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Detailed analyses of planktonic foraminifera at Site 17964 from the southern South China Sea (SCS) disclose that warm-water species have a higher percentage during the Holocene, while temperate-water species have a higher content for the last glacial period. Therefore, the sea surface temperature (SST) is a main factor that affects the foraminiferal assemblage at this site. A remarkable faunal variation...
This paper documents abundant and diverse foraminifers from Permian-Triassic (P-Tr) boundary strata and reports for the first time foraminifers from the Lower Triassic Yinkeng and Helongshan Formations in the Meishan section, the global stratotype for the P-Tr boundary. The important foraminifer elements are illustrated and described. Most of these foraminifers were the Permian holdovers, occurring...
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