Hydraulic failure and tree dieback are associated with high wood density in a temperate forest under extreme drought

2011 ◽  
Vol 17 (8) ◽  
pp. 2731-2742 ◽  
Author(s):  
WILLIAM A. HOFFMANN ◽  
RENÉE M. MARCHIN ◽  
PAMELA ABIT ◽  
ON LEE LAU
2021 ◽  
Vol 502 ◽  
pp. 119723
Author(s):  
Adrián Jauregui ◽  
Sabrina Andrea Rodríguez ◽  
Lucas Nahuel González García ◽  
Exequiel Gonzalez ◽  
Luciano Noel Segura

2011 ◽  
Vol 31 (2) ◽  
pp. 117-130 ◽  
Author(s):  
J. M. Warren ◽  
R. J. Norby ◽  
S. D. Wullschleger

2021 ◽  
Author(s):  
Rachael H. Nolan ◽  
Alice Gauthey ◽  
Adriano Losso ◽  
Belinda E. Medlyn ◽  
Rhiannon Smith ◽  
...  

2018 ◽  
Vol 373 (1760) ◽  
pp. 20170308 ◽  
Author(s):  
Erika Berenguer ◽  
Yadvinder Malhi ◽  
Paulo Brando ◽  
Amanda Cardoso Nunes Cordeiro ◽  
Joice Ferreira ◽  
...  

Human-modified forests are an ever-increasing feature across the Amazon Basin, but little is known about how stem growth is influenced by extreme climatic events and the resulting wildfires. Here we assess for the first time the impacts of human-driven disturbance in combination with El Niño–mediated droughts and fires on tree growth and carbon accumulation. We found that after 2.5 years of continuous measurements, there was no difference in stem carbon accumulation between undisturbed and human-modified forests. Furthermore, the extreme drought caused by the El Niño did not affect carbon accumulation rates in surviving trees. In recently burned forests, trees grew significantly more than in unburned ones, regardless of their history of previous human disturbance. Wood density was the only significant factor that helped explain the difference in growth between trees in burned and unburned forests, with low wood–density trees growing significantly more in burned sites. Our results suggest stem carbon accumulation is resistant to human disturbance and one-off extreme drought events, and it is stimulated immediately after wildfires. However, these results should be seen with caution—without accounting for carbon losses, recruitment and longer-term changes in species composition, we cannot fully understand the impacts of drought and fire in the carbon balance of human-modified forests. This article is part of a discussion meeting issue ‘The impact of the 2015/2016 El Nino on the terrestrial tropical carbon cycle: patterns, mechanisms and implications’.


2015 ◽  
Vol 21 (10) ◽  
pp. 3657-3674 ◽  
Author(s):  
Roger Seco ◽  
Thomas Karl ◽  
Alex Guenther ◽  
Kevin P. Hosman ◽  
Stephen G. Pallardy ◽  
...  

Author(s):  
Hervé Cochard ◽  
François Pimont ◽  
Julien Ruffault ◽  
Nicolas Martin-StPaul

SummaryWe describe the operating principle of the detailed version of the soil-plant-atmosphere model SurEau that allows, among other things, to predict the risk of hydraulic failure under extreme drought. It is based on the formalization of key physiological processes of plant response to water stress. The hydraulic functioning of the plant is at the core of this model, which focuses on both water flows and water pools using variable hydraulic conductances. The model considers the elementary flow of water from the soil to the atmosphere through different plant organs (roots, trunk branches, leaves and buds) that are described by their symplasm and their apoplasm compartments. Within each organ the flow of water between the apoplasm and the symplasm is also represented; as well as the flow outside the system, from the symplasm of each organ to the atmosphere, through the cuticular conductance. For each organ, the symplasm is described by a pressure volume curves and the apoplasm by the vulnerability curve to cavitation of the xylem. The model can thus compute the loss of conductance caused by cavitation, a leading mechanisms of plant desiccation and drought-induced mortality. Some example simulations are shown to illustrate how the model works.


2019 ◽  
Author(s):  
Lia Lamacque ◽  
Guillaume Charrier ◽  
Fernanda dos Santos Farnese ◽  
Benjamin Lemaire ◽  
Thierry Améglio ◽  
...  

AbstractIn the context of climate changes, water availability is expected to severely decline. Consequently, there is a need to predict mortality of woody species, especially to find a physiological threshold to drought-induced mortality. Lavender species (Lavandula angustifolia and Lavandula x intermedia) which are important crops of the Mediterranean region are affected by a decline, notably caused by successive intense drought events. Lavender response to extreme drought events was monitored using continuous stem diameter measurements. Water potential, stomatal conductance, loss of xylem hydraulic conductivity and electrolyte leakage were also measured during desiccation, and recovery was evaluated after rewatering. Two parameters computed from stem diameter variations were related to stress intensity and resilience to stress: PLD (Percentage Loss of Diameter) and stem PLRC (Percentage Loss of Rehydration Capacity of the stem), respectively. We showed that plants did not recover when the PLD reached its maximal value (PLDmax) which was 21.27 ± 0.57% in both lavender species and whatever the growing conditions. This point of no return was associated with a high level of cell lysis evaluated by electrolyte leakage, and occurred far after the xylem hydraulic failure. We discussed the relevance of PLDmax as a threshold for drought-induced mortality and its physiological significance, in relation to the mortality mechanisms.One-sentence summaryUnder extreme drought, lavender death occurs when the water storage of the elastic compartment of the stem is exhausted.


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