What is it about?
δ18O and δ13C in fossil shells of Radix sp. from the sediment succession of a dammed palaeo-lake in the Yarlung Tsangpo valley, Tibet, China
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Why is it important?
d18Oshell values of modern Radix sp. significantly depend on the d18Owater of the ambient water body and its hydrological status.
Perspectives
The d18Owater values of the palaeo-water body and hydrological regime could be reconstructed using the d18Oshell values of Radix sp. fossil shells.
Prof. Jin-Liang FENG
Institute of Tibetan Plateau Research, Chinese Academy of Sciences
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This page is a summary of: δ18O and δ13C in fossil shells ofRadixsp. from the sediment succession of a dammed palaeo-lake in the Yarlung Tsangpo valley, Tibet, China, Boreas, February 2017, Wiley,
DOI: 10.1111/bor.12231.
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