Magnetic and mineralogic properties, summer sea surface temperature for core MD12-3401Cq for the last deglaciation

The volume low-field susceptibility (k) and the Anhysteretic Remanent Magnetization (ARM) divided by k were measured using u-channel sampling technique on 2G cryogenic magnetometers at the Laboratoire des Sciences du Climat et de l'Environnement (LSCE). The Summer sea surface temperature has be...

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Bibliographic Details
Main Authors: Michel, Elisabeth, Mazaud, Alain, Bout-Roumazeilles, Viviane
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2024
Subjects:
Antarctic Circumpolar Current
magnetic parameters
mineralogic parameters
Summer sea surface temperature
Antarctic
Antarc*
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.958410
https://doi.org/10.1594/PANGAEA.958410
Description
Summary:The volume low-field susceptibility (k) and the Anhysteretic Remanent Magnetization (ARM) divided by k were measured using u-channel sampling technique on 2G cryogenic magnetometers at the Laboratoire des Sciences du Climat et de l'Environnement (LSCE). The Summer sea surface temperature has been determined by N. pachyderma s. percentages and planktic foraminifera assemblages (in the >150µ fraction) at LSCE. The percentage of clay and silt were measured at Laboratoire d'Océanologie et de Géosciences, Université de Lille, using a laser (0.02 -2000 µm) Malvern Mastersizer 2000.

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