Literature DB >> 15578226

Forest soil respiration rate and delta13C is regulated by recent above ground weather conditions.

Alf Ekblad1, Björn Boström, Anders Holm, Daniel Comstedt.   

Abstract

Soil respiration, a key component of the global carbon cycle, is a major source of uncertainty when estimating terrestrial carbon budgets at ecosystem and higher levels. Rates of soil and root respiration are assumed to be dependent on soil temperature and soil moisture yet these factors often barely explain half the seasonal variation in soil respiration. We here found that soil moisture (range 16.5-27.6% of dry weight) and soil temperature (range 8-17.5 degrees C) together explained 55% of the variance (cross-validated explained variance; Q2) in soil respiration rate (range 1.0-3.4 micromol C m(-2) s(-1)) in a Norway spruce (Picea abies) forest. We hypothesised that this was due to that the two components of soil respiration, root respiration and decomposition, are governed by different factors. We therefore applied PLS (partial least squares regression) multivariate modelling in which we, together with below ground temperature and soil moisture, used the recent above ground air temperature and air humidity (vapour pressure deficit, VPD) conditions as x-variables. We found that air temperature and VPD data collected 1-4 days before respiration measurements explained 86% of the seasonal variation in the rate of soil respiration. The addition of soil moisture and soil temperature to the PLS-models increased the Q2 to 93%. delta13C analysis of soil respiration supported the hypotheses that there was a fast flux of photosynthates to root respiration and a dependence on recent above ground weather conditions. Taken together, our results suggest that shoot activities the preceding 1-6 days influence, to a large degree, the rate of root and soil respiration. We propose this above ground influence on soil respiration to be proportionally largest in the middle of the growing season and in situations when there is large day-to-day shifts in the above ground weather conditions. During such conditions soil temperature may not exert the major control on root respiration.

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Year:  2004        PMID: 15578226     DOI: 10.1007/s00442-004-1776-z

Source DB:  PubMed          Journal:  Oecologia        ISSN: 0029-8549            Impact factor:   3.225


  15 in total

1.  Evidence that decomposition rates of organic carbon in mineral soil do not vary with temperature.

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3.  Large-scale forest girdling shows that current photosynthesis drives soil respiration.

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Review 4.  Thermal acclimation and the dynamic response of plant respiration to temperature.

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Journal:  Planta       Date:  1990-07       Impact factor: 4.116

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7.  13C content of ecosystem respiration is linked to precipitation and vapor pressure deficit.

Authors:  David R Bowling; Nate G McDowell; Barbara J Bond; Beverly E Law; James R Ehleringer
Journal:  Oecologia       Date:  2002-03-01       Impact factor: 3.225

8.  Natural abundance of 13C in CO2 respired from forest soils reveals speed of link between tree photosynthesis and root respiration.

Authors:  A Ekblad; P Högberg
Journal:  Oecologia       Date:  2001-05-01       Impact factor: 3.225

9.  Root production, turnover and respiration under two grassland types along an altitudinal gradient: influence of temperature and solar radiation.

Authors:  A H Fitter; J D Graves; G K Self; T K Brown; D S Bogie; K Taylor
Journal:  Oecologia       Date:  1998-03       Impact factor: 3.225

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  10 in total

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2.  Phenophases alter the soil respiration-temperature relationship in an oak-dominated forest.

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3.  Disentangling drought-induced variation in ecosystem and soil respiration using stable carbon isotopes.

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4.  Soil Respiration in European Grasslands in Relation to Climate and Assimilate Supply.

Authors:  Michael Bahn; Mirco Rodeghiero; Margaret Anderson-Dunn; Sabina Dore; Cristina Gimeno; Matthias Drösler; Michael Williams; Christof Ammann; Frank Berninger; Chris Flechard; Stephanie Jones; Manuela Balzarolo; Suresh Kumar; Christian Newesely; Tibor Priwitzer; Antonio Raschi; Rolf Siegwolf; Sanna Susiluoto; John Tenhunen; Georg Wohlfahrt; Alexander Cernusca
Journal:  Ecosystems       Date:  2008-12       Impact factor: 4.217

5.  Toward using delta13C of ecosystem respiration to monitor canopy physiology in complex terrain.

Authors:  T G Pypker; M Hauck; E W Sulzman; M H Unsworth; A C Mix; Z Kayler; D Conklin; A M Kennedy; H R Barnard; C Phillips; B J Bond
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6.  Temporal dynamics of the carbon isotope composition in a Pinus sylvestris stand: from newly assimilated organic carbon to respired carbon dioxide.

Authors:  Naomi Kodama; Romain L Barnard; Yann Salmon; Christopher Weston; Juan Pedro Ferrio; Jutta Holst; Roland A Werner; Matthias Saurer; Heinz Rennenberg; Nina Buchmann; Arthur Gessler
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7.  Long-term ¹³C labeling provides evidence for temporal and spatial carbon allocation patterns in mature Picea abies.

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Journal:  Oecologia       Date:  2014-04-03       Impact factor: 3.225

8.  Isotope fractionation and 13C enrichment in soil profiles during the decomposition of soil organic matter.

Authors:  Björn Boström; Daniel Comstedt; Alf Ekblad
Journal:  Oecologia       Date:  2007-03-31       Impact factor: 3.298

9.  Vegetation types alter soil respiration and its temperature sensitivity at the field scale in an estuary wetland.

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Journal:  PLoS One       Date:  2014-03-07       Impact factor: 3.240

10.  Does the different photosynthetic pathway of plants affect soil respiration in a subtropical wetland?

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  10 in total

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