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Only in springtime, when the hard winter slowly subsides, are the ice-cold waters suitable for divers who can dive around a iceberg that floats in crystal-clear water, Tasiilaq, East GreenlandOnly in springtime, when the hard winter slowly subsides, are the ice-cold waters suitable for divers who can dive around a iceberg that floats in crystal-clear water, Tasiilaq, East GreenlandOnly in springtime, when the hard winter slowly subsides, are the ice-cold waters suitable for divers who can dive around a iceberg that floats in crystal-clear water, Tasiilaq, East Greenland© Franco Banfi / BiosphotoJPG - RMNon exclusive sale, exclusive sale possible in France

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Only in springtime, when the hard winter slowly subsides, are the

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White-spotted pufferfish, Torquigener albomaculosus. Male with characteristic circular nest in the sand on the foreground. Males never reuse a nest. The spectacular nest with 2 meters in diameter is excavated on the sand to attract the females with the impressive design. Amami Oshima Island. Japan Digital composite. Composite imageWhite-spotted pufferfish, Torquigener albomaculosus. Male with characteristic circular nest in the sand on the foreground. Males never reuse a nest. The spectacular nest with 2 meters in diameter is excavated on the sand to attract the females with the impressive design. Amami Oshima Island. Japan Digital composite. Composite imageWhite-spotted pufferfish, Torquigener albomaculosus. Male with characteristic circular nest in the sand on the foreground. Males never reuse a nest. The spectacular nest with 2 meters in diameter is excavated on the sand to attract the females with the impressive design. Amami Oshima Island. Japan Digital composite. Composite image© Paulo de Oliveira / BiosphotoJPG - RMNon exclusive sale
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White-spotted pufferfish, Torquigener albomaculosus. Male with

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Pumpkin sea star (Astrosarkus sp.) attached to rock wall, 90 meters depth, indian Ocean, Mayotte. Possibly new species.Pumpkin sea star (Astrosarkus sp.) attached to rock wall, 90 meters depth, indian Ocean, Mayotte. Possibly new species.Pumpkin sea star (Astrosarkus sp.) attached to rock wall, 90 meters depth, indian Ocean, Mayotte. Possibly new species.© Gabriel Barathieu / BiosphotoJPG - RM

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Pumpkin sea star (Astrosarkus sp.) attached to rock wall, 90

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To try to defend the colony from this incessant predation, the bees fight back by forming a cluster on the flight board. They thus save a few foraging bees returning after gathering nectar and pollen from the flowers. FranceTo try to defend the colony from this incessant predation, the bees fight back by forming a cluster on the flight board. They thus save a few foraging bees returning after gathering nectar and pollen from the flowers. FranceTo try to defend the colony from this incessant predation, the bees fight back by forming a cluster on the flight board. They thus save a few foraging bees returning after gathering nectar and pollen from the flowers. France© Eric Tourneret / BiosphotoJPG - RMNon exclusive sale
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To try to defend the colony from this incessant predation, the

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Face-off between David and Goliath. The bee has no chance of defeating the formidable predator that is the Asian hornet Vespa velutina.Face-off between David and Goliath. The bee has no chance of defeating the formidable predator that is the Asian hornet Vespa velutina.Face-off between David and Goliath. The bee has no chance of defeating the formidable predator that is the Asian hornet Vespa velutina.© Eric Tourneret / BiosphotoJPG - RMNon exclusive sale
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Face-off between David and Goliath. The bee has no chance of

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Apidologie - Bees in a flight tunnel. This procedure was used to show that the evaluation of distance by bees proceeds from their visual system. And through the white and black stripes, its has been shown that it also depends on the landscape's structure. This experiment was carried out by then calculating the length of the bees's dance in relation to the food source of which the distance was identified. /Apidologie - Bees in a flight tunnel. This procedure was used to show that the evaluation of distance by bees proceeds from their visual system. And through the white and black stripes, its has been shown that it also depends on the landscape's structure. This experiment was carried out by then calculating the length of the bees's dance in relation to the food source of which the distance was identified. /Apidologie - Bees in a flight tunnel. This procedure was used to show that the evaluation of distance by bees proceeds from their visual system. And through the white and black stripes, its has been shown that it also depends on the landscape's structure. This experiment was carried out by then calculating the length of the bees's dance in relation to the food source of which the distance was identified. /© Eric Tourneret / BiosphotoJPG - RMNon exclusive sale
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Apidologie - Bees in a flight tunnel. This procedure was used to

