FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2885261657> ?p ?o ?g. }

• W2885261657 endingPage "48" @default.
• W2885261657 startingPage "35" @default.
• W2885261657 abstract "The collision between India and Eurasia and the subsequent uplift of the Qinghai–Xizang plateau region of the Eurasian continent during the latest Mesozoic and Cenozoic had a significant environmental impact on the region. Understanding the vegetation of both palaeocontinents prior to the collision is crucial for interpreting the evolution of their floras and climatic changes during this period. The composition of the vegetation and climate of the plateau from the Middle Jurassic until the end of the Oligocene are inferred herein from the composition of 14 palynofloras and compared with other regions of China. The palynofloras are similar to those of eastern and northwestern parts of China but bear their own unique features brought about by differing climatic influences. Overall, a warm–hot, arid–semi-arid climate prevailed over the plateau during most of the period from the Middle Jurassic until the end of the Cretaceous. The climate cooled and humidity increased in the Paleogene, and especially during the Oligocene. The long-term climatic change in the Qinghai–Xizang plateau region of the Eurasian continent during the Middle Jurassic–Paleogene that is indicated by the miospore assemblages is broadly comparable to the isotope-based SST (sea-surface temperature) changes that have been identified. It is apparent that climatic changes on a global scale were primarily responsible for controlling the composition and distribution of the vegetation on the plateau; no monsoon features are detectable in the northwestern interior of China. A maximum estimation of 2890 m surface palaeoelevation is inferred for the central and northern plateau during the Oligocene based on vegetation analysis, which is lower than previous estimations based on oxygen isotope and coexistence analyses. The elevation of the southern part of the study area, i.e. the area south of the Gandise Mountains, was low, close to sea-level." @default.
• W2885261657 created "2018-08-22" @default.
• W2885261657 creator A5016560378 @default.
• W2885261657 creator A5031514811 @default.
• W2885261657 creator A5064146459 @default.
• W2885261657 creator A5075577831 @default.
• W2885261657 date "2019-05-01" @default.
• W2885261657 modified "2023-10-15" @default.
• W2885261657 title "Vegetation and climate of the central and northern Qinghai–Xizang plateau from the Middle Jurassic to the end of the Paleogene inferred from palynology" @default.
• W2885261657 cites W1571584391 @default.
• W2885261657 cites W1637856870 @default.
• W2885261657 cites W1959048442 @default.
• W2885261657 cites W1968771872 @default.
• W2885261657 cites W1969685321 @default.
• W2885261657 cites W1974467019 @default.
• W2885261657 cites W1976467450 @default.
• W2885261657 cites W1977613474 @default.
• W2885261657 cites W1986254813 @default.
• W2885261657 cites W1994476706 @default.
• W2885261657 cites W1997758176 @default.
• W2885261657 cites W1999924690 @default.
• W2885261657 cites W2000746384 @default.
• W2885261657 cites W2002325302 @default.
• W2885261657 cites W2012170355 @default.
• W2885261657 cites W2016760315 @default.
• W2885261657 cites W2027993166 @default.
• W2885261657 cites W2032185537 @default.
• W2885261657 cites W2032772121 @default.
• W2885261657 cites W2034283902 @default.
• W2885261657 cites W2034597289 @default.
• W2885261657 cites W2041774199 @default.
• W2885261657 cites W2050487135 @default.
• W2885261657 cites W2055356153 @default.
• W2885261657 cites W2060188274 @default.
• W2885261657 cites W2071483826 @default.
• W2885261657 cites W2078635223 @default.
• W2885261657 cites W2084899260 @default.
• W2885261657 cites W2089069736 @default.
• W2885261657 cites W2093114941 @default.
• W2885261657 cites W2096276260 @default.
• W2885261657 cites W2114125023 @default.
• W2885261657 cites W2115518283 @default.
• W2885261657 cites W2116868398 @default.
• W2885261657 cites W2121568633 @default.
• W2885261657 cites W2135640029 @default.
• W2885261657 cites W2140736107 @default.
• W2885261657 cites W2141391066 @default.
• W2885261657 cites W2161702350 @default.
• W2885261657 cites W2605276217 @default.
• W2885261657 doi "https://doi.org/10.1016/j.jseaes.2018.08.012" @default.
• W2885261657 hasPublicationYear "2019" @default.
• W2885261657 type Work @default.
• W2885261657 sameAs 2885261657 @default.
• W2885261657 citedByCount "9" @default.
• W2885261657 countsByYear W28852616572020 @default.
• W2885261657 countsByYear W28852616572021 @default.
• W2885261657 countsByYear W28852616572022 @default.
• W2885261657 countsByYear W28852616572023 @default.
• W2885261657 crossrefType "journal-article" @default.
• W2885261657 hasAuthorship W2885261657A5016560378 @default.
• W2885261657 hasAuthorship W2885261657A5031514811 @default.
• W2885261657 hasAuthorship W2885261657A5064146459 @default.
• W2885261657 hasAuthorship W2885261657A5075577831 @default.
• W2885261657 hasConcept C100970517 @default.
• W2885261657 hasConcept C109007969 @default.
• W2885261657 hasConcept C111368507 @default.
• W2885261657 hasConcept C117935615 @default.
• W2885261657 hasConcept C121332964 @default.
• W2885261657 hasConcept C12294951 @default.
• W2885261657 hasConcept C127313418 @default.
• W2885261657 hasConcept C132651083 @default.
• W2885261657 hasConcept C134306372 @default.
• W2885261657 hasConcept C136996986 @default.
• W2885261657 hasConcept C140345934 @default.
• W2885261657 hasConcept C142724271 @default.
• W2885261657 hasConcept C150772632 @default.
• W2885261657 hasConcept C151730666 @default.
• W2885261657 hasConcept C162501224 @default.
• W2885261657 hasConcept C18903297 @default.
• W2885261657 hasConcept C204330871 @default.
• W2885261657 hasConcept C205649164 @default.
• W2885261657 hasConcept C23095489 @default.
• W2885261657 hasConcept C24890656 @default.
• W2885261657 hasConcept C2776133958 @default.
• W2885261657 hasConcept C2777802808 @default.
• W2885261657 hasConcept C2780030769 @default.
• W2885261657 hasConcept C2780618852 @default.
• W2885261657 hasConcept C2781291010 @default.
• W2885261657 hasConcept C33923547 @default.
• W2885261657 hasConcept C49204034 @default.
• W2885261657 hasConcept C71924100 @default.
• W2885261657 hasConcept C73707237 @default.
• W2885261657 hasConcept C86803240 @default.
• W2885261657 hasConceptScore W2885261657C100970517 @default.
• W2885261657 hasConceptScore W2885261657C109007969 @default.
• W2885261657 hasConceptScore W2885261657C111368507 @default.
• W2885261657 hasConceptScore W2885261657C117935615 @default.
• W2885261657 hasConceptScore W2885261657C121332964 @default.

• next