Stratigraphic gaps at northern South China Sea margin reflect changes in Pacific deepwater inflow at glacial Termination II

Stratigraphic gaps at northern South China Sea margin reflect changes in Pacific deepwater inflow at glacial Termination II
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南海北部边缘的地层间隙反映了冰川终止处太平洋深水流入的变化

DOI:
10.1007/s11430-013-4678-2
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发表时间:
2013-08
期刊:
Science China Earth Sciences
影响因子:
--
通讯作者:
Sarnthein, M., Sadatzki, H., Jian, Z.
Sarnthein, M., Sadatzki, H., Jian, Z.
中科院分区:
其他
文献类型:
--
作者:
Sarnthein, M., Sadatzki, H., Jian, Z.;Sarnthein, M., Sadatzki, H., Jian, Z.

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To constrain short-term changes of climate and oceanography in the northern South China Sea (SCS) over interglacial marine isotope stage (MIS) 5.5, we studied planktic and benthic δ18O records of seven marine sediment cores with a time resolution of 70–70
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