Articles | Volume 2, issue 4
https://doi.org/10.5194/soil-2-583-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/soil-2-583-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Soil microbial biomass and function are altered by 12 years of crop rotation
Marshall D. McDaniel
CORRESPONDING AUTHOR
Department of Natural Resources and the Environment, University of New Hampshire, Durham, NH, USA
current address: Department of Agronomy, Iowa State University, 2517 Agronomy Hall, 716 Farm House Lane, Ames, IA 50011, USA
A. Stuart Grandy
Department of Natural Resources and the Environment, University of New Hampshire, Durham, NH, USA
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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.
William R. Wieder, Derek Pierson, Stevan Earl, Kate Lajtha, Sara G. Baer, Ford Ballantyne, Asmeret Asefaw Berhe, Sharon A. Billings, Laurel M. Brigham, Stephany S. Chacon, Jennifer Fraterrigo, Serita D. Frey, Katerina Georgiou, Marie-Anne de Graaff, A. Stuart Grandy, Melannie D. Hartman, Sarah E. Hobbie, Chris Johnson, Jason Kaye, Emily Kyker-Snowman, Marcy E. Litvak, Michelle C. Mack, Avni Malhotra, Jessica A. M. Moore, Knute Nadelhoffer, Craig Rasmussen, Whendee L. Silver, Benjamin N. Sulman, Xanthe Walker, and Samantha Weintraub
Earth Syst. Sci. Data, 13, 1843–1854, https://doi.org/10.5194/essd-13-1843-2021, https://doi.org/10.5194/essd-13-1843-2021, 2021
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Data collected from research networks present opportunities to test theories and develop models about factors responsible for the long-term persistence and vulnerability of soil organic matter (SOM). Here we present the SOils DAta Harmonization database (SoDaH), a flexible database designed to harmonize diverse SOM datasets from multiple research networks.
Emily Kyker-Snowman, William R. Wieder, Serita D. Frey, and A. Stuart Grandy
Geosci. Model Dev., 13, 4413–4434, https://doi.org/10.5194/gmd-13-4413-2020, https://doi.org/10.5194/gmd-13-4413-2020, 2020
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Microbes drive carbon (C) and nitrogen (N) transformations in soil, and soil models have started to include explicit microbial physiology and functioning to try to reduce uncertainty in soil–climate feedbacks. Here, we add N cycling to a microbially explicit soil C model and reproduce C and N dynamics in soil during litter decomposition across a range of sites. We discuss model-generated hypotheses about soil C and N cycling and highlight the need for landscape-scale model evaluation data.
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.
W. R. Wieder, A. S. Grandy, C. M. Kallenbach, P. G. Taylor, and G. B. Bonan
Geosci. Model Dev., 8, 1789–1808, https://doi.org/10.5194/gmd-8-1789-2015, https://doi.org/10.5194/gmd-8-1789-2015, 2015
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Projecting biogeochemical responses to environmental change requires multi-scaled perspectives. However, microbes, the drivers of soil organic matter decomposition and stabilization, remain notably absent from models used to project carbon cycle–climate feedbacks. Here, we apply and evaluate representations of microbial functional diversity across scales and find that such representations may be critical to accurately project soil carbon dynamics in a changing world.
W. R. Wieder, A. S. Grandy, C. M. Kallenbach, and G. B. Bonan
Biogeosciences, 11, 3899–3917, https://doi.org/10.5194/bg-11-3899-2014, https://doi.org/10.5194/bg-11-3899-2014, 2014
Related subject area
Soil biodiversity and soil health
Ectomycorrhizal fungal network complexity determines soil multi-enzymatic activity
Unraveling biogeographical patterns and environmental drivers of soil fungal diversity at the French national scale
Biochar promotes soil aggregate stability and associated organic carbon sequestration and regulates microbial community structures in Mollisols from northeast China
Only a minority of bacteria grow after wetting in both natural and post-mining biocrusts in a hyperarid phosphate mine
Lower functional redundancy in “narrow” than “broad” functions in global soil metagenomics
Pairing litter decomposition with microbial community structures using the Tea Bag Index (TBI)
Network complexity of rubber plantations is lower than tropical forests for soil bacteria but not for fungi
Changes in soil physicochemical properties and bacterial communities at different soil depths after long-term straw mulching under a no-till system
Microbial communities and their predictive functional profiles in the arid soil of Saudi Arabia
Development of a soil biological quality index for soils of semi-arid tropics
What do we know about how the terrestrial multicellular soil fauna reacts to microplastic?
