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Reconstruction of the generation, development, and evolution of modern storms through paleotempestology is used to understand the regularity of storm activity and the relationship between storm activity and global climate change. Existing paleotempestology research in China is concentrated mainly on the low latitude sediments deposited since the Holocene (about 7000a). In this study, we examine the...
The influence of the Kuroshio Current (KC) intrusion on the depositional environment of the northern South China Sea (SCS) is discussed based on multi-proxies of surface sediments including planktonic foraminifera, clay minerals and geochemical elements. The results reveal that four typical planktonic foraminifera (Globigerinoides ruber, G. sacculifer, Neogloboquadrina dutertrei and Pulleniatina obliquiloculata)...
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