Confirmed archaeological evidence of water deer in Vietnam: Relics of the Pleistocene or a shifting baseline?

C. M. Stimpson*, S. O'Donnell, N. T.M. Huong, R. Holmes, B. Utting, T. Kahlert, R. J. Rabett

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)
28 Downloads (Pure)

Abstract

Studies of archaeological and palaeontological bone assemblages increasingly show that the historical distributions of many mammal species are unrepresentative of their longer-term geographical ranges in the Quaternary. Consequently, the geographical and ecological scope of potential conservation efforts may be inappropriately narrow. Here, we consider a case-in-point, the water deer Hydropotes inermis, which has historical native distributions in eastern China and the Korean peninsula. We present morphological and metric criteria for the taxonomic diagnosis of mandibles and maxillary canine fragments from Hang Thung Binh 1 cave in Tràng An World Heritage Site, which confirm the prehistoric presence of water deer in Vietnam. Dated to between 13 000 and 16 000 years before the present, the specimens are further evidence of a wider Quaternary distribution for these Vulnerable cervids, are valuable additions to a sparse Pleistocene fossil record and confirm water deer as a component of the Upper Pleistocene fauna of northern Vietnam. Palaeoenvironmental proxies suggest that the Tràng An water deer occupied cooler, but not necessarily drier, conditions than today. We consider if the specimens represent extirpated Pleistocene populations or indicate a previously unrecognized, longer-standing southerly distribution with possible implications for the conservation of the species in the future.

Original languageEnglish
Article number210529
Number of pages15
JournalRoyal Society Open Science
Volume8
Issue number6
DOIs
Publication statusPublished - 30 Jun 2021
Externally publishedYes

Keywords

  • Hydropotes inermis
  • Pleistocene
  • Vietnam
  • water deer
  • zooarchaeology

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