Articles | Volume 22, issue 15
https://doi.org/10.5194/bg-22-4013-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-22-4013-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Fertilization turns a rubber plantation from sink to methane source
Daniel Epron
CORRESPONDING AUTHOR
Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan
Faculty of Agriculture, Kasetsart University, Bangkok 10900, Thailand
Rawiwan Chotiphan
Sithiporn Kridakara Research Station, Faculty of Agriculture at Kamphaeng Saen, Kasetsart University, Prachuap Khiri Khan 77170, Thailand
Zixiao Wang
Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan
Ornuma Duangngam
DORAS Centre, Kasetsart University, Bangkok 10900, Thailand
Makoto Shibata
Graduate School of Global Environmental Studies, Kyoto University, Kyoto 606-8501, Japan
Sumonta Kumar Paul
Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan
Takumi Mochidome
Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan
Jate Sathornkich
Faculty of Agriculture, Kasetsart University, Bangkok 10900, Thailand
Wakana A. Azuma
Graduate School of Agricultural Science, Kobe University, Kobe 657-8501, Japan
Jun Murase
Faculty of Agriculture, Kasetsart University, Bangkok 10900, Thailand
Graduate School of Bioagricultural Sciences, Nagoya University, Nagoya 464-8601, Japan
Yann Nouvellon
DORAS Centre, Kasetsart University, Bangkok 10900, Thailand
UMR Eco&Sols, CIRAD, 2 Place Viala, 34060 Montpellier CEDEX 2, France
Poonpipope Kasemsap
Faculty of Agriculture, Kasetsart University, Bangkok 10900, Thailand
DORAS Centre, Kasetsart University, Bangkok 10900, Thailand
Kannika Sajjaphan
CORRESPONDING AUTHOR
Faculty of Agriculture, Kasetsart University, Bangkok 10900, Thailand
Related authors
Sumonta Kumar Paul, Keisuke Yuasa, Masako Dannoura, and Daniel Epron
EGUsphere, https://doi.org/10.5194/egusphere-2025-3449, https://doi.org/10.5194/egusphere-2025-3449, 2025
This preprint is open for discussion and under review for Biogeosciences (BG).
Short summary
Short summary
This study used a machine learning approach to scale soil CH4 fluxes over time in a topographically complex mountain forest. Within the landscape, predicted upland CH4 fluxes varied significantly across topographic positions, with the greater uptake on ridges and slopes than in the plain and foot slopes. Recent past precipitations significantly influenced seasonal CH4 uptake. Our findings highlight the role of topography and the potential of remote sensing and machine learning to map CH4 fluxes.
Jun Murase, Kannika Sajjaphan, Chatprawee Dechjiraratthanasiri, Ornuma Duangngam, Rawiwan Chotiphan, Wutthida Rattanapichai, Wakana Azuma, Makoto Shibata, Poonpipope Kasemsap, and Daniel Epron
SOIL, 11, 457–466, https://doi.org/10.5194/soil-11-457-2025, https://doi.org/10.5194/soil-11-457-2025, 2025
Short summary
Short summary
Tropical forest soils are vital for methane uptake, but deforestation and agriculture can alter soil methane oxidation. An experiment in Thailand shows that fertilization significantly suppresses methane oxidation in rubber plantation soils, affecting depths up to 60 cm. Without fertilization, deeper soil layers (below 10 cm) actively oxidize methane. These findings suggest that fertilization negatively impacts the methane uptake capacity of deep-layer soils in rubber plantations.
Emilie Delogu, Bernard Longdoz, Caroline Plain, and Daniel Epron
Biogeosciences Discuss., https://doi.org/10.5194/bg-2016-194, https://doi.org/10.5194/bg-2016-194, 2016
Preprint withdrawn
Sumonta Kumar Paul, Keisuke Yuasa, Masako Dannoura, and Daniel Epron
EGUsphere, https://doi.org/10.5194/egusphere-2025-3449, https://doi.org/10.5194/egusphere-2025-3449, 2025
This preprint is open for discussion and under review for Biogeosciences (BG).
Short summary
Short summary
This study used a machine learning approach to scale soil CH4 fluxes over time in a topographically complex mountain forest. Within the landscape, predicted upland CH4 fluxes varied significantly across topographic positions, with the greater uptake on ridges and slopes than in the plain and foot slopes. Recent past precipitations significantly influenced seasonal CH4 uptake. Our findings highlight the role of topography and the potential of remote sensing and machine learning to map CH4 fluxes.
Jun Murase, Kannika Sajjaphan, Chatprawee Dechjiraratthanasiri, Ornuma Duangngam, Rawiwan Chotiphan, Wutthida Rattanapichai, Wakana Azuma, Makoto Shibata, Poonpipope Kasemsap, and Daniel Epron
SOIL, 11, 457–466, https://doi.org/10.5194/soil-11-457-2025, https://doi.org/10.5194/soil-11-457-2025, 2025
Short summary
Short summary
Tropical forest soils are vital for methane uptake, but deforestation and agriculture can alter soil methane oxidation. An experiment in Thailand shows that fertilization significantly suppresses methane oxidation in rubber plantation soils, affecting depths up to 60 cm. Without fertilization, deeper soil layers (below 10 cm) actively oxidize methane. These findings suggest that fertilization negatively impacts the methane uptake capacity of deep-layer soils in rubber plantations.
Ivan Cornut, Nicolas Delpierre, Jean-Paul Laclau, Joannès Guillemot, Yann Nouvellon, Otavio Campoe, Jose Luiz Stape, Vitoria Fernanda Santos, and Guerric le Maire
Biogeosciences, 20, 3093–3117, https://doi.org/10.5194/bg-20-3093-2023, https://doi.org/10.5194/bg-20-3093-2023, 2023
Short summary
Short summary
Potassium is an essential element for living organisms. Trees are dependent upon this element for certain functions that allow them to build their trunks using carbon dioxide. Using data from experiments in eucalypt plantations in Brazil and a simplified computer model of the plantations, we were able to investigate the effect that a lack of potassium can have on the production of wood. Understanding nutrient cycles is useful to understand the response of forests to environmental change.
Ivan Cornut, Guerric le Maire, Jean-Paul Laclau, Joannès Guillemot, Yann Nouvellon, and Nicolas Delpierre
Biogeosciences, 20, 3119–3135, https://doi.org/10.5194/bg-20-3119-2023, https://doi.org/10.5194/bg-20-3119-2023, 2023
Short summary
Short summary
After simulating the effects of low levels of potassium on the canopy of trees and the uptake of carbon dioxide from the atmosphere by leaves in Part 1, here we tried to simulate the way the trees use the carbon they have acquired and the interaction with the potassium cycle in the tree. We show that the effect of low potassium on the efficiency of the trees in acquiring carbon is enough to explain why they produce less wood when they are in soils with low levels of potassium.
Anna B. Harper, Karina E. Williams, Patrick C. McGuire, Maria Carolina Duran Rojas, Debbie Hemming, Anne Verhoef, Chris Huntingford, Lucy Rowland, Toby Marthews, Cleiton Breder Eller, Camilla Mathison, Rodolfo L. B. Nobrega, Nicola Gedney, Pier Luigi Vidale, Fred Otu-Larbi, Divya Pandey, Sebastien Garrigues, Azin Wright, Darren Slevin, Martin G. De Kauwe, Eleanor Blyth, Jonas Ardö, Andrew Black, Damien Bonal, Nina Buchmann, Benoit Burban, Kathrin Fuchs, Agnès de Grandcourt, Ivan Mammarella, Lutz Merbold, Leonardo Montagnani, Yann Nouvellon, Natalia Restrepo-Coupe, and Georg Wohlfahrt
Geosci. Model Dev., 14, 3269–3294, https://doi.org/10.5194/gmd-14-3269-2021, https://doi.org/10.5194/gmd-14-3269-2021, 2021
Short summary
Short summary
We evaluated 10 representations of soil moisture stress in the JULES land surface model against site observations of GPP and latent heat flux. Increasing the soil depth and plant access to deep soil moisture improved many aspects of the simulations, and we recommend these settings in future work using JULES. In addition, using soil matric potential presents the opportunity to include parameters specific to plant functional type to further improve modeled fluxes.
Anteneh Getachew Mengistu, Gizaw Mengistu Tsidu, Gerbrand Koren, Maurits L. Kooreman, K. Folkert Boersma, Torbern Tagesson, Jonas Ardö, Yann Nouvellon, and Wouter Peters
Biogeosciences, 18, 2843–2857, https://doi.org/10.5194/bg-18-2843-2021, https://doi.org/10.5194/bg-18-2843-2021, 2021
Short summary
Short summary
In this study, we assess the usefulness of Sun-Induced Fluorescence of Terrestrial Ecosystems Retrieval (SIFTER) data from the GOME-2A instrument and near-infrared reflectance of vegetation (NIRv) from MODIS to capture the seasonality and magnitudes of gross primary production (GPP) derived from six eddy-covariance flux towers in Africa in the overlap years between 2007–2014. We also test the robustness of sun-induced fluoresence and NIRv to compare the seasonality of GPP for the major biomes.
Rosa M. Poch, Lucia H. C. dos Anjos, Rafla Attia, Megan Balks, Adalberto Benavides-Mendoza, Martha M. Bolaños-Benavides, Costanza Calzolari, Lydia M. Chabala, Peter C. de Ruiter, Samuel Francke-Campaña, Fernando García Préchac, Ellen R. Graber, Siosiua Halavatau, Kutaiba M. Hassan, Edmond Hien, Ke Jin, Mohammad Khan, Maria Konyushkova, David A. Lobb, Matshwene E. Moshia, Jun Murase, Generose Nziguheba, Ashok K. Patra, Gary Pierzynski, Natalia Rodríguez Eugenio, and Ronald Vargas Rojas
SOIL, 6, 541–547, https://doi.org/10.5194/soil-6-541-2020, https://doi.org/10.5194/soil-6-541-2020, 2020
Short summary
Short summary
Humanity depends on the existence of healthy soils, both for the production of food and for ensuring a healthy, biodiverse environment. In the face of global crises like the COVID-19 pandemic, a sustainable soil management strategy is essential to ensure food security based on more diverse, locally oriented, and resilient food production systems through improving access to land, sound land use planning, sustainable soil management, enhanced research, and investment in education and extension.
Jun Murase, Atsuko Sugimoto, Ryo Shingubara, Tomoki Morozumi, Shinya Takano, and Trofim C. Maximov
Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-98, https://doi.org/10.5194/bg-2019-98, 2019
Manuscript not accepted for further review
Short summary
Short summary
We determined the potential methane oxidation rate of the wetland soils in northeastern Siberia in situ or immediately after sampling to avoid the possible influence of sample storage. The soils had a high methane oxidation potential even under anoxic and frozen conditions, while the plant-associated methane oxidation is negligible. The results show the high tolerance and resilience of methane oxidation to the unfavorable conditions, contributing to understanding the methane cycle in the Arctic.
Ryo Shingubara, Atsuko Sugimoto, Jun Murase, Go Iwahana, Shunsuke Tei, Maochang Liang, Shinya Takano, Tomoki Morozumi, and Trofim C. Maximov
Biogeosciences, 16, 755–768, https://doi.org/10.5194/bg-16-755-2019, https://doi.org/10.5194/bg-16-755-2019, 2019
Short summary
Short summary
(1) Wetting event with extreme precipitation increased methane emission from wetland, especially two summers later, despite the decline in water level after the wetting. (2) Isotopic compositions of methane in soil pore water suggested enhancement of production and less significance of oxidation in the following two summers after the wetting event. (3) Duration of water saturation in the active layer may be important for predicting methane emission after a wetting event in permafrost ecosystems.
