FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2060855462> ?p ?o ?g. }

• W2060855462 endingPage "191" @default.
• W2060855462 startingPage "174" @default.
• W2060855462 abstract "The benthonic ostracod communities of 93 Recent northeast Atlantic shallow marine sites have been studied. The ostracod assemblages from 76 of these sites were previously undescribed while an additional 17 sites, predominantly from British stations, were assessed from the available literature. Excluding mesohaline genera a total of 102 podocopid ostracod genera were recognized on the northeast Atlantic shelf between the Niger Delta and the Barents Sea. Using both semi-quantitative (most northerly and southerly occurrences of genera) and quantitative (Q-mode analysis, site-site) methods it becomes apparent that ocean currents and water-mass temperature exact a considerable control on the spatial (latitudinal) distribution of benthonic Ostracoda, at the generic level. It has been demonstrated that the majority of northeast Atlantic shelf Ostracoda are restricted to one or several zoogeographical regions or provinces: Nigerian (most southerly), Liberian, Sierra Leonian, Guinean, Mauritanian, Moroccan, Lusitanian, Celtic, Norwegian and Arctic. These provinces are themselves contained within two larger zoogeographical domains, the African and European realms. Each of the 10 provinces are distinguished, not only by the variations in the generic structure of the ostracod assemblages but also in their water-mass characteristics. Ostracod provincial boundaries, in essence, trace zones of intense vertical circulation (Arctic Polar Front and the southern edge of the Guinea Dome) or areas of current divergence (bifurcation of the North Atlantic Drift at Cape Finisterre). Differences also exist in the zoogeographical limits of northeastern and northwestern Atlantic ostracod provinces. The 'concertina' effect on the latitudinal bounds of northwest Atlantic ostracod shelf provinces appears to be intrinsically linked to the presence of a steep thermal gradient associated with the pervasive, southward flowing, Labrador Current. Diametrically, the ameliorating effect of the Gulf Stream has led to the augmentation of provinces within the European realm and assist in the development of broad ecotones, notably in the mid-latitudes. The development of this large modern database and the verification of ostracod provincialism greatly enhances their use, as proxy data, in palaeotemperature and palaeoenvironmental reconstruction of late Cainozoic successions." @default.
• W2060855462 created "2016-06-24" @default.
• W2060855462 creator A5022231955 @default.
• W2060855462 creator A5056803378 @default.
• W2060855462 date "1994-06-01" @default.
• W2060855462 modified "2023-09-23" @default.
• W2060855462 title "Northeastern Atlantic and Arctic faunal provinces based on the distribution of Recent ostracod genera" @default.
• W2060855462 cites W114781204 @default.
• W2060855462 cites W1531499192 @default.
• W2060855462 cites W1717128431 @default.
• W2060855462 cites W1777511926 @default.
• W2060855462 cites W189624547 @default.
• W2060855462 cites W1986998324 @default.
• W2060855462 cites W1990101832 @default.
• W2060855462 cites W1992476248 @default.
• W2060855462 cites W1996543235 @default.
• W2060855462 cites W1999780502 @default.
• W2060855462 cites W2000433131 @default.
• W2060855462 cites W2007137128 @default.
• W2060855462 cites W2014425565 @default.
• W2060855462 cites W2028311673 @default.
• W2060855462 cites W2087878259 @default.
• W2060855462 cites W2089880393 @default.
• W2060855462 cites W2101091451 @default.
• W2060855462 cites W2138868325 @default.
• W2060855462 cites W2146368895 @default.
• W2060855462 cites W2254707524 @default.
• W2060855462 cites W2284933418 @default.
• W2060855462 cites W2314207223 @default.
• W2060855462 cites W2315360474 @default.
• W2060855462 cites W2319034030 @default.
• W2060855462 cites W2323154823 @default.
• W2060855462 cites W2324467255 @default.
• W2060855462 cites W2476809997 @default.
• W2060855462 cites W2503278870 @default.
• W2060855462 cites W4239512124 @default.
• W2060855462 cites W4246653459 @default.
• W2060855462 cites W4247237152 @default.
• W2060855462 cites W4247543773 @default.
• W2060855462 cites W4255526716 @default.
• W2060855462 cites W95418469 @default.
• W2060855462 cites W1999587977 @default.
• W2060855462 doi "https://doi.org/10.1177/095968369400400207" @default.
• W2060855462 hasPublicationYear "1994" @default.
• W2060855462 type Work @default.
• W2060855462 sameAs 2060855462 @default.
• W2060855462 citedByCount "18" @default.
• W2060855462 countsByYear W20608554622012 @default.
• W2060855462 countsByYear W20608554622014 @default.
• W2060855462 countsByYear W20608554622015 @default.
• W2060855462 countsByYear W20608554622020 @default.
• W2060855462 countsByYear W20608554622022 @default.
• W2060855462 crossrefType "journal-article" @default.
• W2060855462 hasAuthorship W2060855462A5022231955 @default.
• W2060855462 hasAuthorship W2060855462A5056803378 @default.
• W2060855462 hasConcept C111368507 @default.
• W2060855462 hasConcept C120221134 @default.
• W2060855462 hasConcept C127313418 @default.
• W2060855462 hasConcept C140302290 @default.
• W2060855462 hasConcept C151730666 @default.
• W2060855462 hasConcept C2776077807 @default.
• W2060855462 hasConcept C518008717 @default.
• W2060855462 hasConceptScore W2060855462C111368507 @default.
• W2060855462 hasConceptScore W2060855462C120221134 @default.
• W2060855462 hasConceptScore W2060855462C127313418 @default.
• W2060855462 hasConceptScore W2060855462C140302290 @default.
• W2060855462 hasConceptScore W2060855462C151730666 @default.
• W2060855462 hasConceptScore W2060855462C2776077807 @default.
• W2060855462 hasConceptScore W2060855462C518008717 @default.
• W2060855462 hasIssue "2" @default.
• W2060855462 hasLocation W20608554621 @default.
• W2060855462 hasOpenAccess W2060855462 @default.
• W2060855462 hasPrimaryLocation W20608554621 @default.
• W2060855462 hasRelatedWork W1964234713 @default.
• W2060855462 hasRelatedWork W1987259969 @default.
• W2060855462 hasRelatedWork W2012094571 @default.
• W2060855462 hasRelatedWork W2035537734 @default.
• W2060855462 hasRelatedWork W2888988925 @default.
• W2060855462 hasRelatedWork W3094494770 @default.
• W2060855462 hasRelatedWork W3203442774 @default.
• W2060855462 hasRelatedWork W3214003923 @default.
• W2060855462 hasRelatedWork W620934038 @default.
• W2060855462 hasRelatedWork W81576150 @default.
• W2060855462 hasVolume "4" @default.
• W2060855462 isParatext "false" @default.
• W2060855462 isRetracted "false" @default.
• W2060855462 magId "2060855462" @default.
• W2060855462 workType "article" @default.