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  4. Productivity History of the Central Okhotsk Sea and Northeast Russia During the Mid‐Pleistocene Transition
 
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Productivity History of the Central Okhotsk Sea and Northeast Russia During the Mid‐Pleistocene Transition

Journal
Paleoceanography and Paleoclimatology
Journal Volume
40
Journal Issue
12
ISSN
2572-4517
2572-4525
Date Issued
2025-11-25
Author(s)
Lo, Li  
Chen, Wei‐Zhu
Lattaud, Julie
Tsai, Yi‐Hsueh
Belt, Simon T.
Smik, Lukas
Wan, Yuen Tung Kiki
DOI
10.1029/2024pa005092
URI
https://www.scopus.com/pages/publications/105023121034
https://scholars.lib.ntu.edu.tw/handle/123456789/734934
Abstract
Biological productivity, shaped by climate and environmental factors, is critical to climate feedback mechanisms and the global carbon cycle. This study investigates the measurement of six phytosterols (β-sitosterol, stigmasterol, campesterol, dinosterol, epi-brassicasterol, and 24-methylene cholesterol) from core MD01-2414 in the central Okhotsk Sea, covering the past 1.5 million years (Ma). These sterols serve as proxies for terrestrial and marine productivity in the central Okhotsk Sea and northeast Siberia. Sterol concentrations reflect global glacial/interglacial cycles between 1.2 and 0.6 Ma, with higher and lower values during interglacial and glacials intervals, respectively. X-ray fluorescence (Ba/Ti) and total organic carbon/total nitrogen (TOC/TN) ratios indicate shifts in marine and terrestrial sources, confirming biological productivity as a key driver of sterol deposition. Sterol fluxes, combined with sea surface temperature records from the northwest Pacific and sea ice proxies from the Bering Sea, reveal an extreme cold interglacial (Marine Isotope Stage, MIS 23) and prolonged glacial conditions during MIS 22, which stressed both terrestrial and marine ecosystems. Increased sea ice expansion during this period likely fostered North Pacific Intermediate Water formation, reducing upwelling and CO2 exchange between bottom waters and the atmosphere. Integration of sterol data with regional records, including pollen, temperature, and sedimentary facies from Lake El'gygytgyn, highlights a warming event at the onset of MIS 32, peaking in late MIS 32. This warming precedes the “super-interglacial” MIS 31 and coincides with maxima in boreal and austral summer insolation, underscoring its significance in regional climate evolution.
Subjects
Mid-Pleistocene Transition
Okhotsk Sea
sterol
super-interglacial periods
Publisher
American Geophysical Union (AGU)
Type
journal article

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