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van Breugel M, Bongers F, Norden N, Meave JA, Amissah L, Chanthorn W, Chazdon R, Craven D, Farrior C, Hall JS, Hérault B, Jakovac C, Lebrija-Trejos E, Martínez-Ramos M, Muñoz R, Poorter L, Rüger N, van der Sande M, Dent DH. Feedback loops drive ecological succession: towards a unified conceptual framework. Biol Rev Camb Philos Soc 2024; 99:928-949. [PMID: 38226776 DOI: 10.1111/brv.13051] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/28/2023] [Revised: 12/29/2023] [Accepted: 12/29/2023] [Indexed: 01/17/2024]
Abstract
The core principle shared by most theories and models of succession is that, following a major disturbance, plant-environment feedback dynamics drive a directional change in the plant community. The most commonly studied feedback loops are those in which the regrowth of the plant community causes changes to the abiotic (e.g. soil nutrients) or biotic (e.g. dispersers) environment, which differentially affect species availability or performance. This, in turn, leads to shifts in the species composition of the plant community. However, there are many other PE feedback loops that potentially drive succession, each of which can be considered a model of succession. While plant-environment feedback loops in principle generate predictable successional trajectories, succession is generally observed to be highly variable. Factors contributing to this variability are the stochastic processes involved in feedback dynamics, such as individual mortality and seed dispersal, and extrinsic causes of succession, which are not affected by changes in the plant community but do affect species performance or availability. Both can lead to variation in the identity of dominant species within communities. This, in turn, leads to further contingencies if these species differ in their effect on their environment (priority effects). Predictability and variability are thus intrinsically linked features of ecological succession. We present a new conceptual framework of ecological succession that integrates the propositions discussed above. This framework defines seven general causes: landscape context, disturbance and land-use, biotic factors, abiotic factors, species availability, species performance, and the plant community. When involved in a feedback loop, these general causes drive succession and when not, they are extrinsic causes that create variability in successional trajectories and dynamics. The proposed framework provides a guide for linking these general causes into causal pathways that represent specific models of succession. Our framework represents a systematic approach to identifying the main feedback processes and causes of variation at different successional stages. It can be used for systematic comparisons among study sites and along environmental gradients, to conceptualise studies, and to guide the formulation of research questions and design of field studies. Mapping an extensive field study onto our conceptual framework revealed that the pathways representing the study's empirical outcomes and conceptual model had important differences, underlining the need to move beyond the conceptual models that currently dominate in specific fields and to find ways to examine the importance of and interactions among alternative causal pathways of succession. To further this aim, we argue for integrating long-term studies across environmental and anthropogenic gradients, combined with controlled experiments and dynamic modelling.
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Affiliation(s)
- Michiel van Breugel
- Department of Geography, National University of Singapore, Arts Link, #03-01 Block AS2, 117570, Singapore
- Yale-NUS College, 16 College Avenue West, Singapore, 138527, Singapore
- Smithsonian Tropical Research Institute, Roosevelt Ave. Tupper Building - 401, Panama City, 0843-03092, Panama
| | - Frans Bongers
- Forest Ecology and Forest Management Group, Wageningen University & Research, PO Box 47, 6700 AA, Wageningen, The Netherlands
| | - Natalia Norden
- Centro de Estudios Socioecológicos y Cambio Global, Instituto de Investigación de Recursos Biológicos Alexander von Humboldt, Avenida Circunvalar #16-20, Bogotá, Colombia
| | - Jorge A Meave
- Departamento de Ecología y Recursos Naturales, Facultad de Ciencias, Universidad Nacional Autónoma de México. Circuito Exterior s/n, Ciudad Universitaria, Coyoacán, Ciudad de México, C.P. 04510, Mexico
| | - Lucy Amissah
- CSIR-Forestry Research Institute of Ghana, UPO Box 63, Kumasi, Ghana
| | - Wirong Chanthorn
