Holocene ostracoda and sedimentary environment implication in The core NG93-1 from the Great Wall Bay, Antarctica

极地研究 ›› 1996, Vol. 7 ›› Issue (2-English): 141-149.

Holocene ostracoda and sedimentary environment implication in The core NG93-1 from the Great Wall Bay, Antarctica

Cai Huimei

South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

出版日期:1946-06-30 发布日期:1946-06-30
通讯作者: Cai Huimei
基金资助:
The project was supported by the State Anarctic Committee of China.

Holocene ostracoda and sedimentary environment implication in The core NG93-1 from the Great Wall Bay, Antarctica

Cai Huimei

South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

Online:1946-06-30 Published:1946-06-30
Contact: Cai Huimei
Supported by:
The project was supported by the State Anarctic Committee of China.

摘要/Abstract

摘要：

The Holocene ostracode are analyzed from the core sample NG93-1 collectedIn the Great Wall Bay, Antarctica during 1992～1993. Totally 11 genera 21 species have been identified in the sediments, of which the most abundant is Loxoreticulatum fallax, the second abundant are Xestoleberis keguelenensis, Xestoleberis spp., Semicytherura spp., Australicythere polylyca, etc. Most species of ostracodes are those known in Antarctic area. Base on the study of ostracodes from the core NG93-1, their sedimentary environment may be of shore-shallow sea.

关键词: the Great Wall Bay, Antarctica, ostracoda, sedimentary environment

Abstract:

Key words: the Great Wall Bay, Antarctica, ostracoda, sedimentary environment

Cai Huimei. Holocene ostracoda and sedimentary environment implication in The core NG93-1 from the Great Wall Bay, Antarctica[J]. 极地研究, 1996, 7(2-English): 141-149.

Cai Huimei. Holocene ostracoda and sedimentary environment implication in The core NG93-1 from the Great Wall Bay, Antarctica[J]. ADVANCES IN POLAR SCIENCE, 1996, 7(2-English): 141-149.

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Holocene ostracoda and sedimentary environment implication in The core NG93-1 from the Great Wall Bay, Antarctica

Holocene ostracoda and sedimentary environment implication in The core NG93-1 from the Great Wall Bay, Antarctica

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