Cement Mills, Gore
Basic information
Sample name: Cement Mills, Gore
Reference: A. Bartholomai. 1977. The fossil vertebrate fauna from Pleistocene deposits at Cement Mills, Gore, southeastern Queensland. Memoirs of the Queensland Museum 18(1):41-51 [ER 3691]
Geography
Country: Australia
State: Queensland
Coordinate: 28° 16' 48" S, 151° 28' 48" E
Coordinate basis: stated in text
Time interval: Late Pleistocene
Min Ma: 0.0536
Age basis: U/Th
Geography comments: "Cement Mills, Gore, is located approximately 70 km northeast of Texas", a town in the Goondiwindi Region of southern Queensland.
U/Th dating of two megafaunal teeth from the deposit "yielded almost identical ages of 53.6 ± 0.2 ka and 53.9 ± 0.3 ka" (Price et al. 2009).
These dates most likely represent minimum ages for the fossil accumulation, due to the nature of U/Th dating on fossil bone and teeth.
U/Th dating of two megafaunal teeth from the deposit "yielded almost identical ages of 53.6 ± 0.2 ka and 53.9 ± 0.3 ka" (Price et al. 2009).
These dates most likely represent minimum ages for the fossil accumulation, due to the nature of U/Th dating on fossil bone and teeth.
Environment
Lithology: siliciclastic (mixed)
Taphonomic context: carnivore accumulation,cave,fissure fill
Habitat comments: "The cave and fissure deposits from Cement Mills occur in the Devonian–Carboniferous limestones of the Texas Beds that form part of the larger Wooloomin-Texas Block of the New England Fold Belt".
"Fossiliferous sediments are represented by cemented breccia fissure-fills and cemented cave floor sediments that are dominated by clays, silts and carbonate nodules".
"Only a single stratigraphic faunal-bearing unit has been recognised within the deposit".
"Faunal elements likely entered the caves and fissures via marsupial predators that used the caves as lairs, and wash and fill processes".
"Fossiliferous sediments are represented by cemented breccia fissure-fills and cemented cave floor sediments that are dominated by clays, silts and carbonate nodules".
"Only a single stratigraphic faunal-bearing unit has been recognised within the deposit".
"Faunal elements likely entered the caves and fissures via marsupial predators that used the caves as lairs, and wash and fill processes".
Methods
Life forms: rodents,other large mammals,other small mammals,birds,lizards
Sampling methods: quarry
Sample size: 291 specimens
Sampling comments: No specific excavation details are provided. The counts below are of the remains described by Bartholomai (1977), which seems to report all faunal material that has ever been collected from the site.
Metadata
Sample number: 3868
Contributor: Benjamin Carter
Enterer: Benjamin Carter
Created: 2022-01-31 15:13:28
Modified: 2022-03-04 03:05:12
Abundance distribution
30 species
13 singletons
total count 291
geometric series index: 73.2
Fisher's α: 8.393
geometric series k: 0.8509
Hurlbert's PIE: 0.8059
Shannon's H: 2.1749
Good's u: 0.9555
Each square represents a species. Square sizes are proportional to counts.
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Register
Tiliqua scincoides | 1 | |
Latagallina naracoortensis | 1 | |
"Progura naracoortensis" | ||
Dasyurus cf. viverrinus | 1 | |
Sarcophilus laniarius | 33 | |
Thylacinus cynocephalus | 2 | |
Isoodon sp. | 2 | |
Perameles nasuta | 32 | 992 g |
Phascolarctos stirtoni | 1 | |
Thylacoleo carnifex | 9 | |
Vombatus ursinus | 5 | 29 kg |
Phascolonus gigas | 2 | |
Ramsayia magna | 2 | |
"Phascolomis magnus" | ||
Palorchestes azael | 1 | |
Palorchestes cf. parvus | 1 | |
Nototherium inerme | 1 | |
also 2 Diprotodontidae indet. | ||
Potorous cf. tridactylus | 3 | 731 g |
Aepyprymnus rufescens | 22 | 2.9 kg |
Bettongia sp. | 1 | |
Sthenurus oreas | 1 | |
Procoptodon cf. rapha | 1 | |
Protemnodon anak | 2 | |
Protemnodon brehus | 1 | |
Protemnodon roechus | 2 | |
Thylogale sp. | 1 | |
Macropus giganteus | 3 | 38 kg grazer |
Macropus titan | 1 | |
Notamacropus cf. agilis siva | 3 | 14 kg browser-grazer |
"Macropus agilis siva" | ||
Notamacropus dorsalis | 44 | |
"Macropus dorsalis" | ||
Notamacropus parryi | 108 | |
"Macropus parryi" | ||
Rodentia indet. | 4 |