Articles | Volume 10, issue 2
https://doi.org/10.5194/soil-10-813-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/soil-10-813-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Original research article
| 
19 Nov 2024
Original research article |
| 19 Nov 2024
| 19 Nov 2024
Soil organic matter interactions along the elevation gradient of the James Ross Island (Antarctica)
Vítězslav Vlček
CORRESPONDING AUTHOR
Department of Agrochemistry, Soil Science, Microbiology and Plant Nutrition, Faculty of AgriSciences, Mendel University in Brno, Zemědělská 1, 613 00 Brno, Czech Republic
David Juřička
Department of Geology and Soil Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemědělská 3, 613 00 Brno, Czech Republic
Martin Valtera
Department of Forest Botany, Dendrology and Geobiocoenology, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemědělská 3, 613 00 Brno, Czech Republic
Helena Dvořáčková
Department of Agrochemistry, Soil Science, Microbiology and Plant Nutrition, Faculty of AgriSciences, Mendel University in Brno, Zemědělská 1, 613 00 Brno, Czech Republic
Vojtěch Štulc
Department of Agrochemistry, Soil Science, Microbiology and Plant Nutrition, Faculty of AgriSciences, Mendel University in Brno, Zemědělská 1, 613 00 Brno, Czech Republic
Michaela Bednaříková
Department of Experimental Biology, Faculty of Science, Masaryk University, Kamenice 5, 625 00 Brno, Czech Republic
Jana Šimečková
Department of Agrochemistry, Soil Science, Microbiology and Plant Nutrition, Faculty of AgriSciences, Mendel University in Brno, Zemědělská 1, 613 00 Brno, Czech Republic
Peter Váczi
Department of Experimental Biology, Faculty of Science, Masaryk University, Kamenice 5, 625 00 Brno, Czech Republic
Miroslav Pohanka
Faculty of Military Health Sciences, University of Defence, Třebešská 1575, 500 01 Hradec Králové, Czech Republic
Pavel Kapler
Department of Geography, Faculty of Science, Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic
Miloš Barták
Department of Experimental Biology, Faculty of Science, Masaryk University, Kamenice 5, 625 00 Brno, Czech Republic
Vojtěch Enev
Institute of Physical and Applied Chemistry, Faculty of Chemistry, Brno University of Technology, Purkynova 118, 612 00 Brno, Czech Republic
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Antonín Kintl, Vítězslav Vlček, Martin Brtnický, Jan Nedělník, and Jakub Elbl
SOIL, 8, 349–372, https://doi.org/10.5194/soil-8-349-2022, https://doi.org/10.5194/soil-8-349-2022, 2022
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We have started to address this issue because the application of wetting agents is very widespread within the European Union and is often considered desirable because it increases the effectiveness of pesticides. While pesticides are thoroughly tested for their impact on the environment as a whole, testing for the effects of wetting agents is minimal. Today, there is no research on their impact on the soil environment.
Antonín Kintl, Vítězslav Vlček, Martin Brtnický, Jan Nedělník, and Jakub Elbl
SOIL, 8, 349–372, https://doi.org/10.5194/soil-8-349-2022, https://doi.org/10.5194/soil-8-349-2022, 2022
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We have started to address this issue because the application of wetting agents is very widespread within the European Union and is often considered desirable because it increases the effectiveness of pesticides. While pesticides are thoroughly tested for their impact on the environment as a whole, testing for the effects of wetting agents is minimal. Today, there is no research on their impact on the soil environment.
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Amicie A. Delahaie, Lauric Cécillon, Marija Stojanova, Samuel Abiven, Pierre Arbelet, Dominique Arrouays, François Baudin, Antonio Bispo, Line Boulonne, Claire Chenu, Jussi Heinonsalo, Claudy Jolivet, Kristiina Karhu, Manuel Martin, Lorenza Pacini, Christopher Poeplau, Céline Ratié, Pierre Roudier, Nicolas P. A. Saby, Florence Savignac, and Pierre Barré
SOIL, 10, 795–812, https://doi.org/10.5194/soil-10-795-2024, https://doi.org/10.5194/soil-10-795-2024, 2024
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This paper compares the soil organic carbon fractions obtained from a new thermal fractionation scheme and a well-known physical fractionation scheme on an unprecedented dataset of French topsoil samples. For each fraction, we use a machine learning model to determine its environmental drivers (pedology, climate, and land cover). Our results suggest that these two fractionation schemes provide different fractions, which means they provide complementary information.
Lingfei Wang, Gab Abramowitz, Ying-Ping Wang, Andy Pitman, and Raphael A. Viscarra Rossel
SOIL, 10, 619–636, https://doi.org/10.5194/soil-10-619-2024, https://doi.org/10.5194/soil-10-619-2024, 2024
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Effective management of soil organic carbon (SOC) requires accurate knowledge of its distribution and factors influencing its dynamics. We identify the importance of variables in spatial SOC variation and estimate SOC stocks in Australia using various models. We find there are significant disparities in SOC estimates when different models are used, highlighting the need for a critical re-evaluation of land management strategies that rely on the SOC distribution derived from a single approach.
Tchodjowiè P. I. Kpemoua, Pierre Barré, Sabine Houot, François Baudin, Cédric Plessis, and Claire Chenu
SOIL, 10, 533–549, https://doi.org/10.5194/soil-10-533-2024, https://doi.org/10.5194/soil-10-533-2024, 2024
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Several agroecological management options foster soil organic C stock accrual. What is behind the persistence of this "additional" C? We used three different methodological approaches and >20 years of field experiments under temperate conditions to find out. We found that the additional C is less stable at the pluri-decadal scale than the baseline C. This highlights the need to maintain agroecological practices to keep these carbon stocks at a high level over time.
Jörg Schnecker, Theresa Böckle, Julia Horak, Victoria Martin, Taru Sandén, and Heide Spiegel
SOIL, 10, 521–531, https://doi.org/10.5194/soil-10-521-2024, https://doi.org/10.5194/soil-10-521-2024, 2024
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Microbial processes are driving the formation and decomposition of soil organic matter. In contrast to respiration and growth, microbial death rates currently lack distinct methods to be determined. Here, we propose a new approach to measure microbial death rates. This new approach to determine microbial death rates as well as dynamics of intracellular and extracellular DNA separately will help to improve concepts and models of C dynamics in soils in the future.
Ruizhe Wang and Xia Hu
EGUsphere, https://doi.org/10.5194/egusphere-2024-1833, https://doi.org/10.5194/egusphere-2024-1833, 2024
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In this paper, we studied the impact of seasonal freeze-thaw processes on pore structure and SOC fraction contents of aggregates in typical alpine ecosystems in the Qinghai Lake basin. We sampled soils in four freeze-thaw periods and pore structure was quantified using X-ray compyuted tomography. Also, we revealed that the freezing and thawing corresponded to the protection and loss for SOC of aggregates, respectively, through regulating pore structure.
Laura Hondroudakis, Peter M. Kopittke, Ram C. Dalal, Meghan Barnard, and Zhe H. Weng
SOIL, 10, 451–465, https://doi.org/10.5194/soil-10-451-2024, https://doi.org/10.5194/soil-10-451-2024, 2024
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Land use change to cropping is known to greatly reduced organic carbon and nitrogen concentrations, but much remains unknown about the mechanisms influencing their persistence in soil. In a soil from a subtropical Australian cropping system, we demonstrate that organic carbon is protected by mineral associations but not particulate forms. Importantly, we also show that reversion from cropping to pasture or plantation can partially restore this organic carbon.
