formation

Thématique

189 image(s) · 11 Actualités

Galerie d'images

Locality map: Grand Staircase-Escalante National Monument, southern Utah.
Map showing locality (indicated by star) of Nasutoceratops titusi holotype UMNH VP 16800, recovered from the Kaiparowits Formation of Grand Staircase-Escalante National Monument (GSENM). GSENM is bounded by the red rectangle and silhouetted in dark gray on the inset of Utah and surrounding states (modified from [1]).

The original map has been modified to show Nasutoceratops instead of Machairoceratops as in the original source. New location based on map in Ceratopsid Dinosaurs from the Grand Staircase of Southern Utah, page 489.

Locality map: Grand Staircase-Escalante National Monument, southern Utah. Map showing locality (indicated by star) of Nasutoceratops titusi holotype UMNH VP 16800, recovered from the Kaiparowits Formation of Grand Staircase-Escalante National Monument (GSENM). GSENM is bounded by the red rectangle and silhouetted in dark gray on the inset of Utah and surrounding states (modified from [1]). The original map has been modified to show Nasutoceratops instead of Machairoceratops as in the original source. New location based on map in Ceratopsid Dinosaurs from the Grand Staircase of Southern Utah, page 489.

Kaiparowits holotype Ceratopsidae Dinosauria +3
Locality map: Grand Staircase-Escalante National Monument, southern Utah.
Map showing locality (indicated by star) of Kosmoceratops richardsoni holotype UMNH VP 17000 and assigned subadult UMNH VP 16878, recovered from the Kaiparowits Formation of Grand Staircase-Escalante National Monument (GSENM). GSENM is bounded by the red rectangle and silhouetted in dark gray on the inset of Utah and surrounding states (modified from [1]).

The original map has been modified to show Kosmoceratops instead of Machairoceratops as in the original source. New location based on map in Ceratopsid Dinosaurs from the Grand Staircase of Southern Utah, page 489.

Locality map: Grand Staircase-Escalante National Monument, southern Utah. Map showing locality (indicated by star) of Kosmoceratops richardsoni holotype UMNH VP 17000 and assigned subadult UMNH VP 16878, recovered from the Kaiparowits Formation of Grand Staircase-Escalante National Monument (GSENM). GSENM is bounded by the red rectangle and silhouetted in dark gray on the inset of Utah and surrounding states (modified from [1]). The original map has been modified to show Kosmoceratops instead of Machairoceratops as in the original source. New location based on map in Ceratopsid Dinosaurs from the Grand Staircase of Southern Utah, page 489.

Kaiparowits holotype Ceratopsidae Dinosauria +3
Kaiparowits Formation (Campanian; Upper Cretaceous) at The Blues, near Powell Point (peak to the left) composed of the Claron Formation.

Kaiparowits Formation (Campanian; Upper Cretaceous) at The Blues, near Powell Point (peak to the left) composed of the Claron Formation.

Kaiparowits Campanien Crétacé formation
Natural-colour satellite image of part of the Kaiparowits Basin (a central portion of Grand Staircase-Escalante). The branch-like shapes are networks of canyons carved by rivers that dried up millions of years ago. The ridge running roughly north-south through the scene is the Cockscomb, which is surrounded by distinct rock formations deposited at different times in the geologic past. West of the Cockscomb is the Navajo Sandstone, dating from the Triassic. East of the Cockscomb are two formations from the Cretaceous: the light-toned Wahweap and darker Kaiparowits.

Natural-colour satellite image of part of the Kaiparowits Basin (a central portion of Grand Staircase-Escalante). The branch-like shapes are networks of canyons carved by rivers that dried up millions of years ago. The ridge running roughly north-south through the scene is the Cockscomb, which is surrounded by distinct rock formations deposited at different times in the geologic past. West of the Cockscomb is the Navajo Sandstone, dating from the Triassic. East of the Cockscomb are two formations from the Cretaceous: the light-toned Wahweap and darker Kaiparowits.

