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Climate and vegetation variations since the LGM recorded by biomarkers from a sediment core in the northern South China SeaNARA Subscribed
Variations in stable carbon isotopic compositions of n ‐alkanes (δ 13 C alk ) and n ‐alkane proxies (CPI, C 31 /C 27 and ACL) from core MD05‐2905 (20° 08.17′ N, 117° 21.6′ E) in the northern South China Sea (SCS), provided evidence of biological responses on adjacent land areas in the form of changes in terrestrial vegetation and provenance of the remains of land plants during and since the Last Glacial Maximum (LGM). Decrease...
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