Data for: The geochemical and mineralogical fingerprint of West Antarctica's weak underbelly: Pine Island and Thwaites glaciers

Published: 26 April 2021| Version 1 | DOI: 10.17632/cfnhps54h7.1
Patric Simões Pereira


The full dataset is based on seafloor surface sediment from 26 sites and consists of strontium and neodymium isotope, and major and trace element compositions of fine-grained sediments, as well as 40Ar/39Ar ages of individual ice-rafted hornblende and biotite grains, clay mineral compositions and rock magnetic properties of bulk sediment fractions.