- Department of Environmental Technology and Management, Faculty of Environment, Kasetsart University, 50 Ngamwongwan Road, Jatujak District, 10900, Thailand
| | - Robin Chazdon
- Forest Research Institute, University of the Sunshine Coast, 90 Sippy Downs Dr, Sippy Downs, Queensland, 4556, Australia
| | - Dylan Craven
- Center for Genomics, Ecology & Environment, Universidad Mayor, Camino La Piramide 5750, Huechuraba, Santiago, 8580745, Chile
| | - Caroline Farrior
- Department of Integrative Biology, University of Texas at Austin, 2415 Speedway, Stop C0930, Austin, Texas, 78705, USA
| | - Jefferson S Hall
- Smithsonian Tropical Research Institute, Roosevelt Ave. Tupper Building - 401, Panama City, 0843-03092, Panama
| | - Bruno Hérault
- CIRAD, UPR Forêts et Sociétés, F-34398 Montpellier, France & Forêts et Sociétés, Univ Montpellier, CIRAD, Montpellier, France
| | - Catarina Jakovac
- Departamento de Fitotecnia, Centro de Ciências Agrárias, Universidade Federal de Santa Catarina, Rod. Admar Gonzaga, 1346, 88034-000, Florianópolis, Brazil
| | - Edwin Lebrija-Trejos
- Department of Biology and Environment, University of Haifa-Oranim, Tivon, 36006, Israel
| | - Miguel Martínez-Ramos
- Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autónoma de México, Campus Morelia, Antigua Carretera a Pátzcuaro # 8701, Col. Ex-Hacienda de San José de la Huerta, CP 58190, Morelia, Michoacán, Mexico
| | - Rodrigo Muñoz
- Forest Ecology and Forest Management Group, Wageningen University & Research, PO Box 47, 6700 AA, Wageningen, The Netherlands
| | - Lourens Poorter
- Forest Ecology and Forest Management Group, Wageningen University & Research, PO Box 47, 6700 AA, Wageningen, The Netherlands
| | - Nadja Rüger
- Smithsonian Tropical Research Institute, Roosevelt Ave. Tupper Building - 401, Panama City, 0843-03092, Panama
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Puschstr. 4, 04103, Leipzig, Germany
- Department of Economics, Institute of Empirical Economic Research, University of Leipzig, Grimmaische Str. 12, 04109, Leipzig, Germany
| | - Masha van der Sande
- Forest Ecology and Forest Management Group, Wageningen University & Research, PO Box 47, 6700 AA, Wageningen, The Netherlands
| | - Daisy H Dent
- Smithsonian Tropical Research Institute, Roosevelt Ave. Tupper Building - 401, Panama City, 0843-03092, Panama
- ETH Zürich, Department of Environmental Systems Science, Institute for Integrative Biology, Universitätstrasse 16, 8092, Zürich, Switzerland
- Max Planck Institute for Animal Behavior, Am Obstberg 1, 78315 Radolfzell, Germany
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Qiu T, Peñuelas J, Chen Y, Sardans J, Yu J, Xu Z, Cui Q, Liu J, Cui Y, Zhao S, Chen J, Wang Y, Fang L. Arbuscular mycorrhizal fungal interactions bridge the support of root-associated microbiota for slope multifunctionality in an erosion-prone ecosystem. IMETA 2024; 3:e187. [PMID: 38898982 PMCID: PMC11183171 DOI: 10.1002/imt2.187] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 02/16/2024] [Revised: 03/05/2024] [Accepted: 03/06/2024] [Indexed: 06/21/2024]
Abstract
The role of diverse soil microbiota in restoring erosion-induced degraded lands is well recognized. Yet, the facilitative interactions among symbiotic arbuscular mycorrhizal (AM) fungi, rhizobia, and heterotrophic bacteria, which underpin multiple functions in eroded ecosystems, remain unclear. Here, we utilized quantitative microbiota profiling and ecological network analyses to explore the interplay between the diversity and biotic associations of root-associated microbiota and multifunctionality across an eroded slope of a Robinia pseudoacacia plantation on the Loess Plateau. We found explicit variations in slope multifunctionality across different slope positions, associated with shifts in limiting resources, including soil phosphorus (P) and moisture. To cope with P limitation, AM fungi were recruited by R. pseudoacacia, assuming pivotal roles as keystones and connectors within cross-kingdom networks. Furthermore, AM fungi facilitated the assembly and composition of bacterial and rhizobial communities, collectively driving slope multifunctionality. The symbiotic association among R. pseudoacacia, AM fungi, and rhizobia promoted slope multifunctionality through enhanced decomposition of recalcitrant compounds, improved P mineralization potential, and optimized microbial metabolism. Overall, our findings highlight the crucial role of AM fungal-centered microbiota associated with R. pseudoacacia in functional delivery within eroded landscapes, providing valuable insights for the sustainable restoration of degraded ecosystems in erosion-prone regions.
