1431 / 2019-08-10 14:49:57
What factors govern sedimentary CaCO3 distributions in marginal sea: A case study from the Western Pacific regions
Abstract Pending
Marginal sea biogeochemical cycles are either dominated by continental processes, or oceanic processes where deep marginal-sea basins are effectively influenced by the global ocean deep water. However, how those different processes influence the global carbon cycles under different hydrological settings are not fully understood. By studying the sedimentary calcium carbonate (CaCO3) distributions in several Western-Pacific (WP) marginal seas, we theoretically explain how their distribution features are shaped by different conditions. Our results suggest that, among all sedimentary CaCO3 data only records from the Tasman Sea present similar patterns with those from the global ocean, reflecting remarkable ocean dominated features in carbonate chemistry. While in other basins, carbonate distributions show different characteristics mostly associated with their unique hydrological settings and ecosystem features. Therefore, future interpretation of marginal-sea CaCO3 data in terms of global carbon cycles and large-scale climate changes should be treated with particular cautions.
Important Date
  • Conference Date

    Oct 12

    2019

    to

    Oct 15

    2019

  • Sep 30 2019

    Draft paper submission deadline

  • Oct 15 2019

    Registration deadline

  • Jul 21 2020

    Contribution Submission Deadline

Sponsored By
青年地学论坛理事会
Organized By
中国科学院青海盐湖研究所
中国科学院西北高原生物研究所
青海师范大学
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