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e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">A Preliminary Study of the espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />eName w:st="on">HoloceneeName> eType w:st="on">LakeeType> Level Changes and Their Causes Derived from the Sediment Record of e w:st="on">eName w:st="on">ZigetangeName> eType w:st="on">LakeeType>e>, Tibetan Plateau
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e="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>e="FONT-FAMILY: ’Times New Roman’; FONT-SIZE: 14pt; mso-fareast-font-family: 宋体; mso-ansi-language: EN-US; mso-fareast-language: ZH-CN; mso-bidi-language: AR-SA" lang=EN-US>The espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />e w:st="on">eName w:st="on">ZigetangeName> eType w:st="on">LakeeType>e> is an enclosed lake, located in the hinterland of the North Tibetan Plateau and within the marginal region of southwest monsoon. There is no distribution of glacier in the catchment, and the precipitation controlled by the southwest monsoon is the main water supply for the e w:st="on">eName w:st="on">ZigetangeName> eType w:st="on">LakeeType>e>. Therefore, the expansion and contraction of lake water area reflects the changes of southwest monsoon directly. The analysis results for a etcnv w:st="on" TCSC="0" NumberType="1" Negative="False" HasSpace="True" SourceValue="740" UnitName="cm">740 cmetcnv>-long core drilled in the central Zigetang Lake show that this core has completely covered the="FONT-FAMILY: ’Times New Roman’; FONT-SIZE: 14pt; mso-fareast-font-family: 宋体; mso-ansi-language: EN-US; mso-fareast-language: ZH-CN; mso-bidi-language: AR-SA" lang=EN-US>e whole Holocene period and that the carbonate concentration decreased greatly during 9.3~8.9, 8.3~7.8, 5.0~4.7, 4.0~3.8, and 3.1~2.7 cal ka B.P., respectively, indicating the desalination of the lake and the rise of the lake level.

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