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Affiliation(s)
- Tianyi Qiu
- State Key Laboratory of Soil Erosion and Dryland Farming on the Loess PlateauNorthwest A&F UniversityYanglingChina
- College of Natural Resources and EnvironmentNorthwest A&F UniversityYanglingChina
- Key Laboratory of Green Utilization of Critical Non‐metallic Mineral Resources, Ministry of EducationWuhan University of TechnologyWuhanChina
| | - Josep Peñuelas
- Consejo Superior de Investigaciones CientíficasGlobal Ecology Unit Centre de Recerca Ecològica i Aplicacions Forestals‐Consejo Superior de Investigaciones Científicas‐Universitat Autònoma de BarcelonaBellaterraSpain
- Centre de Recerca Ecològica i Aplicacions ForestalsCerdanyola del VallèsCataloniaSpain
| | - Yinglong Chen
- State Key Laboratory of Soil Erosion and Dryland Farming on the Loess PlateauNorthwest A&F UniversityYanglingChina
- College of Natural Resources and EnvironmentNorthwest A&F UniversityYanglingChina
- School of Agriculture and Environment, Institute of AgricultureThe University of Western AustraliaPerthWestern AustraliaAustralia
| | - Jordi Sardans
- Consejo Superior de Investigaciones CientíficasGlobal Ecology Unit Centre de Recerca Ecològica i Aplicacions Forestals‐Consejo Superior de Investigaciones Científicas‐Universitat Autònoma de BarcelonaBellaterraSpain
- Centre de Recerca Ecològica i Aplicacions ForestalsCerdanyola del VallèsCataloniaSpain
| | - Jialuo Yu
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources ResearchChinese Academy of SciencesBeijingChina
| | - Zhiyuan Xu
- State Key Laboratory of Soil Erosion and Dryland Farming on the Loess PlateauNorthwest A&F UniversityYanglingChina
- College of Natural Resources and EnvironmentNorthwest A&F UniversityYanglingChina
| | - Qingliang Cui
- Institute of Soil and Water ConservationChinese Academy of Sciences and Ministry of Water ResourcesYanglingChina
| | - Ji Liu
- Hubei Province Key Laboratory for Geographical Process Analysis and SimulationCentral China Normal UniversityWuhanChina
| | - Yongxing Cui
- Institute of BiologyFreie Universität BerlinBerlinGermany
| | - Shuling Zhao
- Institute of Soil and Water ConservationChinese Academy of Sciences and Ministry of Water ResourcesYanglingChina
| | - Jing Chen
- Department of CardiologyRenmin Hospital of Wuhan UniversityWuhanChina
| | - Yunqiang Wang
- Chinese Academy of Sciences Center for Excellence in Quaternary Science and Global ChangeChinese Academy of SciencesXi'anChina
| | - Linchuan Fang
- State Key Laboratory of Soil Erosion and Dryland Farming on the Loess PlateauNorthwest A&F UniversityYanglingChina
- Key Laboratory of Green Utilization of Critical Non‐metallic Mineral Resources, Ministry of EducationWuhan University of TechnologyWuhanChina
- Institute of Soil and Water ConservationChinese Academy of Sciences and Ministry of Water ResourcesYanglingChina
- Chinese Academy of Sciences Center for Excellence in Quaternary Science and Global ChangeChinese Academy of SciencesXi'anChina
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3
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Beerling DJ, Epihov DZ, Kantola IB, Masters MD, Reershemius T, Planavsky NJ, Reinhard CT, Jordan JS, Thorne SJ, Weber J, Val Martin M, Freckleton RP, Hartley SE, James RH, Pearce CR, DeLucia EH, Banwart SA. Enhanced weathering in the US Corn Belt delivers carbon removal with agronomic benefits. Proc Natl Acad Sci U S A 2024; 121:e2319436121. [PMID: 38386712 PMCID: PMC10907306 DOI: 10.1073/pnas.2319436121] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/14/2023] [Accepted: 12/30/2023] [Indexed: 02/24/2024] Open
Abstract
Terrestrial enhanced weathering (EW) of silicate rocks, such as crushed basalt, on farmlands is a promising scalable atmospheric carbon dioxide removal (CDR) strategy that urgently requires performance assessment with commercial farming practices. We report findings from a large-scale replicated EW field trial across a typical maize-soybean rotation on an experimental farm in the heart of the United Sates Corn Belt over 4 y (2016 to 2020). We show an average combined loss of major cations (Ca2+ and Mg2+) from crushed basalt applied each fall over 4 y (50 t ha-1 y-1) gave a conservative time-integrated cumulative CDR potential of 10.5 ± 3.8 t CO2 ha-1. Maize and soybean yields increased significantly (P < 0.05) by 12 to 16% with EW following improved soil fertility, decreased soil acidification, and upregulation of root nutrient transport genes. Yield enhancements with EW were achieved with significantly (P < 0.05) increased key micro- and macronutrient concentrations (including potassium, magnesium, manganese, phosphorus, and zinc), thus improving or maintaining crop nutritional status. We observed no significant increase in the content of trace metals in grains of maize or soybean or soil exchangeable pools relative to controls. Our findings suggest that widespread adoption of EW across farming sectors has the potential to contribute significantly to net-zero greenhouse gas emissions goals while simultaneously improving food and soil security.