Qintana Si, Kangli Chen, Bin Wei, Yaowen Zhang, Xun Sun, and Junyi Liang
SOIL, 10, 441–450, https://doi.org/10.5194/soil-10-441-2024, https://doi.org/10.5194/soil-10-441-2024, 2024
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Our soil incubation experiment demonstrates that dissolved labile carbon substrate is a significant contributor to the soil particulate organic carbon pool. Dissolved carbon flow to particulate organic carbon is regulated by microbial biomass carbon and soil texture. The soil carbon model underestimates soil carbon sequestration when carbon flow from dissolved substrates to particulate organic carbon through microbial processes is not considered.
Yuyang Yan, Xinran Zhang, Chenyang Xu, Junjun Liu, Feinan Hu, and Zengchao Geng
EGUsphere, https://doi.org/10.5194/egusphere-2024-1266, https://doi.org/10.5194/egusphere-2024-1266, 2024
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With decreasing colloidal particle diameter, the total carbon content, organic carbon, organic functional groups content and illite content all increased. The critical coagulation concentrations (CCCs) values of soil colloids followed the descending order of d < 100 nm, d < 1 μm, d < 2 μm, thus soil nanoparticles exhibited strongest suspension stability.
Clémentine Chirol, Geoffroy Séré, Paul-Olivier Redon, Claire Chenu, and Delphine Derrien
EGUsphere, https://doi.org/10.5194/egusphere-2024-1284, https://doi.org/10.5194/egusphere-2024-1284, 2024
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W. Marijn van der Meij, Svenja Riedesel, and Tony Reimann
EGUsphere, https://doi.org/10.5194/egusphere-2024-1466, https://doi.org/10.5194/egusphere-2024-1466, 2024
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Soil mixing (bioturbation) plays a key role in soil functions, but the underlying processes are poorly understood and difficult to quantify. In this study, we use luminescence, a light-sensitive soil mineral property, and numerical models to better understand different types of bioturbation. We provide a conceptual model that helps to determine what type of bioturbation processes occur in a soil and a numerical model that can derive quantitative process rates from luminescence measurements.
Sam J. Leuthold, Jocelyn M. Lavallee, Bruno Basso, William F. Brinton, and M. Francesca Cotrufo
SOIL, 10, 307–319, https://doi.org/10.5194/soil-10-307-2024, https://doi.org/10.5194/soil-10-307-2024, 2024
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We examined physical soil organic matter fractions to understand their relationship to temporal variability in crop yield at field scale. We found that interactions between crop productivity, topography, and climate led to variability in soil organic matter stocks among different yield stability zones. Our results imply that linkages between soil organic matter and yield stability may be scale-dependent and that particulate organic matter may be an indicator of unstable areas within croplands.
Johan Six, Sebastian Doetterl, Moritz Laub, Claude R. Müller, and Marijn Van de Broek
SOIL, 10, 275–279, https://doi.org/10.5194/soil-10-275-2024, https://doi.org/10.5194/soil-10-275-2024, 2024
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Soil C saturation has been tested in several recent studies and led to a debate about its existence. We argue that, to test C saturation, one should pay attention to six fundamental principles: the right measures, the right units, the right dispersive energy and application, the right soil type, the right clay type, and the right saturation level. Once we take care of those six rights across studies, we find support for a maximum of C stabilized by minerals and thus soil C saturation.
Yuri Suzuki, Syuntaro Hiradate, Jun Koarashi, Mariko Atarashi-Andoh, Takumi Yomogida, Yuki Kanda, and Hirohiko Nagano
EGUsphere, https://doi.org/10.5194/egusphere-2024-419, https://doi.org/10.5194/egusphere-2024-419, 2024
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We incubated 10 Japanese soils to study CO2 release under drying-rewetting cycles (DWCs). CO2 release was increased by DWCs among all soils, showing soil-by-soil variations in CO2 release increase magnitude. Organo-Al complex was the primary predictor for the increase magnitude, suggesting vulnerability of carbon protection by reactive minerals against DWCs. Microbial biomass decrease by DWCs was also suggested, although its linkage with the CO2 release increase is unclear yet.
Laura Kuusemets, Ülo Mander, Jordi Escuer-Gatius, Alar Astover, Karin Kauer, Kaido Soosaar, and Mikk Espenberg
EGUsphere, https://doi.org/10.5194/egusphere-2024-593, https://doi.org/10.5194/egusphere-2024-593, 2024
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We investigated relationships between mineral nitrogen (N) fertilisation rates and additional manure amendment with different crop types through the analysis of soil environmental characteristics and microbiome, soil N2O and N2 emissions, and biomass production. Results show that wheat was growing well at a fertilisation rate of 80 kg N ha−1, and newly introduced sorghum showed good potential for cultivation in temperate climate.
Norman Gentsch, Florin Laura Riechers, Jens Boy, Dörte Schweneker, Ulf Feuerstein, Diana Heuermann, and Georg Guggenberger
SOIL, 10, 139–150, https://doi.org/10.5194/soil-10-139-2024, https://doi.org/10.5194/soil-10-139-2024, 2024
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Cover crops have substantial impacts on soil properties, but so far it is not clear how long a legacy effect of cover cropping will remain in the soil. We found that cover crops attenuate negative effects on soil structure that come from soil cultivation. The combination of plants with different litter qualities and rhizodeposits in biodiverse cover crop mixtures can improve the positive effects of cover cropping on soil structure amelioration.
Che-Jen Hsiao, Pedro A. M. Leite, Ayumi Hyodo, and Thomas W. Boutton
SOIL, 10, 93–108, https://doi.org/10.5194/soil-10-93-2024, https://doi.org/10.5194/soil-10-93-2024, 2024
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Tree cover has increased in grasslands worldwide, with juniper and oak trees expanding in the southern Great Plains, USA. Here, we examine how these changes interact with geology to affect soil C, N, and P storage. Soil concentrations of these elements were significantly higher under trees than grasslands but increased more under trees growing on Edwards soils. Our results suggest that geology and vegetation change should be considered when predicting soil storage in dryland ecosystems globally.
David S. McLagan, Carina Esser, Lorenz Schwab, Jan G. Wiederhold, Jan-Helge Richard, and Harald Biester
SOIL, 10, 77–92, https://doi.org/10.5194/soil-10-77-2024, https://doi.org/10.5194/soil-10-77-2024, 2024
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Sorption of mercury in soils, aquifer materials, and sediments is primarily linked to organic matter. Using column experiments, mercury concentration, speciation, and stable isotope analyses, we show that large quantities of mercury in soil water and groundwater can be sorbed to inorganic minerals; sorption to the solid phase favours lighter isotopes. Data provide important insights on the transport and fate of mercury in soil–groundwater systems and particularly in low-organic-matter systems.
Orly Mendoza, Stefaan De Neve, Heleen Deroo, Haichao Li, Astrid Françoys, and Steven Sleutel
EGUsphere, https://doi.org/10.5194/egusphere-2024-107, https://doi.org/10.5194/egusphere-2024-107, 2024
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Farmers frequently apply fresh organic matter such as crop residues to soil to boost its carbon content. Yet, one burning question remains: Does the quantity of applied organic matter affect its decomposition and that of native soil organic matter? Our experiments indicate that smaller application doses might deplete soil organic matter more rapidly. In contrast, applying intermediate or high doses might be a promising strategy for maintaining it.
Marketa Stepanova, Martin Novak, Bohuslava Cejkova, Ivana Jackova, Frantisek Buzek, Frantisek Veselovsky, Jan Curik, Eva Prechova, Arnost Komarek, and Leona Bohdalkova
SOIL, 9, 623–640, https://doi.org/10.5194/soil-9-623-2023, https://doi.org/10.5194/soil-9-623-2023, 2023
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Biological N2 fixation helps to sustain carbon accumulation in peatlands and to remove CO2 from the atmosphere. Changes in N2 fixation may affect the dynamics of global change. Increasing inputs of reactive N from air pollution should lead to downregulation of N2 fixation. Data from three N-polluted peat bogs show an interplay of N2-fixation rates with 10 potential drivers of this process. N2 fixation was measurable only at one site characterized by high phosphorus and low sulfate availability.
