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Blue intensity from a tropical conifer’s annual rings for climate reconstruction: An ecophysiological perspective

Brendan M. Buckley; Kyle Hansen; Kevin L. Griffin; Stephanie Christine Schmiege; Rose C. Oelkers; Rosanne Dorothy D’Arrigo; Daniel K. Stahle; Nicole K. Davi; Tran Quoc Trung Nguyen; Canh Nam Le; Robert J. Wilson

Title:
Blue intensity from a tropical conifer’s annual rings for climate reconstruction: An ecophysiological perspective
Author(s):
Buckley, Brendan M.
Hansen, Kyle
Griffin, Kevin L.
Schmiege, Stephanie Christine
Oelkers, Rose C.
D’Arrigo, Rosanne Dorothy
Stahle, Daniel K.
Davi, Nicole K.
Nguyen, Tran Quoc Trung
Le, Canh Nam
Wilson, Robert J.
Date:
Type:
Articles
Department(s):
Lamont-Doherty Earth Observatory
Ecology, Evolution, and Environmental Biology
Volume:
50
Persistent URL:
Book/Journal Title:
Dendrochronologia
Geographic Area:
Vietnam
Abstract:
We developed Blue Intensity (BI) measurements from the crossdated ring sequences of Fokienia hodginsii (of the family Cupressaceae) from central Vietnam. BI has been utilized primarily as an indirect proxy measurement of latewood (LW) density of conifers (i.e., LWBI) from high latitude, temperature-limited boreal forests. As such, BI closely approximates maximum latewood density (MXD) measurements made from soft x-ray. The less commonly used earlywood (EW) BI (EWBI) represents the minimum density of EW and is influenced by the lighter pixels from the vacuoles or lumens of cells. The correlation of our BI measurements with climate, strongest for EWBI, rivals that for total ring width (RW), and we demonstrate that it can be successfully employed as an independent predictor for reconstruction models. EWBI exhibits robust spatial correlations with winter and spring land temperature, sea surface temperature (SST) over the regional domain of ENSO, and the Standardized Precipitation Evapotranspiration Index (SPEI) over Indochina. However, in order to mitigate the effects of color changes at the heartwood – sapwood boundary we calculated ΔBI (EWBI-LWBI), and it too exhibits a significant (p < 0.05), temporally stable response to prior autumn (Oct-Nov) rainfall and winter (December to April) dry season temperature. We interpret this response as reflecting a potential cavitation defense by reducing lumen diameter as a means to safeguard hydraulic conductivity in the stem, and to prevent the xylem from imploding due to negative pressure. This study has wide implications for the further use of BI from the global tropics, though it is unclear how many tropical tree species will be appropriate for use. It seems very likely that other wood anatomical measurements can be combined with BI and RW for climate reconstruction.
Subject(s):
Dendrochronology
Monsoons
Cupressaceae
Ecology
Environmental sciences
Publisher DOI:
https://doi.org/10.1016/j.dendro.2018.04.003
Item views
37
Metadata:
text | xml
Suggested Citation:
Brendan M. Buckley, Kyle Hansen, Kevin L. Griffin, Stephanie Christine Schmiege, Rose C. Oelkers, Rosanne Dorothy D’Arrigo, Daniel K. Stahle, Nicole K. Davi, Tran Quoc Trung Nguyen, Canh Nam Le, Robert J. Wilson, , Blue intensity from a tropical conifer’s annual rings for climate reconstruction: An ecophysiological perspective, Columbia University Academic Commons, .

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