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Grey Heron (Ardea cinerea). A adult bird standing on the ice during a snowstorm. Taken on a wintering spot in Sweden.Grey Heron (Ardea cinerea). A adult bird standing on the ice during a snowstorm. Taken on a wintering spot in Sweden.Grey Heron (Ardea cinerea). A adult bird standing on the ice during a snowstorm. Taken on a wintering spot in Sweden.© Ivan Sjögren / BiosphotoJPG - RMNon exclusive sale

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Grey Heron (Ardea cinerea). A adult bird standing on the ice

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Titan triggerfish, Balistoides viridescens. Biting a plastic bottled lid. A lot of sea animals ingest plastic garbage because they think it's edible food. Huge amount of plastic garbage at the surface and in midwater. Thilafushi Island. Maldives Digital composite. Composite imageTitan triggerfish, Balistoides viridescens. Biting a plastic bottled lid. A lot of sea animals ingest plastic garbage because they think it's edible food. Huge amount of plastic garbage at the surface and in midwater. Thilafushi Island. Maldives Digital composite. Composite imageTitan triggerfish, Balistoides viridescens. Biting a plastic bottled lid. A lot of sea animals ingest plastic garbage because they think it's edible food. Huge amount of plastic garbage at the surface and in midwater. Thilafushi Island. Maldives Digital composite. Composite image© Paulo de Oliveira / BiosphotoJPG - RMNon exclusive sale
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2395410

Titan triggerfish, Balistoides viridescens. Biting a plastic

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Barn owl (Tyto alba) perched on a fence post while snowing, AnglandBarn owl (Tyto alba) perched on a fence post while snowing, AnglandBarn owl (Tyto alba) perched on a fence post while snowing, Angland© Frédéric Desmette / BiosphotoJPG - RMNon exclusive sale
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2194109

Barn owl (Tyto alba) perched on a fence post while snowing,

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Polar bear inspects a boat from the ice, Spitsbergen, Svalbard, Norwegian archipelago, Norway, Arctic OceanPolar bear inspects a boat from the ice, Spitsbergen, Svalbard, Norwegian archipelago, Norway, Arctic OceanPolar bear inspects a boat from the ice, Spitsbergen, Svalbard, Norwegian archipelago, Norway, Arctic Ocean© Franco Banfi / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

2135052

Polar bear inspects a boat from the ice, Spitsbergen, Svalbard,

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Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017© Franck Gueffier / BiosphotoJPG - RM

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Strong eruption at Mount Sinabung generating large pyroclastic

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Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017Strong eruption at Mount Sinabung generating large pyroclastic flow, August 02, 2017© Franck Gueffier / BiosphotoJPG - RM

2134953

Strong eruption at Mount Sinabung generating large pyroclastic

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Skinny and exhausted Polar bear (Ursus maritimus) on the shore, Spitzbergen, Norway, August 2016Skinny and exhausted Polar bear (Ursus maritimus) on the shore, Spitzbergen, Norway, August 2016Skinny and exhausted Polar bear (Ursus maritimus) on the shore, Spitzbergen, Norway, August 2016© Thierry Vezon / BiosphotoJPG - RM

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Skinny and exhausted Polar bear (Ursus maritimus) on the shore,

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Gull (Larus sp) flying over the ocean unleashed, IcelandGull (Larus sp) flying over the ocean unleashed, IcelandGull (Larus sp) flying over the ocean unleashed, Iceland© Philippe Moës / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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2087854

Gull (Larus sp) flying over the ocean unleashed, Iceland

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Setting midnight sun lights Polar Bear (Ursus maritimus) walking along rocky shoreline by Hudson Bay, Nunavut Territory, CanadaSetting midnight sun lights Polar Bear (Ursus maritimus) walking along rocky shoreline by Hudson Bay, Nunavut Territory, CanadaSetting midnight sun lights Polar Bear (Ursus maritimus) walking along rocky shoreline by Hudson Bay, Nunavut Territory, Canada© Paul Souders / BiosphotoJPG - RMNon exclusive sale

2050876

Setting midnight sun lights Polar Bear (Ursus maritimus) walking

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Polar Bear (Ursus maritimus) swimming past melting iceberg near Harbour Islands, Repulse Bay, Nunavut Territory, CanadaPolar Bear (Ursus maritimus) swimming past melting iceberg near Harbour Islands, Repulse Bay, Nunavut Territory, CanadaPolar Bear (Ursus maritimus) swimming past melting iceberg near Harbour Islands, Repulse Bay, Nunavut Territory, Canada© Paul Souders / BiosphotoJPG - RMNon exclusive sale