Tatjana C. Speckert, Jeannine Suremann, Konstantin Gavazov, Maria J. Santos, Frank Hagedorn, and Guido L. B. Wiesenberg
SOIL, 9, 609–621, https://doi.org/10.5194/soil-9-609-2023, https://doi.org/10.5194/soil-9-609-2023, 2023
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Soil organic carbon (SOC) is key player in the global carbon cycle. Afforestation on pastures potentially alters organic matter input and SOC sequestration. We investigated the effects of a Picea abies L. afforestation sequence (0 to 130 years) on a former subalpine pasture on SOC stocks and dynamics. We found no difference in the SOC stock after 130 years of afforestation and thus no additional SOC sequestration. SOC composition was altered due to a modified SOC input following afforestation.
Lauren M. Gillespie, Nathalie Y. Triches, Diego Abalos, Peter Finke, Sophie Zechmeister-Boltenstern, Stephan Glatzel, and Eugenio Díaz-Pinés
SOIL, 9, 517–531, https://doi.org/10.5194/soil-9-517-2023, https://doi.org/10.5194/soil-9-517-2023, 2023
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Forest soil is potentially an important source or sink of greenhouse gases (CO2, N2O, and CH4), but this is affected by soil conditions. We studied how land inclination and soil/litter properties influence the flux of these gases. CO2 and N2O were more affected by inclination than CH4; all were affected by soil/litter properties. This study underlines the importance of inclination and soil/litter properties in predicting greenhouse gas fluxes from forest soil and potential source–sink balance.
Sastrika Anindita, Peter Finke, and Steven Sleutel
SOIL, 9, 443–459, https://doi.org/10.5194/soil-9-443-2023, https://doi.org/10.5194/soil-9-443-2023, 2023
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This study investigated how land use, through its impact on soil geochemistry, might indirectly control soil organic carbon (SOC) content in tropical volcanic soils in Indonesia. We analyzed SOC fractions, substrate-specific mineralization, and net priming of SOC. Our results indicated that the enhanced formation of aluminum (hydr)oxides promoted aggregation and physical occlusion of OC, which is consistent with the lesser degradability of SOC in agricultural soils.
Amicie A. Delahaie, Pierre Barré, François Baudin, Dominique Arrouays, Antonio Bispo, Line Boulonne, Claire Chenu, Claudy Jolivet, Manuel P. Martin, Céline Ratié, Nicolas P. A. Saby, Florence Savignac, and Lauric Cécillon
SOIL, 9, 209–229, https://doi.org/10.5194/soil-9-209-2023, https://doi.org/10.5194/soil-9-209-2023, 2023
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We characterized organic matter in French soils by analysing samples from the French RMQS network using Rock-Eval thermal analysis. We found that thermal analysis is appropriate to characterize large set of samples (ca. 2000) and provides interpretation references for Rock-Eval parameter values. This shows that organic matter in managed soils is on average more oxidized and more thermally stable and that some Rock-Eval parameters are good proxies for organic matter biogeochemical stability.
Britta Greenshields, Barbara von der Lühe, Harold J. Hughes, Christian Stiegler, Suria Tarigan, Aiyen Tjoa, and Daniela Sauer
SOIL, 9, 169–188, https://doi.org/10.5194/soil-9-169-2023, https://doi.org/10.5194/soil-9-169-2023, 2023
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Silicon (Si) research could provide complementary measures in sustainably cultivating oil-palm monocultures. Our study shows that current oil-palm management practices and topsoil erosion on oil-palm plantations in Indonesia have caused a spatial distribution of essential Si pools in soil. A lack of well-balanced Si levels in topsoil could negatively affect crop yield and soil fertility for future replanting at the same plantation site. Potential measures are suggested to maintain Si cycling.
Kenji Fujisaki, Tiphaine Chevallier, Antonio Bispo, Jean-Baptiste Laurent, François Thevenin, Lydie Chapuis-Lardy, Rémi Cardinael, Christine Le Bas, Vincent Freycon, Fabrice Bénédet, Vincent Blanfort, Michel Brossard, Marie Tella, and Julien Demenois
SOIL, 9, 89–100, https://doi.org/10.5194/soil-9-89-2023, https://doi.org/10.5194/soil-9-89-2023, 2023
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This paper presents a first comprehensive thesaurus for management practices driving soil organic carbon (SOC) storage. So far, a comprehensive thesaurus of management practices in agriculture and forestry has been lacking. It will help to merge datasets, a promising way to evaluate the impacts of management practices in agriculture and forestry on SOC. Identifying the drivers of SOC stock changes is of utmost importance to contribute to global challenges (climate change, food security).
Oliver van Straaten, Larissa Kulp, Guntars O. Martinson, Dan Paul Zederer, and Ulrike Talkner
SOIL, 9, 39–54, https://doi.org/10.5194/soil-9-39-2023, https://doi.org/10.5194/soil-9-39-2023, 2023
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Across northern Europe, millions of hectares of forest have been limed to counteract soil acidification and restore forest ecosystems. In this study, we investigated how restorative liming affects the forest soil organic carbon (SOC) stocks and correspondingly ecosystem greenhouse gas fluxes. We found that the magnitude and direction of SOC stock changes hinge on the inherent site characteristics, namely, forest type, soil texture, initial soil pH, and initial soil SOC stocks (before liming).
Junxiao Pan, Jinsong Wang, Dashuan Tian, Ruiyang Zhang, Yang Li, Lei Song, Jiaming Yang, Chunxue Wei, and Shuli Niu
SOIL, 8, 687–698, https://doi.org/10.5194/soil-8-687-2022, https://doi.org/10.5194/soil-8-687-2022, 2022
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We found that climatic, edaphic, plant and microbial variables jointly affect soil inorganic carbon (SIC) stock in Tibetan grasslands, and biotic factors have a larger contribution than abiotic factors to the variation in SIC stock. The effects of microbial and plant variables on SIC stock weakened with soil depth, while the effects of edaphic variables strengthened. The contrasting responses and drivers of SIC stock highlight differential mechanisms underlying SIC preservation with soil depth.
Yifeng Zhang, Sen Dou, Batande Sinovuyo Ndzelu, Rui Ma, Dandan Zhang, Xiaowei Zhang, Shufen Ye, and Hongrui Wang
SOIL, 8, 605–619, https://doi.org/10.5194/soil-8-605-2022, https://doi.org/10.5194/soil-8-605-2022, 2022
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How to effectively convert corn straw into humic substances and return them to the soil in a relatively stable form is a concerning topic. Through a 360 d field experiment under equal carbon (C) mass, we found that return of the fermented corn straw treated with Trichoderma reesei to the field is more valuable and conducive to increasing easily oxidizable organic C, humus C content, and carbon pool management index than the direct application of corn straw.
Ling Mao, Shaoming Ye, and Shengqiang Wang
SOIL, 8, 487–505, https://doi.org/10.5194/soil-8-487-2022, https://doi.org/10.5194/soil-8-487-2022, 2022
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Soil ecological stoichiometry offers a tool to explore the distribution, cycling, limitation, and balance of chemical elements. This study improved the understanding of soil organic carbon and nutrient dynamics in tea plantation ecosystems and also provided supplementary information for soil ecological stoichiometry in global terrestrial ecosystems.
