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- W4386793986 abstract "The availability of both ancient and modern wood samples enables the Chinese fir (Cunninghamia lanceolata) in Central East China to become a potential tree species for dendroclimatic reconstruction over the Common Era. However, the potential of using tree-ring α-cellulose oxygen isotope ratios (δ18OTRC) in Chinese fir for the purposes of cross-dating and climatic reconstruction remains unexplored. Here we presented the three δ18OTRC chronologies (1954–2006 CE) for the whole-ring (δ18OWR), earlywood (δ18OEW), and latewood (δ18OLW) in Chinese fir. The results indicated that the δ18OWR had the highest correlation among individual trees. Using the δ18OWR instead of the conventionally employed TRW can facilitate the cross-dating procedure. The δ18OWR, δ18OEW, and δ18OLW exhibited the strongest relationships with the hydroclimate variables during the entire (June–September), early (June–July), and late (August–September) summer, respectively. The climate conditions preceding the growing season influenced δ18OEW more than δ18OLW. Using the δ18OWR and δ18OEW to reconstruct the hydroclimate variations may result in greater bias than the use of δ18OLW. Our study demonstrated that the δ18OTRC in Chinese fir from Central East China has the potential for cross-dating and summer hydroclimate reconstruction." @default.
- W4386793986 created "2023-09-16" @default.
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- W4386793986 date "2023-10-01" @default.
- W4386793986 modified "2023-10-16" @default.
- W4386793986 title "Inter-tree correlation and climatic response of tree-ring δ18O in Chinese fir: implications for cross-dating and climatic reconstruction in Central East China" @default.
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- W4386793986 doi "https://doi.org/10.1016/j.dendro.2023.126134" @default.
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