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- W3092586919 abstract "Stable organic carbon and nitrogen isotopes can be used to interpret past vegetation patterns and ecosystem qualities. Here we present these proxies for two loess‐palaeosol sequences from the southern Carpathian Basin to reconstruct the palaeoenvironment during the past 350 ka and establish regional commonalities and differences. Before now, isotopic studies on loess sequences from this region were only conducted on deposits from the last glacial cycle. We conducted methodological tests involving the complete decalcification of the samples prior to stable isotope analyses. Two decalcification methods (fumigation method and wet chemical acidification), different treatment times, and the reproducibility of carbon isotope analyses were tested. Obtained results indicate that the choice of the decalcification method is important for organic carbon stable isotope analyses of loess‐palaeosol sequences because ratios vary by more than 10‰ between the wet chemical and fumigation methods, due to incomplete carbonate removal by the latter. Therefore, we suggest avoiding the fumigation method for studies on loess‐palaeosol sequences. In addition, our data show that samples with TOC content <0.2% bear increased potential for misinterpretation of their carbon isotope ratios. For our sites, C 3 ‐vegetation is predominant and no palaeoenvironmental shifts leading to a change of the dominant photosynthesis pathway can be detected during the Middle to Late Pleistocene. Furthermore, the importance of further stable nitrogen isotope studies is highlighted, since this proxy seems to reflect past precipitation patterns and reveals favourable conditions in the southern Carpathian Basin, especially during interstadials." @default.
- W3092586919 created "2020-10-15" @default.
- W3092586919 creator A5003012432 @default.
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- W3092586919 date "2020-10-06" @default.
- W3092586919 modified "2023-10-17" @default.
- W3092586919 title "Middle to Late Pleistocene environments based on stable organic carbon and nitrogen isotopes of loess‐palaeosol sequences from the Carpathian Basin" @default.
- W3092586919 cites W1542631547 @default.
- W3092586919 cites W1571318702 @default.
- W3092586919 cites W1600254138 @default.
- W3092586919 cites W1899286304 @default.
- W3092586919 cites W1966751137 @default.
- W3092586919 cites W1967337985 @default.
- W3092586919 cites W1969422783 @default.
- W3092586919 cites W1972113362 @default.
- W3092586919 cites W1973095033 @default.
- W3092586919 cites W1973422613 @default.
- W3092586919 cites W1975783446 @default.
- W3092586919 cites W1977151751 @default.
- W3092586919 cites W1979358171 @default.
- W3092586919 cites W1983088895 @default.
- W3092586919 cites W1986469614 @default.
- W3092586919 cites W1989682203 @default.
- W3092586919 cites W1990294291 @default.
- W3092586919 cites W1994914827 @default.
- W3092586919 cites W1995160959 @default.
- W3092586919 cites W1995375834 @default.
- W3092586919 cites W1995732740 @default.
- W3092586919 cites W1997062636 @default.
- W3092586919 cites W1997211819 @default.
- W3092586919 cites W1998371736 @default.
- W3092586919 cites W2000261909 @default.
- W3092586919 cites W2001035747 @default.
- W3092586919 cites W2005435672 @default.
- W3092586919 cites W2006004149 @default.
- W3092586919 cites W2006571602 @default.
- W3092586919 cites W2008555110 @default.
- W3092586919 cites W2012045156 @default.
- W3092586919 cites W2013556228 @default.
- W3092586919 cites W2015215683 @default.
- W3092586919 cites W2016754172 @default.
- W3092586919 cites W2017704156 @default.
- W3092586919 cites W2017749448 @default.
- W3092586919 cites W2018984403 @default.
- W3092586919 cites W2022652437 @default.
- W3092586919 cites W2023126057 @default.
- W3092586919 cites W2027099455 @default.
- W3092586919 cites W2028085751 @default.
- W3092586919 cites W2030794362 @default.
- W3092586919 cites W2031247021 @default.
- W3092586919 cites W2031928640 @default.
- W3092586919 cites W2042955915 @default.
- W3092586919 cites W2044227859 @default.
- W3092586919 cites W2046065891 @default.
- W3092586919 cites W2049978961 @default.
- W3092586919 cites W2050825125 @default.
- W3092586919 cites W205557920 @default.
- W3092586919 cites W2057974551 @default.
- W3092586919 cites W2058198327 @default.
- W3092586919 cites W2063987912 @default.
- W3092586919 cites W2067982977 @default.
- W3092586919 cites W2071561936 @default.
- W3092586919 cites W2074622157 @default.
- W3092586919 cites W2075493516 @default.
- W3092586919 cites W2079303863 @default.
- W3092586919 cites W2082271619 @default.
- W3092586919 cites W2082978512 @default.
- W3092586919 cites W2085672579 @default.
- W3092586919 cites W2092461401 @default.
- W3092586919 cites W2092677927 @default.
- W3092586919 cites W2092709528 @default.
- W3092586919 cites W2093344609 @default.
- W3092586919 cites W2093830806 @default.
- W3092586919 cites W2094119903 @default.
- W3092586919 cites W2096727849 @default.
- W3092586919 cites W2097762260 @default.
- W3092586919 cites W2107200594 @default.
- W3092586919 cites W2107927038 @default.
- W3092586919 cites W2108081147 @default.
- W3092586919 cites W2114415381 @default.
- W3092586919 cites W2120797621 @default.
- W3092586919 cites W2127931712 @default.
- W3092586919 cites W2128483600 @default.
- W3092586919 cites W2133338840 @default.
- W3092586919 cites W2135023776 @default.
- W3092586919 cites W2140807334 @default.
- W3092586919 cites W2142419812 @default.
- W3092586919 cites W2142991772 @default.
- W3092586919 cites W2143804637 @default.
- W3092586919 cites W2147677239 @default.
- W3092586919 cites W2149777825 @default.