FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3048483094> ?p ?o ?g. }

• W3048483094 endingPage "195" @default.
• W3048483094 startingPage "175" @default.
• W3048483094 abstract "The paucity of ammonite recovery from North Sea wells has meant that offshore correlations are largely dependent upon microfossil assemblages. While rare, ammonites have been found in a few boreholes during the course of oil exploration activities. The occurrence of ammonites in ten wells in the UK sector of the Viking Graben and the Moray Firth rift arms provides a new basis by which to demonstrate that there was a distinct separation between Arctic and sub-Mediterranean species that lasted from Bajocian to Early Callovian times. Five wells contain ‘Boreal Bathonian' ammonites from the Arctic Realm. Arctocephalites from the Boreal Arcticus Zone (uppermost Bajocian) correlates basinal partly anoxic mudstones in the Beryl Embayment (9/13b) with both bioturbated siltstones in the southern Viking Graben (9/10b), and calcareous mudstones in the East Shetland Basin (211/21). Upper Bajocian Pompeckji Zone Cranocephalites and younger Arcticoceras from Lower to Middle Bathonian Greenlandicus, Ishmae and Cranocephaloide zones are confined to 211/21 demonstrating that the marine transgression began earlier and lasted longer. A Cadoceras from well 3/3-8 dates to the Lower Callovian Koenigi and Calloviense zones during which renewed extensional faulting re-established ammonite migration routes between the Boreal and sub-Mediterranean realms. A Middle Oxfordian (Densiplicatum Zone) Perisphinctes from well 22/5b-8 confirms an episode of northward migration from the sub-Mediterranean into the Boreal Realm. Upper Oxfordian (Regulare to Rosenkantzi zones) Amoeboceras in wells 211/21-1 and 9/13b-19 are close to Upper Bajocian/Lower Bathonian faunas, suggesting an absence of Upper Bathonian to Middle Oxfordian strata as a result of rift-related footwall uplift and erosion. In four wells from Block 15/21 (-4, -11, -12A and -25) Lower Kimmeridgian ammonites have been documented, including Rasenia , Amoebites , Aulacostephanoides and Zenostephanoides , from the Baylei (?), Cymodoce, Mutabilis and Eudoxus zones, the latter (confirmed at well 13/28b-8) dating a widespread regional marine flooding surface in the Inner Moray Firth. Supplementary material: The detailed measurements of dimensions of the ammonites described are available at: https://doi.org/10.6084/m9.figshare.c.5087313" @default.
• W3048483094 created "2020-08-18" @default.
• W3048483094 creator A5028736509 @default.
• W3048483094 creator A5031155861 @default.
• W3048483094 creator A5040075667 @default.
• W3048483094 date "2020-10-13" @default.
• W3048483094 modified "2023-10-10" @default.
• W3048483094 title "Ammonite occurrences in North Sea cores: implications for Jurassic Arctic–Mediterranean marine seaway connectivity" @default.
• W3048483094 cites W1869057322 @default.
• W3048483094 cites W1869607883 @default.
• W3048483094 cites W1969872003 @default.
• W3048483094 cites W1973326483 @default.
• W3048483094 cites W1994359712 @default.
• W3048483094 cites W2003433424 @default.
• W3048483094 cites W2009287621 @default.
• W3048483094 cites W2014453732 @default.
• W3048483094 cites W2021556231 @default.
• W3048483094 cites W2022545458 @default.
• W3048483094 cites W2042442879 @default.
• W3048483094 cites W2043064468 @default.
• W3048483094 cites W2047130448 @default.
• W3048483094 cites W2056774884 @default.
• W3048483094 cites W2069928772 @default.
• W3048483094 cites W2069989425 @default.
• W3048483094 cites W2079039719 @default.
• W3048483094 cites W2093868116 @default.
• W3048483094 cites W2118602128 @default.
• W3048483094 cites W2132575590 @default.
• W3048483094 cites W2136659112 @default.
