Kinney Quarry, Manzanita Mountains, unit 2: Virgilian, New Mexico
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Chondrichthyes
- Acanthodiformes
- Acanthodidae
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Acanthodes kinneyi n. sp.
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Zidek 1992 | |||||||||
NMMNH P-19208; paratypes CM 47842a, b; USNM 187147; OMNH 00447, 00448, 00449 | ||||||||||
Eurynotiformes
- Amphicentridae
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Amphicentrum jurgenai n. sp.
Zidek 1992
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Zidek 1992 | |||||||||
holotype: CM 47845a, b; paratypes CM 47843a, b, CM 47844a, b, CM 47846, NMMNH P-19112a, b, P-19116, KUVP 86170a, b | ||||||||||
Palaeonisciformes
- Platysomidae
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Platysomus schultzei n. sp.
Zidek 1992
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Zidek 1992 | |||||||||
holotype: NMMNH P-19195; paratypes: CM 47832, 47836, 47840a, b, KUVP 86176, NMMNH P-19114, P-19117a, b, P-19194a, b | ||||||||||
Gastropoda
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Gastropoda indet.
Cuvier 1795
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high-spired | ||||||||||
Bivalvia
- Pectinida
- Pterinopectinidae
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Dunbarella sp.
Newell 1938
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Feldman et al. 1992 | |||||||||
unclassified
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Fish indet.
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Lorenz et al. 1992 | |||||||||
one of the main horizons; highest concentration off well-preserved, articulated fish | ||||||||||
Plantae indet.
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Lorenz et al. 1992 | |||||||||
terrestrial, rare | ||||||||||
Ostracoda
- Podocopida
- Cyprididae
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? Carbonita sp.
Strand 1928
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Kietzke and Kaesler 1992 | |||||||||
Ostracoda
- Podocopida
- Darwinulidae
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? Darwinula sp.
Brady and Robertson 1885
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Kietzke and Kaesler 1992 | |||||||||
Ostracoda
- Palaeocopida
- Knoxitidae
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Geisina gregaria
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Kietzke and Kaesler 1992 | |||||||||
Branchiopoda
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Branchiopoda indet.
Latreille 1817
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Feldman et al. 1992 | |||||||||
Conchostraca indet.
(Sars 1867)
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Biseriamminidae
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Globivalvulina sp.
Schubert 1921
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Kietzke and Kaesler 1992 | |||||||||
see common names |
Geography
Country: | United States | State/province: | New Mexico | County: | Bernalillo |
Coordinates: | 34.9° North, 106.3° West (view map) | ||||
Paleocoordinates: | 0.4° South, 36.9° West | ||||
Basis of coordinate: | estimated from map |
Time
Period: | Carboniferous | Epoch: | Pennsylvanian |
Stage: | Gzhelian | 10 m.y. bin: | Carboniferous 5 |
Key time interval: | Virgilian | ||
Age range of interval: | 303.7 - 298.9 m.y. ago |
Stratigraphy
Formation: | Wild Cow | Member: | Pine Shadow | ||
Stratigraphy comments: Wild Cow Formation, which is composed of rhythmic sequences of arkosic sandstone, gray, tan, and red shale, and gray marine limestone of Missourian to earliest Wolfcamian age. Myers (1973, 1988) recognized three members of the Wild Cow, in ascending order Sol de Mete, Pine Shadow, and La Casa. About 28 m of the Pine Shadow Member (lower Virgilian) are exposed in the Kinney Quarry... the member consiste generally of gray marine limstones alternating with marine or nonmarine shale, sandstone, and conglomerate. Lateral facies changes within the Pine Shadow Member are pronounced...early Virgilian age is based on studies of fusulinids. |
Lithology and environment
Primary lithology: | "limestone" |
Includes fossils? | Y |
Lithology description: Thickness: 0.1 m Fig. 5: shaly limestone; olive black (5 Y 2/1), mottled and streaked grayish orange (10 YR 7/4); well indurated; highly fossiliferous text: basal limestone becomes more platy to laminar, and more argillaceous through an interval of approx. 10 cm, most major elements of the limestone fauna disappear through this transition zone and are absent from the overlying shale (unit 3) ref #75170: clayey, laminated micrite; organic-rich ref #75181: thickness ranges from 6-14 cm; well laminated throughout, breaks readily along these laminations, laminations not truncated by burrow, some laminations are crudely graded from microspar and shell hash at base to organic-rich micrite at top | |
Environment: | lagoonal/restricted shallow subtidal |
Geology comments: deposition in conditions of lowered salinity; deposition occurred in quiet, possibly oxygen-poor waters with restricted circulation; conection with normal marine environments persisted
ref #75181: increasing dominance of rapid siliciclastic deposition in a tidal environment ref #75238: ostracods are characteristic of a mixed mear-shore -marine and brackish-water fauna that appears to have become less marine above the basal limestone |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils,mesofossils |
Collection methods and comments
Reason for describing collection: | general faunal/floral analysis |
Metadata
Database number: | 216992 | ||
Authorizer: | B. Seuss | Enterer: | B. Seuss |
Modifier: | B. Seuss | Research group: | marine invertebrate,paleobotany,vertebrate |
Created: | 2021-01-12 05:38:04 | Last modified: | 2021-01-21 01:57:16 |
Access level: | the public | Released: | 2021-01-12 05:38:04 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
75139. | B.S. Kues and S.G. Lucas. 1992. Overview of Upper Pennsylvanian stratigraphy and paleontology, Kinney Quarry, Manzanita Mountains, New Mexico. New Mexico Bureau of Mines & Mineral Resources, Bulletin 138:1-11 [B. Seuss/B. Seuss/B. Seuss] |
Secondary references:
75181 | H.R. Feldman, A.W. Archer, R.R. West and C.G. Maples. 1992. The Kinney Brick Company Quarry: Preliminary analysis using an estuarine depositional model. New Mexico Bureau of Mines & Mineral Resources, Bulletin 138:21-26 [B. Seuss/B. Seuss/B. Seuss] | |
75238 | K.K. Kietzke and R.L. Kaesler. 1992. Late Pennsylvanian Ostracoda from the Kinney Brick Quarry, Bernalillo County, New Mexico, with notes on other microfossils. New Mexico Bureau of Mines & Mineral Resources, Bulletin 138:127-133 [B. Seuss/B. Seuss/B. Seuss] | |
75170 | J.C. Lorenz, G.A. Smith, and S.G. Lucas. 1992. Sedimentary patterns in Pennsylvanian strata at the Kinney Brick Company Quarry, Bernalillo County, New Mexico. New Mexico Bureau of Mines & Mineral Resources, Bulletin 138:13-19 [B. Seuss/B. Seuss/B. Seuss] | |
75240 | J. Zidek. 1992. Late Pennsylvanian Chondrichthyes, Acanthodii, and deep-bodied Actinopterygii from the Kinney Quarry, Manzanita Mountains, New Mexico. New Mexico Bureau of Mines & Mineral Resources, Bulletin 138:145-181 [B. Seuss/B. Seuss/B. Seuss] |