FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2154900720> ?p ?o ?g. }

• W2154900720 endingPage "227" @default.
• W2154900720 startingPage "189" @default.
• W2154900720 abstract "Biogeographical patterns of late Palaeozoic rugose coral genera are analysed for the Lower Carboniferous (Visean), early Lower Permian (Asselian/Sakmarian), late Lower Permian (Qixian) and early Upper Permian (Maokoan) of East Asia. Boundaries to the biotic regions are defined to coincide with tectonically significant suture zones to test rival hypotheses about the plate tectonic reconstruction of that region. Three numerical techniques are employed to cluster areas on the basis of shared endemic taxa; parsimony analysis of endemism, principal coordinates analysis and single linkage cluster analysis. Geographical variation in overall diversity is also considered. These results are compared with empirically derived patterns based on other groups of organisms. Major conclusions from this work are as follows, (i) During the Carboniferous and early Permian, the Cathaysian region (North and South China Blocks, Tarim Terrane, Kunlun Terrane, Qiangtang Terrane) formed one cohesive biotic region lying tropically or subtropically; it did not start to fragment until the Upper Permian, (ii) This region was biotically isolated from Central Asia at least during the Carboniferous and Lower Permian, (iii) The southern boundary to the Cathaysian region does not coincide with a single suture zone through time, nor is it sharply defined. Instead there appears to be a gradual faunal impoverishment southwards across the Tibetan Plateau. This implies that faunal ranges are controlled only by the prevailing global climatic regime and not by a geographical barrier, (iv) The Lhasa and Himalaya Terranes shared a similar fauna until the mid-Permian, when a marked faunal disjunction developed coincident with the Zangbo Suture, (v) For terrestrial floras, the barrier to biotic exchange between the North China Block and Angaraland started to break down in the late Permian. It follows that no major oceanic break (‘Palaeotethys’) can be recognized within the Cathaysian region during the late Palaeozoic on palaeontological evidence. This region then formed an integral part of the Gondwanaland craton, extending up into broadly tropical latitudes, and did not become separated from it until the late Lower Permian. The Tienshan-Yinshan Suture is the most likely site of ‘Palaeotethys’, which appears to have occupied a broadly equatorial latitude. Combined with evidence on the ages of the various Asian sutures, this raises significant problems for those who demand a large ocean in their Carboniferous to early Permian palaeogeographical reconstructions of this region." @default.
• W2154900720 created "2016-06-24" @default.
• W2154900720 creator A5016570491 @default.
• W2154900720 date "1988-09-01" @default.
• W2154900720 modified "2023-09-23" @default.
• W2154900720 title "Late Palaeozoic biogeography of East Asia and palaeontological constraints on plate tectonic reconstructions" @default.
• W2154900720 cites W1981431827 @default.
• W2154900720 cites W1982874785 @default.
• W2154900720 cites W1991369222 @default.
• W2154900720 cites W2082815954 @default.
• W2154900720 cites W2093488339 @default.
• W2154900720 cites W2120560912 @default.
• W2154900720 cites W2201017773 @default.
• W2154900720 cites W2488450842 @default.
• W2154900720 cites W4239451055 @default.
• W2154900720 cites W4239623078 @default.
• W2154900720 cites W4244740266 @default.
• W2154900720 cites W4249013635 @default.
• W2154900720 cites W4253813671 @default.
• W2154900720 doi "https://doi.org/10.1098/rsta.1988.0085" @default.
• W2154900720 hasPublicationYear "1988" @default.
• W2154900720 type Work @default.
• W2154900720 sameAs 2154900720 @default.
• W2154900720 citedByCount "33" @default.
• W2154900720 countsByYear W21549007202012 @default.
• W2154900720 countsByYear W21549007202014 @default.
• W2154900720 countsByYear W21549007202016 @default.
• W2154900720 countsByYear W21549007202018 @default.
• W2154900720 countsByYear W21549007202019 @default.
• W2154900720 countsByYear W21549007202020 @default.
• W2154900720 countsByYear W21549007202021 @default.
• W2154900720 crossrefType "journal-article" @default.
• W2154900720 hasAuthorship W2154900720A5016570491 @default.
• W2154900720 hasConcept C105702510 @default.
• W2154900720 hasConcept C109007969 @default.
• W2154900720 hasConcept C127313418 @default.
• W2154900720 hasConcept C13106087 @default.
• W2154900720 hasConcept C149918038 @default.
• W2154900720 hasConcept C150999391 @default.
• W2154900720 hasConcept C151730666 @default.
• W2154900720 hasConcept C2777327002 @default.
• W2154900720 hasConcept C2781148125 @default.
• W2154900720 hasConcept C77928131 @default.
• W2154900720 hasConcept C83365034 @default.
• W2154900720 hasConcept C86803240 @default.
• W2154900720 hasConceptScore W2154900720C105702510 @default.
• W2154900720 hasConceptScore W2154900720C109007969 @default.
• W2154900720 hasConceptScore W2154900720C127313418 @default.
• W2154900720 hasConceptScore W2154900720C13106087 @default.
• W2154900720 hasConceptScore W2154900720C149918038 @default.
• W2154900720 hasConceptScore W2154900720C150999391 @default.
• W2154900720 hasConceptScore W2154900720C151730666 @default.
• W2154900720 hasConceptScore W2154900720C2777327002 @default.
• W2154900720 hasConceptScore W2154900720C2781148125 @default.
• W2154900720 hasConceptScore W2154900720C77928131 @default.
• W2154900720 hasConceptScore W2154900720C83365034 @default.
• W2154900720 hasConceptScore W2154900720C86803240 @default.
• W2154900720 hasIssue "1589" @default.
• W2154900720 hasLocation W21549007201 @default.
• W2154900720 hasOpenAccess W2154900720 @default.
• W2154900720 hasPrimaryLocation W21549007201 @default.
• W2154900720 hasRelatedWork W1964585008 @default.
• W2154900720 hasRelatedWork W1983575308 @default.
• W2154900720 hasRelatedWork W2009900653 @default.
• W2154900720 hasRelatedWork W2032839284 @default.
• W2154900720 hasRelatedWork W2039722155 @default.
• W2154900720 hasRelatedWork W2154900720 @default.
• W2154900720 hasRelatedWork W2174435089 @default.
• W2154900720 hasRelatedWork W2328375679 @default.
• W2154900720 hasRelatedWork W3111929196 @default.
• W2154900720 hasRelatedWork W4244478830 @default.
• W2154900720 hasVolume "326" @default.
• W2154900720 isParatext "false" @default.
• W2154900720 isRetracted "false" @default.
• W2154900720 magId "2154900720" @default.
• W2154900720 workType "article" @default.