fossile

Nature du spécimen

371 image(s) · 183 Actualités

Galerie d'images

Permineralized Jurassic fern rhizome from Korsaröd (Sweden) of Osmundastrum pulchellum. It has preserved Nuclei and Chromosomes, a fine subcellular detail has rarely been documented in fossils. It´s Rooted in DNA content was used to extrapolate relative genome, finding relationships with extant Osmundastrum cinnamomeum, and confirmed a monophyletic Osmunda. Osmundastrum pulchellum is one of the earliest fossil Osmundastrum rhizomes known so far, and the first of its kind from the Mesozoic of Europe. Its impressive preservation has lead to know even the biotic interactions with the Plant. It also has recovered the only know case know to preserve the ongoing mitosis processes in plant cells via calcification from volcanic hydrothermal brine.

Permineralized Jurassic fern rhizome from Korsaröd (Sweden) of Osmundastrum pulchellum. It has preserved Nuclei and Chromosomes, a fine subcellular detail has rarely been documented in fossils. It´s Rooted in DNA content was used to extrapolate relative genome, finding relationships with extant Osmundastrum cinnamomeum, and confirmed a monophyletic Osmunda. Osmundastrum pulchellum is one of the earliest fossil Osmundastrum rhizomes known so far, and the first of its kind from the Mesozoic of Europe. Its impressive preservation has lead to know even the biotic interactions with the Plant. It also has recovered the only know case know to preserve the ongoing mitosis processes in plant cells via calcification from volcanic hydrothermal brine.

ADN Suède Jurassique Mésozoïque +1
Reprodução a partir da gravura original do Holótipo, Hybodus acutus Agassiz, 1837, na publicação e prancha: L. Agassiz. 1837. Recherches sur les poissons fossiles Vol.3 (Atlas); Tab 10

Reprodução a partir da gravura original do Holótipo, Hybodus acutus Agassiz, 1837, na publicação e prancha: L. Agassiz. 1837. Recherches sur les poissons fossiles Vol.3 (Atlas); Tab 10

fossile poisson
Graph of relative Dinosaur fossil populations from each period of geologic time in the Mesozoic, ordered by major clade

Graph of relative Dinosaur fossil populations from each period of geologic time in the Mesozoic, ordered by major clade

Mésozoïque fossile Dinosauria
Fossil of the Decapod Cycleryon

Fossil of the Decapod Cycleryon

fossile
Fig 2. Geological section of the “Mittlerer Kimmeridge”.
This figure is based on Fischer and modified from Lallensack et al. Beds yielding terrestrial fossils are listed.

Fig 2. Geological section of the “Mittlerer Kimmeridge”. This figure is based on Fischer and modified from Lallensack et al. Beds yielding terrestrial fossils are listed.

fossile
Fossil shell of Aulacostephanus yo from France, on display at Gallery of Paleontology and Comparative Anatomy, Paris.
Intervalles Kimmeridgian

Fossil shell of Aulacostephanus yo from France, on display at Gallery of Paleontology and Comparative Anatomy, Paris.

France fossile anatomie
The GSSP for the Hirnantian stage in the ICS geological timescale (uppermost Ordovician stage), located in the Wangjiawan profile (an outcrop of black shale, brownishly weathered siliceous shale and chert layers of the Wufeng Formation) along the G241 road, about 40 km north of Yichang, Hubei, China. An exact golden spike is missing in the profile (2025) but a memorial plague marks the place. The GSSP occurs at the first appearance of fossils of the graptolite species Normalograptus extraordinarius. It was ratified in 2006.

The GSSP for the Hirnantian stage in the ICS geological timescale (uppermost Ordovician stage), located in the Wangjiawan profile (an outcrop of black shale, brownishly weathered siliceous shale and chert layers of the Wufeng Formation) along the G241 road, about 40 km north of Yichang, Hubei, China. An exact golden spike is missing in the profile (2025) but a memorial plague marks the place. The GSSP occurs at the first appearance of fossils of the graptolite species Normalograptus extraordinarius. It was ratified in 2006.

Chine Hirnantien Ordovicien fossile +1
Crioceratites fabreae fossils on display at the French National Museum of Natural History in Paris, France.

Crioceratites fabreae fossils on display at the French National Museum of Natural History in Paris, France.

musée France fossile
Crioceratites duvali fossil on display at the French National Museum of Natural History in Paris, France.

Crioceratites duvali fossil on display at the French National Museum of Natural History in Paris, France.

musée France fossile
“Sternberger Kuchen” (“Sternberg cake”), a large late Pleistocene glaciofluvial pebble of a highly fossiliferous, shallow marine sandstone of the North German Paleogene (Sülstorf beds, formerly known as “Sternberg rock”, Chattian, Oligocene, about 25 million years old). The fossil content is mainly made up of mollusks (pelecypods, gastropods, scaphopods). Provenance: Sternberg, Mecklenburg-Vorpommern, Northeast Germany.

“Sternberger Kuchen” (“Sternberg cake”), a large late Pleistocene glaciofluvial pebble of a highly fossiliferous, shallow marine sandstone of the North German Paleogene (Sülstorf beds, formerly known as “Sternberg rock”, Chattian, Oligocene, about 25 million years old). The fossil content is mainly made up of mollusks (pelecypods, gastropods, scaphopods). Provenance: Sternberg, Mecklenburg-Vorpommern, Northeast Germany.

