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西太平洋富钴结壳中钙质超微化石和分子化石研究

陈荣华 赵庆英 张海生 卢冰 Pulyaeva I A

陈荣华, 赵庆英, 张海生, 卢冰, Pulyaeva I A. 西太平洋富钴结壳中钙质超微化石和分子化石研究[J]. 海洋学报, 2015, 37(7): 132-141.
引用本文: 陈荣华, 赵庆英, 张海生, 卢冰, Pulyaeva I A. 西太平洋富钴结壳中钙质超微化石和分子化石研究[J]. 海洋学报, 2015, 37(7): 132-141.
Chen Ronghua, Zhao Qingying, Zhang Haisheng, Lu Bing, Pulyaeva I A. Calcareous nannofossil stratigraphy and molecular fossils in the Co-rich ferromanganese crust from the Western Pacific[J]. Haiyang Xuebao, 2015, 37(7): 132-141.
Citation: Chen Ronghua, Zhao Qingying, Zhang Haisheng, Lu Bing, Pulyaeva I A. Calcareous nannofossil stratigraphy and molecular fossils in the Co-rich ferromanganese crust from the Western Pacific[J]. Haiyang Xuebao, 2015, 37(7): 132-141.

西太平洋富钴结壳中钙质超微化石和分子化石研究

基金项目: 国家自然科学基金(41076072);国家自然科学基金重点基金项目(91128212).

Calcareous nannofossil stratigraphy and molecular fossils in the Co-rich ferromanganese crust from the Western Pacific

  • 摘要: 本文对西太平洋麦哲伦海山CM3D06富钴结壳进行了钙质超微化石生物地层学研究,发现结壳中有代表白垩纪(晚期)、古新世(晚期)、始新世(早、中、晚期)、中新世(中期)、上新世(晚期)和更新世等各时代的标准钙质超微化石,表明结壳的形成始于白垩纪(晚期);在富钴结壳中检出正构烷烃、类异戊二烯烃、甾烷类等众多分子化石,分子化石组合特征指数、主峰碳、ΣC23-/C24+、CPI 、Pr/Ph、Pr/nC17、Ph/nC18和nC31/nC17显示有机质生物母源主要为海洋浮游植物、浮游动物和底栖非光合作用的菌类,而甾烷类的C29、C28和C27含量分布的变化则说明生物种群具有快速演变的特征.此外,还探讨了CM3D06结壳中Pr/Ph和有机碳同位素组成变化与结壳生长过程中的海洋环境演化的关联程度.
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  • 收稿日期:  2014-06-25
  • 修回日期:  2015-02-10

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