The Deep Root System of Fagus sylvatica on Sandy Soil: Structure and Variation Across a Precipitation Gradient

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Ina Christin Meier
  • Florian Knutzen
  • Lucia Muriel Eder
  • Hilmar Müller-Haubold
  • Marc Oliver Goebel
  • Jörg Bachmann
  • Dietrich Hertel
  • Christoph Leuschner

Externe Organisationen

  • Georg-August-Universität Göttingen
  • Philipps-Universität Marburg
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Details

OriginalspracheEnglisch
Seiten (von - bis)280-296
Seitenumfang17
FachzeitschriftECOSYSTEMS
Jahrgang21
Ausgabenummer2
Frühes Online-Datum8 Mai 2017
PublikationsstatusVeröffentlicht - März 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.].

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The Deep Root System of Fagus sylvatica on Sandy Soil: Structure and Variation Across a Precipitation Gradient. / Meier, Ina Christin; Knutzen, Florian; Eder, Lucia Muriel et al.
in: ECOSYSTEMS, Jahrgang 21, Nr. 2, 03.2018, S. 280-296.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Meier, IC, Knutzen, F, Eder, LM, Müller-Haubold, H, Goebel, MO, Bachmann, J, Hertel, D & Leuschner, C 2018, 'The Deep Root System of Fagus sylvatica on Sandy Soil: Structure and Variation Across a Precipitation Gradient', ECOSYSTEMS, Jg. 21, Nr. 2, S. 280-296. https://doi.org/10.1007/s10021-017-0148-6
Meier, I. C., Knutzen, F., Eder, L. M., Müller-Haubold, H., Goebel, M. O., Bachmann, J., Hertel, D., & Leuschner, C. (2018). The Deep Root System of Fagus sylvatica on Sandy Soil: Structure and Variation Across a Precipitation Gradient. ECOSYSTEMS, 21(2), 280-296. https://doi.org/10.1007/s10021-017-0148-6
Meier IC, Knutzen F, Eder LM, Müller-Haubold H, Goebel MO, Bachmann J et al. The Deep Root System of Fagus sylvatica on Sandy Soil: Structure and Variation Across a Precipitation Gradient. ECOSYSTEMS. 2018 Mär;21(2):280-296. Epub 2017 Mai 8. doi: 10.1007/s10021-017-0148-6
Meier, Ina Christin ; Knutzen, Florian ; Eder, Lucia Muriel et al. / The Deep Root System of Fagus sylvatica on Sandy Soil : Structure and Variation Across a Precipitation Gradient. in: ECOSYSTEMS. 2018 ; Jahrgang 21, Nr. 2. S. 280-296.
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title = "The Deep Root System of Fagus sylvatica on Sandy Soil: Structure and Variation Across a Precipitation Gradient",
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.].",
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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

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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.].

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