2050870

Polar Bear (Ursus maritimus) swimming past melting iceberg near

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Polar Bear (Ursus maritimus) climbing onto melting iceberg near Harbour Islands, Repulse Bay, Nunavut Territory, CanadaPolar Bear (Ursus maritimus) climbing onto melting iceberg near Harbour Islands, Repulse Bay, Nunavut Territory, CanadaPolar Bear (Ursus maritimus) climbing onto melting iceberg near Harbour Islands, Repulse Bay, Nunavut Territory, Canada© Paul Souders / BiosphotoJPG - RMNon exclusive sale

2050868

Polar Bear (Ursus maritimus) climbing onto melting iceberg near

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Polar Bear Cub (Ursus maritimus) beneath mother while standing on sea ice near Harbour Islands, Repulse Bay, Nunavut Territory, CanadaPolar Bear Cub (Ursus maritimus) beneath mother while standing on sea ice near Harbour Islands, Repulse Bay, Nunavut Territory, CanadaPolar Bear Cub (Ursus maritimus) beneath mother while standing on sea ice near Harbour Islands, Repulse Bay, Nunavut Territory, Canada© Paul Souders / BiosphotoJPG - RMNon exclusive sale

2050848

Polar Bear Cub (Ursus maritimus) beneath mother while standing on

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Polar Bear and young cub (Ursus maritimus) cling to melting sea ice at sunset near Harbour Islands, Repulse Bay, Nunavut Territory, CanadaPolar Bear and young cub (Ursus maritimus) cling to melting sea ice at sunset near Harbour Islands, Repulse Bay, Nunavut Territory, CanadaPolar Bear and young cub (Ursus maritimus) cling to melting sea ice at sunset near Harbour Islands, Repulse Bay, Nunavut Territory, Canada© Paul Souders / BiosphotoJPG - RMNon exclusive sale

2050841

Polar Bear and young cub (Ursus maritimus) cling to melting sea

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Thimble jellyfish bloom off Cabilao Island - PhilippinesThimble jellyfish bloom off Cabilao Island - PhilippinesThimble jellyfish bloom off Cabilao Island - Philippines© Franco Banfi / BiosphotoJPG - RM

2048022

Thimble jellyfish bloom off Cabilao Island - Philippines

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White storkin flight at the edge of a bush fire - Masai MaraWhite storkin flight at the edge of a bush fire - Masai MaraWhite storkin flight at the edge of a bush fire - Masai Mara© Michel & Christine Denis-Huot / BiosphotoJPG - RMNon exclusive sale

2034061

White storkin flight at the edge of a bush fire - Masai Mara

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Gentoo penguins in a sandstorm - Falkland Islands Gentoo penguins in a sandstorm - Falkland Islands Gentoo penguins in a sandstorm - Falkland Islands © Alain Mafart-Renodier / BiosphotoJPG - RMNon exclusive sale

2012806

Gentoo penguins in a sandstorm - Falkland Islands

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Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia © Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

1987862

Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia

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Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia © Juan-Carlos Muñoz / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

1987861

Dead acacia trees at Dead Vlei - Sossusvlei Namib Namibia

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Pink anemonefish in bleached Anemone - Raja Ampat IndonesiaPink anemonefish in bleached Anemone - Raja Ampat IndonesiaPink anemonefish in bleached Anemone - Raja Ampat Indonesia© Mike Veitch / BiosphotoJPG - RMNon exclusive sale, exclusive sale in France
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1961855

Pink anemonefish in bleached Anemone - Raja Ampat Indonesia

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Burchell's Zebra in burned savannah - Kruger South AfricaBurchell's Zebra in burned savannah - Kruger South AfricaBurchell's Zebra in burned savannah - Kruger South Africa© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