Allemagne Chattien Pléistocène supérieur Oligocène +3
Fossil of Cainotherium, an extinct mammal https://hdl.handle.net/21.12123/66925 in ferruginous rock of Oligocene (Chattian) age from Ingolstadt in Bavaria, Germany - Took the photo at Museon museum, Den Haag
Intervalles Chattian

Fossil of Cainotherium, an extinct mammal https://hdl.handle.net/21.12123/66925 in ferruginous rock of Oligocene (Chattian) age from Ingolstadt in Bavaria, Germany - Took the photo at Museon museum, Den Haag

musée Allemagne Chattien Oligocène +1
A fossil tree from the Coal Creek region, Fruitland Formation, latest Cretaceous (Late Campanian), San Juan Basin, New Mexico

A fossil tree from the Coal Creek region, Fruitland Formation, latest Cretaceous (Late Campanian), San Juan Basin, New Mexico

Mexique Fruitland Campanien Crétacé +2
Glyptostrobus europaeus fossil leaves of Burdigalian stage in the early Miocene epoch, from a brown coal mine in Bilina, Czech Republic.

Glyptostrobus europaeus fossil leaves of Burdigalian stage in the early Miocene epoch, from a brown coal mine in Bilina, Czech Republic.

Tchéquie Burdigalien Miocène fossile
Brachipotherium aurelianense, from Rubí. Fossils. Collection of paleontology of the Geological Museum of the Barcelona Seminari (Museu Geològic del Seminari de Barcelona).

Brachipotherium aurelianense, from Rubí. Fossils. Collection of paleontology of the Geological Museum of the Barcelona Seminari (Museu Geològic del Seminari de Barcelona).

musée fossile
Ficus truncata fossil leaf from the early Miocene epoch 20 Ma, of the Třetihorní flóra from Bílina, Czech Republic.

Ficus truncata fossil leaf from the early Miocene epoch 20 Ma, of the Třetihorní flóra from Bílina, Czech Republic.

Tchéquie Miocène fossile
Comptonia acutiloba fossil leaves from the early Miocene epoch 20 Ma, of the Třetihorní flóra from Bílina, Czech Republic.

Comptonia acutiloba fossil leaves from the early Miocene epoch 20 Ma, of the Třetihorní flóra from Bílina, Czech Republic.

Tchéquie Miocène fossile
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Actualités

Une créature vieille de 518 millions d'années révèle les origines des crocs d'araignée
membre tissus fossile
Une minuscule créature marine vieille de 518 millions d’années a révélé les premières preuves connues des structures qui sont finalement devenues des crocs d’araignées. Cachés à l’intérieur du fossile se trouvaient des membres en forme de pinces et des tissus mous préservés qui aident à expliquer comment les ancêtres des araignées et des scorpions sont devenus de redoutables chasseurs.
04/08/2026 sciencedaily-paleo ⚙ Traduction automatique
Les fossiles remarquables d'Eoceras shaanxiense réécrivent l'évolution des céphalopodes
Chine Cambrien Étage 3 du Cambrien fossile évolution formation
Les chercheurs ont identifié de minuscules fossiles de la formation Shuijingtuo (stade cambrien 3) du sud de la Chine qui pourraient transformer notre compréhension de l'évolution des céphalopodes. L'espèce nouvellement décrite, Eoceras shaanxiense, fournit la plus ancienne preuve connue d'un siphoncle primordial, une caractéristique anatomique cruciale qui a permis aux céphalopodes de réguler la flottabilité et de devenir finalement certains des océans.
03/08/2026 everythingdinosaur ⚙ Traduction automatique
Célébration de Peter Trusler Palaeoart – Redonner vie aux océans anciens
os fossile Ichthyosauria découverte
L’un des points forts du reportage sur les nouvelles découvertes scientifiques est de voir les œuvres d’art remarquables qui accompagnent de nombreux articles de recherche. Bien que les fossiles en fournissent la preuve, il faut souvent l'habileté d'un paléoartiste talentueux pour transformer les os et les impressions en scènes vivantes des temps profonds. Par exemple, nous avons récemment parlé d’un remarquable fossile d’ichtyosaure.
02/08/2026 everythingdinosaur ⚙ Traduction automatique
520-Million-Year-Old Fossil from China Fills Gap in Evolutionary History of Cephalopods
Un fossile chinois vieux de 520 millions d’années comble une lacune dans l’histoire évolutive des céphalopodes
Chine Cambrien fossile évolution
Les paléontologues ont identifié le plus ancien céphalopode connu équipé d'un siphoncle - une extension tubulaire du manteau trouvée chez les céphalopodes à coquille - remontant les archives fossiles de cette caractéristique clé de l'évolution au Cambrien inférieur, il y a environ 520 millions d'années. L'article Un fossile chinois vieux de 520 millions d'années comble une lacune dans l'histoire évolutive des céphalopodes est apparu en premier sur Sci.News : Breaking Science News.
30/07/2026 sci-news ⚙ Traduction automatique
Un fossile oublié vient de révéler un nouveau prédateur du Trias datant d'il y a 210 millions d'années
mâchoire prédateur proie Mexique Trias fossile crâne
Un fossile négligé depuis près de 80 ans a révélé un parent de crocodile jusqu'alors inconnu qui vivait il y a 210 millions d'années dans ce qui est aujourd'hui le Nouveau-Mexique. Nommé Eosphorosuchus lacrimosa, ce prédateur de la taille d'un chacal avait un crâne renforcé, des muscles de mâchoire puissants et un museau court conçu pour s'attaquer à des proies plus grosses.
30/07/2026 sciencedaily ⚙ Traduction automatique
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