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Wolf (Canis lupus) on mudflats, Great Bear Rainforest, British Columbia, CanadaWolf (Canis lupus) on mudflats, Great Bear Rainforest, British Columbia, CanadaWolf (Canis lupus) on mudflats, Great Bear Rainforest, British Columbia, Canada© Jack Chapman / BiosphotoJPG - RM

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Wolf (Canis lupus) on mudflats, Great Bear Rainforest, British

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Octopus (Octopus sp.) spewing his ink in the lagoon, Mayotte, Indian Ocean.Octopus (Octopus sp.) spewing his ink in the lagoon, Mayotte, Indian Ocean.Octopus (Octopus sp.) spewing his ink in the lagoon, Mayotte, Indian Ocean.© Gabriel Barathieu / BiosphotoJPG - RM

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Octopus (Octopus sp.) spewing his ink in the lagoon, Mayotte,

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Octopus (Octopus sp) displaying in the lagoon, Mayotte, Indian Ocean. Winner of the UPY 2017 (Underwater Photographer of the year).Octopus (Octopus sp) displaying in the lagoon, Mayotte, Indian Ocean. Winner of the UPY 2017 (Underwater Photographer of the year).Octopus (Octopus sp) displaying in the lagoon, Mayotte, Indian Ocean. Winner of the UPY 2017 (Underwater Photographer of the year).© Gabriel Barathieu / BiosphotoJPG - RM

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Octopus (Octopus sp) displaying in the lagoon, Mayotte, Indian

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Octopus (Octopus sp) spreading its tentacles in the lagoon, Mayotte, Indian Ocean.Octopus (Octopus sp) spreading its tentacles in the lagoon, Mayotte, Indian Ocean.Octopus (Octopus sp) spreading its tentacles in the lagoon, Mayotte, Indian Ocean.© Gabriel Barathieu / BiosphotoJPG - RM

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Octopus (Octopus sp) spreading its tentacles in the lagoon,

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Octopus (Octopus sp) displaying in the lagoon, Mayotte, Indian Ocean.Octopus (Octopus sp) displaying in the lagoon, Mayotte, Indian Ocean.Octopus (Octopus sp) displaying in the lagoon, Mayotte, Indian Ocean.© Gabriel Barathieu / BiosphotoJPG - RM

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Octopus (Octopus sp) displaying in the lagoon, Mayotte, Indian

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Corals on the surface of the water during the great tides in the lagoon of Mayotte, in the background : Mount Choungi, Indian OceanCorals on the surface of the water during the great tides in the lagoon of Mayotte, in the background : Mount Choungi, Indian OceanCorals on the surface of the water during the great tides in the lagoon of Mayotte, in the background : Mount Choungi, Indian Ocean© Gabriel Barathieu / BiosphotoJPG - RM

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Corals on the surface of the water during the great tides in the

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Night Storm over the Bridge of Oléron Island - France ; Many storms have succeeded on the night of 7 to 8 May 2015 at Fort Louvois.Night Storm over the Bridge of Oléron Island - FranceNight Storm over the Bridge of Oléron Island - France ; Many storms have succeeded on the night of 7 to 8 May 2015 at Fort Louvois.© Xavier Delorme / BiosphotoJPG - RM

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Night Storm over the Bridge of Oléron Island - France ; Many

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Degradation stormy night on the Fort Louvois - France ; Many storms have succeeded on the night of 7 to 8 May 2015 at Fort Louvois.Degradation stormy night on the Fort Louvois - FranceDegradation stormy night on the Fort Louvois - France ; Many storms have succeeded on the night of 7 to 8 May 2015 at Fort Louvois.© Xavier Delorme / BiosphotoJPG - RM

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Degradation stormy night on the Fort Louvois - France ; Many

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Degradation stormy night on the Fort Louvois - France ; Many storms have succeeded on the night of May 4 to 5, 2015 at Fort Louvois.<br>Overlays 5 photos 30 seconds of exposure is 2 minutes 30.Degradation stormy night on the Fort Louvois - FranceDegradation stormy night on the Fort Louvois - France ; Many storms have succeeded on the night of May 4 to 5, 2015 at Fort Louvois.
Overlays 5 photos 30 seconds of exposure is 2 minutes 30.
© Xavier Delorme / BiosphotoJPG - RM

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Degradation stormy night on the Fort Louvois - France ; Many