Soil denitrifier community size changes with land use change to perennial bioenergy cropping systems
Knowledge needs, available practices, and future challenges in agricultural soils
Technological advancements and their importance for nematode identification
Fire affects root decomposition, soil food web structure, and carbon flow in tallgrass prairie
Case study of microarthropod communities to assess soil quality in different managed vineyards
A meta-analysis of soil biodiversity impacts on the carbon cycle
Jorge Prieto-Rubio, José L. Garrido, Julio M. Alcántara, Concepción Azcón-Aguilar, Ana Rincón, and Álvaro López-García
SOIL, 10, 425–439, https://doi.org/10.5194/soil-10-425-2024, https://doi.org/10.5194/soil-10-425-2024, 2024
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Changes in soil biological activity when microbial taxa interact remain little understood. To address this, we approach network analyses of ectomycorrhizal fungal communities. The study highlights how distinct fungi contribute to explaining community structure, whilst others mainly do for soil enzymatic activity. This differentiation between structural and functional roles of ectomycorrhizal fungi adds new insights to understand soil fungal community complexity and its functionality in soils.
Christophe Djemiel, Samuel Dequiedt, Walid Horrigue, Arthur Bailly, Mélanie Lelièvre, Julie Tripied, Charles Guilland, Solène Perrin, Gwendoline Comment, Nicolas P. A. Saby, Claudy Jolivet, Antonio Bispo, Line Boulonne, Antoine Pierart, Patrick Wincker, Corinne Cruaud, Pierre-Alain Maron, Sébastien Terrat, and Lionel Ranjard
SOIL, 10, 251–273, https://doi.org/10.5194/soil-10-251-2024, https://doi.org/10.5194/soil-10-251-2024, 2024
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The fungal kingdom has been diversifying for more than 800 million years by colonizing a large number of habitats on Earth. Based on a unique dataset (18S rDNA meta-barcoding), we described the spatial distribution of fungal diversity at the scale of France and the environmental drivers by tackling biogeographical patterns. We also explored the fungal network interactions across land uses and climate types.
Jing Sun, Xinrui Lu, Guoshuang Chen, Nana Luo, Qilin Zhang, and Xiujun Li
SOIL, 9, 261–275, https://doi.org/10.5194/soil-9-261-2023, https://doi.org/10.5194/soil-9-261-2023, 2023
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A field experiment was conducted to compare and analyze the effects of combined application of biochar and nitrogen fertilizer on soil aggregate stability mechanism, the dynamic characteristics of aggregate organic carbon, and the microbial community structure in northeast black soil. We provide a scientific basis for formulating effective strategies to slow down soil quality degradation and ensure the sustainable development of the agroecosystem.
Talia Gabay, Eva Petrova, Osnat Gillor, Yaron Ziv, and Roey Angel
SOIL, 9, 231–242, https://doi.org/10.5194/soil-9-231-2023, https://doi.org/10.5194/soil-9-231-2023, 2023
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This paper evaluates bacterial growth in biocrusts after a large-scale mining disturbance in a hyperarid desert, using a stable isotope probing assay.
We discovered that biocrust bacteria from both natural and post-mining plots resumed photosynthetic activity but did not grow following hydration. Our paper provides insights into the effects of a large-scale disturbance (mining) on biocrusts and their response to hydration, with implications for biocrust restoration practices in Zin mines.
Huaihai Chen, Kayan Ma, Yu Huang, Qi Fu, Yingbo Qiu, Jiajiang Lin, Christopher W. Schadt, and Hao Chen
SOIL, 8, 297–308, https://doi.org/10.5194/soil-8-297-2022, https://doi.org/10.5194/soil-8-297-2022, 2022
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By analyzing and generalizing microbial taxonomic and functional profiles, we provide strong evidence that the degree of soil microbial functional redundancy differs significantly between “broad” and “narrow” functions across the globe. Future sequencing efforts will likely increase our confidence in comparative metagenomes and provide time-series information to further identify to what extent microbial functional redundancy regulates dynamic ecological fluxes across space and time.
