Southward shift of the Intertropical Convergence Zone due to Northern Hemisphere cooling at the Oligocene-Miocene boundary SCIE SCOPUS
DC Field | Value | Language |
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dc.contributor.author | Hyeong, Kiseong | - |
dc.contributor.author | Lee, Jongmin | - |
dc.contributor.author | Seo, Inah | - |
dc.contributor.author | Lee, Mi Jung | - |
dc.contributor.author | Yoo, Chan Min | - |
dc.contributor.author | Khim, Boo-Keun | - |
dc.date.accessioned | 2020-04-20T04:40:17Z | - |
dc.date.available | 2020-04-20T04:40:17Z | - |
dc.date.created | 2020-01-28 | - |
dc.date.issued | 2014-08 | - |
dc.identifier.issn | 0091-7613 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/2763 | - |
dc.description.abstract | The Mi-1 glaciation (ca. 23 Ma), which marks the Oligocene-Miocene boundary, was an aberrant cooling event that led to a build-up of the Antarctic ice sheet, which reached the near-modern volume (or greater) from its ephemeral or partial existence. An increase of similar to 1% in the delta O-18 of benthic foraminifera during this interval has been attributed to the development of Antarctic ice sheets and deep-water cooling. Without definitive evidence, Northern Hemisphere (NH) glaciation has not been a material consideration for the delta O-18 increase. Here we investigate the interhemispheric temperature contrast during Mi-1, with the movement of the Intertropical Convergence Zone (ITCZ) at a site (10 degrees 31'N) in the East Pacific (Integrated Ocean Drilling Program Site U1333), to understand NH cooling and the possibility of NH glaciation. The measured Nd-143/Nd-144, Sr-87/Sr-86, and clay mineral compositions of eolian dust fractions indicate unequivocally the deposition of Asian dust during Mi-1, and of Central American and South American dust before and after Mi-1. This is attributed to the southward displacement of the ITCZ over Site U1333 during Mi-1. The ITCZ shifts toward the warmer hemisphere. Thus our results suggest that the cooling during Mi-1 was more significant in the NH than in the Southern Hemisphere, which underwent a sudden expansion of continental ice sheets. Our data call for a forcing mechanism to drive significant NH cooling during this episode. Based on the available data, we propose that the widespread growth of NH ice sheets and/or changes in the production of North Atlantic-origin deep water could be possible causes of the NH cooling at that time. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | GEOLOGICAL SOC AMER, INC | - |
dc.subject | ANTARCTIC ICE-SHEET | - |
dc.subject | CARBON-CYCLE | - |
dc.subject | CLIMATE | - |
dc.subject | SEDIMENT | - |
dc.subject | SEA | - |
dc.subject | VARIABILITY | - |
dc.subject | DUST | - |
dc.title | Southward shift of the Intertropical Convergence Zone due to Northern Hemisphere cooling at the Oligocene-Miocene boundary | - |
dc.type | Article | - |
dc.citation.endPage | 670 | - |
dc.citation.startPage | 667 | - |
dc.citation.title | GEOLOGY | - |
dc.citation.volume | 42 | - |
dc.citation.number | 8 | - |
dc.contributor.alternativeName | 형기성 | - |
dc.contributor.alternativeName | 서인아 | - |
dc.contributor.alternativeName | 유찬민 | - |
dc.identifier.bibliographicCitation | GEOLOGY, v.42, no.8, pp.667 - 670 | - |
dc.identifier.doi | 10.1130/G35664.1 | - |
dc.identifier.scopusid | 2-s2.0-84905157307 | - |
dc.identifier.wosid | 000339961600007 | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.subject.keywordPlus | ANTARCTIC ICE-SHEET | - |
dc.subject.keywordPlus | CARBON-CYCLE | - |
dc.subject.keywordPlus | CLIMATE | - |
dc.subject.keywordPlus | SEDIMENT | - |
dc.subject.keywordPlus | SEA | - |
dc.subject.keywordPlus | VARIABILITY | - |
dc.subject.keywordPlus | DUST | - |
dc.relation.journalWebOfScienceCategory | Geology | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Geology | - |