Pete Smith’s research while affiliated with University of Aberdeen and other places

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Publications (673)


Conceptual framework of this study showing the relationship between plants and belowground soil organisms in response to GCFs across global forests, grasslands, and croplands
The diagram in the upper right corner shows the distribution of the study sites in the Whittaker biomes⁷⁸ mapped based on mean annual temperature and mean annual precipitation. The numbers in parentheses show sample sizes of plants and soil biota, respectively. Lines in different colors show the hypothetical relationships between the plant and soil-biota responses under GCFs; the dark blue line indicates a positive correlation between plant and soil-biota responses, the yellow line shows a negative correlation, and the gray line shows no significant relationship. CO2, elevated CO2; W, increased temperature; PRE-, precipitation reduction; PRE +, precipitation addition; N, nitrogen fertilization; P, phosphorus fertilization; N + P, nitrogen plus phosphorus fertilization. Symbols of global change factors, plants, soil microbes, and fauna were created by Qingshui Yu and Chenqi He.
Responses of attributes of plant and soil biota to GCFs among global forests, grasslands, and croplands
a Mean effect sizes of plant and soil biota attributes under GCFs across all (combined forests, grasslands, and croplands) ecosystems. Green shapes indicate plant attributes, and yellow are soil biota attributes. Circles, regular triangles, squares, and inverted triangles denote plant aboveground biomass or soil biota biomass, plant belowground biomass, diversity, and abundance, respectively. b–d Effect sizes on plant aboveground biomass, plant belowground biomass, and plant diversity under GCFs among global forests, grasslands, and croplands. Different colored circles indicate various biomes. e–g Effect sizes of biomass, diversity, and abundance of soil biota under GCFs among global forests, grasslands, and croplands. Closed shapes are statistically significant and open shapes are not significant. Weighted means and their 95% confidence intervals of effect sizes are given. Numbers are sample sizes for each global change factor.
Overall relationships between the responses of plant and belowground soil biota under GCFs
Overall relationships between the responses of plant and belowground soil biota for seven GCFs (a–g) at the left panel, and the effect of experimental treatments (duration and intensity) on the coupling coefficients of the relationships for each GCF at the right of the panel. The aboveground and belowground responses represent the relative changes of biomass, diversity, and abundance in plants and soil biota to different GCFs based on paired data. Relative changes were calculated as the logarithm of the ratio of the variable within each treatment plot divided by the same variable in the control plot. Point size indicates the weight of the sample size. P-values represent the statistical significance of coefficients by the two-sided z-test, and n represents study observations, respectively. Different lines indicate fitted relationships for each treatment based on the “REML” method in mixed-effects meta-regression. The solid lines indicate a significant difference (P < 0.05) from zero for the coupling coefficient, and the dashed lines indicate non-significance.
Significant linkages between the responses of plant and belowground soil biota under specific GCFs and relationship types
a Positive relationships between the responses of the plants and soil biota under CO2 in forests and (b) under PRE+ in grasslands. Point size indicates the weight of the sample size. P values represent the statistical significance of coefficients by the two-sided z-test, and n represents study observations, respectively. The solid lines indicate a significant difference (P < 0.05) from zero for the coupling coefficient, and the dashed lines indicate non-significance. Black lines show overall relationships between the responses of the aboveground and belowground compartments, the shades represent 95% confidence intervals. Other colored lines show different relationship types between corresponding variables of plants and soil biota. The posterior distribution of the coefficient is based on the Bayesian hierarchical meta-regression. The gray distribution indicates the posterior coefficient distribution of the overall relationship. c Different colored posterior distributions represent corresponding relationship types between plant aboveground biomass (AGB), plant belowground biomass (BGB), plant diversity (AGD) and soil biota diversity (SBD), soil biota abundance (SBA), soil biota biomass (SBB). Points indicate the mean of coefficients, and thick and thin bars represent 95% and 90% confidence intervals, respectively.
Decoupled responses of plants and soil biota to global change across the world’s land ecosystems
  • Article
  • Full-text available

