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Scratching the surface: a marine sediment provenance record from the continental slope of central Wilkes Land, East Antarctica

Citation

Tooze, S and Halpin, JA and Noble, TL and Chase, Z and O'Brien, PE and Armand, L, Scratching the surface: a marine sediment provenance record from the continental slope of central Wilkes Land, East Antarctica, Geochemistry Geophysics Geosystems, 21, (11) Article e2020GC009156. ISSN 1525-2027 (2020) [Refereed Article]


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Copyright 2020 the authors. Licensed under Creative Commons Attribution 4.0 International (CC BY 4.0) https://creativecommons.org/licenses/by/4.0/

DOI: doi:10.1029/2020GC009156

Abstract

The geology of Wilkes Land, East Antarctica, is masked by kilometers of ice and remains largely unexplored. Defining the sediment provenance adjacent to this hidden region is important for distinguishing the proximal subglacial basement terranes and refining the dynamic regional glaciological history. This study presents a detrital sediment provenance record spanning c. 23.5 ka from the continental slope of central Wilkes Land. Sediment provenance was characterized using U‐Pb geochronology and trace element geochemistry from detrital zircon, titanite and apatite and Pb‐isotopic signatures from detrital feldspar. These data were compared with new feldspar Pb‐isotopic signatures and existing U‐Pb zircon datasets from rare nearby coastal outcrop. A principally igneous source was revealed with dominant age populations between c. 1360‐1100 Ma and c. 1620‐1490 Ma, characteristic of rocks of the proximal Wilkes and Banzare provinces, respectively. Minor detritus was additionally sourced from the proximal Nuyina Province (c. 1450‐1390 Ma). Temporal variation in the climate and ice sheet configuration are likely responsible for subtle downcore changes observed in detrital sediment provenance. High sedimentation rates during the glacial period suggest reworking of continental shelf sediments and downslope transport in debris flows during ice sheet advance. Glacial meltwater fluxes fed largely by the Totten Glacier were responsible for supplying detritus during deglaciation. During interglacials, detritus was derived from a broad coastal region and delivered to the slope via multiple glacial outlets. These results present the first substantial offshore evidence to support recent interpretations that the subglacial crust of central Wilkes Land has a dominantly Mesoproterozoic history.

Item Details

Item Type:Refereed Article
Keywords:geochronology, geochemistry, Wilkes Land, East Antarctica, sediment provenance, subglacial geology
Research Division:Earth Sciences
Research Group:Geology
Research Field:Geochronology
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Understanding climate change
Objective Field:Effects of climate change on Antarctic and sub-Antarctic environments (excl. social impacts)
UTAS Author:Tooze, S (Miss Sian Tooze)
UTAS Author:Halpin, JA (Dr Jacqueline Halpin)
UTAS Author:Noble, TL (Dr Taryn Noble)
UTAS Author:Chase, Z (Professor Zanna Chase)
ID Code:141370
Year Published:2020
Web of Science® Times Cited:3
Deposited By:Oceans and Cryosphere
Deposited On:2020-10-16
Last Modified:2021-04-28
Downloads:2 View Download Statistics

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