The terrestrial land surface has a crucial role in the global carbon cycle, providing feedbacks to changes in atmospheric levels of carbon dioxide and associated climate change1. Increases in atmospheric CO2 concentrations and in soil and air temperatures worldwide over the past several decades have been paralleled by an increase in the metabolism of organisms at the land surface — as demonstrated by enhanced rates of CO2 uptake, mainly by plants through photosynthesis, and of CO2 loss from plants and soil microorganisms, mostly owing to respiratory processes2–6. In a paper in Nature, Bond-Lamberty et al.7 report that the rate of increase of CO2 loss is outpacing that of CO2 uptake by plants. The authors attribute the imbalance in these rates of increase to enhanced activity of microbes that obtain nutrition by decomposing or mineralizing organic matter in soil. If the observed trend continues, then respiration by microbes could contribute substantially to global warming by releasing CO2 from organic matter that has previously been stored in soil for decades to millennia.
A variety of processes underlie the exchange of CO2 between the land surface and the atmosphere. Bond-Lamberty et al. focused on soil respiration, which is arguably one of the largest fluxes of CO2. The authors analysed previously published soil-respiration data8 from many sites around the world that covered a broad range of ecosystems, including cropland, temperate forest and desert. They used these data to estimate the annual rates of soil respiration at various sites and to evaluate trends between 1990 and 2014.
Bond-Lamberty and colleagues then compared trends in soil respiration (CO2 loss) with those of plant productivity (CO2 uptake) that were derived from different data sources, including satellites. They found that the ratio of the rate of soil respiration to that of plant productivity has, in general, increased over the period covered by their data set. The ratio rarely exceeded 1, except at certain sites in particular years, which indicates that specific situations can lead to more CO2 being lost from soil than is taken up by plants.
The findings beg the question of whether the average global ratio could become greater than 1 in the future, and, if so, when? Such an event would mark the tipping point at which the land surface stops operating mainly as a sink that helps to remove atmospheric CO2 that is derived from fossil-fuel emissions9,10, and starts acting as a source of CO2 — exacerbating rising CO2 levels and accelerating the pace of climate change11 (Fig. 1).
The authors next focused on studies in their data set that broke down total soil respiration into respiration dominated by decomposition by microbes and that associated with plant roots. Analysis of the microbial-dominated respiration rates led them to conclude that the disproportionately faster increase in the rate of total soil respiration is due to the enhanced activity of soil microbes. However, to understand whether accelerated rates of soil respiration will cause the land surface to become a source of CO2, the temporal trends in respiratory losses associated with aboveground plant biomass must also be considered — the total loss of biologically derived CO2 from the terrestrial biosphere is the sum of the soil and non-soil losses.
As Bond-Lamberty et al. acknowledge, previously published long-term data12,13 recorded by eddy-covariance towers, which continuously monitor CO2 concentrations and fluxes at specific sites across a range of ecosystems, suggest that the rate of increase of plant productivity has been faster than that of the total aboveground and belowground respiratory CO2 losses. Further data and analyses are required to explain why those findings apparently contradict the authors’ results.
If Bond-Lamberty and colleagues’ findings are correct, which mechanisms could explain the markedly enhanced stimulation of the activity of soil microbes relative to plant productivity and plant respiration? Studies in the past few years have shown that the ability of plants to downregulate respiration in response to long-term increases in temperature14 is much greater than that of short-lived soil microbes4,15–17. The authors suggest that the increased microbial activity observed in their study probably reflects the stimulatory effects of elevated temperatures associated with climate change.
There are, however, potential issues when drawing global inferences from the data analysed by Bond-Lamberty and co-workers. Most of the data came from spot measurements of soil-respiration rates that were obtained by many different researchers, who used a variety of methods to work out the contributions of soil microbes. This diversity of methods might have led those researchers to come to contrasting conclusions about the relative importance of soil microbes in their studies. Moreover, Bond-Lamberty et al. used simplifying assumptions to translate hourly or daily snapshots of respiration rates into annual fluxes of CO2, but did not take into account the uncertainty in these calculations. The soil-respiration data set is also limited in its temporal coverage of individual sites: repeated observations were available for only a handful of sites, yet recurrent observations are necessary to prevent temporal trends from being obscured by factors that vary between sites.
The authors acknowledge and account for some of these limitations in their statistical analyses, but clearly there is room for a more rigorous investigation. This would require researchers to gather continuous time series of soil respiration and its component fluxes, and demands the use of precise methods for quantifying uncertainty and for extrapolating local measurements to determine trends in larger regions. Despite the limitations, Bond-Lamberty and colleagues’ work is valuable because it aids our understanding of soil’s long-term potential for sequestering carbon — as well as how this sequestration might be threatened by accelerated rates of organic-matter decomposition by soil microbes. Their findings will be crucial for developing and testing models of the global carbon budget, of which soil carbon is a central component.
Fluxes of CO2 across whole ecosystems are often measured using eddy-covariance towers. By contrast, continuous measurements of soil respiration and decomposition by microbes are not broadly available for sites worldwide or do not cover multi-year periods. The establishment of long-term observational projects such as the US National Ecological Observatory Network (NEON), which monitors fluxes of soil CO2 among other ecological measures, will create opportunities for the systematic evaluation of temporal trends and the underlying causes of changes in the rates at which CO2 is lost from soil. Such data will be paramount for developing regional and global models of the carbon cycle, as well as for assessing climate change and the strategies by which it might be mitigated18.
Nature 560, 32-33 (2018)
Green, J. K. et al. Nature Geosci. 10, 410–414 (2017).
Lu, M. et al. Ecology 94, 726–738 (2013).
Piao, S. et al. Nature 451, 49–52 (2008).
Wang, X. et al. Glob. Change Biol. 20, 3229–3237 (2014).
Zhou, L. et al. Glob. Change Biol. 22, 3157–3169 (2016).
Zhu, Z. et al. Nature Clim. Change 6, 791–795 (2016).
Bond-Lamberty, B., Bailey, V. L., Chen, M., Gough, C. M. & Vargas, R. Nature 560, 80–83 (2018).
Bond-Lamberty, B. & Thomson, A. Nature 464, 579–582 (2010).
Le Quéré, C. et al. Nature Geosci. 2, 831–836 (2009).
Pan, Y. et al. Science 333, 988–993 (2011).
Wieder, W. R., Cleveland, C. C., Smith, W. K. & Todd-Brown, K. Nature Geosci. 8, 441–444 (2015).
Keenan, T. F. et al. Nature 499, 324–327 (2013).
Urbanski, S. et al. J. Geophys. Res-Biogeo. 112, G02020 (2007).
Reich, P. B. et al. Nature 531, 633–636 (2016).
Karhu, K. et al. Nature 513, 81–84 (2014).
Oliverio, A. M., Bradford, M. A. & Fierer, N. Glob. Change Biol. 23, 2117–2129 (2017).
Schindlbacher, A., Schnecker, J., Takriti, M., Borken, W. & Wanek, W. Glob. Change Biol. 21, 4265–4277 (2015).
Walsh, B. et al. Nature Commun. 8, 14856 (2017).