Steffen Schlüter, Tim Roussety, Lena Rohe, Vusal Guliyev, Evgenia Blagodatskaya, and Thomas Reitz
SOIL, 8, 253–267, https://doi.org/10.5194/soil-8-253-2022, https://doi.org/10.5194/soil-8-253-2022, 2022
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We combined microstructure analysis via X-ray CT with carbon mineralization analysis via respirometry of intact soil cores from different land uses. We found that the amount of particulate organic matter (POM) exerted a dominant control on carbon mineralization in well-aerated topsoils, whereas soil moisture and macroporosity did not play role. This is because carbon mineralization mainly occurs in microbial hotspots around degrading POM, where it is decoupled from conditions of the bulk soil.
Roberta Pulcher, Enrico Balugani, Maurizio Ventura, Nicolas Greggio, and Diego Marazza
SOIL, 8, 199–211, https://doi.org/10.5194/soil-8-199-2022, https://doi.org/10.5194/soil-8-199-2022, 2022
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Biochar, a solid product from the thermal conversion of biomass, can be used as a climate change mitigation strategy, since it can sequester carbon from the atmosphere and store it in the soil. The aim of this study is to assess the potential of biochar as a mitigation strategy in the long term, by modelling the results obtained from an 8-year field experiment. As far as we know, this is the first time that a model for biochar degradation has been validated with long-term field data.
Daniel Rath, Nathaniel Bogie, Leonardo Deiss, Sanjai J. Parikh, Daoyuan Wang, Samantha Ying, Nicole Tautges, Asmeret Asefaw Berhe, Teamrat A. Ghezzehei, and Kate M. Scow
SOIL, 8, 59–83, https://doi.org/10.5194/soil-8-59-2022, https://doi.org/10.5194/soil-8-59-2022, 2022
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Storing C in subsoils can help mitigate climate change, but this requires a better understanding of subsoil C dynamics. We investigated changes in subsoil C storage under a combination of compost, cover crops (WCC), and mineral fertilizer and found that systems with compost + WCC had ~19 Mg/ha more C after 25 years. This increase was attributed to increased transport of soluble C and nutrients via WCC root pores and demonstrates the potential for subsoil C storage in tilled agricultural systems.
Zuzana Frkova, Chiara Pistocchi, Yuliya Vystavna, Katerina Capkova, Jiri Dolezal, and Federica Tamburini
SOIL, 8, 1–15, https://doi.org/10.5194/soil-8-1-2022, https://doi.org/10.5194/soil-8-1-2022, 2022
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Phosphorus (P) is essential for life. We studied microbial processes driving the P cycle in soils developed on the same rock but with different ages (0–100 years) in a cold desert. Compared to previous studies under cold climate, we found much slower weathering of P-containing minerals of soil development, likely due to aridity. However, microbes dominate short-term dynamics and progressively redistribute P from the rock into more available forms, making it available for plants at later stages.
Carrie L. Thomas, Boris Jansen, E. Emiel van Loon, and Guido L. B. Wiesenberg
SOIL, 7, 785–809, https://doi.org/10.5194/soil-7-785-2021, https://doi.org/10.5194/soil-7-785-2021, 2021
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Plant organs, such as leaves, contain a variety of chemicals that are eventually deposited into soil and can be useful for studying organic carbon cycling. We performed a systematic review of available data of one type of plant-derived chemical, n-alkanes, to determine patterns of degradation or preservation from the source plant to the soil. We found that while there was degradation in the amount of n-alkanes from plant to soil, some aspects of the chemical signature were preserved.
Benjamin Bukombe, Peter Fiener, Alison M. Hoyt, Laurent K. Kidinda, and Sebastian Doetterl
SOIL, 7, 639–659, https://doi.org/10.5194/soil-7-639-2021, https://doi.org/10.5194/soil-7-639-2021, 2021
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Through a laboratory incubation experiment, we investigated the spatial patterns of specific maximum heterotrophic respiration in tropical African mountain forest soils developed from contrasting parent material along slope gradients. We found distinct differences in soil respiration between soil depths and geochemical regions related to soil fertility and the chemistry of the soil solution. The topographic origin of our samples was not a major determinant of the observed rates of respiration.
Patricia Merdy, Yves Lucas, Bruno Coulomb, Adolpho J. Melfi, and Célia R. Montes
SOIL, 7, 585–594, https://doi.org/10.5194/soil-7-585-2021, https://doi.org/10.5194/soil-7-585-2021, 2021
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Transfer of organic C from topsoil to deeper horizons and the water table is little documented, especially in equatorial environments, despite high primary productivity in the evergreen forest. Using column experiments with podzol soil and a percolating solution sampled in an Amazonian podzol area, we show how the C-rich Bh horizon plays a role in natural organic matter transfer and Si, Fe and Al mobility after a kaolinitic layer transition, thus giving insight to the genesis of tropical podzol.
Jörg Schnecker, D. Boone Meeden, Francisco Calderon, Michel Cavigelli, R. Michael Lehman, Lisa K. Tiemann, and A. Stuart Grandy
SOIL, 7, 547–561, https://doi.org/10.5194/soil-7-547-2021, https://doi.org/10.5194/soil-7-547-2021, 2021
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Drought and flooding challenge agricultural systems and their management globally. Here we investigated the response of soils from long-term agricultural field sites with simple and diverse crop rotations to either drought or flooding. We found that irrespective of crop rotation complexity, soil and microbial properties were more resistant to flooding than to drought and highly resilient to drought and flooding during single or repeated stress pulses.
Mario Reichenbach, Peter Fiener, Gina Garland, Marco Griepentrog, Johan Six, and Sebastian Doetterl
SOIL, 7, 453–475, https://doi.org/10.5194/soil-7-453-2021, https://doi.org/10.5194/soil-7-453-2021, 2021
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In deeply weathered tropical rainforest soils of Africa, we found that patterns of soil organic carbon stocks differ between soils developed from geochemically contrasting parent material due to differences in the abundance of organo-mineral complexes, the presence/absence of chemical stabilization mechanisms of carbon with minerals and the presence of fossil organic carbon from sedimentary rocks. Physical stabilization mechanisms by aggregation provide additional protection of soil carbon.
Fabian Kalks, Gabriel Noren, Carsten W. Mueller, Mirjam Helfrich, Janet Rethemeyer, and Axel Don
SOIL, 7, 347–362, https://doi.org/10.5194/soil-7-347-2021, https://doi.org/10.5194/soil-7-347-2021, 2021
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Sedimentary rocks contain organic carbon that may end up as soil carbon. However, this source of soil carbon is overlooked and has not been quantified sufficiently. We analysed 10 m long sediment cores with three different sedimentary rocks. All sediments contain considerable amounts of geogenic carbon contributing 3 %–12 % to the total soil carbon below 30 cm depth. The low 14C content of geogenic carbon can result in underestimations of soil carbon turnover derived from 14C data.
Maximilian Kirsten, Robert Mikutta, Didas N. Kimaro, Karl-Heinz Feger, and Karsten Kalbitz
SOIL, 7, 363–375, https://doi.org/10.5194/soil-7-363-2021, https://doi.org/10.5194/soil-7-363-2021, 2021
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Mineralogical combinations of aluminous clay and pedogenic Fe oxides revealed significant effects on soil structure and related organic carbon (OC) storage.
The mineralogical combination resulting in the largest aggregate stability does not better preserve OC during conversion of forests into croplands.
Structural changes in the direction of smaller mean weight diameters do not cancel out the stabilizing effect of soil minerals.
