Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

The causes of Mid-Pleistocene Transition global cooling 1 million years ago are still unknown. Here, the authors find the subarctic North Pacific became stratified during these glaciations due to closure of the Bering Strait, which would have removed CO2 from the atmosphere and caused global cooling...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Sev Kender, Ana Christina Ravelo, Savannah Worne, George E. A. Swann, Melanie J. Leng, Hirofumi Asahi, Julia Becker, Henrieka Detlef, Ivano W. Aiello, Dyke Andreasen, Ian R. Hall
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2018
Materias:
Q
Acceso en línea:https://doaj.org/article/66fa5f167de24bb1b71227a993df911e
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
Descripción
Sumario:The causes of Mid-Pleistocene Transition global cooling 1 million years ago are still unknown. Here, the authors find the subarctic North Pacific became stratified during these glaciations due to closure of the Bering Strait, which would have removed CO2 from the atmosphere and caused global cooling.