Increased terrigenous input from North America to the northern Mendeleev Ridge (western Arctic Ocean) since the mid-Brunhes Event

Mid-Brunhes Event (MBE) occurred at approximately 420 ka between Marine Isotope Stage 11 and 12, and is considered the most pronounced climatic shift during the last ~ 800 kyrs. On the other hand, it is unclear if the MBE was global, despite being observed in the high-latitude Northern Hemispheric c...

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Detalles Bibliográficos
Autores principales: Park, Kwangkyu, Wang, Rujian, Xiao, Wenshen, Polyak, Leonid, Cho, Hyen Goo, Khim, Boo-Keun
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9452527/
https://www.ncbi.nlm.nih.gov/pubmed/36071079
http://dx.doi.org/10.1038/s41598-022-19082-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9452527/
https://www.ncbi.nlm.nih.gov/pubmed/36071079
http://dx.doi.org/10.1038/s41598-022-19082-y

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