Keet Seel, Segi Canyon (UCMP V3308): Pliensbachian - Toarcian, Arizona
collected by R. H. Thomas & M. Littlesalt 1933

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia - Coelophysidae
Dinosauria indet. (Owen 1842)
1 individual
(2 measurements)
    = Saurischia indet. Seeley 1888
Camp and Vander Hoof 1934
    = Segisaurus halli n. gen., n. sp. Camp 1936
Camp 1936
UCMP 32101
see common names

Geography
Country:United States State/province:Arizona County:Coconino
Coordinates: 36.8° North, 110.5° West (view map)
Paleocoordinates:23.9° North, 48.3° West
Basis of coordinate:stated in text
Geographic resolution:small collection
Time
Period:Jurassic Epoch:Early/Lower Jurassic
*Period:Early/Lower Jurassic
*International age/stage:Early/Lower Hettangian - Late/Upper Toarcian
Key time interval:Pliensbachian - Toarcian
Age range of interval:192.90000 - 174.70000 m.y. ago
* legacy (obsolete) database fields
Stratigraphy
Geological group:Glen Canyon Formation:Navajo Sandstone
Stratigraphic resolution:bed
Stratigraphy comments: fossil found 500 feet above the base of the Navajo Sandstone, measured from the top of the underlying Wingate Sandstone, "and 100 feet below its upper level as exposed on the plateau of Skeleton (Zilh-nez') Mesa"

Navajo Sandstone forms uppermost part of Glen Canyon Group, and is Early Jurassic, but probably not older than Pliensbachian (Irmis 2005. A review of the vertebrate fauna of the Lower Jurassic Navajo Sandstone in Arizona. Mesa Southwest Museum Bulletin 11:55–71)
Lithology and environment
Primary lithology:dunes,"cross stratification",hematitic,red,yellow lithified calcareous sandstone
Secondary lithology:red poorly lithified "shale"
Includes fossils?Y
Lithology description: Navajo Sandstone is a homogenous, friable, fine-grained, aeolian sediment almost exclusively quartzose and with a calcareous cement. The constituent sand grains, though somewhat angular, are frosted and pitted and in most cases are covered with a thin film of iron oxide which imparts a brick red color to the rock. In some places [it] is poor or entirely lacking in iron oxide, resulting in a buff to nearly white aspect...the aeolian origin...is best shown by the type of cross-bedding of the sediments. At the point where the fossil occurred this cross-bedding is exposed in the long sweeping curves of the fore-set beds, sharply truncated above and set together like wedges at various angles." There is also a fine-grained, carbonaceous, supposedly freshwater limestone lens above the specimen. The shale appears as "soft lumps" that increase in frequency in the layers above the specimen and below the limestone.
Environment:dune
Taphonomy
Modes of preservation:body
Degree of concentration:dispersed
Size of fossils:macrofossils
Spatial orientation:life position
Preservation of anatomical detail:good
Abundance in sediment:rare
Articulated whole bodies:all
Fragmentation:occasional
Encrustation:none
Temporal resolution:snapshot
Spatial resolution:autochthonous
Collection methods and comments
Collection methods:selective quarrying,mechanical,field collection
Collection size:1 individuals
Reason for describing collection:taxonomic analysis
Museum repositories:UCMP
Collectors:R. H. Thomas & M. Littlesalt Collection dates:1933
Collection method comments: Collected during the 1933 Rainbow Bridge-Monument Valley Expedition, led by A. Hall, VanderHoof & Camp. Discovered by student Robert H. Thomas and Navajo Max Littlesalt.
Metadata
Also known as:Segisaurus type, UCMP V338, Camp
Database number:25306
Authorizer:M. Carrano Enterer:M. Carrano
Modifier:M. Carrano Research group:vertebrate
Created:2002-09-07 21:00:26 Last modified:2023-09-08 14:14:34
Access level:the public Released:2002-09-07 21:00:26
Creative Commons license:CC BY
Reference information

Primary reference:

54283. Anonymous. 1933. Bones of a bird-like dinosaur. Science 78 (supp.)(2033):6-7 [M. Carrano/M. Carrano]

Secondary references:

63594 A. A. Baker, C. H. Dane, and J. B. Reeside. 1936. Correlation of the Jurassic formations of parts of Utah, Arizona, New Mexico and Colorado. United States Department of the Interior Geological Survey Professional Paper 183:1-66 [M. Carrano/M. Carrano/M. Carrano]
7096 C. L. Camp. 1936. A new type of bipedal dinosaur from the Navajo Sandstone of Arizona. University of California Publications in Geological Sciences 24(2):39-56 [M. Carrano/M. Carrano/M. Carrano]
55545 C. L. Camp and V. L. Vander Hoof. 1934. Bipedal dinosaur from Jurassic of northern Arizona. Pan-American Geologist 62(1):70 [M. Carrano/M. Carrano]
16598ETE M. T. Carrano, J. R. Hutchinson, and S. D. Sampson. 2005. New information on Segisaurus halli, a small theropod dinosaur from the Early Jurassic of Arizona. Journal of Vertebrate Paleontology 25(4):835-849 [M. Carrano/K. Maguire/M. Carrano]
12617ETE P. M. Galton. 1971. The prosauropod dinosaur Ammosaurus, the crocodile Protosuchus, and their bearing on the age of the Navajo Sandstone of northeastern Arizona. Journal of Paleontology 45(5):781-795 [M. Carrano/M. Carrano/M. Carrano]
63054 C. W. Gilmore. 1939. A review of recent progress in reptilian paleontology. Bulletin of the Geological Society of America 50:337-348 [M. Carrano/M. Carrano]
80483 J. W. Harshbarger, C. A. Repenning, and J. H. Irwin. 1957. Stratigraphy of the uppermost Triassic and the Jurassic rocks of the Navajo country. United States Geological Survey Professional Paper 291:1-74 [T. Hegna/M. Pankowski/M. Carrano]
24406ETE R. B. Irmis. 2005. A review of the vertebrate fauna of the Lower Jurassic Navajo Sandstone in Arizona. In R. D. McCord (ed.), Vertebrate Paleontolgy of Arizona. Mesa Southwest Museum Bulletin 11:55-71 [M. Carrano/M. Carrano]
71257 E. T. McKnight. 1940. Geology of area between Green and Colorado rivers, Grand and San Juan counties, Utah. United States Geological Survey Bulletin 908:v-147 [M. Carrano/M. Carrano]
84543 J. S. Tweet and V. L. Santucci. 2018. An inventory of non-avian dinosaurs from National Park Service areas. In S. G. Lucas & R. M. Sullivan (ed.), Fossil Record 6. New Mexico Museum of Natural History and Science Bulletin 79:703-730 [M. Carrano/M. Carrano]