpteris ovata), Carboniferus, New Mexico

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    Fossil Fern (Neurpteris ovata), Carboniferus, New Mexico

    © John Cancalosi / Biosphoto

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    © John Cancalosi / Biosphoto

    Fossil Fern (Neurpteris ovata), Carboniferus, New Mexico

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    Fossil Crinoid - Siphocrinite sp. - Ordovician - Morocco

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    Fossil Crinoid - Siphocrinite sp. - Ordovician - Morocco

    © John Cancalosi / Biosphoto

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    © John Cancalosi / Biosphoto

    Fossil Crinoid - Siphocrinite sp. - Ordovician - Morocco

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    Fossil Trilobites - Symphysurus sp. - Ordovician - Morocco

    RM2443409JPG

    Fossil Trilobites - Symphysurus sp. - Ordovician - Morocco

    © John Cancalosi / Biosphoto

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    © John Cancalosi / Biosphoto

    Fossil Trilobites - Symphysurus sp. - Ordovician - Morocco

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    Fossil Lungfish - Osteolepis panderi - Mid Devonian - Caithness - Scotland

    RM2443407JPG

    Fossil Lungfish - Osteolepis panderi - Mid Devonian - Caithness - Scotland

    © John Cancalosi / Biosphoto

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    © John Cancalosi / Biosphoto

    Fossil Lungfish - Osteolepis panderi - Mid Devonian - Caithness - Scotland

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    Fossil lungfish - Dipterus sp. - Mid Devonian - Caithness - Scotland

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    Fossil lungfish - Dipterus sp. - Mid Devonian - Caithness - Scotland

    © John Cancalosi / Biosphoto

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    © John Cancalosi / Biosphoto

    Fossil lungfish - Dipterus sp. - Mid Devonian - Caithness - Scotland

    Restrictions:
    • Sale prohibited in Spain and Portugal
    • Non exclusive sale, exclusive sale possible in France
    Coelacanths - Cardiosuctor sp. - Carboniferous - Bear Gulch - Montana - USA - 250 million years old

    RM2443403JPG

    Coelacanths - Cardiosuctor sp. - Carboniferous - Bear Gulch - Montana - USA - 250 million years old

    © John Cancalosi / Biosphoto

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    © John Cancalosi / Biosphoto

    Coelacanths - Cardiosuctor sp. - Carboniferous - Bear Gulch - Montana - USA - 250 million years old

    Restrictions:
    • Sale prohibited in Spain and Portugal
    • Non exclusive sale, exclusive sale possible in France
    Fossil Amphibian (Sclerocephalus hauseri) - Germany - Permian

    RM2443402JPG

    Fossil Amphibian (Sclerocephalus hauseri) - Germany - Permian

    © John Cancalosi / Biosphoto

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    2443402
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    © John Cancalosi / Biosphoto

    Fossil Amphibian (Sclerocephalus hauseri) - Germany - Permian

    Restrictions:
    • Sale prohibited in Spain and Portugal
    • Non exclusive sale, exclusive sale possible in France
    Fossil Stromatolite - Conophytum basalticum - Cambrian - Australia - Katherine - Northern Territory

    RM2443398JPG

    Fossil Stromatolite - Conophytum basalticum - Cambrian - Australia - Katherine - Northern Territory

    © John Cancalosi / Biosphoto

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    2443398
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    © John Cancalosi / Biosphoto

    Fossil Stromatolite - Conophytum basalticum - Cambrian - Australia - Katherine - Northern Territory

    Restrictions:
    • Sale prohibited in Spain and Portugal
    • Non exclusive sale, exclusive sale possible in France
    Fossil Stromatolite - Conophytum basalticum - Cambrian - Australia - Katherine - Northern Territory

    RM2443397JPG

    Fossil Stromatolite - Conophytum basalticum - Cambrian -

    © John Cancalosi / Biosphoto

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    2443397
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    © John Cancalosi / Biosphoto

