FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2914496502> ?p ?o ?g. }

• W2914496502 endingPage "7" @default.
• W2914496502 startingPage "1" @default.
• W2914496502 abstract "The timing and structure of Termination II (T-II) is still debatable as the number of high-quality records is insufficient. This study presents precisely dated stalagmite δ18O data between 133.4±0.3 to 126.6±0.3 ka BP (covering most of T-II) from north China, near the northern limit of the East Asian summer monsoon (EASM), an area sensitive to climate change. The onset of the last interglacial is constrained at 129.4±0.3 ka BP, consistent with south Chinese speleothem records, further supporting the idea that Northern Hemisphere summer insolation plays an important role in initiating glacial terminations. An extended interval of heavy δ18O is observed immediately prior to this abrupt transition, named as the “Weak Monsoon Interval” (WMI) in south Chinese cave records, which was associated with the Heinrich Stadial 11 (H11) in the North Atlantic. A significant millennial-scale interstadial peaking at 132.7±0.3 ka BP is identified preceding the weakest phase of the WMI. A synchronous counterpart is also found in some south Chinese speleothem and North Atlantic alkenone Mg/Ca SST records. It is inferred that the main H11 freshwater penetration possibly occurred after 131.5 ka BP, leaving some aspects of ocean and atmospheric circulation still in interstadial mode from 134 to 131.5 ka BP. Following the onset of the last interglacial, there was a millennial-scale “pause” in our δ18O record, synchronized with a “slowdown” in the rate of decrease in δ18O in south Chinese cave records. This is possibly a large regional climate oscillation, as it is also identified in some North Atlantic records, but one which is too weak to be a Younger Dryas (YD)-type event. In summary, compared to south Chinese cave records, significant millennial-scale climate oscillations before and after the synchronous onset of the last interglacial is the main feature of our record. Nevertheless, the sequence of these climate events remains very different from Termination I (T-I), which is possibly ascribed to the stronger insolation, higher atmosphere CO2, and the resultant faster and greater meltwater pulse to the North Atlantic during T-II than during T-I." @default.
• W2914496502 created "2019-02-21" @default.
• W2914496502 creator A5000787646 @default.
• W2914496502 creator A5007139673 @default.
• W2914496502 creator A5020270533 @default.
• W2914496502 creator A5023065107 @default.
• W2914496502 creator A5057788539 @default.
• W2914496502 date "2019-04-01" @default.
• W2914496502 modified "2023-10-17" @default.
• W2914496502 title "Timing and structure of Termination II in north China constrained by a precisely dated stalagmite record" @default.
• W2914496502 cites W1016151245 @default.
• W2914496502 cites W1510553457 @default.
• W2914496502 cites W1511524149 @default.
• W2914496502 cites W1598369120 @default.
• W2914496502 cites W1738999171 @default.
• W2914496502 cites W1889491352 @default.
• W2914496502 cites W1967596498 @default.
• W2914496502 cites W1978206086 @default.
• W2914496502 cites W1978347718 @default.
• W2914496502 cites W1982150954 @default.
• W2914496502 cites W1984682253 @default.
• W2914496502 cites W1987571636 @default.
• W2914496502 cites W1994007098 @default.
• W2914496502 cites W2004587064 @default.
• W2914496502 cites W2006518213 @default.
• W2914496502 cites W2015252820 @default.
• W2914496502 cites W2026828112 @default.
• W2914496502 cites W2026976482 @default.
• W2914496502 cites W2027385173 @default.
• W2914496502 cites W2028658915 @default.
• W2914496502 cites W2035647653 @default.
• W2914496502 cites W2042476750 @default.
• W2914496502 cites W2052814244 @default.
• W2914496502 cites W2054647796 @default.
• W2914496502 cites W2059588660 @default.
• W2914496502 cites W2063009391 @default.
• W2914496502 cites W2074551196 @default.
• W2914496502 cites W2077280380 @default.
• W2914496502 cites W2083519852 @default.
• W2914496502 cites W2086192317 @default.
• W2914496502 cites W2089028175 @default.
• W2914496502 cites W2092697663 @default.
• W2914496502 cites W2100027246 @default.
• W2914496502 cites W2103402476 @default.
• W2914496502 cites W2113988819 @default.
• W2914496502 cites W2114031949 @default.
• W2914496502 cites W2118324297 @default.
• W2914496502 cites W2125275246 @default.
• W2914496502 cites W2133747346 @default.
• W2914496502 cites W2135377114 @default.
• W2914496502 cites W2141643578 @default.
• W2914496502 cites W2141812989 @default.
• W2914496502 cites W2147061362 @default.
• W2914496502 cites W2159304277 @default.
• W2914496502 cites W2161480748 @default.
• W2914496502 cites W2259983367 @default.
• W2914496502 cites W2335961020 @default.
• W2914496502 cites W2338996410 @default.
• W2914496502 cites W2510138258 @default.
• W2914496502 cites W2888123502 @default.
• W2914496502 cites W2896170448 @default.
• W2914496502 doi "https://doi.org/10.1016/j.epsl.2019.01.043" @default.
• W2914496502 hasPublicationYear "2019" @default.
• W2914496502 type Work @default.
• W2914496502 sameAs 2914496502 @default.
• W2914496502 citedByCount "10" @default.
• W2914496502 countsByYear W29144965022020 @default.
• W2914496502 countsByYear W29144965022021 @default.
• W2914496502 countsByYear W29144965022022 @default.
• W2914496502 countsByYear W29144965022023 @default.
• W2914496502 crossrefType "journal-article" @default.
• W2914496502 hasAuthorship W2914496502A5000787646 @default.
• W2914496502 hasAuthorship W2914496502A5007139673 @default.
• W2914496502 hasAuthorship W2914496502A5020270533 @default.
• W2914496502 hasAuthorship W2914496502A5023065107 @default.
• W2914496502 hasAuthorship W2914496502A5057788539 @default.
• W2914496502 hasBestOaLocation W29144965021 @default.
• W2914496502 hasConcept C111368507 @default.
• W2914496502 hasConcept C121332964 @default.
• W2914496502 hasConcept C127313418 @default.
• W2914496502 hasConcept C136996986 @default.
• W2914496502 hasConcept C140345934 @default.
• W2914496502 hasConcept C151730666 @default.
• W2914496502 hasConcept C156579228 @default.
• W2914496502 hasConcept C15739521 @default.
• W2914496502 hasConcept C166957645 @default.
• W2914496502 hasConcept C171878925 @default.
• W2914496502 hasConcept C186240526 @default.
• W2914496502 hasConcept C205649164 @default.
• W2914496502 hasConcept C22117777 @default.
• W2914496502 hasConcept C23095489 @default.
• W2914496502 hasConcept C2778835443 @default.
• W2914496502 hasConcept C2778883040 @default.
• W2914496502 hasConcept C49204034 @default.
• W2914496502 hasConcept C62520636 @default.
• W2914496502 hasConcept C65814071 @default.
• W2914496502 hasConcept C69384203 @default.
• W2914496502 hasConceptScore W2914496502C111368507 @default.

• next