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High tide at Mont Saint-Michel at night - France High tide at Mont Saint-Michel at night - France High tide at Mont Saint-Michel at night - France © Vincent M. & E. Studler / BiosphotoJPG - RMSale prohibited by Agents

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High tide at Mont Saint-Michel at night - France

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High tide at Mont Saint-Michel at night - France High tide at Mont Saint-Michel at night - France High tide at Mont Saint-Michel at night - France © Vincent M. & E. Studler / BiosphotoJPG - RMSale prohibited by Agents

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High tide at Mont Saint-Michel at night - France

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High tide at Mont Saint-Michel at night - France High tide at Mont Saint-Michel at night - France High tide at Mont Saint-Michel at night - France © Vincent M. & E. Studler / BiosphotoJPG - RMSale prohibited by Agents

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High tide at Mont Saint-Michel at night - France

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Gathering of Red Knots for large tidal Norfolk ; Grand Prix Festival of Namur in 2012.<br>Highly Commended in Russian Contest Golden Turtle'7Gathering of Red Knots for large tidal NorfolkGathering of Red Knots for large tidal Norfolk ; Grand Prix Festival of Namur in 2012.
Highly Commended in Russian Contest Golden Turtle'7
© Marc Weber / BiosphotoJPG - RM

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Gathering of Red Knots for large tidal Norfolk ; Grand Prix

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Giants Causeway Ireland Giants Causeway Ireland Giants Causeway Ireland © David Allemand / BiosphotoJPG - RM

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Giants Causeway Ireland 

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Bar-tailed Godwit (Limosa lapponica) immature migrating sounding seawater at low tide looking for annelid worms, Finistère, FranceBar-tailed Godwit (Limosa lapponica) immature migrating sounding seawater at low tide looking for annelid worms, Finistère, FranceBar-tailed Godwit (Limosa lapponica) immature migrating sounding seawater at low tide looking for annelid worms, Finistère, France© Jean Mayet / BiosphotoJPG - RM

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Bar-tailed Godwit (Limosa lapponica) immature migrating sounding

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Common Cuttlefish (Sepia officinalis) at low tide in the Jospinet mussels in Planguenoual, Brittany, FranceCommon Cuttlefish (Sepia officinalis) at low tide in the Jospinet mussels in Planguenoual, Brittany, FranceCommon Cuttlefish (Sepia officinalis) at low tide in the Jospinet mussels in Planguenoual, Brittany, France© Jean-Luc & Françoise Ziegler / BiosphotoJPG - RM

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Common Cuttlefish (Sepia officinalis) at low tide in the Jospinet

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Strips of paper flutter with the wind to scare the birds in the Jospinet mussels in Planguenoual, Brittany, FranceStrips of paper flutter with the wind to scare the birds in the Jospinet mussels in Planguenoual, Brittany, FranceStrips of paper flutter with the wind to scare the birds in the Jospinet mussels in Planguenoual, Brittany, France© Jean-Luc & Françoise Ziegler / BiosphotoJPG - RM

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Strips of paper flutter with the wind to scare the birds in the

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Young Herring Gull (Larus argentatus) on the beach with Sanderling (Calidris alba), Brittany, FranceYoung Herring Gull (Larus argentatus) on the beach with Sanderling (Calidris alba), Brittany, FranceYoung Herring Gull (Larus argentatus) on the beach with Sanderling (Calidris alba), Brittany, France© Michel Rauch / BiosphotoJPG - RM

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Young Herring Gull (Larus argentatus) on the beach with

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Oscillation Ripples at Low Tide, Praia de Amoreira, PortugalOscillation Ripples at Low Tide, Praia de Amoreira, PortugalOscillation Ripples at Low Tide, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Oscillation Ripples at Low Tide, Praia de Amoreira, Portugal

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Oscillation Ripples at Low Tide, Praia de Amoreira, PortugalOscillation Ripples at Low Tide, Praia de Amoreira, PortugalOscillation Ripples at Low Tide, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Oscillation Ripples at Low Tide, Praia de Amoreira, Portugal

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular flysch formations in southern Portugal, The flysch

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular flysch formations in southern Portugal, The flysch

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular flysch formations in southern Portugal, The flysch

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular flysch formations in southern Portugal, The flysch