    Fossil Stromatolite - Conophytum basalticum - Cambrian - Australia - Katherine - Northern Territory

    Restrictions:
    • Sale prohibited in Spain and Portugal
    • Non exclusive sale, exclusive sale possible in France
    Fossil Crinoid (Jimbacrinus bostocki) - Early Permian - Gascoyne Junction - Western Australia

    RM2443396JPG

    Fossil Crinoid (Jimbacrinus bostocki) - Early Permian - Gascoyne Junction - Western Australia

    © John Cancalosi / Biosphoto

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    2443396
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    © John Cancalosi / Biosphoto

    Fossil Crinoid (Jimbacrinus bostocki) - Early Permian - Gascoyne Junction - Western Australia

    Restrictions:
    • Sale prohibited in Spain and Portugal
    • Non exclusive sale, exclusive sale possible in France
    Fossil fish - Paramblypterus sp. - Permian - Germany - Actinopte

    RM2443388JPG

    Fossil fish - Paramblypterus sp. - Permian - Germany - Actinopte

    © John Cancalosi / Biosphoto

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    2443388
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    © John Cancalosi / Biosphoto

    Fossil fish - Paramblypterus sp. - Permian - Germany - Actinopte

    Restrictions:
    • Sale prohibited in Spain and Portugal
    • Non exclusive sale, exclusive sale possible in France
    Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, nodular granite of Castanheira, Geopark of Arouca, Portugal. These nodules are symbol of fertility in the local tradition (Pedras Parideiras)

    RM2437634JPG

    Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, nodular granite of Castanheira, Geopark of

    © Jean-Philippe Delobelle / Biosphoto

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    2437634
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    © Jean-Philippe Delobelle / Biosphoto

    Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, nodular granite of Castanheira, Geopark of Arouca, Portugal. These nodules are symbol of fertility in the local tradition (Pedras Parideiras)

    Erosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, Portugal

    RM2437626JPG

    Erosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, Portugal

    © Jean-Philippe Delobelle / Biosphoto

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    2437626
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    © Jean-Philippe Delobelle / Biosphoto

    Erosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, Portugal

    Observation system of the nodular granite of Castanheira, Geopark of Arouca, Portugal. Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, These nodules are symbol of fertility in the local tradition, Pedras Parideiras.

    RM2437625JPG

    Observation system of the nodular granite of Castanheira, Geopark of Arouca, Portugal. Exceptional granite of Hercynian age, rich in enormous nodules

    © Jean-Philippe Delobelle / Biosphoto

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    2437625
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    © Jean-Philippe Delobelle / Biosphoto

    Observation system of the nodular granite of Castanheira, Geopark of Arouca, Portugal. Exceptional granite of Hercynian age, rich in enormous nodules of biotite, surrounding a quartz nucleus, These nodules are symbol of fertility in the local tradition, Pedras Parideiras.

    Daedalus desglandi trace fossil in a quarzite of the Ordovician, enigmatic fossil of a few centimeters, present in the quarzites of the Lower Paleozoic, Geopark of Villuercas, Extremadura, Spain

    RM2437345JPG

    Daedalus desglandi trace fossil in a quarzite of the Ordovician, enigmatic fossil of a few centimeters, present in the quarzites of the Lower

    © Jean-Philippe Delobelle / Biosphoto

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    2437345
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    © Jean-Philippe Delobelle / Biosphoto

    Daedalus desglandi trace fossil in a quarzite of the Ordovician, enigmatic fossil of a few centimeters, present in the quarzites of the Lower Paleozoic, Geopark of Villuercas, Extremadura, Spain

    Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)

    RM2437333JPG

    Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by

    © Jean-Philippe Delobelle / Biosphoto

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    2437333
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    © Jean-Philippe Delobelle / Biosphoto

    Polychrome strata of Playa del Silencio, Asturias, Spain. Spectacular variegated and tortured strata of quartzite, sandstone and schists, deformed by the tectonic and dating from the Paleozoic (Cambrian / Ordovician)

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