High-resolution ∼55 ka paleomagnetic record of Biển Hồ maar lake sediment from Vietnam in relation to detailed 14C and 137Cs geochronologies

dc.contributor.authorOjala Antti E.K.
dc.contributor.authorNguyễn-Văn Huong
dc.contributor.authorUnkel Ingmar
dc.contributor.authorNguyễn-Thùy Duong
dc.contributor.authorNguyễn-Đình Thyn
dc.contributor.authorĐỗ-Trọng Quoc
dc.contributor.authorSun Chunqing
dc.contributor.authorSauer Peter E.
dc.contributor.authorSchimmelmann Arndt
dc.contributor.organizationfi=geologia|en=Geology |
dc.contributor.organization-code1.2.246.10.2458963.20.72020864681
dc.converis.publication-id180244026
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/180244026
dc.date.accessioned2025-08-27T23:04:00Z
dc.date.available2025-08-27T23:04:00Z
dc.description.abstract<p>Vietnam's Central Highlands in Pleiku feature numerous volcanic craters (i.e. maars) formed over 0.2 Ma ago that contain continuous high-resolution lacustrine sediment records extending from the Late Pleistocene through the Holocene. Their evolution and sedimentary proxies are potentially powerful archives for interpretation of East-Asian monsoon variability across Vietnam, as well as for local to regional changes in landcover. The focus of this study is to develop a reliable chronology for the Biển Hồ 25-m-long lake sediment sequence in Vietnam's Central Highlands. We present a combined sediment chronology extending back to 55 ka cal BP that is based on 137Cs surface sediment chronology, paleomagnetic dating, and 47 14C dates distributed evenly throughout the sequence. Based on sedimentary facies analysis and a smooth age-depth model based on 137Cs and 14C data, we infer a long-term stable rate of sedimentation in Biển Hồ lake without unconformities or erosional hiatuses, except for the uppermost section (ca. 100 years) where human activities increase the rate of sedimentation significantly. The Biển Hồ sequence thus provides a complete and uninterrupted record of the lake's depositional history. The present contribution is a geochronologic opening salvo for future contributions from Biển Hồ lake featuring multi-disciplinary evidence for longer-term paleoclimate and environmental changes</p>
dc.identifier.jour-issn1871-1014
dc.identifier.olddbid203322
dc.identifier.oldhandle10024/186349
dc.identifier.urihttps://www.utupub.fi/handle/11111/32870
dc.identifier.urlhttps://doi.org/10.1016/j.quageo.2023.101443
dc.identifier.urnURN:NBN:fi-fe2025082786040
dc.language.isoen
dc.okm.affiliatedauthorOjala, Antti
dc.okm.discipline1171 Geosciencesen_GB
dc.okm.discipline1171 Geotieteetfi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherElsevier B.V.
dc.publisher.countryNetherlandsen_GB
dc.publisher.countryAlankomaatfi_FI
dc.publisher.country-codeNL
dc.relation.articlenumber101443
dc.relation.doi10.1016/j.quageo.2023.101443
dc.relation.ispartofjournalQuaternary Geochronology
dc.relation.volume76
dc.source.identifierhttps://www.utupub.fi/handle/10024/186349
dc.titleHigh-resolution ∼55 ka paleomagnetic record of Biển Hồ maar lake sediment from Vietnam in relation to detailed 14C and 137Cs geochronologies
dc.year.issued2023

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