Illuminating the Meaning of Asian Monsoon Cave Speleothem Records

被引：7
|
作者：
Lachniet, Matthew S. [1 ]
机构：
[1] Univ Nevada, Dept Geosci, Las Vegas, NV 89154 USA
来源：
PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY | 2020年 / 35卷 / 01期
关键词：
Paleoclimate; Asian Monsoon; oxygen isotopes; isotope enabled models;
D O I：
10.1029/2019PA003841
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
The Asian Monsoon is one of Earth's major climatic zones, and its past history is of prime interest to paleoclimatologists interested in disentangling the various forcings that have controlled its strength over time. With the iconic speleothem (cave calcite) records from oxygen isotopes (d18O) now reaching back 650,000 years (Cheng et al., 2016), much attention has focused on the origins of the Asian Monsoon variations. The speleothem records showed a strong control Earth's 23,000 year orbital precession cycle on variations in d18O, and these isotope variations in turn have been interpreted as proxies of monsoon processes.
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