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Affiliation(s)
- David J. Beerling
- Leverhulme Centre for Climate Change Mitigation, School of Biosciences, University of Sheffield, SheffieldS10 2TN, United Kingdom
| | - Dimitar Z. Epihov
- Leverhulme Centre for Climate Change Mitigation, School of Biosciences, University of Sheffield, SheffieldS10 2TN, United Kingdom
| | - Ilsa B. Kantola
- Institute for Sustainability, Energy, and Environment, University of Illinois at Urbana-Champaign, Urbana, IL 61801
| | - Michael D. Masters
- Institute for Sustainability, Energy, and Environment, University of Illinois at Urbana-Champaign, Urbana, IL 61801
| | - Tom Reershemius
- Yale Center for Natural Carbon Capture, Department of Earth & Planetary Sciences, Yale University, New Haven, CT 06511
| | - Noah J. Planavsky
- Yale Center for Natural Carbon Capture, Department of Earth & Planetary Sciences, Yale University, New Haven, CT 06511
| | - Christopher T. Reinhard
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332
| | | | - Sarah J. Thorne
- Leverhulme Centre for Climate Change Mitigation, School of Biosciences, University of Sheffield, SheffieldS10 2TN, United Kingdom
| | - James Weber
- Leverhulme Centre for Climate Change Mitigation, School of Biosciences, University of Sheffield, SheffieldS10 2TN, United Kingdom
| | - Maria Val Martin
- Leverhulme Centre for Climate Change Mitigation, School of Biosciences, University of Sheffield, SheffieldS10 2TN, United Kingdom
| | - Robert P. Freckleton
- Leverhulme Centre for Climate Change Mitigation, School of Biosciences, University of Sheffield, SheffieldS10 2TN, United Kingdom
| | - Sue E. Hartley
- Leverhulme Centre for Climate Change Mitigation, School of Biosciences, University of Sheffield, SheffieldS10 2TN, United Kingdom
| | - Rachael H. James
- School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, SouthamptonSO14 3ZH, United Kingdom
| | | | - Evan H. DeLucia
- Institute for Sustainability, Energy, and Environment, University of Illinois at Urbana-Champaign, Urbana, IL 61801
| | - Steven A. Banwart
- Global Food and Environment Institute, University of Leeds, LeedsLS2 9JT, United Kingdom
- School of Earth and Environment, University of Leeds, Leeds LS2 9JT, United Kingdom
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4
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Vermeij GJ. The illusion of balance in the history of the biosphere. GEOBIOLOGY 2024; 22:e12584. [PMID: 38385604 DOI: 10.1111/gbi.12584] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/12/2023] [Revised: 12/15/2023] [Accepted: 01/03/2024] [Indexed: 02/23/2024]
Abstract
Earth's surface has been irreversibly altered by the activity of organisms, a process that has accelerated as the power of the biosphere (the rate at which life extracts and deploys energy) has increased over time. This trend is incompatible with the expectation that the inputs to Earth's surface of life's materials from the crust and mantle be matched by export from Earth's surface to long-term reservoirs. Here, I suggest that the collective activity of organisms has always violated this balance. The biosphere's ability to extract, retain, recycle, and accumulate materials has allowed living biomass to increase and for exports to decrease over very long timescales. This collective metabolism implies a net transfer of materials from the planet's interior to its surface. The combination of metabolic innovations, competition, adaptive evolution, and the establishment of collaborative economic feedback in ecosystems created dynamic ecological stability despite great spatial and temporal heterogeneity in physical and biological inputs and export of nutrients into and out of the biosphere. Models of geochemical cycling must take the fundamental role of living organisms and the evolutionary changes in these roles into account to explain past and future conditions.
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5
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Kantola IB, Blanc-Betes E, Masters MD, Chang E, Marklein A, Moore CE, von Haden A, Bernacchi CJ, Wolf A, Epihov DZ, Beerling DJ, DeLucia EH. Improved net carbon budgets in the US Midwest through direct measured impacts of enhanced weathering. GLOBAL CHANGE BIOLOGY 2023; 29:7012-7028. [PMID: 37589204 DOI: 10.1111/gcb.16903] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/09/2023] [Accepted: 06/23/2023] [Indexed: 08/18/2023]
Abstract
Terrestrial enhanced weathering (EW) through the application of Mg- or Ca-rich rock dust to soil is a negative emission technology with the potential to address impacts of climate change. The effectiveness of EW was tested over 4 years by spreading ground basalt (50 t ha-1 year-1 ) on maize/soybean and miscanthus cropping systems in the Midwest US. The major elements of the carbon budget were quantified through measurements of eddy covariance, soil carbon flux, and biomass. The movement of Mg and Ca to deep soil, released by weathering, balanced by a corresponding alkalinity flux, was used to measure the drawdown of CO2 , where the release of cations from basalt was measured as the ratio of rare earth elements to base cations in the applied rock dust and in the surface soil. Basalt application stimulated peak biomass and net primary production in both cropping systems and caused a small but significant stimulation of soil respiration. Net ecosystem carbon balance (NECB) was strongly negative for maize/soybean (-199 to -453 g C m-2 year-1 ) indicating this system was losing carbon to the atmosphere. Average EW (102 g C m-2 year-1 ) offset carbon loss in the maize/soybean by 23%-42%. NECB of miscanthus was positive (63-129 g C m-2 year-1 ), indicating carbon gain in the system, and EW greatly increased inorganic carbon storage by an additional 234 g C m-2 year-1 . Our analysis indicates a co-deployment of a perennial biofuel crop (miscanthus) with EW leads to major wins-increased harvested yields of 29%-42% with additional carbon dioxide removal (CDR) of 8.6 t CO2 ha-1 year-1 . EW applied to maize/soybean drives a CDR of 3.7 t CO2 ha-1 year-1 , which partially offsets well-established carbon losses from soil from this crop rotation. EW applied in the US Midwest creates measurable improvements to the carbon budgets perennial bioenergy crops and conventional row crops.