1935125

Burchell's Zebra in burned savannah - Kruger South Africa

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Visualization flow of water in a sponge - Aquarius Reef Base ; Fluorescein dye is used to visualize how water is absorbed at the outside and then exhausted by a sponge.The Caribbean barrel sponge, Xestospongia muta, is a large and common member of the coral reef communities at depths greater than 10 m, and has been called the “redwood of the deep”, due to its up to 2000 year lifespan as well as its size and color. Despite its prominence, high biomass and importance to habitat complexity and reef health, very little is know about the basic biology of this massive sponge, including rates of mortality and recruitment, reproduction, growth and age. Like reef corals, this sponge is subject to bleaching and subsequent mortality.<br>With support from NOAA's Aquarius Reef Base at UNCW, NOAA's Coral Reef Conservation Program, and the Florida Keys National Marine Sanctuary, a research group has been monitoring populations of X. muta in the Florida Keys since 1997.Visualization flow of water in a sponge - Aquarius Reef BaseVisualization flow of water in a sponge - Aquarius Reef Base ; Fluorescein dye is used to visualize how water is absorbed at the outside and then exhausted by a sponge.The Caribbean barrel sponge, Xestospongia muta, is a large and common member of the coral reef communities at depths greater than 10 m, and has been called the “redwood of the deep”, due to its up to 2000 year lifespan as well as its size and color. Despite its prominence, high biomass and importance to habitat complexity and reef health, very little is know about the basic biology of this massive sponge, including rates of mortality and recruitment, reproduction, growth and age. Like reef corals, this sponge is subject to bleaching and subsequent mortality.
With support from NOAA's Aquarius Reef Base at UNCW, NOAA's Coral Reef Conservation Program, and the Florida Keys National Marine Sanctuary, a research group has been monitoring populations of X. muta in the Florida Keys since 1997.© Christoph Gerigk / BiosphotoJPG - RM

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Visualization flow of water in a sponge - Aquarius Reef Base ;

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Visualization flow of water in a sponge - Aquarius Reef Base ; Fluorescein dye is used to visualize how water is absorbed at the outside and then exhausted by a sponge.The Caribbean barrel sponge, Xestospongia muta, is a large and common member of the coral reef communities at depths greater than 10 m, and has been called the “redwood of the deep”, due to its up to 2000 year lifespan as well as its size and color. Despite its prominence, high biomass and importance to habitat complexity and reef health, very little is know about the basic biology of this massive sponge, including rates of mortality and recruitment, reproduction, growth and age. Like reef corals, this sponge is subject to bleaching and subsequent mortality.<br>With support from NOAA's Aquarius Reef Base at UNCW, NOAA's Coral Reef Conservation Program, and the Florida Keys National Marine Sanctuary, a research group has been monitoring populations of X. muta in the Florida Keys since 1997.Visualization flow of water in a sponge - Aquarius Reef BaseVisualization flow of water in a sponge - Aquarius Reef Base ; Fluorescein dye is used to visualize how water is absorbed at the outside and then exhausted by a sponge.The Caribbean barrel sponge, Xestospongia muta, is a large and common member of the coral reef communities at depths greater than 10 m, and has been called the “redwood of the deep”, due to its up to 2000 year lifespan as well as its size and color. Despite its prominence, high biomass and importance to habitat complexity and reef health, very little is know about the basic biology of this massive sponge, including rates of mortality and recruitment, reproduction, growth and age. Like reef corals, this sponge is subject to bleaching and subsequent mortality.
With support from NOAA's Aquarius Reef Base at UNCW, NOAA's Coral Reef Conservation Program, and the Florida Keys National Marine Sanctuary, a research group has been monitoring populations of X. muta in the Florida Keys since 1997.© Christoph Gerigk / BiosphotoJPG - RM

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Visualization flow of water in a sponge - Aquarius Reef Base ;

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Visualization flow of water in a sponge - Aquarius Reef Base ; Fluorescein dye is used to visualize how water is absorbed at the outside and then exhausted by a sponge.The Caribbean barrel sponge, Xestospongia muta, is a large and common member of the coral reef communities at depths greater than 10 m, and has been called the “redwood of the deep”, due to its up to 2000 year lifespan as well as its size and color. Despite its prominence, high biomass and importance to habitat complexity and reef health, very little is know about the basic biology of this massive sponge, including rates of mortality and recruitment, reproduction, growth and age. Like reef corals, this sponge is subject to bleaching and subsequent mortality.<br>With support from NOAA's Aquarius Reef Base at UNCW, NOAA's Coral Reef Conservation Program, and the Florida Keys National Marine Sanctuary, a research group has been monitoring populations of X. muta in the Florida Keys since 1997.Visualization flow of water in a sponge - Aquarius Reef BaseVisualization flow of water in a sponge - Aquarius Reef Base ; Fluorescein dye is used to visualize how water is absorbed at the outside and then exhausted by a sponge.The Caribbean barrel sponge, Xestospongia muta, is a large and common member of the coral reef communities at depths greater than 10 m, and has been called the “redwood of the deep”, due to its up to 2000 year lifespan as well as its size and color. Despite its prominence, high biomass and importance to habitat complexity and reef health, very little is know about the basic biology of this massive sponge, including rates of mortality and recruitment, reproduction, growth and age. Like reef corals, this sponge is subject to bleaching and subsequent mortality.
With support from NOAA's Aquarius Reef Base at UNCW, NOAA's Coral Reef Conservation Program, and the Florida Keys National Marine Sanctuary, a research group has been monitoring populations of X. muta in the Florida Keys since 1997.© Christoph Gerigk / BiosphotoJPG - RM

