Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006753371> ?p ?o ?g. }
- W2006753371 endingPage "358" @default.
- W2006753371 startingPage "337" @default.
- W2006753371 abstract "Thailand has long held a key position in South–East Asia because of its location at the boundary of the Indochinese and Sundaic provinces, the major biogeographical regions of South–East Asia. These provinces are distinct climatically, floristically and faunistically. The present-day limit between them is located at the Kra Isthmus, in peninsular Thailand. Previous studies of the Javanese large mammal fossil faunas and the recent study of fossil large mammal faunas from Thailand strengthen the hypothesis of a “continental” migration route (in contrast with the “insular” hypothesis via Taiwan and the Philippines) during the Late Middle/Late Pleistocene period. Thailand was even part of this migration route. During the glacial periods, the faunal exchanges were favored by the emersion of a huge continental shelf called Sundaland (South–East Asian continental area connected to Borneo and Indonesia islands by land bridges), when the sea level was low. No geological, biogeographical or paleobiogeographical evidence supports the hypothesis of a migration route via Taiwan and the Philippines. Analysis of the extant and Late Middle Pleistocene large mammal faunas (Carnivora, Primates, Proboscidea and Ungulata) points out the antiquity of the Indochinese and Sundaic provinces. This idea is also supported by the fact that mainland faunas already displayed modern character, whereas the Javanese faunas were mainly composed of endemic forms. However, the occurrence of the extinct species, Elephas namadicus found in a Malaysian site (Tambun) indicates that the limit between the two provinces, if not close to the present place, was located more southward than today, possibly in peninsular Malaysia. It is also confirmed by the presence of northern species, such as Ailuropoda melanoleuca baconi and Crocuta crocuta ultima, in Late Middle Pleistocene sites of Thailand. In fact, because of climatic cooling that occurred in the northern hemisphere during the Pleistocene, the northern faunas had to move southward. To our knowledge, the hypothesis of the antiquity of the South–East Asian provinces with a boundary south of the present-day one is mentioned here for the first time. Previous biogeographical studies were based mainly on insular data from the Philippine Archipelago (geological and mainly present-day zoogeographical data) but also from Indonesia and Borneo (paleontological data). However, the recent discovery of Thai large mammal faunas from Late Middle Pleistocene allows to bridge the gap in the fossil record between the northern faunas of South–East Asia and the southern ones. These Thai faunas are characterized mainly by extant forms but some are today absent from the Thai territory (Ailuropoda melanoleuca, Crocuta crocuta, Pongo pygmaeus, Sus cf. barbatus, Rhinoceros cf. unicornis, Cervus eldii)." @default.
- W2006753371 created "2016-06-24" @default.
- W2006753371 creator A5069251996 @default.
- W2006753371 date "2001-04-01" @default.
- W2006753371 modified "2023-10-13" @default.
- W2006753371 title "Biogeography and migration routes of large mammal faunas in South–East Asia during the Late Middle Pleistocene: focus on the fossil and extant faunas from Thailand" @default.
- W2006753371 cites W1973833145 @default.
- W2006753371 cites W1983044404 @default.
- W2006753371 cites W1999001885 @default.
- W2006753371 cites W2002064121 @default.
- W2006753371 cites W2002325302 @default.
- W2006753371 cites W2013820873 @default.
- W2006753371 cites W2028973301 @default.
- W2006753371 cites W2029911103 @default.
- W2006753371 cites W2040663151 @default.
- W2006753371 cites W2044526339 @default.
- W2006753371 cites W2091031232 @default.
- W2006753371 cites W2153331827 @default.
- W2006753371 cites W4241384735 @default.
- W2006753371 doi "https://doi.org/10.1016/s0031-0182(00)00243-1" @default.
- W2006753371 hasPublicationYear "2001" @default.
- W2006753371 type Work @default.
- W2006753371 sameAs 2006753371 @default.
- W2006753371 citedByCount "184" @default.
- W2006753371 countsByYear W20067533712012 @default.
- W2006753371 countsByYear W20067533712013 @default.
- W2006753371 countsByYear W20067533712014 @default.
- W2006753371 countsByYear W20067533712015 @default.
- W2006753371 countsByYear W20067533712016 @default.
- W2006753371 countsByYear W20067533712017 @default.
