Gordon Valley: Anisian, Antarctica
collected by Hammer 1985-

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Amphibia - Temnospondyli
Kryostega collinsoni Sidor et al. 2008
1 specimen
AMNH 24419, skull fragment
Amphibia - Temnospondyli - Benthosuchidae
Benthosuchidae indet. Efremov 1940
Wang et al. 2013 1 specimen
AMNH 24415
Amphibia - Temnospondyli
Antarctosuchus polyodon Sidor et al. 2014
Sidor et al. 2014 1 specimen
AMNH 24411
Kannemeyeriiformes
Kannemeyeriidae indet. Huene 1948
Hammer 1995 1 specimen
AMNH 24403, right maxillary fragment
    = Kannemeyeriiformes indet. Huene 1948
Fröbisch 2009
Anomodontia
Kannemeyeriiformes indet. (Huene 1948)
Smith et al. 2020 2 specimens
AMNH FARB 24412 (maxillary tooth root including a small portion of maxillary bone) and LACM-DI 160748 (Smith et al. 2020 also describe AMNH 24403)
Cynognathidae
Cynognathidae indet.
Hammer 1995 3 specimens
AMNH 24407, partial dentary; AMNH 24406, jaw fragment; AMNH 24423, partial right mandible
unclassified
Diademodontidae indet. Haughton 1925
Hammer 1995 1 specimen
AMNH 24421, skull fragment
    = Diademodon sp. Seeley 1895
Kammerer et al. 2010
Cynognathus sp. Seeley 1895
Hammer 1995 1 specimen
AMNH 24422, left mandible
see common names

Geography
Country:Antarctica
Coordinates: 84.3° South, 164.1° East (view map)
Paleocoordinates:76.9° South, 79.5° East
Basis of coordinate:estimated from map
Geographic resolution:outcrop
Time
Period:Triassic Epoch:Middle Triassic
Stage:Anisian 10 m.y. bin:Triassic 2
Key time interval:Anisian
Age range of interval:247.20000 - 242.00000 m.y. ago
Stratigraphy
Formation:Fremouw Member:Upper
Stratigraphic resolution:member
Stratigraphy comments: Correlated to the Cynognathus Assemblage Zone Subzone C of southern Africa, and thus Anisian in age. Fauna occurs at the base of the "upper" member of the Fremouw Formation
Lithology and environment
Primary lithology:quartzose,intraclastic lithified silty conglomerate
Includes fossils?Y
Lithology description: Hammer 1995 says "8 meter thick quartzose sandstone containing sizeable logs and siltstone clasts" Sidor et al. 2008 says "Most of the clasts in the conglomerate are rounded and are made up of greenish-gray siltstone that is lithologically the same as a siltstone that underlies the bone bed. The elongate clasts in the conglomerate exhibit no preferred orientation; however, the underlying sandstones indicate a general northwest paleocurrent. The clasts range in diameter from 5 mm to about 60 cm, with an average size of 5–10 cm. The conglomerate has a matrix of medium-grained, quartz-rich sand, similar to un- derlying channel sands. The fact that the conglomerate is domi- nated by intraclasts that were derived from underlying siltstones indicates that the transporting flow was carrying locally eroded material that was transported a relatively short distance. The nature of the unit suggests rapid deposition from a large flow of relatively high viscosity and moderate to lower velocity (Krissek et al., 1991). "
Environment:"channel" Tectonic setting:foreland basin
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Preservation of anatomical detail:medium
Temporal resolution:snapshot
Collection methods and comments
Collection methods:surface (in situ),field collection
Reason for describing collection:taxonomic analysis
Museum repositories:AMNH
Collectors:Hammer Collection dates:1985-86
Metadata
Database number:105296
Authorizer:R. Butler, C. Sidor, E. Dunne Enterer:R. Butler, C. Sidor, E. Dunne
Modifier:R. Butler Research group:vertebrate
Created:2011-02-18 23:17:23 Last modified:2015-12-15 19:57:24
Access level:the public Released:2011-02-18 23:17:23
Creative Commons license:CC BY
Reference information

Primary reference:

38098. C. A. Sidor, R. Damiani, and W. R. Hammer. 2008. A new Triassic temnospondyl from Antarctica and a review of Fremouw Formation biostratigraphy. Journal of Vertebrate Paleontology 28(3):656-663 [C. Sidor/B. Peecook]

Secondary references:

33223 J. Fröbisch. 2009. Composition and similarity of global anomodont-bearing tetrapod faunas. Earth-Science Reviews 95:119-157 [R. Butler/R. Butler]
35220 W. R. Hammer. 1995. New therapsids from the Upper Fremouw Formation of Antarctica. Journal of Vertebrate Paleontology 15:105-112 [R. Butler/R. Butler]
34461 C. F. Kammerer, J. J. Flynn, L. Ranivoharimanana and A. R. Wyss. 2010. The first record of a probainognathian (Cynodontia: Chiniquodontidae) from the Triassic of Madagascar. Journal of Vertebrate Paleontology 30(6):1889-1894 [R. Butler/R. Butler]
55307 C. A. Sidor, J. S. Steyer, and W. R. Hammer. 2014. A new capitosauroid temnospondyl from the Middle Triassic upper Fremouw Formation of Antarctica. 34:539-548 [C. Sidor/C. Sidor]
74294 N. D. Smith, P. J. Makovicky, C. A. Sidor and W. R. Hammer. 2020. A kannemeyeriiform (Synapsida: Dicynodontia) occipital plate from the Middle Triassic upper Fremouw Formation of Antarctica. Journal of Vertebrate Paleontology e1829634 [E. Dunne/E. Dunne/P. Mannion]
57427 R. Wang, S. Xu, X. Wu, C. Li, and S. Wang. 2013. A new specimen of Shansisuchus shansisuchus Young, 1964 (Diapsida: Archosauriformes) from the Triassic of Shanxi, China. Acta Geologica Sinica 87(5):1185-1197 [R. Butler/R. Butler]