Sophie F. von Fromm, Alison M. Hoyt, Markus Lange, Gifty E. Acquah, Ermias Aynekulu, Asmeret Asefaw Berhe, Stephan M. Haefele, Steve P. McGrath, Keith D. Shepherd, Andrew M. Sila, Johan Six, Erick K. Towett, Susan E. Trumbore, Tor-G. Vågen, Elvis Weullow, Leigh A. Winowiecki, and Sebastian Doetterl
SOIL, 7, 305–332, https://doi.org/10.5194/soil-7-305-2021, https://doi.org/10.5194/soil-7-305-2021, 2021
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We investigated various soil and climate properties that influence soil organic carbon (SOC) concentrations in sub-Saharan Africa. Our findings indicate that climate and geochemistry are equally important for explaining SOC variations. The key SOC-controlling factors are broadly similar to those for temperate regions, despite differences in soil development history between the two regions.
Claudia Cagnarini, Stephen Lofts, Luigi Paolo D'Acqui, Jochen Mayer, Roman Grüter, Susan Tandy, Rainer Schulin, Benjamin Costerousse, Simone Orlandini, and Giancarlo Renella
SOIL, 7, 107–123, https://doi.org/10.5194/soil-7-107-2021, https://doi.org/10.5194/soil-7-107-2021, 2021
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Application of organic amendments, although considered a sustainable form of soil fertilisation, may cause an accumulation of trace elements (TEs) in the topsoil. In this research, we analysed the concentration of zinc, copper, lead and cadmium in a > 60-year experiment in Switzerland and showed that the dynamic model IDMM adequately predicted the historical TE concentrations in plots amended with farmyard manure, sewage sludge and compost and produced reasonable concentration trends up to 2100.
Simon Baumgartner, Marijn Bauters, Matti Barthel, Travis W. Drake, Landry C. Ntaboba, Basile M. Bazirake, Johan Six, Pascal Boeckx, and Kristof Van Oost
SOIL, 7, 83–94, https://doi.org/10.5194/soil-7-83-2021, https://doi.org/10.5194/soil-7-83-2021, 2021
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We compared stable isotope signatures of soil profiles in different forest ecosystems within the Congo Basin to assess ecosystem-level differences in N cycling, and we examined the local effect of topography on the isotopic signature of soil N. Soil δ15N profiles indicated that the N cycling in in the montane forest is more closed, whereas the lowland forest and Miombo woodland experienced a more open N cycle. Topography only alters soil δ15N values in forests with high erosional forces.
Rota Wagai, Masako Kajiura, and Maki Asano
SOIL, 6, 597–627, https://doi.org/10.5194/soil-6-597-2020, https://doi.org/10.5194/soil-6-597-2020, 2020
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Global significance of metals (extractable Fe and Al phases) to control organic matter (OM) in recognized. Next key questions include the identification of their localization and mechanism behind OM–metal relationships. Across 23 soils of contrasting mineralogy, Fe and Al phases were mainly associated with microbially processed OM as meso-density microaggregates. OM- and metal-rich nanocomposites with a narrow OM : metal ratio likely acted as binding agents. A new conceptual model was proposed.
Marco Panettieri, Denis Courtier-Murias, Cornelia Rumpel, Marie-France Dignac, Gonzalo Almendros, and Abad Chabbi
SOIL, 6, 435–451, https://doi.org/10.5194/soil-6-435-2020, https://doi.org/10.5194/soil-6-435-2020, 2020
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In the context of global change, soil has been identified as a potential C sink, depending on land-use strategies. This work is devoted to identifying the processes affecting labile soil C pools resulting from changes in land use. We show that the land-use change in ley grassland provoked a decoupling of the storage and degradation processes after the grassland phase. Overall, the study enables us to develop a sufficient understanding of fine-scale C dynamics to refine soil C prediction models.
Miriam Groß-Schmölders, Pascal von Sengbusch, Jan Paul Krüger, Kristy Klein, Axel Birkholz, Jens Leifeld, and Christine Alewell
SOIL, 6, 299–313, https://doi.org/10.5194/soil-6-299-2020, https://doi.org/10.5194/soil-6-299-2020, 2020
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Degradation turns peatlands into a source of CO2. There is no cost- or time-efficient method available for indicating peatland hydrology or the success of restoration. We found that 15N values have a clear link to microbial communities and degradation. We identified trends in natural, drained and rewetted conditions and concluded that 15N depth profiles can act as a reliable and efficient tool for obtaining information on current hydrology, restoration success and drainage history.
Martin Erlandsson Lampa, Harald U. Sverdrup, Kevin H. Bishop, Salim Belyazid, Ali Ameli, and Stephan J. Köhler
SOIL, 6, 231–244, https://doi.org/10.5194/soil-6-231-2020, https://doi.org/10.5194/soil-6-231-2020, 2020
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In this study, we demonstrate how new equations describing base cation release from mineral weathering can reproduce patterns in observations from stream and soil water. This is a major step towards modeling base cation cycling on the catchment scale, which would be valuable for defining the highest sustainable rates of forest harvest and levels of acidifying deposition.
Benjamin Andrieux, David Paré, Julien Beguin, Pierre Grondin, and Yves Bergeron
SOIL, 6, 195–213, https://doi.org/10.5194/soil-6-195-2020, https://doi.org/10.5194/soil-6-195-2020, 2020
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Our study aimed to disentangle the contribution of several drivers to explaining the proportion of soil carbon that can be released to CO2 through microbial respiration. We found that boreal-forest soil chemistry is an important driver of the amount of carbon that microbes can process. Our results emphasize the need to include the effects of soil chemistry into models of carbon cycling to better anticipate the role played by boreal-forest soils in carbon-cycle–climate feedbacks.
Jonathan Sanderman and A. Stuart Grandy
SOIL, 6, 131–144, https://doi.org/10.5194/soil-6-131-2020, https://doi.org/10.5194/soil-6-131-2020, 2020
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Soils contain one of the largest and most dynamic pools of carbon on Earth, yet scientists still struggle to understand the reactivity and fate of soil organic matter upon disturbance. In this study, we found that with increasing thermal stability, the turnover time of organic matter increased from decades to centuries with a concurrent shift in chemical composition. In this proof-of-concept study, we found that ramped thermal analyses can provide new insights for understanding soil carbon.
Carlos Alberto Quesada, Claudia Paz, Erick Oblitas Mendoza, Oliver Lawrence Phillips, Gustavo Saiz, and Jon Lloyd
SOIL, 6, 53–88, https://doi.org/10.5194/soil-6-53-2020, https://doi.org/10.5194/soil-6-53-2020, 2020
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Amazon soils hold as much carbon (C) as is contained in the vegetation. In this work we sampled soils across 8 different Amazonian countries to try to understand which soil properties control current Amazonian soil C concentrations. We confirm previous knowledge that highly developed soils hold C through clay content interactions but also show a previously unreported mechanism of soil C stabilization in the younger Amazonian soil types which hold C through aluminium organic matter interactions.
Cited articles
Aerts, R.: Climate, leaf litter chemistry and leaf litter decomposition in terrestrial ecosystems: A triangular relationship, Oikos, 79, 439–449, https://doi.org/10.2307/3546886, 1997.
Alaei, L., Ashengroph, M., and Moosavi-Movahedi, A. A.: The concept of protein folding/unfolding and its impacts on human health, Adv. Protein Chem. Str., 126, 227–278, https://doi.org/10.1016/bs.apcsb.2021.01.007, 2021.
Alewell, C., Ringeval, B., Ballabio, C., Robinson, D. A., Panagos, P., and Borrelli, P.: Global phosphorus shortage will be aggravated by soil erosion, Nat. Commun., 11, 4546, https://doi.org/10.1038/s41467-020-18326-7, 2020.
