Calcareous nannofossil bioevents and microtektite stratigraphy in the Western Philippine Sea during the Quaternary
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- 作者：HanJie Sun (1) (2)
TieGang Li (1)
RongTao Sun (3)
XinKe Yu (1)
FengMing Chang (1)
Zheng Tang (1) (4) - 关键词：Western Philippine Sea ; Quaternary Period ; calcareous nannofossil biostratigraphy ; oxygen isotope stratigraphy ; Australasian microtektites
- 刊名：Chinese Science Bulletin
- 出版年：2011
- 出版时间：September 2011
- 年：2011
- 卷：56
- 期：25
- 页码：2732-2738
- 全文大小：658KB
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TieGang Li (1)
RongTao Sun (3)
XinKe Yu (1)
FengMing Chang (1)
Zheng Tang (1) (4)
1. Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China
2. Graduate University of the Chinese Academy of Sciences, Beijing, 100049, China
3. School of Resource & Environment Engineering, Shandong University of Technology, Zibo, 255049, China
4. China Geological Survey, Qingdao Institute of Marine Geology, Qingdao, 266007, China - ISSN：1861-9541
文摘
Two sediment cores, MD06-3050 and MD06-3047, were analyzed to study the Quaternary calcareous nannofossil and microtektite records. We dated bioevents and the microtektite impact event by calibrating with oxygen isotope stratigraphy. Seven calcareous nannofossil bioevents were identified over the past 2.36 Ma including the last appearance of data for Discoaster brouweri, Calcidiscus macintyrei, large Gephyrocapsa and Pseudoemiliania lacunosa, the first appearance of data for large Gephyrocapsa and Emiliania huxleyi, and the abrupt increase in the abundance of Gephyrocapsa caribbeanica. In addition, we fortunately observed that Australasian microtektites were distributed in core MD06-3050 from 1340 to 1374 cm.