Emilie Delogu, Bernard Longdoz, Caroline Plain, and Daniel Epron
Biogeosciences Discuss., https://doi.org/10.5194/bg-2016-194, https://doi.org/10.5194/bg-2016-194, 2016
Preprint withdrawn
Related subject area
Biogeochemistry: Land
On the added value of sequential deep learning for the upscaling of evapotranspiration
Seasonality and synchrony of photosynthesis in African forests inferred from spaceborne chlorophyll fluorescence and vegetation indices
Altitudinal distribution of soil organic and inorganic carbon in a dry alpine rangeland of northern Qinghai-Tibetan Plateau
Precipitation–fire functional interactions control biomass stocks and carbon exchanges across the world's largest savanna
Nitrogen concentrations in boreal and temperate tree tissues vary with tree age/size, growth rate, and climate
Burn severity and vegetation type control phosphorus concentration, molecular composition, and mobilization
Comparison of shortwave radiation dynamics between boreal forest and open peatland pairs in southern and northern Finland
Subsurface CO2 dynamics in a temperate karst system reveal complex seasonal and spatial variations
Cropland expansion drives vegetation greenness decline in Southeast Asia
How to measure the efficiency of bioenergy crops compared to forestation
Annual net CO2 fluxes from drained organic soils used for agriculture in the hemiboreal region of Europe
Implications of climate and litter quality for simulations of litterbag decomposition at high latitudes
Soil carbon-concentration and carbon-climate feedbacks in CMIP6 Earth system models
Monitoring the impact of forest changes on carbon uptake with solar-induced fluorescence measurements from GOME-2A and TROPOMI for an Australian and Chinese case study
Technical note: Flagging inconsistencies in flux tower data
Uncertainty in Amazon vegetation productivity in CMIP6 projections driven by surface energy fluxes
Relevance of near-surface soil moisture vs. terrestrial water storage for global vegetation functioning
High-resolution spatial patterns and drivers of terrestrial ecosystem carbon dioxide, methane, and nitrous oxide fluxes in the tundra
Long-term additions of ammonium nitrate to montane forest ecosystems may cause limited soil acidification, even in the presence of soil carbonate
Leaf carbon and nitrogen stoichiometric variation along environmental gradients
Gross primary productivity and the predictability of CO2: more uncertainty in what we predict than how well we predict it
Scale variance in the carbon dynamics of fragmented, mixed-use landscapes estimated using model–data fusion
Seasonal controls override forest harvesting effects on the composition of dissolved organic matter mobilized from boreal forest soil organic horizons
Carbon cycle extremes accelerate weakening of the land carbon sink in the late 21st century
Estimating oil-palm Si storage, Si return to soils, and Si losses through harvest in smallholder oil-palm plantations of Sumatra, Indonesia
Assessing the sensitivity of multi-frequency passive microwave vegetation optical depth to vegetation properties
Seasonal variation of mercury concentration of ancient olive groves of Lebanon
Soil organic matter diagenetic state informs boreal forest ecosystem feedbacks to climate change
Upscaling dryland carbon and water fluxes with artificial neural networks of optical, thermal, and microwave satellite remote sensing
Sun-induced fluorescence as a proxy for primary productivity across vegetation types and climates
Technical note: A view from space on global flux towers by MODIS and Landsat: the FluxnetEO data set
Changing sub-Arctic tundra vegetation upon permafrost degradation: impact on foliar mineral element cycling
Land Management Contributes significantly to observed Vegetation Browning in Syria during 2001–2018
MODIS Vegetation Continuous Fields tree cover needs calibrating in tropical savannas
Assessing the representation of the Australian carbon cycle in global vegetation models
Assessing the response of soil carbon in Australia to changing inputs and climate using a consistent modelling framework
Reviews and syntheses: Ongoing and emerging opportunities to improve environmental science using observations from the Advanced Baseline Imager on the Geostationary Operational Environmental Satellites
First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region
The impact of wildfire on biogeochemical fluxes and water quality in boreal catchments
Examining the sensitivity of the terrestrial carbon cycle to the expression of El Niño
Subalpine grassland productivity increased with warmer and drier conditions, but not with higher N deposition, in an altitudinal transplantation experiment
Reviews and syntheses: Impacts of plant-silica–herbivore interactions on terrestrial biogeochemical cycling
Implementation of nitrogen cycle in the CLASSIC land model
Combined effects of ozone and drought stress on the emission of biogenic volatile organic compounds from Quercus robur L.
A bottom-up quantification of foliar mercury uptake fluxes across Europe
Lagged effects regulate the inter-annual variability of the tropical carbon balance
Spatial variations in terrestrial net ecosystem productivity and its local indicators
Nitrogen cycling in CMIP6 land surface models: progress and limitations
Decomposing reflectance spectra to track gross primary production in a subalpine evergreen forest
Sensitivity of 21st century simulated ecosystem indicators to model parameters, prescribed climate drivers, RCP scenarios and forest management actions for two Finnish boreal forest sites
Basil Kraft, Jacob A. Nelson, Sophia Walther, Fabian Gans, Ulrich Weber, Gregory Duveiller, Markus Reichstein, Weijie Zhang, Marc Rußwurm, Devis Tuia, Marco Körner, Zayd Hamdi, and Martin Jung
Biogeosciences, 22, 3965–3987, https://doi.org/10.5194/bg-22-3965-2025, https://doi.org/10.5194/bg-22-3965-2025, 2025
Short summary
Short summary
This study evaluates machine learning approaches for upscaling evapotranspiration from the site to the global scale. Sequential models capture temporal dynamics better, especially with precipitation data, but all models show biases in data-scarce regions. Improved upscaling requires richer training data, informed covariate selection, and physical constraints to enhance robustness and reduce extrapolation errors.
Russell Doughty, Michael C. Wimberly, Dan Wanyama, Helene Peiro, Nicholas Parazoo, Sean Crowell, and Moses Azong Cho
Biogeosciences, 22, 1985–2004, https://doi.org/10.5194/bg-22-1985-2025, https://doi.org/10.5194/bg-22-1985-2025, 2025
Short summary
Short summary
We find West African solar-induced fluorescence (SIF) increases during the dry season and peaks before precipitation, similar to the Amazon. In central Africa, a continental-scale bimodal SIF seasonality appears; its minimum aligns with precipitation, but its maximum seems less environmentally driven. Notably, differences between SIF and vegetation index (VI) seasonality indicate VI-based photosynthesis estimates may be inaccurate.
Qinglin Liu, Ailin Zhang, Xiangyi Li, Jinfei Yin, Yuxue Zhang, Osbert Jianxin Sun, and Yong Jiang
EGUsphere, https://doi.org/10.5194/egusphere-2025-1269, https://doi.org/10.5194/egusphere-2025-1269, 2025
Short summary
Short summary
The arid region of the plateau is a fragile ecosystem sensitive to environmental change. Changes in the soil carbon pool in this ecosystem will affect the terrestrial carbon cycle. The soil carbon pool in this region is mainly composed of soil inorganic carbon, and the response to environmental changes is more obvious. At the same time, the impact of environment on vegetation is also an important part of the carbon cycle of terrestrial organisms.
Mathew Williams, David T. Milodowski, T. Luke Smallman, Kyle G. Dexter, Gabi C. Hegerl, Iain M. McNicol, Michael O'Sullivan, Carla M. Roesch, Casey M. Ryan, Stephen Sitch, and Aude Valade
Biogeosciences, 22, 1597–1614, https://doi.org/10.5194/bg-22-1597-2025, https://doi.org/10.5194/bg-22-1597-2025, 2025
Short summary
Short summary
Southern African woodlands are important in both regional and global carbon cycles. A new carbon analysis created by combining satellite data with ecosystem modelling shows that the region has a neutral C balance overall but with important spatial variations. Patterns of biomass and C balance across the region are the outcome of climate controls on production and vegetation–fire interactions, which determine the mortality of vegetation and spatial variations in vegetation function.
Martin Thurner, Kailiang Yu, Stefano Manzoni, Anatoly Prokushkin, Melanie A. Thurner, Zhiqiang Wang, and Thomas Hickler
Biogeosciences, 22, 1475–1493, https://doi.org/10.5194/bg-22-1475-2025, https://doi.org/10.5194/bg-22-1475-2025, 2025
Short summary
Short summary
Nitrogen concentrations in tree tissues (leaves, branches, stems, and roots) are related to photosynthesis, growth, and respiration and thus to vegetation carbon uptake. Our novel database allows us to identify the controls of tree tissue nitrogen concentrations in boreal and temperate forests, such as tree age/size, species, and climate. Changes therein will affect tissue nitrogen concentrations and thus also vegetation carbon uptake.
Morgan E. Barnes, Jesse Alan Roebuck Jr., Samantha Grieger, Paul J. Aronstein, Vanessa A. Garayburu-Caruso, Kathleen Munson, Robert P. Young, Kevin D. Bladon, John D. Bailey, Emily B. Graham, Lupita Renteria, Peggy A. O'Day, Timothy D. Scheibe, and Allison N. Myers-Pigg
EGUsphere, https://doi.org/10.5194/egusphere-2025-21, https://doi.org/10.5194/egusphere-2025-21, 2025
Short summary
Short summary
Wildfires impact nutrient cycles on land and in water. We used burning experiments to understand the types of phosphorous (P), an essential nutrient, that might be released to the environment after different types of fires. We found that the amount of P moving through the environment post-fire is dependent on the type of vegetation and degree of burning which may influence when and where this material is processed or stored.
Otso Peräkylä, Erkka Rinne, Ekaterina Ezhova, Anna Lintunen, Annalea Lohila, Juho Aalto, Mika Aurela, Pasi Kolari, and Markku Kulmala
Biogeosciences, 22, 153–179, https://doi.org/10.5194/bg-22-153-2025, https://doi.org/10.5194/bg-22-153-2025, 2025
Short summary
Short summary
Forests are seen as good for climate. Yet, in areas with snow, trees break up the white snow surface and absorb more sunlight than open areas. This has a warming effect, negating some of the climate benefit of trees. We studied two site pairs in Finland, both with an open peatland and a forest. We found that the later the snow melts, the more extra energy the forest absorbs as compared to the peatland. This has implications for the future, as snow cover duration is affected by global warming.
Sarah Ann Rowan, Marc Luetscher, Thomas Laemmel, Anna Harrison, Sönke Szidat, and Franziska A. Lechleitner
EGUsphere, https://doi.org/10.5194/egusphere-2024-3775, https://doi.org/10.5194/egusphere-2024-3775, 2024
Short summary
Short summary
We explored CO2 from soil to subsurface at Milandre cave, finding very high concentrations at all depths. While forest soils produced modern CO2 year-round, cave and meadow soil CO2 influences varies with temperature controlled cave ventilation, with older CO2 input in winter from old organic matter stored underground. These findings show that CO2 fluxes in karst systems are highly dynamic, and a better understanding of them is important for accurate carbon cycle modelling.
Ruiying Zhao, Xiangzhong Luo, Yuheng Yang, Luri Nurlaila Syahid, Chi Chen, and Janice Ser Huay Lee
Biogeosciences, 21, 5393–5406, https://doi.org/10.5194/bg-21-5393-2024, https://doi.org/10.5194/bg-21-5393-2024, 2024
Short summary
Short summary
Southeast Asia has been a global hot spot of land-use change over the past 50 years. Meanwhile, it also hosts some of the most carbon-dense and diverse ecosystems in the world. Here, we explore the impact of land-use change, along with other environmental factors, on the ecosystem in Southeast Asia. We find that elevated CO2 imposed a positive impact on vegetation greenness, but the positive impact was largely offset by intensive land-use changes in the region, particularly cropland expansion.
Sabine Egerer, Stefanie Falk, Dorothea Mayer, Tobias Nützel, Wolfgang A. Obermeier, and Julia Pongratz
Biogeosciences, 21, 5005–5025, https://doi.org/10.5194/bg-21-5005-2024, https://doi.org/10.5194/bg-21-5005-2024, 2024
Short summary
Short summary
Using a state-of-the-art land model, we find that bioenergy plants can store carbon more efficiently than forests over long periods in the soil, in geological reservoirs, or by substituting fossil-fuel-based energy. Planting forests is more suitable for reaching climate targets by 2050. The carbon removal potential depends also on local environmental conditions. These considerations have important implications for climate policy, spatial planning, nature conservation, and agriculture.
