FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2491373302> ?p ?o ?g. }

• W2491373302 endingPage "218" @default.
• W2491373302 startingPage "204" @default.
• W2491373302 abstract "The exceptionally preserved Triassic (Anisian) Grès à Voltzia fauna from the Vosges of northeastern France is compared with four major Carboniferous Konservat-Lagerstätten. The problem of comparing faunas with different types of preservation and degrees of taxonomic determination is addressed with a newly devised similarity coefficient. This coefficient quantifies and combines data from different levels in the taxonomic hierarchy and allows comparisons between biotas in a consistent direction regardless of relative diversity. The rank order of similarity between the four Carboniferous Konservat-Lagerstätten and the Grès à Voltzia is as follows: 1. Mazon Creek (Westphalian D) of Illinois; 2. Glencartholm (Visean) of southern Scotland; 3. Bear Gulch (Namurian) of Montana; and 4. Blanzy-Montceau (Stephanian) of France. These occurrences represent conditions transitional between nearshore fully marine and fresh water. The Grès à Voltzia fauna is significantly closer to the Mazon Creek fauna than to the others; the taxonomic overlap with Blanzy-Montceau and Bear Gulch is limited. Stratigraphic age has an insignificant influence on the result; indeed, the fauna closest in age to the Grès à Voltzia, that of Blanzy-Montceau, is least similar. Taphonomic factors are important in determining the range of organisms preserved. The Glencartholm fauna is represented only by forms with either mineralized or robust chitinous skeletons, implying a greater degree of decay prior to the onset of diagenetic mineralization than in the other Konservat-Lagerstätten. Environment, however, is the major control on similarity. The Mazon Creek biota, like that of Grès à Voltzia, represents settings transitional between terrestrial and marine-influenced delta. Groups common to both Konservat-Lagerstätten include medusae, brachiopods, polychaetes, bivalve and gastropod molluscs, limulids, scorpions, spiders, branchiopods, ostracodes, malacostracans, cycloids, euthycarcinoid and myriapod uniramians, insects, fish, and tetrapods. There is a striking continuity between the faunas of Carboniferous and Triassic transitional sedimentary environments. Groups that were adapted to fluctuating conditions (e.g., shifting salinity) show strong congruence at the family and lower levels and were little affected by Permian extinctions. The major taxonomic contrasts are in the eumalacostracans and insects: many of the groups represented in the Grès à Voltzia appeared in the Permian and radiated across the Permo-Triassic boundary as Paleozoic forms became extinct." @default.
• W2491373302 created "2016-08-23" @default.
• W2491373302 creator A5019794882 @default.
• W2491373302 creator A5044541579 @default.
• W2491373302 date "1990-01-01" @default.
• W2491373302 modified "2023-09-26" @default.
• W2491373302 title "The continuum in soft-bodied biotas from transitional environments: a quantitative comparison of Triassic and Carboniferous Konservat-Lagerstätten" @default.
• W2491373302 cites W173805114 @default.
• W2491373302 cites W1781130633 @default.
• W2491373302 cites W18334028 @default.
• W2491373302 cites W1951180716 @default.
• W2491373302 cites W1967012933 @default.
• W2491373302 cites W198051380 @default.
• W2491373302 cites W1986573889 @default.
• W2491373302 cites W1990025853 @default.
• W2491373302 cites W1998153396 @default.
• W2491373302 cites W2011954528 @default.
• W2491373302 cites W2013568067 @default.
• W2491373302 cites W2019537755 @default.
• W2491373302 cites W2058736628 @default.
• W2491373302 cites W2071751028 @default.
• W2491373302 cites W2076175009 @default.
• W2491373302 cites W2111944730 @default.
• W2491373302 cites W2125974788 @default.
• W2491373302 cites W2132364743 @default.
• W2491373302 cites W2132748177 @default.
• W2491373302 cites W2162201296 @default.
• W2491373302 cites W2162977102 @default.
• W2491373302 cites W2318245656 @default.
• W2491373302 cites W2336833489 @default.
