Holocene environmental change at Lake Shudu, Yunnan Province, southwestern China

Jones, Richard T., Cook, Charlotte G., Zhang, Enlou, Langdon, Peter G., Jordan, Jason and Turney, Chris (2012) Holocene environmental change at Lake Shudu, Yunnan Province, southwestern China. Hydrobiologia (doi:10.1007/s10750-012-1124-y).


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A Holocene palaeorecord from Lake Shudu, Yunnan Province, southwestern China is dominated by (1) a pronounced basin-wide sedimentary hiatus after ca. 7.2 kcal yr BP, spanning some 4,000 years and (2) significant changes in sediment source/supply and an increase in heavy metal influx coupled with a shift to more eutrophic lake conditions from ca. 0.9 kcal yr BP, lasting ~300 years. The hiatus is most likely a due to a significant and abrupt reduction in sedimentation rates, the driver of which is unclear; although it appears likely to have been climatically driven. The environmental changes captured in the Lake Shudu palaeorecord provide unambiguous evidence of late Holocene anthropogenic activity, most likely linked to mining activity.

Item Type: Article
Digital Object Identifier (DOI): doi:10.1007/s10750-012-1124-y
ISSNs: 0018-8158 (print)
1573-5117 (electronic)
Keywords: holocene, southwestern china, asian monsoon, lake sediments, past climate change
Subjects: D History General and Old World > DS Asia
G Geography. Anthropology. Recreation > G Geography (General)
Q Science > QH Natural history
Divisions : Faculty of Social and Human Sciences > Geography and Environment > Palaeoenvironment Laboratory
ePrint ID: 339662
Accepted Date and Publication Date:
13 May 2012Published
Date Deposited: 29 May 2012 10:08
Last Modified: 31 Mar 2016 14:29
URI: http://eprints.soton.ac.uk/id/eprint/339662

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