FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2789322052> ?p ?o ?g. }

• W2789322052 endingPage "108704" @default.
• W2789322052 startingPage "108704" @default.
• W2789322052 abstract "Palynological assemblages from the Tulong succession in South Tibet enabled the recognition of three miospore biozones within the Zhangdong and ‘Yali’ formations. In ascending order, they are the Retispora lepidophyta–Verrucosisporites nitidus (LN) Biozone, the Vallatisporites vallatus–Foveosporites pellucidus (VP) Biozone and the Rugospora polyptycha–Tricidarisporites arcuatus (PA) Biozone. The LN Biozone in the Tulong section can be correlated to the LN Biozone of Western Europe, based on the first and last appearances of many index miospore species. However, Tournaisian palynological assemblages of Western Europe and South Tibet show compositional differences. The VP and PA biozones of South Tibet are correlated tentatively to the VI–HD and BP–TC biozones of Western Europe based on the occurrences of rare miospore index species in both regions. The Zhangdong and ‘Yali’ formations are now dated as Famennian to possibly earliest Visean. This age assessment is supported by rare conodonts and ammonoids recovered from intercalated limestones in the basal part of ‘Yali’ Formation. In the Everest region, the Devonian–Carboniferous boundary is now placed c. 10 m above the lower boundary of the ‘Yali’ Formation, which was originally suggested by Lin and Qiu (1985) to be position of the D–C boundary. Unlike western Gondwana, i.e. Bolivia and Brazil, the Himalaya-Tethys zone at the northeastern margin of Gondwana does not show obvious lithological evidence for glaciations. The new palynostratigraphic data, including information on sea-level changes reflected by variations in palynological composition and lithology around the Devonian–Carboniferous boundary allow, an interregional, approximate correlation with the classical Hangenberg Event sequence in the Rhenish Massif. The analogous Hangenberg Event sequence in South Tibet further supports the hypothesis that the rapid Hangenberg Event regression/transgression was a global eustatic event of significant magnitude. The co-occurrence of probably reworked Frasnian Geminospora lemurata and Archaeoperisaccus spores in the Himalaya-Tethys zone indicates the palaeogeographical proximity of the northern margin of Gondwana to the South China Block in the palaeoequatorial belt." @default.
• W2789322052 created "2018-03-29" @default.
• W2789322052 creator A5009288717 @default.
• W2789322052 creator A5010740814 @default.
• W2789322052 creator A5044469264 @default.
• W2789322052 creator A5060470951 @default.
• W2789322052 creator A5078494464 @default.
• W2789322052 date "2019-10-01" @default.
• W2789322052 modified "2023-10-12" @default.
• W2789322052 title "Palynostratigraphy of the Devonian–Carboniferous transition in the Tulong section in South Tibet: A Hangenberg Event sequence analogue in the Himalaya-Tethys zone" @default.
• W2789322052 cites W1971036111 @default.
• W2789322052 cites W2003311821 @default.
• W2789322052 cites W2009566539 @default.
• W2789322052 cites W2017729385 @default.
• W2789322052 cites W2019748000 @default.
• W2789322052 cites W2019839279 @default.
• W2789322052 cites W2023899094 @default.
• W2789322052 cites W2034397592 @default.
• W2789322052 cites W2037279734 @default.
• W2789322052 cites W2040023581 @default.
• W2789322052 cites W2064725572 @default.
• W2789322052 cites W2082150583 @default.
• W2789322052 cites W2085366644 @default.
• W2789322052 cites W2091539779 @default.
• W2789322052 cites W2101755502 @default.
• W2789322052 cites W2289667625 @default.
• W2789322052 cites W2298114143 @default.
• W2789322052 cites W2329084582 @default.
• W2789322052 cites W2330644089 @default.
• W2789322052 doi "https://doi.org/10.1016/j.palaeo.2018.03.016" @default.
• W2789322052 hasPublicationYear "2019" @default.
• W2789322052 type Work @default.
• W2789322052 sameAs 2789322052 @default.
• W2789322052 citedByCount "9" @default.
