Romeria (reptile)
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Romeria (reptile)
''Romeria'' is an extinct genus of Early Permian captorhinid known from Texas of the United States. It was first named by Llewellyn Ivor Price in 1937 and the type species is ''Romeria texana''. ''R. texana'' is known from the holotype MCZ 1480, a three-dimensionally preserved skull. It was collected in the Archer City Bonebed 1 site, from the Archer City Formation, dating to the Asselian stage of the Cisuralian epoch, about 299–294.6 million years ago. A second species, ''Romeria primus'', was first named by Clark and Carroll in 1973. In 1979, it was corrected as ''Romeria prima'' by Heaton. ''R. prima'' is known from the holotype A holotype (Latin: ''holotypus'') is a single physical example (or illustration) of an organism used when the species (or lower-ranked taxon) was formally described. It is either the single such physical example (or illustration) or one of s ... MCZ 1963, a three-dimensionally preserved skull. It was collected in the Cottonwood Creek ...
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Early Permian
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Archer City Formation
The Archer City Formation is a Formation (geology), geological formation in north-central Texas, preserving fossils from the Asselian and early Sakmarian Stage (stratigraphy), stages of the Permian Period (geologic time), period. It is the earliest component of the Red Beds of Texas and Oklahoma, Texas red beds, introducing a tropical ecosystem which will persist in the area through the rest of the Cisuralian, Early Permian. The Archer City Formation is preceded by the cool Carboniferous swamp sediments of the Markley Formation, and succeeded by the equally fossiliferous red beds of the Nocona Formation. The Archer City Formation was not named as a unique geological unit until the late 1980s. Older studies generally labelled its outcrops as the Moran Formation, Moran or Putnam Formation, Putnam formations, which are age-equivalent marine units to the southwest. The sediments of the Archer City Formation reconstruct a coastal floodplain crossed by small Meander, meandering rivers a ...
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Fossils Of Texas
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Though the fossil record is incomplete, numerous studies have demonstrated that there is enough information available to give a good understanding of the pattern of diversification of life on Earth. In addition, the record can predict and fill gaps such as the discovery of ''Tiktaalik'' in the arctic of Canada. Paleontology includes the study of fossils: their age, method of formation, and evolutionary significance. Specimens are sometimes considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years to 4.1 billion years old. Early edition, published online before print. The ob ...
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