Tephrochronology and Provenance of an Early Pleistocene (Calabrian) Tephra From IODP Expedition 374 Site U1524, Ross Sea (Antarctica)

AbstractWe present a full characterization of a 20 cmâ€thick tephra layer found intercalated in the marine sediments recovered at Site U1524 during International Ocean Discovery Program (IODP) Expedition 374, in the Ross Sea, Antarctica. Tephra bedforms, mineral paragenesis, and major†and traceâ€e...

Full description

Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Di Roberto, A., Scateni, B., Di Vincenzo, G., Petrelli, M., Fisauli, G., Barker, S. J., Del Carlo, P., Colleoni, F., Kulhanek, D. K., McKay, R., De Santis, L., The IODP Expedition 374 Scientific Party
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Geochemistry and Petrology
Geophysics
Antarc*
Antarctica
Marie Byrd Land
Ross Sea
West Antarctica
Online Access:https://www.openaccessrepository.it/record/210074
https://doi.org/10.1029/2021gc009739
Description
Summary:AbstractWe present a full characterization of a 20 cmâ€thick tephra layer found intercalated in the marine sediments recovered at Site U1524 during International Ocean Discovery Program (IODP) Expedition 374, in the Ross Sea, Antarctica. Tephra bedforms, mineral paragenesis, and major†and traceâ€element composition on individual glass shards were investigated and the tephra age was constrained by 40Arâ€39Ar on sanidine crystals. The 40Arâ€39Ar data indicate that sanidine grains are variably contaminated by excess Ar, with the best age estimate of 1.282 ± 0.012 Ma, based on both singleâ€grain total fusion analyses and stepâ€heating experiments on multiâ€grain aliquots. The tephra is characterized by a very homogeneous rhyolitic composition and a peculiar mineral assemblage, dominated by sanidine, quartz, and minor aenigmatite and arfvedsoniteâ€riebeckite amphiboles. The tephra from Site U1524 compositionally matches with a ca. 1.3 Ma, rhyolitic pumice fall deposit on the rim of the Chang Peak volcano summit caldera, in the Marie Byrd Land, located ca. 1,300 km from Site U1524. This contribution offers important volcanological data on the eruptive history of Chang Peak volcano and adds a new tephrochronologic marker for the dating, correlation, and synchronization of marine and continental early Pleistocene records of West Antarctica.

Similar Items