south side of the Quebrada La Pola, Eastern flank of Sierra de Villicum: Caradoc, Argentina
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Pterobranchia
- Graptoloidea
- Dicranograptidae
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Dicranograptus aff. ramosus
(Hall 1847)
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Bivalvia
- Nuculanida
- Malletiidae
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Concavoleda braulense n. gen., n. sp.
Sanchez 1999
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4 specimens | |||||||||
Spec. #s: CEGH-UNC 16714a (holotype), 16153d, 17361d, 16780b (2 measurements) | ||||||||||
Bivalvia
- Nuculida
- Praenuculidae
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Praenucula sp.
Pfab 1934
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1 specimen | |||||||||
Spec. #: CEGH-UNC 16170b (1 measurement) | ||||||||||
Trigonoconcha acuta n. gen., n. sp.
Sanchez 1999
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13 specimens | |||||||||
Spec. #s: CEGH-UNC 16158 (holotype), 16153b, 16153c, 16159, 16160, 16161a, 16162, 16163, 16167b, 16172d, 16715b, 16756b, 16715b (6 measurements) | ||||||||||
Villicumia canteraensis n. gen., n. sp.
Sanchez 1999
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9 specimens | |||||||||
Spec. #s: CEGH-UNC 16152a (holotype), 16153a, 16154, 16155a, 16156, 16157, 16172c, 16772b, 17361b (6 measurements) | ||||||||||
Cuyopsis symmetricus n. gen., n. sp.
Sanchez 1999
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9 specimens | |||||||||
Spec. #s: CEGH-UNC 16719 (holotype), 16155b, 16720, 16721, 16756c, 17357, 17358, 17362b, 17364 (5 measurements) | ||||||||||
Concavodonta ovalis n. sp.
Sanchez 1999
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7 specimens | |||||||||
Spec. #'s: CEGH-UNC 16168 (holotype), 16166, 16169, 17351, 17352, 17353, 17356 [entered as Cocavodonta ovalis] (4 measurements) | ||||||||||
Emiliania cuerdai n. gen., n. sp.
Sanchez 1999
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9 specimens | |||||||||
Spec. #: CEGH-UNC 16164a, 16161b, 16165, 16170a, 16756d, 16767b, 17354, 17355, 17361c (7 measurements) | ||||||||||
1 specimen | ||||||||||
Spec. #: CEGH-UNC 16172b (1 measurement) | ||||||||||
Hemiconcavodonta minuta n. gen., n. sp.
Sanchez 1999
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6 specimens | |||||||||
Spec. #s: CEGH-UNC 16171 (holotype), 16152b, 16172a, 16714b, 16777b, 17363 (5 measurements) | ||||||||||
Bivalvia
- Actinodontida
- Cycloconchidae
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Cycloconchidae indet.
Ulrich 1884
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4 specimens | |||||||||
Spec. #s: CEGH-UNC 16718, 16716, 16717, 17350 | ||||||||||
Sánchez et al. 2003 | ||||||||||
Rhynchonellata
- Orthida
- Draboviidae
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? Drabovia sp.
Havlicek 1950
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Rhynchonellata
- Orthida
- Dalmanellidae
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Rhynchonellata
- Orthida
- Hesperorthidae
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Hesperorthis sp.
Schuchert and Cooper 1931
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Rhynchonellata
- Orthida
- Plaesiomyidae
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Dinorthis sp.
Hall and Clarke 1892
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Strophomenata
- Strophomenida
- Leptellinidae
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Strophomenata
- Strophomenida
- Aegiromenidae
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see common names |
Geography
Country: | Argentina | State/province: | San Juan |
Coordinates: | 31.3° South, 68.5° West (view map) | ||
Paleocoordinates: | 31.6° South, 170.2° East (Wright 2013) | ||
Geographic resolution: | outcrop |
Time
Period: | Ordovician | Epoch: | Late Ordovician |
10 m.y. bin: | Ordovician 4-5 | ||
*Period: | Late/Upper Ordovician | ||
*International age/stage: | Early/Lower Caradocian | ||
Key time interval: | Caradoc | Graptolite zone: | Climacograptus bicornis |
Age range of interval: | 458.2 - 449.5 m.y. ago | ||
* legacy (obsolete) database fields |
Stratigraphy
Formation: | La Cantera | Member: | Upper | ||
Stratigraphic resolution: | formation | ||||
Stratigraphy comments: Villas (1995) notes that the clasts containing fossils probably originated from the underlying La Cantera formation. The upper half is Climacograptus bicornis zone, the lower half is Hustedograptus teretiusculus zone. |
Lithology and environment
Primary lithology: | pebbly conglomerate |
Lithology description: Fossils described come from the upper part of the lower member of the Don Braulio Fm. The lower member (8-12 m) is composed of pebbly mudstones capped by channelized conglomerates. This succession is interpretted as a diamictite. Studied fossils have come from coquinites in the diamictite. | |
Environment: | marine indet. |
Geology comments: "Fossils described in this paper come from pebbles of the upper part of the lower diamictite member of the Don Braulio Fm. Clasts consist of sandstones, limestones, quatzites, quartz, and volcanic rocks, some of them being striated and facetted. This succession is interpretted as glacimarine in origin and is synchronous with the Late Ashgillian world-wide glaciation event." |
Taphonomy
Modes of preservation: | body,cast |
Degree of concentration: | concentrated |
Size of fossils: | macrofossils,mesofossils |
Spatial orientation: | random |
Preservation of anatomical detail: | good |
Fragmentation: | frequent |
Temporal resolution: | time-averaged |
Collection methods and comments
Collection excludes: | some genera,some macrofossils,some microfossils |
Collection methods: | chemical,field collection |
Reason for describing collection: | taxonomic analysis |
Collection method comments: "In order to enhance exposure of teeth and muscle scars, shells were dissolved with hydrochloric acid (10%). |
Metadata
Database number: | 13513 | ||
Authorizer: | A. Miller, P. Wagner | Enterer: | R. Krause, P. Wagner |
Modifier: | P. Wagner | Research group: | marine invertebrate |
Created: | 2002-04-10 12:21:02 | Last modified: | 2025-02-22 15:12:02 |
Access level: | the public | Released: | 2002-04-10 12:21:02 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
6121. | T. M. Sanchez. 1999. New late Ordovician (Early Caradoc) Bivalves from the Sierra De Villicum (Argentine Precordillera). Journal of Paleontology 73(1):66-76 [A. Miller/R. Krause/P. Wagner] |
Secondary references:
86266 | T. M. Sánchez, L. Marengo, and R. A. Astini. 2003. Late Ordovician Bivalvia Heteroconchia (Cycloconchidae and Glyptarcidae) from western Argentina. Ameghiniana 40(3):433-440 [P. Wagner/P. Wagner] |