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Spectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, PortugalSpectacular flysch formations in southern Portugal, The flysch result from repeated submarine avalanches over millions of years, depositing alternating strata of limestone, marl and sandstone, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular flysch formations in southern Portugal, The flysch

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Erosion Pots on the Portuguese Coast, Praia de Amoreira, PortugalErosion Pots on the Portuguese Coast, Praia de Amoreira, PortugalErosion Pots on the Portuguese Coast, Praia de Amoreira, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Erosion Pots on the Portuguese Coast, Praia de Amoreira, Portugal

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Spectacular marine cave of Algar de Benagil, Algarve, PortugalSpectacular marine cave of Algar de Benagil, Algarve, PortugalSpectacular marine cave of Algar de Benagil, Algarve, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular marine cave of Algar de Benagil, Algarve, Portugal

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Spectacular marine cave of Algar de Benagil, Algarve, PortugalSpectacular marine cave of Algar de Benagil, Algarve, PortugalSpectacular marine cave of Algar de Benagil, Algarve, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Spectacular marine cave of Algar de Benagil, Algarve, Portugal

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Ponta da Piedade at rising tide, Jagged ocher cliffs, reference landscape of the Algarve, southern province of PortugalPonta da Piedade at rising tide, Jagged ocher cliffs, reference landscape of the Algarve, southern province of PortugalPonta da Piedade at rising tide, Jagged ocher cliffs, reference landscape of the Algarve, southern province of Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Ponta da Piedade at rising tide, Jagged ocher cliffs, reference

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Coastal fog and pebbles, Praia do Abano, Portugal. Mists forming daily on the still cold sea in May, Cape Roca Region, PortugalCoastal fog and pebbles, Praia do Abano, Portugal. Mists forming daily on the still cold sea in May, Cape Roca Region, PortugalCoastal fog and pebbles, Praia do Abano, Portugal. Mists forming daily on the still cold sea in May, Cape Roca Region, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Coastal fog and pebbles, Praia do Abano, Portugal. Mists forming

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Coastal fog and pebbles, Praia do Abano, Portugal. Mists forming daily on the still cold sea in May, Cape Roca Region, PortugalCoastal fog and pebbles, Praia do Abano, Portugal. Mists forming daily on the still cold sea in May, Cape Roca Region, PortugalCoastal fog and pebbles, Praia do Abano, Portugal. Mists forming daily on the still cold sea in May, Cape Roca Region, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Coastal fog and pebbles, Praia do Abano, Portugal. Mists forming

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437365

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437364

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437363

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437362

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437361

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437359

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437358

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437357

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437356

Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Remarkable flysch formations of Deba, Basque Coast Geopark,

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Petrified quartzite wave from 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)Petrified quartzite wave from 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)Petrified quartzite wave from 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)© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Petrified quartzite wave from Playa del Silencio, Asturias,

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Le fort d'Ambleteuse, Hauts de France, FranceLe fort d'Ambleteuse, Hauts de France, FranceLe fort d'Ambleteuse, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Le fort d'Ambleteuse, Hauts de France, France

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Le fort d'Ambleteuse, Hauts de France, FranceLe fort d'Ambleteuse, Hauts de France, FranceLe fort d'Ambleteuse, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Le fort d'Ambleteuse, Hauts de France, France

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Sangatte beach at sunset, Hauts de France, FranceSangatte beach at sunset, Hauts de France, FranceSangatte beach at sunset, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Sangatte beach at sunset, Hauts de France, France

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The English coast from Escalles, Hauts de France, FranceThe English coast from Escalles, Hauts de France, FranceThe English coast from Escalles, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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The English coast from Escalles, Hauts de France, France

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Sky at sunset, Escalles, Hauts de France, FranceSky at sunset, Escalles, Hauts de France, FranceSky at sunset, Escalles, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Sky at sunset, Escalles, Hauts de France, France

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Latice fence chestnut wood retaining the sand on the beach of Calais, autumn, Hauts de France, FranceLatice fence chestnut wood retaining the sand on the beach of Calais, autumn, Hauts de France, FranceLatice fence chestnut wood retaining the sand on the beach of Calais, autumn, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Latice fence chestnut wood retaining the sand on the beach of

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Beach cabins, Calais, Hauts de France, FranceBeach cabins, Calais, Hauts de France, FranceBeach cabins, Calais, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Beach cabins, Calais, Hauts de France, France

