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Río Roble: Early/Lower Barremian, Argentina

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Malacostraca - Decapoda
Decapoda indet. Latreille 1802
Kellner et al. 2003
Cephalopoda - Ammonoidea - Oppeliidae
Sanmartinoceras africanum
Kellner et al. 2003
Subspecies: insignicostatum
Cephalopoda - Ammonoidea - Neocomitidae
Hatchericeras patagonense Stanton 1901
Kellner et al. 2003
unclassified
Cryptocrioceras yrigoyeni
Kellner et al. 2003
Reptilia - Pterosauria - Anhangueridae
? Anhangueridae indet. Campos and Kellner 1985
Kellner et al. 2003 2 specimens
MACN-SC 3617, ulna and isolated ?wing metacarpal
see common names
Geography
Country:Argentina State/province:Santa Cruz
Coordinates: 48.0° South, 72.0° West (view map)
Paleocoordinates:48.0° South, 35.5° West
Basis of coordinate:estimated from map
Geographic resolution:small collection
Time
Period:Cretaceous Epoch:Early/Lower Cretaceous
Stage:Barremian 10 m.y. bin:Cretaceous 2
Key time interval:Early/Lower Barremian Ammonoid zone: Hatchericeras patagonense
Age range of interval:130.0 - 125.0 m.y. ago
Stratigraphy
Formation:Río Belgrano
Stratigraphic resolution:bed
Stratigraphy comments: Early-Middle Barremian based upon ammonoids
Lithology and environment
Primary lithology:concretionary sandstone
Includes fossils?Y
Lithology description: "Green sandstones with parallel bedding, organised in coarsening up sequences, with green brownish shales at the base. Epidiagenetic red sandy concretions are common a few meters above the contact with the underlying Río Mayer Formation. Ammonoids, crustacean decapods and the pterosaur bones were found at this level"
Environment:coastal indet. Tectonic setting:back-arc basin
Geology comments: "A series of transgressive and regressive cycles from the Pacific sea characterises a retroarc basin where important accumulations of continental and marine deposits are recorded during the Cretaceous" "The green sandstones of the Río Belgrano Formation show the beginning of the marine regression in the area. Facies indicate the transition to a littoral near coast high energy environmental. The pterosaur remains were found in a near-shore environment, which to the top shows an even higher energy facies that finally changes to fluviatile continental facies."
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Preservation of anatomical detail:medium
Disassociated major elements:some
Disassociated minor elements:some
Fragmentation:frequent
Collection methods and comments
Collection methods:field collection
Reason for describing collection:taxonomic analysis
Museum repositories:MACN
Metadata
Database number:92232
Authorizer:R. Butler Enterer:R. Butler
Modifier:R. Butler Research group:vertebrate
Created:2009-11-04 01:46:11 Last modified:2009-11-04 03:52:56
Access level:the public Released:2009-11-04 01:46:11
Reference information
Primary reference:
30953 L. Codorniú and Z. Gasparini. 2007. Pterosauria. In Z. Gasparini, L. Salgado, R. A. Coria (eds.), Patagonian Mesozoic Reptiles. Indiana University Press, Bloomington, IN 143-166 [R. Butler/R. Butler]

Secondary references:

31074 A. W. A. Kellner, M. B. Aguirre-Urreta, and V. A. Ramos. 2003. On the pterosaur remains from the Río Belgrano Formation (Barremian), Patagonian Andes of Argentina. Anais da Academia Brasileira de Ciências 75(4):487-495 [R. Butler/R. Butler]