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Affiliation(s)
- Ilsa B Kantola
- Institute for Sustainability, Energy, and Environment, Carl R. Woese Institute for Genomic Biology, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
- Carl R. Woese Institute for Genomic Biology, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
| | - Elena Blanc-Betes
- Center for Applied Bioenergy and Bioproducts Innovation, Institute for Sustainability, Energy, and Environment, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
| | - Michael D Masters
- Institute for Sustainability, Energy, and Environment, Carl R. Woese Institute for Genomic Biology, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
| | | | | | - Caitlin E Moore
- School of Agriculture and Environment, The University of Western Australia, Crawley, Western Australia, Australia
| | - Adam von Haden
- Department of Agronomy, University of Wisconsin, Madison, Wisconsin, USA
| | - Carl J Bernacchi
- Global Change Photosynthesis Research Unit, USDA/ARS, Urbana, Illinois, USA
- Department of Plant Biology, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
| | - Adam Wolf
- Eion Corp., Princeton, New Jersey, USA
| | - Dimitar Z Epihov
- Department of Animal and Plant Sciences, Leverhulme Centre for Climate Change Mitigation, University of Sheffield, Sheffield, UK
| | - David J Beerling
- Department of Animal and Plant Sciences, Leverhulme Centre for Climate Change Mitigation, University of Sheffield, Sheffield, UK
| | - Evan H DeLucia
- Institute for Sustainability, Energy, and Environment, Carl R. Woese Institute for Genomic Biology, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
- Carl R. Woese Institute for Genomic Biology, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
- Center for Applied Bioenergy and Bioproducts Innovation, Institute for Sustainability, Energy, and Environment, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
- Department of Plant Biology, University of Illinois at Urbana-Champaign, Urbana, Illinois, USA
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6
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Melikov CH, Bukoski JJ, Cook-Patton SC, Ban H, Chen JL, Potts MD. Quantifying the Effect Size of Management Actions on Aboveground Carbon Stocks in Forest Plantations. CURRENT FORESTRY REPORTS 2023; 9:131-148. [PMID: 37426633 PMCID: PMC10328870 DOI: 10.1007/s40725-023-00182-5] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Accepted: 02/22/2023] [Indexed: 07/11/2023]
Abstract
Purpose of the Review Improved forest management is a promising avenue for climate change mitigation. However, we lack synthetic understanding of how different management actions impact aboveground carbon stocks, particularly at scales relevant for designing and implementing forest-based climate solutions. Here, we quantitatively assess and review the impacts of three common practices-application of inorganic NPK fertilizer, interplanting with N-fixing species, and thinning-on aboveground carbon stocks in plantation forests. Recent Findings Site-level empirical studies show both positive and negative effects of inorganic fertilization, interplanting, and thinning on aboveground carbon stocks in plantation forests. Recent findings and the results of our analysis suggest that these effects are heavily moderated by factors such as species selection, precipitation, time since practice, soil moisture regime, and previous land use. Interplanting of N-fixing crops initially has no effect on carbon storage in main tree crops, but the effect becomes positive in older stands. Conversely, the application of NPK fertilizers increases aboveground carbon stocks, though the effect lessens with time. Moreover, increases in aboveground carbon stocks may be partially or completely offset by emissions from the application of inorganic fertilizer. Thinning results in a strong reduction of aboveground carbon stocks, though the effect lessens with time. Summary Management practices tend to have strong directional effects on aboveground carbon stocks in plantation forests but are moderated by site-specific management, climatic, and edaphic factors. The effect sizes quantified in our meta-analysis can serve as benchmarks for the design and scoping of improved forest management projects as forest-based climate solutions. Overall, management actions can enhance the climate mitigation potential of plantation forests, if performed with sufficient attention to the nuances of local conditions. Supplementary Information The online version contains supplementary material available at 10.1007/s40725-023-00182-5.
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Affiliation(s)
- Cyril H. Melikov
- Environmental Defense Fund, New York, NY USA
- Department of Environmental Science, Policy and Management, University of California, Berkeley, CA USA
| | - Jacob J. Bukoski
- Moore Center for Science, Conservation International, Arlington, VA USA
- Department of Forest Ecosystems and Society, Oregon State University, Corvallis, OR USA
| | | | - Hongyi Ban
- Department of Environmental Science, Policy and Management, University of California, Berkeley, CA USA
| | - Jessica L. Chen
- Department of Environmental Science, Policy and Management, University of California, Berkeley, CA USA
| | - Matthew D. Potts
- Department of Environmental Science, Policy and Management, University of California, Berkeley, CA USA
- Carbon Direct Inc, New York, NY USA
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7
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Yao X, Hui D, Hou E, Xiong J, Xing S, Deng Q. Differential responses and mechanistic controls of soil phosphorus transformation in Eucalyptus plantations with N fertilization and introduced N 2 -fixing tree species. THE NEW PHYTOLOGIST 2023; 237:2039-2053. [PMID: 36513603 DOI: 10.1111/nph.18673] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/26/2022] [Accepted: 12/02/2022] [Indexed: 06/17/2023]
Abstract
Introducing N2 -fixing tree species into Eucalyptus plantations could replace nitrogen (N) fertilization to maintain high levels of N consumption and productivity. However, N enrichment may exacerbate phosphorus (P) limitation as Eucalyptus robusta Smith is extensively planted in P-poor tropical and subtropical soils. We conducted a field experiment in a pure plantation of Eucalyptus urophylla × grandis to investigate the impacts of N fertilization and introduced an N2 -fixing tree of Dalbergia odorifera T. Chen on soil P transformation. Nitrogen fertilization significantly enhanced soil occluded P pool and reduced the other P pools due to acidification-induced pH-sensitive geochemical processes, lowering Eucalyptus leaf P concentration with higher N : P ratio. By contrast, introduced N2 -fixing tree species did not change soil pH, labile inorganic P pool, and Eucalyptus leaf N : P ratio, even enhanced organic P pools and reduced occluded P pool probably due to altering microbial community composition particularly stimulating arbuscular mycorrhiza fungal abundance. Our results revealed differential responses and mechanistic controls of soil P transformation in Eucalyptus plantations with N fertilization and introduced N2 -fixing tree species. The dissolution of occluded P pool along with organic P accumulation observed in the mixed plantations may represent a promising future to better manage soil P availability.
