Where: Venezuela (10.7° N, 71.6° W: paleocoordinates 8.2° N, 64.2° W)
• coordinate based on nearby landmark
• small collection-level geographic resolution
When: Pauji Formation, Bartonian (41.3 - 38.0 Ma)
• STRATIGRAPHIC RELATIONS: From the Las Flores Fm, correlative with the upper part of the Pauji Formation in the correlation chart of Sutton (1946). The Pauji Formation appears to be the name used in the Maracaibo Basin now. AGE: In the Río San Pedro Section, nannofossils indicate an undifferentiated Middle Eocene age (NP15-NP16; Lutetian) for the base of the Pauji Formation. Planktonic foraminifera are characteristic of the late Middle Eocene Truncorotaloides Zone (Walton, 1966 in L.E.V., 1999). According to Medina (2008), On the basis of Turborotalia cerroazulensis and Truncorotaloides rohri a Middle Eocene Age (Zones P11/P14 of Bolli & Saunders 1985 - mid-Lutetian to mid-Bartonian) has been determined. STRATIGRAPHIC POSITION: From thin sandstone bed in unknown part of formation.
• bed-level stratigraphic resolution
Environment/lithology: marine; lithified, ferruginous sandstone
Size class: macrofossils
Preservation: cast, mold/impression
Collected by Sutton, Furnish; reposited in the PRI, SUI, UCMP
Collection methods: surface (in situ),
• COLLECTORS: Possibly Sutton, ~ early 1940's. REPOSITORY: State University of Iowa; University of California.
Primary reference: A. K. Miller and C. Collinson. 1951. A new species of Hercoglossa from Maracaibo. Journal of Paleontology 25(3):377-379 [A. Hendy/A. Hendy]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 82031: authorized by Austin Hendy, entered by Austin Hendy on 20.07.2008
Creative Commons license: CC BY (attribution)
Taxonomic list
Cephalopoda | |
Hercoglossa maracaiboensis Miller and Collinson 1951 nautiloid SUI 9541, SUI 9542, SUI 9543, PRI 20135, UCMP 31282
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