Kiser Lake, Ohio.

 Petroglyph, Tamgaly, Kazakhstan.

 Lake Peten Itza, Guatemala.

 Lake Erkhel, Mongolia.

 The Maya site of Palenque, Mexico.

 Alta Lake, Washington State.

 Lake Kastoria, Greece.

 Deerstones near Lake Erkhel, Mongolia.  Limnes basin, western Crete.

 Lake Uzunkul, Russia.

 
RESEARCH IN CENTRAL ASIA:
 

Lake Sediment Records of Holocene Climate Variability in Central Asia:

I am currently reconstructing Holocene environmental changes in Central Asia using sediment records from multiple lake systems. This research program builds upon the success of a number of U.S.-led and joint German-Mongolian-Russian field expeditions. We are examining laminated sediment records from two sites in Mongolia, and decadal to century-scale environmental changes from nearly forty additional lake sediment core sites along east-west and north-south environmental gradients in Mongolia, northern and southeastern Kazakhstan, and southern Siberia. Geochemical assays (carbonate mineral oxygen and carbon isotopic analyses) and sedimentological (scanning XRF, rock-magnetic) and biological (diatoms, photosynthetic pigments, fossil pollen) studies of the sediment cores are providing information on the local and regional extent of regional Holocene climate transitions. This study will also provide insight into the external and internal forcing mechanisms of extreme continentality and abrupt changes within the Asian interior and will provide insight on twentieth century warming by extending proxy data beyond existing instrumental and tree-ring records.

The most recent component of this collaborative project included paleoenvironmental field research within the Russian Federation (Chelyabinsk Oblast and the Republic of Bashkortostan) during a three-week period in late June and July 2008. During the field campaign, we recovered multiple sediment cores from five lake sites located along the eastern slope of the southern Ural Mountains (along a north-south transect that spanned ~190 km). Waters of the study lakes are rich in carbonate and bicarbonate and thereby promote shell formation. Because of the high density of carbonate microfossils (ostracode and gastropod shells) preserved in the sediments of the lakes, we expect to generate stable isotope data sets that, when coupled with sedimentological and biological analyses, will provide valuable climate information and thereby an environmental context for the emergence of a complex socio-economic formation in the Eurasian steppe region.

Related Programs:

Carnegie Museum of Natural History - Department of Anthropology (Dr. Sandra Olsen)
Kent State University - Department of Geology (Dr. Joseph Ortiz)
National University of Mongolia - Faculty of Biology (Dr. Soninkhishig Nergui)
National University of Mongolia - Mongolian Landscape Research Centre (Dr. Michael Walther)
University of Akron - Department of Geology and Environmental Science (Dr. John Peck)
University of Pittsburgh - Department of Anthropology (Dr. Bryan Hanks)
Washington University in St. Louis - Department of Anthropology (Dr. Michael Frachetti)
 

 Sanjin Nuur, Mongolia - June 2003.    Sediment cores from Mongolia - June 2003.    Bol'shoe Chebach'e, northern Kazakhstan - July 2005.
 Ozero Uzunkul, Southern Urals - July 2008.
 

Isotopic Analysis of Fossil Horse Teeth from Archaeological Sites in Mongolia and Kazakhstan:

Within the framework of a related project, horse teeth collected from archaeological sites within Mongolian and Kazakhstan will be analyzed for oxygen and carbon isotopic compositions. Inter and intra-tooth variation in enamel oxygen and carbon isotopic values is controlled largely by the isotopic composition of water and food ingested by mammals during the period of enamel formation. Tooth remains from different archaeological strata at a single locality can thus be used to reconstruct past dietary patterns of grazing horses (the relative contribution of C3 and C4 plants) and climate changes (isotopic shifts attributed to temperature or moisture availability). Collection of horse teeth was completed over four field seasons (2004 and 2005 in Mongolia, 2005 and 2007 in Kazakhstan). Initial results from the stable isotopic analyses of modern specimens confirms correlation with temperature, precipitation, and vegetation gradients within Mongolia and Kazakhstan, and thereby establishes the utility of tooth enamel stable isotope measurements as a record of climate, seasonality, and vegetation in the region.  Maps generated of the oxygen and carbon isotopic values in modern horse remains will thus serve as a baseline for interpreting the isotope signals preserved in archaeological materials and thereby increase the accuracy of paleoenvironmental reconstructions. 

Related Programs:

Carnegie Museum of Natural History - Department of Anthropology (Dr. Sandra Olsen)
Indiana University of Pennsylvania - Department of Anthropology (Dr. Francis Allard)
Smithsonian Institution - Department of Anthropology (Dr. William Fitzhugh)
Yale University - Department of Anthropology (Dr. William Honeychurch)
 

 Horses on the Mongolian steppe - July 2004.    Summer ger camp, central Mongolia - July 2004.    Bronze Age deerstone, northern Mongolia - June 2004.
 Horse mandible field collections - July 2004.    Horse remains from an excavation, Mongolia - July 2004.    Sequentially sampled modern horse tooth.