Sedimentology of sediment core ANT34/A2-10

Explore the West Antarctic Ice Sheet instability through Pleistocene glacial/interglacial cycles can provide fundamental constraints on interactions between the climate system and cryosphere. To achieve this goal, we provide continuous records of iceberg-rafted debris (IRD) content and clay mineralo...

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Bibliographic Details
Main Authors: Wang, Jiakai, Li, Tiegang, Li, Dongyong
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Amundsen Sea
ANT34/A2-10
Antarctica
Chlorite
clay minerals
DEPTH
sediment/rock
GC
Gravity corer
Ice rafted debris
Illite
Illite chemistry index
Illite crystallinity
IRD
Kaolinite
Pleistocene
Smectite
Smectite crystallinity
Sr-Nd isotopes
water content
sediment
Amundsen Abyssal Plain
Antarctic
West Antarctic Ice Sheet
Antarc*
Ice Sheet
Iceberg*
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.949150
Description
Summary:Explore the West Antarctic Ice Sheet instability through Pleistocene glacial/interglacial cycles can provide fundamental constraints on interactions between the climate system and cryosphere. To achieve this goal, we provide continuous records of iceberg-rafted debris (IRD) content and clay mineralogy in gravity core ANT34/A2-10 from the Amundsen abyssal plain.

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