Assessing earlywood-latewood proportion influence on tree-ring stable isotopes
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F23%3A00580084" target="_blank" >RIV/86652079:_____/23:00580084 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216224:14310/23:00133106 RIV/62156489:43210/23:43924176 RIV/62156489:43410/23:43924176
Výsledek na webu
<a href="https://www.sciencedirect.com/science/article/pii/S1125786523000978?ref=pdf_download&fr=RR-2&rr=842b95ba0a7c6e98" target="_blank" >https://www.sciencedirect.com/science/article/pii/S1125786523000978?ref=pdf_download&fr=RR-2&rr=842b95ba0a7c6e98</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.dendro.2023.126147" target="_blank" >10.1016/j.dendro.2023.126147</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Assessing earlywood-latewood proportion influence on tree-ring stable isotopes
Popis výsledku v původním jazyce
Tree-ring stable isotopes are typically measured in latewood cellulose to mitigate potential carry-over effects from previous year storage pools. The isotopic composition of individual tree-ring segments is thought to include considerable intra-annual variability. This sampling strategy may be complicated by steep intra-annual isotope gradients that can rival the inter-annual variability, however. Consistent sampling of latewood material may not always be possible due to low sample availability or high prevalence of narrow rings or low amounts of latewood because of species-specific changes in ring width. Therefore, years that contain samples with higher portions of non-latewood (earlywood) material may influence the final chronology of isotopic variability. Here, we analyze the potential influence that changing earlywood and latewood components of individual tree rings can have on stable carbon and oxygen records from Quercus spp. and Pinus heldreichii chronologies. Analysis of stable isotopes in oak tree rings with varying amounts of latewood show no statistically significant differences in the range of isotopic composition, nor any major differences when considering the same calendric year. Similar results were found for the pine data, when comparing stable isotope measurements with earlywood-to-latewood ratio and maximum density. We argue that this simple approach should be applied to any long-term tree-ring stable isotope record in order to provide a better understanding of the potential biases that could arise from previously recorded intra-annual variability in the wood.
Název v anglickém jazyce
Assessing earlywood-latewood proportion influence on tree-ring stable isotopes
Popis výsledku anglicky
Tree-ring stable isotopes are typically measured in latewood cellulose to mitigate potential carry-over effects from previous year storage pools. The isotopic composition of individual tree-ring segments is thought to include considerable intra-annual variability. This sampling strategy may be complicated by steep intra-annual isotope gradients that can rival the inter-annual variability, however. Consistent sampling of latewood material may not always be possible due to low sample availability or high prevalence of narrow rings or low amounts of latewood because of species-specific changes in ring width. Therefore, years that contain samples with higher portions of non-latewood (earlywood) material may influence the final chronology of isotopic variability. Here, we analyze the potential influence that changing earlywood and latewood components of individual tree rings can have on stable carbon and oxygen records from Quercus spp. and Pinus heldreichii chronologies. Analysis of stable isotopes in oak tree rings with varying amounts of latewood show no statistically significant differences in the range of isotopic composition, nor any major differences when considering the same calendric year. Similar results were found for the pine data, when comparing stable isotope measurements with earlywood-to-latewood ratio and maximum density. We argue that this simple approach should be applied to any long-term tree-ring stable isotope record in order to provide a better understanding of the potential biases that could arise from previously recorded intra-annual variability in the wood.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
40102 - Forestry
Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2023
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Dendrochronologia
ISSN
1125-7865
e-ISSN
1612-0051
Svazek periodika
82
Číslo periodika v rámci svazku
DEC
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
6
Strana od-do
126147
Kód UT WoS článku
001111344700001
EID výsledku v databázi Scopus
2-s2.0-85175526259