Evolution of a Late Pleistocene palaeolake in Dali Nor area of southeastern Inner Mongolia Plateau, China
Lithological, geochronological, granulometric, and scanning electron microscope (SEM) analyses of eight lacustrine outcrops indicate the existence of a large palaeolake in Dali Nor area during 149e24.6 ka (MIS5-3) and a small one in upstream of the Xilamulun River during 12.96-11.69 ka. The large pa...
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| Veröffentlicht in: | Di xue qian yuan. 2018, Vol.9 (1), p.223-237 |
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| creator | Lan, Yuanhong Tian, Mingzhong Zhang, Xujiao Wen, Xuefeng Kang, Chunjing |
| description | Lithological, geochronological, granulometric, and scanning electron microscope (SEM) analyses of eight lacustrine outcrops indicate the existence of a large palaeolake in Dali Nor area during 149e24.6 ka (MIS5-3) and a small one in upstream of the Xilamulun River during 12.96-11.69 ka. The large palaeolake recorded its highest water level above 1300 m during the MIS3 and covered the whole Dali Nor basin and upstream of the Xilamulun River within an area of about 3000 km2. However, the small palaeolake with a highest water level above 1200 m, covered an area of about 600 km2. Besides the reconstruction of palaeolake areas, this study also looked into the evolutionary process of the palaeolake during the Late Pleistocene. Our data provide insights on the timing of appearance of the large palaeolakes and a better understanding of the mechanism responsible for variations in the environment conditions of dry lands in middle latitudes. |
| doi_str_mv | 10.1016/j.gsf.2017.03.003 |
| format | Article |
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The large palaeolake recorded its highest water level above 1300 m during the MIS3 and covered the whole Dali Nor basin and upstream of the Xilamulun River within an area of about 3000 km2. However, the small palaeolake with a highest water level above 1200 m, covered an area of about 600 km2. Besides the reconstruction of palaeolake areas, this study also looked into the evolutionary process of the palaeolake during the Late Pleistocene. Our data provide insights on the timing of appearance of the large palaeolakes and a better understanding of the mechanism responsible for variations in the environment conditions of dry lands in middle latitudes.</description><identifier>ISSN: 1674-9871</identifier><identifier>EISSN: 2588-9192</identifier><identifier>DOI: 10.1016/j.gsf.2017.03.003</identifier><language>eng</language><publisher>Oxford: Elsevier B.V</publisher><subject>area;Palaeolake ; Dali Nor area ; Geochronology ; Geological time ; High lake level ; lake ; Lakes ; Late ; Late Pleistocene ; level;Dali ; Lithology ; Nor ; Outcrops ; Palaeolake ; Pleistocene ; Pleistocene;High ; Scanning electron microscopy ; Sediments ; Upstream ; Water levels</subject><ispartof>Di xue qian yuan., 2018, Vol.9 (1), p.223-237</ispartof><rights>2017 China University of Geosciences (Beijing) and Peking University</rights><rights>Copyright Elsevier Science Ltd. Jan 2018</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a451t-f9be4ac54e9e5e9e918de9482f0bf8f71cf4dc801f552bdce59c6eac111e6fe23</citedby><cites>FETCH-LOGICAL-a451t-f9be4ac54e9e5e9e918de9482f0bf8f71cf4dc801f552bdce59c6eac111e6fe23</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/71129X/71129X.jpg</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S1674987117300506$$EHTML$$P50$$Gelsevier$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,3537,4010,27900,27901,27902,65306</link.rule.ids></links><search><creatorcontrib>Lan, Yuanhong</creatorcontrib><creatorcontrib>Tian, Mingzhong</creatorcontrib><creatorcontrib>Zhang, Xujiao</creatorcontrib><creatorcontrib>Wen, Xuefeng</creatorcontrib><creatorcontrib>Kang, Chunjing</creatorcontrib><title>Evolution of a Late Pleistocene palaeolake in Dali Nor area of southeastern Inner Mongolia Plateau, China</title><title>Di xue qian yuan.