• W3048483094 cites W2145499653 @default.
• W3048483094 cites W2157991732 @default.
• W3048483094 cites W2162042906 @default.
• W3048483094 cites W2171813691 @default.
• W3048483094 cites W2173221366 @default.
• W3048483094 cites W2184380072 @default.
• W3048483094 cites W2185758217 @default.
• W3048483094 cites W2192197685 @default.
• W3048483094 cites W2244657119 @default.
• W3048483094 cites W2496136483 @default.
• W3048483094 cites W2498965353 @default.
• W3048483094 cites W2588392923 @default.
• W3048483094 cites W2773480489 @default.
• W3048483094 cites W2900864507 @default.
• W3048483094 cites W2931567018 @default.
• W3048483094 cites W3009405513 @default.
• W3048483094 cites W3180200459 @default.
• W3048483094 cites W4206763869 @default.
• W3048483094 doi "https://doi.org/10.1144/sjg2019-030" @default.
• W3048483094 hasPublicationYear "2020" @default.
• W3048483094 type Work @default.
• W3048483094 sameAs 3048483094 @default.
• W3048483094 citedByCount "9" @default.
• W3048483094 countsByYear W30484830942021 @default.
• W3048483094 countsByYear W30484830942023 @default.
• W3048483094 crossrefType "journal-article" @default.
• W3048483094 hasAuthorship W3048483094A5028736509 @default.
• W3048483094 hasAuthorship W3048483094A5031155861 @default.
• W3048483094 hasAuthorship W3048483094A5040075667 @default.
• W3048483094 hasConcept C111368507 @default.
• W3048483094 hasConcept C12294951 @default.
• W3048483094 hasConcept C127313418 @default.
• W3048483094 hasConcept C151730666 @default.
• W3048483094 hasConcept C166957645 @default.
• W3048483094 hasConcept C205649164 @default.
• W3048483094 hasConcept C2779032034 @default.
• W3048483094 hasConcept C2779043415 @default.
• W3048483094 hasConcept C3018378255 @default.
• W3048483094 hasConcept C4646841 @default.
• W3048483094 hasConcept C518008717 @default.
• W3048483094 hasConceptScore W3048483094C111368507 @default.
• W3048483094 hasConceptScore W3048483094C12294951 @default.
• W3048483094 hasConceptScore W3048483094C127313418 @default.
• W3048483094 hasConceptScore W3048483094C151730666 @default.
• W3048483094 hasConceptScore W3048483094C166957645 @default.
• W3048483094 hasConceptScore W3048483094C205649164 @default.
• W3048483094 hasConceptScore W3048483094C2779032034 @default.
• W3048483094 hasConceptScore W3048483094C2779043415 @default.
• W3048483094 hasConceptScore W3048483094C3018378255 @default.
• W3048483094 hasConceptScore W3048483094C4646841 @default.
• W3048483094 hasConceptScore W3048483094C518008717 @default.
• W3048483094 hasIssue "2" @default.
• W3048483094 hasLocation W30484830941 @default.
• W3048483094 hasOpenAccess W3048483094 @default.
• W3048483094 hasPrimaryLocation W30484830941 @default.
• W3048483094 hasRelatedWork W168060249 @default.
• W3048483094 hasRelatedWork W1969368076 @default.
• W3048483094 hasRelatedWork W1977404960 @default.
• W3048483094 hasRelatedWork W1999539277 @default.
• W3048483094 hasRelatedWork W2592784435 @default.
• W3048483094 hasRelatedWork W2792801937 @default.
• W3048483094 hasRelatedWork W306193203 @default.
• W3048483094 hasRelatedWork W3107727085 @default.
• W3048483094 hasRelatedWork W3136355531 @default.
• W3048483094 hasRelatedWork W4206575885 @default.
• W3048483094 hasVolume "56" @default.
• W3048483094 isParatext "false" @default.
• W3048483094 isRetracted "false" @default.
• W3048483094 magId "3048483094" @default.

• next