Arta Bārdule, Raija Laiho, Jyrki Jauhiainen, Kaido Soosaar, Andis Lazdiņš, Kęstutis Armolaitis, Aldis Butlers, Dovilė Čiuldienė, Andreas Haberl, Ain Kull, Milda Muraškienė, Ivika Ostonen, Gristin Rohula-Okunev, Muhammad Kamil-Sardar, Thomas Schindler, Hanna Vahter, Egidijus Vigricas, and Ieva Līcīte
EGUsphere, https://doi.org/10.5194/egusphere-2024-2523, https://doi.org/10.5194/egusphere-2024-2523, 2024
Short summary
Short summary
Estimates of CO2 fluxes from drained nutrient-rich organic soils in cropland and grassland in the hemiboreal region of Europe revealed that annual net CO2 fluxes were lower than the latest (2014) IPCC emission factors provided for the whole temperate zone including hemiboreal region. Contribution of CO2 fluxes from shallow highly decomposed organic soils, former peatlands that no longer meet the IPCC criterion for organic soils, to total emissions can be high and should not be underestimated.
Elin Ristorp Aas, Inge Althuizen, Hui Tang, Sonya Geange, Eva Lieungh, Vigdis Vandvik, and Terje Koren Berntsen
Biogeosciences, 21, 3789–3817, https://doi.org/10.5194/bg-21-3789-2024, https://doi.org/10.5194/bg-21-3789-2024, 2024
Short summary
Short summary
We used a soil model to replicate two litterbag decomposition experiments to examine the implications of climate, litter quality, and soil microclimate representation. We found that macroclimate was more important than litter quality for modeled mass loss. By comparing different representations of soil temperature and moisture we found that using observed data did not improve model results. We discuss causes for this and suggest possible improvements to both the model and experimental design.
Rebecca M. Varney, Pierre Friedlingstein, Sarah E. Chadburn, Eleanor J. Burke, and Peter M. Cox
Biogeosciences, 21, 2759–2776, https://doi.org/10.5194/bg-21-2759-2024, https://doi.org/10.5194/bg-21-2759-2024, 2024
Short summary
Short summary
Soil carbon is the largest store of carbon on the land surface of Earth and is known to be particularly sensitive to climate change. Understanding this future response is vital to successfully meeting Paris Agreement targets, which rely heavily on carbon uptake by the land surface. In this study, the individual responses of soil carbon are quantified and compared amongst CMIP6 Earth system models used within the most recent IPCC report, and the role of soils in the land response is highlighted.
Juliëtte C. S. Anema, Klaas Folkert Boersma, Piet Stammes, Gerbrand Koren, William Woodgate, Philipp Köhler, Christian Frankenberg, and Jacqui Stol
Biogeosciences, 21, 2297–2311, https://doi.org/10.5194/bg-21-2297-2024, https://doi.org/10.5194/bg-21-2297-2024, 2024
Short summary
Short summary
To keep the Paris agreement goals within reach, negative emissions are necessary. They can be achieved with mitigation techniques, such as reforestation, which remove CO2 from the atmosphere. While governments have pinned their hopes on them, there is not yet a good set of tools to objectively determine whether negative emissions do what they promise. Here we show how satellite measurements of plant fluorescence are useful in detecting carbon uptake due to reforestation and vegetation regrowth.
Martin Jung, Jacob Nelson, Mirco Migliavacca, Tarek El-Madany, Dario Papale, Markus Reichstein, Sophia Walther, and Thomas Wutzler
Biogeosciences, 21, 1827–1846, https://doi.org/10.5194/bg-21-1827-2024, https://doi.org/10.5194/bg-21-1827-2024, 2024
Short summary
Short summary
We present a methodology to detect inconsistencies in perhaps the most important data source for measurements of ecosystem–atmosphere carbon, water, and energy fluxes. We expect that the derived consistency flags will be relevant for data users and will help in improving our understanding of and our ability to model ecosystem–climate interactions.
Matteo Mastropierro, Daniele Peano, and Davide Zanchettin
EGUsphere, https://doi.org/10.5194/egusphere-2024-823, https://doi.org/10.5194/egusphere-2024-823, 2024
Short summary
Short summary
We address how different ESMs represent vegetation productivity, in terms of carbon fluxes, within the Amazon basin. By statistically assessing the role of climatological and model specific factors that influence vegetation, we showed that surface energy fluxes and the implementation of Phosphorous limitation resulted to be the main drivers of model uncertainties in a future scenario. Reducing these uncertainties allows to increase the reliability of tropical land carbon and climate projections
Prajwal Khanal, Anne J. Hoek Van Dijke, Timo Schaffhauser, Wantong Li, Sinikka J. Paulus, Chunhui Zhan, and René Orth
Biogeosciences, 21, 1533–1547, https://doi.org/10.5194/bg-21-1533-2024, https://doi.org/10.5194/bg-21-1533-2024, 2024
Short summary
Short summary
Water availability is essential for vegetation functioning, but the depth of vegetation water uptake is largely unknown due to sparse ground measurements. This study correlates vegetation growth with soil moisture availability globally to infer vegetation water uptake depth using only satellite-based data. We find that the vegetation water uptake depth varies across climate regimes and vegetation types and also changes during dry months at a global scale.
Anna-Maria Virkkala, Pekka Niittynen, Julia Kemppinen, Maija E. Marushchak, Carolina Voigt, Geert Hensgens, Johanna Kerttula, Konsta Happonen, Vilna Tyystjärvi, Christina Biasi, Jenni Hultman, Janne Rinne, and Miska Luoto
Biogeosciences, 21, 335–355, https://doi.org/10.5194/bg-21-335-2024, https://doi.org/10.5194/bg-21-335-2024, 2024
Short summary
Short summary
Arctic greenhouse gas (GHG) fluxes of CO2, CH4, and N2O are important for climate feedbacks. We combined extensive in situ measurements and remote sensing data to develop machine-learning models to predict GHG fluxes at a 2 m resolution across a tundra landscape. The analysis revealed that the system was a net GHG sink and showed widespread CH4 uptake in upland vegetation types, almost surpassing the high wetland CH4 emissions at the landscape scale.
Thomas Baer, Gerhard Furrer, Stephan Zimmermann, and Patrick Schleppi
Biogeosciences, 20, 4577–4589, https://doi.org/10.5194/bg-20-4577-2023, https://doi.org/10.5194/bg-20-4577-2023, 2023
Short summary
Short summary
Nitrogen (N) deposition to forest ecosystems is a matter of concern because it affects their nutrient status and makes their soil acidic. We observed an ongoing acidification in a montane forest in central Switzerland even if the subsoil of this site contains carbonates and is thus well buffered. We experimentally added N to simulate a higher pollution, and this increased the acidification. After 25 years of study, however, we can see the first signs of recovery, also under higher N deposition.
Huiying Xu, Han Wang, Iain Colin Prentice, and Sandy P. Harrison
Biogeosciences, 20, 4511–4525, https://doi.org/10.5194/bg-20-4511-2023, https://doi.org/10.5194/bg-20-4511-2023, 2023
Short summary
Short summary
Leaf carbon (C) and nitrogen (N) are crucial elements in leaf construction and physiological processes. This study reconciled the roles of phylogeny, species identity, and climate in stoichiometric traits at individual and community levels. The variations in community-level leaf N and C : N ratio were captured by optimality-based models using climate data. Our results provide an approach to improve the representation of leaf stoichiometry in vegetation models to better couple N with C cycling.
István Dunkl, Nicole Lovenduski, Alessio Collalti, Vivek K. Arora, Tatiana Ilyina, and Victor Brovkin
Biogeosciences, 20, 3523–3538, https://doi.org/10.5194/bg-20-3523-2023, https://doi.org/10.5194/bg-20-3523-2023, 2023
Short summary
Short summary
Despite differences in the reproduction of gross primary productivity (GPP) by Earth system models (ESMs), ESMs have similar predictability of the global carbon cycle. We found that, although GPP variability originates from different regions and is driven by different climatic variables across the ESMs, the ESMs rely on the same mechanisms to predict their own GPP. This shows that the predictability of the carbon cycle is limited by our understanding of variability rather than predictability.
David T. Milodowski, T. Luke Smallman, and Mathew Williams
Biogeosciences, 20, 3301–3327, https://doi.org/10.5194/bg-20-3301-2023, https://doi.org/10.5194/bg-20-3301-2023, 2023
Short summary
Short summary
Model–data fusion (MDF) allows us to combine ecosystem models with Earth observation data. Fragmented landscapes, with a mosaic of contrasting ecosystems, pose a challenge for MDF. We develop a novel MDF framework to estimate the carbon balance of fragmented landscapes and show the importance of accounting for ecosystem heterogeneity to prevent scale-dependent bias in estimated carbon fluxes, disturbance fluxes in particular, and to improve ecological fidelity of the calibrated models.
Keri L. Bowering, Kate A. Edwards, and Susan E. Ziegler
Biogeosciences, 20, 2189–2206, https://doi.org/10.5194/bg-20-2189-2023, https://doi.org/10.5194/bg-20-2189-2023, 2023
Short summary
Short summary
Dissolved organic matter (DOM) mobilized from surface soils is a source of carbon (C) for deeper mineral horizons but also a mechanism of C loss. Composition of DOM mobilized in boreal forests varied more by season than as a result of forest harvesting. Results suggest reduced snowmelt and increased fall precipitation enhance DOM properties promoting mineral soil C stores. These findings, coupled with hydrology, can inform on soil C fate and boreal forest C balance in response to climate change.
Bharat Sharma, Jitendra Kumar, Auroop R. Ganguly, and Forrest M. Hoffman
Biogeosciences, 20, 1829–1841, https://doi.org/10.5194/bg-20-1829-2023, https://doi.org/10.5194/bg-20-1829-2023, 2023
Short summary
Short summary
Rising atmospheric carbon dioxide increases vegetation growth and causes more heatwaves and droughts. The impact of such climate extremes is detrimental to terrestrial carbon uptake capacity. We found that due to overall climate warming, about 88 % of the world's regions towards the end of 2100 will show anomalous losses in net biospheric productivity (NBP) rather than gains. More than 50 % of all negative NBP extremes were driven by the compound effect of dry, hot, and fire conditions.
Britta Greenshields, Barbara von der Lühe, Felix Schwarz, Harold J. Hughes, Aiyen Tjoa, Martyna Kotowska, Fabian Brambach, and Daniela Sauer
Biogeosciences, 20, 1259–1276, https://doi.org/10.5194/bg-20-1259-2023, https://doi.org/10.5194/bg-20-1259-2023, 2023
Short summary
Short summary
Silicon (Si) can have multiple beneficial effects on crops such as oil palms. In this study, we quantified Si concentrations in various parts of an oil palm (leaflets, rachises, fruit-bunch parts) to derive Si storage estimates for the total above-ground biomass of an oil palm and 1 ha of an oil-palm plantation. We proposed a Si balance by identifying Si return (via palm fronds) and losses (via harvest) in the system and recommend management measures that enhance Si cycling.
Luisa Schmidt, Matthias Forkel, Ruxandra-Maria Zotta, Samuel Scherrer, Wouter A. Dorigo, Alexander Kuhn-Régnier, Robin van der Schalie, and Marta Yebra
Biogeosciences, 20, 1027–1046, https://doi.org/10.5194/bg-20-1027-2023, https://doi.org/10.5194/bg-20-1027-2023, 2023
Short summary
Short summary
Vegetation attenuates natural microwave emissions from the land surface. The strength of this attenuation is quantified as the vegetation optical depth (VOD) parameter and is influenced by the vegetation mass, structure, water content, and observation wavelength. Here we model the VOD signal as a multi-variate function of several descriptive vegetation variables. The results help in understanding the effects of ecosystem properties on VOD.
