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ZHANG Yixuan, BAI Chenyang, LIU Yujia, YANG Hailin, LIVIO Ruffine, LAI Yong, LU Hailong. Sedimentary characteristics of the northern continental slope of the Danube Canyon in the northwest of the Black Sea and its relation with paleoclimate changes[J]. GEOLOGY IN CHINA, 2022, 49(3): 880-900. DOI: 10.12029/gc20220314
Citation: ZHANG Yixuan, BAI Chenyang, LIU Yujia, YANG Hailin, LIVIO Ruffine, LAI Yong, LU Hailong. Sedimentary characteristics of the northern continental slope of the Danube Canyon in the northwest of the Black Sea and its relation with paleoclimate changes[J]. GEOLOGY IN CHINA, 2022, 49(3): 880-900. DOI: 10.12029/gc20220314

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

Funds: 

program of Marine Geological Survey DD20190234

More Information
  • Author Bio:

    ZHANG Yixuan, female, born in 1996, master, mainly engaged in the study of marine sedimentary geology; E-mail: zhyixuan@pku.edu.cn

  • Corresponding author:

    LU Hailong, male, born in 1964, professor, mainly engaged in the study of gas hydrate; E-mail: hlu@pku.edu.cn

  • Received Date: March 01, 2020
  • Revised Date: May 07, 2020
  • Available Online: September 25, 2023
  • 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.

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