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El Breal de Orocual 2 (Pleistocene to of Venezuela)

Where: Monagas, Venezuela (9.8° N, 63.3° W: paleocoordinates 9.8° N, 63.1° W)

• coordinate stated in text

• local area-level geographic resolution

When: Mesa Formation, Early/Lower Pleistocene to Early/Lower Pleistocene (2.6 - 0.1 Ma)

• The Mesa Formation is early to middle Pleistocene age, based on thermoluminescence dates of 0.5 to 1.0 Ma (Carbón et al., 1992).

• formation-level stratigraphic resolution

Environment/lithology: fluvial-deltaic; lithology not reported and tar

• The faunal assemblage suggests that the El Breal de Orocual paleoenvironment were savannahs.
• This deposit has been interpreted as a tar seep deposit lying in the Mesa Formation (Hackley et al., 2006), a unit that consists of fluvio-deltaic strata.

Size class: mesofossils

Collection methods: Museum repositories: Instituto Venezolano de Investigaciones Cientificas

Primary reference: E. C. Holanda and A. D. Rincon. 2012. Tapirs from the Pleistocene of Venezuela. Acta Palaeontologica Polonica 53(3):463-473 [C. Jaramillo/M. Vallejo/A. Cardenas ] more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 147081: authorized by Carlos Jaramillo, entered by Maria Vallejo on 05.07.2013

Creative Commons license: CC BY (attribution)