Nagham Tabaja, David Amouroux, Lamis Chalak, François Fourel, Emmanuel Tessier, Ihab Jomaa, Milad El Riachy, and Ilham Bentaleb
Biogeosciences, 20, 619–633, https://doi.org/10.5194/bg-20-619-2023, https://doi.org/10.5194/bg-20-619-2023, 2023
Short summary
Short summary
This study investigates the seasonality of the mercury (Hg) concentration of olive trees. Hg concentrations of foliage, stems, soil surface, and litter were analyzed on a monthly basis in ancient olive trees growing in two groves in Lebanon. Our study draws an adequate baseline for the eastern Mediterranean and for the region with similar climatic inventories on Hg vegetation uptake in addition to being a baseline for new studies on olive trees in the Mediterranean.
Allison N. Myers-Pigg, Karl Kaiser, Ronald Benner, and Susan E. Ziegler
Biogeosciences, 20, 489–503, https://doi.org/10.5194/bg-20-489-2023, https://doi.org/10.5194/bg-20-489-2023, 2023
Short summary
Short summary
Boreal forests, historically a global sink for atmospheric CO2, store carbon in vast soil reservoirs. To predict how such stores will respond to climate warming we need to understand climate–ecosystem feedbacks. We find boreal forest soil carbon stores are maintained through enhanced nitrogen cycling with climate warming, providing direct evidence for a key feedback. Further application of the approach demonstrated here will improve our understanding of the limits of climate–ecosystem feedbacks.
Matthew P. Dannenberg, Mallory L. Barnes, William K. Smith, Miriam R. Johnston, Susan K. Meerdink, Xian Wang, Russell L. Scott, and Joel A. Biederman
Biogeosciences, 20, 383–404, https://doi.org/10.5194/bg-20-383-2023, https://doi.org/10.5194/bg-20-383-2023, 2023
Short summary
Short summary
Earth's drylands provide ecosystem services to many people and will likely be strongly affected by climate change, but it is quite challenging to monitor the productivity and water use of dryland plants with satellites. We developed and tested an approach for estimating dryland vegetation activity using machine learning to combine information from multiple satellite sensors. Our approach excelled at estimating photosynthesis and water use largely due to the inclusion of satellite soil moisture.
Mark Pickering, Alessandro Cescatti, and Gregory Duveiller
Biogeosciences, 19, 4833–4864, https://doi.org/10.5194/bg-19-4833-2022, https://doi.org/10.5194/bg-19-4833-2022, 2022
Short summary
Short summary
This study explores two of the most recent products in carbon productivity estimation, FLUXCOM gross primary productivity (GPP), calculated by upscaling local measurements of CO2 exchange, and remotely sensed sun-induced chlorophyll a fluorescence (SIF). High-resolution SIF data are valuable in demonstrating similarity in the SIF–GPP relationship between vegetation covers, provide an independent probe of the FLUXCOM GPP model and demonstrate the response of SIF to meteorological fluctuations.
Sophia Walther, Simon Besnard, Jacob Allen Nelson, Tarek Sebastian El-Madany, Mirco Migliavacca, Ulrich Weber, Nuno Carvalhais, Sofia Lorena Ermida, Christian Brümmer, Frederik Schrader, Anatoly Stanislavovich Prokushkin, Alexey Vasilevich Panov, and Martin Jung
Biogeosciences, 19, 2805–2840, https://doi.org/10.5194/bg-19-2805-2022, https://doi.org/10.5194/bg-19-2805-2022, 2022
Short summary
Short summary
Satellite observations help interpret station measurements of local carbon, water, and energy exchange between the land surface and the atmosphere and are indispensable for simulations of the same in land surface models and their evaluation. We propose generalisable and efficient approaches to systematically ensure high quality and to estimate values in data gaps. We apply them to satellite data of surface reflectance and temperature with different resolutions at the stations.
Elisabeth Mauclet, Yannick Agnan, Catherine Hirst, Arthur Monhonval, Benoît Pereira, Aubry Vandeuren, Maëlle Villani, Justin Ledman, Meghan Taylor, Briana L. Jasinski, Edward A. G. Schuur, and Sophie Opfergelt
Biogeosciences, 19, 2333–2351, https://doi.org/10.5194/bg-19-2333-2022, https://doi.org/10.5194/bg-19-2333-2022, 2022
Short summary
Short summary
Arctic warming and permafrost degradation largely affect tundra vegetation. Wetter lowlands show an increase in sedges, whereas drier uplands favor shrub expansion. Here, we demonstrate that the difference in the foliar elemental composition of typical tundra vegetation species controls the change in local foliar elemental stock and potential mineral element cycling through litter production upon a shift in tundra vegetation.
Tiexi Chen, Renjie Guo, Qingyun Yan, Xin Chen, Shengjie Zhou, Chuanzhuang Liang, Xueqiong Wei, and Han Dolman
Biogeosciences, 19, 1515–1525, https://doi.org/10.5194/bg-19-1515-2022, https://doi.org/10.5194/bg-19-1515-2022, 2022
Short summary
Short summary
Currently people are very concerned about vegetation changes and their driving factors, including natural and anthropogenic drivers. In this study, a general browning trend is found in Syria during 2001–2018, indicated by the vegetation index. We found that land management caused by social unrest is the main cause of this browning phenomenon. The mechanism initially reported here highlights the importance of land management impacts at the regional scale.
Rahayu Adzhar, Douglas I. Kelley, Ning Dong, Charles George, Mireia Torello Raventos, Elmar Veenendaal, Ted R. Feldpausch, Oliver L. Phillips, Simon L. Lewis, Bonaventure Sonké, Herman Taedoumg, Beatriz Schwantes Marimon, Tomas Domingues, Luzmila Arroyo, Gloria Djagbletey, Gustavo Saiz, and France Gerard
Biogeosciences, 19, 1377–1394, https://doi.org/10.5194/bg-19-1377-2022, https://doi.org/10.5194/bg-19-1377-2022, 2022
Short summary
Short summary
The MODIS Vegetation Continuous Fields (VCF) product underestimates tree cover compared to field data and could be underestimating tree cover significantly across the tropics. VCF is used to represent land cover or validate model performance in many land surface and global vegetation models and to train finer-scaled Earth observation products. Because underestimation in VCF may render it unsuitable for training data and bias model predictions, it should be calibrated before use in the tropics.
Lina Teckentrup, Martin G. De Kauwe, Andrew J. Pitman, Daniel S. Goll, Vanessa Haverd, Atul K. Jain, Emilie Joetzjer, Etsushi Kato, Sebastian Lienert, Danica Lombardozzi, Patrick C. McGuire, Joe R. Melton, Julia E. M. S. Nabel, Julia Pongratz, Stephen Sitch, Anthony P. Walker, and Sönke Zaehle
Biogeosciences, 18, 5639–5668, https://doi.org/10.5194/bg-18-5639-2021, https://doi.org/10.5194/bg-18-5639-2021, 2021
Short summary
Short summary
The Australian continent is included in global assessments of the carbon cycle such as the global carbon budget, yet the performance of dynamic global vegetation models (DGVMs) over Australia has rarely been evaluated. We assessed simulations by an ensemble of dynamic global vegetation models over Australia and highlighted a number of key areas that lead to model divergence on both short (inter-annual) and long (decadal) timescales.
Juhwan Lee, Raphael A. Viscarra Rossel, Mingxi Zhang, Zhongkui Luo, and Ying-Ping Wang
Biogeosciences, 18, 5185–5202, https://doi.org/10.5194/bg-18-5185-2021, https://doi.org/10.5194/bg-18-5185-2021, 2021
Short summary
Short summary
We performed Roth C simulations across Australia and assessed the response of soil carbon to changing inputs and future climate change using a consistent modelling framework. Site-specific initialisation of the C pools with measurements of the C fractions is essential for accurate simulations of soil organic C stocks and composition at a large scale. With further warming, Australian soils will become more vulnerable to C loss: natural environments > native grazing > cropping > modified grazing.
Anam M. Khan, Paul C. Stoy, James T. Douglas, Martha Anderson, George Diak, Jason A. Otkin, Christopher Hain, Elizabeth M. Rehbein, and Joel McCorkel
Biogeosciences, 18, 4117–4141, https://doi.org/10.5194/bg-18-4117-2021, https://doi.org/10.5194/bg-18-4117-2021, 2021
Short summary
Short summary
Remote sensing has played an important role in the study of land surface processes. Geostationary satellites, such as the GOES-R series, can observe the Earth every 5–15 min, providing us with more observations than widely used polar-orbiting satellites. Here, we outline current efforts utilizing geostationary observations in environmental science and look towards the future of GOES observations in the carbon cycle, ecosystem disturbance, and other areas of application in environmental science.
Lydia Stolpmann, Caroline Coch, Anne Morgenstern, Julia Boike, Michael Fritz, Ulrike Herzschuh, Kathleen Stoof-Leichsenring, Yury Dvornikov, Birgit Heim, Josefine Lenz, Amy Larsen, Katey Walter Anthony, Benjamin Jones, Karen Frey, and Guido Grosse
Biogeosciences, 18, 3917–3936, https://doi.org/10.5194/bg-18-3917-2021, https://doi.org/10.5194/bg-18-3917-2021, 2021
Short summary
Short summary
Our new database summarizes DOC concentrations of 2167 water samples from 1833 lakes in permafrost regions across the Arctic to provide insights into linkages between DOC and environment. We found increasing lake DOC concentration with decreasing permafrost extent and higher DOC concentrations in boreal permafrost sites compared to tundra sites. Our study shows that DOC concentration depends on the environmental properties of a lake, especially permafrost extent, ecoregion, and vegetation.
Gustaf Granath, Christopher D. Evans, Joachim Strengbom, Jens Fölster, Achim Grelle, Johan Strömqvist, and Stephan J. Köhler
Biogeosciences, 18, 3243–3261, https://doi.org/10.5194/bg-18-3243-2021, https://doi.org/10.5194/bg-18-3243-2021, 2021
Short summary
Short summary
We measured element losses and impacts on water quality following a wildfire in Sweden. We observed the largest carbon and nitrogen losses during the fire and a strong pulse of elements 1–3 months after the fire that showed a fast (weeks) and a slow (months) release from the catchments. Total carbon export through water did not increase post-fire. Overall, we observed a rapid recovery of the biogeochemical cycling of elements within 3 years but still an annual net release of carbon dioxide.
Lina Teckentrup, Martin G. De Kauwe, Andrew J. Pitman, and Benjamin Smith
Biogeosciences, 18, 2181–2203, https://doi.org/10.5194/bg-18-2181-2021, https://doi.org/10.5194/bg-18-2181-2021, 2021
Short summary
Short summary
The El Niño–Southern Oscillation (ENSO) describes changes in the sea surface temperature patterns of the Pacific Ocean. This influences the global weather, impacting vegetation on land. There are two types of El Niño: central Pacific (CP) and eastern Pacific (EP). In this study, we explored the long-term impacts on the carbon balance on land linked to the two El Niño types. Using a dynamic vegetation model, we simulated what would happen if only either CP or EP El Niño events had occurred.
Matthias Volk, Matthias Suter, Anne-Lena Wahl, and Seraina Bassin
Biogeosciences, 18, 2075–2090, https://doi.org/10.5194/bg-18-2075-2021, https://doi.org/10.5194/bg-18-2075-2021, 2021
Short summary
Short summary
Grassland ecosystem services like forage production and greenhouse gas storage in the soil depend on plant growth.
In an experiment in the mountains with warming treatments, we found that despite dwindling soil water content, the grassland growth increased with up to +1.3 °C warming (annual mean) compared to present temperatures. Even at +2.4 °C the growth was still larger than at the reference site.
This suggests that plant growth will increase due to global warming in the near future.
