FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2076786508> ?p ?o ?g. }

• W2076786508 abstract "This study is based on measured and sampled sections in Peregrina Canyon, Tamaulipas, Santa Rosa Canyon, Nuevo Leon, and at several localities in the Sierra de Catorce, San Luis Potosi. All sections included some covered intervals. The Cuesta del Cura and the Agua Nueva(?) are composed of gray to black well indurated, laminated, microcrystalline, cherty limestones and dark fissile limestones and calcareous shales. The fissile limestones and shales are voluminous in the Agua Nueva(?), giving it a more clastic aspect which is the basis for its separation. Typically the Cuesta grades over a short interval into the underlying lighter gray, thicker bedded, unlaminated limestones of the Tamaulipas to form a distinct change in lithic properties, but the upper contact is obscure and necessarily arbitrary. The Cuesta del Cura averages 150 m in thickness; a maximum of 190 m of Agua Nueva(?) was measured and sampled. Foraminifers and calcispheres are common to abundant in most samples. Along with radiolarians, they form the grains of wackestones and packstones. Planktonic forms dominate, giving faunules a strongly pelagic aspect. Induration allowed study by thin section only. Recrystallization and two dimensional specimens made identification difficult. However, many critical species of the middle Cretaceous fauna were recognized, including Favusella washitensis, Ticinella roberti, Globigerinelloides breggiensis, Thalmanninella subticinensis, T. ticinensis, Planomalina buxtorfi, Rotalipora apenninica, Praeglobotruncana stephani, P. delrioensis, Globigerinelloides bentonensis, Rotalipora gandolfi, R. greenhornensis, R. cushmani, and Globotruncana helvetica. The distribution of the foregoing forms permitted division of the succession into eight informal biostratigraphic zones: Globotruncana helvetica zone (First occurrence); Grandes globigerines zone (Interval); Rotalipora cushmani zone (Total Range); Rotalipora greenhornensis zone (First occurrence); Rotalipora gandolfi zone (Partial Range); Planomalina buxtorfi zone (Total Range); Thalmanninella ticinensis zone (First occurrence); Thalmanninella subticinensis zone (First occurrence). The foraminiferal distribution establishes a range of middle Albian to middle Cenomanian for the Cuesta del Cura and middle Cenomanian to middle Turonian for the lower Agua Nueva(?). Calcispheres present include: Calcisphaerula innominata, Pithonella ovalis, P. trejoi, Stomiosphaera conoidea, and S. sphaerica. The ranges reported for these forms are long. Their distribution generally reinforced foraminiferal implications. Microcalamoides diversus (forma C) of unknown affinity occurs in the basalmost few meters of the Cuesta del Cura, suggesting correlation with the middle Albian. End_of_Article - Last_Page 1560------------" @default.
• W2076786508 created "2016-06-24" @default.
• W2076786508 creator A5041259543 @default.
• W2076786508 creator A5070787293 @default.
• W2076786508 date "1980-01-01" @default.
• W2076786508 modified "2023-09-23" @default.
• W2076786508 title "Foraminifers and Calcispheres from Cuesta del Cura and Lower Agua Nueva(?) Formations (Cretaceous), East-Central Mexico: ABSTRACT" @default.
• W2076786508 doi "https://doi.org/10.1306/2f91963e-16ce-11d7-8645000102c1865d" @default.
• W2076786508 hasPublicationYear "1980" @default.
• W2076786508 type Work @default.
• W2076786508 sameAs 2076786508 @default.
• W2076786508 citedByCount "0" @default.
• W2076786508 crossrefType "journal-article" @default.
• W2076786508 hasAuthorship W2076786508A5041259543 @default.
• W2076786508 hasAuthorship W2076786508A5070787293 @default.
• W2076786508 hasConcept C114793014 @default.
• W2076786508 hasConcept C12294951 @default.
• W2076786508 hasConcept C127313418 @default.
• W2076786508 hasConcept C138170599 @default.
• W2076786508 hasConcept C151730666 @default.
• W2076786508 hasConcept C17409809 @default.
• W2076786508 hasConcept C199285206 @default.
• W2076786508 hasConcept C6494504 @default.
• W2076786508 hasConcept C84859931 @default.
• W2076786508 hasConceptScore W2076786508C114793014 @default.
• W2076786508 hasConceptScore W2076786508C12294951 @default.
• W2076786508 hasConceptScore W2076786508C127313418 @default.
• W2076786508 hasConceptScore W2076786508C138170599 @default.
• W2076786508 hasConceptScore W2076786508C151730666 @default.
• W2076786508 hasConceptScore W2076786508C17409809 @default.
• W2076786508 hasConceptScore W2076786508C199285206 @default.
• W2076786508 hasConceptScore W2076786508C6494504 @default.
• W2076786508 hasConceptScore W2076786508C84859931 @default.
• W2076786508 hasLocation W20767865081 @default.
• W2076786508 hasOpenAccess W2076786508 @default.
• W2076786508 hasPrimaryLocation W20767865081 @default.
• W2076786508 hasRelatedWork W1497383680 @default.
• W2076786508 hasRelatedWork W1508295798 @default.
• W2076786508 hasRelatedWork W1514626861 @default.
• W2076786508 hasRelatedWork W2034134100 @default.
• W2076786508 hasRelatedWork W2067971827 @default.
• W2076786508 hasRelatedWork W2076429108 @default.
• W2076786508 hasRelatedWork W2102315746 @default.
• W2076786508 hasRelatedWork W2143967046 @default.
• W2076786508 hasRelatedWork W2144880197 @default.
• W2076786508 hasRelatedWork W2179305153 @default.
• W2076786508 hasRelatedWork W2182938667 @default.
• W2076786508 hasRelatedWork W2254613418 @default.
• W2076786508 hasRelatedWork W2313967761 @default.
• W2076786508 hasRelatedWork W2318469331 @default.
• W2076786508 hasRelatedWork W2324660574 @default.
• W2076786508 hasRelatedWork W2556043981 @default.
• W2076786508 hasRelatedWork W2788076489 @default.
• W2076786508 hasRelatedWork W2911329961 @default.
• W2076786508 hasRelatedWork W3122453054 @default.
• W2076786508 hasRelatedWork W2336483971 @default.
• W2076786508 isParatext "false" @default.
• W2076786508 isRetracted "false" @default.
• W2076786508 magId "2076786508" @default.
• W2076786508 workType "article" @default.