Arenz, B. E., Blanchette, R. A., and Farrell, R. L.: Fungal diversity in Antarctic soils, in: Antarctic Terrestrial Microbiology, edited by: Cowan, D. A., Springer-Verlag, Berlin Heiderberg, 35–53, https://doi.org/10.1007/978-3-642-45213-0_3, 2014.
Barták, M., Váczi, P., Stachoň, Z., and Kubešová, S.: Vegetation mapping of moss-dominated areas of northern part of James Ross Island (Antarctica) and a suggestion of protective measures, Czech Polar Rep., 5, 75–87, https://doi.org/10.5817/CPR2015-1-8, 2015.
Basu, S., Rabara, R. C., and Negi, S.: AMF: The future prospect for sustainable agriculture, Physiol. Mol. Plant P., 102, 36–45, https://doi.org/10.1016/j.pmpp.2017.11.007, 2018.
Batjes, N. H.: Total carbon and nitrogen in the soils of the world, Eur. J. Soil Sci., 47, 151–163, https://doi.org/10.1111/j.1365-2389.1996.tb01386.x, 1996.
Blackwell, M.: Evolution. Terrestrial life – fungal from the start?, Science, 289, 1884–1885, https://doi.org/10.1126/science.289.5486.1884, 2000.
Błaszkowski, J.: Glomeromycota, W. Szafer Institute of Botany, Polish Academy of Sciences, Kraków, 303 pp., ISBN 978-83-89648-82-2, 2012.
Bonanomi, G., Incerti, G., Giannino, F., Mingo, A., Lanzotti, V., and Mazzoleni, S.: Litter quality assessed by solid state 13C NMR spectroscopy predicts decay rate better than
Bond-Lamberty, B. and Thomson, A.: A global database of soil respiration data, Biogeosciences, 7, 1915–1926, https://doi.org/10.5194/bg-7-1915-2010, 2010.
Bradford, M. M.: A rapid and sensitive method for the quantitation of microgram quantities of protein utilizing the principle of protein-dye binding, Anal. Biochem., 72, 248–254, https://doi.org/10.1016/0003-2697(76)90527-3, 1976.
Bridge, P. D. and Newsham, K. K.: Soil fungal community composition at Mars Oasis, a southern maritime Antarctic site, assessed by PCR amplification and cloning, Fungal Ecol., 2, 66–74, https://doi.org/10.1016/j.funeco.2008.10.008, 2009.
Campbell, I. B. and Claridge, G. G. C.: Antarctica: Soils, Weathering Processes and Environment. Developments in Soil Science 16, Elsevier Science, 367 pp., ISBN 9780444427847, 1987.
Cross, A. F. and Schlesinger, W. H.: Biological and geochemical controls on phosphorus fractions in semiarid soils, Biogeochemistry, 52, 155–172, https://doi.org/10.1023/A:1006437504494, 2001.
Czech Geological Survey: James Ross Island – Northern Part. Topographic map 1 : 25 000, CGS, Praha, ISBN 978-80-7075-734-5, 2009.
Durán, J., Rodríguez, A., Heiðmarsson, S., Lehmann, J. R. K., del Moral, Á., Garrido-Benavent, I., and De los Ríos, A.: Cryptogamic cover determines soil attributes and functioning in polar terrestrial ecosystems, Sci. Total Environ., 762, 143169, https://doi.org/10.1016/j.scitotenv.2020.143169, 2021.
FAO: Measuring and modelling soil carbon stock and stock changes in livestock production systems. Guidelines for assessment (Version 1), Livestock Environmental Assessment and Performance (LEAP) Partnership, FAO, Rome, 170 pp., ISBN 978-92-5-131408-1, 2019.
Fassbender, A. J., Orr, J. C., and Dickson, A. G.: Technical note: Interpreting pH changes, Biogeosciences, 18, 1407–1415, https://doi.org/10.5194/bg-18-1407-2021, 2021.
Filippelli, G. M. and Souch, C.: Effects of climate and landscape development on the terrestrial phosphorus cycle, Geology, 27, 171–174, https://doi.org/10.1130/0091-7613(1999)027<0171:EOCALD>2.3.CO;2, 1999.
Fitter, A. H., Heinemeyer, A., and Staddon, P. L.: The impact of elevated CO2 and global climate change on arbuscular mycorrhizas: a mycocentric approach, New Phytol., 147, 179–187, https://doi.org/10.1046/j.1469-8137.2000.00680.x, 2008.
Gao, M. R., Xu, Q. D., He, Q., Sun, Q., and Zeng, W.-C.: A theoretical and experimental study: the influence of different standards on the determination of total phenol content in the Folin–Ciocalteu assay, J. Food Meas. Charact., 13, 1349–1356, https://doi.org/10.1007/s11694-019-00050-6, 2019.
Gillespie, A. W., Farrell, R. E., Walley, F. L., Ross, A. R., Leinweber, P., Eckhardt, K. U., Regier, T. Z., and Blyth, R. I.: Glomalin-related soil protein contains non-mycorrhizal-related heat-stable proteins, lipids and humic materials, Soil. Biol. Biochem., 43, 766–777, https://doi.org/10.1016/j.soilbio.2010.12.010, 2011.
Golchin, A., Baldock, J. A., and Oades, J. M.: A model linking organic matter decomposition, chemistry, and aggregate dynamics, in: Soil processes and the carbon cycle, edited by: Lal, R., Kimble, J. M., Follet, F., and Stewart, B. A., CRC Press, 245–266, https://doi.org/10.1201/9780203739273, 2018.
Green, T. G. A., Nash, T. H., and Lange, O. L.: Physiological ecology of carbon dioxide Exchange, in: Lichen Biology, edited by: Nash III, T. H., Cambridge University Press, 152–181, https://doi.org/10.1017/CBO9780511790478.010, 2008.
Grewal, K. S., Buchan, G. D., and Sherlock, R. R.: Comparison of three methods of organic carbon determination in some New Zealand soils, Eur. J. Soil Sci., 42, 251–257, https://doi.org/10.1111/j.1365-2389.1991.tb00406.x, 1991.
Harper, C. J., Taylor, T. N., Krings, M., and Taylor, E. L.: Mycorrhizal symbiosis in the Paleozoic seed fern Glossopteris from Antarctica, Rev. Palaeobot. Palyno., 192, 22–31, https://doi.org/10.1016/j.revpalbo.2013.01.002, 2013.
Holátko, J., Brtnický, M., Kučerík, J., Kotianová, M., Elbl, J., Kintl, A., Kynický, J., Benada, O., Datta, R., and Jansa, J.: Glomalin – Truths, myths, and the future of this elusive soil glycoprotein, Soil Biol. Biochem., 153, 108116, https://doi.org/10.1016/j.soilbio.2020.108116, 2021.
Houghton, R. A.: Balancing the global carbon budget, Annu. Rev. Earth Pl. Sc., 35, 313–347, https://doi.org/10.1146/annurev.earth.35.031306.140057, 2007.
Huang, Y., Wang, D. W., Cai, J. L., and Zheng, W. S.: Review of glomalin-related soil protein and its environmental function in the rhizosphere, Chin. J. Plant Ecol., 35, 232–236, https://www.plant-ecology.com/EN/10.3724/SP.J.1258.2011.00232 (last access: 14 November 2024), 2011.
Kelley, A. P.: Mycotrophy in plants. Chronica Botanica, Waltham, MA, 223 pp., ISBN-13 978-1121005679, 1950.
Keuskamp, J. A., Dingemans, B. J. J., Lehtinen, T., Sarneel, J. M., and Hefting, M. M.: Tea Bag Index: a novel approach to collect uniform decomposition data across ecosystems, Method. Ecol. Evol., 4, 1070–1075, https://doi.org/10.1111/2041-210X.12097, 2013.
