Paléocène

Intervalle géologique

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“Golden spike” at the GSSP of the Selandian stage (lower Upper Paleocene) at Zumaia section, Spanish Basque Country. The spike sits on the top plane of the uppermost limestone bed of the Aitzgorri Limestone Formation which is identical to the basal plane of the overlying red marls of the lowest part of the Itzurun Formation (right-hand outside the picture).[1]

“Golden spike” at the GSSP of the Selandian stage (lower Upper Paleocene) at Zumaia section, Spanish Basque Country. The spike sits on the top plane of the uppermost limestone bed of the Aitzgorri Limestone Formation which is identical to the basal plane of the overlying red marls of the lowest part of the Itzurun Formation (right-hand outside the picture).[1]

Paléocène Sélandien formation
Information sign for the GSSP of the Seelandian stage (lower Upper Paleocene) at Zumaia section, Spanish Basque Country. The sign is mounted near the “golden spike” on the top plane of the uppermost limestone bed of the Aitzgorri Limestone Formation which is identical to the basal plane of the overlying red marls of the lowest part of the Itzurun Formation (right-hand outside the picture).[1]

Information sign for the GSSP of the Seelandian stage (lower Upper Paleocene) at Zumaia section, Spanish Basque Country. The sign is mounted near the “golden spike” on the top plane of the uppermost limestone bed of the Aitzgorri Limestone Formation which is identical to the basal plane of the overlying red marls of the lowest part of the Itzurun Formation (right-hand outside the picture).[1]

Paléocène formation
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

Actualités

Fish Fossils from Early Paleocene Fill 10-Million-Year Gap after Dinosaur Extinction
Des fossiles de poissons du début du Paléocène comblent un écart de 10 millions d'années après l'extinction des dinosaures
Égypte Paléocène fossile Dinosauria extinction
Les paléontologues ont décrit un assemblage de fossiles de poissons marins provenant du site de Qreiya 3, vieux de 62,2 millions d'années, dans le désert oriental d'Égypte, ouvrant ainsi une fenêtre sur cette transition. L'article Les fossiles de poissons du début du Paléocène comblent un écart de 10 millions d'années après l'extinction des dinosaures est apparu en premier sur Sci.News : Breaking Science News.
05/06/2026 sci-news ⚙ Traduction automatique