Los Espejos Formation, Facies B1, Cerro del Fuerte section: Ludlow, Argentina
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Trilobita
- Phacopida
- Phacopidae
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Phacops argentinus
Thomas 1905
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recombined as Paciphacops argentinus | |||||||
Trilobita
- Phacopida
- Dalmanitidae
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Dalmanites cf. sudamericanus
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Rhynchonellata
- Orthida
- Dalmanellidae
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Isorthis (Protocortezorthis) cuyanum
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Rhynchonellata
- Rhynchonellida
- Leptocoeliidae
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Harringtonina acutiplicata
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synonym of Anabaia | |||||||
Bivalvia
- Nuculanida
- Nuculanidae
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Anthracoleda (Pseudoleda) minuta
Sanchez et al. 1995
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see common names |
Geography
Country: | Argentina |
Coordinates: | 30.3° South, 68.8° West (view map) |
Paleocoordinates: | 45.6° South, 128.9° West |
Basis of coordinate: | based on nearby landmark |
Geographic resolution: | local area |
Time
Period: | Silurian | Epoch: | Ludlow |
10 m.y. bin: | Silurian 2 | ||
Key time interval: | Ludlow | ||
Age range of interval: | 427.40000 - 423.00000 m.y. ago |
Stratigraphy
Formation: | Los Espejos | ||||
Stratigraphic resolution: | member | ||||
Stratigraphy comments: Middle part of sequence, about 120 to 140 m thick. |
Lithology and environment
Primary lithology: | planar lamination,bioturbation mudstone |
Secondary lithology: | hummocky CS,wave ripples,tool marks,gray,green sandstone |
Lithology description: Hummocky cross-stratifried sandstones and mudstones..fine- to -medium-grained green-gray sst..in beds averaging 20-30 cm thick...beds commonly lenticular..some beds with sharp erosional bases...some beds with tool and scour marks and trace fossil casts..meandering sinuous trals (Torrowangeo, Cosmoraphe, Planolites)...sst beds oftern underlain by shell lag...wave ripple cross-lamination...horizontal plane lamination...mudstones extrensively bioturbated (Planolites, Chondrites)...otherwise parallel to low-angle internal lamination preserved... | |
Environment: | marine indet. |
Geology comments: Increase in thickness and frequency of storm layers in facies B1 relative to facies A may indicate change from distal to proximal tempestites...internal structure of SSt beds indicates proximal storm layers..other signs indicate deposition in nearshore shallow water, slightly below average storm wave base...Associated traces (Cruziana ichnofacies) suggest shallow shelf, below fair weather wave base. |
Taphonomy
Collection methods and comments
Reason for describing collection: | paleoecologic analysis |
Collection method comments: Coquina 9 in Table 2. |
Metadata
Database number: | 25054 | ||
Authorizer: | M. Foote | Enterer: | M. Foote |
Modifier: | M. Foote | Research group: | marine invertebrate |
Subset of collection #: | 25058 | ||
Created: | 2002-08-27 09:08:09 | Last modified: | 2006-09-15 15:14:05 |
Access level: | the public | Released: | 2002-08-27 09:08:09 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
7023. | T. M. Sanchez, B. G. Waisfeld, and J. L. Benedetto. 1991. Lithofacies, taphonomy, and brachiopod assemblages in the Silurian of western Argentina: A review of Malvinokaffric Realm communities. Journal of South American Earth Sciences 4(4):307-329 [M. Foote/M. Foote/O. Alfaro] |