Details
| Original language | English |
|---|---|
| Pages (from-to) | 280-296 |
| Number of pages | 17 |
| Journal | ECOSYSTEMS |
| Volume | 21 |
| Issue number | 2 |
| Early online date | 8 May 2017 |
| Publication status | Published - Mar 2018 |
Abstract
When applied to climate change-related precipitation decline, the optimal partitioning theory (OPT) predicts that plants will allocate a larger portion of carbon to root growth to enhance the capacity to access and acquire water. However, tests of OPT applied to the root system of mature trees or stands exposed to long-term drying show mixed, partly contradicting, results, indicating an overly simplistic understanding of how moisture affects plant-internal carbon allocation. We investigated the response of the root system (0–240 cm depth) of European beech to long-term decrease in water supply in six mature forests located across a precipitation gradient (855–576 mm mean annual precipitation, MAP). With reference to OPT, we hypothesized that declining precipitation across this gradient would: (H1) cause the profile total of fine root biomass (FRB; roots OpenSPiltSPi2 mm) to increase relative to total leaf mass; (H2) trigger a shift to a shallower root system; and (H3) induce different responses in the depth distributions of different root diameter classes. In contradiction to H1, neither total FRB (0–240 cm) nor the FRB:leaf mass ratio changed significantly with the MAP decrease. The support for H2 was only weak: the 95% rooting depth of fine roots decreased with decreasing MAP, whereas the maximum extension of small coarse roots (2–5 mm) increased, indicating contrasting responses of different root diameter classes. We conclude that long-term decline in water supply leads to only minor adaptive modification with respect to the size and structure of the beech root system, with notable change in the depth extension of some root diameter classes but limited capacity to alter the fine root:leaf mass ratio. It appears that OPT cannot adequately predict C allocation shifts in mature trees when exposed to long-term drying. Graphical Abstract: [Figure not available: see fulltext.].
Keywords
- coarse roots, European beech, fine roots, mature trees, optimal partitioning theory, precipitation gradient, root morphology, root-to-shoot ratio, rooting depth
ASJC Scopus subject areas
- Agricultural and Biological Sciences(all)
- Ecology, Evolution, Behavior and Systematics
- Environmental Science(all)
- Environmental Chemistry
- Environmental Science(all)
- Ecology
Sustainable Development Goals
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In: ECOSYSTEMS, Vol. 21, No. 2, 03.2018, p. 280-296.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - The Deep Root System of Fagus sylvatica on Sandy Soil
T2 - Structure and Variation Across a Precipitation Gradient
AU - Meier, Ina Christin
AU - Knutzen, Florian
AU - Eder, Lucia Muriel
AU - Müller-Haubold, Hilmar
AU - Goebel, Marc Oliver
AU - Bachmann, Jörg
AU - Hertel, Dietrich
AU - Leuschner, Christoph
N1 - © 2017, Springer Science Business Media New York
PY - 2018/3
Y1 - 2018/3
N2 - When applied to climate change-related precipitation decline, the optimal partitioning theory (OPT) predicts that plants will allocate a larger portion of carbon to root growth to enhance the capacity to access and acquire water. However, tests of OPT applied to the root system of mature trees or stands exposed to long-term drying show mixed, partly contradicting, results, indicating an overly simplistic understanding of how moisture affects plant-internal carbon allocation. We investigated the response of the root system (0–240 cm depth) of European beech to long-term decrease in water supply in six mature forests located across a precipitation gradient (855–576 mm mean annual precipitation, MAP). With reference to OPT, we hypothesized that declining precipitation across this gradient would: (H1) cause the profile total of fine root biomass (FRB; roots OpenSPiltSPi2 mm) to increase relative to total leaf mass; (H2) trigger a shift to a shallower root system; and (H3) induce different responses in the depth distributions of different root diameter classes. In contradiction to H1, neither total FRB (0–240 cm) nor the FRB:leaf mass ratio changed significantly with the MAP decrease. The support for H2 was only weak: the 95% rooting depth of fine roots decreased with decreasing MAP, whereas the maximum extension of small coarse roots (2–5 mm) increased, indicating contrasting responses of different root diameter classes. We conclude that long-term decline in water supply leads to only minor adaptive modification with respect to the size and structure of the beech root system, with notable change in the depth extension of some root diameter classes but limited capacity to alter the fine root:leaf mass ratio. It appears that OPT cannot adequately predict C allocation shifts in mature trees when exposed to long-term drying. Graphical Abstract: [Figure not available: see fulltext.].
AB - When applied to climate change-related precipitation decline, the optimal partitioning theory (OPT) predicts that plants will allocate a larger portion of carbon to root growth to enhance the capacity to access and acquire water. However, tests of OPT applied to the root system of mature trees or stands exposed to long-term drying show mixed, partly contradicting, results, indicating an overly simplistic understanding of how moisture affects plant-internal carbon allocation. We investigated the response of the root system (0–240 cm depth) of European beech to long-term decrease in water supply in six mature forests located across a precipitation gradient (855–576 mm mean annual precipitation, MAP). With reference to OPT, we hypothesized that declining precipitation across this gradient would: (H1) cause the profile total of fine root biomass (FRB; roots OpenSPiltSPi2 mm) to increase relative to total leaf mass; (H2) trigger a shift to a shallower root system; and (H3) induce different responses in the depth distributions of different root diameter classes. In contradiction to H1, neither total FRB (0–240 cm) nor the FRB:leaf mass ratio changed significantly with the MAP decrease. The support for H2 was only weak: the 95% rooting depth of fine roots decreased with decreasing MAP, whereas the maximum extension of small coarse roots (2–5 mm) increased, indicating contrasting responses of different root diameter classes. We conclude that long-term decline in water supply leads to only minor adaptive modification with respect to the size and structure of the beech root system, with notable change in the depth extension of some root diameter classes but limited capacity to alter the fine root:leaf mass ratio. It appears that OPT cannot adequately predict C allocation shifts in mature trees when exposed to long-term drying. Graphical Abstract: [Figure not available: see fulltext.].
KW - coarse roots
KW - European beech
KW - fine roots
KW - mature trees
KW - optimal partitioning theory
KW - precipitation gradient
KW - root morphology
KW - root-to-shoot ratio
KW - rooting depth
UR - http://www.scopus.com/inward/record.url?scp=85019040294&partnerID=8YFLogxK
U2 - 10.1007/s10021-017-0148-6
DO - 10.1007/s10021-017-0148-6
M3 - Article
AN - SCOPUS:85019040294
VL - 21
SP - 280
EP - 296
JO - ECOSYSTEMS
JF - ECOSYSTEMS
SN - 1432-9840
IS - 2
ER -