FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2275260982> ?p ?o ?g. }

• W2275260982 endingPage "508" @default.
• W2275260982 startingPage "483" @default.
• W2275260982 abstract "Nummulitoidea are larger benthic foraminifera, and were major reef-forming organisms from the Middle Paleogene to Early Neogene. Today, porous nummulitoid limestones, which occur globally from the Atlantic to the Indo-Pacific, form potentially valuable oil reservoirs. Until now the origin, evolution and palaeogeographic development of the nummulitoids have not been fully articulated, but new material allows here the first systematic, global biostratigraphic comparison and correlation of the nummulitoids to be made. It is suggested that the nummulitoids originated in the Americas during the Middle Paleocene (Selandian). These early nummulitoids are inferred to have migrated across theAtlantic in the Late Paleocene (Thanetian) following two paths: south towards SW Africa, and northeastward through the Tethyan corridor. The Tethyan forms evolved during the Eocene into many lineages,which in turn migrated, within a few million years of their first appearance, into the Indo-Pacific, where they became isolated and diversified further. Meanwhile the SW African forms remained small and similar to the original American stock until the Early Miocene (Burdigalian), when assemblages were augmented by forms that migrated from Tethys, an event tablished by the discovery of new Mediterranean-derived species of Planostegina in SW Africa: africana, mcmillania, southernia, langhiana. Climatic and tectonic processes contributed to the Middle Oligocene disappearance of Nummulites and the Early Miocene global extinction of Spiroclypeus and of Cycloclypeus in the Mediterranean. Morphologically small nummulitoids persisted however, and are still present in all provinces to this day." @default.
• W2275260982 created "2016-06-24" @default.
• W2275260982 creator A5066571909 @default.
• W2275260982 creator A5089768640 @default.
• W2275260982 date "2014-01-01" @default.
• W2275260982 modified "2023-09-26" @default.
• W2275260982 title "The phylogenetic and palaeogeographic evolution of the nummulitoid larger benthic foraminifera" @default.
• W2275260982 cites W1925153848 @default.
• W2275260982 cites W1975527432 @default.
• W2275260982 cites W1979381341 @default.
• W2275260982 cites W1993460199 @default.
• W2275260982 cites W2003422261 @default.
• W2275260982 cites W2010775862 @default.
• W2275260982 cites W2024000132 @default.
• W2275260982 cites W2025184418 @default.
• W2275260982 cites W2033661393 @default.
• W2275260982 cites W2046713607 @default.
• W2275260982 cites W2053603161 @default.
• W2275260982 cites W2060204703 @default.
• W2275260982 cites W2073551687 @default.
• W2275260982 cites W2088200736 @default.
• W2275260982 cites W2105321371 @default.
• W2275260982 cites W2125740066 @default.
• W2275260982 cites W2147406779 @default.
• W2275260982 cites W2168277621 @default.
• W2275260982 cites W2172505405 @default.
• W2275260982 cites W2181347509 @default.
• W2275260982 cites W2182973876 @default.
• W2275260982 cites W2184324225 @default.
• W2275260982 cites W2205478918 @default.
• W2275260982 cites W2218244164 @default.
• W2275260982 cites W2270650042 @default.
• W2275260982 cites W2318931337 @default.
• W2275260982 cites W2594529866 @default.
• W2275260982 cites W2603695153 @default.
• W2275260982 cites W3112201367 @default.
• W2275260982 cites W37683324 @default.
• W2275260982 cites W589232144 @default.
• W2275260982 cites W612211758 @default.
• W2275260982 cites W2598602502 @default.
• W2275260982 doi "https://doi.org/10.47894/mpal.60.6.01" @default.
• W2275260982 hasPublicationYear "2014" @default.
• W2275260982 type Work @default.
• W2275260982 sameAs 2275260982 @default.
• W2275260982 citedByCount "20" @default.
• W2275260982 countsByYear W22752609822015 @default.
• W2275260982 countsByYear W22752609822016 @default.
• W2275260982 countsByYear W22752609822017 @default.
• W2275260982 countsByYear W22752609822018 @default.
• W2275260982 countsByYear W22752609822019 @default.
• W2275260982 countsByYear W22752609822020 @default.
• W2275260982 countsByYear W22752609822021 @default.
• W2275260982 countsByYear W22752609822022 @default.
• W2275260982 countsByYear W22752609822023 @default.
• W2275260982 crossrefType "journal-article" @default.
• W2275260982 hasAuthorship W2275260982A5066571909 @default.
• W2275260982 hasAuthorship W2275260982A5089768640 @default.
• W2275260982 hasBestOaLocation W22752609822 @default.
• W2275260982 hasConcept C109007969 @default.
• W2275260982 hasConcept C111368507 @default.
• W2275260982 hasConcept C12294951 @default.
• W2275260982 hasConcept C127313418 @default.
• W2275260982 hasConcept C151730666 @default.
• W2275260982 hasConcept C164375970 @default.
• W2275260982 hasConcept C166957645 @default.
• W2275260982 hasConcept C204330871 @default.
• W2275260982 hasConcept C205649164 @default.
• W2275260982 hasConcept C27492601 @default.
• W2275260982 hasConcept C2777598122 @default.
• W2275260982 hasConcept C2780368712 @default.
• W2275260982 hasConcept C4646841 @default.
• W2275260982 hasConcept C58097730 @default.
• W2275260982 hasConcept C61721801 @default.
• W2275260982 hasConcept C73707237 @default.
• W2275260982 hasConcept C77928131 @default.
• W2275260982 hasConcept C83042747 @default.
• W2275260982 hasConceptScore W2275260982C109007969 @default.
• W2275260982 hasConceptScore W2275260982C111368507 @default.
• W2275260982 hasConceptScore W2275260982C12294951 @default.
• W2275260982 hasConceptScore W2275260982C127313418 @default.
• W2275260982 hasConceptScore W2275260982C151730666 @default.
• W2275260982 hasConceptScore W2275260982C164375970 @default.
• W2275260982 hasConceptScore W2275260982C166957645 @default.
• W2275260982 hasConceptScore W2275260982C204330871 @default.
• W2275260982 hasConceptScore W2275260982C205649164 @default.
• W2275260982 hasConceptScore W2275260982C27492601 @default.
• W2275260982 hasConceptScore W2275260982C2777598122 @default.
• W2275260982 hasConceptScore W2275260982C2780368712 @default.
• W2275260982 hasConceptScore W2275260982C4646841 @default.
• W2275260982 hasConceptScore W2275260982C58097730 @default.
• W2275260982 hasConceptScore W2275260982C61721801 @default.
• W2275260982 hasConceptScore W2275260982C73707237 @default.
• W2275260982 hasConceptScore W2275260982C77928131 @default.
• W2275260982 hasConceptScore W2275260982C83042747 @default.
• W2275260982 hasIssue "6" @default.
• W2275260982 hasLocation W22752609821 @default.
• W2275260982 hasLocation W22752609822 @default.
• W2275260982 hasLocation W22752609823 @default.

• next