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南极长城湾全新世有孔虫研究
引用本文:涂霞,郑范.南极长城湾全新世有孔虫研究[J].海洋地质与第四纪地质,1996,16(3):123-136.
作者姓名:涂霞  郑范
作者单位:中国科学院南海海洋研究所
摘    要:南极长城湾93I(62°17.74′S,58°49.91′W)柱样含有较丰富的有孔虫动物群,计鉴定统计51900个体,归属于86种,有孔虫总丰度以柱样中段较低,浮游类含量较低(〈5%)钙质类底栖有孔虫成占优势,全柱底栖有孔虫分异度变化范围不大,底栖有孔虫五个优势种的优势度占决量的83.3%,优势种及其组合变化显著一定的古海洋学意义,探讨了长城湾海区晚第四纪环境变迁,为南大洋晚第四纪环境与全球变化关

关 键 词:南极  长城湾  有孔虫  古海洋学  全新世

HOLOCENE FORAMINIFERA IN GREAT WALL BAY,ANTARCTICA
Tu Xia Zheng Fan.HOLOCENE FORAMINIFERA IN GREAT WALL BAY,ANTARCTICA[J].Marine Geology & Quaternary Geology,1996,16(3):123-136.
Authors:Tu Xia Zheng Fan
Abstract:Foraminifera faunas in core NG93 I from Great Wall Bay,Antarctica,were ana-lyzed.Foraminifera faunas are relatively abundant in the sediment of core NG93 I.To-tally are found 51900 speciments from the core which belong to 86 species and mainlycalcareous benthonic foraminifera,The planktonic foraminifera only makes up a percent-age of less than 5%, The lowest abundance of foraminifera occurs in the middle of thecore. The variation of benthonic foraminiferal diversity is very small in this region,Con-tent of five dominant species reaches 83.3%,And the dominant species and their assem-blages reflect sedimentary environment and paleooceanographic features,and provide im-portant evidence for paleoclimatic changes.
Keywords:Great Wall Bay Antarctica foraminifera paleooceanography
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