Lasiocrinus Assoc., Thacher Mbr., Manlius Fm., Cementon, NY: Lochkovian, New York
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
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Crinoidea
- Dendrocrinida
- Mastigocrinidae
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Lasiocrinus scoparius
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Crinoidea
- Monobathrida
- Scyphocrinitidae
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Scyphocrinites sp.
Zenker 1833
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| "transported?" | ||||||||||
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Stylophora
- Mitrata
- Anomalocystitidae
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Anomalocystites sp.
Hall 1858
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Bivalvia
- Pterioida
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Pterioida indet.
Newell 1965
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Tentaculitida
- Tentaculitidae
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Tentaculites sp.
von Schlotheim 1820
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Strophomenata
- Strophomenida
- Amphistrophiidae
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Mesodouvillina varistriata
(Conrad 1842)
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Rhynchonellata
- Spiriferida
- Delthyrididae
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Howellella vanuxemi
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unclassified
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Bryozoa indet.
Ehrenberg 1831
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| ramose and encrusting forms | ||||||||||
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Ostracoda
- Leperditicopida
- Leperditiidae
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Leperditiidae indet.
Jones 1856
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| see common names | ||||||||||
Geography
| Country: | United States | State/province: | New York |
| Coordinates: | 42.1° North, 73.9° West (view map) | ||
| Paleocoordinates: | 35.7° South, 33.4° West | ||
| Basis of coordinate: | based on political unit | ||
| Geographic resolution: | local area |
Time
| Period: | Devonian | Epoch: | Early/Lower Devonian |
| Stage: | Lochkovian | 10 m.y. bin: | Devonian 1 |
| *International age/stage: | Early/Lower Lochkovian | ||
| Key time interval: | Lochkovian | ||
| Age range of interval: | 419.20000 - 410.80000 m.y. ago | ||
| * legacy (obsolete) database fields | |||
Stratigraphy
Lithology and environment
| Primary lithology: | grainstone | ||
| Secondary lithology: | argillaceous lime mudstone | ||
| Includes fossils? | Y | ||
| Lithology description: "Lasiocrinus occur in interbedded 'ribbon limestone' facies; typically found on bedding planes of thin (2-4 cm) lamintaed calcisiltite beds interbedded with fine-grained argillaceous lime mudstone and shale layers" | |||
| Environment: | lagoonal/restricted shallow subtidal | Tectonic setting: | foreland basin |
| Geology comments: "The Manlius has bee interpreted as peritidal to lagoonal. Desiccation cracks,, birdseye (fenestral) fabric; cryptalgal laminites and intraclast conglomerates...portions upper intertidal to supratidal...Ribbon limestones interpretd as storm silt and fine sand layers washed into a 'lagoonal' environment: the latter situated between carbonate tidal flats and offshore shoal settings...A nearshore, somewhat unstable silty environment, is indicated; generally low energy background conditions interrupted by frequent storm events...BA 2"
2003:05:03 SEP environmental call based on given description | |||
Taphonomy
Collection methods and comments
| Reason for describing collection: | paleoecologic analysis |
Metadata
| Database number: | 26689 | ||
| Authorizer: | M. Foote | Enterer: | M. Foote |
| Modifier: | S. Peters | Research group: | marine invertebrate |
| Created: | 2002-10-24 08:14:43 | Last modified: | 2003-05-03 15:15:53 |
| Access level: | the public | Released: | 2002-10-24 08:14:43 |
| Creative Commons license: | CC BY |
Reference information
Primary reference:
| 4379. | T. J. Frest, C. E. Brett, and B. J. Witzke. 1999. Caradocian-Gedinnian echinoderm associations of Central and Eastern North America. Paleocommunities--a case study from the Silurian and Lower Devonian 638-783 [M. Foote/K. Koverman/P. Wagner] |