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- W2393060351 abstract "Loess deposit on the Chinese Loess Plateau is an important terrestrial archive for investigating paleoclimatic change.Quantitative reconstruction of loess recording the paleotemperature change is key important factor for understanding the mechanism of climate change.Over the past several decades,magnetic susceptibility,phytoliths,dissociative iron oxide(FeD) and total iron oxide(FeT),and glycerol dialkyl glycerol tetraethers(GDGT) have been employed to quantitatively reconstruct the temperature change recorded in loess deposit.This paper briefly introduces the regular methods for reconstructing the paleotemperature information recorded in loess deposit since Late Quaternary,and discusses their limitations.Accurate quantitative reconstruction of paleotemperature change recorded by loess deposit needs more proxy indexes and methods for cross-check." @default.
- W2393060351 created "2016-06-24" @default.
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- W2393060351 date "2013-01-01" @default.
- W2393060351 modified "2023-09-24" @default.
- W2393060351 title "Research Progress on Quantitative Reconstruction of Paleotemperature Recorded in Loess Deposit Since Late Quaternary" @default.
- W2393060351 hasPublicationYear "2013" @default.
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