Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene

Masayuki Hyodo*, Balázs Bradák, Makoto Okada, Shigehiro Katoh, Ikuko Kitaba, David L. Dettman, Hiroki Hayashi, Koyo Kumazawa, Kotaro Hirose, Osamu Kazaoka, Kizuku Shikoku, Akihisa Kitamura

*この研究の対応する著者

研究成果: Article査読

10 被引用数 (Scopus)

抄録

Suborbital-scale climate variations, possibly caused by solar activity, are observed in the Holocene and last-glacial climates. Recently published bicentennial-resolution paleoceanic environmental records reveal millennial-scale high-amplitude oscillations postdating the last geomagnetic reversal in the Marine Isotope Stage (MIS) 19 interglacial. These oscillations, together with decoupling of post-reversal warming from maximum sea-level highstand in mid-latitudes, are key features for understanding the climate system of MIS 19 and the following Middle Pleistocene. It is unclear whether the oscillations are synchronous, or have the same driver as Holocene cycles. Here we present a high resolution record of western North Pacific submarine anoxia and sea surface bioproductivity from the Chiba Section, central Japan. The record reveals many oxic events in MIS 19, coincident with cold intervals, or with combined cold and sea-level fall events. This allows detailed correlations with paleoceanic records from the mid-latitude North Atlantic and Osaka Bay, southwest Japan. We find that the millennial-scale oscillations are synchronous between East and West hemispheres. In addition, during the two warmest intervals, bioproductivity follows the same pattern of change modulated by bicentennial cycles that are possibly related to solar activity.

本文言語English
論文番号10036
ジャーナルScientific reports
7
1
DOI
出版ステータスPublished - 2017 12 1
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