Bernice C. Hwang and Daniel B. Metcalfe
Biogeosciences, 18, 1259–1268, https://doi.org/10.5194/bg-18-1259-2021, https://doi.org/10.5194/bg-18-1259-2021, 2021
Short summary
Short summary
Despite growing recognition of herbivores as important ecosystem engineers, many major gaps remain in our understanding of how silicon and herbivory interact to shape biogeochemical processes. We highlight the need for more research particularly in natural settings as well as on the potential effects of herbivory on terrestrial silicon cycling to understand potentially critical animal–plant–soil feedbacks.
Ali Asaadi and Vivek K. Arora
Biogeosciences, 18, 669–706, https://doi.org/10.5194/bg-18-669-2021, https://doi.org/10.5194/bg-18-669-2021, 2021
Short summary
Short summary
More than a quarter of the current anthropogenic CO2 emissions are taken up by land, reducing the atmospheric CO2 growth rate. This is because of the CO2 fertilization effect which benefits 80 % of global vegetation. However, if nitrogen and phosphorus nutrients cannot keep up with increasing atmospheric CO2, the magnitude of this terrestrial ecosystem service may reduce in future. This paper implements nitrogen constraints on photosynthesis in a model to understand the mechanisms involved.
Arianna Peron, Lisa Kaser, Anne Charlott Fitzky, Martin Graus, Heidi Halbwirth, Jürgen Greiner, Georg Wohlfahrt, Boris Rewald, Hans Sandén, and Thomas Karl
Biogeosciences, 18, 535–556, https://doi.org/10.5194/bg-18-535-2021, https://doi.org/10.5194/bg-18-535-2021, 2021
Short summary
Short summary
Drought events are expected to become more frequent with climate change. Along with these events atmospheric ozone is also expected to increase. Both can stress plants. Here we investigate to what extent these factors modulate the emission of volatile organic compounds (VOCs) from oak plants. We find an antagonistic effect between drought stress and ozone, impacting the emission of different BVOCs, which is indirectly controlled by stomatal opening, allowing plants to control their water budget.
Lena Wohlgemuth, Stefan Osterwalder, Carl Joseph, Ansgar Kahmen, Günter Hoch, Christine Alewell, and Martin Jiskra
Biogeosciences, 17, 6441–6456, https://doi.org/10.5194/bg-17-6441-2020, https://doi.org/10.5194/bg-17-6441-2020, 2020
Short summary
Short summary
Mercury uptake by trees from the air represents an important but poorly quantified pathway in the global mercury cycle. We determined mercury uptake fluxes by leaves and needles at 10 European forests which were 4 times larger than mercury deposition via rainfall. The amount of mercury taken up by leaves and needles depends on their age and growing height on the tree. Scaling up our measurements to the forest area of Europe, we estimate that each year 20 t of mercury is taken up by trees.
A. Anthony Bloom, Kevin W. Bowman, Junjie Liu, Alexandra G. Konings, John R. Worden, Nicholas C. Parazoo, Victoria Meyer, John T. Reager, Helen M. Worden, Zhe Jiang, Gregory R. Quetin, T. Luke Smallman, Jean-François Exbrayat, Yi Yin, Sassan S. Saatchi, Mathew Williams, and David S. Schimel
Biogeosciences, 17, 6393–6422, https://doi.org/10.5194/bg-17-6393-2020, https://doi.org/10.5194/bg-17-6393-2020, 2020
Short summary
Short summary
We use a model of the 2001–2015 tropical land carbon cycle, with satellite measurements of land and atmospheric carbon, to disentangle lagged and concurrent effects (due to past and concurrent meteorological events, respectively) on annual land–atmosphere carbon exchanges. The variability of lagged effects explains most 2001–2015 inter-annual carbon flux variations. We conclude that concurrent and lagged effects need to be accurately resolved to better predict the world's land carbon sink.
Erqian Cui, Chenyu Bian, Yiqi Luo, Shuli Niu, Yingping Wang, and Jianyang Xia
Biogeosciences, 17, 6237–6246, https://doi.org/10.5194/bg-17-6237-2020, https://doi.org/10.5194/bg-17-6237-2020, 2020
Short summary
Short summary
Mean annual net ecosystem productivity (NEP) is related to the magnitude of the carbon sink of a specific ecosystem, while its inter-annual variation (IAVNEP) characterizes the stability of such a carbon sink. Thus, a better understanding of the co-varying NEP and IAVNEP is critical for locating the major and stable carbon sinks on land. Based on daily NEP observations from eddy-covariance sites, we found local indicators for the spatially varying NEP and IAVNEP, respectively.
Taraka Davies-Barnard, Johannes Meyerholt, Sönke Zaehle, Pierre Friedlingstein, Victor Brovkin, Yuanchao Fan, Rosie A. Fisher, Chris D. Jones, Hanna Lee, Daniele Peano, Benjamin Smith, David Wårlind, and Andy J. Wiltshire
Biogeosciences, 17, 5129–5148, https://doi.org/10.5194/bg-17-5129-2020, https://doi.org/10.5194/bg-17-5129-2020, 2020
Rui Cheng, Troy S. Magney, Debsunder Dutta, David R. Bowling, Barry A. Logan, Sean P. Burns, Peter D. Blanken, Katja Grossmann, Sophia Lopez, Andrew D. Richardson, Jochen Stutz, and Christian Frankenberg
Biogeosciences, 17, 4523–4544, https://doi.org/10.5194/bg-17-4523-2020, https://doi.org/10.5194/bg-17-4523-2020, 2020
Short summary
Short summary
We measured reflected sunlight from an evergreen canopy for a year to detect changes in pigments that play an important role in regulating the seasonality of photosynthesis. Results show a strong mechanistic link between spectral reflectance features and pigment content, which is validated using a biophysical model. Our results show spectrally where, why, and when spectral features change over the course of the season and show promise for estimating photosynthesis remotely.
Jarmo Mäkelä, Francesco Minunno, Tuula Aalto, Annikki Mäkelä, Tiina Markkanen, and Mikko Peltoniemi
Biogeosciences, 17, 2681–2700, https://doi.org/10.5194/bg-17-2681-2020, https://doi.org/10.5194/bg-17-2681-2020, 2020
Short summary
Short summary
We assess the relative magnitude of uncertainty sources on ecosystem indicators of the 21st century climate change on two boreal forest sites. In addition to RCP and climate model uncertainties, we included the overlooked model parameter uncertainty and management actions in our analysis. Management was the dominant uncertainty factor for the more verdant southern site, followed by RCP, climate and parameter uncertainties. The uncertainties were estimated with canonical correlation analysis.
Cited articles
Abalos, D., Liang, Z., Dörsch, P., and Elsgaard, L.: Trade-offs in greenhouse gas emissions across a liming-induced gradient of soil pH: Role of microbial structure and functioning, Soil Biol. Biochem., 150, 108006, https://doi.org/10.1016/j.soilbio.2020.108006, 2020.
Aini, F. K., Hergoualc'h, K., Smith, J. U., Verchot, L., and Martius, C.: How does replacing natural forests with rubber and oil palm plantations affect soil respiration and methane fluxes?, Ecosphere, 11, e03284, https://doi.org/10.1002/ecs2.3284, 2020.
Allen, D., Dalal, R. C., Rennenberg, H., and Schmidt, S.: Seasonal variation in nitrous oxide and methane emissions from subtropical estuary and coastal mangrove sediments, Australia, Plant Biol., 13, 126–133, https://doi.org/10.1111/j.1438-8677.2010.00331.x, 2011.
Annamalainathan, K., Krishnakumar, R., and Jacob, J.: Tapping-induced changes in respiratory metabolism, ATP production and reactive oxygen species scavenging in Hevea, J. Rubber Res., 4, 245–254, 2001.
Aronson, E. L. and Helliker, B. R.: Methane flux in non-wetland soils in response to nitrogen addition: a meta-analysis, Ecology, 91, 3242–3251, https://doi.org/10.1890/09-2185.1, 2010.
Banger, K., Tian, H., and Lu, C.: Do nitrogen fertilizers stimulate or inhibit methane emissions from rice fields?, Glob. Change Biol., 18, 3259–3267, https://doi.org/10.1111/j.1365-2486.2012.02762.x, 2012.
Barba, J., Poyatos, R., and Vargas, R.: Automated measurements of greenhouse gases fluxes from tree stems and soils: magnitudes, patterns and drivers, Sci. Rep., 9, 4005, https://doi.org/10.1038/s41598-019-39663-8, 2019a.
Barba, J., Bradford, M. A., Brewer, P. E., Bruhn, D., Covey, K., van Haren, J., Megonigal, J. P., Mikkelsen, T. N., Pangala, S. R., Pihlatie, M., Poulter, B., Rivas-Ubach, A., Schadt, C. W., Terazawa, K., Warner, D. L., Zhang, Z., and Vargas, R.: Methane emissions from tree stems: a new frontier in the global carbon cycle, New Phytol., 222, 18–28, https://doi.org/10.1111/nph.15582, 2019b.
Bartoń, K.: MuMIn: Multi-Model Inference, R package version 1.47.5, https://CRAN.R-project.org/package=MuMIn, (last access: 8 January 2024), 2023.
Bates, D., Mächler, M., Bolker, B., and Walker, S.: Fitting linear mixed-effects models using lme4, J. Stat. Softw., 67, 1–48, https://doi.org/10.18637/jss.v067.i01, 2015.
Beaulieu, J. J., DelSontro, T., and Downing, J. A.: Eutrophication will increase methane emissions from lakes and impoundments during the 21st century, Nat. Commun., 10, 1375, https://doi.org/10.1038/s41467-019-09100-5, 2019.
Bédard, C. and Knowles, R.: Physiology, biochemistry, and specific inhibitors of CH4, NH , and CO oxidation by methanotrophs and nitrifiers, Microbiol. Rev., 53, 68–84, 1989.
Benstead, J. and King, G. M.: The effect of soil acidification on atmospheric methane uptake by a Maine forest soil, FEMS Microbiol. Ecol., 34, 207–212, https://doi.org/10.1111/j.1574-6941.2001.tb00771.x, 2001.
Bertora, C., Cucu, M. A., Lerda, C., Peyron, M., Bardi, L., Gorra, R., Sacco, D., Celi, L., and Said-Pullicino, D.: Dissolved organic carbon cycling, methane emissions and related microbial populations in temperate rice paddies with contrasting straw and water management, Agr. Ecosyst. Environ., 265, 292–306, https://doi.org/10.1016/j.agee.2018.06.004, 2018.
Bodelier, P. L. E. and Laanbroek, H. J.: Nitrogen as a regulatory factor of methane oxidation in soils and sediments, FEMS Microbiol. Ecol., 47, 265–277, https://doi.org/10.1016/S0168-6496(03)00304-0, 2004.
Börjesson, G. and Nohrstedt, H.-Ö.: Fast recovery of atmospheric methane consumption in a Swedish forest soil after single-shot N-fertilization, Forest Ecol. Manag., 134, 83–88, https://doi.org/10.1016/S0378-1127(99)00249-2, 2000.
Borken, W., Davidson, E. A., Savage, K., Sundquist, E. T., and Steudler, P.: Effect of summer throughfall exclusion, summer drought, and winter snow cover on methane fluxes in a temperate forest soil, Soil Biol. Biochem., 38, 1388–1395, https://doi.org/10.1016/j.soilbio.2005.10.011, 2006.
Bras, N., Plain, C., and Epron, D.: Potential soil methane oxidation in naturally regenerated oak-dominated temperate deciduous forest stands responds to soil water status regardless of their age – an intact core incubation study, Ann. For. Sci., 79, 29, https://doi.org/10.1186/s13595-022-01145-9, 2022.
Bréchet, L. M., Daniel, W., Stahl, C., Burban, B., Goret, J., Salomn, R. L., and Janssens, I. A.: Simultaneous tree stem and soil greenhouse gas (CO2, CH4, N2O) flux measurements: a novel design for continuous monitoring towards improving flux estimates and temporal resolution, New Phytol., 230, 2487–2500, https://doi.org/10.1111/nph.17352, 2021.
