ADVANCES IN POLAR SCIENCE ›› 1998, Vol. 9 ›› Issue (1-English): 1-8.

• Contents •     Next Articles

Silica oxygen isotope record of core PC10 diatoms from the Bransfield Strait, Antarctica and its application in sedimentology

Duan Weiwu1, Li Xuejie1 and Shen Youlin2   

  1. 1Guangzhou Marine Geological Survey, MGMR, Guangzhou 510075, China 2Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
  • Online:1948-03-30 Published:1948-03-30
  • Contact: Duan Weiwu

Abstract:

51 diatom samples taken from the piston core PC10 in the Bransfield Strait of West Antarctica were determined by using silica oxygen isotope analysis.The diatom-based results reveal that the 753 cm long core PC10 was deposited in the area in the last 112.5 ka B. P., representing 1-5 oxygen isotopic stages and including one incomplete glacial/interglacial cycle and a postglacial period. The sedimentation rate in interglacial period seems to be a little higher than that in glacial, owing to the more terrigenous supply by ice-rafting during the interglacial stages.

Key words: Antarctica, Bransfield Strait, diatom oxygen isotope, sedimentology