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  4. Dating the Northwest Shelf of Australia Since the Pliocene
 
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Dating the Northwest Shelf of Australia Since the Pliocene

Journal
Geochemistry, Geophysics, Geosystems
Journal Volume
22
Journal Issue
3
Date Issued
2021
Author(s)
JEROEN GROENEVELD  
De Vleeschouwer D
McCaffrey J.C
Gallagher S.J.
DOI
10.1029/2020GC009418
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85103361012&doi=10.1029%2f2020GC009418&partnerID=40&md5=a47fc0e7af9d57894d57718dca8595c0
https://scholars.lib.ntu.edu.tw/handle/123456789/624737
Abstract
Accurate dating of marine sediments is essential to reconstruct past changes in oceanography and climate. Benthic foraminiferal oxygen isotope series from such sediments record long-term changes in global ice volume and deep-water temperature. They are commonly used in the Plio-Pleistocene to correlate deep ocean records and to construct age models. However, continental margin settings often display much higher sedimentation rates due to variations in regional depositional setting and local input of sediment. Here, it is necessary to create a regional multi-site framework to allow precise dating of strata. We create such a high-resolution regional framework to determine the ages of events for the Northwest Shelf (NWS) of Australia, which was cored by International Ocean Discovery Program (IODP) Expedition 356. We employ benthic foraminiferal oxygen and carbon isotopes to construct an astronomically-tuned age model for IODP Site U1463 (5.16–1.69 Ma). The age model is applied to the IODP Site U1463 downhole-logging natural gamma radiation (NGR) depth-series, which was then correlated to NGR depth-series of several IODP sites and industry wells in the area. This approach allows assigning ages to regional seismic reflectors and the timing of key climate-related siliciclastic phases in a predominantly carbonate-rich sequence, like the late Miocene-Pliocene Bare Formation. This age model is also used to chronologically calibrate planktonic foraminiferal biostratigraphic datums showing that the Indonesian Throughflow (ITF) had shoaled enough in the early Pliocene to act as biogeographical barrier between the Pacific and Indian Ocean. © 2021. The Authors.
Subjects
benthic foraminiferal isotopes; downhole wireline logging; NW-Australia; planktonic foraminiferal biostratigraphy; seismic network
Other Subjects
Isotopes; Oxygen; Submarine geology; Continental margin; Deep water temperature; Depositional setting; Global ice volume; Indonesian throughflow; Plio-pleistocene; Sedimentation rates; Seismic reflectors; Sediments; benthic foraminifera; benthos; biostratigraphy; logging (geophysics); paleoceanography; paleoclimate; planktonic foraminifera; Pliocene; Pliocene-Pleistocene boundary; reconstruction; seismic data; Indian Ocean; Northwest Australian Shelf
Type
journal article

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