A model of the 4000-year paleohydrology (δ18O) record from Lake Salpetén, Guatemala

A simple mass-balance model provides insights into the influence of catchment vegetation changes and climate variability on the hydrologic and stable oxygen isotope (δ18O) evolution of Lake Salpetén, in the Maya Lowlands of northern Guatemala. Model simulations for the last 4000years incorporate pol...

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Veröffentlicht in:	Global and planetary change 2016-03, Vol.138, p.43-55
Hauptverfasser:	Rosenmeier, Michael F., Brenner, Mark, Hodell, David A., Martin, Jonathan B., Curtis, Jason H., Binford, Michael W.
Format:	Artikel
Sprache:	eng
Schlagworte:	Catchments Computer simulation Freshwater Guatemala Holocene Hydrology Inclusions Lakes Maya Oxygen isotopes Paleoclimate Sediments Stable isotopes Vegetation Watershed modeling
Online-Zugang:	Volltext
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