黑海西北部多瑙河峡谷北侧陆坡沉积特征及其与古气候的关系  

Sedimentary characteristics of the northern continental slope of the Danube Canyon in the northwest of the Black Sea and its relation with paleoclimate changes

作　　者：张艺璇 白辰阳 刘宇佳 杨海琳 LIVIO Ruffine 赖勇[1] 卢海龙[2,4] ZHANG Yixuan;BAI Chenyang;LIU Yujia;YANG Hailin;LIVIO Ruffine;LAI Yong;LU Hailong(School of Earth and Space Sciences,Peking University,Beijing 100871,China;Beijing International Center for Gas Hydrate,Peking University,Beijing 100871,China;School of Ocean Sciences,China University of Geosciences(Beijing),Beijing 100083,China;College of Engineering,Peking University,Beijing 100871,China;Institut fran?ais de recherche pour l'exploitation de la mer(IFREMER),Brest 29280,France)

机构地区：[1]北京大学地球与空间科学学院,北京100871 [2]北京大学北京天然气水合物国际研究中心,北京100871 [3]中国地质大学(北京)海洋学院,北京100083 [4]北京大学工学院,北京100871 [5]法国海洋开发研究院(IFREMER),布雷斯特29280

出　　处：《中国地质》2022年第3期880-900,共21页Geology in China

基　　金：国家专项“海洋地质调查和天然气水合物资源勘查试采”项目(DD20190234)。

摘　　要：【研究目的】在末次冰期,全球气候变化以千年尺度的快速、大幅度温度波动旋回为特征,这种波动变化在两极冰芯、深海沉积、中国黄土和洞穴石笋等诸多地质样品中均有记录。黑海位于北大西洋与东亚季风区过渡带,具有极有代表性的沉积记录。本文旨在通过对黑海沉积序列的研究,建立起其区域环境变化与北大西洋及东亚季风气候域气候变化的联系。【研究方法】研究对取自黑海西北部罗马尼亚陆坡区多瑙河峡谷北侧GAS-CS12钻孔的长22.0 m的岩芯样品,进行了粒度、矿物成分、主量元素、有机碳、总氮及碳氮同位素等分析。【研究结果】揭示出该段岩芯沉积于末次冰期中后期“Neoeuxine”湖相阶段,可划分为5个沉积单元,对应于北大西洋H4、H3、H1气候变化事件、末次冰盛期(LGM)及Bolling-Allerod气候变暖事件。【结论】建立起了其沉积序列及区域环境变化与北大西洋及东亚季风气候域气候变化的联系,印证了末次冰期千年尺度的气候变化事件在北大西洋、东亚季风区及两者过渡带上具有高度的一致性。This paper is the result of environmental geological survey engineering.[Objective]In the last glacial period,global climate was characterized by rapid,large-scale temperature cycles on a millennial scale.Such climate changes could be recorded in many geological materials such as ice cores,deep-sea sediments,Chinese loess,and cave stalagmites.The Black Sea is located in the transition zone between the North Atlantic and East Asian monsoon regions and has formed representative sedimentary records.This article is aimed at establishing the connections between the regional environmental changes of the Black Sea and the climate changes in the North Atlantic and East Asian monsoon area through the study of the sedimentary sequences of the Black Sea.[Methods]In this study,a 22.0 m core sample taken from Core GAS-CS12 in the northern slope of the Danube Canyon in the northwest of the Black Sea was analyzed for particle size,mineral composition,major elements,organic carbon,total nitrogen,and carbon and nitrogen isotopes.[Results]It was revealed that the core sediments of this section were deposited in the“Neoeuxine”lacustrine stage in the middle and late period of the last glacial period,and can be divided into 5 sedimentary units,corresponding to H4,H3,and H1 climate change events in the North Atlantic,the Last Glacial Maximum(LGM),and Bolling-Allerod climate warming event.[Conclusions]The connections between the sedimentary sequences and regional environmental changes of the Black Sea with the climate changes in the North Atlantic and East Asian monsoon area were established and this paper also confirmed that the millennium-scale climate changes of the last glacial period were highly consistent in the North Atlantic,East Asian monsoon area and their transition zones.

关 键 词：黑海 沉积学 粒度 同位素地球化学 古海洋 古气候 环境地质调查工程 

分 类 号：P532[天文地球—古生物学与地层学] P736.21[天文地球—地质学]