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 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.

Metadata Access
Creator Michel, Elisabeth ORCID logo; Mazaud, Alain; Bout-Roumazeilles, Viviane (ORCID: 0000-0001-6917-818X)
Publisher PANGAEA
Publication Year 2024
Rights Creative Commons Attribution 4.0 International;
OpenAccess true
Resource Type Bundled Publication of Datasets; Collection
Format application/zip
Size 3 datasets
Discipline Earth System Research
Spatial Coverage (80.394 LON, -44.679 LAT)