Geochemistry of sediments from the continental slope of the Ross Sea, Antarctica
A sediment core, collected from the western part of the continental slope of the Ross Sea at 2380 m water depth, records events of the last two climatic cycles (250 kyr). A 230Thex-based chronology was obtained and boundaries of the isotope stages were set assuming that biological productivity was e...
Main Authors: | , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1998
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.735096 https://doi.org/10.1594/PANGAEA.735096 |