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Palaeoceanography of the Japan Sea Across the Mid‐Pleistocene Transition: Insights From IODP Exp. 346, Site U1427

Henderson, Andrew C. G.; Felder, Sonja; Sagawa, Takuya; Greaves, Mervyn; Leng, Melanie J.; Ikehara, Ken; Kimoto, Katsunori; Hasegawa, Siro; Wagner, Thomas; Henderson, Andrew C.G.

Palaeoceanography of the Japan Sea Across the Mid‐Pleistocene Transition: Insights From IODP Exp. 346, Site U1427 Thumbnail


Authors

Andrew C. G. Henderson

Sonja Felder

Takuya Sagawa

Mervyn Greaves

Ken Ikehara

Katsunori Kimoto

Siro Hasegawa

Thomas Wagner

Andrew C.G. Henderson



Abstract

Large-scale atmospheric circulation patterns, such as the East Asian monsoon, have been proposed as possible feedbacks of the mid-Pleistocene transition (MPT). Marine sediments of the Japan Sea (JS) record variations in the East Asian monsoon over long timescales and may be crucial for understanding of the MPT. To interpret these sediments correctly an understanding of the JS palaeoceanography is necessary. So far, the JS palaeoceanography has been extrapolated across the MPT from studies of the most recent glacial-interglacial cycles. These suggest a good connection and unrestricted water-mass exchange with the open ocean during interglacial sea-level highstands, while during glacial sea-level lowstands the JS is nearly isolated. Glacial isolation often results in poor carbonate preservation and unusually low oxygen isotope (δ18O) ratios from low-saline/low-δ18O waters accumulating in the basin. Using the sediments of Integrated Ocean Drilling Program (IODP) Site U1427, a shallow-water site in the southern JS, we present a continuous foraminiferal δ18O record encompassing the MPT. This record shows the JS-typical low glacial δ18O values in the late phase of the MPT, across Marine Isotope Stages (MIS) 24-17, while earlier MPT glacials, across MIS 39-25, are characterized by high δ18O values. We propose that high glacial δ18O values are the result of an improved connection between the shallow, southern JS and adjacent ocean during early MPT glacials. The impact of this palaeoceanographic mode, if continued to deep-water sites, would make the interpretation of dark/light sediment layers as glacial/interglacial deposits uncertain.

Citation

Henderson, A. C. G., Felder, S., Sagawa, T., Greaves, M., Leng, M. J., Ikehara, K., Kimoto, K., Hasegawa, S., Wagner, T., & Henderson, A. C. (2022). Palaeoceanography of the Japan Sea Across the Mid‐Pleistocene Transition: Insights From IODP Exp. 346, Site U1427. Paleoceanography and Paleoclimatology, 37(1), Article e2021PA004236. https://doi.org/10.1029/2021pa004236

Journal Article Type Article
Acceptance Date Nov 9, 2021
Online Publication Date Dec 7, 2021
Publication Date 2022-01
Deposit Date Dec 13, 2021
Publicly Available Date Jan 28, 2022
Journal Paleoceanography and Paleoclimatology
Print ISSN 2572-4517
Electronic ISSN 2572-4525
Peer Reviewed Peer Reviewed
Volume 37
Issue 1
Article Number e2021PA004236
DOI https://doi.org/10.1029/2021pa004236
Keywords Paleontology; Atmospheric Science; Oceanography
Public URL https://nottingham-repository.worktribe.com/output/7014604
Publisher URL https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021PA004236

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