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 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.
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.
Ovi-caprid dung as an indicator of paleovegetation and paleoclimate in northwestern China.
RG Ruby Ghosh, SG Sudha Gupta, SB Subir Bera… - 2008 - cabidigitallibrary.org
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.
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.
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