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A 1000-yr record of environmental change in NE China indicated by diatom assemblages from maar lake Erlongwan

Wang, Luo; Rioual, Patrick; Panizzo, Virginia N.; Lu, Houyuan; Gu, Zhaoyan; Chu, Guoqiang; Yang, Deguang; Han, Jingtai; Liu, Jiaqi; Mackay, Anson W.

Authors

Luo Wang

Patrick Rioual

Houyuan Lu

Zhaoyan Gu

Guoqiang Chu

Deguang Yang

Jingtai Han

Jiaqi Liu

Anson W. Mackay



Abstract

Past environmental changes based on diatom relative abundances have been inferred from the maar Lake Erlongwan in northeast China. The limnology of Lake Erlongwan is affected by the strongly seasonal regional climate. The composition of diatom assemblages, in turn, responds to changes in the seasonal duration of ice cover in winter, water-column turnover in spring and autumn, and thermal stratification in summer. Statistical analysis of the sedimentary diatom assemblages reveals three significant stratigraphic zones over the past 1000. yr. The highest abundance of the planktonic species . Discostella species occurs between AD 1050 and 1400 and suggests an annual ice-free period of long duration and well-developed summer stratification of the water column. This planktonic diatom peak between ca. AD 1150 and 1200 suggests that this period was the warmest over the past 1000. yr. The interval between AD 1400 and 1800 is marked by a decline in planktonic diatoms and suggests shorter duration of the ice-free season, weaker water stratification and possibly generally cold conditions. After AD 1800 relative abundances of planktonic diatoms, including . Puncticulata praetermissa and . Asterionella formosa, increase again, which indicates lengthening of the duration of the annual ice-free period and a stronger overturn of the water column. All these data imply that the pattern of the seasons is different between the MWP and the 20th century. © 2012 University of Washington.

Journal Article Type Article
Acceptance Date Mar 1, 2012
Online Publication Date Apr 17, 2012
Publication Date Jul 1, 2012
Deposit Date Sep 8, 2020
Journal Quaternary Research
Print ISSN 0033-5894
Electronic ISSN 1096-0287
Publisher Cambridge University Press (CUP)
Peer Reviewed Peer Reviewed
Volume 78
Issue 1
Pages 24-34
DOI https://doi.org/10.1016/j.yqres.2012.03.006
Public URL https://nottingham-repository.worktribe.com/output/4889060
Publisher URL https://www.cambridge.org/core/journals/quaternary-research/article/1000yr-record-of-environmental-change-in-ne-china-indicated-by-diatom-assemblages-from-maar-lake-erlongwan/CE740B948AC193C98BDCA9F0266534E8