Kelly Hill Cave (K1–P2) - Layer 7C
Basic information
Sample name: Kelly Hill Cave (K1–P2) - Layer 7C
Reference: S. J. Adams, M. C. McDowell, and G. J. Prideaux. 2016. Understanding accumulation bias in the ecological interpretation of archaeological and paleontological sites on Kangaroo Island, South Australia. Journal of Archaeological Science: Reports 7:715-729 [ER 3692]
Geography
Country: Australia
State: South Australia
Coordinate: 35° 58' 52" S, 136° 54' 26" E
Coordinate basis: based on nearby landmark
Time interval: Pleistocene - Holocene
Section: 3692
Unit number: 8
Unit order: above to below
Max Ma: 0.01222
Min Ma: 0.00807
Age basis: radiocarbon (uncalibrated)
Geography comments: "Kelly Hill Cave (K1) is a non-cultural cave site on Kangaroo Island consisting of large cavities up to 25 m below the crest of Kelly Hill".
Layer 7C of K1–P2 is constrained by a radiocarbon date for Layer 7A of 8070 ± 40 BP, ranging from 9050–8700 cal. BP., and a radiocarbon date for Layer 7D of 12,220 ± 50 BP, ranging from 14,250–13,800 cal. BP.
Layer 7C of K1–P2 is constrained by a radiocarbon date for Layer 7A of 8070 ± 40 BP, ranging from 9050–8700 cal. BP., and a radiocarbon date for Layer 7D of 12,220 ± 50 BP, ranging from 14,250–13,800 cal. BP.
Environment
Lithology: limestone
Taphonomic context: bird accumulation,cave,pitfall trap
Habitat comments: "The Kelly Hill Cave system consists of a series of cave entrances connected by extensive passages covering at least 36 000 square metres".
The system likely formed through water slowly infiltrating poorly consolidated dune sediments resulting in the dissolution of large lateral cavities that have matured into structurally stable chambers (McDowell et al. 2013).
The faunal remains likely accumulated "through a combination of pitfall entrapment of large hopping species and owl accumulation".
The system likely formed through water slowly infiltrating poorly consolidated dune sediments resulting in the dissolution of large lateral cavities that have matured into structurally stable chambers (McDowell et al. 2013).
The faunal remains likely accumulated "through a combination of pitfall entrapment of large hopping species and owl accumulation".
Methods
Life forms: rodents,other large mammals,other small mammals
Sampling methods: quarry,screenwash
Sample size: 78 specimens
Sampling comments: "A well-stratified late Pleistocene–Holocene accumulation containing abundant faunal material was excavated near the entrance of K1".
"The excavation (K1–P2) consisted of two 1 m × 1 m squares excavated to bedrock in 5-cm spits within layers".
"Sediment was dry sieved through a 12-mm sieve to retrieve large bones then washed through a 1.5-mm sieve to retrieve smaller faunal elements".
"The excavation (K1–P2) consisted of two 1 m × 1 m squares excavated to bedrock in 5-cm spits within layers".
"Sediment was dry sieved through a 12-mm sieve to retrieve large bones then washed through a 1.5-mm sieve to retrieve smaller faunal elements".
Metadata
Sample number: 3876
Contributor: Benjamin Carter
Enterer: Benjamin Carter
Created: 2022-02-01 16:06:01
Modified: 2023-04-29 05:27:10
Abundance distribution
12 species
6 singletons
total count 78
extrapolated richness: 33.0
Fisher's α: 3.961
geometric series k: 0.7007
Hurlbert's PIE: 0.5604
Shannon's H: 1.3798
Good's u: 0.9237
Each square represents a species. Square sizes are proportional to counts.
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Register
| Dasyurus maculatus | 1 | |
| Sminthopsis aitkeni | 2 | |
| Sminthopsis murina | 1 | |
| also 3 Sminthopsis sp. | ||
| Cercartetus lepidus | 1 | |
| Potorous platyops | 1 | |
| Onychogalea fraenata | 2 | 4.0 kg |
| Pseudomys auritus | 1 | |
| Pseudomys australis | 3 | |
| Pseudomys gouldii | 1 | |
| Pseudomys occidentalis | 9 | |
| Pseudomys shortridgei | 6 | |
| also 5 Pseudomys sp. | ||
| Rattus fuscipes | 50 | |
Current reference:
Shotwell 1968 (ER 3992)