Date of Award

3-31-2025

Document Type

Honors Thesis

Department

Biology

First Advisor

Thomas Goodwin

Abstract

The Prillwitz mammoth, a nearly complete mammoth skeleton found in Southwest Michigan in 1962, is one of the geologically youngest mammoths from North America (AMS C-14 date: 11,300 ± 100 BP). Bones are well preserved; some long bones show post-mortem flaking, scratches, or grooves of unknown origin. All long-bone epiphyses remain unfused except the distal humerus, suggesting it was < 28 years old at death. In contrast, the skull and mandible preserve M3s and m3s, respectively, that are in mid-wear, indicating an Asian Elephant Year dental age of ~45-50 years. Long bone size and inferred shoulder height are consistent with the size of a large woolly mammoth (Mammuthus primigenius) or small to mid-sized Columbian mammoth (Mammuthus columbi), but dental evidence is most consistent with M. columbi.

Pelvic dimensions suggest it is a male. The ≥ 17-year mismatch between age inferred from tooth progression and wear (~45 Asian Elephant Years) and age inferred from epiphyseal fusion (< ~28 Asian EY if male) may indicate either substantially accelerated dental progression or delayed skeletal maturation for this mammoth; we deem the latter more likely. Based on modern analogs, delayed maturation could have been due to severe malnutrition, hormonal imbalance, illness, or genetic factors. Given the geologically young age of the Prillwitz mammoth (likely near the time of mammoth extinction), we speculate that delayed skeletal maturation may have been attributed to environmental stressors near the end of the Pleistocene. Further work is warranted on very late mammoths.

Subject Area

Mammoths--Michigan

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