November 2024

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487 Reads

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Mark A. Anthony

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Jingyun Fang

Understanding the concurrent responses of aboveground and belowground biota compartments to global changes is crucial for the maintenance of ecosystem functions and biodiversity conservation. We conduct a comprehensive analysis synthesizing data from 13,209 single observations and 3223 pairwise observations from 1166 publications across the world terrestrial ecosystems to examine the responses of plants and soil organisms and their synchronization. We find that global change factors (GCFs) generally promote plant biomass but decreased plant species diversity. In comparison, the responses of belowground soil biota to GCFs are more variable and harder to predict. The analysis of the paired aboveground and belowground observations demonstrate that responses of plants and soil organisms to GCFs are decoupled among diverse groups of soil organisms for different biomes. Our study highlights the importance of integrative research on the aboveground-belowground system for improving predictions regarding the consequences of global environmental change.

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Assessing the Sustainability of Miscanthus and Willow as Global Bioenergy Crops Under Current and Future Climate Conditions- 1

November 2024

Miscanthus (Miscanthus × giganteus) and Willow (Salix spp.) are promising bioenergy crops due to their high biomass yields and adaptability to diverse climatic conditions. This study applies the MiscanFor/ SalixFor models to assess the sustainability of these crops under current and future climate scenarios, focusing on biomass productivity, carbon intensity (CI), and energy use efficiency (EUE). Under present conditions, both crops show high productivity in tropical and subtropical regions, with Miscanthus generally outperforming Willow. Productivity declines in less favourable climates, emphasizing the crops' sensitivity to environmental factors at the regional scale. The average productivity for Miscanthus and Willow was 19.9 t/ha and 10.4 t/ha, respectively. Future climate scenarios (A1F1 and B1) project significant shifts, with northern and central regions becoming more viable for cultivation due to warmer temperatures and extended growing seasons. However, southern and arid regions may experience reduced productivity, reflecting the uneven impacts of climate change. Miscanthus and Willow are predicted to show productivity declines of 15% and 8%, and 12% and 7% under A1F1 and B1, respectively. CI analysis reveals substantial spatial variability, with higher values in industrialized and temperate regions due to intensive agricultural practices. Future scenarios indicate increased CI in northern latitudes due to intensified land use, while certain Southern Hemisphere regions may stabilize or reduce CI through mitigation strategies. Under climate change, CI for Miscanthus is projected to increase by over 100%, while Willow shows increase of 64% and 57% for A1F1and B1, respectively. EUE patterns suggest that both crops perform optimally in tropical and subtropical climates. Miscanthus shows a slight advantage in EUE, though Willow demonstrates greater adaptability in temperate regions. Climate change is expected to reduce EUE for Miscanthus by 10% and 7%, and for Willow by 9% and 6%. This study underscores the need for region-specific strategies to optimize the sustainability of bioenergy crops under changing climate conditions.


How to make land use policy decisions: Integrating science and economics to deliver connected climate, biodiversity, and food objectives

November 2024

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168 Reads

Proceedings of the National Academy of Sciences

Land use change is crucial to addressing the existential threats of climate change and biodiversity loss while enhancing food security [M. Zurek et al. , Science 376 , 1416–1421 (2022)]. The interconnected and spatially varying nature of the impacts of land use change means that these challenges must be addressed simultaneously [H.-O. Pörtner et al. , Science 380 , eabl4881 (2023)]. However, governments commonly focus on single issues, incentivizing land use change via “Flat-Rate” subsidies offering constant per hectare payments, uptake of which is determined by the economic circumstances of landowners rather than the integrated environmental outcomes that will be delivered [G. Q. Bull et al. , Forest Policy Econ. 9 , 13–31 (2006)]. Here, we compare Flat-Rate subsidies to two alternatives: “Land Use Scenario” allocation of subsidies through consultation across stakeholders and interested parties; and a “Natural Capital” approach which targets subsidies according to expected ecosystem service response. This comparison is achieved by developing a comprehensive decision support system, integrating new and existing natural, physical, and economic science models to quantify environmental, agricultural, and economic outcomes. Applying this system to the United Kingdom’s net zero commitment to increase carbon storage via afforestation, we show that the three approaches result in significantly different outcomes in terms of where planting occurs, their environmental consequences, and economic costs and benefits. The Flat-Rate approach actually increases net carbon emissions while Land Use Scenario allocation yields poor economic outcomes. The Natural Capital targeted approach outperforms both alternatives, providing the highest possible social values while satisfying net zero commitments.


