Interactions between physical and biotic factors influence CO2 flux in Antarctic dry valley soils

Rebecca Ball, Ross A. Virginia, J. E. Barrett, Andy N. Parsons, Diana H. Wall

Research output: Contribution to journalArticle

62 Citations (Scopus)

Abstract

Soil carbon dioxide (CO2) flux is an integrative measure of ecosystem functioning representing both biotic and physical controls over carbon (C) balance. In the McMurdo Dry Valleys of Antarctica, soil CO2 fluxes (approximately -0.1-0.15 μmol m-2 s-1) are generally low, and negative fluxes (uptake of CO2) are sometimes observed. A combination of biological respiration and physical mechanisms, driven by temperature and mediated by soil moisture and mineralogy, determine CO2 flux and, therefore, soil organic C balance. The physical factors important to CO2 flux are being altered with climate variability in many ecosystems including arid forms such as the Antarctic terrestrial ecosystems, making it critical to understand how climate factors interact with biotic drivers to control soil CO2 fluxes and C balances. We measured soil CO2 flux in experimental field manipulations, microcosm incubations and across natural environmental gradients of soil moisture to estimate biotic soil respiration and abiotic sources of CO2 flux in soils over a range of physical and biotic conditions. We determined that temperature fluctuations were the most important factor influencing diel variation in CO2 flux. Variation within these diel CO2 cycles was explained by differences in soil moisture. Increased temperature (as opposed to temperature fluctuations) had little or no effect on CO2 flux if moisture was not also increased. We conclude that CO2 flux in dry valley soils is driven primarily by physical factors such as soil temperature and moisture, indicating that future climate change may alter the dry valley soil C cycle. Negative CO2 fluxes in arid soils have recently been identified as potential net C sinks. We demonstrate the potential for arid polar soils to take up CO2, driven largely by abiotic factors associated with climate change. The low levels of CO2 absorption into soils we observed may not constitute a significant sink of atmospheric CO2, but will influence the interpretation of CO2 flux for the dry valley soil C cycle and possibly other arid environments where biotic controls over C cycling are secondary to physical drivers.

Original languageEnglish (US)
Pages (from-to)1510-1517
Number of pages8
JournalSoil Biology and Biochemistry
Volume41
Issue number7
DOIs
StatePublished - Jul 2009
Externally publishedYes

Fingerprint

biotic factor
Soil
valleys
carbon dioxide
valley
soil
soil moisture
soil water
Temperature
Ecosystem
temperature
biotic factors
Climate Change
diel variation
climate change
moisture flux
Climate
ecosystem
arid environment
climate

Keywords

  • Antarctic soils
  • Carbon cycling
  • Climate change
  • CO flux
  • McMurdo Dry Valleys
  • Nematodes
  • Soil biodiversity
  • Soil respiration

ASJC Scopus subject areas

  • Soil Science
  • Microbiology

Cite this

Interactions between physical and biotic factors influence CO2 flux in Antarctic dry valley soils. / Ball, Rebecca; Virginia, Ross A.; Barrett, J. E.; Parsons, Andy N.; Wall, Diana H.

In: Soil Biology and Biochemistry, Vol. 41, No. 7, 07.2009, p. 1510-1517.

Research output: Contribution to journalArticle

Ball, Rebecca ; Virginia, Ross A. ; Barrett, J. E. ; Parsons, Andy N. ; Wall, Diana H. / Interactions between physical and biotic factors influence CO2 flux in Antarctic dry valley soils. In: Soil Biology and Biochemistry. 2009 ; Vol. 41, No. 7. pp. 1510-1517.
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AB - Soil carbon dioxide (CO2) flux is an integrative measure of ecosystem functioning representing both biotic and physical controls over carbon (C) balance. In the McMurdo Dry Valleys of Antarctica, soil CO2 fluxes (approximately -0.1-0.15 μmol m-2 s-1) are generally low, and negative fluxes (uptake of CO2) are sometimes observed. A combination of biological respiration and physical mechanisms, driven by temperature and mediated by soil moisture and mineralogy, determine CO2 flux and, therefore, soil organic C balance. The physical factors important to CO2 flux are being altered with climate variability in many ecosystems including arid forms such as the Antarctic terrestrial ecosystems, making it critical to understand how climate factors interact with biotic drivers to control soil CO2 fluxes and C balances. We measured soil CO2 flux in experimental field manipulations, microcosm incubations and across natural environmental gradients of soil moisture to estimate biotic soil respiration and abiotic sources of CO2 flux in soils over a range of physical and biotic conditions. We determined that temperature fluctuations were the most important factor influencing diel variation in CO2 flux. Variation within these diel CO2 cycles was explained by differences in soil moisture. Increased temperature (as opposed to temperature fluctuations) had little or no effect on CO2 flux if moisture was not also increased. We conclude that CO2 flux in dry valley soils is driven primarily by physical factors such as soil temperature and moisture, indicating that future climate change may alter the dry valley soil C cycle. Negative CO2 fluxes in arid soils have recently been identified as potential net C sinks. We demonstrate the potential for arid polar soils to take up CO2, driven largely by abiotic factors associated with climate change. The low levels of CO2 absorption into soils we observed may not constitute a significant sink of atmospheric CO2, but will influence the interpretation of CO2 flux for the dry valley soil C cycle and possibly other arid environments where biotic controls over C cycling are secondary to physical drivers.

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KW - Climate change

KW - CO flux

KW - McMurdo Dry Valleys

KW - Nematodes

KW - Soil biodiversity

KW - Soil respiration

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