太平洋海山富钴结壳钙质超微化石生物地层学及生长过程

张海生; 韩正兵; 雷吉江; 赵军; 于培松; 胡佶; 卢冰; PulyaevaI.A.

doi:10.3799/dqkx.2014.073

Volume 39 Issue 7

Jul. 2014

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Article Navigation > Earth Science > 2014 > 39(7): 775-783

Zhang Haisheng, Han Zhengbing, Lei Jijiang, Zhao Jun, Yu Peisong, Hu Ji, Lu Bing, Pulyaeva I.A., 2014. Calcareous Nannofossil Biostratigraphy and Growth Periods of Co-Rich Crusts from Pacific Seamounts. Earth Science, 39(7): 775-783. doi: 10.3799/dqkx.2014.073

Citation:

Zhang Haisheng, Han Zhengbing, Lei Jijiang, Zhao Jun, Yu Peisong, Hu Ji, Lu Bing, Pulyaeva I.A., 2014. Calcareous Nannofossil Biostratigraphy and Growth Periods of Co-Rich Crusts from Pacific Seamounts. Earth Science, 39(7): 775-783. doi: 10.3799/dqkx.2014.073

Citation:

Zhang Haisheng, Han Zhengbing, Lei Jijiang, Zhao Jun, Yu Peisong, Hu Ji, Lu Bing, Pulyaeva I.A., 2014. Calcareous Nannofossil Biostratigraphy and Growth Periods of Co-Rich Crusts from Pacific Seamounts. Earth Science, 39(7): 775-783. doi: 10.3799/dqkx.2014.073

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Calcareous Nannofossil Biostratigraphy and Growth Periods of Co-Rich Crusts from Pacific Seamounts

doi: 10.3799/dqkx.2014.073

Zhang Haisheng^{1, 2
,},
Han Zhengbing^{1, 2},
Lei Jijiang²,
Zhao Jun^{1, 2},
Yu Peisong^{1, 2},
Hu Ji^{1, 2},
Lu Bing^{1, 2},
Pulyaeva I.A.³

1.
Key Laboratory of Marine Ecosystem and Biogeochemistry, SOA, Hangzhou 310012, China
2.
Second Institute of Oceanography, SOA, Hangzhou 310012, China
3.
State Scientific Centre Yuzhmorgeologia, Gelendzhik 353461, Russia

Received Date: 2013-09-10
Publish Date: 2014-07-15

Abstract

Abstract

It enriches the geological history of Co-rich crusts (CRC) formation and the paleoceanography for us to understand the growth ages and periods of CRC. CRC samples collected from the Magellan and mid-Pacific seamounts were studied for the growth geological ages and periods by employing biostratigraphy (biological impressions). The primary formation geological ages and calcareous nannofossil assembly are different between CM3D06 CRC from the Magellan seamount and CB14 CRC from the mid-Pacific seamount. Based on the identification of calcareous nannofossil imprints and original fossil remains,five growth periods are determined for CM3D06 CRC,namely,Cretaceous (or older),Late Paleocene-Early Eocene,Middle-Late Eocene,Middle-Late Miocene,and Pliocene-Pleistocene,whereas four growth periods for CB14 CRC are determined as follows: Late Paleocene,Middle-Late Eocene,Middle Miocene,and Pliocene to Pleistocene. Regional characteristics for the nannofossil combination features of two CRC samples indicate the impact of oceanic environment on marine organisms and their adaptation. The unconformity of sub-layers and variation of structure and texture of the two CRC samples show that the main hiatus occurred during Oligocene.
- Co-rich crust,
- calcareous nannofossil,
- biostratigraphy,
- geological age,
- Pacific seamount,
- geochemistry

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References(61)

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