|
The La Meseta Formation is a sedimentary sequence deposited during the Eocene. The formation is found on Seymour Island, Antarctica. La Meseta Formation lies unconformably on the Cretaceous Lopez de Bertodano Formation. It is an approximately 557 m thick sequence of poorly consolidated sandstones and siltstones. The depositional environment was probably coastal, deltaic or estuarine in character. The top of the sequence is an erosional unconformity to Pleistocene glacial gravels.〔 La Meseta Formation is just one of the sequences that make up the fill of the Late Jurassic to Paleogene James Ross Basin.〔 ==Fossils== La Meseta Formation is extremely rich in fossils. It is famous for its penguin fossils, for example the two genera ''Archaeospheniscus'' and ''Palaeeudyptes''. Other bird fossils include ''Dasornis'', a genus of pseudotooth birds. There are also an abundance of trace fossils. Diplocraterion, Helminthopsis, Muensteria, Oichnus, Ophiomorpha, Skolithos, Teredolites and Zapfella have been described. Over 35 species and 26 families of fish have been described from the Ypresian Cucullaea bed.〔 List of bird fossils: *''Archaeospheniscus wimani'' *''Archaeospheniscus lopdelli'' *''Palaeeudyptes antarcticus'' *''Palaeeudyptes gunnari'' *''Palaeeudyptes klekowskii'' 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「La Meseta Formation」の詳細全文を読む スポンサード リンク
|