Byun, E., Rezanezhad, F., Slowinski, S., Lam, C., Bhusal, S., Wright, S., Quinton, W. L., Webster, K. L., and Van Cappellen, P.: Effects of nitrogen and phosphorus amendments on CO2 and CH4 production in peat soils of Scotty Creek, Northwest Territories: potential considerations for wildfire and permafrost thaw impacts on peatland carbon exchanges, SOIL, 11, 309–321, https://doi.org/10.5194/soil-11-309-2025, 2025.
Caiafa, L., Barros, N. O., and Lopes, J. F. S.: Greenhouse gas emissions from ant nests: A systematic review, Ecol. Entomol., 48, 397–408, https://doi.org/10.1111/een.13238, 2023.
Castro, M. S., Peterjohn, W. T., Melillo, J. M., Steudler, P. A., Gholz, H. L., and Lewis, D.: Effects of nitrogen fertilization on the fluxes of N2O, CH4, and CO2 from soils in a Florida slash pine plantation, Can. J. Forest Res., 24, 9–13, https://doi.org/10.1139/x94-002, 1994.
Cen, X., He, N., Li, M., Xu, L., Yu, X., Cai, W., Li, X., and Butterbach-Bahl, K.: Suppression of nitrogen deposition on global forest soil CH4 uptake depends on nitrogen status, Global Biogeochem. Cy., 38, e2024GB008098, https://doi.org/10.1029/2024GB008098, 2024.
Chambon, B., Dao, X. L., Tongkaemkaew, U., and Gay, F.: What determine smallholders' fertilization practices during the mature period of rubber plantations in Thailand?, Ex. Agric., 54, 824–841, https://doi.org/10.1017/S0014479717000400, 2018.
Chan, A. S. K., Steudler, P. A., Bowden, R. D., Gulledge, J., and Cavanaugh, C. M.: Consequences of nitrogen fertilization on soil methane consumption in a productive temperate deciduous forest, Biol Fertil Soils, 41, 182–189, https://doi.org/10.1007/s00374-004-0822-7, 2005.
Chen, G., Veldkamp, E., Damris, M., Irawan, B., Tjoa, A., and Corre, M. D.: Large contribution of soil N2O emission to the global warming potential of a large-scale oil palm plantation despite changing from conventional to reduced management practices, Biogeosciences, 21, 513–529, https://doi.org/10.5194/bg-21-513-2024, 2024.
Chotiphan, R., Vaysse, L., Lacote, R., Gohet, E., Thaler, P., Sajjaphan, K., Bottier, C., Char, C., Liengprayoon, S., and Gay, F.: Can fertilization be a driver of rubber plantation intensification?, Ind. Crop. Prod., 141, 111813, https://doi.org/10.1016/j.indcrop.2019.111813, 2019.
Chowdhury, T. R. and Dick, R. P.: Ecology of aerobic methanotrophs in controlling methane fluxes from wetlands, Appl. Soil Ecol., 65, 8–22, https://doi.org/10.1016/j.apsoil.2012.12.014, 2013.
Conover, W. J. and Iman, R. L.: Rank transformations as a bridge between parametric and nonparametric statistics, Am. Stat., 35, 124–129, https://doi.org/10.1080/00031305.1981.10479327, 1981.
Cornwell, W. K., Cornelissen, J. H. C., Amatangelo, K., Dorrepaal, E., Eviner, V. T., Godoy, O., Hobbie, S. E., Hoorens, B., Kurokawa, H., Pérez-Harguindeguy, N., Quested, H. M., Santiago, L. S., Wardle, D. A., Wright, I. J., Aerts, R., Allison, S. D., van Bodegom, P., Brovkin, V., Chatain, A., Callaghan, T. V., Díaz, S., Garnier, E., Gurvich, D. E., Kazakou, E., Klein, J. A., Read, J., Reich, P. B., Soudzilovskaia, N. A., Vaieretti, M. V., and Westoby, M.: Plant species traits are the predominant control on litter decomposition rates within biomes worldwide, Ecol. Lett., 11, 1065–1071, https://doi.org/10.1111/j.1461-0248.2008.01219.x, 2008.
Covey, K. R. and Megonigal, J. P.: Methane production and emissions in trees and forests, New Phytol., 222, 35–51, https://doi.org/10.1111/nph.15624, 2019.
Epron, D.: Fertilization turns a rubber plantation from sink to methane source, KURENAI [data set], https://doi.org/10.57723/kds591970, 2025.
Epron, D. and Mochidome, T.: Methane concentration in the heartwood of living trees in a cold temperate mountain forest: variation, transport and emission, Tree Physiol., tpae122, https://doi.org/10.1093/treephys/tpae122, 2024.
Epron, D., Plain, C., Ndiaye, F.-K., Bonnaud, P., Pasquier, C., and Ranger, J.: Effects of compaction by heavy machine traffic on soil fluxes of methane and carbon dioxide in a temperate broadleaved forest, Forest Ecol. Manag., 382, 1–9, https://doi.org/10.1016/j.foreco.2016.09.037, 2016.
Epron, D., Mochidome, T., Tanabe, T., Dannoura, M., and Sakabe, A.: Variability in stem methane emissions and wood methane production of different tree species in a cold temperate mountain forest, Ecosystems, 26, 784–799, https://doi.org/10.1007/s10021-022-00795-0, 2023.
Fonseca de Souza, L., Nakamura, F. M., Kroeger, M., Obregon, D., de Moraes, M. T., Vicente, M. G., Moreira, M. Z., Pellizari, V. H., Tsai, S. M., and Nüsslein, K.: Soil pH modulates the activity of low-affinity methane oxidation in soils from the Amazon region, J. Appl. Microbiol., 136, lxae303, https://doi.org/10.1093/jambio/lxae303, 2025.
Fox, J. M., Castella, J.-C., Ziegler, A. D., and Westley, S. B.: Rubber plantations expand in mountainous Southeast Asia: what are the consequences for the environment?, Asia Pacific Issues, 114, 1–8, 2014.
Gana, C., Nouvellon, Y., Marron, N., Stape, J. L., and Epron, D.: Sampling and interpolation strategies derived from the analysis of continuous soil CO2 flux, J. Plant Nutr. Soil Sc., 181, 12–20, https://doi.org/10.1002/jpln.201600133, 2018.
Gao, J., Zhou, W., Liu, Y., Sha, L., Song, Q., Lin, Y., Yu, G., Zhang, J., Zheng, X., Fang, Y., Grace, J., Zhao, J., Xu, J., Gui, H., Sinclair, F., and Zhang, Y.: Litter-derived nitrogen reduces methane uptake in tropical rainforest soils, Sci. Total Environ., 849, 157891, https://doi.org/10.1016/j.scitotenv.2022.157891, 2022.
Garcia, J.-L., Patel, B. K. C., and Ollivier, B.: Taxonomic, Phylogenetic, and Ecological Diversity of Methanogenic Archaea, Anaerobe, 6, 205–226, https://doi.org/10.1006/anae.2000.0345, 2000.
Gauci, V., Gowing, D. J. G., Hornibrook, E. R. C., Davis, J. M., and Dise, N. B.: Woody stem methane emission in mature wetland alder trees, Atmos. Environ., 44, 2157–2160, https://doi.org/10.1016/j.atmosenv.2010.02.034, 2010.
Gauci, V., Pangala, S. R., Shenkin, A., Barba, J., Bastviken, D., Figueiredo, V., Gomez, C., Enrich-Prast, A., Sayer, E., Stauffer, T., Welch, B., Elias, D., McNamara, N., Allen, M., and Malhi, Y.: Global atmospheric methane uptake by upland tree woody surfaces, Nature, 631, 796–800, https://doi.org/10.1038/s41586-024-07592-w, 2024.
Giambelluca, T. W., Mudd, R. G., Liu, W., Ziegler, A. D., Kobayashi, N., Kumagai, T., Miyazawa, Y., Lim, T. K., Huang, M., Fox, J., Yin, S., Mak, S. V., and Kasemsap, P.: Evapotranspiration of rubber (Hevea brasiliensis) cultivated at two plantation sites in Southeast Asia, Water Resour. Res., 52, 660–679, https://doi.org/10.1002/2015WR017755, 2016.
Gohet, E., Saaban, I., Soumahoro, M., Uche, E., Soumahoro, B., and Cauchy, T.: Sustainable rubber production through good latex harvesting practices: an update on mature rubber fertilization effects on latex cell biochemistry and rubber yield potential., in: IRRDB Workshop on Latex Harvesting Technology, Vietname, Binh Duong, 19–22 November 2013, https://publications.cirad.fr/une_notice.php?dk=574668 (last access: 26 September 2024), 2013.
Guardiola-Claramonte, M., Troch, P. A., Ziegler, A. D., Giambelluca, T. W., Vogler, J. B., and Nullet, M. A.: Local hydrologic effects of introducing non-native vegetation in a tropical catchment, Ecohydrology, 1, 13–22, https://doi.org/10.1002/eco.3, 2008.
Hackstein, J. H. and Stumm, C. K.: Methane production in terrestrial arthropods., Proc. Natl. Acad. Sci. USA, 91, 5441–5445, https://doi.org/10.1073/pnas.91.12.5441, 1994.
Hanson, R. S. and Hanson, T. E.: Methanotrophic bacteria, Microbiol. Rev., 60, 439–471, 1996.
Hassler, E., Corre, M. D., Tjoa, A., Damris, M., Utami, S. R., and Veldkamp, E.: Soil fertility controls soil–atmosphere carbon dioxide and methane fluxes in a tropical landscape converted from lowland forest to rubber and oil palm plantations, Biogeosciences, 12, 5831–5852, https://doi.org/10.5194/bg-12-5831-2015, 2015.
Hobbie, S. E.: Contrasting effects of substrate and fertilizer nitrogen on the early stages of litter decomposition, Ecosystems, 8, 644–656, https://doi.org/10.1007/s10021-003-0110-7, 2005.
Hu, R., Hirano, T., Sakaguchi, K., Yamashita, S., Cui, R., Sun, L., and Liang, N.: Spatiotemporal variation in soil methane uptake in a cool-temperate immature deciduous forest, Soil Biol. Biochem., 184, 109094, https://doi.org/10.1016/j.soilbio.2023.109094, 2023.
Hütsch, B. W., Webster, C. P., and Powlson, D. S.: Methane oxidation in soil as affected by land use, soil pH and N fertilization, Soil Biol. Biochem., 26, 1613–1622, https://doi.org/10.1016/0038-0717(94)90313-1, 1994.
Huttunen, J. T., Alm, J., Liikanen, A., Juutinen, S., Larmola, T., Hammar, T., Silvola, J., and Martikainen, P. J.: Fluxes of methane, carbon dioxide and nitrous oxide in boreal lakes and potential anthropogenic effects on the aquatic greenhouse gas emissions, Chemosphere, 52, 609–621, https://doi.org/10.1016/S0045-6535(03)00243-1, 2003.
IPCC: Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press, Cambridge, United Kingdom, https://doi.org/10.1017/9781009157896, 2021.
IRSG: Rubber Statistical Bulletin, 78 (1-3), The International Rubber Study Group, Singapore, https://www.rubberstudy.org/reports (last access: 10 August 2025), 2023.
Ishizuka, S., Tsuruta, H., and Murdiyarso, D.: An intensive field study on CO2, CH4, and N2O emissions from soils at four land-use types in Sumatra, Indonesia, Global Biogeochem. Cy., 16, 22-1–22–11, https://doi.org/10.1029/2001GB001614, 2002.
Ishizuka, S., Iswandi, A., Nakajima, Y., Yonemura, S., Sudo, S., Tsuruta, H., and Murdiyarso, D.: The variation of greenhouse gas emissions from soils of various land-use/cover types in Jambi province, Indonesia, Nutr. Cycl. Agroecosys., 71, 17–32, https://doi.org/10.1007/s10705-004-0382-0, 2005.
