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Ken Ikehara

Researcher at National Institute of Advanced Industrial Science and Technology

Publications -  198
Citations -  3735

Ken Ikehara is an academic researcher from National Institute of Advanced Industrial Science and Technology. The author has contributed to research in topics: Trench & Holocene. The author has an hindex of 30, co-authored 189 publications receiving 3158 citations.

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Transgressive and highstand systems tracts and post-glacial transgression, the East China Sea

TL;DR: In this paper, the Late Pleistocene-Holocene depositional sequence on the shelf in the East China Sea (ECS) is interpreted on the basis of the analyses of four sediment cores and high-resolution seismic reflection sub-bottom profiler records along a NE-SW across-shelf transect.
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Abrupt ventilation changes in the Japan Sea over the last 30 ky: Evidence from deep-dwelling radiolarians

TL;DR: In this article, the modern depth distribution of radiolarian species and their relation to water masses was elucidated from the study of plankton tows and surface sediments, and seven sediment cores located in water depths ranging from 807 to 3613 m, indicating changes in waterventilation strength in this marginal sea.
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Rock-magnetic changes with reduction diagenesis in Japan Sea sediments and preservation of geomagnetic secular variation in inclination during the last 30,000 years

TL;DR: A rock-magnetic and paleomagnetic study was conducted on a sediment core of about 4.4 m long taken from the northeastern part of the Japan Sea, which was dated by nineteen radiocarbon (14C) ages.
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Orbital-scale stratigraphy and high-resolution analysis of biogenic components and deep-water oxygenation conditions in the Japan Sea during the last 640 kyr

TL;DR: In this article, the authors constructed an orbital-scale stratigraphy of the sediments covering the last 640kyr by comparing the SPECMAP ∂18O curve and the ∂ 18O curve of planktonic foraminifera (∂18Opf) in the Japan Sea together with the combination zones of dominant planktonics foraminifa species.