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Affiliation(s)
- Xianyu Yao
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, Guangdong, 510650, China
- South China National Botanical Garden, Guangzhou, Guangdong, 510650, China
| | - Dafeng Hui
- Department of Biological Sciences, Tennessee State University, Nashville, TN, 37209, USA
| | - Enqing Hou
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, Guangdong, 510650, China
- South China National Botanical Garden, Guangzhou, Guangdong, 510650, China
| | - Junfei Xiong
- Experimental Center of Topical Forestry, Chinese Academy of Forestry, Pingxiang, 532600, China
| | - Shuo Xing
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, Guangdong, 510650, China
- South China National Botanical Garden, Guangzhou, Guangdong, 510650, China
| | - Qi Deng
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, Guangdong, 510650, China
- South China National Botanical Garden, Guangzhou, Guangdong, 510650, China
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8
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Bukombe B, Bauters M, Boeckx P, Cizungu LN, Cooper M, Fiener P, Kidinda LK, Makelele I, Muhindo DI, Rewald B, Verheyen K, Doetterl S. Soil geochemistry - and not topography - as a major driver of carbon allocation, stocks, and dynamics in forests and soils of African tropical montane ecosystems. THE NEW PHYTOLOGIST 2022; 236:1676-1690. [PMID: 36089827 DOI: 10.1111/nph.18469] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/28/2022] [Accepted: 08/14/2022] [Indexed: 06/15/2023]
Abstract
The lack of field-based data in the tropics limits our mechanistic understanding of the drivers of net primary productivity (NPP) and allocation. Specifically, the role of local edaphic factors - such as soil parent material and topography controlling soil fertility as well as water and nutrient fluxes - remains unclear and introduces substantial uncertainty in understanding net ecosystem productivity and carbon (C) stocks. Using a combination of vegetation growth monitoring and soil geochemical properties, we found that soil fertility parameters reflecting the local parent material are the main drivers of NPP and C allocation patterns in tropical montane forests, resulting in significant differences in below- to aboveground biomass components across geochemical (soil) regions. Topography did not constrain the variability in C allocation and NPP. Soil organic C stocks showed no relation to C input in tropical forests. Instead, plant C input seemingly exceeded the maximum potential of these soils to stabilize C. We conclude that, even after many millennia of weathering and the presence of deeply developed soils, above- and belowground C allocation in tropical forests, as well as soil C stocks, vary substantially due to the geochemical properties that soils inherit from parent material.
