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dc.contributor.authorHyodo, Masayuki
dc.contributor.authorBradák, Balázs
dc.contributor.authorOkada, Makoto
dc.contributor.authorKatoh, Shigehiro
dc.contributor.authorKitaba, Ikuko
dc.contributor.authorDettman, David L.
dc.contributor.authorHayashi, Hiroki
dc.contributor.authorKumazawa, Koyo
dc.contributor.authorHirose, Kotaro
dc.contributor.authorKazaoka, Osamu
dc.contributor.authorShikoku, Kizuku
dc.contributor.authorKitamura, Akihisa
dc.date.accessioned2017-10-02T23:15:21Z
dc.date.available2017-10-02T23:15:21Z
dc.date.issued2017-08-30
dc.identifier.citationMillennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene 2017, 7 (1) Scientific Reportsen
dc.identifier.issn2045-2322
dc.identifier.doi10.1038/s41598-017-10552-2
dc.identifier.urihttp://hdl.handle.net/10150/625757
dc.description.abstractSuborbital-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 midlatitude 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.
dc.description.sponsorshipJapan Society for the Promotion of Science (JSPS) [22340154, 20654043]; Mitsubishi Foundation; JAMSTEC [13A001, 14A023, 16A002]; JSPSen
dc.language.isoenen
dc.publisherNATURE PUBLISHING GROUPen
dc.relation.urlhttp://www.nature.com/articles/s41598-017-10552-2en
dc.rights© The Author(s) 2017. Open Access This article is licensed under a Creative Commons Attribution 4.0 International License.en
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleMillennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistoceneen
dc.typeArticleen
dc.contributor.departmentUniv Arizona, Dept Geoscien
dc.identifier.journalScientific Reportsen
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en
dc.eprint.versionFinal published versionen
refterms.dateFOA2018-09-11T23:25:59Z
html.description.abstractSuborbital-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 midlatitude 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.


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© The Author(s) 2017. Open Access This article is licensed under a Creative Commons Attribution 4.0 International License.
Except where otherwise noted, this item's license is described as © The Author(s) 2017. Open Access This article is licensed under a Creative Commons Attribution 4.0 International License.