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Apidologie - A bee in front of an odor gun. This technique allows for an association between an odor and a sugary reward. A sweet solution is applied to the antennas and the bee stretches out its proboscis, its little trunk. This odor-reflex association has brought to light the bees' capacity to remember odors and the time necessary to acquire olfactory memory. But also more complex learning: for example, an odor A is associated with a sugary solution and an odor B is not. Then, shortly after, it is reversed: the odor A is no longer associated with sugar but the odor B is. Result: the bee is capable of replacing the first signal by the new one. Centre for , FranceResearch, CNRS, Université Paul Sabatier, ToulouseApidologie - A bee in front of an odor gun. This technique allows for an association between an odor and a sugary reward. A sweet solution is applied to the antennas and the bee stretches out its proboscis, its little trunk. This odor-reflex association has brought to light the bees' capacity to remember odors and the time necessary to acquire olfactory memory. But also more complex learning: for example, an odor A is associated with a sugary solution and an odor B is not. Then, shortly after, it is reversed: the odor A is no longer associated with sugar but the odor B is. Result: the bee is capable of replacing the first signal by the new one. Centre for , FranceResearch, CNRS, Université Paul Sabatier, ToulouseApidologie - A bee in front of an odor gun. This technique allows for an association between an odor and a sugary reward. A sweet solution is applied to the antennas and the bee stretches out its proboscis, its little trunk. This odor-reflex association has brought to light the bees' capacity to remember odors and the time necessary to acquire olfactory memory. But also more complex learning: for example, an odor A is associated with a sugary solution and an odor B is not. Then, shortly after, it is reversed: the odor A is no longer associated with sugar but the odor B is. Result: the bee is capable of replacing the first signal by the new one. Centre for , FranceResearch, CNRS, Université Paul Sabatier, Toulouse© Eric Tourneret / BiosphotoJPG - RMNon exclusive sale
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Apidologie - A bee in front of an odor gun. This technique allows

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Honey bee (Apis mellifera) - Microchips are used by researchers to mark the bees and identify them with a scanner at the entrance to the hive or near the nurse bees. In that way, it is possible to monitor the bees' activities on an individual level. The times they go out, etc… Research Center HOBOS, Würzburg, Germany.Honey bee (Apis mellifera) - Microchips are used by researchers to mark the bees and identify them with a scanner at the entrance to the hive or near the nurse bees. In that way, it is possible to monitor the bees' activities on an individual level. The times they go out, etc… Research Center HOBOS, Würzburg, Germany.Honey bee (Apis mellifera) - Microchips are used by researchers to mark the bees and identify them with a scanner at the entrance to the hive or near the nurse bees. In that way, it is possible to monitor the bees' activities on an individual level. The times they go out, etc… Research Center HOBOS, Würzburg, Germany.© Eric Tourneret / BiosphotoJPG - RMNon exclusive sale
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Honey bee (Apis mellifera) - Microchips are used by researchers

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Indonesia, Java Island, East Java province, Kawah Ijen volcano, sulfur flamesIndonesia, Java Island, East Java province, Kawah Ijen volcano, sulfur flamesIndonesia, Java Island, East Java province, Kawah Ijen volcano, sulfur flames© Stéphane Godin / BiosphotoJPG - RM

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Indonesia, Java Island, East Java province, Kawah Ijen volcano,

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Indonesia, Java Island, East Java province, Kawah Ijen volcano, sulfur flamesIndonesia, Java Island, East Java province, Kawah Ijen volcano, sulfur flamesIndonesia, Java Island, East Java province, Kawah Ijen volcano, sulfur flames© Stéphane Godin / BiosphotoJPG - RM

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Indonesia, Java Island, East Java province, Kawah Ijen volcano,

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volcanologist on Piton de la Fournaise in activity, Volcano eruption 16 of september 2016, Reunionvolcanologist on Piton de la Fournaise in activity, Volcano eruption 16 of september 2016, Reunionvolcanologist on Piton de la Fournaise in activity, Volcano eruption 16 of september 2016, Reunion© Gabriel Barathieu / BiosphotoJPG - RM