Anne Daebeler, Eva Petrová, Elena Kinz, Susanne Grausenburger, Helene Berthold, Taru Sandén, Roey Angel, and the high-school students of biology project groups I, II, and
III from 2018–2019
SOIL, 8, 163–176, https://doi.org/10.5194/soil-8-163-2022, https://doi.org/10.5194/soil-8-163-2022, 2022
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In this citizen science project, we combined a standardised litter bag method (Tea Bag Index) with microbiome analysis of bacteria and fungi colonising the teabags to gain a holistic understanding of the carbon degradation dynamics in temperate European soils. Our method focuses only on the active part of the soil microbiome. The results show that about one-third of the prokaryotes and one-fifth of the fungal species (ASVs) in the soil were enriched in response to the presence of fresh OM.
Guoyu Lan, Chuan Yang, Zhixiang Wu, Rui Sun, Bangqian Chen, and Xicai Zhang
SOIL, 8, 149–161, https://doi.org/10.5194/soil-8-149-2022, https://doi.org/10.5194/soil-8-149-2022, 2022
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Forest conversion alters both bacterial and fungal soil networks: it reduces bacterial network complexity and enhances fungal network complexity. This is because forest conversion changes the soil pH and other soil properties, which alters the bacterial composition and subsequent network structure. Our study demonstrates the impact of forest conversion on soil network structure, which has important implications for ecosystem functions and the health of soil ecosystems in tropical regions.
Zijun Zhou, Zengqiang Li, Kun Chen, Zhaoming Chen, Xiangzhong Zeng, Hua Yu, Song Guo, Yuxian Shangguan, Qingrui Chen, Hongzhu Fan, Shihua Tu, Mingjiang He, and Yusheng Qin
SOIL, 7, 595–609, https://doi.org/10.5194/soil-7-595-2021, https://doi.org/10.5194/soil-7-595-2021, 2021
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Straw mulching is not always combined with no-till systems during conservation tillage. We explored the effects of long-term straw mulching on soil attributes with soil depths under a no-till system. Compared to straw removal, straw mulching had various effects on soil properties at different depths, the biggest difference occurring at the topsoil depth. Overall, straw mulch is highly recommended for use under the no-till system because of its benefits to soil fertility and bacterial abundance.
Munawwar A. Khan and Shams T. Khan
SOIL, 6, 513–521, https://doi.org/10.5194/soil-6-513-2020, https://doi.org/10.5194/soil-6-513-2020, 2020
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Soil is a renewable resource for purposes ranging from agriculture to mineralization. Soil microbiome plays vital roles in facilitating process like providing nutrients to plants, or their mobilization for plant uptake, consequently improving plant growth and productivity. Therefore, understanding of these microbial communities and their role in soil is crucial for exploring the possibility of using microbial community inoculants for improving desert soil fertility and agricultural potential.
Selvaraj Aravindh, Chinnappan Chinnadurai, and Dananjeyan Balachandar
SOIL, 6, 483–497, https://doi.org/10.5194/soil-6-483-2020, https://doi.org/10.5194/soil-6-483-2020, 2020
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Soil quality is important for functioning of the agricultural ecosystem to sustain productivity. It is combination of several physical, chemical, and biological attributes. In the present work, we developed a soil biological quality index, a sub-set of the soil quality index (SBQI) using six important biological variables. These variables were computed from long-term manurial experimental soils and transformed into a unitless 10-scaled SBQI. This will provide constraints of soil processes.
Frederick Büks, Nicolette Loes van Schaik, and Martin Kaupenjohann
SOIL, 6, 245–267, https://doi.org/10.5194/soil-6-245-2020, https://doi.org/10.5194/soil-6-245-2020, 2020
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Via anthropogenic input, microplastics (MPs) today represent a part of the soil organic matter. We analyzed studies on passive translocation, active ingestion, bioaccumulation and adverse effects of MPs on multicellular soil faunal life. These studies on a wide range of soil organisms found a recurring pattern of adverse effects on motility, growth, metabolism, reproduction, mortality and gut microbiome. However, the shape and type of the experimental MP often did not match natural conditions.