Figure 4 Schematic of a theoretical NbS project, showing the target habitats overlaid onto the existing field boundaries.
Scoring criteria for biodiversity and soil health metrics.
An integrated approach to above- and below-ground ecological monitoring for nature-based solutions

November 2024

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34 Reads

1. As the development of nature-based solutions (NbS) increases globally, it is important to ensure that projects meet the objective of benefiting biodiversity, alongside tackling societal challenges. However, most NbS projects do not directly monitor ecological outcomes, and those that do often focus on a limited set of metrics. It is therefore challenging to assess whether projects fulfil the aim of benefiting biodiversity. 2. We aimed to identify the most informative and feasible ecological metrics, both above- and below-ground, for monitoring ecological outcomes of NbS. We conducted a structured non-systematic literature review to identify possible biodiversity and soil health metrics, then developed a scoring system to rank these based on their informativeness and feasibility for monitoring. 3. Metrics were categorised into compositional, structural, and functional aspects of biodiversity, and biological, physical, and chemical aspects of soil health. We grouped biodiversity and soil health metrics into Tier 1 (the most informative and feasible metrics), Tier 2 (informative metrics with some limitations in scope or feasibility), and Future metrics (highly informative metrics which are currently less feasible to monitor). Tier 1 metrics collectively address multiple aspects of biodiversity and soil health and are currently the highest priority for NbS projects to assess. For biodiversity nine Tier 1, six Tier 2, and 15 Future metrics were identified, and for soil health 11 Tier 1, six Tier 2, and five Future metrics. 4. We identified existing standardised methodologies for monitoring the proposed metrics, noting that for many metrics standardised methodologies are not available and threshold or reference values for each metric are missing. 5. Solution: Our study provides practitioners with a framework for selecting optimum metrics for assessing above- and below-ground ecological outcomes of NbS relevant to the place in which they are being implemented. A definition of each metric and standardised methodologies for collecting data are summarised, providing information to develop an ecological monitoring protocol for an NbS project. The information on each metric has been made freely available as a searchable database in an interactive online interface geared towards UK practitioners, but with wider applicability.





Carbon sequestration potential of tree planting in China

September 2024

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258 Reads

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2 Citations

China’s large-scale tree planting programs are critical for achieving its carbon neutrality by 2060, but determining where and how to plant trees for maximum carbon sequestration has not been rigorously assessed. Here, we developed a comprehensive machine learning framework that integrates diverse environmental variables to quantify tree growth suitability and its relationship with tree numbers. Then, their correlations with biomass carbon stocks were robustly established. Carbon sink potentials were mapped in distinct tree-planting scenarios. Under one of them aligned with China’s ecosystem management policy, 44.7 billion trees could be planted, increasing forest stock by 9.6 ± 0.8 billion m³ and sequestering 5.9 ± 0.5 PgC equivalent to double China’s 2020 industrial CO2 emissions. We found that tree densification within existing forests is an economically viable and effective strategy and so it should be a priority in future large-scale planting programs.


