FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2100870829> ?p ?o ?g. }

• W2100870829 endingPage "485" @default.
• W2100870829 startingPage "463" @default.
• W2100870829 abstract "Three Upper Viséan to Serpukhovian limestone formations from the Adarouch region (central Morocco), North Africa, have been dated precisely using foraminiferans and calcareous algae. The lower and middle part of the oldest formation, the Tizra Formation (Fm), is assigned to the latest Asbian (upper Cf6γ Subzone), and its upper part to the Early Brigantian (lower Cf6δ Subzone). The topmost beds of this formation are assigned to the Late Brigantian (upper Cf6δ Subzone). The lower part of the succeeding Mouarhaz Fm is also assigned to the Late Brigantian (upper Cf6δ Subzone). The Akerchi Fm is younger than the other formations within the region, ranging from the latest Brigantian (uppermost Cf6δ Subzone) up to the Serpukhovian (E1–E2). The base of the Serpukhovian (Pendleian Substage, E1) is repositioned, to coincide with the appearance of a suite of foraminiferans including Archaediscus at tenuis stage, Endothyranopsis plana, Eostaffella pseudostruvei, Loeblichia ukrainica, Loeblichia aff. minima and Biseriella? sp. 1. The upper Serpukhovian (Arnsbergian Substage, E2) is marked by the first appearance of Eostaffellina ex. gr. paraprotvae and Globoomphalotis aff. pseudosamarica. The biostratigraphical scheme used for the reassessment of the foraminiferal zones and subzones in the Adarouch area closely compares with that for the British succession in northern England (Pennine Region), where the stratotypes of the Upper Viséan (Asbian and Brigantian) and Early Serpukhovian (Pendleian) substages are located. Thus, a succession equivalent to an interval from the Melmerby Scar Limestone to the Great (or Little) Limestone is recognized. These assemblages are also compared to other foraminiferal zones proposed in other regions of Morocco. Several foraminiferans have been identified that are proposed as potential Serpukhovian markers for other basins in Western Europe, and compared to sequences in Russia and the Donets Basin, Ukraine. Copyright © 2008 John Wiley & Sons, Ltd." @default.
• W2100870829 created "2016-06-24" @default.
• W2100870829 creator A5005174836 @default.
• W2100870829 creator A5014600402 @default.
• W2100870829 creator A5022478113 @default.
• W2100870829 creator A5043964845 @default.
• W2100870829 creator A5060339965 @default.
• W2100870829 creator A5079931340 @default.
• W2100870829 creator A5090694594 @default.
• W2100870829 date "2008-09-01" @default.
• W2100870829 modified "2023-10-09" @default.
• W2100870829 title "Late Viséan-Serpukhovian foraminiferans and calcareous algae from the Adarouch region (central Morocco), North Africa" @default.
• W2100870829 cites W1969874609 @default.
• W2100870829 cites W1985327110 @default.
• W2100870829 cites W1986406735 @default.
• W2100870829 cites W1996629919 @default.
• W2100870829 cites W1996750724 @default.
• W2100870829 cites W2010763757 @default.
• W2100870829 cites W2011036511 @default.
• W2100870829 cites W2050248837 @default.
• W2100870829 cites W2051650633 @default.
• W2100870829 cites W2060159923 @default.
• W2100870829 cites W2063859961 @default.
• W2100870829 cites W2067689916 @default.
• W2100870829 cites W2070037380 @default.
• W2100870829 cites W2077442072 @default.
• W2100870829 cites W2078582709 @default.
• W2100870829 cites W2092939755 @default.
• W2100870829 cites W2103953123 @default.
• W2100870829 cites W2115161558 @default.
• W2100870829 cites W2149119046 @default.
• W2100870829 cites W2154293592 @default.
• W2100870829 cites W2155993038 @default.
• W2100870829 cites W2174115663 @default.
• W2100870829 cites W2212938730 @default.
• W2100870829 cites W2607287137 @default.
• W2100870829 cites W2889822654 @default.
• W2100870829 cites W2891605903 @default.
• W2100870829 cites W2996160203 @default.
• W2100870829 cites W3082012540 @default.
• W2100870829 doi "https://doi.org/10.1002/gj.1119" @default.
• W2100870829 hasPublicationYear "2008" @default.
• W2100870829 type Work @default.
• W2100870829 sameAs 2100870829 @default.
• W2100870829 citedByCount "52" @default.
• W2100870829 countsByYear W21008708292012 @default.
• W2100870829 countsByYear W21008708292013 @default.
• W2100870829 countsByYear W21008708292014 @default.
• W2100870829 countsByYear W21008708292015 @default.
• W2100870829 countsByYear W21008708292016 @default.
• W2100870829 countsByYear W21008708292017 @default.
• W2100870829 countsByYear W21008708292018 @default.
• W2100870829 countsByYear W21008708292019 @default.
• W2100870829 countsByYear W21008708292020 @default.
• W2100870829 countsByYear W21008708292021 @default.
• W2100870829 countsByYear W21008708292022 @default.
• W2100870829 crossrefType "journal-article" @default.
• W2100870829 hasAuthorship W2100870829A5005174836 @default.
• W2100870829 hasAuthorship W2100870829A5014600402 @default.
• W2100870829 hasAuthorship W2100870829A5022478113 @default.
• W2100870829 hasAuthorship W2100870829A5043964845 @default.
• W2100870829 hasAuthorship W2100870829A5060339965 @default.
• W2100870829 hasAuthorship W2100870829A5079931340 @default.
• W2100870829 hasAuthorship W2100870829A5090694594 @default.
• W2100870829 hasConcept C127313418 @default.
• W2100870829 hasConcept C150117547 @default.
• W2100870829 hasConcept C151730666 @default.
• W2100870829 hasConcept C18903297 @default.
• W2100870829 hasConcept C61721801 @default.
• W2100870829 hasConcept C86803240 @default.
• W2100870829 hasConceptScore W2100870829C127313418 @default.
• W2100870829 hasConceptScore W2100870829C150117547 @default.
• W2100870829 hasConceptScore W2100870829C151730666 @default.
• W2100870829 hasConceptScore W2100870829C18903297 @default.
• W2100870829 hasConceptScore W2100870829C61721801 @default.
• W2100870829 hasConceptScore W2100870829C86803240 @default.
• W2100870829 hasIssue "4" @default.
• W2100870829 hasLocation W21008708291 @default.
• W2100870829 hasOpenAccess W2100870829 @default.
• W2100870829 hasPrimaryLocation W21008708291 @default.
• W2100870829 hasRelatedWork W1985513757 @default.
• W2100870829 hasRelatedWork W2020246637 @default.
• W2100870829 hasRelatedWork W2237244829 @default.
• W2100870829 hasRelatedWork W2491828709 @default.
• W2100870829 hasRelatedWork W2620625521 @default.
• W2100870829 hasRelatedWork W2625397266 @default.
• W2100870829 hasRelatedWork W2909010594 @default.
• W2100870829 hasRelatedWork W2930872225 @default.
• W2100870829 hasRelatedWork W3147539266 @default.
• W2100870829 hasRelatedWork W4297821198 @default.
• W2100870829 hasVolume "43" @default.
• W2100870829 isParatext "false" @default.
• W2100870829 isRetracted "false" @default.
• W2100870829 magId "2100870829" @default.
• W2100870829 workType "article" @default.