Passive infrared technology was used to film diurnal and nocturnal scavenging behavior of brown rats and gray squirrels at the University of Tennessee's Anthropological Research Facility. This direct documentation demonstrated that brown rats modified fat-laden cancellous bone while gray squirrels generally gnawed the thicker bone cortices only after fats had leached away. A case study placed in a shaded portion of the Facility indicated the postmortem interval for initial gnawing by gray squirrels was slightly over 30 months. An examination of 53 human skeletons in the William M. Bass Forensic Skeletal Collection revealed that 10 cases had gnaw marks consistent with those made by gray squirrels. One of the 10 cases had been gnawed within 16 months of time-since-death, while the remaining nine had postmortem intervals >30 months. Additional observed modifications made to nonhuman bone by gray squirrels indicate that squirrel gnaw marks on bone can serve as a minimal estimate of time-since-death in a temperate environment similar to that of East Tennessee.
The explication of prehistoric subsistence economies has been of increasing interest to archaeologists. This emphasis is reflected, in part, by the considerable attention afforded faunal analyses in the recent archaeological literature. However, little effort has been made toward developing methods that permit meaningful comparisons of food resources at the interspecies level. Data pertinent to the calculation of both quantitative and qualitative food potential of many of the vertebrate animals represented in archaeological contexts are extant. These data are lacking for freshwater mussels, frequently found in archaeological sites in eastern North America. Information relevant to determining the food energy provided by freshwater mussels common to much of the Mississippi River drainage is presented. Results are applicable to more credible interpretations of prehistoric subsistence as related to animal food resources.
The previously poorly known “Tapiravus” polkensis Olsen, 1960 (Mammalia, Perissodactyla, Tapiridae) is now known from abundant, well preserved specimens from both the type area in central Florida and from the Gray Fossil Site (GFS) in eastern Tennessee. The latter has produced over 75 individuals, the greatest number of tapirids from a single fossil site, including many articulated skeletons. Almost all linear measurements taken on skulls, mandibles, and cheek teeth from GFS have coefficients of variation less than 10 (most between 3 and 7), indicating the presence of a single species. However, the sample reveals considerable intraspecific variation for a few key morphologic features, including development of the sagittal crest, outline shape of the nasals, and number and relative strength of lingual cusps on the P1. The Florida sample of T. polkensis is more limited, but has the same state as the GFS sample for all preserved characters of systematic significance, and while the Florida teeth are on average smaller (especially narrower lower cheek teeth), they fall either within or just below the observed range of the Gray Fossil Site population. The new material supports a reassignment of “Tapiravus” polkensis to the genus Tapirus, and demonstrates that the geologic age of the species is significantly younger than previously thought, Hemphillian rather than Barstovian. Tapirus polkensis is the smallest known North American Tapirus, and smaller than any of the extant species in the genus, with an estimated average mass of 125 kg.
The recovery of pollen from archaeological sites in Eastern North A merica has not been as successful as it has been in the western part of the continent. The depositional environment of eastern archaeological sites is generally unfavorable for pollen preservation and archaeologists have failed to search out special situations in which pollen may be preserved. At the Rhoads site, a Proto-Historic Indian village in central Illinois, abundant pollen has been found associated with copper artifacts and deeply buried tree bark. Pollen was preserved around copper, apparently due to dissolved copper salts which act as a fungicide. Tree bark, an excellent collection surface for air-borne pollen, can yield abundant pollen when preserved. When the factors involved in pollen deposition and preservation are considered, the prospects for archaeological palynology in eastern North America should be greatly enhanced.
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