FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4311753804> ?p ?o ?g. }

• W4311753804 endingPage "111352" @default.
• W4311753804 startingPage "111352" @default.
• W4311753804 abstract "Knowledge of centennial-scale hydroclimate variability and underlying forcing mechanisms in southern China over the last two millennia remains limited. This study presents multiproxy results of the grain size, elemental ratios (Zr/Rb, and Rb/Sr), total organic carbon (TOC), total nitrogen (TN) and C/N ratios, together with high-precision 137Cs/210Pb and accelerator mass spectrometry (AMS) 14C ages of a sediment core from Lake Baxian, which is a small closed lake in Guangxi Province, southern China. Based on these high-resolution data, the hydroclimate change over the last two millennia is clearly revealed. Relatively high values of the mean grain size, Zr/Rb, TOC and TN, along with low values of Rb/Sr and C/N ratios during the Dark Ages Cold Period (DACP, 500–900 CE) and Little Ice Age (LIA, 1400–1850 CE), indicate a relatively wet climate during these intervals. Conversely, low values of the mean grain size, Zr/Rb, TOC and TN, along with high Rb/Sr ratios during the Roman Warm Period (RWP, 50–400 CE) and Medieval Climate Anomaly (MCA, 1000–1300 CE), suggest relatively dry conditions during these intervals. During the Current Warm Period (CWP, 1850-present), the values of the mean grain size and Zr/Rb increase abruptly and Rb/Sr ratios exhibit large fluctuations, which might be attributed to the impact of human activities. The general pattern of the reconstructed hydroclimate variations in this study is broadly consistent with the North Atlantic ice-rafted detritus and Indo-Pacific Warm Pool (IPWP) records, indicating that the hydroclimate variability on the centennial-scale in southern China has been controlled by both high- and low- latitude forcings over the last two millennia." @default.
• W4311753804 created "2022-12-28" @default.
• W4311753804 creator A5000097978 @default.
• W4311753804 creator A5000827993 @default.
• W4311753804 creator A5008451272 @default.
• W4311753804 creator A5031319811 @default.
• W4311753804 creator A5039638660 @default.
• W4311753804 creator A5042314019 @default.
• W4311753804 creator A5050934604 @default.
• W4311753804 creator A5073110596 @default.
• W4311753804 date "2023-01-01" @default.
• W4311753804 modified "2023-10-16" @default.
• W4311753804 title "High- and low- latitude forcing on hydroclimate variability in southern China over the last two millennia" @default.
• W4311753804 cites W1034987454 @default.
• W4311753804 cites W1498045143 @default.
• W4311753804 cites W1964105245 @default.
• W4311753804 cites W1968630644 @default.
• W4311753804 cites W1968832695 @default.
• W4311753804 cites W1976300365 @default.
• W4311753804 cites W1984655738 @default.
• W4311753804 cites W1984879127 @default.
• W4311753804 cites W1986748464 @default.
• W4311753804 cites W1990899433 @default.
• W4311753804 cites W2007012175 @default.
• W4311753804 cites W2007619330 @default.
• W4311753804 cites W2009607369 @default.
• W4311753804 cites W2013428409 @default.
• W4311753804 cites W2013836135 @default.
• W4311753804 cites W2016349369 @default.
• W4311753804 cites W2027025402 @default.
• W4311753804 cites W2028249130 @default.
• W4311753804 cites W2030603636 @default.
• W4311753804 cites W2037587407 @default.
• W4311753804 cites W2045099339 @default.
• W4311753804 cites W2046697924 @default.
• W4311753804 cites W2048101491 @default.
• W4311753804 cites W2052814244 @default.
• W4311753804 cites W2060139201 @default.
• W4311753804 cites W2060509986 @default.
• W4311753804 cites W2064889999 @default.
• W4311753804 cites W2064983008 @default.
• W4311753804 cites W2071932482 @default.
• W4311753804 cites W2078377676 @default.
• W4311753804 cites W2089168708 @default.
• W4311753804 cites W2089986131 @default.
• W4311753804 cites W2091926733 @default.
• W4311753804 cites W2092651219 @default.
• W4311753804 cites W2096644508 @default.
• W4311753804 cites W2101108516 @default.
• W4311753804 cites W2113361120 @default.
• W4311753804 cites W2135496572 @default.
• W4311753804 cites W2138634218 @default.
• W4311753804 cites W2149010791 @default.
• W4311753804 cites W2163464784 @default.
• W4311753804 cites W2168286357 @default.
• W4311753804 cites W2171474499 @default.
• W4311753804 cites W2317768307 @default.
• W4311753804 cites W2322094486 @default.
• W4311753804 cites W2376979291 @default.
• W4311753804 cites W2379432279 @default.
• W4311753804 cites W2416348078 @default.
• W4311753804 cites W2468173648 @default.
• W4311753804 cites W2516717492 @default.
• W4311753804 cites W2517167870 @default.
• W4311753804 cites W2578390297 @default.
• W4311753804 cites W2603675725 @default.
• W4311753804 cites W2744483661 @default.
• W4311753804 cites W2754740953 @default.
• W4311753804 cites W2884193256 @default.
• W4311753804 cites W2899343070 @default.
• W4311753804 cites W2899736810 @default.
• W4311753804 cites W2901924073 @default.
• W4311753804 cites W2936232392 @default.
• W4311753804 cites W2950700884 @default.
• W4311753804 cites W2975748475 @default.
• W4311753804 cites W2999085096 @default.
• W4311753804 cites W3004351463 @default.
• W4311753804 cites W3007734438 @default.
• W4311753804 cites W3015380626 @default.
• W4311753804 cites W3015391807 @default.
• W4311753804 cites W3083227125 @default.
• W4311753804 cites W3184293327 @default.
• W4311753804 cites W3184633249 @default.
• W4311753804 cites W3202915907 @default.
• W4311753804 cites W4210325382 @default.
• W4311753804 cites W4246027503 @default.
• W4311753804 cites W4306810309 @default.
• W4311753804 cites W521639 @default.
• W4311753804 doi "https://doi.org/10.1016/j.palaeo.2022.111352" @default.
• W4311753804 hasPublicationYear "2023" @default.
• W4311753804 type Work @default.
• W4311753804 citedByCount "1" @default.
• W4311753804 countsByYear W43117538042023 @default.
• W4311753804 crossrefType "journal-article" @default.
• W4311753804 hasAuthorship W4311753804A5000097978 @default.
• W4311753804 hasAuthorship W4311753804A5000827993 @default.
• W4311753804 hasAuthorship W4311753804A5008451272 @default.
• W4311753804 hasAuthorship W4311753804A5031319811 @default.

• next