Spengler, Robert N., III (2019) Origins of the Apple: The Role of Megafaunal Mutualism in the Domestication of Malus and Rosaceous Trees. Frontiers in Plant Science. 10(617):1-18.
The apple (Malus domestica [Suckow] Borkh.) is one of the most economically and culturally significant fruits Continue reading
A new project aims to understand the early prehistoric use of animals and plants along the ancient Silk Road Continue reading
Paleoethnobotany is the scientific investigation of human and plant interactions in the past; Continue reading
Over the past decade research into the paleoeconomy of Bronze Age (3500-800 B.C.) peoples in Central Asia has shown how complex the productive economy was. The agropastoral system involved an array of crops and herd animals. In this article, we present a paleoethnobotanical study conducted on sediment samples from excavation units at the site of Adji Kui, Turkmenistan. Continue reading
During the first millennium A.D., Central Asia was marked by broad networks of exchange and interaction, what many historians collectively refer to as the “Silk Road”. Much of this contact relied on high-elevation mountain valleys, often linking towns and caravanserais through alpine territories. This cultural exchange is thought to have reached a peak in the late first millennium A.D., Continue reading
Spengler, Robert N., III (2018) Vegetation History and Archaeobotany.
In the early 1980s Naomi Miller changed the field of palaeoethnobotany; her research into whether the ancient seed eaters of southwest Asia were human or herbivore opened an ongoing debate over the impact that burning of animal dung had on the formation of archaeobotanical assemblages, and how researchers can differentiate between human and animal food remains. Continue reading
This study presents a high-resolution, chronologically well-constrained pollen record from Lake Kushu (45֯25’ 58”N, 141֯ 02’05”E) and a record of archaeobotanical remains from the nearby Hamanaka 2 archaeological site. The pollen record suggests continuous long-term cooling, which parallels the decline in Northern Hemisphere summer insolation. This cooling trend is overlaid by several rather quick transitions towards cooler conditions (ca. 5540/5350, 1550, and 390 cal BP) and one distinct decadal-scale cold event around 4130 cal BP. Continue reading