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Visualization flow of water in a sponge - Aquarius Reef Base ;

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Barn Owl perched on a post in a snow storm Winter GBBarn Owl perched on a post in a snow storm Winter GBBarn Owl perched on a post in a snow storm Winter GB© Frédéric Desmette / BiosphotoJPG - RMNon exclusive sale
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1874161

Barn Owl perched on a post in a snow storm Winter GB

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Sandstorm at sunset Sahara Morocco Sandstorm at sunset Sahara Morocco Sandstorm at sunset Sahara Morocco © Laurent Rebelle / BiosphotoJPG - RM

1852519

Sandstorm at sunset Sahara Morocco

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King Penguin (Aptenodytes patagonicus) colony, huddled together during snowstorm, Right Whale Bay, South Georgia, novemberKing Penguin (Aptenodytes patagonicus) colony, huddled together during snowstorm, Right Whale Bay, South Georgia, novemberKing Penguin (Aptenodytes patagonicus) colony, huddled together during snowstorm, Right Whale Bay, South Georgia, november© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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1781060

King Penguin (Aptenodytes patagonicus) colony, huddled together

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Arctic hares on the slopes of Cape Greenland GregArctic hares on the slopes of Cape Greenland GregArctic hares on the slopes of Cape Greenland Greg© Pierre Vernay / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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1776686

Arctic hares on the slopes of Cape Greenland Greg

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Dead Vlei Sossusvlei dead acacia Namib Desert Namibia ; Dead Vlei is an old saltpan named for its eery dead appearance. Water was cut off when the flow of the Tsauchab River changed its course approximately 500 years ago. This now provides visitor with the most spectacular sceneryDead Vlei Sossusvlei dead acacia Namib Desert Namibia Dead Vlei Sossusvlei dead acacia Namib Desert Namibia ; Dead Vlei is an old saltpan named for its eery dead appearance. Water was cut off when the flow of the Tsauchab River changed its course approximately 500 years ago. This now provides visitor with the most spectacular scenery© Martin Harvey / BiosphotoJPG - RMSale prohibited in Germany and UK
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1752023

Dead Vlei Sossusvlei dead acacia Namib Desert Namibia ; Dead

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Dead Acacias Dead Vlei Sossusvlei Namib Desert Namibia  ; Water was cut off when the flow of the Tsauchab River changed its course approximately 500 years ago.Dead Acacias Dead Vlei Sossusvlei Namib Desert Namibia Dead Acacias Dead Vlei Sossusvlei Namib Desert Namibia  ; Water was cut off when the flow of the Tsauchab River changed its course approximately 500 years ago.© Martin Harvey / BiosphotoJPG - RMSale prohibited in Germany and UK
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1258959

Dead Acacias Dead Vlei Sossusvlei Namib Desert Namibia  ; Water

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King Penguins huddled together during storm South GeorgiaKing Penguins huddled together during storm South GeorgiaKing Penguins huddled together during storm South Georgia© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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1250654

King Penguins huddled together during storm South Georgia

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King Penguins huddled together during storm South GeorgiaKing Penguins huddled together during storm South GeorgiaKing Penguins huddled together during storm South Georgia© David Tipling / BiosphotoJPG - RMSale prohibited in UK
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1250653

King Penguins huddled together during storm South Georgia

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Red kite on a tree in snow storm GBRed kite on a tree in snow storm GBRed kite on a tree in snow storm GB© Frédéric Desmette / BiosphotoJPG - RMNon exclusive sale
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960719

