Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12136/460
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dc.contributor.authorShanahan, Timothy M.-
dc.contributor.authorPeck, John A.-
dc.contributor.authorMcKay, Nicholas-
dc.contributor.authorHeil, Clifford W.-
dc.contributor.authorKing, John W.-
dc.contributor.authorForman, Steven L.-
dc.contributor.authorHoffmann, Dirk-
dc.contributor.authorRichards, David A.-
dc.contributor.authorOverpeck, Jonathan T.-
dc.contributor.authorScholz, Christopher-
dc.date.accessioned2018-06-
dc.date.accessioned2018-06-13T14:52:51Z-
dc.date.issued2013-02-
dc.identifier.citationQuaternary Geochronology, 2013, 15, 47-60es_ES
dc.identifier.issn1871-1014-
dc.identifier.issn1878-0350-
dc.identifier.urihttp://hdl.handle.net/20.500.12136/460-
dc.description.abstractThe continuous 300-m long drill cores obtained from Lake Bosumtwi, Ghana represent one of the longest, continuous lacustrine sequences obtained from an extant lake, and contain an unprecedented record of late Quaternary climate change in West Africa. However, one of the main challenges associated with generating long paleoclimate time series from terrestrial records such as this is the development of accurate age-depth relationships because unlike marine records, lacustrine sequences cannot be tuned to global ice volume records via δ18O stratigraphy. The Lake Bosumtwi record thus offers an excellent case study for examining the potential and the challenges associated with different geochronological techniques in lacustrine systems. In the present study, we use a combination of radiocarbon, optically stimulated luminescence and U-series dating and paleomagnetic excursions to generate a chronology for the upper ca. 150 ka of sedimentation at Lake Bosumtwi and employ a Bayesian approach to generate a continuous age-depth relationship. The resultant chronology is then used to test the effectiveness of tuning of an environmental magnetic proxy for dust against a well-dated record of high latitude dust. Our approach highlights the advantages of using multiple dating approaches, and the dangers of relying on too few age constraints when dating long sedimentary sequences. However, the excellent agreement between the different approaches over most of the record suggest that well-constrained age-depth models for long sedimentary sequences can be produced using this combination of approaches. Furthermore, our data provide support for extending the chronology beyond the limit of radiocarbon, U-series and OSL in the future using paleomagnetic excursions/reversals and tuning against well-dated high latitude paleoclimate records.es_ES
dc.description.sponsorshipThe research was funded in part by National Science Foundation grants NSF: EAR0602355, EAR0601998, ATM0401908, ATM0214525, and ATM0096232.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectLake Bosumtwies_ES
dc.subjectWest Africaes_ES
dc.subjectPaleoclimatees_ES
dc.subjectLakees_ES
dc.subjectChronologyes_ES
dc.titleAge models for long lacustrine sediment records using multiple dating approaches – An example from Lake Bosumtwi, Ghanaes_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.quageo.2012.12.001-
dc.relation.publisherversionhttps://doi.org/10.1016/j.quageo.2012.12.001es_ES
dc.date.available2018-06-13T14:52:51Z-
Appears in Collections:Geocronología y Geología



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