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volcanologist on Piton de la Fournaise in activity, Volcano

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Marine Iguana feeding at Sea, Amblyrhynchus cristatus, Cabo Douglas, Fernandina Island, Galapagos, EcuadorMarine Iguana feeding at Sea, Amblyrhynchus cristatus, Cabo Douglas, Fernandina Island, Galapagos, EcuadorMarine Iguana feeding at Sea, Amblyrhynchus cristatus, Cabo Douglas, Fernandina Island, Galapagos, Ecuador© Reinhard Dirscherl / BiosphotoJPG - RMNon exclusive sale
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Marine Iguana feeding at Sea, Amblyrhynchus cristatus, Cabo

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Giant Panda (Ailuropoda melanoleuca),captive, Chengdu Panda Base, Sichuan, ChinaGiant Panda (Ailuropoda melanoleuca),captive, Chengdu Panda Base, Sichuan, ChinaGiant Panda (Ailuropoda melanoleuca),captive, Chengdu Panda Base, Sichuan, China© Sylvain Cordier / BiosphotoJPG - RMUse for calendar cover in France prohibited 31-12-2019

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Giant Panda (Ailuropoda melanoleuca),captive, Chengdu Panda Base,

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Egyptian fan-footed gecko (Ptyodactylus hasselquistii) foot detail, EgyptEgyptian fan-footed gecko (Ptyodactylus hasselquistii) foot detail, EgyptEgyptian fan-footed gecko (Ptyodactylus hasselquistii) foot detail, Egypt© Matthijs Kuijpers / BiosphotoJPG - RMNon exclusive sale
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Egyptian fan-footed gecko (Ptyodactylus hasselquistii) foot

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Leaf Katydid from the Santa Lucia cloud forest, Mindo, Pichincha, Ecuador.Leaf Katydid from the Santa Lucia cloud forest, Mindo, Pichincha, Ecuador.Leaf Katydid from the Santa Lucia cloud forest, Mindo, Pichincha, Ecuador.© Javier Aznar Gonzalez de Rueda / BiosphotoJPG - RM

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Leaf Katydid from the Santa Lucia cloud forest, Mindo, Pichincha,

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ISS track, 2016-06-01 05:26, Nyota Observatory, Baringo KenyaISS track, 2016-06-01 05:26, Nyota Observatory, Baringo KenyaISS track, 2016-06-01 05:26, Nyota Observatory, Baringo Kenya© Olivier Sauzereau / BiosphotoJPG - RM

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ISS track, 2016-06-01 05:26, Nyota Observatory, Baringo Kenya

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I want to ride my bicycle - Praying mantis on dry flower seems to ride a bicycleI want to ride my bicycle - Praying mantis on dry flower seems to ride a bicycleI want to ride my bicycle - Praying mantis on dry flower seems to ride a bicycle© Alberto Ghizzi Panizza / BiosphotoJPG - RMNon exclusive sale

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I want to ride my bicycle - Praying mantis on dry flower seems to

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Caribbean flamingo on a nest with chick. Cuba.Caribbean flamingo on a nest with chick. Cuba.Caribbean flamingo on a nest with chick. Cuba.© Andrey Gudkov / BiosphotoJPG - RMNon exclusive sale

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Caribbean flamingo on a nest with chick. Cuba.

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Two Komodo Dragons are fighting each other. Very rare picture.Two Komodo Dragons are fighting each other. Very rare picture.Two Komodo Dragons are fighting each other. Very rare picture.© Andrey Gudkov / BiosphotoJPG - RMNon exclusive sale

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Two Komodo Dragons are fighting each other. Very rare picture.

