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柴达木盆地诺木洪贝壳堤水体演变的介形类证据
引用本文:李玮,屈海英,李莎,周淑敏,宋先腾,王晓楠.柴达木盆地诺木洪贝壳堤水体演变的介形类证据[J].现代地质,2022,36(1):14-26.
作者姓名:李玮  屈海英  李莎  周淑敏  宋先腾  王晓楠
作者单位:1. 青海大学 地质工程系,青海 西宁 8100162. 四川省雅安生态环境监测中心站,四川 雅安 6250003. 中国科学院南京地质古生物研究所,江苏 南京 2100084. 中国地质调查局西宁自然资源综合调查中心,青海 西宁 8100005. 中国地质大学(北京) 地球科学与资源学院,北京 100083
基金项目:青海省科技计划项目(2017-ZJ-955Q);
摘    要:柴达木盆地贝壳堤保存有大量大小混杂及两壳绞合的双壳类化石,是全球干旱区罕见的地貌景观,为青藏高原东北部中晚更新世的气候与环境演化提供了重要的区域地质记录.该记录在诺木洪西北约20 km出露,将其命名为诺木洪贝壳堤.目前诺木洪贝壳堤的沉积属性存在河湖之争,对该贝壳堤剖面开展系统的介形类分析,建立了8个生物组合带,除1带化...

关 键 词:柴达木盆地  诺木洪贝壳堤  介形类  河流沉积
收稿时间:2020-10-16
修稿时间:2020-12-11

Water Evolution of Nuomuhong Shell Ridge in Qaidam Basin: Evidence from Ostracods
LI Wei,QU Haiying,LI Sha,ZHOU Shumin,SONG Xianteng,WANG Xiaonan.Water Evolution of Nuomuhong Shell Ridge in Qaidam Basin: Evidence from Ostracods[J].Geoscience——Journal of Graduate School,China University of Geosciences,2022,36(1):14-26.
Authors:LI Wei  QU Haiying  LI Sha  ZHOU Shumin  SONG Xianteng  WANG Xiaonan
Abstract:As a rare and distinctive geomorphological feature in arid regions around the world, a shell ridge in the Qaidam Basin preserves many bivalve fossils of different sizes and articulated shells, which provides important record for the paleoclimate and paleoenvironmental evolution of the middle-late Pleistocene NE Tibetan Plateau. The Nuomuhong Shell Ridge is newly discovered as fluvial sediments, which is different from early studies of lacustrine deposits. Through systematic analyses, we established eight ostracod assemblages for the Shell Ridge. Though scarce ostracod fossils were found in Assemblage 1 and they were hardly identified, fossils in other assemblages were relatively abundant. We named Assemblage 2 to 8 as follows: Ilyocypris-Candona-Candoniella, Ilyocypris-Candona-Leucocythere-Candoniella-Eucypris inflate, Leucocythere-Ilyocypris, Ilyocypris-Leucocythere-Candoniella-Candona, Ilyocypris-Candoniella-Leucocythere, Ilyocypris bradyi-Ilyocypris echinata and Ilyocypris bradyi-Candoniella. We clarified water evolution of the Shell Ridge based on ostracod fossil characteristics and their paleoecology information. We identified the Nuomuhong Shell Ridge fluvial deposits that went through frequent river diversions within the Assemblage 1 to 5 occurrence, during which the shell ridge sedimentation fluctuated between oxbow lake and shallow river environments. The shallow river environment was favorable for the living of ostracods, whereas the deeper water of oxbow lake was detrimental to their survival. The shallow river condition continued through the time of Assemblage 6 to 8, during which ostracods thrived in warmer climate till the river enclosed and salinity increased, which hampered ostracod survival. Subsequently, salt crust was likely formed after persistent droughts and the deposition of Nuomuhong Shell Ridge ended.
Keywords:Qaidam Basin  Nuomuhong Shell Ridge  ostracod  fluvial deposit  
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