• W2789322052 countsByYear W27893220522020 @default.
• W2789322052 countsByYear W27893220522021 @default.
• W2789322052 countsByYear W27893220522022 @default.
• W2789322052 countsByYear W27893220522023 @default.
• W2789322052 crossrefType "journal-article" @default.
• W2789322052 hasAuthorship W2789322052A5009288717 @default.
• W2789322052 hasAuthorship W2789322052A5010740814 @default.
• W2789322052 hasAuthorship W2789322052A5044469264 @default.
• W2789322052 hasAuthorship W2789322052A5060470951 @default.
• W2789322052 hasAuthorship W2789322052A5078494464 @default.
• W2789322052 hasConcept C107832698 @default.
• W2789322052 hasConcept C109007969 @default.
• W2789322052 hasConcept C127313418 @default.
• W2789322052 hasConcept C146357865 @default.
• W2789322052 hasConcept C149918038 @default.
• W2789322052 hasConcept C151730666 @default.
• W2789322052 hasConcept C162501224 @default.
• W2789322052 hasConcept C164375970 @default.
• W2789322052 hasConcept C170434497 @default.
• W2789322052 hasConcept C181727316 @default.
• W2789322052 hasConcept C18903297 @default.
• W2789322052 hasConcept C192797867 @default.
• W2789322052 hasConcept C2777302187 @default.
• W2789322052 hasConcept C2780187140 @default.
• W2789322052 hasConcept C2780618852 @default.
• W2789322052 hasConcept C2781148125 @default.
• W2789322052 hasConcept C61721801 @default.
• W2789322052 hasConcept C62476579 @default.
• W2789322052 hasConcept C6494504 @default.
• W2789322052 hasConcept C86803240 @default.
• W2789322052 hasConceptScore W2789322052C107832698 @default.
• W2789322052 hasConceptScore W2789322052C109007969 @default.
• W2789322052 hasConceptScore W2789322052C127313418 @default.
• W2789322052 hasConceptScore W2789322052C146357865 @default.
• W2789322052 hasConceptScore W2789322052C149918038 @default.
• W2789322052 hasConceptScore W2789322052C151730666 @default.
• W2789322052 hasConceptScore W2789322052C162501224 @default.
• W2789322052 hasConceptScore W2789322052C164375970 @default.
• W2789322052 hasConceptScore W2789322052C170434497 @default.
• W2789322052 hasConceptScore W2789322052C181727316 @default.
• W2789322052 hasConceptScore W2789322052C18903297 @default.
• W2789322052 hasConceptScore W2789322052C192797867 @default.
• W2789322052 hasConceptScore W2789322052C2777302187 @default.
• W2789322052 hasConceptScore W2789322052C2780187140 @default.
• W2789322052 hasConceptScore W2789322052C2780618852 @default.
• W2789322052 hasConceptScore W2789322052C2781148125 @default.
• W2789322052 hasConceptScore W2789322052C61721801 @default.
• W2789322052 hasConceptScore W2789322052C62476579 @default.
• W2789322052 hasConceptScore W2789322052C6494504 @default.
• W2789322052 hasConceptScore W2789322052C86803240 @default.
• W2789322052 hasFunder F4320308269 @default.
• W2789322052 hasFunder F4320321001 @default.
• W2789322052 hasFunder F4320321133 @default.
• W2789322052 hasFunder F4320322847 @default.
• W2789322052 hasLocation W27893220521 @default.
• W2789322052 hasOpenAccess W2789322052 @default.
• W2789322052 hasPrimaryLocation W27893220521 @default.
• W2789322052 hasRelatedWork W1709818596 @default.
• W2789322052 hasRelatedWork W1996236173 @default.
• W2789322052 hasRelatedWork W2004847488 @default.
• W2789322052 hasRelatedWork W2015715279 @default.
• W2789322052 hasRelatedWork W2357264803 @default.
• W2789322052 hasRelatedWork W2390259965 @default.
• W2789322052 hasRelatedWork W2407076333 @default.

• next