• W2491373302 cites W2487864689 @default.
• W2491373302 cites W2505144080 @default.
• W2491373302 cites W2603909291 @default.
• W2491373302 cites W2808067593 @default.
• W2491373302 cites W4251313306 @default.
• W2491373302 cites W4252464449 @default.
• W2491373302 cites W4290997200 @default.
• W2491373302 cites W53111239 @default.
• W2491373302 cites W67169662 @default.
• W2491373302 cites W69291366 @default.
• W2491373302 cites W80849313 @default.
• W2491373302 cites W93755937 @default.
• W2491373302 doi "https://doi.org/10.1017/s009483730000988x" @default.
• W2491373302 hasPublicationYear "1990" @default.
• W2491373302 type Work @default.
• W2491373302 sameAs 2491373302 @default.
• W2491373302 citedByCount "29" @default.
• W2491373302 countsByYear W24913733022012 @default.
• W2491373302 countsByYear W24913733022013 @default.
• W2491373302 countsByYear W24913733022014 @default.
• W2491373302 countsByYear W24913733022015 @default.
• W2491373302 countsByYear W24913733022017 @default.
• W2491373302 countsByYear W24913733022018 @default.
• W2491373302 countsByYear W24913733022020 @default.
• W2491373302 countsByYear W24913733022022 @default.
• W2491373302 countsByYear W24913733022023 @default.
• W2491373302 crossrefType "journal-article" @default.
• W2491373302 hasAuthorship W2491373302A5019794882 @default.
• W2491373302 hasAuthorship W2491373302A5044541579 @default.
• W2491373302 hasConcept C10277891 @default.
• W2491373302 hasConcept C109007969 @default.
• W2491373302 hasConcept C125471540 @default.
• W2491373302 hasConcept C127313418 @default.
• W2491373302 hasConcept C13106087 @default.
• W2491373302 hasConcept C149918038 @default.
• W2491373302 hasConcept C151730666 @default.
• W2491373302 hasConcept C165730261 @default.
• W2491373302 hasConcept C18903297 @default.
• W2491373302 hasConcept C2777702331 @default.
• W2491373302 hasConcept C2779650180 @default.
• W2491373302 hasConcept C2780187140 @default.
• W2491373302 hasConcept C2781446092 @default.
• W2491373302 hasConcept C86803240 @default.
• W2491373302 hasConceptScore W2491373302C10277891 @default.
• W2491373302 hasConceptScore W2491373302C109007969 @default.
• W2491373302 hasConceptScore W2491373302C125471540 @default.
• W2491373302 hasConceptScore W2491373302C127313418 @default.
• W2491373302 hasConceptScore W2491373302C13106087 @default.
• W2491373302 hasConceptScore W2491373302C149918038 @default.
• W2491373302 hasConceptScore W2491373302C151730666 @default.
• W2491373302 hasConceptScore W2491373302C165730261 @default.
• W2491373302 hasConceptScore W2491373302C18903297 @default.
• W2491373302 hasConceptScore W2491373302C2777702331 @default.
• W2491373302 hasConceptScore W2491373302C2779650180 @default.
• W2491373302 hasConceptScore W2491373302C2780187140 @default.
• W2491373302 hasConceptScore W2491373302C2781446092 @default.
• W2491373302 hasConceptScore W2491373302C86803240 @default.
• W2491373302 hasIssue "2" @default.
• W2491373302 hasLocation W24913733021 @default.
• W2491373302 hasOpenAccess W2491373302 @default.
• W2491373302 hasPrimaryLocation W24913733021 @default.
• W2491373302 hasRelatedWork W1973082154 @default.
• W2491373302 hasRelatedWork W1983603955 @default.
• W2491373302 hasRelatedWork W2007084109 @default.
• W2491373302 hasRelatedWork W2134748672 @default.
• W2491373302 hasRelatedWork W2163321172 @default.
• W2491373302 hasRelatedWork W2170410306 @default.
• W2491373302 hasRelatedWork W2197093321 @default.

• next