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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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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 speciesHave been identified in the sediments, of which the most abundant is loxoreticulatumFallax, the second abundant are xestoleberis keguelenensis, xestoleberis spp., Semicytherura spp., australicythere polylyca, etc. Most species of ostracodes are thoseKnown in antarctic area. Base on the study of ostracodes from the core ng93-1, theirSedimentary environment may be of shore-shallow sea. the holocene ostracode are analyzed from the core sample ng93-1 collectedIn the great wall bay, antarctica during 1992~1993. Totally 11 genera 21 speciesHave been identified in the sediments, of which the most abundant is loxoreticulatumFallax, the second abundant are xestoleberis keguelenensis, xestoleberis spp., Semicytherura spp., australicythere polylyca, etc. Most species of ostracodes are thoseKnown in antarctic area. Base on the study of ostracodes from the core ng93-1, theirSedimentary environment may be of shore-shallow sea.
作者 蔡慧梅
出处 《Chinese Journal of Polar Science》 1996年第2期141-149,共9页 极地研究(英文版)
关键词 the Great Wall Bay ANTARCTICA OSTRACODA sedimentary environment. the Great Wall Bay, Antarctica, ostracoda, sedimentary environment.
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