- W2006753371 countsByYear W20067533712018 @default.
- W2006753371 countsByYear W20067533712019 @default.
- W2006753371 countsByYear W20067533712020 @default.
- W2006753371 countsByYear W20067533712021 @default.
- W2006753371 countsByYear W20067533712022 @default.
- W2006753371 countsByYear W20067533712023 @default.
- W2006753371 crossrefType "journal-article" @default.
- W2006753371 hasAuthorship W2006753371A5069251996 @default.
- W2006753371 hasConcept C123575903 @default.
- W2006753371 hasConcept C125471540 @default.
- W2006753371 hasConcept C127313418 @default.
- W2006753371 hasConcept C144024400 @default.
- W2006753371 hasConcept C149923435 @default.
- W2006753371 hasConcept C151730666 @default.
- W2006753371 hasConcept C166957645 @default.
- W2006753371 hasConcept C188382862 @default.
- W2006753371 hasConcept C18903297 @default.
- W2006753371 hasConcept C191935318 @default.
- W2006753371 hasConcept C205649164 @default.
- W2006753371 hasConcept C2776959937 @default.
- W2006753371 hasConcept C2777808111 @default.
- W2006753371 hasConcept C2778234026 @default.
- W2006753371 hasConcept C2778611284 @default.
- W2006753371 hasConcept C2781300146 @default.
- W2006753371 hasConcept C2908647359 @default.
- W2006753371 hasConcept C2911002212 @default.
- W2006753371 hasConcept C46541322 @default.
- W2006753371 hasConcept C47559259 @default.
- W2006753371 hasConcept C53570757 @default.
- W2006753371 hasConcept C76775654 @default.
- W2006753371 hasConcept C86803240 @default.
- W2006753371 hasConceptScore W2006753371C123575903 @default.
- W2006753371 hasConceptScore W2006753371C125471540 @default.
- W2006753371 hasConceptScore W2006753371C127313418 @default.
- W2006753371 hasConceptScore W2006753371C144024400 @default.
- W2006753371 hasConceptScore W2006753371C149923435 @default.
- W2006753371 hasConceptScore W2006753371C151730666 @default.
- W2006753371 hasConceptScore W2006753371C166957645 @default.
- W2006753371 hasConceptScore W2006753371C188382862 @default.
- W2006753371 hasConceptScore W2006753371C18903297 @default.
- W2006753371 hasConceptScore W2006753371C191935318 @default.
- W2006753371 hasConceptScore W2006753371C205649164 @default.
- W2006753371 hasConceptScore W2006753371C2776959937 @default.
- W2006753371 hasConceptScore W2006753371C2777808111 @default.
- W2006753371 hasConceptScore W2006753371C2778234026 @default.
- W2006753371 hasConceptScore W2006753371C2778611284 @default.
- W2006753371 hasConceptScore W2006753371C2781300146 @default.
- W2006753371 hasConceptScore W2006753371C2908647359 @default.
- W2006753371 hasConceptScore W2006753371C2911002212 @default.
- W2006753371 hasConceptScore W2006753371C46541322 @default.
- W2006753371 hasConceptScore W2006753371C47559259 @default.
- W2006753371 hasConceptScore W2006753371C53570757 @default.
- W2006753371 hasConceptScore W2006753371C76775654 @default.
- W2006753371 hasConceptScore W2006753371C86803240 @default.
- W2006753371 hasIssue "3-4" @default.
- W2006753371 hasLocation W20067533711 @default.
- W2006753371 hasOpenAccess W2006753371 @default.
- W2006753371 hasPrimaryLocation W20067533711 @default.
- W2006753371 hasRelatedWork W1502295812 @default.
- W2006753371 hasRelatedWork W2006753371 @default.
- W2006753371 hasRelatedWork W2050789816 @default.
- W2006753371 hasRelatedWork W2180135016 @default.
- W2006753371 hasRelatedWork W2211975019 @default.
- W2006753371 hasRelatedWork W2911676803 @default.
- W2006753371 hasRelatedWork W2958590071 @default.
- W2006753371 hasRelatedWork W2969421356 @default.
- W2006753371 hasRelatedWork W4243262879 @default.
- W2006753371 hasRelatedWork W4301672860 @default.