Agua de la Mula plesiosar locality, Hoplitocrioceras gentilii subzone: Early Hauterivian, Argentina

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia - Plesiosauria - Elasmosauridae
Elasmosauridae indet. Cope 1869
23 elements
PV-6893/1-23- MOZ: 23 dissarticulated vertebrae (18 cervicals, four dorsals, and one caudal) and other undetermined bone fragments of the postcranial skeleton
see common names

Geography
Country:Argentina State/province:Neuquén
Coordinates: 38.0° South, 70.0° West (view map)
Paleocoordinates:37.5° South, 33.9° West
Basis of coordinate:based on nearby landmark
Geographic resolution:small collection
Time
Period: Cretaceous Epoch: Early Cretaceous
Stage: Hauterivian 10 m.y. bin: Cretaceous 2
Key time interval: Early Hauterivian Ammonoid zone:  Hoplitocrioceras gentilii
Age range of interval: 132.6 - 125.77 m.y. ago
Stratigraphy
Formation:Agrio Member:Lower
Stratigraphic resolution:bed
Stratigraphy comments: "Hoplitocrioceras gentilii subzone, Hoplitocrioceras gentilii zone"
Lithology and environment
Primary lithology:black,gray lithified mudstone
Secondary lithology:tabular,shelly/skeletal lithified "limestone"
Lithology description: "Three facies were recognized. The first one consists of black and gray mudrocks, and appears only at the base of the section. It was probably deposited in a low energy offshore subenvironment, under the stormweather wave base. Intercalated mudrocks and fossiliferous limestones compose the second facies. The limestones are tabular, 0.5 m thick in average, and comprise reworked and fragmented fauna, including plesiosaur remains PV-6894/1-2-MOZ. They were interpreted as storm deposits. The mudrocks represent pelagic background sediments and contained most of the plesiosaur remains studied in this paper (PV-6890/1-10-MOZ, PV-6891-MOZ, PV-6892-MOZ, and PV-6893/1-23-MOZ). This facies has been interpreted as a transitional subenvironment, between the fairweather and the stormweather wave base. The last facies consists mainly of heterolithic sandstones and amalgamated coquinas, and occurs at the top of shallowing-up cycles that begin with facies two. It contains reworked mollusks and corals, and a diverse assemblage of trace fossils. It represents a lower to upper shoreface subenvironment, between low tide level and fairweather wave base."
Environment:transition zone/lower shoreface
Geology comments: "In agreement with Spalletti (1992) and Brinkmann (1994), the Lower Member of the Agrio Formation was interpreted as deposited in a relatively shallow and warm marine environment (offshore to upper shoreface) under periodical storm
influence."
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Spatial orientation:random
Preservation of anatomical detail:poor
Abundance in sediment:rare
Disassociated major elements:some
Fragmentation:occasional
Spatial resolution:parautochthonous
Collection methods and comments
Collection excludes:some macrofossils
Collection methods:surface (in situ),field collection
Collection size:23 specimens
Reason for describing collection:general faunal/floral analysis
Collection method comments: "The described and figured material is deposited in the following collection under the catalogue number listed in the text: Museo Juan Olsacher. Dirección General de Minería de la Provincia de Neuquén. Olascoaga 421, Zapala (8340), Neuquén, Argentina."
Metadata
Database number:102088
Authorizer:M. Carrano Enterer:H. Street
Modifier:F. Aspromonte Research group:vertebrate
Created:2011-01-08 08:03:39 Last modified:2023-11-07 17:05:18
Access level:the public Released:2011-01-08 08:03:39
Creative Commons license:CC BY
Reference information

Primary reference:

34690. D. G. Lazo and M. Cichowolski. 2003. First plesiosaur remains from the Lower Cretaceous of the Neuquen Basin, Argentina. Journal of Paleontology 77(4):784-789 [M. Carrano/H. Street/F. Aspromonte]

Secondary references:

86336 J. P. O'Gorman, D. G. Lazo, L. Luci, C. S. Cataldo, E. Schwarz, M. Lescano, and M. B. Aguirre-Urreta. 2015. New plesiosaur records from the Lower Cretaceous of the Neuquén Basin, west-central Argentina, with an updated picture of occurrences and facies relationships. Cretaceous Research 56:372-387 [E. Vlachos/F. Aspromonte]