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Recovery of a cardinal buoy stranded on the beach of Calais, Hauts de France, FranceRecovery of a cardinal buoy stranded on the beach of Calais, Hauts de France, FranceRecovery of a cardinal buoy stranded on the beach of Calais, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Recovery of a cardinal buoy stranded on the beach of Calais,

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Cardinal buoy stranded on the beach of Calais, Hauts de France, FranceCardinal buoy stranded on the beach of Calais, Hauts de France, FranceCardinal buoy stranded on the beach of Calais, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

2437185

Cardinal buoy stranded on the beach of Calais, Hauts de France,

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St Guénolé Rocks, Penmarc'h, Brittany, FranceSt Guénolé Rocks, Penmarc'h, Brittany, FranceSt Guénolé Rocks, Penmarc'h, Brittany, France© Michel Rauch / BiosphotoJPG - RM

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St Guénolé Rocks, Penmarc'h, Brittany, France

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Sanderling sandpiper (Calidris alba) by the sea, Brittany, FranceSanderling sandpiper (Calidris alba) by the sea, Brittany, FranceSanderling sandpiper (Calidris alba) by the sea, Brittany, France© Michel Rauch / BiosphotoJPG - RM

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Sanderling sandpiper (Calidris alba) by the sea, Brittany, France

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Pointe de la Torche and St Guénolé Rocks, Penmarc'h, Brittany, FrancePointe de la Torche and St Guénolé Rocks, Penmarc'h, Brittany, FrancePointe de la Torche and St Guénolé Rocks, Penmarc'h, Brittany, France© Michel Rauch / BiosphotoJPG - RM

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Pointe de la Torche and St Guénolé Rocks, Penmarc'h, Brittany,

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The wreck of the Lord Grey at blue hour, Opal Coast, Hauts de France, FranceThe wreck of the Lord Grey at blue hour, Opal Coast, Hauts de France, FranceThe wreck of the Lord Grey at blue hour, Opal Coast, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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The wreck of the Lord Grey at blue hour, Opal Coast, Hauts de

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Cliffs of Cap Gris-nez, Opal Coast, Pas de Calais, FranceCliffs of Cap Gris-nez, Opal Coast, Pas de Calais, FranceCliffs of Cap Gris-nez, Opal Coast, Pas de Calais, France© Yann Avril / BiosphotoJPG - RM

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Cliffs of Cap Gris-nez, Opal Coast, Pas de Calais, France

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Cap blanc-nez, Opal Coast, Pas de Calais, FranceCap blanc-nez, Opal Coast, Pas de Calais, FranceCap blanc-nez, Opal Coast, Pas de Calais, France© Yann Avril / BiosphotoJPG - RM

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Cap blanc-nez, Opal Coast, Pas de Calais, France

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Bay of Diego-Suarez, sacred island Nosy Lonja, one of the 3 most beautiful bays in the world, inland sea of 174 km of coastline, North MadagascarBay of Diego-Suarez, sacred island Nosy Lonja, one of the 3 most beautiful bays in the world, inland sea of 174 km of coastline, North MadagascarBay of Diego-Suarez, sacred island Nosy Lonja, one of the 3 most beautiful bays in the world, inland sea of 174 km of coastline, North Madagascar© Jean Mayet / BiosphotoJPG - RM

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Bay of Diego-Suarez, sacred island Nosy Lonja, one of the 3 most

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King penguins, Aptenodytes patagonica, going to the sea, Volunteer Point, Falkland IslandsKing penguins, Aptenodytes patagonica, going to the sea, Volunteer Point, Falkland IslandsKing penguins, Aptenodytes patagonica, going to the sea, Volunteer Point, Falkland Islands© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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King penguins, Aptenodytes patagonica, going to the sea,

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King penguins, Aptenodytes patagonica, going to the sea, Volunteer Point, Falkland IslandsKing penguins, Aptenodytes patagonica, going to the sea, Volunteer Point, Falkland IslandsKing penguins, Aptenodytes patagonica, going to the sea, Volunteer Point, Falkland Islands© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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King penguins, Aptenodytes patagonica, going to the sea,

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Three King penguins, Aptenodytes patagonica, on Volunteer Point beach.Three King penguins, Aptenodytes patagonica, on Volunteer Point beach.Three King penguins, Aptenodytes patagonica, on Volunteer Point beach.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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Three King penguins, Aptenodytes patagonica, on Volunteer Point