Karen A. Thompson, Bill Deen, and Kari E. Dunfield
SOIL, 2, 523–535, https://doi.org/10.5194/soil-2-523-2016, https://doi.org/10.5194/soil-2-523-2016, 2016
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Dedicated bioenergy crops are required for future energy production; however the effects of land use change from traditional crops to biofuel crops on soil microbial communities, which drive greenhouse gas production, are largely unknown. We used quantitative PCR to enumerate these microbial communities to assess the sustainability of different bioenergy crops, including miscanthus and corn. We found that miscanthus may be a suitable crop for bioenergy production in variable Ontario conditions.
Georgina Key, Mike G. Whitfield, Julia Cooper, Franciska T. De Vries, Martin Collison, Thanasis Dedousis, Richard Heathcote, Brendan Roth, Shamal Mohammed, Andrew Molyneux, Wim H. Van der Putten, Lynn V. Dicks, William J. Sutherland, and Richard D. Bardgett
SOIL, 2, 511–521, https://doi.org/10.5194/soil-2-511-2016, https://doi.org/10.5194/soil-2-511-2016, 2016
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Enhancing soil health is key to providing ecosystem services and food security. There are often trade-offs to using a particular practice, or it is not fully understood. This work aimed to identify practices beneficial to soil health and gaps in our knowledge. We reviewed existing research on agricultural practices and an expert panel assessed their effectiveness. The three most beneficial practices used a mix of organic or inorganic material, cover crops, or crop rotations.
Mohammed Ahmed, Melanie Sapp, Thomas Prior, Gerrit Karssen, and Matthew Alan Back
SOIL, 2, 257–270, https://doi.org/10.5194/soil-2-257-2016, https://doi.org/10.5194/soil-2-257-2016, 2016
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This review covers the history and advances made in the area of nematode taxonomy. It highlights the success and limitations of the classical approach to nematode taxonomy and provides reader with a bit of background to the applications of protein and DNA-based methods for identification nematodes. The review also outlines the pros and cons of the use of DNA barcoding in nematology and explains how DNA metabarcoding has been applied in nematology through next-generation sequencing.
E. Ashley Shaw, Karolien Denef, Cecilia Milano de Tomasel, M. Francesca Cotrufo, and Diana H. Wall
SOIL, 2, 199–210, https://doi.org/10.5194/soil-2-199-2016, https://doi.org/10.5194/soil-2-199-2016, 2016
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We investigated fire's effects on root decomposition and carbon (C) flow to the soil food web. We used 13C-labeled dead roots buried in microcosms constructed from two burn treatment soils (annual and infrequent burn). Our results showed greater root decomposition and C flow to the soil food web for the annual burn compared to infrequent burn treatment. Thus, roots are a more important C source for decomposers in annually burned areas where surface plant litter is frequently removed by fire.
E. Gagnarli, D. Goggioli, F. Tarchi, S. Guidi, R. Nannelli, N. Vignozzi, G. Valboa, M. R. Lottero, L. Corino, and S. Simoni
SOIL, 1, 527–536, https://doi.org/10.5194/soil-1-527-2015, https://doi.org/10.5194/soil-1-527-2015, 2015
M.-A. de Graaff, J. Adkins, P. Kardol, and H. L. Throop
SOIL, 1, 257–271, https://doi.org/10.5194/soil-1-257-2015, https://doi.org/10.5194/soil-1-257-2015, 2015
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Short summary
Modern agriculture is dominated by monoculture crop production, having negative effects on soil biology. We used a 12-year crop rotation experiment to examine the effects of increasing crop diversity on soil microorganisms and their activity. Crop rotations increased microbial biomass by up to 112 %, and increased potential ability to supply nitrogen as much as 58 %, compared to monoculture corn. Collectively, our findings show that soil health is increased when crop diversity is increased.
Modern agriculture is dominated by monoculture crop production, having negative effects on soil...