Climate signals in stable carbon and hydrogen isotopes of lignin methoxy groups from southern German beech trees
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F22%3A00560346" target="_blank" >RIV/86652079:_____/22:00560346 - isvavai.cz</a>
Result on the web
<a href="https://cp.copernicus.org/articles/18/1849/2022/" target="_blank" >https://cp.copernicus.org/articles/18/1849/2022/</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5194/cp-18-1849-2022" target="_blank" >10.5194/cp-18-1849-2022</a>
Alternative languages
Result language
angličtina
Original language name
Climate signals in stable carbon and hydrogen isotopes of lignin methoxy groups from southern German beech trees
Original language description
Stable hydrogen and carbon isotope ratios of wood lignin methoxy groups (delta C-13(LM) and delta H-2(LM) values) have been shown to be reliable proxies of past temperature variations. Previous studies showed that delta H-2(LM) values even work in temperate environments where classical tree-ring width and maximum latewood density measurements are less successful for climate reconstructions. Here, we analyse the annually resolved delta C-13(LM) values from 1916-2015 of four beech trees (Fagus sylvatica) from a temperate site near HohenpeiBenberg in southern Germany and compare these data with regional-to continental-scale climate observations. Initial delta(13)C(LM )values were corrected for the Suess effect (a decrease of delta C-13 in atmospheric CO2) and physiological tree responses to increasing atmospheric CO2 concentrations considering a range of published discrimination factors. The calibration of delta C-13(LM) chronologies against instrumental data reveals the highest correlations with regional summer (r = 0.68) and mean annual temperatures (r = 0.66), as well as previous-year September to current-year August temperatures (r = 0.61), all calculated from 1916-2015 and reaching p < 0.001. Additional calibration trials using detrended delta C-13(LM) values and climate data (to constrain effects of autocorrelation on significance levels) returned r(summer) = 0.46 (p < 0.001), r(annual) = 0.25 (p < 0.05) and r(prev.September-August) = 0.18 (p > 0.05). The new delta C-13(LM) chronologies were finally compared with the previously produced delta H-2(LM) values of the same trees in order to evaluate the additional gain of assessing past climate variability using a dual-isotope approach. Compared to delta C-13(LM), delta H-2(LM) values correlate substantially more strongly with large-scale temperatures averaged over western Europe (r(prev.September-August) = 0.69), whereas only weak and mainly insignificant correlations are obtained between precipitation and both isotope chronologies (delta C-13(LM) and delta H-2(LM) values). Our results indicate the great potential of using delta C-13(LM) values from temperate environments as a proxy for local temperatures and, in combination with delta H-2(LM) values, to assess regional- to sub-continental scale temperature patterns.
Czech name
—
Czech description
—
Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10509 - Meteorology and atmospheric sciences
Result continuities
Project
<a href="/en/project/EF16_019%2F0000797" target="_blank" >EF16_019/0000797: SustES - Adaptation strategies for sustainable ecosystem services and food security under adverse environmental conditions</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2022
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Climate of the Past
ISSN
1814-9324
e-ISSN
1814-9332
Volume of the periodical
18
Issue of the periodical within the volume
8
Country of publishing house
DE - GERMANY
Number of pages
17
Pages from-to
1849-1866
UT code for WoS article
000840411200001
EID of the result in the Scopus database
2-s2.0-85136804412