Re #1193 - Cantaure Formation: Burdigalian, Venezuela

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
Chione (Lirophora) quirosensis Hodson 1927
Bivalvia - Ostreida - Ostreidae
Ostrea cf. portoricoensis (Hubbard 1920)
original and current combination Ostrea sellaeformis portoricoensis
Gastropoda - Neogastropoda - Buccinidae
Cymatophos cocoditoensis
Cymatophos paraguanensis (Hodson and Hodson 1931)
Gastropoda - Neogastropoda - Mitridae
Mitra (Tiara) quirosana
Gastropoda - Neogastropoda - Marginellidae
Prunum (Prunum) quirosense (Hodson 1927)
Gastropoda - Neogastropoda - Muricidae
Typhis (Laevityphis) sawkinsi Mansfield 1925
recombined as Siphonochelus (Laevityphis) sawkinsi
Gastropoda - Neogastropoda - Turridae
Knefastia aff. lavinoides (Olsson 1922)
synonym of Knefastia limonensis
Fusiturricula cf. jaquensis (Sowerby 1850)
Gastropoda - Neogastropoda - Borsoniidae
Borsonia (Paraborsonia) cantaurana
original and current combination Paraborsonia
Gastropoda - Sorbeoconcha - Turritellidae
Turritella cocoditana (Hodson 1926)
Gastropoda - Pyramidellidae
Turbonilla falconensis
see common names

Geography
Country:Venezuela State/province:Falcon
Coordinates: 11.9° North, 69.8° West (view map)
Paleocoordinates:11.2° North, 66.6° West
Basis of coordinate:based on nearby landmark
Geographic resolution:local area
Time
Period:Neogene Epoch:Miocene
Stage:Burdigalian 10 m.y. bin:Cenozoic 5
Key time interval:Burdigalian
Age range of interval:20.44000 - 15.97000 m.y. ago
Stratigraphy
Formation:Cantaure
Regional section:Paraguana
Stratigraphic resolution:group of beds
Stratigraphy comments: Clays, sandstone, and limestones of up to 75, thick, although no single section is completely exposed. Collection apparently derived from near middle part of that thickness. Overlies unconformably Cretaceous rocks and is conformably overlain by limestones on middle to upper Miocene. Jung (1965) regarded the collection as early Middle Miocene, though more recent authors, including Vermeij (2001) indicate an Early Miocene (Burdigalian) age. Formation formerly referred to as "Cerro Pelado".
Lithology and environment
Primary lithology:micaceous,shelly/skeletal unlithified silty claystone
Includes fossils?Y
Lithology description: Clay, massive, micaceous, slightly silty, and locally containing abundant fossils.
Environment:coastal indet.
Geology comments: Tropical shallow-water assemblage, neritic, no deep-water genera present, normal salinity, perhaps nearby brackish source.
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Collection excludes:all microfossils,some macrofossils,ichnofossils
Collection methods:selective quarrying,field collection
Reason for describing collection:taxonomic analysis
Museum repositories:BMNH,NMB,PRI,USNM
Collection method comments: All material is reposited in the Natural History Museum (NMB), Basel, Switzerland, with some voucher specimens in the British Museum, PRI, and USNM.
Taxonomic list comments:Exhaustive for Bivalvia and Gastropoda. Balanus, corals, numerous otoliths, and Calianassa fragments are commonly found, though not listed.
Metadata
Database number:60709
Authorizer:A. Hendy Enterer:A. Hendy
Research group:marine invertebrate
Created:2006-05-20 23:42:51 Last modified:2013-11-25 13:37:23
Access level:the public Released:2006-05-20 23:42:50
Creative Commons license:CC BY
Reference information

Primary reference:

17318. P. Jung. 1965. Miocene Mollusca from the Paraguana Peninsula, Venezuela. Bulletins of American Paleontology 49(223):389-652 [A. Miller/A. Hendy]