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西藏台错古湖晚第四纪轮藻类及其生态环境、气候变化探讨
引用本文:刘俊英,王海雷.西藏台错古湖晚第四纪轮藻类及其生态环境、气候变化探讨[J].微体古生物学报,2011(3):13-34.
作者姓名:刘俊英  王海雷
作者单位:国土资源部盐湖资源与环境重点实验室;中国地质科学院盐湖与热水资源研究中心;中国地质科学院地质研究所;中国地质科学院矿产资源研究所;
基金项目:国家自然科学基金重点项目(编号40531002); 国家大地调项目(121201081805、1212010818057)资助成果
摘    要:西藏台错TT-1剖面厚369 cm,为一套碳酸盐粘土和粘土碳酸盐沉积,地层测年为41.4-4.5 ka,含丰富的轮藻化石,分属于11个轮藻植物群,群落所在地层的碳酸盐和钙质含量分别为80%和33%.从老到新(剖面自下而上):①41.4-26.64 ka(369-319 cm),处于末次冰期间冰阶MIS3a暖期,湖区气候...

关 键 词:轮藻类  生态环境  晚第四纪  台错古湖  西藏

STUDY ON THE LATE QUATERNARY CHAROPHYTES,ECOLOGICAL ENVIRONMENT AND CLIMATE AT PALEOLAKE TAICUO,TIBET
LIU Junying, WANG Hailei, Key Laboratory of Saline Lake Resources , Environment,Ministry of L, Resources,Beijing Saline Lake , Thermal liquid Resources Research Centre,Chinese Academy of Geological Sciences,Beijing Institute of Geology,Beijing Institute of Mineral Resources,Beijing.STUDY ON THE LATE QUATERNARY CHAROPHYTES,ECOLOGICAL ENVIRONMENT AND CLIMATE AT PALEOLAKE TAICUO,TIBET[J].Acta Micropalaeontologica Sinica,2011(3):13-34.
Authors:LIU Junying      WANG Hailei  Key Laboratory of Saline Lake Resources  Environment  Ministry of L  Resources  Beijing Saline Lake  Thermal liquid Resources Research Centre  Chinese Academy of Geological Sciences  Beijing Institute of Geology  Beijing Institute of Mineral Resources  Beijing
Institution:LIU Junying1,2,3) and WANG Hailei1,4)1) Key Laboratory of Saline Lake Resources and Environment,Ministry of Land and Resources,Beijing 1000372) Saline Lake and Thermal liquid Resources Research Centre,Chinese Academy of Geological Sciences,Beijing 1000373) Institute of Geology,Beijing 1000374) Institute of Mineral Resources,Beijing 100037
Abstract:The section TT-1 at Taicuo,Tibet is 369 cm of carbonate-bearing clay and clay-bearing carbonate sequence,aged 41.4—4.5 ka,rich in fossil charophyte which can be subdivided into 11 floras.Five palaeoenvironmental development stages of the palaeolake Taicuo can be recognized.(1) 41.4—26.64 ka(369—319 cm),a warm period in MIS 3a,when the climate was warm and wet,the water was deep and unrest,with lower contents of carbonate and calcium(13%—21% and 4.4%—6.6%),and no charophytes existed.(2) 26.64—20.48 ka(319—284 cm),a flourishing period of the floras,when water plants were lush,and the water had a higher content of calcium and organic carbon,especially during 25.20—22.45 ka(319—301 cm).The climate was still warm and wet,after about 22 ka.However,the climate tended to be cold and dry,and the water temperarure was going down.(3)20.48—14.60 ka(284—217 cm),the charophytes were less flourishing as the climate became colder and drier,which caused by the decline of water temperature and nutrients.All this was a reflection of the global LMG climate in the lake.(4) 14.60—10.40 ka(217—125 cm),the charophytes got flourishing again,but the climate was variable in the lake resulted in the frequent water temperature fluctuation.As a result,there was also an inconstant amount of gyrogonites produced.In the period of 13.62—12.35 ka,as it turned comparatively warm and wet and the water temperature went up,the charophytes got quite lush with adequate nutrients and oxygen.But the reproduction of the floras declined later during the Younger Dryas period.(5) 10.43—4.5 ka(125—0 cm),the climate in the lake tended to be warm and wet,and the charophytes were in a well-growing state.The charophytes became more thriving during 6.20—4.5 ka as the environmental humidity got higher and the water temperature increased,and the floras reproduction ranks the second in the section.
Keywords:charophytes  ecological environment  Late Quaternary  Taicuo  palaeolake  Tibet(Xizang)  China  
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