</title><addtitle>Geoscience Frontiers</addtitle><description>Lithological, geochronological, granulometric, and scanning electron microscope (SEM) analyses of eight lacustrine outcrops indicate the existence of a large palaeolake in Dali Nor area during 149e24.6 ka (MIS5-3) and a small one in upstream of the Xilamulun River during 12.96-11.69 ka. The large palaeolake recorded its highest water level above 1300 m during the MIS3 and covered the whole Dali Nor basin and upstream of the Xilamulun River within an area of about 3000 km2. However, the small palaeolake with a highest water level above 1200 m, covered an area of about 600 km2. Besides the reconstruction of palaeolake areas, this study also looked into the evolutionary process of the palaeolake during the Late Pleistocene. Our data provide insights on the timing of appearance of the large palaeolakes and a better understanding of the mechanism responsible for variations in the environment conditions of dry lands in middle latitudes.</description><subject>area;Palaeolake</subject><subject>Dali Nor area</subject><subject>Geochronology</subject><subject>Geological time</subject><subject>High lake level</subject><subject>lake</subject><subject>Lakes</subject><subject>Late</subject><subject>Late Pleistocene</subject><subject>level;Dali</subject><subject>Lithology</subject><subject>Nor</subject><subject>Outcrops</subject><subject>Palaeolake</subject><subject>Pleistocene</subject><subject>Pleistocene;High</subject><subject>Scanning electron microscopy</subject><subject>Sediments</subject><subject>Upstream</subject><subject>Water levels</subject><issn>1674-9871</issn><issn>2588-9192</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNp9kUFPGzEQha2qSI0oP4CbpR64dLf2eje2xQmltEVKCwc4WxPvOHG62Im9S-Hf4yhUvdXSyJf33sx8Q8g5ZzVnfP5lW6-zqxvGZc1EzZh4R2ZNp1SluW7ekxmfy7bSSvIP5CznLStPSiUlmxF__RSHafQx0Ogo0CWMSO8G9HmMFgPSHQyAcYDfSH2gX2Hw9FdMFBLCwZHjNG4Q8ogp0JsQMNGfMazj4KHElDCYPtPFxgf4SE4cDBnP3v5T8vDt-n7xo1refr9ZXC0raDs-Vk6vsAXbtaixK6W56lG3qnFs5ZST3Lq2t4px13XNqrfYaTtHsJxznDtsxCm5OOb-geAgrM02TimUjqZ_3r8YLJiKm_G2KD8dlbsU9xPm8Z-0Ya0QomQe8vhRZVPMOaEzu-QfIb0YzswBv9magt8c8BsmTMFfPJdHD5ZFnzwmk63HYLH3Ce1o-uj_636by24Kyr0vO_xtKcvphNZCKPEKDhGY4A</recordid><startdate>2018</startdate><enddate>2018</enddate><creator>Lan, Yuanhong</creator><creator>Tian, Mingzhong</creator><creator>Zhang, Xujiao</creator><creator>Wen, Xuefeng</creator><creator>Kang, Chunjing</creator><general>Elsevier B.V</general><general>Elsevier Science Ltd</general><general>School of Earth Sciences and Resources, China University of Geosciences (Beijing),29 Xueyuan Road,Beijing 100083,China%College of Agriculture,Guizhou University, Guiyang 550025,China%The Fourth Geological Exploration Institute of Henan Geology and Mineral Bureau,Zhengzhou 450001, China</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>2018</creationdate><title>Evolution of a Late Pleistocene palaeolake in Dali Nor area of southeastern Inner Mongolia Plateau, China</title><author>Lan, Yuanhong ; 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The large palaeolake recorded its highest water level above 1300 m during the MIS3 and covered the whole Dali Nor basin and upstream of the Xilamulun River within an area of about 3000 km2. However, the small palaeolake with a highest water level above 1200 m, covered an area of about 600 km2. Besides the reconstruction of palaeolake areas, this study also looked into the evolutionary process of the palaeolake during the Late Pleistocene. Our data provide insights on the timing of appearance of the large palaeolakes and a better understanding of the mechanism responsible for variations in the environment conditions of dry lands in middle latitudes.</abstract><cop>Oxford</cop><pub>Elsevier B.V</pub><doi>10.1016/j.gsf.2017.03.003</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | area Palaeolake Dali Nor area Geochronology Geological time High lake level lake Lakes Late Late Pleistocene level Dali Lithology Nor Outcrops Palaeolake Pleistocene Pleistocene High Scanning electron microscopy Sediments Upstream Water levels |
| title | Evolution of a Late Pleistocene palaeolake in Dali Nor area of southeastern Inner Mongolia Plateau, China |
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