Low-latitude climate change linked to high-latitude glaciation during the late paleozoic ice age: Evidence from terrigenous detrital kaolinite

Low-latitude climate change linked to high-latitude glaciation during the late paleozoic ice age: Evidence from terrigenous detrital kaolinite

The Late Paleozoic Ice Age (LPIA; ca. 335–260 million years ago) was one of the most significant glacial events in Earth’s history. It records cycles of ice advance and retreat in southern high-latitude Gondwana and provides a deep-time perspective for climate–glaciation coevolution. However, climat...

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Bibliographic Details
Main Authors: Peixin Zhang, Minfang Yang, Jing Lu, Longyi Shao, Ziwei Wang, Jason Hilton
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-08-01
Series:Frontiers in Earth Science
Subjects:
high-latitude glaciation
clay minerals
terrigenous detrital kaolinite
paleoclimate
low-latitudes
north China
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2022.956861/full

Internet

https://www.frontiersin.org/articles/10.3389/feart.2022.956861/full

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