Claudia Chang, professor of archaeology at Sweet Briar College in Virginia, is director of an international field research project on the archaeology of the Iron Age in the Republic of Kazakhstan. Claudia blogged for Bento from Kazakhstan during the exhibition Nomads and Networks: The Ancient Art and Culture of Kazakhstan at the Sackler last fall.
My friends and even a former professor used to joke that archaeologists have a kind of schizophrenic life. We have lovely summers working in the field, doing surveys and excavations. During the winter months, we find ourselves in the laboratory, counting sherds, transposing field notes, and waiting for all the specialists’ reports to be completed, from the radiometric dates of ancient hearths to the metallurgical studies of ancient bronzes. In fact, this charmed existence of field archaeology usually means that you pay for all those good times in the field; for every week of fieldwork you need about three times that for laboratory cataloging, cleaning and processing artifacts, counting, creating statistics and spreadsheets, writing up reports, and interpreting the data. Most of us have learned to make our “deal with the devil.” Since January 1, 2013, I have been holed up in my attic office in Virginia, overlooking the foothills of the Blue Ridge, surrounded by books, papers, and articles, writing the early chapters of a book on Iron Age research on the Talgar fan.
The view out my window is lovely this afternoon, as the sun sets on Paul’s Mountain. I am surrounded by books that range from the philosophy of science to Bronze Age Eurasia. Right now it seems impossible to condense 18 years of fieldwork, let alone the past five months of research on the Talgar fan, into any kind of readable narrative, either for an academic audience or myself.
Recently, Rebecca Beardmore, a PhD student in archaeology at University College, London, called me by Skype from Birmingham, England, where she had just finished graphing all the phytolith counts she made during the 2011 field season at Tuzusai, our Iron Age settlement site. Phytoliths, or plant stones, are the silicate cells of ancient plant remains that can be trapped in archaeological soils, such as ancient mudbricks. Rebecca’s analysis, conducted with a scanning electron microscope, has shown that the reddish-yellow and yellow mudbrick samples have lower densities of ancient plant materials than the brown-red and greenish mudbricks. All four samples of mudbrick seem to have some remnants of wheat plants, as well as wild grass parts, both husks and leaves. This means that the Iron Age builders at Tuzusai probably dumped a bunch of plant material into pits where they mixed the mudbricks, which then formed the walls, floors, and ramps of the adobe architecture we have discovered. But why do some bricks have higher densities of plant material than others?
That question sent me back to my field notes from 2011, which include chicken-scratch drawings of the red-brown and green mudbricks. Those mudbricks appear on my sketches to be large wall or foundation features, while the yellow or reddish-yellow ones are usually the tops of the platform or just beneath the plastered floors. Could it be that the ancient inhabitants of Tuzusai put more straw and debris into the foundation walls and less in the floor bricks? I told Rebecca that she should rename her thesis, “The Unseen Archaeological Record.” She says maybe she’ll title the thesis, “Down and Dirty, Mudbrick and Animal Dung.” Good thing I have those sketches of mudbricks in my notebook.
After we left Tuzusai last fall, the archaeological facts come now from the laboratory, the field notebooks, and an occasional inspiration I might have while staring out the window at the mocking bird perched on the crab apple tree. Central Virginia and the foothills of the Blue Ridge Mountains seem faraway from the Tian Shan Mountains of Kazakhstan, but lest I forget, a large map of the Upper Asi Valley is pinned to the wall by my desk.