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Affiliation(s)
- Benjamin Bukombe
- Institute of Geography, Augsburg University, Augsburg, 86159, Germany
| | - Marijn Bauters
- Department of Environment, Ghent University, Ghent, 9000, Belgium
- Department of Green Chemistry and Technology, Isotope Bioscience Laboratory - ISOFYS, Ghent University, Ghent, 9000, Belgium
| | - Pascal Boeckx
- Department of Green Chemistry and Technology, Isotope Bioscience Laboratory - ISOFYS, Ghent University, Ghent, 9000, Belgium
| | - Landry Ntaboba Cizungu
- Faculty of Agricultural Sciences, Université Catholique de Bukavu, Bugabo 02, Bukavu, Democratic Republic of the Congo
| | - Matthew Cooper
- Department of Environmental Systems Science, ETH Zurich, Zurich, 8092, Switzerland
| | - Peter Fiener
- Institute of Geography, Augsburg University, Augsburg, 86159, Germany
| | - Laurent Kidinda Kidinda
- Institute of Soil Science and Site Ecology, Technische Universität Dresden, Tharandt, 01737, Germany
| | - Isaac Makelele
- Department of Green Chemistry and Technology, Isotope Bioscience Laboratory - ISOFYS, Ghent University, Ghent, 9000, Belgium
| | - Daniel Iragi Muhindo
- Faculty of Agricultural Sciences, Université Catholique de Bukavu, Bugabo 02, Bukavu, Democratic Republic of the Congo
| | - Boris Rewald
- Department of Forest and Soil Sciences, Institute of Forest Ecology, University of Natural Resources and Life Sciences, Vienna (BOKU), Vienna, 1190, Austria
| | - Kris Verheyen
- Department of Environment, Ghent University, Ghent, 9000, Belgium
| | - Sebastian Doetterl
- Institute of Geography, Augsburg University, Augsburg, 86159, Germany
- Department of Environmental Systems Science, ETH Zurich, Zurich, 8092, Switzerland
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9
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Calabrese S, Wild B, Bertagni MB, Bourg IC, White C, Aburto F, Cipolla G, Noto LV, Porporato A. Nano- to Global-Scale Uncertainties in Terrestrial Enhanced Weathering. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:15261-15272. [PMID: 36269897 DOI: 10.1021/acs.est.2c03163] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/16/2023]
Abstract
Enhanced weathering (EW) is one of the most promising negative emissions technologies urgently needed to limit global warming to at least below 2 °C, a goal recently reaffirmed at the UN Global Climate Change conference (i.e., COP26). EW relies on the accelerated dissolution of crushed silicate rocks applied to soils and is considered a sustainable solution requiring limited technology. While EW has a high theoretical potential of sequestering CO2, research is still needed to provide accurate estimates of carbon (C) sequestration when applying different silicate materials across distinct climates and major soil types in combination with a variety of plants. Here we elaborate on fundamental advances that must be addressed before EW can be extensively adopted. These include identifying the most suitable environmental conditions, improving estimates of field dissolution rates and efficacy of CO2 removal, and identifying alternative sources of silicate materials to meet future EW demands. We conclude with considerations on the necessity of integrated modeling-experimental approaches to better coordinate future field experiments and measurements of CO2 removal, as well as on the importance of seamlessly coordinating EW with cropland and forest management.
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Affiliation(s)
- Salvatore Calabrese
- Biological and Agricultural Engineering, Texas A&M University, 333 Spence St., College Station, Texas77843, United States
| | - Bastien Wild
- Civil and Environmental Engineering, Princeton University, 59 Olden St., Princeton, New Jersey08540, United States
- Andlinger Center for Energy and the Environment, Princeton University, 59 Olden St., Princeton, New Jersey08540, United States
| | - Matteo B Bertagni
- High Meadows Environmental Institute, Guyot Hall, Princeton University, Princeton, New Jersey08544, United States
| | - Ian C Bourg
- Civil and Environmental Engineering, Princeton University, 59 Olden St., Princeton, New Jersey08540, United States
- High Meadows Environmental Institute, Guyot Hall, Princeton University, Princeton, New Jersey08544, United States
| | - Claire White
- Civil and Environmental Engineering, Princeton University, 59 Olden St., Princeton, New Jersey08540, United States
- Andlinger Center for Energy and the Environment, Princeton University, 59 Olden St., Princeton, New Jersey08540, United States
| | - Felipe Aburto
- Soil and Crop Sciences, Texas A&M University, 370 Olsen Blvd., College Station, Texas77843, United States
| | - Giuseppe Cipolla
- Dipartimento di Ingegneria, University of Palermo, Viale delle Scienze, 90128Palermo, PA, Italy
| | - Leonardo V Noto
- Dipartimento di Ingegneria, University of Palermo, Viale delle Scienze, 90128Palermo, PA, Italy
| | - Amilcare Porporato
- Civil and Environmental Engineering, Princeton University, 59 Olden St., Princeton, New Jersey08540, United States
- High Meadows Environmental Institute, Guyot Hall, Princeton University, Princeton, New Jersey08544, United States
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10
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Oren A. Candidatus List No. 4: Lists of names of prokaryotic Candidatus taxa. Int J Syst Evol Microbiol 2022; 72. [PMID: 36748458 DOI: 10.1099/ijsem.0.005545] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/26/2022] Open
Affiliation(s)
- Aharon Oren
- The Institute of Life Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, 9190401 Jerusalem, Israel
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11
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Dallstream C, Weemstra M, Soper FM. A framework for fine‐root trait syndromes: syndrome coexistence may support phosphorus partitioning in tropical forests. OIKOS 2022. [DOI: 10.1111/oik.08908] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Affiliation(s)
| | - Monique Weemstra
- Ecology and Evolutionary Biology, Univ. of Michigan Ann Arbor MI USA
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12
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Yu RP, Lambers H, Callaway RM, Wright AJ, Li L. Belowground facilitation and trait matching: two or three to tango? TRENDS IN PLANT SCIENCE 2021; 26:1227-1235. [PMID: 34400074 DOI: 10.1016/j.tplants.2021.07.014] [Citation(s) in RCA: 20] [Impact Index Per Article: 6.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/16/2021] [Revised: 07/15/2021] [Accepted: 07/24/2021] [Indexed: 05/12/2023]
Abstract
High biodiversity increases ecosystem functions; however, belowground facilitation remains poorly understood in this context. Here, we explore mechanisms that operate via 'giving-receiving feedbacks' for belowground facilitation. These include direct effects via root exudates, signals, and root trait plasticity, and indirect biotic facilitation via the effects of root exudates on soil biota and feedback from biota to plants. We then highlight that these two- or three-way mechanisms must affect biodiversity-ecosystem function relationships via specific combinations of matching traits. To tango requires a powerful affinity and harmony between well-matched partners, and such matches link belowground facilitation to the effect of biodiversity on function. Such matching underpins applications in intercropping, forestry, and pasture systems, in which diversity contributes to greater productivity and sustainability.
