Paleoclimatological records of the Great Ghost Lake in Taiwan

Distinctive white laminations appear in the black sediments of the Great Ghost Lake in Taiwan.Compared with the black sediments, these white laminations have lower porosity, organic matter content and C/N ra-tio, but higher C/S and N/S ratios, and with organic matter characterized by the phytoplankt...

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Published inScience China. Earth sciences Vol. 40; no. 3; pp. 284 - 292
Main Author 罗建育 陈镇东 万政康
Format Journal Article
LanguageEnglish
Published Dordrecht Springer Nature B.V 01.06.1997
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ISSN1674-7313
1006-9313
1869-1897
1862-2801
DOI10.1007/bf02877537

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Summary:Distinctive white laminations appear in the black sediments of the Great Ghost Lake in Taiwan.Compared with the black sediments, these white laminations have lower porosity, organic matter content and C/N ra-tio, but higher C/S and N/S ratios, and with organic matter characterized by the phytoplanktons. It suggests thatthey may be deposited in cooler and drier periods. The organic matter of the black sediments was mainiy from landplants, suggesting deposition under warmer and wetter climates. Major white laminations appear in 0 AD, 500 AD,70D AD, 900 AD, 1 350 AD, 1 500 AD, etc., and cortespond to the periods of cold/dry and frequent dust stormsfrom the historical and natural records of China or Peru. These seem to reflect large-scale climatic changes.
Bibliography:LOU Jiann-Yuh , CHEN Chen-Tung Arthurand WANN Jen-Kang(Institute of Marine Geology and Chemistry, Sun Yat-sen University, Gaoxiong, Taiwan, China)
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ISSN:1674-7313
1006-9313
1869-1897
1862-2801
DOI:10.1007/bf02877537