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Milky Way and bioluminescent plankton - Isle of Hœdic France ; Bioluminescent plankton light up the shore where small waves come to die. In the sky, the Milky Way at the Three Belles Summer.Milky Way and bioluminescent plankton - Isle of Hœdic FranceMilky Way and bioluminescent plankton - Isle of Hœdic France ; Bioluminescent plankton light up the shore where small waves come to die. In the sky, the Milky Way at the Three Belles Summer.© Laurent Laveder / BiosphotoJPG - RMNon exclusive sale

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Milky Way and bioluminescent plankton - Isle of Hœdic France ;

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Bioluminescent plankton - Isle of Hœdic FranceBioluminescent plankton - Isle of Hœdic FranceBioluminescent plankton - Isle of Hœdic France© Laurent Laveder / BiosphotoJPG - RMNon exclusive sale

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Bioluminescent plankton - Isle of Hœdic France

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Milky Way and phosporescent plankton - Ile d'Houat France ; The bioluminescent plankton lights in the roll of a wave that breaks on the sand of a beach on the island of Houat. On the horizon, the Hoëdic Island.Milky Way and phosporescent plankton - Ile d'Houat FranceMilky Way and phosporescent plankton - Ile d'Houat France ; The bioluminescent plankton lights in the roll of a wave that breaks on the sand of a beach on the island of Houat. On the horizon, the Hoëdic Island.© Laurent Laveder / BiosphotoJPG - RMNon exclusive sale

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Milky Way and phosporescent plankton - Ile d'Houat France ; The

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Milky Way and phosphorescent plankton - Hœdic France  ; Phosphorescent plankton light up the shore where small waves come to die. In the sky, the Milky Way Scorpio Swan.Milky Way and phosphorescent plankton - Hœdic France Milky Way and phosphorescent plankton - Hœdic France ; Phosphorescent plankton light up the shore where small waves come to die. In the sky, the Milky Way Scorpio Swan.© Laurent Laveder / BiosphotoJPG - RMNon exclusive sale

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Milky Way and phosphorescent plankton - Hœdic France ;

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Milky Way and bioluminescent plankton - Ile d'Houat France. The rollers breaking on the beach of st Treac'h Goured are illuminated by the presence of phosphorescent plankton. In the sky, the Milky Way between Scorpio and Sagittarius is beautiful.Milky Way and bioluminescent plankton - Ile d'Houat France. The rollers breaking on the beach of st Treac'h Goured are illuminated by the presence of phosphorescent plankton. In the sky, the Milky Way between Scorpio and Sagittarius is beautiful.Milky Way and bioluminescent plankton - Ile d'Houat France. The rollers breaking on the beach of st Treac'h Goured are illuminated by the presence of phosphorescent plankton. In the sky, the Milky Way between Scorpio and Sagittarius is beautiful.© Laurent Laveder / BiosphotoJPG - RMNon exclusive sale

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Milky Way and bioluminescent plankton - Ile d'Houat France. The

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Beams of the house-headlight Miellier - Brittany France ; 360 ° A home-built lighthouse at Pointe du Muller. Its light beams do not turn, but flash. They spread in the atmosphere in large light beams. Beams of the house-headlight Miellier - Brittany FranceBeams of the house-headlight Miellier - Brittany France ; 360 ° A home-built lighthouse at Pointe du Muller. Its light beams do not turn, but flash. They spread in the atmosphere in large light beams. © Laurent Laveder / BiosphotoJPG - RMNon exclusive sale

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Beams of the house-headlight Miellier - Brittany France ; 360 °

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Diver into the light shining down through a cenote openingDiver into the light shining down through a cenote openingDiver into the light shining down through a cenote opening© Brandon Cole / BiosphotoJPG - RMSale prohibited by some Agents
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Diver into the light shining down through a cenote opening

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West African Gabon viper's venom removal in a laboratory. Latoxan LaboratoryWest African Gabon viper's venom removal in a laboratory. Latoxan LaboratoryWest African Gabon viper's venom removal in a laboratory. Latoxan Laboratory© Daniel Heuclin / BiosphotoJPG - RMSale prohibited in Japan
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West African Gabon viper's venom removal in a laboratory. Latoxan

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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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Scientists in laboratory - Aquarius Reef Base Florida ; Dr. Chris Martens (front left), Dr.Niels Lindquist (left), UNC Chapel Hill and other members of the saturation diver team /2011 Ocean Acidification MissionScientists in laboratory - Aquarius Reef Base FloridaScientists in laboratory - Aquarius Reef Base Florida ; Dr. Chris Martens (front left), Dr.Niels Lindquist (left), UNC Chapel Hill and other members of the saturation diver team /2011 Ocean Acidification Mission© Christoph Gerigk / BiosphotoJPG - RM

