Kalbarri (UWA collection): Bartonian - Priabonian, Australia

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Demospongiae
Demospongea indet. (Sollas 1875)
corrected as Demospongiae
Cephalopoda - Nautilida - Aturiidae
Aturia sp. Bronn 1838
    = Aturia clarkei Teichert 1944
Darragh and Kendrick 2008
Cephalopoda - Nautilida - Nautilidae
Nautilida indet. Agassiz 1847
    = Eutrephoceras sp. Hyatt 1894
Darragh and Kendrick 2008
unclassified
Bryozoa indet. Ehrenberg 1831
Globigerinidae
Globigerinatheka index
? Catapsydrax sp. Bolli et al. 1957
Subbotina linaperta
Subbotina inaequispira
Subbotina eocaena
transitional to S. corpulenta
unclassified
? Acarinina sp.
Hedbergellidae
? Turborotalia sp. (Cushman and Burmudez 1949)
original and current combination Globorotalia (Turborotalia)
see common names

Geography
Country:Australia State/province:Western Australia
Coordinates: 27.8° South, 114.3° East (view map)
Paleocoordinates:48.7° South, 99.2° East
Basis of coordinate:estimated from map
Geographic resolution:outcrop
Time
Period:Paleogene Epoch:Eocene
10 m.y. bin:Cenozoic 3
Key time interval:Bartonian - Priabonian
Age range of interval:41.20000 - 33.90000 m.y. ago
Stratigraphy
Stratigraphic resolution:bed
Stratigraphy comments: Collectively, the planktonic foraminifers indicate that the newly discovered site belongs within the P13 to P16 zonal range (40.5 – 34.0 Ma BKSA95).
Lithology and environment
Primary lithology: poorly lithified cherty/siliceous mudstone
Secondary lithology: poorly lithified cherty/siliceous sandstone
Lithology description: Iron-stained siliceous argillites with scattered large fragments of silicified bryozoans as well as large (up to about 30 cm) intact siliceous sponges. A relatively clean sponge spicule dominated arenite that includes silicified calcareous skeletal grains (including abundant foraminifers, and common gastropods and bryozoan fragments) is also present.
Environment:transition zone/lower shoreface
Geology comments: Because of the abundance of robust diverse miliolid foraminifers and the low planktonic percentage (about 10%), the new unit probably accumulated in inner neritic conditions (following Murray 1991), at water depths between about 10 and 30 m (based on unpublished observations of DW Haig for present-day assemblages along the Western Australian coast).
Taphonomy
Modes of preservation:body,original silica,replaced with silica
Size of fossils:macrofossils
Collection methods and comments
Reason for describing collection:general faunal/floral analysis
Collection method comments: Repository: University of Western Australia
Metadata
Database number:179822
Authorizer:M. Clapham Enterer:M. Clapham
Modifier:M. Clapham Research group:marine invertebrate
Created:2016-07-02 14:18:39 Last modified:2017-05-23 16:34:15
Access level:the public Released:2016-07-02 14:18:39
Creative Commons license:CC BY
Reference information

Primary reference:

59651. D. W. Haig and A. J. Mory. 2003. New record of siliceous, marine, later Eocene from Kalbarri, Western Australia. Journal of the Royal Society of Western Australia 86:107-113 [M. Clapham/M. Clapham]

Secondary references:

59650 T. A. Darragh and G. W. Kendrick. 2008. Silicified Eocene molluscs from the Lower Murchison district, southern Carnarvon Basin, Western Australia. Records of the Western Australian Museum 24:217-246 [M. Clapham/M. Clapham]