FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2174115663> ?p ?o ?g. }

• W2174115663 endingPage "923" @default.
• W2174115663 startingPage "906" @default.
• W2174115663 abstract "The biostratigraphy of the upper part of the Mississippian Lower Limestone Formation in the Midland Valley, Scotland is revised using foraminiferal assemblages. This formation was previously assigned exclusively to the upper part of the Brigantian Substage (upper Cf6δ, P 2 or latest Visean), whereas the succeeding Limestone Coal Formation (barren of foraminifers and conodonts) was assigned to the Pendleian Substage (lower Cf7, E 1 or early Serpukhovian). The foraminifers, in particular those recorded from the Second Hosie and Top Hosie limestones and their lateral equivalents (Anvil and MacDonald limestones), are comparable to Serpukhovian assemblages from the Ukraine and Russia. Consequently, the Visean/Serpukhovian stage boundary is repositioned at the base of the Second Hosie Limestone. This assignment of the Second Hosie Limestone to the Pendleian is reinforced by the first occurrence of the ammonoid Emstites ( Cravenoceras ), although it occurs 1 m below the Top Hosie Limestone. Pendleian foraminiferal assemblages from northern England, its geographically closest equivalent, are similar but not well enough known for a detailed comparison. A few similarities are found between the foraminiferal assemblages from the Midland Valley and those from southwest Spain and North African basins. Faunas from the Second and Top Hosie limestones and their lateral equivalents allow us to propose an assemblage zone, valid for regional correlations within the British Isles, and the faunas can be potentially used as Serpukhovian markers for western Paleotethyan basins. Two new genera and species are described, Praeplectostaffella anvilensis n. gen. n. sp. and Praeostaffellina macdonaldensis n. gen. n. sp., and two new species, Tubispirodiscus hosiensis n. sp. and Euxinita pendleiensis n. sp." @default.
• W2174115663 created "2016-06-24" @default.
• W2174115663 creator A5014600402 @default.
• W2174115663 creator A5028081959 @default.
• W2174115663 creator A5043964845 @default.
• W2174115663 date "2008-09-01" @default.
• W2174115663 modified "2023-09-26" @default.
• W2174115663 title "New foraminifers in the Visean/Serpukhovian boundary interval of the Lower Limestone Formation, Midland Valley, Scotland" @default.
• W2174115663 cites W1548898812 @default.
• W2174115663 cites W1969874609 @default.
• W2174115663 cites W1971559739 @default.
• W2174115663 cites W1986034248 @default.
• W2174115663 cites W1986406735 @default.
• W2174115663 cites W1990340825 @default.
• W2174115663 cites W1995501460 @default.
• W2174115663 cites W2033565268 @default.
• W2174115663 cites W2038745462 @default.
• W2174115663 cites W2051650633 @default.
• W2174115663 cites W2060159923 @default.
• W2174115663 cites W2070037380 @default.
• W2174115663 cites W2078971321 @default.
• W2174115663 cites W2092939755 @default.
• W2174115663 cites W2100336986 @default.
• W2174115663 cites W2103953123 @default.
• W2174115663 cites W2130597167 @default.
• W2174115663 cites W2141333056 @default.
• W2174115663 cites W2149119046 @default.
• W2174115663 cites W2158457339 @default.
• W2174115663 cites W2166178877 @default.
• W2174115663 cites W2320218315 @default.
• W2174115663 cites W2329084582 @default.
• W2174115663 cites W2331966657 @default.
• W2174115663 cites W2333092433 @default.
• W2174115663 cites W2335769994 @default.
• W2174115663 cites W2488200759 @default.
• W2174115663 cites W2587685076 @default.
• W2174115663 cites W4232328127 @default.
• W2174115663 cites W639074227 @default.
• W2174115663 doi "https://doi.org/10.1666/07-103.1" @default.
• W2174115663 hasPublicationYear "2008" @default.
• W2174115663 type Work @default.
• W2174115663 sameAs 2174115663 @default.
• W2174115663 citedByCount "38" @default.
• W2174115663 countsByYear W21741156632012 @default.
• W2174115663 countsByYear W21741156632013 @default.
• W2174115663 countsByYear W21741156632014 @default.
• W2174115663 countsByYear W21741156632015 @default.
• W2174115663 countsByYear W21741156632016 @default.
• W2174115663 countsByYear W21741156632017 @default.
• W2174115663 countsByYear W21741156632018 @default.
• W2174115663 countsByYear W21741156632019 @default.
• W2174115663 countsByYear W21741156632020 @default.
• W2174115663 countsByYear W21741156632021 @default.
• W2174115663 countsByYear W21741156632022 @default.
• W2174115663 crossrefType "journal-article" @default.
• W2174115663 hasAuthorship W2174115663A5014600402 @default.
• W2174115663 hasAuthorship W2174115663A5028081959 @default.
• W2174115663 hasAuthorship W2174115663A5043964845 @default.
• W2174115663 hasConcept C109007969 @default.
• W2174115663 hasConcept C125471540 @default.
• W2174115663 hasConcept C127313418 @default.
• W2174115663 hasConcept C146357865 @default.
• W2174115663 hasConcept C149918038 @default.
• W2174115663 hasConcept C151730666 @default.
• W2174115663 hasConcept C18903297 @default.
• W2174115663 hasConcept C2780187140 @default.
• W2174115663 hasConcept C61721801 @default.
• W2174115663 hasConcept C86803240 @default.
• W2174115663 hasConceptScore W2174115663C109007969 @default.
• W2174115663 hasConceptScore W2174115663C125471540 @default.
• W2174115663 hasConceptScore W2174115663C127313418 @default.
• W2174115663 hasConceptScore W2174115663C146357865 @default.
• W2174115663 hasConceptScore W2174115663C149918038 @default.
• W2174115663 hasConceptScore W2174115663C151730666 @default.
• W2174115663 hasConceptScore W2174115663C18903297 @default.
• W2174115663 hasConceptScore W2174115663C2780187140 @default.
• W2174115663 hasConceptScore W2174115663C61721801 @default.
• W2174115663 hasConceptScore W2174115663C86803240 @default.
• W2174115663 hasIssue "5" @default.
• W2174115663 hasLocation W21741156631 @default.
• W2174115663 hasOpenAccess W2174115663 @default.
• W2174115663 hasPrimaryLocation W21741156631 @default.
• W2174115663 hasRelatedWork W1032277182 @default.
• W2174115663 hasRelatedWork W1971125061 @default.
• W2174115663 hasRelatedWork W2006696342 @default.
• W2174115663 hasRelatedWork W2112953699 @default.
• W2174115663 hasRelatedWork W2502909090 @default.
• W2174115663 hasRelatedWork W2789304626 @default.
• W2174115663 hasRelatedWork W3135689008 @default.
• W2174115663 hasRelatedWork W1916708974 @default.
• W2174115663 hasRelatedWork W3151351829 @default.
• W2174115663 hasRelatedWork W3158648838 @default.
• W2174115663 hasVolume "82" @default.
• W2174115663 isParatext "false" @default.
• W2174115663 isRetracted "false" @default.
• W2174115663 magId "2174115663" @default.
• W2174115663 workType "article" @default.