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Mesozoic
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Lower Cretaceous
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Albian
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upper Albian (1)
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Glen Rose Formation (2)
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Potomac Group (1)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (1)
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Atokan (1)
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Upper Pennsylvanian
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Virgilian (1)
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Magdalena Group (1)
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palynomorphs
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miospores
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pollen (1)
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Plantae
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shale (1)
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stratigraphy (1)
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United States
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Arkansas
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Searcy County Arkansas (1)
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Van Buren County Arkansas (1)
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Midwest (1)
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Ohio
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Coshocton County Ohio (1)
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Jackson County Ohio (1)
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Lawrence County Ohio (1)
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Muskingum County Ohio (1)
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Oklahoma
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Bryan County Oklahoma (1)
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Love County Oklahoma (1)
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Marshall County Oklahoma (1)
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Texas
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Comanche County Texas (1)
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Cooke County Texas (1)
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Denton County Texas (1)
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Erath County Texas (1)
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Grayson County Texas (1)
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Hood County Texas (10)
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Jack County Texas (1)
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Parker County Texas (2)
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Somervell County Texas (1)
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Tarrant County Texas
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Fort Worth Texas (1)
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Travis County Texas (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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limestone (1)
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clastic rocks
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mudstone (1)
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shale (1)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Hood County Texas
Early Cretaceous (Albian) spores and pollen from the Glen Rose Formation of Texas and their significance for correlation of the Potomac Group
Strontium isotope stratigraphy of the Comanchean Series in north Texas and southern Oklahoma
Ammonites and inoceramid bivalves from close to the middle-upper Albian boundary around Fort Worth, Texas
Cardiarina cordata Cooper, 1956, (Brachiopoda), terebratuloid or rhynchonelloid?
Late Paleozoic problematic sclerites of hercolepadid affinities
Arceodomus prolata n. sp. (Mollusca, Rostroconchia) from the Pennsylvanian of Texas
Some new Paleozoic gastropod opercula (Pennsylvanian, Texas)
Paleoecology and hypsilophodontid behavior at the Proctor Lake dinosaur locality (Early Cretaceous), Texas
A new Early Cretaceous dinosaur locality in the Twin Mountains Formation at Proctor Lake, Texas, reveals information concerning hypsilophodontid social behavior. Both adults and congregations of juvenile hypsilophodontids occur at the site. Recent excavation of one mass of juveniles shows that it occurs in a shallow depression on a paleosol surface. The distribution of skeletal elements and age structure of individuals within congregations may indicate nesting and parental care of the young after hatching. Hypsilophodontids occupied the site over a long period of time, indicating attraction to the area for some reason. The region was a semi-arid flood plain within a lowland valley. Attractive features of the site may have included abundant vegetation and water or protection from predators. The accumulations of juvenile bones may represent attritional mortality of individuals from a single clutch or a succession of clutches in the nest area.