Information om | Engelska ordet KASIMOVIAN

Exempel på hur man kan använda KASIMOVIAN i en mening

• The base of the Kasimovian Stage is at the base of the fusulinid biozone of Obsoletes obsoletes and Protriticites pseudomontiparus or with the first appearance of the ammonite genus Parashumardites.
• It was collected in the Hamilton Quarry, from the Calhouns Shale Formation of the Shawnee Group, dating to the Virgilian stage (or alternatively late Kasimovian to early Gzhelian stage) of the Late Pennsylvanian Series, about 300 million years ago.
• The top of the Moscovian (base of the Kasimovian) is at the base of the fusulinid biozone of Obsoletes obsoletes and Protriticites pseudomontiparus, or with the first appearance of the ammonite genus Parashumardites.
• The Westphalian extends from the approximately the upper half of the Bashkirian Stage through the Moscovian Stage, and possibly includes a small portion of the Kasimovian Stage.
• Even older are the trematopids Actiobates and Anconastes, which are Missourian (Kasimovian) and early Virgilian in age, respectively.
• With fossils found from the Kasimovian (Missourian) stage of the Late Carboniferous of Pennsylvania, Colorado, and New Mexico in the United States, Desmatodon is the oldest known diadectid.
• It was collected in the Hamilton Quarry, from the Calhouns Shale Formation of the Shawnee Group, dating to the Virgilian stage (or alternatively late Kasimovian to early Gzhelian stage) of the Late Pennsylvanian Series, about 300 million years ago.
• eltringhami is known from the Upper Carboniferous of England (Westphalian A = Moscovian, Crock Hey, Wigan, Greater Manchester; Coseley, Dudley, West Midlands; Westhoughton, Lancashire; Sparth Bottoms, Lancashire; and Westphalian B = Kasimovian, Tyne Coalfield, Crawcrook, Durham).
• The lower beds may be Missourian (Kasimovian) in age while the uppermost beds may be Wolfcampian (Cisuralian) in age.
• These rocks have been assigned to the Late Pennsylvanian subperiod of the Carboniferous period, specifically near the transition between the Kasimovian and Gzhelian ages around 304 Ma (million years ago).
• The unit contains middle to upper Missourian (Kasimovian) fusulinids The formation has also produced a lacustrine fauna from one of its shell beds, including the horseshoe crab Euproops danae.
• Fossils of this species were found in the Kasimovian of Iowa, Gzhelian of Nebraska, Asselian of Kansas.
• orodontus lived between 307–304 million years ago, during the latest Moscovian to Kasimovian stages (described by Zangerl as the equivalent Westphalian D substage) of the Pennsylvanian subperiod.

Förberedelsen av sidan tog: 265,27 ms.