Maceral, Total Organic Carbon, and Palynological Analyses of Ross Ice Shelf Project Site J9 Cores
作者： J. H. WRENN , S. W. BECKMAN
DOI: 10.1126/SCIENCE.216.4542.187
关键词: Paleontology 、 Ice shelf 、 Total organic carbon 、 Palynology 、 Paleogene 、 Dinocyst 、 Maceral 、 Project site 、 Geology 、 Flora
摘要: Analyses of macerals and total organic carbon indicate that the low content core sediments from Ross Ice Shelf Project site J9 has been selectively reduced further, probably by postdepositional submarine oxidation. Palynological analysis revealed a reworked Paleogene dinocyst flora diversity (the transantarctic flora). This constitutes most southerly reported thus far. The antarctic distribution supports existence strait during Paleogene. sporomorph assemblage also is in age.
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