Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12136/460
Item metadata
Title: Age models for long lacustrine sediment records using multiple dating approaches – An example from Lake Bosumtwi, Ghana
Authors: Shanahan, Timothy M.
Peck, John A.
McKay, Nicholas
Heil, Clifford W.
King, John W.
Forman, Steven L.
Hoffmann, Dirk
Richards, David A.
Overpeck, Jonathan T.
Scholz, Christopher
Keywords: Lake Bosumtwi;West Africa;Paleoclimate;Lake;Chronology
Issue Date: Feb-2013
Publisher: Elsevier
Citation: Quaternary Geochronology, 2013, 15, 47-60
Abstract: The 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.
URI: http://hdl.handle.net/20.500.12136/460
ISSN: 1871-1014
1878-0350
DOI: 10.1016/j.quageo.2012.12.001
metadata.dc.relation.publisherversion: https://doi.org/10.1016/j.quageo.2012.12.001
Type: Article
Appears in Collections:Geocronología y Geología



This item is licensed under a Creative Commons License Creative Commons