Kirtland Formation facts for kids
Quick facts for kids Kirtland FormationStratigraphic range: Campanian (typically Kirtlandian) 75–73Ma |
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Type | Geological formation |
Sub-units | Hunter Wash, Farmington and De-na-zin Members |
Underlies | Ojo Alamo Formation |
Overlies | Fruitland Formation |
Thickness | 594 m (1,949 ft) |
Lithology | |
Primary | Sandstone |
Other | Shale, mudstone, conglomerate |
Location | |
Coordinates | 36°42′29″N 108°21′00″W / 36.708°N 108.350°W |
Approximate paleocoordinates | 42°36′N 76°18′W / 42.6°N 76.3°W |
Region | New Mexico |
Country | USA |
Extent | San Juan Basin |
Type section | |
Named for | Kirtland Post Office |
Named by | C.M. Bauer |
Year defined | 1916 |
The Kirtland Formation (originally the Kirtland Shale) is a sedimentary geological formation.
Contents
Description
The Kirtland Formation is the product of alluvial muds and overbank sand deposits from the many channels draining the coastal plain that existed on the inland seashore of North America, in the late Cretaceous period. It overlies the Fruitland Formation. It is found in the San Juan Basin in the states of New Mexico and Colorado, in the United States of America.
The base of the Kirtland Formation and its lowest sub-unit, the Hunter Wash member, has been dated to 75.02 ± 0.13 Ma. Together with the upper part of the underlying Fruitland Formation, this contains fossils representing the Hunter Wash local fauna. The border between the Hunter Wash member and overlying Farmington member dates to approximately 74 million years ago. The top of the Farmington member and bottom of the overlying De-na-zin member has been radiometrically dated to 73.37 ± 0.28 Ma ago. The top of the De-na-zin member, which contains the Willow Wash local fauna, has been dated to 73.04 ± 0.25 Ma ago.
Overlying the De-na-zin member is a unit called the Naashoibito member This has often been considered to be part of the Kirtland formation, but more recently has been transferred back to the overlying Ojo Alamo Formation, which it had originally been part of.
History of investigation
The formation was named by C.M. Bauer in 1916 for exposures near the Kirtland Post Office.
Stratigraphy
Vertebrate paleofauna
Crurotarsans
Crurotarsans of the Kirtland Formation | ||||||
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Genus | Species | Location | Member | Abundance | Notes | Images |
Brachychampsa |
B. montana |
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Member of the Willow Wash local fauna. |
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Denazinosuchus |
D. kirtlandicus |
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Member of the Willow Wash local fauna. |
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Leidyosuchus |
Indeterminate |
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Member of the Willow Wash local fauna. |
Ornithischians
Ornithischians reported from the Kirtland Formation | ||||||
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Genus | Species | Location | Member | Material | Notes | Images |
Ahshislepelta |
A. minor |
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Incomplete postcranial skeleton |
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Anasazisaurus |
A. horneri |
"Partial skull." |
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Kritosaurus |
K. navajovius |
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Member of the Willow Wash local fauna. |
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Naashoibitosaurus |
N.ostromi |
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"Partial skull." |
Member of the Willow Wash local fauna. |
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Nodocephalosaurus |
N. kirtlandensis |
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"Partial skull." |
Member of the Willow Wash local fauna. |
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P. tubicen |
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"Disarticulated, associated skull and postcraniua, pertaining to at least [three] individuals." |
Member of the Willow Wash local fauna. |
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P. fenestratus |
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P. sternbergi |
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More common in the lower part of the formation. |
Member of the Willow Wash local fauna. |
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Sphaerotholus |
S. goodwini |
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Member of the Willow Wash local fauna. |
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S. novomexicanum |
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"SMP VP-2790, incomplete parietal" |
Also found in the upper Fruitland Formation. |
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Terminocavus |
T. sealeyi |
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Navajoceratops |
N. sullivani |
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Titanoceratops |
T. ouranos |
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Member of the Willow Wash local fauna. Found to be a synonym of Pentaceratops sternbergii. |
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Ziapelta |
Z. sanjuanensis |
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Complete skull lacking the lower jaws, first two cervical half rings. |
Pterosaurs
Pterosaurs of the Kirtland Formation | ||||||
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Genus | Species | Location | Member | Abundance | Notes | |
Navajodactylus |
N. boerei |
Partial phalanx and ulna fragment |
Hunter Wash Member |
Saurischians
Saurischians of the Kirtland Formation | ||||||
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Genus | Species | Location | Member | Abundance | Notes | Images |
A. sanjuanensis |
Erroneously identified as a member of the Willow Wash fauna, specimens actually from the Naashoibito member of the Ojo Alamo Formation |
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Aublysodon |
A. mirandus |
Remains once attributed to the dubious tooth genus Aublysodon (and later Daspletosaurus) are now referred to Bistahieversor, although these remains (OMNH 10131) may possibly have come from the Fruitland Formation. |
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Bistahieversor |
B. sealeyi |
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Unnamed |
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Remains formerly referred to an unidentified or undescribed species of Daspletosaurus were originally attributed to the dubious tooth genus Aublysodon. These remains were later reclassified as belonging to the new genus Bistahieversor. Some of these remains (OMNH 10131), however, may have originated in the Fruitland Formation. |
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O. sp. |
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Member of the Willow Wash local fauna. |
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Saurornitholestes |
S. sullivani |
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"Saurornitholestes" |
"S." robustus |
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Member of the Willow Wash local fauna. Originally assigned to Saurornitholestes, actually a troodontid. |
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Indeterminate |
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Indeterminate |
Turtles
Turtles of the Kirtland Formation | ||||||
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Genus | Species | Location | Member | Abundance | Notes | |
Basilemys |
B. nobilis |
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Member of the Willow Wash local fauna. |
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Denazinemys |
D. nodosa |
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Member of the Willow Wash local fauna. |
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Neurankylus |
N. baueri |
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Member of the Willow Wash local fauna. |
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Plastomenus |
P. robustus |
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Member of the Willow Wash local fauna. |
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Thescelus |
T. hemispherica |
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Member of the Willow Wash local fauna. |
Bony fish
Bony fishes of the Kirtland Formation | ||||||
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Genus | Species | Location | Member | Abundance | Notes | |
Melvius |
M. chauliodous |
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Member of the Willow Wash local fauna. |
Cartilaginous fish
Cartilaginous fish of the Kirtland Formation | ||||||
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Genus | Species | Location | Member | Abundance | Notes | |
Myledaphus |
M. bipartitus |
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Member of the Willow Wash local fauna. |
Color key
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Notes Uncertain or tentative taxa are in small text; |
Images for kids
See also
In Spanish: Formación Kirtland para niños