Punta la Colorada: Zanclean, Ecuador

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Chondrichthyes - Carcharhiniformes - Galeocerdidae
Galeocerdo aduncus (Agassiz 1835)
Chondrichthyes - Carcharhiniformes - Hemigaleidae
Hemipristis serra Agassiz 1835
Chondrichthyes - Carcharhiniformes - Carcharhinidae
Carcharhinus sp. de Blainville 1816
Carcharhinus priscus Agassiz 1843
Carcharhinus egertoni Agassiz 1843
Negaprion eurybathrodon (Blake 1862)
Chondrichthyes - Lamniformes - Carchariidae
Odontaspis acutissima (Agassiz 1843)
recombined as Carcharias acutissimus
Chondrichthyes - Lamniformes - Otodontidae
Carcharocles megalodon (Agassiz 1835)
recombined as Otodus megalodon
Also studied in Pimiento and Balk
Chondrichthyes - Dalatiidae
Isistius triangulus (Probst 1879)
original and current combination Scymnus triangulus
see common names

Geography
Country:Ecuador State/province:Esmeraldas
Coordinates: 0.6° South, 80.5° West (view map)
Paleocoordinates:0.8° South, 79.7° West
Basis of coordinate:stated in text
Geographic resolution:outcrop
Time
Period:Neogene Epoch:Pliocene
Stage:Zanclean 10 m.y. bin:Cenozoic 6
Key time interval:Zanclean
Age range of interval:5.33300 - 3.60000 m.y. ago
Age estimate:5.33 to 3.4 Ma (other)
Stratigraphy
Formation:Onzole Member:Upper
Stratigraphic resolution:bed
Stratigraphy comments: Age after Boessenecker et al., 2019.
Onzole Fm. considered Miocene in Longbottom (1979). Most recently, Punta La Colorada locality has been considered Pliocene by Cione et al. 2007, based on Aalto and Miller, 1999.
Lithology and environment
Primary lithology: not reported
Environment:marine indet.
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Collection excludes:some genera
Reason for describing collection:taxonomic analysis
Museum repositories:BMNH
Taxonomic list comments:Originally proposed to occur in transitional strata between Borbon and Onzole Fms. (Longbottom, 1979). Both were formerly considered Miocene. Most recently, they have been propose to be Pliocene (Aalto and Miller, 1999).
Metadata
Also known as:CRB123
Database number:151705
Authorizer:C. Jaramillo Enterer:C. Pimiento
Modifier:M. Uhen
Created:2013-10-10 16:30:48 Last modified:2019-02-19 12:45:49
Access level:the public Released:2013-10-10 16:30:48
Creative Commons license:CC BY
Reference information

Primary reference:

48478. A. E. Longbottom. 1979. Miocene Sharks' teeth from Ecuador. Bulletin of The British Museum (Natural History) Geology 32:57-70 [C. Jaramillo/C. Pimiento]

Secondary references:

11138 K. R. Aalto and W. Miller. 1999. Sedimentology of the Pliocene Upper Onzole Formation, an inner-trench slope succession in northwestern Ecuador. Journal of South American Earth Sciences 12:69-85 [A. Miller/A. Hendy/A. Hendy]
13595 R. W. Boessenecker, D. J. Eheret, D. J. Long, M. Churchill, E. Martin and S. J. Boessenecker. 2019. The Early Pliocene extinction of the mega-toothed shark Otodus megalodon: a view from the eastern North Pacific. PeerJ 7:e6088 [M. Uhen/M. Uhen/M. Uhen]
49081 C. Pimiento and M. Balk. 2015. The extinct giant shark Carcharocles megalodon: A model for understanding deep-time body size trends of marine apex predators. [C. Jaramillo/C. Pimiento/C. Pimiento]