Eco-environmental changes in the Chinese Loess Plateau during low-eccentricity interglacial Marine Isotope Stage 19  

作　　者：Yueting ZHANG Naiqin WU Fengjiang LI Qingzhen HAO Yajie DONG Dan ZHANG Houyuan LU 

机构地区：[1]Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China [2]College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100049,China [3]Innovation Academy for Earth Science,Chinese Academy of Sciences,Beijing 100029,China [4]CAS Center for Excellence in Life and Paleoenvironment,Beijing 100044,China [5]Center for Excellence in Tibetan Plateau Earth Science,Chinese Academy of Sciences,Beijing 100101,China

出　　处：《Science China Earth Sciences》2020年第9期1408-1421,共14页中国科学（地球科学英文版）

基　　金：supported by the National Natural Science Foundation of China(Grant No.41430103);the Strategic Priority Research Program of Chinese Academy of Sciences(Grant No.XDB26000000);the China Postdoctoral Science Foundation(Grant No.2017M620895)。

摘　　要：Eco-environmental changes during interglacials with an astronomical background similar to that of the Holocene are potentially helpful for understanding the future climatic evolution.Marine oxygen isotope stage(MIS)19 is similar to the Holocene in astronomical background,both being characterized by a low eccentricity of the Earth’s orbit.However,MIS 19 has attracted research attention only recently and therefore less is known about eco-environmental changes during this interval,especially based on terrestrial records.In the Chinese Loess Plateau(CLP),the S7 paleosol can provide valuable terrestrial paleoclimatic and paleoenvironmental record for MIS 19.Here,high-resolution terrestrial snail records from the L8–L7 strata of the Huining,Xifeng and Luochuan sequences in the CLP were analyzed in order to characterize spatio-temporal changes in climate and eco-environment during MIS 20–18.The results show that in all three sections the late part of MIS 20 was dominated by abundant cold-aridiphilous mollusc species,indicating that cold and dry climatic conditions prevailed across the entire CLP,under the strong influence of the winter monsoon.The mollusc fauna of MIS 19 were dominated by warmth-loving and thermohumidiphilous species that enable the definition of two climatic stages.The early part of MIS 19(~790–778 ka)was marked by warm and humid conditions,as evidenced by high abundances of warmth-loving and thermo-humidiphilous species.This interval was slightly warmer than today and it lasted for^12 kyr.The climate of the later part of MIS 19(~778–761 ka)was more moderate,and increased proportions of cold-aridiphilous and warmth-loving species were recorded.The warmth of this period was similar to that of today,but the climatic fluctuations were stronger.During the early part of MIS 18(~761–745 ka),the Xifeng and Luochuan sections in the eastern CLP still maintained high abundances of warmth-loving and thermo-humidiphilous species,indicating that the moderate climatic conditions during late MIS 19 contin

关 键 词：Chinese loess-paleosol sequences Terrestrial mollusc fossils Low-eccentricity interglacial MIS 19 Climatic and environmental pattern 

分 类 号：P532[天文地球—古生物学与地层学] P59[天文地球—地质学]