Ultra-depleted hydrogen isotopes in hydrated glass record Late Cretaceous glaciation in Antarctica
Demian A. Nelson,
John M. Cottle (),
Ilya N. Bindeman and
Alfredo Camacho
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Demian A. Nelson: University of California
John M. Cottle: University of California
Ilya N. Bindeman: University of Oregon
Alfredo Camacho: University of Manitoba
Nature Communications, 2022, vol. 13, issue 1, 1-9
Abstract:
Abstract The Early Jurassic Butcher Ridge Igneous Complex (BRIC) in the Transantarctic Mountains contains abundant and variably hydrated silicic glass which has the potential to preserve a rich paleoclimate record. Here we present Fourier Transform Infrared Spectroscopic data that indicates BRIC glasses contain up to ~8 wt.% molecular water (H2Om), and low (
Date: 2022
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:13:y:2022:i:1:d:10.1038_s41467-022-32736-9
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DOI: 10.1038/s41467-022-32736-9
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