Abstract

The study of faunal remains from archaeological sites is often complicated by the presence of large numbers of highly fragmented, morphologically unidentifiable bones. In Australia, this is the combined result of harsh preservation conditions and frequent scavenging by marsupial carnivores. The collagen fingerprinting method known as zooarchaeology by mass spectrometry (ZooMS) offers a means to address these challenges and improve identification rates of fragmented bones. Here, we present novel ZooMS peptide markers for 24 extant marsupial and monotreme species that allow for genus-level distinctions between these species. We demonstrate the utility of these new peptide markers by using them to taxonomically identify bone fragments from a nineteenth-century colonial-era pearlshell fishery at Bandicoot Bay, Barrow Island. The suite of peptide biomarkers presented in this study, which focus on a range of ecologically and culturally important species, have the potential to significantly amplify the zooarchaeological and paleontological record of Australia.

Highlights

  • Australia is home to an extremely rich and unique fauna [1], with more than 85% of its terrestrial mammal species classed as endemic [2]

  • In addition to the set of peptide markers that is regularly reported for zooarchaeology by mass spectrometry (ZooMS) studies, we report two additional peptide markers that can be used to distinguish between marsupial taxa

  • The novel set of reference peptide markers developed for this study allow for genus-level identifications of Australian marsupials using ZooMS, with some limitations only with regards to macropods

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Summary

Introduction

Australia is home to an extremely rich and unique fauna [1], with more than 85% of its terrestrial mammal species classed as endemic [2]. It is the only region globally, other than Papua New Guinea, where marsupials, placentals and monotremes coexist [3]. Research on past Australian terrestrial faunas, and marsupials, can provide insight into early human activity on the Australian continent, enable reconstruction of palaeoenvironmental conditions and shifts in biodiversity over time, and help assess the impact of past climate change

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