Abstract

Background

Understanding how trees respond to drought is critical to forecasting both short and long-term impacts of climate change on forests. The isotopic ratio of 13C to 12C stored in wood – referred to as δ13C – is widely used as an indicator of plant water status. Yet whether changes in δ13C linked to drought are also associated with declines in annual carbon assimilation and allocation to stem growth remains unclear.

Methods

Here we used tree ring data from over 3000 trees – representing 26 populations of 16 common European tree species sampled at six locations that span more than 20° in latitude – to test whether drought induces coordinated changes in carbon isotope ratios and stem basal area increments (BAI).

Results

We found that δ13C is a reliable indicator of drought across a wide range of species and environmental conditions. All but one of the populations sampled in this study showed a statistically significant increase in δ13C under drought conditions. However, when considering the effects of these same drought events on BAI, we found no evidence to suggest that increases in δ13C were coupled with significant declines in stem growth. While BAI was 11.9% lower on average in drought years, this decline in BAI was not significant when analysed across species. In fact, only seven of the 26 populations we sampled exhibited significant declines in BAI under drought conditions – four of these from a single study site in the Carpathian Mountains of Romania.

Conclusions

While δ13C responded strongly and consistently to drought across a diverse group of tree species and environmental conditions, we found that most tree species were able to sustain growth even under conditions of low soil water availability. Consequently, while δ13C provides a powerful indicator of past drought occurrence, by themselves carbon isotope ratios tell us little about how carbon sequestration and allocation to wood are affected by conditions of low water availability across Europe’s forests.

Details

Title
Detecting the fingerprint of drought across Europe’s forests: do carbon isotope ratios and stem growth rates tell similar stories?
Author
Jucker, Tommaso 1   VIAFID ORCID Logo  ; Grossiord, Charlotte 2 ; Bonal, Damien 3 ; Bouriaud, Olivier 4 ; Gessler, Arthur 5 ; Coomes, David A 6 

 Ecosystem Change Ecology team, CSIRO Land and Water, Floreat, WA, Australia; Forest Ecology and Conservation group, Department of Plant Sciences, University of Cambridge, Cambridge, UK 
 Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM, USA 
 INRA, Université de Lorraine, UMR EEF, Champenoux, France 
 Ștefan cel Mare University, Suceava, Romania 
 Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Forest Dynamics, Birmensdorf, Switzerland 
 Forest Ecology and Conservation group, Department of Plant Sciences, University of Cambridge, Cambridge, UK 
Pages
1-11
Publication year
2017
Publication date
Dec 2017
Publisher
Elsevier Limited
ISSN
20956355
e-ISSN
21975620
Source type
Scholarly Journal
Language of publication
English
ProQuest document ID
1652948113
Copyright
Forest Ecosystems is a copyright of Springer, (2017). All Rights Reserved., © 2017. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.