Rapid fluvial incision and headward erosion by the Yellow River along the Jinshaan gorge during the past 1.2 Ma as a result of tectonic extension

Understanding past climate events relies for a large part on correlations between various proxy records. For the last glacial cycle, these are mainly marine and ice core records. However, such tele-connections are often based on weak arguments. For terrestrial data the Hengelo interstadial is a key...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Hu, Z., Pan, B., Guo, L., Vandenberghe, J.F., Liu, X., Wang, J., Fan, Y., Mao, J., Gao, H., Hu, X.
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
/dk/atira/pure/sustainabledevelopmentgoals/life_below_water
name=SDG 14 - Life Below Water
ice core
Online Access:https://research.vu.nl/en/publications/377bb552-f4fb-4758-81ea-89b3f6f4fe44
https://doi.org/10.1016/j.quascirev.2015.12.003
https://hdl.handle.net/1871.1/377bb552-f4fb-4758-81ea-89b3f6f4fe44
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Summary:Understanding past climate events relies for a large part on correlations between various proxy records. For the last glacial cycle, these are mainly marine and ice core records. However, such tele-connections are often based on weak arguments. For terrestrial data the Hengelo interstadial is a key event, discovered more than 4 decades ago. Here we review the age of this event, in particular by its

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