FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4220882008> ?p ?o ?g. }

• W4220882008 abstract "Speleothem isotope records have been widely used in the forefront of paleoclimate researches. Although the oxygen isotope (δ18O) records of speleothems remain the most commonly used hydroclimate proxy, the carbon isotope (δ13C) and trace element records of speleothem have also shown their unique advantages in charactering regional-local hydroclimate variations. In this study, we present two high-resolution (seasonal-monthly) and precisely dated speleothem δ13C records (NB2 and NB3) over the past 120 years from Niubi cave in Southeast China. Our analyses show that hydroclimate-induced changes in the regional vegetation coverage appear to be the primary control on the speleothem δ13C values over the past 120 years. However, during the late 1950s to early 1960s, a large high δ13C excursion is observed in the NB record, which is apparently linked to a special human activity in China's modern history, the so-called “Great Leap Forward in Iron and Steel”. We suggest that the large degree of damages to regional vegetation occurred during the time period resulted in the observed high speleothem δ13C values, as the local precipitation remained in an ordinary state inferred from δ18O and trace element data. The persistent decreasing trend in the NB δ13C record during the 1980–2018 CE may be attributed to the increased vegetation effect via increases in precipitation, temperature and atmosphere CO2, as well as the decrease of δ13C of atmospheric CO2." @default.
• W4220882008 created "2022-04-03" @default.
• W4220882008 creator A5010742921 @default.
• W4220882008 creator A5036693010 @default.
• W4220882008 creator A5037269066 @default.
• W4220882008 creator A5041422262 @default.
• W4220882008 creator A5065037360 @default.
• W4220882008 creator A5065852087 @default.
• W4220882008 creator A5068822161 @default.
• W4220882008 creator A5069215384 @default.
• W4220882008 creator A5071460968 @default.
• W4220882008 creator A5073995860 @default.
• W4220882008 creator A5074564038 @default.
• W4220882008 creator A5085512428 @default.
• W4220882008 date "2022-03-01" @default.
• W4220882008 modified "2023-10-16" @default.
• W4220882008 title "Climatic and anthropogenic influence on vegetation in southeastern China during the past 120 years inferred from speleothem" @default.
• W4220882008 cites W1968778244 @default.
• W4220882008 cites W1972183498 @default.
• W4220882008 cites W1974557573 @default.
• W4220882008 cites W1998572667 @default.
• W4220882008 cites W2004587064 @default.
• W4220882008 cites W2005838126 @default.
• W4220882008 cites W2020439563 @default.
• W4220882008 cites W2036499887 @default.
• W4220882008 cites W2050587035 @default.
• W4220882008 cites W2053119700 @default.
• W4220882008 cites W2056007573 @default.
• W4220882008 cites W2060341446 @default.
• W4220882008 cites W2061126774 @default.
• W4220882008 cites W2063009391 @default.
• W4220882008 cites W2073134320 @default.
• W4220882008 cites W2081074636 @default.
• W4220882008 cites W2084721764 @default.
• W4220882008 cites W2086192317 @default.
• W4220882008 cites W2088595478 @default.
• W4220882008 cites W2091494138 @default.
• W4220882008 cites W2093344609 @default.
• W4220882008 cites W2101498051 @default.
• W4220882008 cites W2110773444 @default.
• W4220882008 cites W2118469221 @default.
• W4220882008 cites W2133322244 @default.
• W4220882008 cites W2142940553 @default.
• W4220882008 cites W2199945727 @default.
• W4220882008 cites W2321825318 @default.
• W4220882008 cites W2464339816 @default.
• W4220882008 cites W2987101430 @default.
• W4220882008 cites W3092848545 @default.
• W4220882008 cites W3152901366 @default.
• W4220882008 cites W3175317274 @default.
• W4220882008 cites W3217658932 @default.
• W4220882008 doi "https://doi.org/10.1016/j.quaint.2022.02.026" @default.
• W4220882008 hasPublicationYear "2022" @default.
• W4220882008 type Work @default.
• W4220882008 citedByCount "0" @default.
• W4220882008 crossrefType "journal-article" @default.
• W4220882008 hasAuthorship W4220882008A5010742921 @default.
• W4220882008 hasAuthorship W4220882008A5036693010 @default.
• W4220882008 hasAuthorship W4220882008A5037269066 @default.
• W4220882008 hasAuthorship W4220882008A5041422262 @default.
• W4220882008 hasAuthorship W4220882008A5065037360 @default.
• W4220882008 hasAuthorship W4220882008A5065852087 @default.
• W4220882008 hasAuthorship W4220882008A5068822161 @default.
• W4220882008 hasAuthorship W4220882008A5069215384 @default.
• W4220882008 hasAuthorship W4220882008A5071460968 @default.
• W4220882008 hasAuthorship W4220882008A5073995860 @default.
• W4220882008 hasAuthorship W4220882008A5074564038 @default.
• W4220882008 hasAuthorship W4220882008A5085512428 @default.
• W4220882008 hasConcept C100970517 @default.
• W4220882008 hasConcept C107054158 @default.
• W4220882008 hasConcept C111368507 @default.
• W4220882008 hasConcept C121332964 @default.
• W4220882008 hasConcept C127313418 @default.
• W4220882008 hasConcept C132651083 @default.
• W4220882008 hasConcept C140345934 @default.
• W4220882008 hasConcept C142724271 @default.
• W4220882008 hasConcept C151730666 @default.
• W4220882008 hasConcept C153294291 @default.
• W4220882008 hasConcept C156398188 @default.
• W4220882008 hasConcept C156579228 @default.
• W4220882008 hasConcept C158787203 @default.
• W4220882008 hasConcept C166957645 @default.
• W4220882008 hasConcept C171878925 @default.
• W4220882008 hasConcept C17409809 @default.
• W4220882008 hasConcept C185059815 @default.
• W4220882008 hasConcept C18903297 @default.
• W4220882008 hasConcept C205649164 @default.
• W4220882008 hasConcept C22117777 @default.
• W4220882008 hasConcept C2776133958 @default.
• W4220882008 hasConcept C2778883040 @default.
• W4220882008 hasConcept C33683781 @default.
• W4220882008 hasConcept C34682378 @default.
• W4220882008 hasConcept C39432304 @default.
• W4220882008 hasConcept C49204034 @default.
• W4220882008 hasConcept C62520636 @default.
• W4220882008 hasConcept C69384203 @default.
• W4220882008 hasConcept C71924100 @default.
• W4220882008 hasConcept C86803240 @default.
• W4220882008 hasConceptScore W4220882008C100970517 @default.
• W4220882008 hasConceptScore W4220882008C107054158 @default.

• next