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Four King penguins, Aptenodytes patagonica, walking on Volunteer Point beach, Falkland IslandsFour King penguins, Aptenodytes patagonica, walking on Volunteer Point beach, Falkland IslandsFour King penguins, Aptenodytes patagonica, walking on Volunteer Point beach, Falkland Islands© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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Four King penguins, Aptenodytes patagonica, walking on Volunteer

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Two King penguins, Aptenodytes patagonica, on a white sandy beach, Volunteer Point, Falkland Islands.Two King penguins, Aptenodytes patagonica, on a white sandy beach, Volunteer Point, Falkland Islands.Two King penguins, Aptenodytes patagonica, on a white sandy beach, Volunteer Point, Falkland Islands.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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Two King penguins, Aptenodytes patagonica, on a white sandy

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Portrait of two King penguins, Aptenodytes patagonica, on a white sandy beach, Volunteer Point, Falkland IslandsPortrait of two King penguins, Aptenodytes patagonica, on a white sandy beach, Volunteer Point, Falkland IslandsPortrait of two King penguins, Aptenodytes patagonica, on a white sandy beach, Volunteer Point, Falkland Islands© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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Portrait of two King penguins, Aptenodytes patagonica, on a white

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Bay of Arcachon Delta Leyre at low tide, grouping of mute swans (Cygnus olor) during moulting, Gironde, FranceBay of Arcachon Delta Leyre at low tide, grouping of mute swans (Cygnus olor) during moulting, Gironde, FranceBay of Arcachon Delta Leyre at low tide, grouping of mute swans (Cygnus olor) during moulting, Gironde, France© Stéphan Bonneau / BiosphotoJPG - RM

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Bay of Arcachon Delta Leyre at low tide, grouping of mute swans

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Bassin d'Arcachon, Ile aux oiseaux at low tide, Gironde, FranceBassin d'Arcachon, Ile aux oiseaux at low tide, Gironde, FranceBassin d'Arcachon, Ile aux oiseaux at low tide, Gironde, France© Stéphan Bonneau / BiosphotoJPG - RM

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Bassin d'Arcachon, Ile aux oiseaux at low tide, Gironde, France

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Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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Antarctic fur seal (Arctocephalus gazella), Deception Island,

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Tourists in the warm waters of Whaler's Bay, Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.Tourists in the warm waters of Whaler's Bay, Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.Tourists in the warm waters of Whaler's Bay, Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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Tourists in the warm waters of Whaler's Bay, Antarctic fur seal

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A tourist in the warm waters of Whaler's Bay, Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.A tourist in the warm waters of Whaler's Bay, Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.A tourist in the warm waters of Whaler's Bay, Antarctic fur seal (Arctocephalus gazella), Deception Island, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

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A tourist in the warm waters of Whaler's Bay, Antarctic fur seal

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Coastal erosion, The sea current is taking over the dune few meters every year washing down the forest to the sea, Baie d'Authie, Pas-de-Calais, Hauts-de-France, FranceCoastal erosion, The sea current is taking over the dune few meters every year washing down the forest to the sea, Baie d'Authie, Pas-de-Calais, Hauts-de-France, FranceCoastal erosion, The sea current is taking over the dune few meters every year washing down the forest to the sea, Baie d'Authie, Pas-de-Calais, Hauts-de-France, France© Antoine Lorgnier / BiosphotoJPG - RM

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Coastal erosion, The sea current is taking over the dune few

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Coastal erosion, The sea current is taking over the dune few meters every year washing down the forest to the sea, Baie d'Authie, Pas-de-Calais, Hauts-de-France, FranceCoastal erosion, The sea current is taking over the dune few meters every year washing down the forest to the sea, Baie d'Authie, Pas-de-Calais, Hauts-de-France, FranceCoastal erosion, The sea current is taking over the dune few meters every year washing down the forest to the sea, Baie d'Authie, Pas-de-Calais, Hauts-de-France, France© Antoine Lorgnier / BiosphotoJPG - RM

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Coastal erosion, The sea current is taking over the dune few

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Moon Jellyfish (Aurelia aurita) stranded on a beach in summer, Hauts de France, FranceMoon Jellyfish (Aurelia aurita) stranded on a beach in summer, Hauts de France, FranceMoon Jellyfish (Aurelia aurita) stranded on a beach in summer, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Moon Jellyfish (Aurelia aurita) stranded on a beach in summer,

