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ZHANG Yixuan, BAI Chenyang, LIU Yujia, YANG Hailin, LIVIO Ruffine, LAI Yong, LU Hailong. 2022. 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, 49(3): 880-900. doi: 10.12029/gc20220314
Citation: ZHANG Yixuan, BAI Chenyang, LIU Yujia, YANG Hailin, LIVIO Ruffine, LAI Yong, LU Hailong. 2022. 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, 49(3): 880-900. doi: 10.12029/gc20220314
shu

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

  • 1.

    School of Earth and Space Sciences, Peking University, Beijing 100871, China

  • 2.

    Beijing International Center for Gas Hydrate, Peking University, Beijing 100871, China

  • 3.

    School of Ocean Sciences, China University of Geosciences (Beijing), Beijing 100083, China

  • 4.

    College of Engineering, Peking University, Beijing 100871, China

  • 5.

    Institut français de recherche pour l'exploitation de la mer (IFREMER), Brest 29280, France

    • Fund Project: Supported by program of Marine Geological Survey (No.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:  02 March 2020
Revised Date:  08 May 2020
Publish Date:  25 June 2022
    Abstract

  • 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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