Four Corners Section - 19: Late/Upper Cenomanian, New Mexico
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Polychaeta
- Sabellida
- Serpulidae
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Serpula intrica
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4 individuals | ||||||
Cephalopoda
- Ammonitida
- Anisoceratidae
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Allocrioceras sp.
Spath 1926
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1 individual | ||||||
Bivalvia
- Solemyida
- Solemyidae
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Solemya obscura
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2 individuals | ||||||
Bivalvia
- Lucinida
- Lucinidae
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Lucina sp.
Bruguière 1797
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1 individual | ||||||
Bivalvia
- Ostreida
- Gryphaeidae
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Gryphaeostrea sp.
Conrad 1865
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1 individual | ||||||
Exogyra aff. acroumbonata
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3 individuals | ||||||
Pycnodonte aff. kellumi
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344 individuals | ||||||
Bivalvia
- Pectinida
- Plicatulidae
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Plicatula cf. ferryi
Coquand 1862
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31 individuals | ||||||
recombined as Plicatula (Plicatula) ferryi | |||||||
Bivalvia
- Myalinida
- Inoceramidae
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Inoceramus sp.
Sowerby 1814
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1 individual | ||||||
Gastropoda
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Gastropoda indet.
Cuvier 1795
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1 individual | ||||||
Gastropoda
- Turritellidae
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Turritella sp.
Lamarck 1799
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4 individuals | ||||||
see common names |
Geography
Country: | United States | State/province: | New Mexico | County: | San Juan |
Coordinates: | 36.5° North, 108.6° West (view map) | ||||
Paleocoordinates: | 37.3° North, 71.6° West | ||||
Basis of coordinate: | stated in text |
Time
Period: | Cretaceous | Epoch: | Late/Upper Cretaceous |
Stage: | Cenomanian | 10 m.y. bin: | Cretaceous 5 |
Key time interval: | Late/Upper Cenomanian | ||
Age range of interval: | 100.50000 - 93.90000 m.y. ago |
Stratigraphy
Formation: | Mancos | ||||
Stratigraphy comments: "to time equivalent [to the Upper Cenomanian Hartland Shale Member, Greenhorn Formation] proximal offshore deposits (prodelta and equivilants; Danke et al.,1993) of the Tropic and Mancos Shales (Utah and Arizona; Fig. 2)." |
Lithology and environment
Primary lithology: | burrows lithified "shale" | ||
Includes fossils? | Y | ||
Lithology description: Tropic and Mancos Shales | |||
Environment: | prodelta | Tectonic setting: | foreland basin |
Geology comments: "proximal offshore deposits (prodelta and equivilants; Danke et al.,1993) ... During the Cenomanian and Turonian, foreland basin subsidence and tectonoeustatic sea-level rise resulted in widespread flooding of the Western Interior U.S." |
Taphonomy
Modes of preservation: | body,mold/impression,original aragonite,original calcite |
Size of fossils: | macrofossils,mesofossils,microfossils |
Spatial orientation: | random |
Preservation of anatomical detail: | good |
Associated major elements: | some |
Disassociated major elements: | many |
Fragmentation: | frequent |
Temporal resolution: | condensed |
Spatial resolution: | parautochthonous |
Collection methods and comments
Collection methods: | bulk,field collection |
Reason for describing collection: | paleoecologic analysis |
Metadata
Database number: | 44282 | ||
Authorizer: | L. Ivany | Enterer: | P. Wall |
Modifier: | M. Clapham | Research group: | marine invertebrate |
Created: | 2004-09-08 09:23:55 | Last modified: | 2017-08-01 20:01:11 |
Access level: | the public | Released: | 2004-09-08 09:23:55 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
11587. | B. S. Sageman and C. R. Bina. 1997. Diversity and Species Abundance Patterns in Late Cenomanian Black Shale Biofacies, Western Interior, U.S. Palaios 12:449-466 [L. Ivany/P. Wall/P. Wall] |