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Affiliation(s)
- Rui-Peng Yu
- Key Laboratory of Plant-Soil Interactions, Ministry of Education, Beijing Key Laboratory of Biodiversity and Organic Farming, College of Resources and Environmental Sciences, China Agricultural University, 2 Yuan Ming Yuan West Road, Beijing 100193, PR China
| | - Hans Lambers
- School of Biological Sciences and Institute of Agriculture, The University of Western Australia, 35 Stirling Highway, Crawley, Perth, WA 6009, Australia; National Academy of Agriculture Green Development, China Agricultural University, 2 Yuan Ming Yuan West Road, Beijing 100193, PR China
| | - Ragan M Callaway
- Division of Biological Sciences and Institute on Ecosystems, University of Montana, 32 Campus Drive, Missoula, MT 59812, USA
| | - Alexandra J Wright
- Department of Biological Sciences, California State University Los Angeles, 5151 State University Drive, Los Angeles, CA 90032, USA
| | - Long Li
- Key Laboratory of Plant-Soil Interactions, Ministry of Education, Beijing Key Laboratory of Biodiversity and Organic Farming, College of Resources and Environmental Sciences, China Agricultural University, 2 Yuan Ming Yuan West Road, Beijing 100193, PR China.
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13
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Land use influences stream bacterial communities in lowland tropical watersheds. Sci Rep 2021; 11:21752. [PMID: 34741067 PMCID: PMC8571290 DOI: 10.1038/s41598-021-01193-7] [Citation(s) in RCA: 6] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/06/2021] [Accepted: 10/18/2021] [Indexed: 01/04/2023] Open
Abstract
Land use is known to affect water quality yet the impact it has on aquatic microbial communities in tropical systems is poorly understood. We used 16S metabarcoding to assess the impact of land use on bacterial communities in the water column of four streams in central Panama. Each stream was influenced by a common Neotropical land use: mature forest, secondary forest, silvopasture and traditional cattle pasture. Bacterial community diversity and composition were significantly influenced by nearby land uses. Streams bordered by forests had higher phylogenetic diversity (Faith’s PD) and similar community structure (based on weighted UniFrac distance), whereas the stream surrounded by traditional cattle pasture had lower diversity and unique bacterial communities. The silvopasture stream showed strong seasonal shifts, with communities similar to forested catchments during the wet seasons and cattle pasture during dry seasons. We demonstrate that natural forest regrowth and targeted management, such as maintaining and restoring riparian corridors, benefit stream-water microbiomes in tropical landscapes and can provide a rapid and efficient approach to balancing agricultural activities and water quality protection.
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14
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Glick BR, Gamalero E. Recent Developments in the Study of Plant Microbiomes. Microorganisms 2021; 9:microorganisms9071533. [PMID: 34361969 PMCID: PMC8306116 DOI: 10.3390/microorganisms9071533] [Citation(s) in RCA: 44] [Impact Index Per Article: 14.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/25/2021] [Revised: 07/11/2021] [Accepted: 07/16/2021] [Indexed: 02/06/2023] Open
Abstract
To date, an understanding of how plant growth-promoting bacteria facilitate plant growth has been primarily based on studies of individual bacteria interacting with plants under different conditions. More recently, it has become clear that specific soil microorganisms interact with one another in consortia with the collective being responsible for the positive effects on plant growth. Different plants attract different cross-sections of the bacteria and fungi in the soil, initially based on the composition of the unique root exudates from each plant. Thus, plants mostly attract those microorganisms that are beneficial to plants and exclude those that are potentially pathogenic. Beneficial bacterial consortia not only help to promote plant growth, these consortia also protect plants from a wide range of direct and indirect environmental stresses. Moreover, it is currently possible to engineer plant seeds to contain desired bacterial strains and thereby benefit the next generation of plants. In this way, it may no longer be necessary to deliver beneficial microbiota to each individual growing plant. As we develop a better understanding of beneficial bacterial microbiomes, it may become possible to develop synthetic microbiomes where compatible bacteria work together to facilitate plant growth under a wide range of natural conditions.
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Affiliation(s)
- Bernard R. Glick
- Department of Biology, University of Waterloo, Waterloo, ON N2L 3G1, Canada;
| | - Elisa Gamalero
- Dipartimento di Scienze e Innovazione Tecnologica, Università del Piemonte Orientale “A. Avogadro”, Viale Teresa Michel, 11, 15121 Alessandria, Italy
- Correspondence:
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