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...

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Bibliographic Details
Main Authors: Ceccaroni, L, Frank, Martin, Frignani, M, Langone, Leonardo, Ravaioli, Mariangela, Mangini, Augusto
Format: Dataset
Language:English
Published: PANGAEA 1998
Subjects:
GC
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.735096
https://doi.org/10.1594/PANGAEA.735096