{"title":"fleminggostrea elegans, n. sp.:新墨西哥中部下Coniacian(上白垩纪)地层的海相指导化石","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":"{\"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}","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
摘要
海洋牡蛎Flemingostrea elegans, n.sp .,突然出现在新墨西哥州中部的下Coniacian(上白垩纪)地层中。它在美国西部内陆没有直系祖先,也没有在新墨西哥州中部以外的任何地方发现过。fleminggostrea elegans出现在Socorro县Mancos页岩的Mulatto舌和Lincoln县Gallup砂岩的近岸砂岩中。这种中等大小的牡蛎,具有独特的非脊椎类褶皱,是下科尼亚纪的极好指导化石,是区分索科罗县曼科斯页岩的穆拉托语和其他语言以及区分林肯县科尼亚纪和Turonian砂岩的巨大帮助。它大量出现,通常是铰接的壳,很容易通过其下瓣的褶皱与所有其他Turonian至Coniacian牡蛎物种区分开来。它在克雷瓦斯峡谷地层下部煤层之上的存在,为晚白垩世海道西部海岸线的第三轮海侵/回归提供了明确的证据,从新墨西哥州向南一直延伸到索科罗县中部。圣东尼亚矮种,Flemingostrea nanus (Johnson 1903),仅在新墨西哥州的圣达菲县已知,被重新描述和说明。fleminggostrea nanus, F. elegans, n. sp.和upper Cenomanian F. prudentia (White 1877)是唯一已知的来自西部内陆的fleminggostrea物种。Ostrea elegantula Newberry 1876,在文献中与F. elegans, n.sp混淆,应该被正式视为nomen oblitum(一个被遗忘的名字)而不再使用。在j·n·马科姆船长1859年圣胡安探险的地质报告中,j·s·纽伯里命名了秀丽Ostrea elegantula,但没有描述或说明。F. B. Meek写了一份关于那次探险所收集的白垩纪化石的古生物学报告,他没有描述、说明或提及这件事。纽伯里的模式标本在1883年由c·a·怀特(C. A. White)绘制,同样没有描述。试图在新墨西哥州科尔法克斯县的加拿大河沿岸恢复纽贝里的类型位置,没有成功。
Flemingostrea elegans, n. sp.: guide fossil to marine, lower Coniacian (Upper Cretaceous) strata of central New Mexico
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.