Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene
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...
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Online Access: | http://hdl.handle.net/10150/625757 https://doi.org/10.1038/s41598-017-10552-2 |
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ftunivarizona:oai:repository.arizona.edu:10150/625757 2023-05-15T17:34:30+02:00 Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene Hyodo, Masayuki Bradák, Balázs Okada, Makoto Katoh, Shigehiro Kitaba, Ikuko Dettman, David L. Hayashi, Hiroki Kumazawa, Koyo Hirose, Kotaro Kazaoka, Osamu Shikoku, Kizuku Kitamura, Akihisa Univ Arizona, Dept Geosci 2017-08-30 http://hdl.handle.net/10150/625757 https://doi.org/10.1038/s41598-017-10552-2 en eng NATURE PUBLISHING GROUP http://www.nature.com/articles/s41598-017-10552-2 Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene 2017, 7 (1) Scientific Reports 2045-2322 doi:10.1038/s41598-017-10552-2 http://hdl.handle.net/10150/625757 Scientific Reports © The Author(s) 2017. Open Access This article is licensed under a Creative Commons Attribution 4.0 International License. CC-BY Article 2017 ftunivarizona https://doi.org/10.1038/s41598-017-10552-2 2020-06-14T08:15:53Z 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 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. Japan Society for the Promotion of Science (JSPS) [22340154, 20654043]; Mitsubishi Foundation; JAMSTEC [13A001, 14A023, 16A002]; JSPS This 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. Article in Journal/Newspaper North Atlantic The University of Arizona: UA Campus Repository Pacific Scientific Reports 7 1 |
institution |
Open Polar |
collection |
The University of Arizona: UA Campus Repository |
op_collection_id |
ftunivarizona |
language |
English |
description |
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 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. Japan Society for the Promotion of Science (JSPS) [22340154, 20654043]; Mitsubishi Foundation; JAMSTEC [13A001, 14A023, 16A002]; JSPS This 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. |
author2 |
Univ Arizona, Dept Geosci |
format |
Article in Journal/Newspaper |
author |
Hyodo, Masayuki Bradák, Balázs Okada, Makoto Katoh, Shigehiro Kitaba, Ikuko Dettman, David L. Hayashi, Hiroki Kumazawa, Koyo Hirose, Kotaro Kazaoka, Osamu Shikoku, Kizuku Kitamura, Akihisa |
spellingShingle |
Hyodo, Masayuki Bradák, Balázs Okada, Makoto Katoh, Shigehiro Kitaba, Ikuko Dettman, David L. Hayashi, Hiroki Kumazawa, Koyo Hirose, Kotaro Kazaoka, Osamu Shikoku, Kizuku Kitamura, Akihisa Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene |
author_facet |
Hyodo, Masayuki Bradák, Balázs Okada, Makoto Katoh, Shigehiro Kitaba, Ikuko Dettman, David L. Hayashi, Hiroki Kumazawa, Koyo Hirose, Kotaro Kazaoka, Osamu Shikoku, Kizuku Kitamura, Akihisa |
author_sort |
Hyodo, Masayuki |
title |
Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene |
title_short |
Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene |
title_full |
Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene |
title_fullStr |
Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene |
title_full_unstemmed |
Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene |
title_sort |
millennial-scale northern hemisphere atlantic-pacific climate teleconnections in the earliest middle pleistocene |
publisher |
NATURE PUBLISHING GROUP |
publishDate |
2017 |
url |
http://hdl.handle.net/10150/625757 https://doi.org/10.1038/s41598-017-10552-2 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
http://www.nature.com/articles/s41598-017-10552-2 Millennial-scale northern Hemisphere Atlantic-Pacific climate teleconnections in the earliest Middle Pleistocene 2017, 7 (1) Scientific Reports 2045-2322 doi:10.1038/s41598-017-10552-2 http://hdl.handle.net/10150/625757 Scientific Reports |
op_rights |
© The Author(s) 2017. Open Access This article is licensed under a Creative Commons Attribution 4.0 International License. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41598-017-10552-2 |
container_title |
Scientific Reports |
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7 |
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1 |
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1766133353892806656 |