Middle to late Holocene initiation of the annual flood pulse in Tonle Sap Lake, Cambodia

Mary Beth Day, David A. Hodell, Mark Brenner, Jason H. Curtis, George D. Kamenov, Thomas P. Guilderson, Larry C Peterson, William F. Kenney, Alan L. Kolata

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Tonle Sap Lake, Cambodia, possesses one of the most productive inland fisheries in the world and is a vital natural resource for the country. The lake is connected to the Mekong River via the Tonle Sap River. Flow in the Tonle Sap River reverses seasonally, with water exiting the lake in the dry season and entering the lake during the summer monsoon. This flood pulse drives the lake's biological productivity. We used Sr, Nd, and Pb isotopes and elemental concentrations in lake sediment cores to track changes in the provenance of deposits in Tonle Sap Lake. We sought to determine when the lake first began to receive water and sediment input via the Mekong River, which initiated flood pulse processes. The transition from a non-pulsing lake to the Mekong-connected system is marked by shifts to values of 87Sr/86Sr, εNd, and 207Pb/204Pb that are characteristic of Mekong River sediments. In addition, magnetic susceptibility increased and sediment elemental composition changed. Elemental (P) measures point to enhanced phosphorus loading and C/N and isotope ratios of bulk organic matter indicate a shift to greater relative contribution of organic material from aquatic versus terrestrial environments, coinciding with the initiation of flood pulse processes. On the basis of radiocarbon dating in two cores, we estimate the initiation of the annual flood pulse occurred between ~4,450 and 3,910 cal year BP.

Original languageEnglish (US)
Pages (from-to)85-99
Number of pages15
JournalJournal of Paleolimnology
Volume45
Issue number1
DOIs
StatePublished - 2011

Fingerprint

Cambodia
sap
Holocene
lakes
lake
Mekong River
sediments
river
isotopes
inland fishery
isotope
freshwater fisheries
radiocarbon dating
terrestrial environment
rivers
magnetic susceptibility
sap flow
fluvial deposit
sediment
provenance

Keywords

  • Cambodia
  • Flood pulse
  • Mekong River
  • Radiogenic isotopes
  • Tonle Sap Lake

ASJC Scopus subject areas

  • Aquatic Science
  • Earth-Surface Processes

Cite this

Day, M. B., Hodell, D. A., Brenner, M., Curtis, J. H., Kamenov, G. D., Guilderson, T. P., ... Kolata, A. L. (2011). Middle to late Holocene initiation of the annual flood pulse in Tonle Sap Lake, Cambodia. Journal of Paleolimnology, 45(1), 85-99. https://doi.org/10.1007/s10933-010-9482-9

Middle to late Holocene initiation of the annual flood pulse in Tonle Sap Lake, Cambodia. / Day, Mary Beth; Hodell, David A.; Brenner, Mark; Curtis, Jason H.; Kamenov, George D.; Guilderson, Thomas P.; Peterson, Larry C; Kenney, William F.; Kolata, Alan L.

In: Journal of Paleolimnology, Vol. 45, No. 1, 2011, p. 85-99.

Research output: Contribution to journalArticle

Day, MB, Hodell, DA, Brenner, M, Curtis, JH, Kamenov, GD, Guilderson, TP, Peterson, LC, Kenney, WF & Kolata, AL 2011, 'Middle to late Holocene initiation of the annual flood pulse in Tonle Sap Lake, Cambodia', Journal of Paleolimnology, vol. 45, no. 1, pp. 85-99. https://doi.org/10.1007/s10933-010-9482-9
Day, Mary Beth ; Hodell, David A. ; Brenner, Mark ; Curtis, Jason H. ; Kamenov, George D. ; Guilderson, Thomas P. ; Peterson, Larry C ; Kenney, William F. ; Kolata, Alan L. / Middle to late Holocene initiation of the annual flood pulse in Tonle Sap Lake, Cambodia. In: Journal of Paleolimnology. 2011 ; Vol. 45, No. 1. pp. 85-99.
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