FLMNH XJ-002 (1990 <4 mm) [Bowden Fm]: Late Pliocene, Jamaica
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Bivalvia
- Pholadida
- Corbulidae
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Corbula (Corbula) heterogena
(Guppy 1898)
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1 specimen | |||||||||
Gastropoda
- Opisthobranchiata
- Cavoliniidae
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Cavolinia vendryesiana
Ujihara 1996
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4 specimens | |||||||||
Cavolinia tridentata
(Niebuhr 1775)
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1 specimen | |||||||||
Cavolinia ventricosa
(Guppy 1882)
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3 specimens | |||||||||
Diacria trispinosa
(de Blainville 1821)
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1 specimen | |||||||||
Diacria digitata
(Guppy 1882)
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64 specimens | |||||||||
Clio pyramidata
Linnaeus 1767
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1 specimen | |||||||||
SUBSPECIES: C. pyramidata lanceolata | ||||||||||
Gastropoda
- Neogastropoda
- Columbellidae
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20 specimens | ||||||||||
see common names |
Geography
Country: | Jamaica |
Coordinates: | 17.9° North, 76.3° West (view map) |
Paleocoordinates: | |
Basis of coordinate: | estimated from map |
Geographic resolution: | small collection |
Time
Period: | Neogene | Epoch: | Pliocene |
Stage: | Piacenzian | 10 m.y. bin: | Cenozoic 6 |
Key time interval: | Late Pliocene | ||
Age range of interval: | 3.6 - 2.58 m.y. ago |
Stratigraphy
Geological group: | Coastal | Formation: | Bowden | ||
Stratigraphic resolution: | bed | ||||
Stratigraphy comments: STRATIGRAPHIC RELATIONS: From Pickerill et al. (1998). Bowden Formation is the uppermost stratigraphic unit of the Lower Coastal Group. The top of the formation is defined by the nonconformably overlying, early Pleistocene Old Pera Beds of the Upper Coastal Group. AGE: Late Pliocene. The unit was formely regarded as Miocene in age, even Oligocene, but foraminiferal and planktic gastropod biostratigraphy points to a late Pliocene age. THICKNESS: The formation has an extimated maximum thickness of 150m, although the basal part of the formation is unexposed. STRATIGRAPHIC POSITION: Unknown position within formation. COMMENTS: In its type area of the Bowden district, natural exposures of the formation are poor and discontinuous, so that a complete and detailed stratigraphy of the entire sequence cannot be determined. |
Lithology and environment
Primary lithology: | pebbly unlithified conglomeratic marl |
Includes fossils? | Y |
Lithology description: SPECIFIC LITHOLOGY: Imperfectly consolidated gravel consisting of pebbles and grains of igneous rocks, limestone, and other sorts of rock in a marly matrix. LITHIFICATION: Unlithified, based on observation of specimens. | |
Environment: | offshore |
Geology comments: ENVIRONMENT: The conglomeratic lithofacies are interpretated as a product of sediment gravity flows, more specifically turbidites, and constitute and integral component of the Bowden Shell bed. The marlstone lithofacies is interpreted as a product of pelagic and hemiplegaic deposition from low density turbidity currents, or possibly even bottom water nepheloid layers. |
Taphonomy
Modes of preservation: | body,original aragonite,original calcite |
Degree of concentration: | concentrated |
Size of fossils: | macrofossils |
Preservation of anatomical detail: | good |
Collection methods and comments
Collection methods: | bulk,sieve,field collection | ||
Minimum sieve size: | 1.000 | Maximum sieve size: | 4.000 |
Reason for describing collection: | paleoecologic analysis | ||
Museum repositories: | FMNH | ||
Collection method comments: COLLECTOR: R. Portell (1990). REPOSITORY: FLMNH. FIDELITY: High ecological fidelity. ASSOCIATED COLLECTIONS: Small (<4mm) split of XJ-002. | |||
Taxonomic list comments:TAXONOMY: Identified by R. Portell; nomenclature revised by A. Hendy. |
Metadata
Database number: | 69091 | ||
Authorizer: | A. Hendy | Enterer: | A. Hendy |
Modifier: | A. Hendy | Research group: | marine invertebrate |
Created: | 2007-02-17 20:40:21 | Last modified: | 2025-02-22 15:12:02 |
Access level: | authorizer only | Released: | 2008-02-17 20:40:21 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
19909. | A. J. W. Hendy, D. P. Buick, K. V. Bulinski, C. A. Ferguson, and A. I. Miller. 2008. Unpublished census data from Atlantic coastal plain and circum-Caribbean Neogene assemblages and taxonomic opinions. [A. Hendy/A. Hendy/A. Hendy] |