Red kite on a tree in snow storm GB

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Polar Bears mother & cub distressed on little ice floe drift ; The little ice floe drifting 12 miles from the coast in the Strait. The cub will probably not make it since iceberg was melting rapidly and cubs are unable to swim that long.Polar Bears mother & cub distressed on little ice floe driftPolar Bears mother & cub distressed on little ice floe drift ; The little ice floe drifting 12 miles from the coast in the Strait. The cub will probably not make it since iceberg was melting rapidly and cubs are unable to swim that long.© Eric Lefranc / BiosphotoJPG - RMSale prohibited in Netherlands and UK
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751889

Polar Bears mother & cub distressed on little ice floe drift ;

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Sea bird landed on a sailboat before the thunderstormSea bird landed on a sailboat before the thunderstormSea bird landed on a sailboat before the thunderstorm© Didier Brandelet / BiosphotoJPG - RM

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Sea bird landed on a sailboat before the thunderstorm

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Collapse of ice-floe on the coast of Cornwallis Island ; @ Cornwallis (Island)<br>Collapse of ice-floe on the coast of Cornwallis IslandCollapse of ice-floe on the coast of Cornwallis Island ; @ Cornwallis (Island)
© Pierre Vernay / Polar Lys / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France
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499204

Collapse of ice-floe on the coast of Cornwallis Island ; @

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Young Locust posed on a dry Pea field Switzerland ; During a dryness in a cultivated Pea field, in edge of the natural reserve.<br>The farmer decided not to mow his production because of the weak one<br>output due to the dryness.<br>The identification of the species is not possible because it's about a youthful individual: the characteristics of the species are not apparent enough.Young Locust posed on a dry Pea field SwitzerlandYoung Locust posed on a dry Pea field Switzerland ; During a dryness in a cultivated Pea field, in edge of the natural reserve.
The farmer decided not to mow his production because of the weak one
output due to the dryness.
The identification of the species is not possible because it's about a youthful individual: the characteristics of the species are not apparent enough.© André Maurer / BiosphotoJPG - RM

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Young Locust posed on a dry Pea field Switzerland ; During a

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White-backed Vulture (Gyps africanus) standing with wings outstretched covered in dustWhite-backed Vulture (Gyps africanus) standing with wings outstretched covered in dustWhite-backed Vulture (Gyps africanus) standing with wings outstretched covered in dust© Peter Delaney / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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2103216

White-backed Vulture (Gyps africanus) standing with wings

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Emperor penguin - Antarctica Southern Ocean ; Emperor penguins in blizzard, Aptenodytes forsteri, Weddell Sea, AntarcticaEmperor penguin - Antarctica Southern OceanEmperor penguin - Antarctica Southern Ocean ; Emperor penguins in blizzard, Aptenodytes forsteri, Weddell Sea, Antarctica© Frans Lanting / Mint Images / BiosphotoJPG - RMNon exclusive sale
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1933459

Emperor penguin - Antarctica Southern Ocean ; Emperor penguins in

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Chinstrap penguin - Antarctica Southern Ocean ; Chinstrap penguins on iceberg, Pygoscelis antarcticus, AntarcticaChinstrap penguin - Antarctica Southern OceanChinstrap penguin - Antarctica Southern Ocean ; Chinstrap penguins on iceberg, Pygoscelis antarcticus, Antarctica© Frans Lanting / Mint Images / BiosphotoJPG - RMNon exclusive sale
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1933366

Chinstrap penguin - Antarctica Southern Ocean ; Chinstrap

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Sunrise on the Atlantic coast of Gran Canaria after the storm, Bufadera de la Garita, Gran Canaria, SpainSunrise on the Atlantic coast of Gran Canaria after the storm, Bufadera de la Garita, Gran Canaria, SpainSunrise on the Atlantic coast of Gran Canaria after the storm, Bufadera de la Garita, Gran Canaria, Spain© David Jerez / BiosphotoJPG - RMNon exclusive sale

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Sunrise on the Atlantic coast of Gran Canaria after the storm,

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Gas embolism following a drought, in a beech tree, Autumn, Moselle, FranceGas embolism following a drought, in a beech tree, Autumn, Moselle, FranceGas embolism following a drought, in a beech tree, Autumn, Moselle, France© Yann Avril / BiosphotoJPG - RM

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Gas embolism following a drought, in a beech tree, Autumn,

