Also known as Albritton locality 8
Where: Comanche County, Texas (31.9° N, 98.6° W: paleocoordinates 29.7° N, 56.5° W)
• coordinate based on nearby landmark
• small collection-level geographic resolution
When: Glen Rose Limestone Formation (Trinity Group), Early/Lower Albian (112.0 - 109.0 Ma)
• level 22
•The Glen Rose formation spans through four ammonite zones with ages between latest Aptian and early Albian. Young 1974 suggested the Kasanskyella spathi ammonite zone is latest aptian, the Hypacanthoplites cragini zone is earliest Albian, the Douvilleiceras mammillatum and Hypacanthoplites comalensis zones are early Albian and may extend into the middle Albian. The benthic foraminifera Orbitolina texana also suggests a late aptian - early albian age and is found in basal levels and in the upper member (Stricklin et al. 1971). Scott et al. (2007) estimated that the age of the Glen Rose Formation ranges from 113.3 to 108.0 Ma.
• bed-level stratigraphic resolution
Environment/lithology: terrestrial; burrowed, bioturbated, shelly/skeletal, yellow, argillaceous, silty limestone
Size classes: macrofossils, microfossils
Preservation: mold/impression, trace, original calcite
Collected by Albritton in 1925
Collection methods: surface (in situ),
Primary reference: C. C. Albritton. 1942. Dinosaur tracks near Comanche, Texas. Field & Laboratory 10(2):160-181 [M. Carrano/M. Carrano/M. Carrano]more details
Purpose of describing collection: paleoecologic analysis
PaleoDB collection 51421: authorized by Matthew Carrano, entered by Matthew Carrano on 03.06.2005, edited by Kaitlin Maguire
Creative Commons license: CC BY (attribution)
Taxonomic list
Foraminifera | |
Foraminifera indet. foram | |
Reptilia | |
"Irenesauripus glenrosensis" = Eubrontes glenrosensis
| |
Deuteropoda | |
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