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Scientists in laboratory - Aquarius Reef Base Florida ; Dr. Chris

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Star trails Dead Vlei Sossusvlei NamibiaStar trails Dead Vlei Sossusvlei NamibiaStar trails Dead Vlei Sossusvlei Namibia© Martin Harvey / BiosphotoJPG - RMSale prohibited in Germany and UK
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1752789

Star trails Dead Vlei Sossusvlei Namibia

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Transversal cut of a spine of sea urchin  ; Lighting in bright background, magnification x 40. Colors by computer processing.Transversal cut of a spine of sea urchin Transversal cut of a spine of sea urchin  ; Lighting in bright background, magnification x 40. Colors by computer processing.© Christian Gautier / BiosphotoJPG - RM

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Transversal cut of a spine of sea urchin  ; Lighting in bright

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Sponge spicules Chondrilla nucula polarized light Sponge spicules Chondrilla nucula polarized light Sponge spicules Chondrilla nucula polarized light © Christian Gautier / BiosphotoJPG - RM

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Sponge spicules Chondrilla nucula polarized light 

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Microscopic view of moss branch Tortula papillosa Microscopic view of moss branch Tortula papillosa Microscopic view of moss branch Tortula papillosa © Christian Gautier / BiosphotoJPG - RM

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Microscopic view of moss branch Tortula papillosa 

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Jaguar yawning Encontros das Aguas Pantanal Brazil Jaguar yawning Encontros das Aguas Pantanal Brazil Jaguar yawning Encontros das Aguas Pantanal Brazil © Bruno Pambour / BiosphotoJPG - RM

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Jaguar yawning Encontros das Aguas Pantanal Brazil 

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Jaguar yawning Encontros das Aguas Pantanal Brazil Jaguar yawning Encontros das Aguas Pantanal Brazil Jaguar yawning Encontros das Aguas Pantanal Brazil © Bruno Pambour / BiosphotoJPG - RM

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Jaguar yawning Encontros das Aguas Pantanal Brazil 

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Jaguar yawning Encontros das Aguas Pantanal Brazil Jaguar yawning Encontros das Aguas Pantanal Brazil Jaguar yawning Encontros das Aguas Pantanal Brazil © Bruno Pambour / BiosphotoJPG - RM

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Jaguar yawning Encontros das Aguas Pantanal Brazil 

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Spicules of sea cuncumber under microscope ; Lighting in polarized light with blade compensatory gypsum, magnified x 100. Spicules of sea cuncumber under microscopeSpicules of sea cuncumber under microscope ; Lighting in polarized light with blade compensatory gypsum, magnified x 100. © Christian Gautier / BiosphotoJPG - RM

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Spicules of sea cuncumber under microscope ; Lighting in

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Grand Duke Desert flight, United Arab EmiratesGrand Duke Desert flight, United Arab EmiratesGrand Duke Desert flight, United Arab Emirates© Xavier Eichaker / BiosphotoJPG - RMSale prohibited in United Arab Emirates
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Grand Duke Desert flight, United Arab Emirates

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Rose Chafer with the wings spread in collectionRose Chafer with the wings spread in collectionRose Chafer with the wings spread in collection© Tristan Da Cunha / BiosphotoJPG - RM

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Rose Chafer with the wings spread in collection

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Mount Bromo volcanic crater at sunrise, Bromo Tengger Semeru National Park, Java, Indonesia, Southeast Asia, AsiaMount Bromo volcanic crater at sunrise, Bromo Tengger Semeru National Park, Java, Indonesia, Southeast Asia, AsiaMount Bromo volcanic crater at sunrise, Bromo Tengger Semeru National Park, Java, Indonesia, Southeast Asia, Asia© Michael Runkel / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Mount Bromo volcanic crater at sunrise, Bromo Tengger Semeru

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Acid Crater Lake, White Island Volcano, an active volcano in the Bay of Plenty, North Island, New Zealand, PacificAcid Crater Lake, White Island Volcano, an active volcano in the Bay of Plenty, North Island, New Zealand, PacificAcid Crater Lake, White Island Volcano, an active volcano in the Bay of Plenty, North Island, New Zealand, Pacific© Matthew Williams-Ellis / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Acid Crater Lake, White Island Volcano, an active volcano in the