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Crown-of-thorns sea star (Acanthaster planci) on Coral, (Acropora sp), Gulf of Tadjoura, DjiboutiCrown-of-thorns sea star (Acanthaster planci) on Coral, (Acropora sp), Gulf of Tadjoura, DjiboutiCrown-of-thorns sea star (Acanthaster planci) on Coral, (Acropora sp), Gulf of Tadjoura, Djibouti© Mathieu Foulquié / BiosphotoJPG - RMSale prohibited by some Agents

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Crown-of-thorns sea star (Acanthaster planci) on Coral, (Acropora

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Crown-of-thorns sea star (Acanthaster planci), Gulf of Tadjoura, DjiboutiCrown-of-thorns sea star (Acanthaster planci), Gulf of Tadjoura, DjiboutiCrown-of-thorns sea star (Acanthaster planci), Gulf of Tadjoura, Djibouti© Mathieu Foulquié / BiosphotoJPG - RMSale prohibited by some Agents

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Crown-of-thorns sea star (Acanthaster planci), Gulf of Tadjoura,

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque Country, Spain. Ichnofossil: Helminthorhaphe and Paleodictyon on the right - Flysch formed at the end of the Mesozoic era, in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, caused by earthquakes, and producing after compaction and crystallization of very regular layers of sandstone and limestone, here corrected by the Pyrenean orogeny and released by erosion.© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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

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Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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

2437372

Ichnofossils on flysch Deba, Geopark of the Basque Coast, Basque

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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

2437366

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

2437360

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

2437355

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

2437354

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

2437353

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

2437352

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

2437351

Remarkable flysch formations of Deba, Basque Coast Geopark,

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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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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

2437188

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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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437006

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437005

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437004

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437003

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Southern Giraffe (Giraffa giraffa). Fighting males in the dry and barren Auob riverbed, raising a lot of dust. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2437002

Southern Giraffe (Giraffa giraffa). Fighting males in the dry and

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Cheetah (Acinonyx jubatus). Female walking in front of her two subadult male cubs in the dry and barren Auob riverbed. Behind them a thunderstorm. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female walking in front of her two subadult male cubs in the dry and barren Auob riverbed. Behind them a thunderstorm. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female walking in front of her two subadult male cubs in the dry and barren Auob riverbed. Behind them a thunderstorm. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436999

Cheetah (Acinonyx jubatus). Female walking in front of her two

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Cheetah (Acinonyx jubatus). Female behind her two subadult male cubs. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female behind her two subadult male cubs. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female behind her two subadult male cubs. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436994

Cheetah (Acinonyx jubatus). Female behind her two subadult male

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Cheetah (Acinonyx jubatus). Female. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Female. Roaming in the dry and barren Auob riverbed during a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436993

Cheetah (Acinonyx jubatus). Female. Roaming in the dry and barren

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436992

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436991

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436990

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436989

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436988

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436987

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.Cheetah (Acinonyx jubatus). Two playful subadult males in the dry and barren Auob riverbed. During a severe drought. Kalahari Desert, Kgalagadi Transfrontier Park, South Africa.© Thomas Dressler / BiosphotoJPG - RMExclusive sale possible

2436986

Cheetah (Acinonyx jubatus). Two playful subadult males in the dry

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Hiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435858

Hiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m),

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Hiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m), Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435857

Hiking to the Ecrins refuge, crevasse du Glacier Blanc (2875m),

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The White Glacier (3023m), hiking to the refuge of the Ecrins, left view on Mount Pelvoux (3932m), right Bar des Ecrins (4101m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes -Alpes, FranceThe White Glacier (3023m), hiking to the refuge of the Ecrins, left view on Mount Pelvoux (3932m), right Bar des Ecrins (4101m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes -Alpes, FranceThe White Glacier (3023m), hiking to the refuge of the Ecrins, left view on Mount Pelvoux (3932m), right Bar des Ecrins (4101m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes -Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435856

The White Glacier (3023m), hiking to the refuge of the Ecrins,

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View of Mount Pelvoux (3932m) and the Pointe de la Grande Sagne (3660m), in the foreground the White Glacier (3023m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceView of Mount Pelvoux (3932m) and the Pointe de la Grande Sagne (3660m), in the foreground the White Glacier (3023m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceView of Mount Pelvoux (3932m) and the Pointe de la Grande Sagne (3660m), in the foreground the White Glacier (3023m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435855

