T
Tomohisa Irino
Researcher at Hokkaido University
Publications - 90
Citations - 2369
Tomohisa Irino is an academic researcher from Hokkaido University. The author has contributed to research in topics: Glacial period & Holocene. The author has an hindex of 24, co-authored 84 publications receiving 1969 citations. Previous affiliations of Tomohisa Irino include University of Tokyo.
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Land‐ocean linkages over orbital and millennial timescales recorded in Late Quaternary sediments of the Japan Sea
TL;DR: In this paper, high-resolution analyses of the sediments from Ocean Drilling Program site 797 reveal that deposition of the meter-scale alternations reflect variations in paleoceanographic conditions which were closely associated with glacio-eustatic sea level changes through the modulation of the volume and character of the influx to the sea through the Tsushima Strait.
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Orbital- and millennial-scale variations in Asian dust transport path to the Japan Sea
TL;DR: In this paper, the authors examined grain size, flux, and provenance of aeolian dust in the sediments of the Japan Sea in order to understand the spatial variability of Asian monsoon.
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The 1500-year climate oscillation in the midlatitude North Pacific during the Holocene
Dai Isono,Masanobu Yamamoto,Tomohisa Irino,Tadamichi Oba,Masafumi Murayama,Toshio Nakamura,Hodaka Kawahata +6 more
TL;DR: In this article, a multidecade resolution record of alkenone sea surface temperature (SST) in the northwestern Pacific off central Japan during the Holocene was generated, and the SST record showed centennial and millennial variability with an amplitude of ~1 °C throughout the entire Holocene.
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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.
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Paleoceanographic change off central Japan since the last 144,000 years based on high-resolution oxygen and carbon isotope records
TL;DR: Oda et al. as mentioned in this paper conducted high-resolution oxygen and carbon isotope analysis of both benthic and planktonic foraminifera from an ocean core off central Japan.