FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2035697773> ?p ?o ?g. }

• W2035697773 endingPage "160" @default.
• W2035697773 startingPage "147" @default.
• W2035697773 abstract "During several joint Chinese–German expeditions, the Quaternary landscape and paleoclimatic evolution of the mountain ranges and grabens surrounding the Loess Plateau of central China was studied. The results are compared with proxy data from the interior Loess Plateau, to help reconstruct atmospheric circulation during Late Pleistocene times. Middle to Late Pleistocene alluvial terraces and fans, capped with loess units and paleosols, show that aggradational episodes correlate with periods of glaciation and increased loess accumulation. In turn, degradation correlates with interglacials or interstadials and increased soil formation. This implies that climate is the primary control on Quaternary paleohydrology and alluvial sedimentation and erosion. The high mountains, which barely reached the last glacial ELA, were only glaciated during the most favourable climatic period of glaciation. The glaciation, the glacial and alluvial forms point to a cool early to maximum glacial period with increased precipitation and to a maximum to final period with cold–dry conditions. During the last glaciation, the maximum advance of the small glaciers took place towards the end of a relatively humid and cold period between ca. 32 and 23 ka. The following dry–cold stage between ca. 23 and 13 ka was rather unfavourable for glacial advance. Proxy data from the Loess Plateau supports the view, that glaciations were more or less dominated by cold–dry winter monsoon climate, whereas during the interglacial/interstadials a warmer and more humid climate prevailed, implying a strengthening of the summer monsoon influence. The results prove variations of the monsoon, that in turn modulates paleohydrology, periglacial dynamics, glacier advances, dust flux and soil formation." @default.
• W2035697773 created "2016-06-24" @default.
• W2035697773 creator A5084255651 @default.
• W2035697773 date "2000-04-01" @default.
• W2035697773 modified "2023-09-27" @default.
• W2035697773 title "Pleistocene paleoenvironmental changes in the high mountain ranges of central China and adjacent regions" @default.
• W2035697773 cites W1996437630 @default.
• W2035697773 cites W2008642188 @default.
• W2035697773 cites W2012108278 @default.
• W2035697773 cites W2012324561 @default.
• W2035697773 cites W2015285597 @default.
• W2035697773 cites W2021150751 @default.
• W2035697773 cites W2021277058 @default.
• W2035697773 cites W2023013227 @default.
• W2035697773 cites W2025255739 @default.
• W2035697773 cites W2031368983 @default.
• W2035697773 cites W2040399010 @default.
• W2035697773 cites W2050311837 @default.
• W2035697773 cites W2050609645 @default.
• W2035697773 cites W2052971706 @default.
• W2035697773 cites W2054833444 @default.
• W2035697773 cites W2054897620 @default.
• W2035697773 cites W2055353337 @default.
• W2035697773 cites W2055583031 @default.
• W2035697773 cites W2055792591 @default.
• W2035697773 cites W2061780966 @default.
• W2035697773 cites W2061988632 @default.
• W2035697773 cites W2074034719 @default.
• W2035697773 cites W2095518472 @default.
• W2035697773 cites W2321483993 @default.
• W2035697773 cites W4299346994 @default.
• W2035697773 doi "https://doi.org/10.1016/s1040-6182(99)00041-5" @default.
• W2035697773 hasPublicationYear "2000" @default.
• W2035697773 type Work @default.
• W2035697773 sameAs 2035697773 @default.
• W2035697773 citedByCount "48" @default.
• W2035697773 countsByYear W20356977732012 @default.
• W2035697773 countsByYear W20356977732013 @default.
• W2035697773 countsByYear W20356977732015 @default.
• W2035697773 countsByYear W20356977732016 @default.
• W2035697773 countsByYear W20356977732017 @default.
• W2035697773 countsByYear W20356977732018 @default.
• W2035697773 countsByYear W20356977732019 @default.
• W2035697773 countsByYear W20356977732020 @default.
• W2035697773 countsByYear W20356977732021 @default.
• W2035697773 countsByYear W20356977732022 @default.
• W2035697773 countsByYear W20356977732023 @default.
• W2035697773 crossrefType "journal-article" @default.
• W2035697773 hasAuthorship W2035697773A5084255651 @default.
• W2035697773 hasConcept C100834320 @default.
• W2035697773 hasConcept C100970517 @default.
• W2035697773 hasConcept C111368507 @default.
• W2035697773 hasConcept C127313418 @default.
• W2035697773 hasConcept C132651083 @default.
• W2035697773 hasConcept C136996986 @default.
• W2035697773 hasConcept C151730666 @default.
• W2035697773 hasConcept C15739521 @default.
• W2035697773 hasConcept C160464908 @default.
• W2035697773 hasConcept C185515318 @default.
• W2035697773 hasConcept C186240526 @default.
• W2035697773 hasConcept C188291805 @default.
• W2035697773 hasConcept C205649164 @default.
• W2035697773 hasConcept C33683781 @default.
• W2035697773 hasConcept C49204034 @default.
• W2035697773 hasConcept C53570757 @default.
• W2035697773 hasConcept C65814071 @default.
• W2035697773 hasConcept C76123530 @default.
• W2035697773 hasConceptScore W2035697773C100834320 @default.
• W2035697773 hasConceptScore W2035697773C100970517 @default.
• W2035697773 hasConceptScore W2035697773C111368507 @default.
• W2035697773 hasConceptScore W2035697773C127313418 @default.
• W2035697773 hasConceptScore W2035697773C132651083 @default.
• W2035697773 hasConceptScore W2035697773C136996986 @default.
• W2035697773 hasConceptScore W2035697773C151730666 @default.
• W2035697773 hasConceptScore W2035697773C15739521 @default.
• W2035697773 hasConceptScore W2035697773C160464908 @default.
• W2035697773 hasConceptScore W2035697773C185515318 @default.
• W2035697773 hasConceptScore W2035697773C186240526 @default.
• W2035697773 hasConceptScore W2035697773C188291805 @default.
• W2035697773 hasConceptScore W2035697773C205649164 @default.
• W2035697773 hasConceptScore W2035697773C33683781 @default.
• W2035697773 hasConceptScore W2035697773C49204034 @default.
• W2035697773 hasConceptScore W2035697773C53570757 @default.
• W2035697773 hasConceptScore W2035697773C65814071 @default.
• W2035697773 hasConceptScore W2035697773C76123530 @default.
• W2035697773 hasLocation W20356977731 @default.
• W2035697773 hasOpenAccess W2035697773 @default.
• W2035697773 hasPrimaryLocation W20356977731 @default.
• W2035697773 hasRelatedWork W2030147696 @default.
• W2035697773 hasRelatedWork W2080372345 @default.
• W2035697773 hasRelatedWork W2086394837 @default.
• W2035697773 hasRelatedWork W2164238648 @default.
• W2035697773 hasRelatedWork W2791550625 @default.
• W2035697773 hasRelatedWork W2912828907 @default.
• W2035697773 hasRelatedWork W3134571911 @default.
• W2035697773 hasRelatedWork W3140641473 @default.
• W2035697773 hasRelatedWork W3149400631 @default.
• W2035697773 hasRelatedWork W4232401073 @default.

• next