2020
DOI: 10.1007/978-3-030-40659-2_3
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Assessing Mid-pleistocene to Holocene Sea-Ice Extent and Carbonate Compensation Depth Fluctuations in the Japan Sea: A Multiproxy Approach

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Cited by 5 publications
(17 citation statements)
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“…Glacial‐interglacial seas level changes additionally controlled the intensity of the KC intensity and the Tsushima warm current into the Japan Sea (Das et al., 2018, 2020; Gallagher et al., 2018; Saavedra‐Pellitero et al., 2019). Spectral analysis of the oxic genus Quinqueloculina (%), suboxic genus Bulimina (%), dysoxic genus Globobulimina (%), and productivity indicator δ 13 C pf additionally reveals a prominent ∼23 kyr cyclicity, likely related to KC‐driven productivity changes in the ECS.…”
Section: Discussionmentioning
confidence: 99%
“…Glacial‐interglacial seas level changes additionally controlled the intensity of the KC intensity and the Tsushima warm current into the Japan Sea (Das et al., 2018, 2020; Gallagher et al., 2018; Saavedra‐Pellitero et al., 2019). Spectral analysis of the oxic genus Quinqueloculina (%), suboxic genus Bulimina (%), dysoxic genus Globobulimina (%), and productivity indicator δ 13 C pf additionally reveals a prominent ∼23 kyr cyclicity, likely related to KC‐driven productivity changes in the ECS.…”
Section: Discussionmentioning
confidence: 99%
“…346) Site U1423 in the Japan Sea is marked by the red filled circle. Red arrows mark surface current directions, and black arrows mark EAWM and Westerly wind directions, following Das et al (2018Das et al ( , 2020. This map has been prepared using Ocean Data View (Schlitzer, 2021).…”
Section: Grain-size Analysismentioning
confidence: 99%
“…Periodic fluctuations in the depositional environment were vigorous during this period. The permanent sea ice condition in the northern Japan Sea (Das et al, 2020) continued between 780 and 450 ka, marked by an increase in sand (%), which may be sand size IRD and decrease in silt (%). The calm environment of deposition is characterized by the peak of clay (%) and low-energy condition EM2, except for a brief period during MIS 14 (Figures S1, 5).…”
Section: After Middle Pleistocene Transitionmentioning
confidence: 99%
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