View of Mount Pelvoux (3932m) and the Pointe de la Grande Sagne

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Seracs and crevasses of the Glacier Blanc (2810m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceSeracs and crevasses of the Glacier Blanc (2810m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceSeracs and crevasses of the Glacier Blanc (2810m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435854

Seracs and crevasses of the Glacier Blanc (2810m), Valley of

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Le Glacier Blanc (3023m), view on Mount Pelvoux (3932m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceLe Glacier Blanc (3023m), view on Mount Pelvoux (3932m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceLe Glacier Blanc (3023m), view on Mount Pelvoux (3932m), Valley of Vallouise, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435852

Le Glacier Blanc (3023m), view on Mount Pelvoux (3932m), Valley

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La Barre des Écrins (4101m) and its snow dome, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceLa Barre des Écrins (4101m) and its snow dome, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceLa Barre des Écrins (4101m) and its snow dome, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435851

La Barre des Écrins (4101m) and its snow dome, Vallouise valley,

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La Barre des Écrins (4101m) and its snow dome, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceLa Barre des Écrins (4101m) and its snow dome, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceLa Barre des Écrins (4101m) and its snow dome, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435850

La Barre des Écrins (4101m) and its snow dome, Vallouise valley,

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The White Glacier (3023m) illuminated by a full moon night, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceThe White Glacier (3023m) illuminated by a full moon night, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceThe White Glacier (3023m) illuminated by a full moon night, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435848

The White Glacier (3023m) illuminated by a full moon night,

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Hiking from Madame Carle's Pres near the Glacier Blanc refuge, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking from Madame Carle's Pres near the Glacier Blanc refuge, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, FranceHiking from Madame Carle's Pres near the Glacier Blanc refuge, Vallouise valley, Briançonnais region, Ecrins National Park, Hautes-Alpes, France© Michel Cavalier / BiosphotoJPG - RM

2435846

Hiking from Madame Carle's Pres near the Glacier Blanc refuge,

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Aerial view of an African elephant (Loxodonta africana) walking in the Okavango Delta after a bushfire, Botswana.Aerial view of an African elephant (Loxodonta africana) walking in the Okavango Delta after a bushfire, Botswana.Aerial view of an African elephant (Loxodonta africana) walking in the Okavango Delta after a bushfire, Botswana.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434944

Aerial view of an African elephant (Loxodonta africana) walking

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Aerial view of a bushfire in the Okavango Delta, Botswana.Aerial view of a bushfire in the Okavango Delta, Botswana.Aerial view of a bushfire in the Okavango Delta, Botswana.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434923

Aerial view of a bushfire in the Okavango Delta, Botswana.

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Aerial view of a bushfire in the Okavango Delta, Botswana.Aerial view of a bushfire in the Okavango Delta, Botswana.Aerial view of a bushfire in the Okavango Delta, Botswana.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434922

Aerial view of a bushfire in the Okavango Delta, Botswana.

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Aerial view of a bushfire in the Okavango Delta, Botswana.Aerial view of a bushfire in the Okavango Delta, Botswana.Aerial view of a bushfire in the Okavango Delta, Botswana.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434921

Aerial view of a bushfire in the Okavango Delta, Botswana.

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A snowstorm hits a tourist watching the landscape in Neko Harbour, Antarctica.A snowstorm hits a tourist watching the landscape in Neko Harbour, Antarctica.A snowstorm hits a tourist watching the landscape in Neko Harbour, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434460

A snowstorm hits a tourist watching the landscape in Neko

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A snowstorm hits two tourists watching the landscape in Neko Harbour, Antarctica.A snowstorm hits two tourists watching the landscape in Neko Harbour, Antarctica.A snowstorm hits two tourists watching the landscape in Neko Harbour, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434459

A snowstorm hits two tourists watching the landscape in Neko

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A tourist hiking in Neko Harbour, Antarctica.A tourist hiking in Neko Harbour, Antarctica.A tourist hiking in Neko Harbour, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434458

A tourist hiking in Neko Harbour, Antarctica.

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A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434426

A snowstorm hits tourist in Portal Point, Antarctica.

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A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434425

A snowstorm hits tourist in Portal Point, Antarctica.

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A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.A snowstorm hits tourist in Portal Point, Antarctica.© Sergio Pitamitz / BiosphotoJPG - RMNon exclusive sale

2434424

A snowstorm hits tourist in Portal Point, Antarctica.

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