Mean nitrous oxide (N2O) emissions as affected by elevated carbon dioxide (eCO2) and crop straw amendment. a Y1, the field experiment in 2020–2021; b Y2, the field experiment in 2021–2022; c N0, the pot experiment #1 under 0 kg N ha⁻¹; d N1, the pot experiment #1 under 150 kg N ha⁻¹; e N2, the pot experiment #1 under 250 kg N ha⁻¹; f C1, the pot experiment #2 under yangmai 13; g C2, the pot experiment #2 under yangmai 25. aCO2, ambient CO2; eCO2, elevated CO2. Bars represent means ± standard errors
The (nirK + nirS)/nosZ affected by elevated carbon dioxide (eCO2) under crop straw management. a Y1, the field experiment in 2020–2021; b Y2, the field experiment in 2021–2022; c N0, the pot experiment #1 under 0 kg N ha⁻¹; d N1, the pot experiment #1 under 150 kg N ha⁻¹; e N2, the pot experiment #1 under 250 kg N ha⁻¹; f C1, the pot experiment #2 under yangmai 13; g C2, the pot experiment #2 under yangmai 25. aCO2, ambient CO2; eCO2, elevated CO2. Bars represent means ± standard errors
Soil dissolved organic C to total dissolved N (DOC/TDN) affected by elevated carbon dioxide (eCO2) and crop straw amendment. a Y1, the field experiment in 2020–2021; b Y2, the field experiment in 2021–2022; c N0, the pot experiment #1 under 0 kg N ha⁻¹; d N1, the pot experiment #1 under 150 kg N ha⁻¹; e N2, the pot experiment #1 under 250 kg N ha⁻¹; f C1, the pot experiment #2 under yangmai 13; g C2, the pot experiment #2 under yangmai 25. aCO2, ambient CO2; eCO2, elevated CO2. Bars represent means ± standard errors
The relationship between soil dissolved organic C to total dissolved N (DOC/TDN) and soil water content (SWC) affected crop straw amendment at elevated and ambient carbon dioxide (aCO2 and eCO2). The grey areas indicate the 95% confidence intervals of the regression line
Synergistic effect of elevated CO2 and straw amendment on N2O emissions from a rice–wheat cropping system

September 2024

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85 Reads

Biology and Fertility of Soils

Nitrous oxide (N2O) is one of the most important climate-forcing gases, and a large portion of global anthropogenic N2O emissions come from agricultural soils. Yet, how contrasting global change factors and agricultural management can interact to drive N2O emissions remains poorly understood. Here, conducted within a rice–wheat cropping system, we combined a two-year field experiment with two pot experiments to investigate the influences of elevated atmospheric carbon dioxide (eCO2) and crop straw addition to soil in altering N2O emissions under wheat cropping. Our analyses identified consistent and significant interactions between eCO2 and straw addition, whereby eCO2 increased N2O emissions (+ 19.9%) only when straw was added, and independent of different N fertilizer gradients and wheat varieties. Compared with the control (i.e., ambient CO2 without straw addition), eCO2 + straw addition increased N2O emission by 44.7% and dissolved organic carbon to total dissolved nitrogen (DOC/TDN) ratio by 115.3%. Similarly, eCO2 and straw addition significantly impacted soil N2O-related microbial activity. For instance, the ratio of the abundance of N2O production genes (i.e., nirK and nirS) to the abundance of the N2O reduction gene (i.e., nosZ) with straw addition was 26.0% higher than that without straw under eCO2. This indicates an increased denitrification potential and suggests a change in the stoichiometry of denitrification products, affecting the balance between N2O production and reduction, leading to an increase in N2O emissions. Taken together, our results emphasize the critical role of the interaction between the specific agronomic practice of straw addition and eCO2 in shaping greenhouse gas emissions in the wheat production system studied, and underline the need to test the efficacy of greenhouse gas mitigation measures under various management practices and global change scenarios. Graphical abstract


