中太平洋海山铁锰结壳生物地层学研究

武光海; PULYAEVAIA; 刘捷红; 李雪富

中太平洋海山铁锰结壳生物地层学研究

1.
国家海洋局第二海洋研究所海洋生态系统与生物地球化学国家海洋局重点实验室,浙江杭州,310012
2.
Federal State Unitary Geological Enterprise"Kavkazgeolsyomka",Pyatigorsk,Russia

基金项目: 国家自然科学基金资助项目(40676025);中国大洋专项(DYXM-115-01-1-07)资助。

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出版历程
- 收稿日期: 2010-09-09

Biostratigraphic research on the seamount ferromanganese crusts of the mid-Pacific Ocean

1.
Key Laboratory of State Oceanic Administration for Marine Ecosystem & Biogeochemistry,Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
2.
Federal State Unitary Geological Enterprise"Kavkazgeolsyomka",Pyatigorsk,Russia

摘要

摘要: 用生物地层学方法对位于中太平洋同一座海山上的2块铁锰结壳样品进行了生物地层学详细研究,发现2块样品的生长层位对应,生物组合也相同。经鉴定,2块结壳的主要生长期都是晚古新世、中始新世至晚始新世、中中新世至上新世、上新世至更新世,2个主要的结壳生长间断分别在渐新世和早始新世。
- 中太平洋 /
- 海山铁锰结壳 /
- 生物地层学
Abstract: The detailed biostratigraphic research has been applied to two ferromanganese crusts which are sampled on a mid-Pacific seamount using the method of biostratigraphy.The results reveal that the growth layers of these two samples are homologous and their calcareous nannofossil complexes are the same,too. Based on the identification of calcareous nannofossil imprints and original fossil remains,the main growth periods of the two samples are Late Paleocene,Mid-Late Eocene,Mid Miocene to Pliocene and Pliocene to Pleistocene. On the other hand,the two main growth gaps are at Oligocene and Early Eocene.
- mid-Pacific Ocean /
- seamount ferromanganese crusts /
- biostratigraphy

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参考文献(38)

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