Kinney Quarry bivalve-lingula faunal assemblage: Kasimovian, New Mexico
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
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Bryozoa indet.
Ehrenberg 1831
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Strophomenata
- Strophomenida
- Rugosochonetidae
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Chonetinella flemingi
Dunbar and Condra 1932
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Strophomenata
- Orthotetida
- Derbyiidae
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Derbyia sp.
Waagen 1884
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Strophomenata
- Productida
- Productellidae
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Antiquatonia sp.
Miloradovich 1945
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Strophomenata
- Productida
- Linoproductidae
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Linoproductus sp.
(Chao 1927)
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Rhynchonellata
- Athyridida
- Athyrididae
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Composita subtilita
(Hall 1852)
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Lingulata
- Lingulida
- Lingulidae
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Lingula carbonaria
Shumard and Swallow 1858
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Cephalopoda
- Ammonoidea
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Ammonoidea indet.
Zittel 1884
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Cephalopoda
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Nautiloidea indet.
Agassiz 1847
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Bivalvia
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Bivalvia indet.
Linnaeus 1758
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Bivalvia
- Arcida
- Parallelodontidae
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? Parallelodon sp.
Meek and Worthen 1866
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Bivalvia
- Ostreida
- Pterineidae
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Leptodesma (Leptodesma) sp.
Hall 1883
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Bivalvia
- Pectinida
- Streblochondriidae
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? Streblochondria sp.
Newell 1938
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Bivalvia
- Pectinida
- Pterinopectinidae
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Dunbarella striata
(Stevens 1858)
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Bivalvia
- Pectinida
- Aviculopectinidae
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Aviculopecten basilicus
Newell 1938
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[entered as Aviculopectin basilicus] | ||||||||||
Bivalvia
- Myalinida
- Myalinidae
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Myalina aff. wyomingensis
(Lea 1853)
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Bivalvia
- Solemyida
- Solemyidae
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Clinopistha levis
(Meek and Worthen 1870)
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Solemya trapezoides
(Meek 1874)
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Solemya radiata
(Meek and Worthen 1860)
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Gastropoda
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Gastropoda indet.
Cuvier 1795
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High-spired | ||||||||||
Gastropoda
- Murchisoniina
- Gosseletinidae
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Glabrocingulum (Glabrocingulum) sp.
Thomas 1940
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Gastropoda
- Bellerophontida
- Euphemitidae
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Euphemites sp.
Warthin 1930
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Ostracoda
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Ostracoda indet.
Latreille 1802
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unclassified
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Conchostaca indet.
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Crinoidea
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Crinoidea indet.
Miller 1821
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Stems | ||||||||||
see common names |
Geography
Country: | United States | State/province: | New Mexico | County: | Bernalillo County |
Coordinates: | 34.8° North, 106.3° West (view map) | ||||
Paleocoordinates: | 1.3° South, 37.8° West | ||||
Basis of coordinate: | estimated from map | ||||
Geographic resolution: | outcrop |
Time
Period: | Carboniferous | Epoch: | Pennsylvanian |
Stage: | Kasimovian | 10 m.y. bin: | Carboniferous 5 |
Key time interval: | Kasimovian | ||
Age range of interval: | 307 - 303.7 m.y. ago |
Stratigraphy
Geological group: | Madera | Formation: | Wild Cow | Member: | Pine Shadow |
Local section: | Kinney Quarry | Local bed: | 1 | ||
Local order: | bottom to top | ||||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: The section of the quarry is part of the Pine Shadow Member of the Wild Cow Formation, Madera Group. The entire member has an average thickness of 70m in the Manzanita/Manzano Mountains, and has been reliably dated a s early to middle Virgilian on the basis of fusulinids described from localities elsewhere in these mountains. The dark limestone containing the marine fauna discussed here forms the floor of the quarry and is the basal unit (unit 1) of the stratigraphic section exposed in the quarry. Total thickness of this limestone unit is not known; it does not crop out significantly in areas immediately around the quarry. About 0.5 m is exposed in the quarry, and the upper 20 to 30 cm are widely present there. According to Lucas et al., 2011: The Kinney conodont fauna is characterized by Idiognathodus corrugatus and I. cherryvalensis, which suggest an assignment to the Idiognathodus confragus Zone of the North America Midcontinent region (Dennis cyclothem; middle Missourian). |
Lithology and environment
Primary lithology: | micaceous,black,gray lithified argillaceous "limestone" |
Includes fossils? | Y |
Lithology description: The limestone is a hard, dense, splintery, dark-gray to black, argillaceous micrite rich in organic material and producing a faintly fetid odor when broken. it becomes platy to laminated and less clacareous through a 10 cm thick transitional zone (unit 2), above which the lithology becomes a soft, fissile, brown to gray shale with little calcium carbonate. Most of the characteristic marine invertebrates of the basal limestone disappear rather abruptly through the transition zone. | |
Environment: | lagoonal/restricted shallow subtidal |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Collection methods and comments
Collection excludes: | difficult macrofossils |
Collection methods: | field collection |
Reason for describing collection: | taxonomic analysis |
Metadata
Also known as: | Kinney Quarry, basal limestone | ||
Database number: | 41988 | ||
Authorizer: | J. Alroy | Enterer: | C. Simpson |
Modifier: | M. Clapham | Research group: | marine invertebrate |
Created: | 2004-07-22 12:27:20 | Last modified: | 2013-01-09 23:15:04 |
Access level: | the public | Released: | 2004-07-22 12:27:20 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
11204. | B. S. Kues. 1992. A Late Pennsylvanian restricted-marine fauna from the Kinney Quarry, Manzanita Mountains, New Mexico in Geology and paleontology of the Kinney Brick Quarry, Late Pennsylvanian, central New Mexico, Jiri Zidek, editor. Bulletin - New Mexico Bureau of Mines & Mineral Resources 138:87-97 [J. Alroy/C. Simpson/C. Simpson] |