Insolation-paced sea level and sediment flux during the early Pleistocene in Southeast Asia
dc.bibliographicCitation.firstPage | 16707 | |
dc.bibliographicCitation.journalTitle | Scientific reports | eng |
dc.bibliographicCitation.volume | 11 | |
dc.contributor.author | Vaucher, Romain | |
dc.contributor.author | Dashtgard, Shahin E. | |
dc.contributor.author | Horng, Chorng-Shern | |
dc.contributor.author | Zeeden, Christian | |
dc.contributor.author | Dillinger, Antoine | |
dc.contributor.author | Pan, Yu-Yen | |
dc.contributor.author | Setiaji, Romy A. | |
dc.contributor.author | Chi, Wen-Rong | |
dc.contributor.author | Löwemark, Ludvig | |
dc.date.accessioned | 2023-03-30T05:20:38Z | |
dc.date.available | 2023-03-30T05:20:38Z | |
dc.date.issued | 2021 | |
dc.description.abstract | Global marine archives from the early Pleistocene indicate that glacial-interglacial cycles, and their corresponding sea-level cycles, have predominantly a periodicity of ~ 41 kyrs driven by Earth’s obliquity. Here, we present a clastic shallow-marine record from the early Pleistocene in Southeast Asia (Cholan Formation, Taiwan). The studied strata comprise stacked cyclic successions deposited in offshore to nearshore environments in the paleo-Taiwan Strait. The stratigraphy was compared to both a δ18O isotope record of benthic foraminifera and orbital parameters driving insolation at the time of deposition. Analyses indicate a strong correlation between depositional cycles and Northern Hemisphere summer insolation, which is precession-dominated with an obliquity component. Our results represent geological evidence of precession-dominated sea-level fluctuations during the early Pleistocene, independent of a global ice-volume proxy. Preservation of this signal is possible due to the high-accommodation creation and high-sedimentation rate in the basin enhancing the completeness of the stratigraphic record. | eng |
dc.description.version | publishedVersion | eng |
dc.identifier.uri | https://oa.tib.eu/renate/handle/123456789/11807 | |
dc.identifier.uri | http://dx.doi.org/10.34657/10840 | |
dc.language.iso | eng | |
dc.publisher | [London] : Macmillan Publishers Limited, part of Springer Nature | |
dc.relation.doi | https://doi.org/10.1038/s41598-021-96372-x | |
dc.relation.essn | 2045-2322 | |
dc.rights.license | CC BY 4.0 Unported | |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0 | |
dc.subject.ddc | 500 | |
dc.subject.ddc | 600 | |
dc.subject.other | foreland basin | eng |
dc.subject.other | Western Taiwan | eng |
dc.subject.other | monsoon variability | eng |
dc.subject.other | mountainous river | eng |
dc.subject.other | Typhoon Mindulle | eng |
dc.title | Insolation-paced sea level and sediment flux during the early Pleistocene in Southeast Asia | eng |
dc.type | Article | eng |
dc.type | Text | eng |
tib.accessRights | openAccess | |
wgl.contributor | LIAG | |
wgl.subject | Geowissenschaften | ger |
wgl.type | Zeitschriftenartikel | ger |
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