Fig. 1. Areas expected to be affected by green water scarcity in a 3°C global climate warming scenario. Affected areas are shown in ivory yellow [data from (29)], and current rates of groundwater depletion are in blue to green yellow (152).
Fig. 2. Global regions likely to experience increases in nitrogen pollution of ground and surface waters due to projected precipitation increases. Regions with excessive N fertilizer application (red to yellow colors) [data from (153)] and increased precipitation (dots) will likely observe greater N losses to the environment. Dots indicate regions where precipitation is projected to increase, according to most (≥80%) global climate models of the Coupled Model Intercomparison Project (CMIP6) [data from (154)].
Fig. 3. Impacts of climate change on pest pressure, pesticide use, and pesticide fate and toxicity. How the various aspects of pest pressure and pesticides are affected by climate change is described in the boxes. Up arrows indicate that climate change generally has positive effects and down arrows, negative effects.
Fig. 4. The major environmental impacts of agricultural systems and potentially exacerbating
effects of climate change. The dark red circle in the center represents climate change. The yellow donut represents agricultural systems, and the small circles inside indicate the processes through which it affects the environment (black arrows). Dark red arrows indicate impacts of climate change on agriculture, and plus signs indicate its reinforcing effects on agriculture’s environmental problems, including direct feedback to climate change (e.g., intensified CH4 and N2O emissions). Dashed arrows indicate indirect climate-change
feedback from the different environmental impacts of agriculture (e.g., stimulated CH4 emissions in lakes from nutrient runoff).
Climate change exacerbates the environmental impacts of agriculture

September 2024

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1,283 Reads

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10 Citations

Science

Agriculture’s global environmental impacts are widely expected to continue expanding, driven by population and economic growth and dietary changes. This Review highlights climate change as an additional amplifier of agriculture’s environmental impacts, by reducing agricultural productivity, reducing the efficacy of agrochemicals, increasing soil erosion, accelerating the growth and expanding the range of crop diseases and pests, and increasing land clearing. We identify multiple pathways through which climate change intensifies agricultural greenhouse gas emissions, creating a potentially powerful climate change–reinforcing feedback loop. The challenges raised by climate change underscore the urgent need to transition to sustainable, climate-resilient agricultural systems. This requires investments that both accelerate adoption of proven solutions that provide multiple benefits, and that discover and scale new beneficial processes and food products.


Citations (66)


... However, due to its unconstructively divisive nature, misleading aspects, epistemically questionable foundations, and nebulous statements, there appears little reason to consider the DD suitable for advancing the debate, much less for advancing it in an effective manner. Rather than providing a foundation to build on, the DD causes epistemic damage, setting back progress on the topic and necessitating efforts to repair the harm (for two such efforts, see the Nature Food pieces by Herzon et al., 2023 andBryant et al., 2024). We find no significant epistemic benefit to the DD except that it serves as an entry point to examine the influence of the meat industry on science, policy, and public discourse, a benefit which presumably was not intended by its authors. ...

Reference:

The Dublin Declaration: Gain for the Meat Industry, Loss for Science
The Dublin Declaration fails to recognize the need to reduce industrial animal agriculture

Nature Food

... The study predicts a larger potential forestation area in China's drywet transition areas compared to other forecasts. For instance, one study using a machine learning framework estimated the future forestation potential in China to be between 58 and 70 Mha [55], while another study suggested that 8.1 % of China's land area, equivalent to about 78 Mha, could be forested in the future, with approximately half of it in the dry-wet transition areas [25]. while another study suggested that 8.1 % of China's land area, equivalent to about 78 million hectares, could be forested in the future, with approximately half of it in the drywet transition areas. ...

Carbon sequestration potential of tree planting in China

... Evidence from extensive long-term field experiments reveals that the productivity and environmental impact of cropping systems vary with different agricultural management practices [2][3][4]. In the current context of frequent extreme weather events, certain conventional agricultural practices, such as intensive tillage and monocropping, may exacerbate the environmental impacts of agricultural systems, thereby hindering the development of sustainable agriculture [1,5]. ...