Kondratyuk, S. Y. and Kärnefelt, I.: Revision of three natural groups of xanthorioid lichens (Teloschistaceae, Ascomycota), Ukrainskiy Botanichnyi Zhurnal, 60, 427–437, 2003.
Kouchi, H., Shimomura, K., Hata, S., Hirota, A., Wu, G. J., Kumagai, H., Tajima, S., Suganuma, N., Suzuki, A., Aoki, T., Hayashi, M., Yokoyama, T., Ohyama, T., Asamizu, E., Kuwata, Ch., Shibata, D., and Tabata, S.: Large-scale analysis of gene expression profiles during early stages of root nodule formation in a model legume, Lotus japonicus, DNA Res., 11, 263–274, https://doi.org/10.1093/dnares/11.4.263, 2004.
Láska, K. and Prošek, P.: Klima a klimatický výzkum ostrova James Ross, in: Antarktida, edited by: Prošek, P., Academia, 348 pp., ISBN 978-80-200-2140-3, 2013.
Lovato, P. E., Schuepp, H., Trouvelot, A., and Gianinazzi, S.: Application of arbuscular mycorrhizal fungi (AMF) in orchid and ornamental plants, in: Mycorrhiza, edited by: Varma, A. and Hock, B., Springer, Berlin Heidelberg New York, 443–468, https://doi.org/10.1007/978-3-662-03779-9_19, 1995.
Makkonen, M., Berg, M. P., Handa, I. T., Hättenschwiler, S., van Ruijven, J., van Bodegom, P. M., and Aerts, R.: Highly consistent effects of plant litter identity and functional traits on decomposition across a latitudinal gradient, Ecol. Lett., 15, 1033–1041, https://doi.org/10.1111/j.1461-0248.2012.01826.x, 2012.
Martins, M. C. B., de Lima, M. J. G., Silva, F. P., Azevedo-Ximenes, E., da Silva, N. H., and Pereira, E. C.: Cladia aggregata (lichen) from Brazilian Northeast: chemical characterization and antimicrobial activity, Braz. Arch. Biol. Techn., 53, 115–122, https://doi.org/10.1590/S1516-89132010000100015, 2010.
Masson-Delmotte, V., Kageyama, M., Braconnot, P., Charbit, S., Krinner, G., Ritz, C., Guilyardi, E., Jouzel, J., Abe-Ouchi, A., Crucifix, M., Gladstone, R. M., Hewitt, C. D., Kitoh, A., LeGrande, A. N., Marti, O., Merkel, U., Motoi, T., Ohgaito, R., Otto-Bliesner, B., Peltier, W. R., Ross, I., Valdes, P. J., Vettoretti, G., Weber, S. L., Wolk, F., and Yu, Y.: Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints, Clim. Dynam., 26, 513–529, https://doi.org/10.1007/s00382-005-0081-9, 2006.
Matějka, M., Láska, K., Jeklová, K., and Hošek, J.: High-Resolution Numerical Modelling of Near-Surface Atmospheric Fields in the Complex Terrain of James Ross Island, Antarctic Peninsula, Atmosphere-Basel, 12, 360, https://doi.org/10.3390/atmos12030360, 2021.
McCraw, J. D.: Soils of the Ross Dependency, Antarctica. A preliminary note, N. Z. Soc. Soil Sci. Proc., 4, 30–35, 1960.
Mehlich, A.: Mehlich 3 soil test extractant: A modification of the Mehlich 2 extractant, Commun. Soil Sci. Plan., 15, 1409–1416, https://doi.org/10.1080/00103628409367568, 1984.
Melo, C. D., Walker, C., Krüger, C., Borges, P. A. V., Luna, S., Mendoca, D., Fonseca, H. M. A. C., and Machado, A. C.: Environmental factors driving arbuscular mycorrhizal fungal communities associated with endemic woody plant Picconiaazorica on native forest of Azores, Ann. Microbiol., 69, 1309–1327, https://doi.org/10.1007/s13213-019-01535-x, 2019.
Mlčoch, B., Nývlt, D., and Mixa, P.: Geological map of James Ross Island Northern Part 1 : 25 000, Czech Geol. Survey, Prague, ISBN 978-80-7075-996-7, 2020.
Paul, E. (Ed.): Soil microbiology, ecology and biochemistry, Academic Press, 604 pp., ISBN 9780124159556, 2014.
Pirozynski, K. A. and Malloch, D. W.: The origin of land plants: a matter of mycotropism, Biosystems, 6, 153–164, https://doi.org/10.1016/0303-2647(75)90023-4, 1975.
Pohanka, M. and Vlček, V.: Assay of glomalin using a quartz crystal microbalance biosensor, Electroanalysis, 30, 453–458, https://doi.org/10.1002/elan.201700772, 2018.
Pospíšilová, L., Vlček, V., Hybler, V., and Uhlík, P.: Carbon content and macroelement in cryosols, Humic Substances Research, 13, 13–17, 2017.
R Core Team: R: A Language and Environment for Statistical Computing, R Foundation for Statistical Computing, Vienna, Austria, https://www.R-project.org/ (last access: 15 December 2022), 2022.
Rackley, S. A.: Carbon capture and storage, Butterworth-Heinemann, 698 pp., ISBN 9780128120415, 2017.
Rayner, M. C.: Mycorrhiza – An Account of Non-Pathogenic Infection by Fungi in Vascular Plants and Bryophytes, White Press, ISBN-10: 152870763X, ISBN-13: 978-1528707633, 2018.
Redecker, D., Kodner, R., and Graham, L. E.: Glomalean fungi from the Ordovician, Science, 289, 1920–1921, https://doi.org/10.1126/science.289.5486.1920, 2000.
Remy, W., Taylor, T. N., Hass, H., and Kerp, H.: Four hundred-million-year-old vesicular arbuscular mycorrhizae, P. Natl. Acad. Sci. USA, 91, 11841–11843, https://doi.org/10.1073/pnas.91.25.11841, 1994.
Röder, J., Detsch, F., Otte, I., Appelhans, T., Nauss, T., Peters, M. K., and Brandl, R.: Heterogeneous patterns of abundance of epigeic arthropod taxa along a major elevation gradient, Biotropica, 49, 217–228, https://doi.org/10.1111/btp.12403, 2016.
Russell, J. and Bulman, S.: The liverwort Marchantia foliacea forms a specialized symbiosis with arbuscular mycorrhizal fungi in the genus Glomus, New Phytol., 165, 567–579, https://doi.org/10.1111/j.1469-8137.2004.01251.x, 2005.
Santiago, R., Silva, N. H., Silva, F. P., Martins, M. C. B., de Vasconcelos, T. L., Yano-Melo, A. M., and Pereira, E. C.: Interactions of the lichen Cladonia salzmannii Nyl. with soil, microbiota, mycorrhizae and Genipa Americana, J. Soil Sci. Plant Nut., 18, 833–850, https://doi.org/10.4067/S0718-95162018005002402, 2018.
Schüßler, A., Schwarzott, D., and Walker, Ch.: A new fungal phylum, the Glomeromycota: phylogeny and evolution, Mycol. Res., 105, 1413–1421, https://doi.org/10.1017/S0953756201005196, 2001.
Shukla, V., Bajpai, R., Pandey, U., and Upreti, D. K.: Do Lichens have the Ability to Remove Arsenic from Water?, Int. J. Plant Environ., 5, 47–49, https://doi.org/10.18811/ijpen.v5i01.8, 2019.
Siewert, Ch.: Rapid screening of soil properties using thermogravimetry, Soil Sci. Soc. Am. J., 68, 1656–1661, https://doi.org/10.2136/sssaj2004.1656, 2004.
