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Chinese Academy of Sciences Institutional Repositories Grid
Potential water sources for Late Quaternary Megalake Jilantai-Hetao, China, inferred from mollusk shell Sr-87/Sr-86 ratios

文献类型:期刊论文

作者Fan, Yu-Xin1,2; Chen, Fa-Hu1; Wei, Guo-Xiao1; Madsen, David B.3; Oviatt, Charles G.4; Zhao, Hui1,5; Chun, Xi1; Yang, Li-Ping1; Fan, Tian-Lai1; Li, Guo-Qiang1
刊名JOURNAL OF PALEOLIMNOLOGY
出版日期2010-03-01
卷号43期号:3页码:577-587
关键词Strontium isotope ratios Water sources Late Quaternary Megalake Jilantai-Hetao
ISSN号0921-2728
DOI10.1007/s10933-009-9353-4
通讯作者Fan, Yu-Xin(yxfan@lzu.edu.cn)
英文摘要Lake Jilantai-Hetao, a megalake, was formed some time before 60-50 ka, along the Great North Bend of the Yellow River. The basin is now dry, with most of the area covered by aeolian sand. We are investigating this profound hydrologic change using a number of research approaches. Paleoshorelines of this megalake are best preserved in the Jilantai area in the southwestern portion of the megalake basin. We collected aquatic mollusk shells from littoral sediments at different altitudes around Jilantai and measured their strontium isotope compositions. Sr-87/Sr-86 ratios in shell carbonates are different between the high lake phase (similar to 1,080-1,050 m altitude) and the low lake phase (similar to 1,044-1,030 m altitude), with a small shift in average strontium ratios to more radiogenic values during the low lake phase. Based on regional hydrology and physical geography, we conclude that water from the Yellow River was the dominant water source supplying this megalake. Sr-87/Sr-86 ratios of modern water samples suggest the Yellow River was the dominant water source during the high lake phase, but that the relative contribution of Yellow River water to the megalake was reduced, and that the relative contributions of local precipitation and groundwater increased, during the low lake phase.
收录类别SCI
WOS关键词TENGGER-DESERT ; NW CHINA ; LAKE ; HISTORY
WOS研究方向Environmental Sciences & Ecology ; Geology ; Marine & Freshwater Biology
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary ; Limnology
语种英语
WOS记录号WOS:000275415900012
出版者SPRINGER
URI标识http://www.irgrid.ac.cn/handle/1471x/2556417
专题寒区旱区环境与工程研究所
通讯作者Fan, Yu-Xin
作者单位1.Lanzhou Univ, CAEP, MOE Key Lab W Chinas Environm Syst, Lanzhou 730000, Peoples R China
2.Northwest Univ, State Key Lab Continental Dynam, Xian 710069, Peoples R China
3.Univ Texas Austin, Texas Archeol Res Lab, Austin, TX 78712 USA
4.Kansas State Univ, Dept Geol, Manhattan, KS 66506 USA
5.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Fan, Yu-Xin,Chen, Fa-Hu,Wei, Guo-Xiao,et al. Potential water sources for Late Quaternary Megalake Jilantai-Hetao, China, inferred from mollusk shell Sr-87/Sr-86 ratios[J]. JOURNAL OF PALEOLIMNOLOGY,2010,43(3):577-587.
APA Fan, Yu-Xin.,Chen, Fa-Hu.,Wei, Guo-Xiao.,Madsen, David B..,Oviatt, Charles G..,...&Li, Guo-Qiang.(2010).Potential water sources for Late Quaternary Megalake Jilantai-Hetao, China, inferred from mollusk shell Sr-87/Sr-86 ratios.JOURNAL OF PALEOLIMNOLOGY,43(3),577-587.
MLA Fan, Yu-Xin,et al."Potential water sources for Late Quaternary Megalake Jilantai-Hetao, China, inferred from mollusk shell Sr-87/Sr-86 ratios".JOURNAL OF PALEOLIMNOLOGY 43.3(2010):577-587.

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