{"title":"Flemingostrea elegans, n. sp.: guide fossil to marine, lower Coniacian (Upper Cretaceous) strata of central New Mexico","authors":"S. Hook","doi":"10.58799/nmg-v32n2.35","DOIUrl":null,"url":null,"abstract":"The marine oyster Flemingostrea elegans, n. sp., appears suddenly in lower Coniacian (Upper Cretaceous) strata of central New Mexico. It has no immediate ancestor in the Western Interior of the United States and has not been found anywhere outside central New Mexico. Flemingostrea elegans occurs in nearshore sandstones in the Mulatto Tongue of the Mancos Shale in Socorro County and the Gallup Sandstone of Lincoln County. This medium-sized oyster, with its distinctive terebratuloid fold, is an excellent guide fossil to the lower Coniacian, and is a great aid in distinguishing the Mulatto Tongue from other tongues of the Mancos Shale in Socorro County and in differentiating Coniacian from Turonian sandstones in Lincoln County. It occurs in great numbers, often as articulated shells, and is easily distinguished from all other Turonian through Coniacian oyster species by the fold in its lower valve. Its presence above coal beds in the lower part of the Crevasse Canyon Formation provides definitive evidence for a third cycle of transgression/regression of the western shoreline of the Late Cretaceous Seaway as far south in New Mexico as central Socorro County. The Santonian dwarf species, Flemingostrea nanus (Johnson 1903), known only from Santa Fe County, New Mexico, is redescribed and illustrated. Flemingostrea nanus, F. elegans, n. sp., and the upper Cenomanian F. prudentia (White 1877) are the only species of Flemingostrea known from the Western Interior. Ostrea elegantula Newberry 1876, which has been confused in the literature with F. elegans, n. sp., should be considered formally as a nomen oblitum (a forgotten name) and not used again. Ostrea elegantula was named but not described or illustrated by J. S. Newberry in his geological report of Captain J. N. Macomb’s 1859 San Juan exploring expedition. F. B. Meek, who wrote the paleontological report on the Cretaceous fossils collected on that expedition, did not describe, illustrate, or mention it. Newberry’s type specimens were illustrated in 1883 by C. A. White, again without description. Attempts to recover Newberry’s type locality along the Canadian River, Colfax County, New Mexico, were unsuccessful.","PeriodicalId":35824,"journal":{"name":"New Mexico Geology","volume":"395 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2010-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"7","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"New Mexico Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.58799/nmg-v32n2.35","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 7
Abstract
The marine oyster Flemingostrea elegans, n. sp., appears suddenly in lower Coniacian (Upper Cretaceous) strata of central New Mexico. It has no immediate ancestor in the Western Interior of the United States and has not been found anywhere outside central New Mexico. Flemingostrea elegans occurs in nearshore sandstones in the Mulatto Tongue of the Mancos Shale in Socorro County and the Gallup Sandstone of Lincoln County. This medium-sized oyster, with its distinctive terebratuloid fold, is an excellent guide fossil to the lower Coniacian, and is a great aid in distinguishing the Mulatto Tongue from other tongues of the Mancos Shale in Socorro County and in differentiating Coniacian from Turonian sandstones in Lincoln County. It occurs in great numbers, often as articulated shells, and is easily distinguished from all other Turonian through Coniacian oyster species by the fold in its lower valve. Its presence above coal beds in the lower part of the Crevasse Canyon Formation provides definitive evidence for a third cycle of transgression/regression of the western shoreline of the Late Cretaceous Seaway as far south in New Mexico as central Socorro County. The Santonian dwarf species, Flemingostrea nanus (Johnson 1903), known only from Santa Fe County, New Mexico, is redescribed and illustrated. Flemingostrea nanus, F. elegans, n. sp., and the upper Cenomanian F. prudentia (White 1877) are the only species of Flemingostrea known from the Western Interior. Ostrea elegantula Newberry 1876, which has been confused in the literature with F. elegans, n. sp., should be considered formally as a nomen oblitum (a forgotten name) and not used again. Ostrea elegantula was named but not described or illustrated by J. S. Newberry in his geological report of Captain J. N. Macomb’s 1859 San Juan exploring expedition. F. B. Meek, who wrote the paleontological report on the Cretaceous fossils collected on that expedition, did not describe, illustrate, or mention it. Newberry’s type specimens were illustrated in 1883 by C. A. White, again without description. Attempts to recover Newberry’s type locality along the Canadian River, Colfax County, New Mexico, were unsuccessful.
期刊介绍:
New Mexico Geology is a quarterly, peer-reviewed journal available by subscription. Articles of original research are generally less than 10,000 words in length and pertain to the geology of New Mexico and neighboring states, primarily for an audience of professional geologists or those with an interest in the geologic story behind the landscape. The journal also publishes abstracts from regional meetings, theses, and dissertations (NM schools), descriptions of new publications, book reviews, and upcoming meetings. Research papers, short articles, and abstracts from selected back issues of New Mexico Geology are now available as free downloads in PDF format. Back issues are also available in hard copy for a nominal fee.