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Panoramic view of the Bernina Group with blood moon, Piz Palü, Bellavista, Crast Agüzza, Piz Bernina, Piz Morteratsch, Pers Glacier, Morteratsch Glacier, Diavolezza, Eastern Alps, Engadin, Switzerland, EuropePanoramic view of the Bernina Group with blood moon, Piz Palü, Bellavista, Crast Agüzza, Piz Bernina, Piz Morteratsch, Pers Glacier, Morteratsch Glacier, Diavolezza, Eastern Alps, Engadin, Switzerland, EuropePanoramic view of the Bernina Group with blood moon, Piz Palü, Bellavista, Crast Agüzza, Piz Bernina, Piz Morteratsch, Pers Glacier, Morteratsch Glacier, Diavolezza, Eastern Alps, Engadin, Switzerland, Europe© Bernd Zoller / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Panoramic view of the Bernina Group with blood moon, Piz Palü,

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Landscape shaped by hydro-thermal activity at the Dallol volcano, Danakil-Senke, Hamed Ela, Wollo, Ethiopia, AfricaLandscape shaped by hydro-thermal activity at the Dallol volcano, Danakil-Senke, Hamed Ela, Wollo, Ethiopia, AfricaLandscape shaped by hydro-thermal activity at the Dallol volcano, Danakil-Senke, Hamed Ela, Wollo, Ethiopia, Africa© Heiko Beyer / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Landscape shaped by hydro-thermal activity at the Dallol volcano,

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Redeye goby - Egypt Red Sea ; Pair of Purple Eye Dwarf Gobies, Marsa Alam, Red Sea, EgyptRedeye goby - Egypt Red SeaRedeye goby - Egypt Red Sea ; Pair of Purple Eye Dwarf Gobies, Marsa Alam, Red Sea, Egypt© Tobias Friedrich / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Redeye goby - Egypt Red Sea ; Pair of Purple Eye Dwarf Gobies,

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Humphead wrasse - Egypt Red Sea ; Napoleon Humpback Wrasse, Brother Islands, Red Sea, EgyptHumphead wrasse - Egypt Red SeaHumphead wrasse - Egypt Red Sea ; Napoleon Humpback Wrasse, Brother Islands, Red Sea, Egypt© Tobias Friedrich / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Humphead wrasse - Egypt Red Sea ; Napoleon Humpback Wrasse,

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Cape fur seal Kelp - Atlantic Ocean South Africa ; Brown Fur Seal, False Bay, Atlantic Ocean, South AfricaCape fur seal Kelp - Atlantic Ocean South AfricaCape fur seal Kelp - Atlantic Ocean South Africa ; Brown Fur Seal, False Bay, Atlantic Ocean, South Africa© Tobias Friedrich / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Cape fur seal Kelp - Atlantic Ocean South Africa ; Brown Fur

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Blue shark - Atlantic Ocean South Africa ; Blue Shark, False Bay, Atlantic Ocean, South AfricaBlue shark - Atlantic Ocean South AfricaBlue shark - Atlantic Ocean South Africa ; Blue Shark, False Bay, Atlantic Ocean, South Africa© Tobias Friedrich / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Blue shark - Atlantic Ocean South Africa ; Blue Shark, False Bay,

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Blue shark - Atlantic Ocean South Africa ; Blue Shark, False Bay, Atlantic Ocean, South AfricaBlue shark - Atlantic Ocean South AfricaBlue shark - Atlantic Ocean South Africa ; Blue Shark, False Bay, Atlantic Ocean, South Africa© Tobias Friedrich / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Blue shark - Atlantic Ocean South Africa ; Blue Shark, False Bay,

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Giant manta - Asia Indian Ocean ; Group of Mantas, Baa Atoll, MaldivesGiant manta - Asia Indian OceanGiant manta - Asia Indian Ocean ; Group of Mantas, Baa Atoll, Maldives© Tobias Friedrich / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Giant manta - Asia Indian Ocean ; Group of Mantas, Baa Atoll,

