Foraminiferal assemblages and CaCO3 dissolution since the last deglaciation in the Maxwell Bay, King George Island, Antarctica
Three sediment cores (A10-01, -02 and -08) from the Maxwell Bay, King George Island, Antarctica were quantitatively analyzed for foraminiferal fauna. Planktonic foraminifera of three cores are rare due to the special Antarctica environment. Benthic foraminifera is mainly composed of Globocassidulina...
Main Authors: | , , |
---|---|
Format: | Report |
Language: | English |
Published: |
ELSEVIER SCIENCE BV
2000
|
Subjects: | |
Online Access: | http://ir.nigpas.ac.cn/handle/332004/801 |