IUSS Working Group WRB: World Reference Base for Soil Resources. International soil classification system for naming soils and creating legends for soil maps. 4th edition, International Union of Soil Sciences (IUSS), Vienna, Austria, 236 pp., ISBN 979-8-9862451-1-9, 2022.
Jackson, R. B., Abernethy, S., Canadell, J. G., Cargnello, M., Davis, S. J., Féron, S., Fuss, S., Heyer, A. J., Hong, C., Jones, C. D., Damon Matthews, H., O'Connor, F. M., Pisciotta, M., Rhoda, H. M., De Richter, R., Solomon, E. I., Wilcox, J. L., and Zickfeld, K.: Atmospheric methane removal: a research agenda, Philos. T. R. Soc. A., 379, 20200454, https://doi.org/10.1098/rsta.2020.0454, 2021.
Jassal, R. S., Black, T. A., Roy, R., and Ethier, G.: Effect of nitrogen fertilization on soil CH4 and N2O fluxes, and soil and bole respiration, Geoderma, 162, 182–186, https://doi.org/10.1016/j.geoderma.2011.02.002, 2011.
Jeffrey, L. C., Maher, D. T., Chiri, E., Leung, P. M., Nauer, P. A., Arndt, S. K., Tait, D. R., Greening, C., and Johnston, S. G.: Bark-dwelling methanotrophic bacteria decrease methane emissions from trees, Nat. Commun., 12, 2127, https://doi.org/10.1038/s41467-021-22333-7, 2021.
Kammann, C., Hepp, S., Lenhart, K., and Müller, C.: Stimulation of methane consumption by endogenous CH4 production in aerobic grassland soil, Soil Biol. Biochem., 41, 622–629, https://doi.org/10.1016/j.soilbio.2008.12.025, 2009.
Kim, S. Y., Veraart, A. J., Meima-Franke, M., and Bodelier, P. L. E.: Combined effects of carbon, nitrogen and phosphorus on CH4 production and denitrification in wetland sediments, Geoderma, 259–260, 354–361, https://doi.org/10.1016/j.geoderma.2015.03.015, 2015.
King, G. M. and Schnell, S.: Ammonium and nitrite inhibition of methane oxidation by Methylobacter albus BG8 and Methylosinus trichosporium OB3b at low methane concentrations, Appl. Environ. Microbiol., 60, 3508–3513, https://doi.org/10.1128/aem.60.10.3508-3513.1994, 1994.
King, G. M. and Schnell, S.: Effects of ammonium and non-ammonium salt additions on methane oxidation by Methylosinus trichosporium OB3b and maine forest soils, Appl. Environ. Microb., 64, 253–257, https://doi.org/10.1128/AEM.64.1.253-257.1998, 1998.
Kruse, C. W., Moldrup, P., and Iversen, N.: Modeling diffusion and reaction in soils: ii. atmospheric methane diffusion and consumption in a forest soil, Soil Sci., 161, 355–365, 1996.
Kuznetsova, A., Brockhoff, P. B., and Christensen, R. H. B.: lmerTest package: Tests in linear mixed effects models, J. Stat. Soft., 82, 1–26, https://doi.org/10.18637/jss.v082.i13, 2017.
Lacroix, E. M., Aeppli, M., Boye, K., Brodie, E., Fendorf, S., Keiluweit, M., Naughton, H. R., Noël, V., and Sihi, D.: Consider the anoxic microsite: acknowledging and appreciating spatiotemporal redox heterogeneity in soils and sediments, ACS Earth Space Chem., 7, 1592–1609, https://doi.org/10.1021/acsearthspacechem.3c00032, 2023.
Lang, R., Blagodatsky, S., Xu, J., and Cadisch, G.: Seasonal differences in soil respiration and methane uptake in rubber plantation and rainforest, Agr. Ecosyst. Environ., 240, 314–328, https://doi.org/10.1016/j.agee.2017.02.032, 2017.
Lang, R., Goldberg, S., Blagodatsky, S., Piepho, H., Harrison, R. D., Xu, J., and Cadisch, G.: Converting forests into rubber plantations weakened the soil CH4 sink in tropical uplands, Land Degrad. Dev., 30, 2311–2322, https://doi.org/10.1002/ldr.3417, 2019.
Lang, R., Goldberg, S. D., Blagodatsky, S., Piepho, H.-P., Hoyt, A. M., Harrison, R. D., Xu, J., and Cadisch, G.: Mechanism of methane uptake in profiles of tropical soils converted from forest to rubber plantations, Soil Biol. Biochem., 145, 107796, https://doi.org/10.1016/j.soilbio.2020.107796, 2020.
Le Mer, J. and Roger, P.: Production, oxidation, emission and consumption of methane by soils: A review, Eur. J. Soil Biol., 37, 25–50, https://doi.org/10.1016/S1164-5563(01)01067-6, 2001.
Lee, J., Yun, J., Yang, Y., Jung, J. Y., Lee, Y. K., Yuan, J., Ding, W., Freeman, C., and Kang, H.: Attenuation of methane oxidation by nitrogen availability in arctic tundra soils, Environ. Sci. Technol., 57, 2647–2659, https://doi.org/10.1021/acs.est.2c05228, 2023.
Liu, D. Y., Ding, W. X., Jia, Z. J., and Cai, Z. C.: Relation between methanogenic archaea and methane production potential in selected natural wetland ecosystems across China, Biogeosciences, 8, 329–338, https://doi.org/10.5194/bg-8-329-2011, 2011.
Lu, Y. and Conrad, R.: In situ stable isotope probing of methanogenic Archaea in the rice rhizosphere, Science, 309, 1088–1090, https://doi.org/10.1126/science.1113435, 2005.
Machacova, K., Borak, L., Agyei, T., Schindler, T., Soosaar, K., Mander, Ü., and Ah-Peng, C.: Trees as net sinks for methane (CH4) and nitrous oxide (N2O) in the lowland tropical rain forest on volcanic Réunion Island, New Phytol., 229, 1983–1994, https://doi.org/10.1111/nph.17002, 2021.
Martinson, G. O., Müller, A. K., Matson, A. L., Corre, M. D., and Veldkamp, E.: Nitrogen and phosphorus control soil methane uptake in tropical montane forests, J. Geophys. Res.-Biogeo., 126, e2020JG005970, https://doi.org/10.1029/2020JG005970, 2021.
Mehring, A. S., Martin, R. M., Delavaux, C. S., James, E. B., Quispe, J. J., and Yaffar, D.: Leaf-cutting ant (Atta cephalotes) nests may be hotspots of methane and carbon dioxide emissions in tropical forests, Pedobiologia, 87–88, 150754, https://doi.org/10.1016/j.pedobi.2021.150754, 2021.
Melillo, J. M., Aber, J. D., and Muratore, J. F.: Nitrogen and lignin control of hardwood leaf litter decomposition dynamics, Ecology, 63, 621–626, https://doi.org/10.2307/1936780, 1982.
Minoda, T. and Kimura, M.: Contribution of photosynthesized carbon to the methane emitted from paddy fields, Geophys. Res. Lett., 21, 2007–2010, https://doi.org/10.1029/94GL01595, 1994.
Minoda, T., Kimura, M., and Wada, E.: Photosynthates as dominant source of CH4 and CO2 in soil water and CH4 emitted to the atmosphere from paddy fields, J. Geophys. Res, 101, 21091–21097, https://doi.org/10.1029/96JD01710, 1996.
Mochizuki, Y., Koba, K., and Yoh, M.: Strong inhibitory effect of nitrate on atmospheric methane oxidation in forest soils, Soil Biol. Biochem., 50, 164–166, https://doi.org/10.1016/j.soilbio.2012.03.013, 2012.
Murase, J., Sajjaphan, K., Dechjiraratthanasiri, C., Duangngam, O., Chotiphan, R., Rattanapichai, W., Azuma, W., Shibata, M., Kasemsap, P., and Epron, D.: Methane oxidation potential of soils in a rubber plantation in Thailand affected by fertilization, SOIL, 11, 457–466, https://doi.org/10.5194/soil-11-457-2025, 2025.
Nakagawa, S. and Schielzeth, H.: A general and simple method for obtaining R2 from generalized linear mixed-effects models, Meth. Ecol. Evol., 4, 133–142, https://doi.org/10.1111/j.2041-210x.2012.00261.x, 2013.
Niu, F., Röll, A., Meijide, A., Hendrayanto, and Hölscher, D.: Rubber tree transpiration in the lowlands of Sumatra, Ecohydrology, 10, e1882, https://doi.org/10.1002/eco.1882, 2017.
O'Neill, J. G. and Wilkinson, J. F.: Oxidation of ammonia by methane-oxidizing bacteria and the effects of ammonia on methane oxidation, J. Gen. Microbiol., 100, 407–412, 1977.
Pangala, S. R., Moore, S., Hornibrook, E. R. C., and Gauci, V.: Trees are major conduits for methane egress from tropical forested wetlands, New Phytol., 197, 524–531, https://doi.org/10.1111/nph.12031, 2013.
Papen, H., Daum, M., Steinkamp, R., and Butterbach-Bahl, K.: N2O- and CH4-fluxes from soils of a N-limited and N-fertilized spruce forest ecosystem of the temperate zone, J. Appl. Bot., 75, 159–163, 2001.
Phelps, T. J. and Zeikus, J. G.: Influence of ph on terminal carbon metabolism in anoxic sediments from a mildly acidic lake, Appl. Environ. Microb., 48, 1088–1095, https://doi.org/10.1128/aem.48.6.1088-1095.1984, 1984.
Pitz, S. L., Megonigal, J. P., Chang, C.-H., and Szlavecz, K.: Methane fluxes from tree stems and soils along a habitat gradient, Biogeochemistry, 137, 307–320, https://doi.org/10.1007/s10533-017-0400-3, 2018.
Plain, C., Ndiaye, F.-K., Bonnaud, P., Ranger, J., and Epron, D.: Impact of vegetation on the methane budget of a temperate forest, New Phytol., 221, 1447–1456, https://doi.org/10.1111/nph.15452, 2019.
Purvaja, R. and Ramesh, R.: Natural and anthropogenic methane emission from coastal wetlands of south india, Environ. Manage., 27, 547–557, https://doi.org/10.1007/s002670010169, 2001.
Qiu, Q., Ding, C., Mgelwa, A. S., Feng, J., Lei, M., Gan, Z., Zhu, B., and Hu, Y.: Contrasting impacts of fertilization on topsoil and subsoil greenhouse gas fluxes in a thinned Chinese fir plantation, J. Environ. Manage., 359, 121055, https://doi.org/10.1016/j.jenvman.2024.121055, 2024.
Qu, Z., Wang, J., Almøy, T., and Bakken, L. R.: Excessive use of nitrogen in Chinese agriculture results in high N2O/(N2O+N2) product ratio of denitrification, primarily due to acidification of the soils, Glob. Change Biol., 20, 1685–1698, https://doi.org/10.1111/gcb.12461, 2014.
R Core Team: R: A language and environment for statistical computing, http://www.R-project.org/ (last access: 16 February 2024), 2023.
Rabbai, A., Barba, J., Canducci, M., Hart, K. M., MacKenzie, A. R., Kettridge, N., Curioni, G., Ullah, S., and Krause, S.: Fertilization-induced greenhouse gas emissions partially offset carbon sequestration during afforestation, Soil Biol. Biochem., 199, 109577, https://doi.org/10.1016/j.soilbio.2024.109577, 2024.
Räsänen, M., Vesala, R., Rönnholm, P., Arppe, L., Manninen, P., Jylhä, M., Rikkinen, J., Pellikka, P., and Rinne, J.: Carbon dioxide and methane fluxes from mounds of African fungus-growing termites, Biogeosciences, 20, 4029–4042, https://doi.org/10.5194/bg-20-4029-2023, 2023.
Rasmussen, R. A. and Khalil, M. A. K.: Global production of methane by termites, Nature, 301, 700–702, https://doi.org/10.1038/301700a0, 1983.