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Great barracuda - Papua New Guinea ; Great Barracuda, Kimbe Bay, New Britain, Papua New GuineaGreat barracuda - Papua New GuineaGreat barracuda - Papua New Guinea ; Great Barracuda, Kimbe Bay, New Britain, Papua New Guinea© Tobias Friedrich / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Great barracuda - Papua New Guinea ; Great Barracuda, Kimbe Bay,

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Sea anemone Spinecheek anemonefish - Papua New Guinea ; Spinecheek Clownfish in white Sea Anemone, Kimbe Bay, New Britain, Papua New GuineaSea anemone Spinecheek anemonefish - Papua New GuineaSea anemone Spinecheek anemonefish - Papua New Guinea ; Spinecheek Clownfish in white Sea Anemone, Kimbe Bay, New Britain, Papua New Guinea© Tobias Friedrich / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Sea anemone Spinecheek anemonefish - Papua New Guinea ;

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Indian Mackerel - Egypt Red Sea ; Feeding Indian Mackerel, Red Sea, EgyptIndian Mackerel - Egypt Red SeaIndian Mackerel - Egypt Red Sea ; Feeding Indian Mackerel, Red Sea, Egypt© Alex Tattersall / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Indian Mackerel - Egypt Red Sea ; Feeding Indian Mackerel, Red

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Devil firefish - Egypt Red Sea ; Lionfish in Cave, Sharm el Sheikh, Red Sea, EgyptDevil firefish - Egypt Red SeaDevil firefish - Egypt Red Sea ; Lionfish in Cave, Sharm el Sheikh, Red Sea, Egypt© Alex Tattersall / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Devil firefish - Egypt Red Sea ; Lionfish in Cave, Sharm el

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Scalloped hammerhead - Cocos Island National Park Pacific Ocean ; Silhouette of Scalloped Hammerhead Shark School, Cocos Island, Pacific Ocean, Costa RicaScalloped hammerhead - Cocos Island National Park Pacific OceanScalloped hammerhead - Cocos Island National Park Pacific Ocean ; Silhouette of Scalloped Hammerhead Shark School, Cocos Island, Pacific Ocean, Costa Rica© Ethan Daniels / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Scalloped hammerhead - Cocos Island National Park Pacific Ocean ;

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Ghost Goby on Seafan, Komodo, IndonesiaGhost Goby on Seafan, Komodo, IndonesiaGhost Goby on Seafan, Komodo, Indonesia© Mirko Zanni / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Ghost Goby on Seafan, Komodo, Indonesia

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Silhouette of Spinner Dolphin, Big Island, Hawaii, USASilhouette of Spinner Dolphin, Big Island, Hawaii, USASilhouette of Spinner Dolphin, Big Island, Hawaii, USA© Masa Ushioda / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Silhouette of Spinner Dolphin, Big Island, Hawaii, USA

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Male Mahi-Mahi Dorado, Kona Coast, Big Island, Hawaii, USAMale Mahi-Mahi Dorado, Kona Coast, Big Island, Hawaii, USAMale Mahi-Mahi Dorado, Kona Coast, Big Island, Hawaii, USA© Masa Ushioda / WaterFrame - Agence / BiosphotoJPG - RMNon exclusive sale
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Male Mahi-Mahi Dorado, Kona Coast, Big Island, Hawaii, USA

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European Roe Deer (Capreolus capreolus) fawn in wild garlicEuropean Roe Deer (Capreolus capreolus) fawn in wild garlicEuropean Roe Deer (Capreolus capreolus) fawn in wild garlic© Alfons Hauke / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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European Roe Deer (Capreolus capreolus) fawn in wild garlic

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Orange Ladybird or Orange Ladybug (Halyzia sedecimguttata), in flightOrange Ladybird or Orange Ladybug (Halyzia sedecimguttata), in flightOrange Ladybird or Orange Ladybug (Halyzia sedecimguttata), in flight© André Skonieczny / imageBROKER / BiosphotoJPG - RMNon exclusive sale
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Orange Ladybird or Orange Ladybug (Halyzia sedecimguttata), in

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Mont Ventoux under the snow in winter, Vaucluse, Provence, FranceMont Ventoux under the snow in winter, Vaucluse, Provence, FranceMont Ventoux under the snow in winter, Vaucluse, Provence, France© David Tatin / BiosphotoJPG - RM