Simon, L., Bousquet, J., Levesque, R. C., and Lalonde, M.: Origin and diversification of endomycorrhizal fungi and coincidence with vascular land plants, Nature, 363, 67–69, https://doi.org/10.1038/363067a0, 1993.
Smith, S. E. and Read, D. J.: Mycorrhizal Symbiosis. San Diego, CA, Academic Press, https://doi.org/10.1016/B978-0-12-652840-4.X5000-1, 1997.
Smith, S. E. and Read, D. J.: Mycorrhizal Symbiosis, Academic Press, San Diego, USA, 800 pp., https://doi.org/10.1016/B978-0-12-370526-6.X5001-6, 2008.
Stark, S. and Hyvärinen, M.: Are phenolics leaching from the lichen Cladina stellaris sources of energy rather than allelophatic agents for soil microorganisms?, Soil Biol. Biochem., 35, 1381–1385, https://doi.org/10.1016/S0038-0717(03)00217-7, 2003.
Strelin, J. A. and Sone, T.: Rock glaciers on James Ross Island, Antarctica, in: Permafrost, 7th International Conference Proceedings, Yellowknife (Canada), edited by: Lewkowicz, A. G. and Allard, M., Collection Nordicana University Laval, Quebec, 1027–1032, 23–27 June 1998, OCLC No 40770716, ISBN: 9782920197572, 2920197576, 1998.
Swati, J., Bajpai, A., and Narain Johri, B.: Extremophilic fungi at the interface of climate change, in: Fungi Bio-Prospects in Sustainable Agriculture, Environment and Nano-technology, edited by: Kumar, V. S., Shah, M. P., Parmar, S., and Kumar, A., Academic Press, 1–22, ISBN 9780128219256, https://doi.org/10.1016/B978-0-12-821925-6.00001-0, 2021.
Tarnocai, C., Canadell, J. G., Schuur, E. A. G., Kuhry, P., Mazhitova, G., and Zimov, S.: Soil organic carbon pools in the northern circumpolar permafrost region, Global Biogeochem. Cy., 23, GB2023, https://doi.org/10.1029/2008GB003327, 2009.
Tigre, R. C., Silva, N. H., Santos, M. G., Honda, N. K., Falcao, E. P. S., and Pereira, E. C.: Allelopathic and bioherbicidal potential of Cladonia verticillaris on the germination and growth of Lactuca sativa, Ecotoxicol. Environ. Safety, 84, 125–132, https://doi.org/10.1016/j.ecoenv.2012.06.026, 2012.
Tóth, Z., Táncsics, A., Kriszt, B., Kröel-Dulay, G., Ónodi, G., and Hornung, E.: Extreme effects of drought on composition of the soil bacterial community and decomposition of plant tissue, Eur. J. Soil Sci., 68, 504–513, https://doi.org/10.1111/ejss.12429, 2017.
Turner, J., Colwell, S. R., Marshall, G. J., Lachlan-Cope, T. A., Carleton, A. M., Jones, P. D., Lagun, V., Reid, P. A., and Iagovkina, S.: Antarctic climate change during the last 50 years, Int. J. Climatol., 25, 279–294, https://doi.org/10.1002/joc.1130, 2005.
Utaile, Y. U., Honnay, O., Muys, B., Cheche, S. S., and Helsen, K.: Effect of Dichrostachys cinerea encroachment on plant species diversity, functional traits and litter decomposition in an East‐African savannah ecosystem, J. Veg. Sci., 32, e12949, https://doi.org/10.1111/jvs.12949, 2021.
van Bemmelen, J. M.: Über die Bestimmungen des Wassers, den Humus, des Schwefels, der in den colloidalen Silikaten gebunden Kieselsäuren, des Mangans, u.s.w. im Ackerboden, Landwirtschaftliche Versuch Station, 37, 279–290, 1889.
Vingiani, S., Adamo, P., and Giordano, S.: Sulphur, nitrogen and carbon content of Sphagnum capillifolium and Pseudevernia furfuracea exposed in bags in the Naples urban area, Environ. Pollut., 129, 145–158, https://doi.org/10.1016/j.envpol.2003.09.016, 2004.
Vlček, V., Pospíšilová, L., and Uhlík, P.: Mineralogy and chemical composition of Cryosols and Andosols in Antarctica, Soil Water Res., 13, 61–73, https://doi.org/10.17221/231/2016-SWR, 2018.
Walkley, A.: A Critical Examination of a Rapid Method for Determining Organic Carbon in Soils: Effect of Variations in Digestion Conditions and of Inorganic Soil Constituents, Soil Sci., 63, 251–264, https://doi.org/10.1097/00010694-194704000-00001, 1947.
Walkley, A. and Black, I. A.: An examination of the Degtjareff method for determining soil organic matter, and a proposed modification of the chromic acid titration method, Soil Sci., 37, 29–38, https://doi.org/10.1097/00010694-193401000-00003, 1934.
Wilcke, W., Oelmann, Y., Schmitt, A., Valarezo, C., Zech, W., and Homeier, J.: Soil properties and tree growth along an altitudinal transect in Ecuadorian tropical montane forest, J. Plant Nutr. Soil Sc., 171, 220–230, https://doi.org/10.1002/jpln.200625210, 2008.
Wright, S. F. and Anderson, R. L.: Aggregate stability and glomalin in alternative crop rotations for the central Great Plains, Biol. Fert. Soils, 31, 249–253, https://doi.org/10.1007/s003740050653, 2000.
Wright, S. F. and Upadhyaya, A.: Extraction of an abundant and unusual protein from soil and comparison with hyphal protein of arbuscular mycorrhizal fungi, Soil Sci., 161, 575–586, https://doi.org/10.1097/00010694-199609000-00003, 1996.
Wuest, S. B., Caesar-TonThat, T. C., Wright, S. F., and Williams, J. D.: Organic matter addition, N, and residue burning effects on infiltration, biological, and physical properties of an intensively tilled silt–loam soil, Soil Till. Res., 84, 154–167, https://doi.org/10.1016/j.still.2004.11.008, 2005.
Zech, W., Senesi, N., Guggenberger, G., Kaiser, K., Lehmann, J., Miano, T., Miltner, A., and Schroth, G.: Factors controlling humification and mineralization of soil organic matter in the tropics, Geoderma, 79, 117–161, https://doi.org/10.1016/S0016-7061(97)00040-2, 1997.
Zhu, R., Wang, Q., Wang, C., Hou, L., and Ma, D.: Penguins significantly increased phosphine formation and phosphorus contribution in maritime Antarctic soils, Sci. Rep.-UK, 4, 7055, https://doi.org/10.1038/srep07055, 2014.
Zhu, Y.-G. and Miller, R. M.: Carbon cycling by arbuscular mycorrhizal fungi in soil-plant systems, Trends Plant Sci., 8, 407–409, https://doi.org/10.1016/s1360-1385(03)00184-5, 2003.
Zvěřina, O., Coufalík, P., Vaculovič, T., Kuta, J., Zeman, J., and Komárek, J.: Macro-and microelements in soil profile of the moss-covered area in James Ross Island, Antarctica, Czech Polar Rep., 2, 1–7, https://doi.org/10.5817/CPR2012-1-1, 2012.
Short summary
The aim of this work was to evaluate the correlation between soil organic carbon (SOC) and various soil properties. Nine plots across an altitudinal range from 10 to 320 m were investigated in the deglaciated region of James Ross Island (Antarctica). Our results indicate that the primary factor influencing the SOC content is likely not altitude or coarse-fraction content; rather, other hard-to-quantify factors, such as the presence of liquid water during the summer period, impact SOC content.
The aim of this work was to evaluate the correlation between soil organic carbon (SOC) and...