Allen Kaiparowits Navajo Sandstone Crétacé +3
Map of Grand Staircase-Escalante National Monument (GSENM), southern Utah (A), and generalized stratigraphic section of the upper Campanian Kaiprowits Formation (B). The approximate stratigraphic position of Akainacephalus johnsoni is located near the base of the middle unit within the Kaiparowits Formation. The map highlights the GSENM boundary (dashed line), showing the geological distribution and outcrops of the Cretaceous Kaiparowits, Wahweap, and Straight Cliffs formations. The red star indicates the Horse Mountain area, from which Akainacephalus johnsoni was recorded. Map and stratigraphic column modified from Roberts (2005). Radioisotopic dates used from Roberts, Deino & Chan (2005) and Roberts et al. (2013), respectively.
Formations Kaiparowits

Map of Grand Staircase-Escalante National Monument (GSENM), southern Utah (A), and generalized stratigraphic section of the upper Campanian Kaiprowits Formation (B). The approximate stratigraphic position of Akainacephalus johnsoni is located near the base of the middle unit within the Kaiparowits Formation. The map highlights the GSENM boundary (dashed line), showing the geological distribution and outcrops of the Cretaceous Kaiparowits, Wahweap, and Straight Cliffs formations. The red star indicates the Horse Mountain area, from which Akainacephalus johnsoni was recorded. Map and stratigraphic column modified from Roberts (2005). Radioisotopic dates used from Roberts, Deino & Chan (2005) and Roberts et al. (2013), respectively.

Kaiparowits Campanien Crétacé Akainacephalus +1
Psittacosaurus skeletal mount (Early Cretaceous, Jiufotang Formation) and unidentified Late Cretaceous dinosaur egg from Xixia, Hennan, on display in the Li Siguang Memorial Museum in Huangzhou.
Formations Jiufotang

Psittacosaurus skeletal mount (Early Cretaceous, Jiufotang Formation) and unidentified Late Cretaceous dinosaur egg from Xixia, Hennan, on display in the Li Siguang Memorial Museum in Huangzhou.

musée Jiufotang Crétacé Crétacé inférieur +4
Shestakovsky Yar (paleontological site Shestakovo-1, Ilek Formation).

Shestakovsky Yar (paleontological site Shestakovo-1, Ilek Formation).

Ilek formation
Paleontological locality Shestakovo 3 (Ilek Formation, Lower Cretaceous), July 2022.
Formations Ilek

Paleontological locality Shestakovo 3 (Ilek Formation, Lower Cretaceous), July 2022.

Ilek Crétacé formation
(A) Present day map of Australia with the town of Lightning Ridge indicated by the star. (B) Regional map of the Lightning Ridge region showing localities (where known) for specimens described in this text. Sealed (solid black lines) and unsealed roads (dashed lines) are indicated. The ephemeral Coocoran Lake is marked with a dotted blue line. (C) Correlative stratigraphy of the major Cretaceous depositional basins and geological units discussed in this study. The ornithopod icon and arrow indicate the approximate level of the Griman Creek Formation from which the current material pertains. Informal units are in quotation marks. Maps in (A) and (B) redrawn and modified from Bell et al. (2016) and Opal Fields—Lightning Ridge Region map produced by the NSW Department of Mineral Resources, respectively. Stratigraphy based on Toslini, McLoughlin & Drinnan (1999) and Cook, Bryan & Draper (2013). Ornithopod silhouette created by Caleb M. Brown and used under the Creative Commons Attribution-ShareAlike 3.0 Unported license.

(A) Present day map of Australia with the town of Lightning Ridge indicated by the star. (B) Regional map of the Lightning Ridge region showing localities (where known) for specimens described in this text. Sealed (solid black lines) and unsealed roads (dashed lines) are indicated. The ephemeral Coocoran Lake is marked with a dotted blue line. (C) Correlative stratigraphy of the major Cretaceous depositional basins and geological units discussed in this study. The ornithopod icon and arrow indicate the approximate level of the Griman Creek Formation from which the current material pertains. Informal units are in quotation marks. Maps in (A) and (B) redrawn and modified from Bell et al. (2016) and Opal Fields—Lightning Ridge Region map produced by the NSW Department of Mineral Resources, respectively. Stratigraphy based on Toslini, McLoughlin & Drinnan (1999) and Cook, Bryan & Draper (2013). Ornithopod silhouette created by Caleb M. Brown and used under the Creative Commons Attribution-ShareAlike 3.0 Unported license.