Climate change exacerbates the environmental impacts of agriculture
  • Citing Article
  • September 2024

Science

... We find that while the prototype scheme agrees with key features of the best-fit deposition scheme, the prototype deposition scheme would better reproduce observations with a lag of +3 months in its seasonality in the tropics. Other sources of hysteresis on the 325 seasonality may be explained by dependence on: irreversible degeneration of free enzymes in soils where seasonal temperatures fluctuate above 30 • C (Chowdhury and Conrad, 2010); variations in the soil organic carbon content (King et al., 2008;Karbin et al., 2024); or even the life-cycle of soil microbes (Meredith et al., 2014). Our results indicate that deeper investigations into the H 2 flux in tropical soils are needed to build our understanding of the links between these soil microbial processes and the planetary scale H 2 signal. ...

Modelling Hydrogen Uptake in Soil: Exploring the Role of Microbial Activity
  • Citing Preprint
  • August 2024

... Here, we aimed to reveal the general pattern of the effects and mechanisms of nutrient (N and P) addition on the temperature sensitivity of SOC decomposition. We hypothesized that (1) nutrient addition would increase Q 10 , as nutrient addition usually increases substrate availability (Widdig et al. 2020), which usually has a positive effect on Q 10 (Gershenson, Bader, and Cheng 2009); (2) nutrient-induced changes in Q 10 would vary across different climatic regions, with potentially greater impacts in warmer climates than in colder climates because soil microbial nutrient limitation is usually greater in warm areas (Cui et al. 2024;Jing et al. 2020); and (3) nutrient-induced changes in substrate availability would mainly mediate the effects of nutrient addition on Q 10 , given its pivotal role in regulating soil microbial activity and the carbon turnover rate (Domeignoz-Horta et al. 2023;Eberwein et al. 2015). To test these hypotheses, soil samples collected from 36 sites across six distinct forest ecosystems in China ( Figure 1) were supplemented with nutrients (i.e., N addition, P addition, and N + P addition), after which the Q 10 was determined. ...

Limiting Resources Define the Global Pattern of Soil Microbial Carbon Use Efficiency

... Xu et al. found that long-term nitrogen addition increased SOC content increased due to enhanced plant carbon inputs and reduced soil microbial biomass and respiration, which decreased carbon losses from decomposition [57]. In addition, nitrogen input affects soil organic matter decomposition, likely due to changes in enzyme activities due to shifts in microbial community [58]. Nitrogen addition promotes the growth of copiotrophic bacteria, which can effectively degrade labile substances by producing hydrolytic and oxidative enzymes, thereby influencing the decomposition of soil organic matter [59,60]. ...

Not all soil carbon is created equal: Labile and stable pools under nitrogen input

Global Change Biology

... Biomass waste has become a new raw material for renewable energy production, and generating bioenergy from waste is environmentally friendly [4][5][6]. The development of bioenergy plays a significant role in achieving carbon neutrality [7]. The demand for biomass as an energy source is expected to increase in the future, which may lead to a supply shortage relative to biomass consumption as early moisture, active calcium content, etc.). ...

Sustainable bioenergy contributes to cost-effective climate change mitigation in China

iScience

... During the 154-day incubation, the trends in soil CO 2 , CH 4 (Tables S1-S4). The cumulative emissions of CO2, CH4, and N2O under the control treatment were 4400.77 ...

Enhanced response of soil respiration to experimental warming upon thermokarst formation

... The developed search queries were partly informed by the queries used in the review and map by ref. 17, and ref. 48. The CDR queries were combined with additional subqueries to restrict the selection to articles explicitly discussing positive or negative side effects of CDR, as well as potential threats to CDR deployment. ...

Scientific literature on carbon dioxide removal much larger than previously suggested: insights from an AI-enhanced systematic map

... Improving N use efficiency (NUE) of crop farms through better management of N fertilizer application would provide sustained levels of crop production despite lower N inputs 42 . Many technologies and management practices, including enhanced efficiency fertilizers, cover copping and no-till farming, improve NUE at the plot scale [56][57][58][59][60] . However, there is a limit to how much inputs can be reduced, as N is needed in crop production systems to boost yield and avoid soil N depletion. ...

The global potential for mitigating nitrous oxide emissions from croplands
  • Citing Article
  • March 2024

One Earth