Centennial to millennial changes in maar-lake deposition during the last 45,000 years in tropical Southern Africa (Lake Masoko, Tanzania)

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dc.contributor.authorGarcina, Yannick
dc.contributor.authorWilliamsona, David
dc.contributor.authorTaieba, Maurice
dc.contributor.authorVincensa, Annie
dc.contributor.authorMathéa, Pierre-Etienne
dc.contributor.authorMajule, Amos
dc.date.accessioned2016-02-22T08:53:19Z
dc.date.available2016-02-22T08:53:19Z
dc.date.issued2006
dc.description.abstractThe Masoko maar (southern Tanzania) provides one of the most continuous Late Quaternary lacustrine sedimentary records from Africa. A detailed chronostratigraphic framework coupled with sedimentological and magnetic measurements allows us construct a 30-year resolution continuous sedimentary sequence covering the last 45,000 years and to address local depositional environment and climate variability in the tropical Southern Africa. Based on present-day observations and measurements, our results indicate that the low-field magnetic susceptibility of the sediment is highly controlled by climate-driven processes (wind-stress and/or lake-level amplitude changes) acting on the titanomagnetite-rich shoreline reservoir. The tephra- and turbidite-free magnetic susceptibility record is strongly modulated by a persistent multi-decadal to centennial variability (∼80 to 200 years), probably linked to the Gleissberg and Suess cycles of solar activity. At lower frequency, the variability of deposition is controlled by the precessional cycle and its harmonics, suggesting a dominant multi-millennial forcing of low-latitude insolation on climatic changes in tropical Southern Africa. Inferred wetter conditions during the Last Glacial Maximum and the Younger Dryas at Masoko (9°S) indicate southward shifts of the Intertropical Convergence Zone associated with the North Atlantic glacial dynamics, and/or contrasted hydrological changes in the Rungwe highlands compared to the neighbouring areas. Finally, former regional transfer function between diatom assemblages and water chemistry suggested drier conditions during the Last Glacial Maximum at Lake Masoko [Barker, P., Williamson, D., Gasse, F., Gibert, E., 2003. Climatic and volcanic forcing revealed in a 50,000-year diatom record from Lake Massoko, Tanzania. Quaternary Research 60, 368–376]. In this context, further climate-proxy data (such as pollen) and hydrobiological studies in small, deep lakes are needed to support our alternative interpretation of the Masoko record.en_US
dc.identifier.citationGarcin, Y; Williamson, D; Taieb, M.; Vincens, A.; Mathé, P-E and Majule, A (2006) Centennial to millennial changes in maar-lake deposition during the last 45,000 years in tropical Southern Africa: Lake Masoko, Tanzania. Elsevier B.V. PALEO. Available at www.elsevier.com/locate.paleoen_US
dc.identifier.other10.1016/j.palaeo.2006.02.002
dc.identifier.urihttp://hdl.handle.net/123456789/477
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectLake Masokoen_US
dc.subjectRungween_US
dc.subjectSouthern Africaen_US
dc.subjectLate Quaternaryen_US
dc.subjectIntertropical Convergence Zoneen_US
dc.subjectPrecessionen_US
dc.subjectSolar cyclesen_US
dc.subjectMagnetic susceptibilityen_US
dc.titleCentennial to millennial changes in maar-lake deposition during the last 45,000 years in tropical Southern Africa (Lake Masoko, Tanzania)en_US
dc.typeJournal Articleen_US
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