Australie Griman Creek Crétacé spécimen +3
View north across Frenchman River of Upper Cretaceous and Paleocene age strata of the Bearpaw, Whitemud, Battle, Frenchman, and Ravenscrag Formations in the Cypress Hills of southern Saskatchewan. Foreground strata on other side of (tree lined) creek represent a slumped section. Note the bright white zone is the Whitemud Formation. View includes type area of Frenchman and Ravenscrag Formations.

View north across Frenchman River of Upper Cretaceous and Paleocene age strata of the Bearpaw, Whitemud, Battle, Frenchman, and Ravenscrag Formations in the Cypress Hills of southern Saskatchewan. Foreground strata on other side of (tree lined) creek represent a slumped section. Note the bright white zone is the Whitemud Formation. View includes type area of Frenchman and Ravenscrag Formations.

Frenchman Crétacé Paléocène formation
View northeast across Frenchman River of Upper Cretaceous and Paleocene age strata of the Bearpaw, Whitemud, Battle, Frenchman, and Ravenscrag Formations in the Cypress Hills of southern Saskatchewan. Foreground strata on other side of (tree lined) creek represent a slumped section. Note the bright white zone is the Whitemud Formation. View includes type area of Frenchman and Ravenscrag Formations.

View northeast across Frenchman River of Upper Cretaceous and Paleocene age strata of the Bearpaw, Whitemud, Battle, Frenchman, and Ravenscrag Formations in the Cypress Hills of southern Saskatchewan. Foreground strata on other side of (tree lined) creek represent a slumped section. Note the bright white zone is the Whitemud Formation. View includes type area of Frenchman and Ravenscrag Formations.

Frenchman Crétacé Paléocène formation
Dryolestidan mammal Crusafontia amoae sp. nov., MPZ CC2−1 M4 or M5, holotype, from the site of Cuesta Corrales 2, Colladico Blanco level, El Castellar Formation, Galve, Teruel, Spain in, occlusal (A), mesial (B), labial (C), distal (D), and lingual (E) views. The schematic drawing of C. amoae, in the box in the lower left−hand corner shows the main anatomical elements of the occlusal surface of a dryolestidan.
Formations El Castellar

Dryolestidan mammal Crusafontia amoae sp. nov., MPZ CC2−1 M4 or M5, holotype, from the site of Cuesta Corrales 2, Colladico Blanco level, El Castellar Formation, Galve, Teruel, Spain in, occlusal (A), mesial (B), labial (C), distal (D), and lingual (E) views. The schematic drawing of C. amoae, in the box in the lower left−hand corner shows the main anatomical elements of the occlusal surface of a dryolestidan.

dessin Espagne El Castellar holotype +1
The type specimen of the ichnogenus Cheliceratichnus, from the Early Jurassic East Berlin Formation of Holyoke, Massachusetts.

The type specimen of the ichnogenus Cheliceratichnus, from the Early Jurassic East Berlin Formation of Holyoke, Massachusetts.

East Berlin Jurassique inférieur Jurassique spécimen +1
Bifurculapes laqueatus trackway (positive hyporelief, i.e. casts on the bottom surface of the bed) from the Early Jurassic East Berlin Formation (Hartford Basin) of Holyoke, Massachusetts (not the same specimen as this one). See coin (1 U.S. cent, 19.05 mm in diameter) for scale.

Bifurculapes laqueatus trackway (positive hyporelief, i.e. casts on the bottom surface of the bed) from the Early Jurassic East Berlin Formation (Hartford Basin) of Holyoke, Massachusetts (not the same specimen as this one). See coin (1 U.S. cent, 19.05 mm in diameter) for scale.

écaille East Berlin Jurassique inférieur Jurassique +3
Bifurculapes laqueatus trackway (positive hyporelief, i.e. casts on the bottom surface of the bed) from the Early Jurassic East Berlin Formation (Hartford Basin) of Holyoke, Massachusetts (not the same specimen as this one). See coin (1 U.S. cent, 19.05 mm in diameter) for scale.

Bifurculapes laqueatus trackway (positive hyporelief, i.e. casts on the bottom surface of the bed) from the Early Jurassic East Berlin Formation (Hartford Basin) of Holyoke, Massachusetts (not the same specimen as this one). See coin (1 U.S. cent, 19.05 mm in diameter) for scale.

