热带海洋学报 ›› 2018, Vol. 37 ›› Issue (1): 64-71.doi: 10.11978/2017022CSTR: 32234.14.2017022

所属专题: 南海专题

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南海北部冷泉区深水珊瑚的发现及其特征

陈忠1(), 莫爱彬1,2, 赵美霞1, 仲义1,2, 颜文1,2   

  1. 1. 中国科学院边缘海与大洋地质重点实验室(南海海洋研究所), 广东 广州 510301
    2. 中国科学院大学, 北京 100049
  • 收稿日期:2017-02-26 修回日期:2017-05-10 出版日期:2018-01-20 发布日期:2018-02-02
  • 作者简介:

    作者简介:陈忠(1970—), 男, 云南省石屏县人, 研究员, 主要从事海洋地质与资源环境研究。E-mail: chzhsouth@scsio.ac.cn

  • 基金资助:
    国家自然科学基金面上项目(41376057、41676056)

The discovery of deep-water corals from cold seep area in the northern South China Sea and their characteristics

Zhong CHEN1(), Aibin MO1,2, Meixia ZHAO1, Yi ZHONG1,2, Wen YAN1,2   

  1. 1. CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Guangzhou 510301, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2017-02-26 Revised:2017-05-10 Online:2018-01-20 Published:2018-02-02
  • Supported by:
    National Natural Science Foundation (41376057, 41676056)

摘要:

冷水珊瑚也称为深水珊瑚, 在生物多样性、生态资源和科研价值等方面具有重要意义。文章对采自南海北部冷泉区的冷水珊瑚骨骼碎屑进行测定, 鉴定出冷水珊瑚2个种(Crispatotrochus sp.1和Crispatotrochus sp.2), 以及4个属[Balanophyllia (Balanophyllia)、Balanophyllia (Eupsammia)、LochmaeotrochusEnallopsammia]。测定的冷水珊瑚的δ13C为-7.36‰~-1.15‰, δ18O为-1.38‰~3.67‰, 与全球冷水珊瑚碳氧同位素组成相似, 但明显不同于南海暖水珊瑚、冷泉碳酸盐岩及低温热液成因碳酸盐岩的碳氧同位素组成。

关键词: 冷水珊瑚, 冷泉渗漏, 碳氧同位素, 海底底流, 南海北部

Abstract:

Cold-water corals, also known as deep-water corals, are newly found ecological resources with high biological diversity and attract scientific research on environmental changes. In this study, we investigated cold-water corals retrieved from the cold seep area in the northern South China Sea. We identified two species (Crispatotrochus sp.1, Crispatotrochus sp.2) and four genera [Balanophyllia (Balanophyllia), Balanophyllia (Eupsammia), Lochmaeotrochus, and Enallopsammia]. Stable carbon and oxygen isotopic analyses revealed that the δ13C and δ18O of cold-water corals were -7.36‰ ~ -1.15‰ and -1.38‰ ~ 3.67‰, respectively. The δ13C and δ18O results were close to the carbon and oxygen isotopic values of cold-water corals in other parts of the world, but were quite different from those of warm-water corals, cold-seep carbonate rocks and low-temperature hydrothermal carbonate rocks. This research discovered cold-water corals in a cold seep region of the northern South China Sea. This discovery is important for the studies on environmental effects of deep-water currents and of cold springs in the region.

Key words: deep-water corals, hydrocarbon seepage, C-O isotope, bottom current, northern South China Sea

中图分类号: 

  • P736.2