Publication Date:
2021-07-21
Description:
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.
Description:
Plain Language Summary:
Determining the age of marine sediments is essential to reconstruct past changes in oceanography and climate. The oxygen isotopes of benthic foraminifera record long‐term changes in global ice volume and deep‐water temperature, and are commonly used to construct age models. However, continental margin settings often display much higher sedimentation rates due to regional input by rivers. Here, it is necessary to create a regional framework to allow precise dating of strata. We created such a framework for the Northwest Shelf (NWS) of Australia, which was cored by IODP Expedition 356. We used oxygen and carbon isotopes in benthic foraminifera to construct an astronomically‐tuned age model for IODP Site U1463. The natural gamma radiation (NGR) variations for IODP Site U1463 were then correlated to those of other IODP sites and industry wells in the area. The IODP Site U1463 age‐depth model provides a reference for other archives on the NWS allowing to assign ages to regional seismic reflectors and the timing of sediment input. This age model is also used to determine first and last occurrences of foraminiferal species showing that the Indonesian Throughflow (ITF) blocked the migration of foraminifera from the Pacific to the Indian Ocean after 5 Ma.
Description:
Key Points:
Independent, orbitally tuned age model for IODP Site U1463
Correlation of natural gamma radiation and seismic profiling allow a consistent age model for the shelf of northwest Australia
Independent age model allows updating planktonic foraminiferal biostratigraphy for the Plio‐Pleistocene
Description:
DAAD | German Academic Exchange Service
Description:
Deutsche Forschungsgemeinschaft
Description:
Australian IODP office and the ARC Basins Genesis Hub
Keywords:
559
;
563
;
benthic foraminiferal isotopes
;
downhole wireline logging
;
NW‐Australia
;
planktonic foraminiferal biostratigraphy
;
seismic network
Type:
article
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