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Moon Jellyfish (Aurelia aurita) stranded on a beach in summer, Hauts de France, FranceMoon Jellyfish (Aurelia aurita) stranded on a beach in summer, Hauts de France, FranceMoon Jellyfish (Aurelia aurita) stranded on a beach in summer, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Moon Jellyfish (Aurelia aurita) stranded on a beach in summer,

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Kayaks on Scoresbysund beach, North East GreenlandKayaks on Scoresbysund beach, North East GreenlandKayaks on Scoresbysund beach, North East Greenland© Pierre Vernay / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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Kayaks on Scoresbysund beach, North East Greenland

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Kayakers pulling their kayaks on sandy shoals, in Scoresbysund, North East GreenlandKayakers pulling their kayaks on sandy shoals, in Scoresbysund, North East GreenlandKayakers pulling their kayaks on sandy shoals, in Scoresbysund, North East Greenland© Pierre Vernay / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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Kayakers pulling their kayaks on sandy shoals, in Scoresbysund,

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Progression at low tide in Scoresbysund where sandbanks are numerous on the north shore, North East GreenlandProgression at low tide in Scoresbysund where sandbanks are numerous on the north shore, North East GreenlandProgression at low tide in Scoresbysund where sandbanks are numerous on the north shore, North East Greenland© Pierre Vernay / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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Progression at low tide in Scoresbysund where sandbanks are

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Kayaker pulling his kayak on the shoals of Scoresbysund, North East GreenlandKayaker pulling his kayak on the shoals of Scoresbysund, North East GreenlandKayaker pulling his kayak on the shoals of Scoresbysund, North East Greenland© Pierre Vernay / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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Kayaker pulling his kayak on the shoals of Scoresbysund, North

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Kayak explorer in Scoresbysund, North East GreenlandKayak explorer in Scoresbysund, North East GreenlandKayak explorer in Scoresbysund, North East Greenland© Pierre Vernay / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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Kayak explorer in Scoresbysund, North East Greenland

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Dune and Grande Côte Beach, La Barre-de-Monts, Ocean-Marais de Monts, Vendée, FranceDune and Grande Côte Beach, La Barre-de-Monts, Ocean-Marais de Monts, Vendée, FranceDune and Grande Côte Beach, La Barre-de-Monts, Ocean-Marais de Monts, Vendée, France© Emile Barbelette / BiosphotoJPG - RM

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Dune and Grande Côte Beach, La Barre-de-Monts, Ocean-Marais de

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Fisherman coming back from the clam fishery, Bourgneuf Bay, Pays de Loire, FranceFisherman coming back from the clam fishery, Bourgneuf Bay, Pays de Loire, FranceFisherman coming back from the clam fishery, Bourgneuf Bay, Pays de Loire, France© Emile Barbelette / BiosphotoJPG - RM

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Fisherman coming back from the clam fishery, Bourgneuf Bay, Pays

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Landscape of mudflat with background oyster activity, Baie de Bourgneuf, Pays de RetzLandscape of mudflat with background oyster activity, Baie de Bourgneuf, Pays de RetzLandscape of mudflat with background oyster activity, Baie de Bourgneuf, Pays de Retz© Emile Barbelette / BiosphotoJPG - RM

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Landscape of mudflat with background oyster activity, Baie de

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Waders: Dunlin (Calidris alpina), Black-bellied plover (Pluvialis squatarola), Red Knot (Calidris canutus)on a reef at high tide, North Atlantic, FranceWaders: Dunlin (Calidris alpina), Black-bellied plover (Pluvialis squatarola), Red Knot (Calidris canutus)on a reef at high tide, North Atlantic, FranceWaders: Dunlin (Calidris alpina), Black-bellied plover (Pluvialis squatarola), Red Knot (Calidris canutus)on a reef at high tide, North Atlantic, France© Emile Barbelette / BiosphotoJPG - RM

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Waders: Dunlin (Calidris alpina), Black-bellied plover (Pluvialis

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Lagoon of Dain, Bouin, Reserve LPO, Vendée, FranceLagoon of Dain, Bouin, Reserve LPO, Vendée, FranceLagoon of Dain, Bouin, Reserve LPO, Vendée, France© Emile Barbelette / BiosphotoJPG - RM

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Lagoon of Dain, Bouin, Reserve LPO, Vendée, France

