Quantitative Reconstruction of Paleoclimatic Changes in the Late Miocene Eastern Zhejiang Based on Plant Fossils

With a series of Cenozoic climate fluctuations, the global paleoclimate shifted from a warm climate to a cold climate, causing Arctic ice caps to be formed. The Late Miocene is a critical time in this transition period, in which the climate was rapidly cooling. Plant fossils from this epoch could be...

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Bibliographic Details
Main Authors: Liang Xiao, Jian Wang, Deshuang Ji, Liyan Guo, Xing Wang, Jiaqi Liang, Xiaoyuan Xia, Wenxiu Ren, Xiangchuan Li
Format: Article
Language:English
Published: MDPI AG 2023-06-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/14/6/986