Richard T. Jones

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John M Kelso1
Chris Turney1
Jason Jordan1
Enlou Zhang1
1John M Kelso
1Chris Turney
1Jason Jordan
1Enlou Zhang
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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(More)
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