Reay, D. S. and Nedwell, D. B.: Methane oxidation in temperate soils: effects of inorganic N, Soil Biol. Biochem., 36, 2059–2065, https://doi.org/10.1016/j.soilbio.2004.06.002, 2004.
Roy, R. and Conrad, R.: effect of methanogenic precursors (acetate, hydrogen, propionate) on the suppression of methane production by nitrate in anoxic rice field soil, FEMS Microbiol. Ecol., https://doi.org/10.1111/j.1574-6941.1999.tb00560.x, 1999.
Saiyasitpanich, P., Ratisoonthorn, J., and Panmanee, N.: Thailand's Fourth National Communication (NC4), Ministry of Natural Resources and Environment, Bangkok, Thailand, https://unfccc.int/documents/624738 (last access: 27 September 2024), 2024.
Sakabe, A., Takahashi, K., Azuma, W., Itoh, M., Tateishi, M., and Kosugi, Y.: Controlling factors of seasonal variation of stem methane emissions from Alnus japonica in a riparian wetland of a temperate forest, J. Geophys. Res.-Biogeo., 126, e2021JG006326, https://doi.org/10.1029/2021JG006326, 2021.
Schnell, S. and King, G. M.: Mechanistic analysis of ammonium inhibition of atmospheric methane consumption in forest soils, Appl. Environ. Microb., 60, 3514–3521, https://doi.org/10.1128/aem.60.10.3514-3521.1994, 1994.
Sexstone, A. J., Revsbech, N. P., Parkin, T. B., and Tiedje, J. M.: Direct measurement of oxygen profiles and denitrification rates in soil aggregates, Soil Sci. Soc. Am. J., 49, 645–651, https://doi.org/10.2136/sssaj1985.03615995004900030024x, 1985.
Smith, K. A., Ball, T., Conen, F., Dobbie, K. E., Massheder, J., and Rey, A.: Exchange of greenhouse gases between soil and atmosphere: interactions of soil physical factors and biological processes, Eur. J. Soil Sci., 54, 779–791, https://doi.org/10.1046/j.1351-0754.2003.0567.x, 2003.
Smith, P., Reay, D., and Smith, J.: Agricultural methane emissions and the potential for mitigation, Philos. T. R. Soc. A., 379, 20200451, https://doi.org/10.1098/rsta.2020.0451, 2021.
Soil Survey Staff: Keys to Soil Taxonomy, 13th edition, USDA Natural Resources Conservation Service, 410 pp., https://www.nrcs.usda.gov/resources/guides-and-instructions/keys-to-soil-taxonomy (last access: 3 October 2014) 2022.
Sotomayor, D., Corredor, J. E., and Morell, J. M.: Methane flux from mangrove sediments along the southwestern coast of Puerto Rico, Estuaries, 17, 140, https://doi.org/10.2307/1352563, 1994.
Steudler, P. A., Bowden, R. D., Melillo, J. M., and Aber, J. D.: Influence of nitrogen fertilization on methane uptake in temperate forest soils, Nature, 341, 314–316, https://doi.org/10.1038/341314a0, 1989.
Tan, Z.-H., Zhang, Y.-P., Song, Q.-H., Liu, W.-J., Deng, X.-B., Tang, J.-W., Deng, Y., Zhou, W.-J., Yang, L.-Y., Yu, G.-R., Sun, X.-M., and Liang, N.-S.: Rubber plantations act as water pumps in tropical China, Geophys. Res. Lett., 38, L24406, https://doi.org/10.1029/2011GL050006, 2011.
Tang, J., Qian, H., Zhu, X., Liu, Z., Kuzyakov, Y., Zou, J., Wang, J., Xu, Q., Li, G., Liu, Z., Wang, S., Zhang, W., Zhang, J., Huang, S., Ding, Y., Van Groenigen, K. J., and Jiang, Y.: Soil pH determines nitrogen effects on methane emissions from rice paddies, Glob. Change Biol., 30, e17577, https://doi.org/10.1111/gcb.17577, 2024.
Teh, Y. A., Silver, W. L., and Conrad, M. E.: Oxygen effects on methane production and oxidation in humid tropical forest soils, Glob. Change Biol., 11, 1283–1297, https://doi.org/10.1111/j.1365-2486.2005.00983.x, 2005.
Terazawa, K., Yamada, K., Ohno, Y., Sakata, T., and Ishizuka, S.: Spatial and temporal variability in methane emissions from tree stems of Fraxinus mandshurica in a cool-temperate floodplain forest, Biogeochemistry, 123, 349–362, https://doi.org/10.1007/s10533-015-0070-y, 2015.
Veldkamp, E., Koehler, B., and Corre, M. D.: Indications of nitrogen-limited methane uptake in tropical forest soils, Biogeosciences, 10, 5367–5379, https://doi.org/10.5194/bg-10-5367-2013, 2013.
Veraart, A. J., Steenbergh, A. K., Ho, A., Kim, S. Y., and Bodelier, P. L. E.: Beyond nitrogen: The importance of phosphorus for CH4 oxidation in soils and sediments, Geoderma, 259–260, 337–346, https://doi.org/10.1016/j.geoderma.2015.03.025, 2015.
von Fischer, J. C. and Hedin, L. O.: Controls on soil methane fluxes: Tests of biophysical mechanisms using stable isotope tracers, Global Biogeochem. Cy., 21, GB2007, https://doi.org/10.1029/2006GB002687, 2007.
von Fischer, J. C., Butters, G., Duchateau, P. C., Thelwell, R. J., and Siller, R.: In situ measures of methanotroph activity in upland soils: A reaction-diffusion model and field observation of water stress, J. Geophys. Res.-Biogeo., 114, G01015, https://doi.org/10.1029/2008JG000731, 2009.
Wachinger, G., Fiedler, S., Zepp, K., Gattinger, A., Sommer, M., and Roth, K.: Variability of soil methane production on the micro-scale: spatial association with hot spots of organic material and Archaeal populations, Soil Biol. Biochem., 32, 1121–1130, https://doi.org/10.1016/S0038-0717(00)00024-9, 2000.
Wang, Y., Hollingsworth, P. M., Zhai, D., West, C. D., Green, J. M. H., Chen, H., Hurni, K., Su, Y., Warren-Thomas, E., Xu, J., and Ahrends, A.: High-resolution maps show that rubber causes substantial deforestation, Nature, 623, 340–346, https://doi.org/10.1038/s41586-023-06642-z, 2023.
Wang, Z. P., DeLaune, R. D., Patrick, W. H., and Masscheleyn, P. H.: Soil redox and pH effects on methane production in a flooded rice soil, Soil Sci. Soc. Am. J., 57, 382–385, https://doi.org/10.2136/sssaj1993.03615995005700020016x, 1993.
Wang, Z.-P. and Ineson, P.: Methane oxidation in a temperate coniferous forest soil: effects of inorganic N, Soil Biol. Biochem., 35, 427–433, https://doi.org/10.1016/S0038-0717(02)00294-8, 2003.
Wang, Z.-P., Han, S.-J., Li, H.-L., Deng, F.-D., Zheng, Y.-H., Liu, H.-F., and Han, X.-G.: Methane production explained largely by water content in the heartwood of living trees in upland forests, J. Geophys. Res.-Biogeo., 122, 2479–2489, https://doi.org/10.1002/2017JG003991, 2017.
Werner, C., Zheng, X., Tang, J., Xie, B., Liu, C., Kiese, R., and Butterbach-Bahl, K.: N2O, CH4 and CO2 emissions from seasonal tropical rainforests and a rubber plantation in southwest china, Plant Soil, 289, 335–353, https://doi.org/10.1007/s11104-006-9143-y, 2006.
Whiting, G. J. and Chanton, J. P.: Primary production control of methane emission from wetlands, Nature, 364, 794–795, https://doi.org/10.1038/364794a0, 1993.
Whittenbury, R., Phillips, K. C., and Wilkinson, J. F.: Enrichment, isolation and some properties of methane-utilizing bacteria, J. Gen. Microbiol., 61, 205–218, https://doi.org/10.1099/00221287-61-2-205, 1970.
Wobbrock, J. O., Findlater, L., Gergle, D., and Higgins, J. J.: The aligned rank transform for nonparametric factorial analyses using only anova procedures, in: Proceedings of the SIGCHI Conference on Human Factors in Computing Systems, CHI '11: CHI Conference on Human Factors in Computing Systems, Vancouver BC Canada, 7–12 May 2011, 143–146, https://doi.org/10.1145/1978942.1978963, 2011.
Yao, X., Wang, J., and Hu, B.: How methanotrophs respond to pH: A review of ecophysiology, Front. Microbiol., 13, 1034164, https://doi.org/10.3389/fmicb.2022.1034164, 2023.
Ye, R., Jin, Q., Bohannan, B., Keller, J. K., McAllister, S. A., and Bridgham, S. D.: pH controls over anaerobic carbon mineralization, the efficiency of methane production, and methanogenic pathways in peatlands across an ombrotrophic–minerotrophic gradient, Soil Biol. Biochem., 54, 36–47, https://doi.org/10.1016/j.soilbio.2012.05.015, 2012.
Zhang, L., Yuan, F., Bai, J., Duan, H., Gu, X., Hou, L., Huang, Y., Yang, M., He, J., Zhang, Z., Yu, L., Song, C., Lipson, D. A., Zona, D., Oechel, W., Janssens, I. A., and Xu, X.: Phosphorus alleviation of nitrogen-suppressed methane sink in global grasslands, Ecol. Lett., 23, 821–830, https://doi.org/10.1111/ele.13480, 2020.
Zhang, T., Zhu, W., Mo, J., Liu, L., and Dong, S.: Increased phosphorus availability mitigates the inhibition of nitrogen deposition on CH4 uptake in an old-growth tropical forest, southern China, Biogeosciences, 8, 2805–2813, https://doi.org/10.5194/bg-8-2805-2011, 2011.
Zhang, W., Mo, J., Zhou, G., Gundersen, P., Fang, Y., Lu, X., Zhang, T., and Dong, S.: Methane uptake responses to nitrogen deposition in three tropical forests in southern China, J. Geophys. Res., 113, D11116, https://doi.org/10.1029/2007JD009195, 2008.
Zheng, M., Zhang, T., Liu, L., Zhang, W., Lu, X., and Mo, J.: Effects of nitrogen and phosphorus additions on soil methane uptake in disturbed forests: N and P regulate CH4 uptake in forests, J. Geophys. Res.-Biogeo., 121, 3089–3100, https://doi.org/10.1002/2016JG003476, 2016.
Zhou, W., Zhu, J., Ji, H., Grace, J., Sha, L., Song, Q., Liu, Y., Bai, X., Lin, Y., Gao, J., Fei, X., Zhou, R., Tang, J., Deng, X., Yu, G., Zhang, J., Zheng, X., Zhao, J., and Zhang, Y.: Drivers of difference in CO2 and CH4 emissions between rubber plantation and tropical rainforest soils, Agr. Forest Meteorol., 304–305, 108391, https://doi.org/10.1016/j.agrformet.2021.108391, 2021.
Zhu, F., Yoh, M., Gilliam, F. S., Lu, X., and Mo, J.: Nutrient limitation in three lowland tropical forests in Southern China receiving high nitrogen deposition: insights from fine root responses to nutrient additions, PLoS ONE, 8, e82661, https://doi.org/10.1371/journal.pone.0082661, 2013.
Short summary
The rapid expansion of rubber cultivation constitutes a significant land-use change in Southeast Asia. Despite fertilization being a common practice in rubber plantations, its impact on soil methane (CH4) dynamics has remained poorly understood. Our study demonstrates that fertilization not only reduces soil CH4 consumption but also increases CH4 production, transforming rubber plantations from a net CH4 sink to a source. Implementing rational fertilization could enhance atmospheric CH4 removal.
The rapid expansion of rubber cultivation constitutes a significant land-use change in Southeast...
Altmetrics
Final-revised paper
Preprint