FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4306958879> ?p ?o ?g. }

• W4306958879 endingPage "111289" @default.
• W4306958879 startingPage "111289" @default.
• W4306958879 abstract "The relative contribution of the westerlies and the Asian monsoon has played a critical role in regulating the evolution of the Cenozoic Asian interior environment in response to regional tectonic uplift and global climate change. Here, we reconstruct a long-term record of atmospheric moisture oxygen isotopes in the Asian interior using the oxygen isotopic composition of authigenic carbonates in terrestrial sediments from the Xining Basin on the northeastern Tibetan Plateau spanning the last 52 Myrs. On the VPDB scale, the average carbonate δ18O is characterised by a long-term decrease from −1.5‰ at ca. 43 Ma to −7.5‰ at 33 Ma and smaller variations from −7‰ to −8.5‰ after 33 Ma, with the exception of one period that contains samples with higher δ18O values at −6‰ at 17–14 Ma. At the same time, there is a corresponding long-term rise in average carbon isotope δ13C values from −9.5‰ at ca. 43 Ma to −3.5‰ at 33 Ma, followed by a less variable but similar variation in δ18O values after 33 Ma. The oxygen and carbonate isotopic compositions are negatively correlated before 33 Ma and positively after, suggesting a transition at ∼33 Ma in the context of atmospheric circulation coupled with regional aridity. The δ18O record can be explained by a simple binary mixing model of the atmospheric moisture between the recycling moisture with a positive δ18O value in the westerlies-dominated region and the monsoon rainfall or related moisture with a negative δ18O value from the Indo-Pacific Ocean. In that case, the first-order carbonate δ18O decrease from ca. 43 Ma to 33 Ma was primarily controlled by the retreat of the Para-Tethys Sea, which induced a remarkable decline in westerly rainfall relative to the monsoon. After ∼33 Ma, the contribution from the westerlies could be constant and the lower limits of the carbonate δ18O values are modelled by episodic increases in monsoon rainfall corresponding to enhanced Asian monsoon periods at 26–24 Ma, 17–14 Ma, and 9–8 Ma induced by the tectonic uplift of the Tibetan Plateau and the global climate. Our study, also, suggests that the Oligocene was a transitional stage of moisture sources from the dominance of Eocene westerlies to the Miocene-Quaternary monsoon in continental Asian environments." @default.
• W4306958879 created "2022-10-21" @default.
• W4306958879 creator A5003026398 @default.
• W4306958879 creator A5016887977 @default.
• W4306958879 creator A5025530049 @default.
• W4306958879 creator A5062980907 @default.
• W4306958879 creator A5083268016 @default.
• W4306958879 date "2022-12-01" @default.
• W4306958879 modified "2023-10-15" @default.
• W4306958879 title "Terrestrial carbonate oxygen isotopes constraints on the interplay between westerlies and monsoonal rains modulating the Cenozoic climate on the northeastern Tibetan Plateau" @default.
• W4306958879 cites W1546521836 @default.
• W4306958879 cites W1571877807 @default.
• W4306958879 cites W1774412088 @default.
• W4306958879 cites W1973698825 @default.
• W4306958879 cites W1974674024 @default.
• W4306958879 cites W2003679151 @default.
• W4306958879 cites W2011253272 @default.
• W4306958879 cites W2016581298 @default.
• W4306958879 cites W2017913935 @default.
• W4306958879 cites W2017977879 @default.
• W4306958879 cites W2018828860 @default.
• W4306958879 cites W2035424634 @default.
• W4306958879 cites W2040770303 @default.
• W4306958879 cites W2041774199 @default.
• W4306958879 cites W2052031839 @default.
• W4306958879 cites W2055442076 @default.
• W4306958879 cites W2071953894 @default.
• W4306958879 cites W2072698856 @default.
• W4306958879 cites W2094108291 @default.
• W4306958879 cites W2098056587 @default.
• W4306958879 cites W2098507597 @default.
• W4306958879 cites W2099678070 @default.
• W4306958879 cites W2099985906 @default.
• W4306958879 cites W2107391155 @default.
• W4306958879 cites W2120682695 @default.
• W4306958879 cites W2129965289 @default.
• W4306958879 cites W2130176715 @default.
• W4306958879 cites W2135644396 @default.
• W4306958879 cites W2152270195 @default.
• W4306958879 cites W2164336439 @default.
• W4306958879 cites W2167965354 @default.
• W4306958879 cites W2180064451 @default.
• W4306958879 cites W2254037092 @default.
• W4306958879 cites W2391289185 @default.
• W4306958879 cites W2513653685 @default.
• W4306958879 cites W2519916942 @default.
• W4306958879 cites W2625086608 @default.
• W4306958879 cites W2760497279 @default.
• W4306958879 cites W2762943565 @default.
• W4306958879 cites W2891101351 @default.
• W4306958879 cites W2898562113 @default.
• W4306958879 cites W2903574275 @default.
• W4306958879 cites W2909604753 @default.
• W4306958879 cites W2910279170 @default.
• W4306958879 cites W2910370487 @default.
• W4306958879 cites W2910467803 @default.
• W4306958879 cites W2912025427 @default.
• W4306958879 cites W2912803914 @default.
• W4306958879 cites W2916675945 @default.
• W4306958879 cites W2935081892 @default.
• W4306958879 cites W2958420169 @default.
• W4306958879 cites W2971774951 @default.
• W4306958879 cites W3007007133 @default.
• W4306958879 cites W3023091956 @default.
• W4306958879 cites W3025530072 @default.
• W4306958879 cites W3038582643 @default.
• W4306958879 cites W3040937848 @default.
• W4306958879 cites W3083794395 @default.
• W4306958879 cites W3105133657 @default.
• W4306958879 cites W3111397166 @default.
• W4306958879 cites W3120733094 @default.
• W4306958879 cites W3128503432 @default.
• W4306958879 cites W3153115129 @default.
• W4306958879 cites W3208324825 @default.
• W4306958879 cites W976492822 @default.
• W4306958879 doi "https://doi.org/10.1016/j.palaeo.2022.111289" @default.
• W4306958879 hasPublicationYear "2022" @default.
• W4306958879 type Work @default.
• W4306958879 citedByCount "0" @default.
• W4306958879 crossrefType "journal-article" @default.
• W4306958879 hasAuthorship W4306958879A5003026398 @default.
• W4306958879 hasAuthorship W4306958879A5016887977 @default.
• W4306958879 hasAuthorship W4306958879A5025530049 @default.
• W4306958879 hasAuthorship W4306958879A5062980907 @default.
• W4306958879 hasAuthorship W4306958879A5083268016 @default.
• W4306958879 hasConcept C109007969 @default.
• W4306958879 hasConcept C114793014 @default.
• W4306958879 hasConcept C121332964 @default.
• W4306958879 hasConcept C127313418 @default.
• W4306958879 hasConcept C134306372 @default.
• W4306958879 hasConcept C136996986 @default.
• W4306958879 hasConcept C142756592 @default.
• W4306958879 hasConcept C17409809 @default.
• W4306958879 hasConcept C178790620 @default.
• W4306958879 hasConcept C185592680 @default.
• W4306958879 hasConcept C22117777 @default.
• W4306958879 hasConcept C23095489 @default.
• W4306958879 hasConcept C2780030769 @default.

• next