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Tube-building worm (Sabellaria alveolata) tubal worm at low tideTube-building worm (Sabellaria alveolata) tubal worm at low tideTube-building worm (Sabellaria alveolata) tubal worm at low tide© Emile Barbelette / BiosphotoJPG - RM

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Tube-building worm (Sabellaria alveolata) tubal worm at low tide

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Tube-building worm (Sabellaria alveolata) tubal worm at low tideTube-building worm (Sabellaria alveolata) tubal worm at low tideTube-building worm (Sabellaria alveolata) tubal worm at low tide© Emile Barbelette / BiosphotoJPG - RM

2433579

Tube-building worm (Sabellaria alveolata) tubal worm at low tide

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Common cockle (Cerastoderma edule) on a sandy bottom at low tideCommon cockle (Cerastoderma edule) on a sandy bottom at low tideCommon cockle (Cerastoderma edule) on a sandy bottom at low tide© Emile Barbelette / BiosphotoJPG - RM

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Common cockle (Cerastoderma edule) on a sandy bottom at low tide

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Bécasseau variable (Calidris alpina) et Pluvier argenté (Pluvialis squatarola) groupe sur reposoir de marré haute lors du passage migratoire en automneBécasseau variable (Calidris alpina) et Pluvier argenté (Pluvialis squatarola) groupe sur reposoir de marré haute lors du passage migratoire en automneBécasseau variable (Calidris alpina) et Pluvier argenté (Pluvialis squatarola) groupe sur reposoir de marré haute lors du passage migratoire en automne© Emile Barbelette / BiosphotoJPG - RM

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Bécasseau variable (Calidris alpina) et Pluvier argenté

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Sunset from the beach of Sohoa in the North West of Mayotte.Sunset from the beach of Sohoa in the North West of Mayotte.Sunset from the beach of Sohoa in the North West of Mayotte.© Gabriel Barathieu / BiosphotoJPG - RM

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Sunset from the beach of Sohoa in the North West of Mayotte.

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Escalles beach at the foot of Cap Blanc-nez, winter, Hauts de France, FranceEscalles beach at the foot of Cap Blanc-nez, winter, Hauts de France, FranceEscalles beach at the foot of Cap Blanc-nez, winter, Hauts de France, France© Yann Avril / BiosphotoJPG - RM

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Escalles beach at the foot of Cap Blanc-nez, winter, Hauts de

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Panneau information aménagement hydroélectrique de Kembs sur le Rhin, Alsace, FrancePanneau information aménagement hydroélectrique de Kembs sur le Rhin, Alsace, FrancePanneau information aménagement hydroélectrique de Kembs sur le Rhin, Alsace, France© Dominique Delfino / BiosphotoJPG - RM

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Panneau information aménagement hydroélectrique de Kembs sur le

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Baobab and small basin filled with water during high tide and sunset. South MayotteBaobab and small basin filled with water during high tide and sunset. South MayotteBaobab and small basin filled with water during high tide and sunset. South Mayotte© Gabriel Barathieu / BiosphotoJPG - RM

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Baobab and small basin filled with water during high tide and

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Mangrove pneumatophores in the mangrove at low tide at sunset, MayotteMangrove pneumatophores in the mangrove at low tide at sunset, MayotteMangrove pneumatophores in the mangrove at low tide at sunset, Mayotte© Gabriel Barathieu / BiosphotoJPG - RM

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Mangrove pneumatophores in the mangrove at low tide at sunset,

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Grey plover (Pluvialis squatarola) resting at high tide, Bay of St Brieuc, Brittany, FranceGrey plover (Pluvialis squatarola) resting at high tide, Bay of St Brieuc, Brittany, FranceGrey plover (Pluvialis squatarola) resting at high tide, Bay of St Brieuc, Brittany, France© Emile Barbelette / BiosphotoJPG - RM

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Grey plover (Pluvialis squatarola) resting at high tide, Bay of

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Grey plover (Pluvialis squatarola) resting at high tide, Bay of mont Saint Michel, Brittany, FranceGrey plover (Pluvialis squatarola) resting at high tide, Bay of mont Saint Michel, Brittany, FranceGrey plover (Pluvialis squatarola) resting at high tide, Bay of mont Saint Michel, Brittany, France© Emile Barbelette / BiosphotoJPG - RM

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Grey plover (Pluvialis squatarola) resting at high tide, Bay of

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