Interim report on the vertebrate deposits recovered from the Capricorn Caves, Rockhampton, Queensland
Creators: name: Louys, Julien
name: Cramb, Jonathan
name: Ferguson, Kyle
name: Kemp, Justine
name: Wood, Rachel
name: Miszkiewicz, Justyna J.
name: Guimarães, Nathalia R. Dias
name: Higgins, Pennilyn
name: Travouillon, Kenny J.
name: Hocknull, Scott A.
name: Webb, Gregory E.
name: Price, Gilbert J.
Publisher: name: Taylor & Francis
Year: 2023
Subjects: subject: Evolutionary Biology
subject: FOS: Biological sciences
subject: 59999 Environmental Sciences not elsewhere classified
subject: FOS: Earth and related environmental sciences
subject: 39999 Chemical Sciences not elsewhere classified
subject: FOS: Chemical sciences
subject: Ecology
subject: 69999 Biological Sciences not elsewhere classified
subject: Science Policy

description: Late Pleistocene to Holocene-aged microfaunal assemblages are rarely reported in Australia despite their critical importance for palaeoecological studies, as well as their bearing on the megafaunal extinction debate. Capricorn Caves, central-eastern Queensland, hosts three Late Pleistocene to Holocene deposits containing significant faunal records. Excavations were conducted on these deposits over several seasons, with analyses of recovered material ongoing. Here, we report interim results and explore their implications for our understanding of the microfaunal record of central eastern Queensland. Fern Chamber was previously dated using U-series to the Holocene (&gt;7.6 ± 0.2 ka). Honeymoon Suite was dated to &gt;6.4 ± 0.2 ka using U-series. However, new charcoal dates from the deposit span approximately 7.5–15.5 ka, although the association between charcoal and fauna is unresolved. The fauna is likely Holocene. Colosseum Chamber is the oldest of the deposits, and new single-grain luminescence ages and age-depth modelling suggest that the deposit likely spans MIS 1–4. We use abundant fragmentary rodent remains to examine palaeoenvironmental change over this period. Carbon and oxygen isotope analyses of rodent incisor fragments reveal broad diets within the rodent community, and significant differences in precipitation between glacial and interglacial conditions. Rodent long bone histological analyses indicate significant differences in bone metabolism at the family level between the MIS 3 and 2 samples, but not MIS 1. We suggest that these data support evidence for a mid-Holocene arid anomaly in the region, and increased aridity through the Holocene relative to the terminal Pleistocene. The sites contain at least 10 small mammal species either globally extinct or locally extirpated, including the Capricorn rabbit-rat (<i>Conilurus capricornensis</i>), the white-footed rabbit-rat (<i>Conilurus albipes</i>), the plains mouse (<i>Pseudomys australis</i>), Gould’s mouse (<i>Pseudomys gouldii</i>), Forrest’s mouse (<i>Leggadina forresti</i>), the long-tailed hopping mouse (<i>Notomys longicaudatus</i>), swamp rat (<i>Rattus lutreolus</i>), the white-tailed rat (<i>Uromys caudimaculatus</i>), the narrow-nosed planigale (<i>Planigale tenuirostris</i>), the Liverpool Plains striped bandicoot (<i>Perameles fasciata</i>), the Cape York brown bandicoot (<i>Isoodon peninsulae</i>), and the southern brown bandicoot (<i>Isoodon obesulus</i>). We also record significant range contractions for frogs (<i>Philoria</i> sp., <i>Neobatrachus</i> sp.) and earless dragons (<i>Tympanocryptis</i> sp.). This study demonstrates that significant changes in the microfaunal community of tropical Queensland occurred between the Late Pleistocene and the late Holocene. It also reinforces how poorly recorded native faunas are from the late Holocene through the historical period, to today. Such records underpin and are thus vital for modern biodiversity conservation efforts. <i>Julien Louys</i><i>[j.louys@griffith.edu.au</i><i>], Australian Research Centre for Human Evolution, Griffith University, Brisbane, Australia; Jonathan Cramb</i><i>[jonathan.cramb@qm.qld.gov.au</i><i>], Queensland Museum, Brisbane, Australia; Kyle Ferguson</i><i>[k.ferguson81@outlook.com.au</i><i>], School of Earth and Environmental Science, The University of Queensland, Brisbane, Australia; Justine Kemp</i><i>[j.kemp@griffith.edu.au</i><i>], Australian Research Centre for Human Evolution, Griffith University, Brisbane, Australia; Rachel Wood</i><i>[rachel.wood@arch.ox.ac.uk</i><i>], School of Archaeology and Anthropology, Australian National University, Canberra, Australia and Oxford Radiocarbon Accelerator Unit (ORAU), University of Oxford, Oxford, UK; Justyna J. Miszkiewicz [j.miszkiewicz@uq.edu.au], School of Social Science, University of Queensland, Brisbane, Australia and Naturalis Biodiversity Center, Leiden, the Netherlands; Nathalia R. Dias Guimarães</i><i>[ndg0601@gmail.com</i><i>], School of Archaeology and Anthropology, Australian National University, Canberra, Australia; Penny Higgins</i><i>[pennilyn.higgins@gmail.com</i><i>], EPOCH Isotopes, 6606 E Townline Road, Williamson, NY 14589, USA; Kenny J. Travouillon</i><i>[Kenny.Travouillon@museum.wa.gov.au</i><i>], Western Australian Museum, Perth, Australia; Scott A. Hocknull</i><i>[scott.hocknull@qm.qld.gov.au</i><i>], Geosciences, Queensland Museum, Brisbane, Australia; Gregory E. Webb</i><i>[g.webb@uq.edu.au</i><i>], School of Earth and Environmental Science, The University of Queensland, Brisbane, Australia; Gilbert J. Price</i><i>[g.price1@uq.edu.au</i><i>], School of Earth and Environmental Science, The University of Queensland, Brisbane, Australia.</i>