Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Hangfang Xiao"'
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 13, Pp n/a-n/a (2023)
Abstract The 4.2 ka BP Event is an abrupt climate change that might have contributed to the collapse of ancient civilizations and marks the transition between the mid‐ and late‐Holocene. Despite considerable research on this event, our understand
Externí odkaz:
https://doaj.org/article/4704b19e6312402d8f54376e3eeb3c3a
Autor:
Hangfang Xiao, Wenfeng Deng, Gangjian Wei, Jiubin Chen, Xinqing Zheng, Tuo Shi, Xuefei Chen, Chenying Wang, Xi Liu, Ti Zeng
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 11, Pp n/a-n/a (2020)
Abstract The trace metal element zinc (Zn) participates in coral metabolic processes and therefore accumulates in their skeletons. These metabolic processes are largely controlled by the changes of environment in which they live, so Zn isotopic compo
Externí odkaz:
https://doaj.org/article/10c35fb79bd248d89ccc7e3934a00131
Autor:
Xi Liu, Jian-xin Zhao, Xuefei Chen, Wenfeng Deng, Ti Zeng, Gangjian Wei, Hangfang Xiao, Yangrui Guo
Publikováno v:
Journal of Geophysical Research: Oceans. 126
Climate change in the mid‐to‐late Holocene transition is very important for predicting future climate trends and understanding the relationship between abrupt climate change and the development of past human civilization. In this study, Sr/Ca rat
Autor:
Chenying Wang, Jiubin Chen, Xinqing Zheng, Hangfang Xiao, Ti Zeng, Xuefei Chen, Tuo Shi, Gangjian Wei, Xi Liu, Wenfeng Deng
Publikováno v:
Geochemistry, Geophysics, Geosystems. 21
Publikováno v:
Journal of Asian Earth Sciences. 135:25-34
The past two millennia include some distinct climate intervals, such as the Medieval Warm Period (MWP) and the Little Ice Age (LIA), which were caused by natural forcing factors, as well as the Current Warm Period (CWP) that has been linked to anthro
Publikováno v:
Regional Studies in Marine Science. 33:100950
The complicated effects of climatic and environmental conditions on coral δ 13 C have hindered its use as a universal proxy for biological activity and climate change. Changes in annual resolution δ 13 C levels from the South China Sea (SCS) were s
Autor:
Hangfang Xiao1,2, Wenfeng Deng1,3 wfdeng@gig.ac.cn, Xi Liu1,3, Xuefei Chen1,3, Yangrui Guo1,3, Jian-xin Zhao4, Ti Zeng3,5, Gangjian Wei1,3
Publikováno v:
Journal of Geophysical Research. Oceans. Feb2021, Vol. 126 Issue 2, p1-15. 15p.