FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3209724633> ?p ?o ?g. }

• W3209724633 endingPage "107258" @default.
• W3209724633 startingPage "107258" @default.
• W3209724633 abstract "The paper presents a comprehensive review on lake-level history of Qinghai Lake since marine isotope stage (MIS) 5, after re-examining the sedimentary and geomorphological nature of highstand deposits and re-evaluating the published dating results (318 luminescence ages and 17 14C ages) of shorelines, near shoreline, lacustrine, alluvial, and aeolian deposits. It is concluded that 1) Three lake shoreline sets were classified in the Qinghai Lake Basin with the corresponding elevations of 3220–3260, 3206–3215 and 3194–3205 m. 2) 14C dating on lake sediments is restricted by the upper dating limit of ∼35 thousand years (ka) BP in practice, availability of dating materials and reservoir effect, and that quartz optically stimulated luminescence (OSL) ages older than 80–60 ka may be underestimated while feldspar post-infrared infrared stimulated luminescence (pIRIR) ages could be reliable for dating these older samples. 3) Four highstands were detected by ages. The highest lake-levels at elevations of 3220–3260 m with 26–66 m above the present lake-level occurred in MIS 5, and highstands also occurred in MIS 3 (∼42–38 ka), the last deglaciation (∼16–12 ka), and the Holocene (∼6–5 ka) with similar heights at elevations of ∼3200–3209 m. During the Holocene, lake-levels were relatively low in the early Holocene (∼11–8 ka), increasing substantially after ∼8 ka and reaching the highest lake-levels (elevation of 3203.1 m) at ∼6–5 ka, then decreasing with an interruption by a highstand (elevation of 3202.4 m) at ∼1.8 ka. 4) Shoreline-based lake-level variations are consistent with major climatic proxies (e.g., δ13Corg and %thaum) of drilling cores from the lake, regional aeolian activity/pedogenesis and climate change. 5) Compared with the representative lake-levels and moisture records in the Westerlies and East Asia summer monsoon (EASM) dominances, it is suggested that lake-level variations in the southern Qilian Mountains exhibited simultaneity with changes in the intensity of EASM, while those in the northern part were synchronous with the moisture records in arid central Asia, suggesting that EASM did not extend further to the northern Qilian Mountains where the Westerlies prevailed." @default.
• W3209724633 created "2021-11-08" @default.
• W3209724633 creator A5039893067 @default.
• W3209724633 creator A5046345934 @default.
• W3209724633 creator A5067702320 @default.
• W3209724633 creator A5075815385 @default.
• W3209724633 date "2021-12-01" @default.
• W3209724633 modified "2023-10-17" @default.
• W3209724633 title "Lake-level history of Qinghai Lake on the NE Tibetan Plateau and its implications for Asian monsoon pattern - A review" @default.
• W3209724633 cites W1240312767 @default.
• W3209724633 cites W1547357997 @default.
• W3209724633 cites W1766766367 @default.
• W3209724633 cites W1873522794 @default.
• W3209724633 cites W1899663275 @default.
• W3209724633 cites W1957039123 @default.
• W3209724633 cites W1966468376 @default.
• W3209724633 cites W1971566635 @default.
• W3209724633 cites W1974629649 @default.
• W3209724633 cites W1981477554 @default.
• W3209724633 cites W1982071821 @default.
• W3209724633 cites W1984683396 @default.
• W3209724633 cites W1985420352 @default.
• W3209724633 cites W1986663262 @default.
• W3209724633 cites W1989268475 @default.
• W3209724633 cites W1989643610 @default.
• W3209724633 cites W1994458240 @default.
• W3209724633 cites W1994758570 @default.
• W3209724633 cites W1999745977 @default.
• W3209724633 cites W2000655296 @default.
• W3209724633 cites W2000891916 @default.
• W3209724633 cites W2005300331 @default.
• W3209724633 cites W2010651073 @default.
• W3209724633 cites W2013878295 @default.
• W3209724633 cites W2015492949 @default.
• W3209724633 cites W2024001474 @default.
• W3209724633 cites W2024583496 @default.
• W3209724633 cites W2030062413 @default.
• W3209724633 cites W2033839798 @default.
• W3209724633 cites W2036258677 @default.
• W3209724633 cites W2038128466 @default.
• W3209724633 cites W2040399010 @default.
• W3209724633 cites W2045398401 @default.
• W3209724633 cites W2048742978 @default.
• W3209724633 cites W2048989325 @default.
• W3209724633 cites W2049696180 @default.
• W3209724633 cites W2051204190 @default.
• W3209724633 cites W2051773982 @default.
• W3209724633 cites W2054167812 @default.
• W3209724633 cites W2054268913 @default.
• W3209724633 cites W2055792591 @default.
• W3209724633 cites W2056891117 @default.
• W3209724633 cites W2058894612 @default.
• W3209724633 cites W2060874043 @default.
• W3209724633 cites W2066487271 @default.
• W3209724633 cites W2068418136 @default.
• W3209724633 cites W2071061666 @default.
• W3209724633 cites W2071101781 @default.
• W3209724633 cites W2071632003 @default.
• W3209724633 cites W2080480192 @default.
• W3209724633 cites W2081400988 @default.
• W3209724633 cites W2082114398 @default.
• W3209724633 cites W2096484028 @default.
• W3209724633 cites W2097481580 @default.
• W3209724633 cites W2105848941 @default.
• W3209724633 cites W2111212031 @default.
• W3209724633 cites W2111590126 @default.
• W3209724633 cites W2117551699 @default.
• W3209724633 cites W2117827079 @default.
• W3209724633 cites W2123793538 @default.
• W3209724633 cites W2145431934 @default.
• W3209724633 cites W2146164822 @default.
• W3209724633 cites W2148361166 @default.
• W3209724633 cites W2153754396 @default.
• W3209724633 cites W2154624923 @default.
• W3209724633 cites W2169688799 @default.
• W3209724633 cites W2172709381 @default.
• W3209724633 cites W2173251738 @default.
• W3209724633 cites W2266279946 @default.
• W3209724633 cites W2404462665 @default.
• W3209724633 cites W2473752769 @default.
• W3209724633 cites W2507506815 @default.
• W3209724633 cites W2510459335 @default.
• W3209724633 cites W2553106456 @default.
• W3209724633 cites W2584621696 @default.
• W3209724633 cites W2591352480 @default.
• W3209724633 cites W2593810770 @default.
• W3209724633 cites W2605848685 @default.
• W3209724633 cites W2609777692 @default.
• W3209724633 cites W2619799759 @default.
• W3209724633 cites W2623995715 @default.
• W3209724633 cites W2791692308 @default.
• W3209724633 cites W2791732754 @default.
• W3209724633 cites W2792680039 @default.
• W3209724633 cites W2795983788 @default.
• W3209724633 cites W2802211863 @default.
• W3209724633 cites W2809003113 @default.
• W3209724633 cites W2810732729 @default.
• W3209724633 cites W2884316213 @default.

• next