Global climate warming disproportionately affects high-latitude and mountainous terrestrial ecosystems. Warming is accompanied by permafrost thaw, shorter winters, earlier snowmelt, more intense soil freeze-thaw cycles, drier summers, and longer fire seasons. These environmental changes in turn impact surface water and groundwater flow regimes, water quality, greenhouse gas emissions, soil stability, vegetation cover, and soil (micro)biological communities. Warming also facilitates agricultural expansion, urban growth, and natural resource development, adding growing anthropogenic pressures to cold regions’ landscapes, soil health, and biodiversity. Further advances in the predictive understanding of how cold regions’ critical zone processes, functions, and ecosystem services will continue to respond to climate warming and land use changes require multiscale monitoring technologies coupled with integrated observational and modeling tools. We highlight some of the major challenges, knowledge gaps, and opportunities in cold region critical zone research, with an emphasis on subsurface processes and responses in both natural and agricultural ecosystems. Expected final online publication date for the Annual Review of Environment and Resources, Volume 46 is October 2021. Please see http://www.annualreviews.org/page/journal/pubdates for revised estimates.

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Bioenergy will be one of the most important renewable energy sources in the conversion from fossil fuels to bio-based products. Short rotation coppice Salix could be a key player in this conversion since Salix has rapid growth, positive energy balance, easy to manage cultivation system with vegetative propagation of plant material and multiple harvests from the same plantation. The aim of the present paper is to provide an overview of the main challenges and key issues in willow genetic improvement toward sustainable biofuel value chains. Primarily based on results from the research project "Optimized Utilization of Salix" (OPTUS), the influence of Salix wood quality on the potential for biofuel use is discussed, followed by issues related to the conversion of Salix biomass into liquid and gaseous transportation fuels. Thereafter, the studies address genotypic influence on soil carbon sequestration in Salix plantations, as well as on soil carbon dynamics and climate change impacts. Finally, the opportunities for plant breeding are discussed using willow as a resource for sustainable biofuel production. Substantial phenotypic and genotypic variation was reported for different wood quality traits important in biological (i.e., enzymatic and anaerobic) and thermochemical conversion processes, which is a prerequisite for plant breeding. Furthermore, different Salix genotypes can affect soil carbon sequestration variably, and life cycle assessment illustrates that these differences can result in different climate mitigation potential depending on genotype. Thus, the potential of Salix plantations for sustainable biomass production and its conversion into biofuels is shown. Large genetic variation in various wood and biomass traits, important for different conversion processes and carbon sequestration, provides opportunities to enhance the sustainability of the production system via plant breeding. This includes new breeding targets in addition to traditional targets for high yield to improve biomass quality and carbon sequestration potential.

<p>Microbial communities are a critical component of the soil carbon (C) cycle as they are responsible for the decomposition of both organic inputs from plants and of soil organic C. However, there is still no consensus about how to explicitly represent their role in terrestrial C cycling. The objective of the study was to determine how the properties of organic matter affect the metabolic response of the resident microbial communities in soils, using a bioenergetics approach. This was achieved by cross-amending six soils with excess water-soluble organic matter (WSOM) extracted from the same six soils and measuring heat dissipated due to the increase in microbial metabolic activity. The conditions of the experiment were chosen in order to replicate conditions in activity hotspots. The metabolic activity was then related to the potential return on investment (ROI) that the microbial communities could derive from the WSOM. The objective of the study was to determine how different energetic profiles in available organic avec the metabolic response of different microbial communities.</p><p>The ROI was calculated as the ratio between the total net energy available (ΔE) in the WSOM and the weighted average standard state Gibbs energies of oxidation half reactions of organic C (ΔG°Cox) of the molecules present in the WSOM. The ΔE was measured as the heat of combustion of the WSOM, which was measured using bomb calorimetry. ΔG°Cox was estimated from the average nominal oxidation state of C (NOSC), which itself was determined from the elemental composition of each molecular species in the organic matter amendments analyzed by Fourier transform ion cyclotron resonance mass spectrometry. The soil bacterial community structure was determined by 16S rRNA gene sequencing and using the weighted UniFrac distance of rarefied amplicon sequence variants data.</p><p>We found that the potential ROI that microbial communities could obtain from the consumption of the added organic matter was positively related to the overall metabolic response of microbial decomposers. However, the observed temporal differences in metabolism across soils indicate that bacterial communities do not exploit energetic return-on-investment in the same ways. Overall, our results suggest that microbial communities preferentially use organic matter with a high energetic return on investment.</p>

<p>It has recently been suggested that microbial-derived material is an important constituent of soil organic matter, and accumulation of organic matter in soil is related to microbial activity and the composition of the microbial communities present. However, microbial activity is generally intimately related to the properties of the carbon substrate (e.g. molecular diversity, energy content) available for decomposition. It is important, therefore, to understand in more detail what the drivers of microbial activity and their associated metabolic pathways are: the composition of the microbial communities or the properties of the available organic substrate.</p> <p>Water extractable organic matter from 6 different grassland and forest soils were added cross-wise to samples of each of the soils. The total heat dissipation was measured by isothermal calorimetry during a 23 h incubation period. Heat dissipation is a measure of total metabolic activity in the soil. The total CO<sub>2</sub> emission was also determined, by gas chromatography-mass spectrometry. The elemental composition of low molecular weight organic substances (LMWOS) was obtained by Fourier-Transform Ion Cyclotron Resonance Mass Spectrometry, which allowed us to calculate the Nominal Oxidation State of Carbon (NOSC) from each exact molecular mass detected. The NOSC is related to the energy content of the molecules. The microbial composition was determined by 16S rRNA gene sequencing. This experimental design allowed us to evaluate potential links between microbial community composition and their metabolic pathways when different LMWOS are undergoing decomposition.</p> <p>First, we found that the total heat dissipated and CO<sub>2</sub> emitted were associated with differences in the composition of LMWOS, independent of microbial community composition in the soil. We observed that the median of the total CO<sub>2</sub> emission was positively correlated with the weighted sum of the NOSC of each detected LMWOS. These results emphasise that a supply in available substrate with lower energy density (i.e. higher NOSC) may result in an increase in decarboxylation processes. Furthermore, total heat dissipated but not CO<sub>2</sub> was positively correlated to the molecular richness of LMWOS. This indicates that substrate with a higher molecular richness include also other metabolic pathways where CO<sub>2</sub> is not a decomposition end-product. Finally, we observed three different dynamics of heat dissipation during the 23 h incubation period. These dynamics were related to the microbial communities, but were independent of the LMWOS composition. The dynamic of heat dissipation were summarised by a Q<sub>t50</sub> index, i.e. the time required to release half of the heat dissipated in 23 h. The Q<sub>t50</sub> index was significantly correlated to the relative abundance of different bacterial taxa. In conclusion, whilst the short-term dynamics of substrate use appear to be associated with microbial community composition, the overall activity is more closely related to the composition of the available substrate.</p>