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Mont Ventoux under the snow in winter, Vaucluse, Provence, France

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

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Exceptional granite of Hercynian age, rich in enormous nodules of

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Erosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, PortugalErosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, PortugalErosion in crust of bread on granite, one of the symbols of the Geopark of Arouca, Portugal© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Erosion in crust of bread on granite, one of the symbols of the

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

2437625

Observation system of the nodular granite of Castanheira, Geopark

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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

2437622

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

2437621

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

2437620

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

2437619

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

2437618

Spectacular flysch formations in southern Portugal, The flysch

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The Stralsund Museum has various collections such as the natural history one, open in 1858 in the St Catherine's monastery, Stralsund, Mecklenburg-Vorpommern, GermanyThe Stralsund Museum has various collections such as the natural history one, open in 1858 in the St Catherine's monastery, Stralsund, Mecklenburg-Vorpommern, GermanyThe Stralsund Museum has various collections such as the natural history one, open in 1858 in the St Catherine's monastery, Stralsund, Mecklenburg-Vorpommern, Germany© Antoine Lorgnier / BiosphotoJPG - RM

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The Stralsund Museum has various collections such as the natural

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The Stralsund Museum has various collections such as the natural history one, open in 1858 in the St Catherine's monastery, Stralsund, Mecklenburg-Vorpommern, GermanyThe Stralsund Museum has various collections such as the natural history one, open in 1858 in the St Catherine's monastery, Stralsund, Mecklenburg-Vorpommern, GermanyThe Stralsund Museum has various collections such as the natural history one, open in 1858 in the St Catherine's monastery, Stralsund, Mecklenburg-Vorpommern, Germany© Antoine Lorgnier / BiosphotoJPG - RM

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The Stralsund Museum has various collections such as the natural

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437390

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437389

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437388

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrowsNatural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remains of paramoudra, concretions around worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437387

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437386

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437385

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437384

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437383

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437382

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437381

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437380

Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrowsGeoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated by erosion - the yellow discs are undoubtedly remains of paramoudra, concretions around the worm burrows© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Geoforms in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque

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Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remnants of paramoudra, concretions around worm burrows.Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remnants of paramoudra, concretions around worm burrows.Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel Coastal Massif, Basque Country, Spain. Remarkable sculptures of Eocene sandstone (geoforms) of origin in part biological (fossil biological activities) and updated then sculpted by erosion - the hollow spheres are probably remnants of paramoudra, concretions around worm burrows.© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437378

Natural Sculptures (Geoforms) in Jaizkibel Sandstone, Jaizkibel

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originally© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437377

Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originally© Jean-Philippe Delobelle / BiosphotoJPG - RM

2437376

Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originallyParamoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque Country, Spain. Spectacular fossil sandstone concretions formed around the worm burrows living several hundred meters deep, 45 million years ago (Eocene) - These spheres or tubes have a diameter of 20 to 40 cm in diameter and were flexible originally© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Paramoudras of Jaizkibel, Coastal Massif of Jaizkibel, Basque

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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

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

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Daedalus desglandi trace fossil in a quarzite of the Ordovician, enigmatic fossil of a few centimeters, present in the quarzites of the Lower Paleozoic, Geopark of Villuercas, Extremadura, SpainDaedalus desglandi trace fossil in a quarzite of the Ordovician, enigmatic fossil of a few centimeters, present in the quarzites of the Lower Paleozoic, Geopark of Villuercas, Extremadura, SpainDaedalus desglandi trace fossil in a quarzite of the Ordovician, enigmatic fossil of a few centimeters, present in the quarzites of the Lower Paleozoic, Geopark of Villuercas, Extremadura, Spain© Jean-Philippe Delobelle / BiosphotoJPG - RM

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Daedalus desglandi trace fossil in a quarzite of the Ordovician,

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

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Polychrome strata of Playa del Silencio, Asturias, Spain.

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

2437330

Polychrome strata of Playa del Silencio, Asturias, Spain.

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

2437329

Polychrome strata of Playa del Silencio, Asturias, Spain.

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

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Polychrome strata of Playa del Silencio, Asturias, Spain.

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