écaille East Berlin Jurassique inférieur Jurassique +3
A trackway of the trace fossil Bifurculapes laqueatus (positive hyporelief, i.e. casts on the bottom surface of the bed) from the Early Jurassic East Berlin Formation (Hartford Basin) of Holyoke, Massachusetts (not the same specimen as this one). Scale is in cm.
Formations East Berlin

A trackway of the trace fossil Bifurculapes laqueatus (positive hyporelief, i.e. casts on the bottom surface of the bed) from the Early Jurassic East Berlin Formation (Hartford Basin) of Holyoke, Massachusetts (not the same specimen as this one). Scale is in cm.

écaille East Berlin Jurassique inférieur Jurassique +4
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Actualités

Des scientifiques viennent de découvrir que l’Afrique est plus proche de l’éclatement que nous le pensions
fossile formation
Sous le rift Turkana, en Afrique de l’Est, les scientifiques ont découvert que la croûte s’amincit jusqu’à atteindre un point critique, ce qui suggère que le continent se désagrège progressivement. Ce processus de « rétrécissement » marque un stade avancé de rifting qui pourrait éventuellement conduire à la formation d’un nouvel océan dans des millions d’années. Étonnamment, les mêmes forces géologiques qui divisent la terre peuvent également expliquer pourquoi la région détient un registre fossile si riche. Au lieu d'être le berceau de l'humanité, Turkana pourrait bien être simplement le lieu où
25/04/2026 sciencedaily-paleo ⚙ Traduction automatique
D’étranges roches en « peau d’éléphant » révèlent une vie ancienne dans l’océan sombre
Maroc fossile découverte formation
Une étrange formation rocheuse ridée au Maroc a amené les scientifiques à repenser l'endroit où pourraient vivre d'anciens microbes. Au lieu d’eaux peu profondes et ensoleillées, ces microbes pourraient avoir prospéré dans les profondeurs de l’océan, alimentés par les produits chimiques libérés par les glissements de terrain sous-marins. La découverte suggère que les environnements sombres et riches en nutriments ont abrité des écosystèmes prospères beaucoup plus tôt que prévu. Cela soulève également la possibilité que de nombreux fossiles similaires aient été négligés ou mal interprétés.
03/04/2026 sciencedaily-paleo ⚙ Traduction automatique
Épisode 173 : Forêt pétrifiée
États-Unis Chinle Trias supérieur Trias formation
Le parc national de la Forêt Pétrifiée, dans le nord-est de l'Arizona, aux États-Unis, est une plaque tournante de la paléontologie du Trias et présente des affleurements représentant 20 millions d'années de la formation Chinle du Trias supérieur. Les visiteurs s'émerveillent devant les arbres fossilisés colorés dont le parc tire son nom, mais toute une série d'animaux ont élu domicile dans ces forêts marécageuses il y a 225 millions d'années [&hellip
17/03/2026 palaeocast ⚙ Traduction automatique
Des fossiles de poissons vieux de 400 millions d'années révèlent comment la vie a commencé à s'installer sur terre
Australie Chine fossile formation crâne
Les scientifiques ont découvert de nouveaux indices sur certains des premiers poissons de la Terre, mettant ainsi en lumière les origines anciennes des vertébrés qui ont fini par s’installer sur terre. En réanalysant de mystérieux fossiles de la célèbre formation australienne Gogo et en étudiant un crâne de poisson-poumon récemment reconstruit, vieux de 410 millions d'années et provenant de Chine, les chercheurs révèlent comment ces créatures primitives ont évolué.
12/03/2026 sciencedaily ⚙ Traduction automatique
Une ancienne sécheresse aurait pu anéantir les vrais hobbits il y a 61 000 ans
extinction formation
Une sécheresse massive qui a duré des siècles pourrait avoir entraîné l’extinction des « hobbits » de Flores. Les enregistrements climatiques conservés dans les formations souterraines montrent que les précipitations ont chuté au moment même où la petite espèce humaine disparaissait. Dans le même temps, le nombre d’éléphants pygmées dont ils dépendaient a fortement diminué à mesure que les rivières s’asséchaient. Avec la disparition de la nourriture et de l'eau, les hobbits ont peut-être été repoussés et entrés dans leur dernier chapitre.
19/02/2026 sciencedaily-human-evo ⚙ Traduction automatique
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