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Ovi-caprid dung as an indicator of paleovegetation and paleoclimate in northwestern China
Diverse palynomorphs and phytoliths recovered from coprolites of ovi-caprids (sheep, goat) collected from Yang-Hai Tomb at Xinjiang Province, China, have been used to elucidate the dietary pattern of ancient livestock and to reconstruct the paleovegetation and paleoclimate of this part of northwest...
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Published in: | Quaternary research 2008-09, Vol.70 (2), p.149-157 |
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creator | Ghosh, Ruby Gupta, Sudha Bera, Subir Jiang, Hong-en Li, Xiao Li, Cheng-Sen |
description | Diverse palynomorphs and phytoliths recovered from coprolites of ovi-caprids (sheep, goat) collected from Yang-Hai Tomb at Xinjiang Province, China, have been used to elucidate the dietary pattern of ancient livestock and to reconstruct the paleovegetation and paleoclimate of this part of northwest China ca. 2500 14C yr BP. Palynological and phytolith data suggest that a rich dry temperate vegetation prevailed in the area during the said period. Climatic conditions and grassland vegetation type of the area are explored using phytolith indices. |
doi_str_mv | 10.1016/j.yqres.2008.02.007 |
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subjects | ca. 2500 years BP China Original Articles Ovi-caprid dung Paleoclimate Paleovegetation Phytoliths Pollens Xinjiang Province |
title | Ovi-caprid dung as an indicator of paleovegetation and paleoclimate in northwestern China |
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