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Muelbaier H, Arthen F, Collins G, Hickler T, Hohberg K, Lehmitz R, Pauchet Y, Pfenninger M, Potapov A, Romahn J, Schaefer I, Scheu S, Schneider C, Ebersberger I, Bálint M. Genomic evidence for the widespread presence of GH45 cellulases among soil invertebrates. Mol Ecol 2024:e17351. [PMID: 38712904 DOI: 10.1111/mec.17351] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/05/2023] [Revised: 12/06/2023] [Accepted: 02/26/2024] [Indexed: 05/08/2024]
Abstract
Lignocellulose is a major component of vascular plant biomass. Its decomposition is crucial for the terrestrial carbon cycle. Microorganisms are considered primary decomposers, but evidence increases that some invertebrates may also decompose lignocellulose. We investigated the taxonomic distribution and evolutionary origins of GH45 hydrolases, important enzymes for the decomposition of cellulose and hemicellulose, in a collection of soil invertebrate genomes. We found that these genes are common in springtails and oribatid mites. Phylogenetic analysis revealed that cellulase genes were acquired early in the evolutionary history of these groups. Domain architectures and predicted 3D enzyme structures indicate that these cellulases are functional. Patterns of presence and absence of these genes across different lineages prompt further investigation into their evolutionary and ecological benefits. The ubiquity of cellulase genes suggests that soil invertebrates may play a role in lignocellulose decomposition, independently or in synergy with microorganisms. Understanding the ecological and evolutionary implications might be crucial for understanding soil food webs and the carbon cycle.
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Affiliation(s)
- Hannah Muelbaier
- Applied Bioinformatics Group, Inst. of Cell Biology and Neuroscience, Goethe University, Frankfurt am Main, Germany
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
| | - Freya Arthen
- Applied Bioinformatics Group, Inst. of Cell Biology and Neuroscience, Goethe University, Frankfurt am Main, Germany
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
| | - Gemma Collins
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
- Manaaki Whenua - Landcare Research, Auckland, New Zealand
| | - Thomas Hickler
- Senckenberg Biodiversity and Climate Research Centre, Frankfurt am Main, Germany
- Department of Physical Geography, Goethe University, Frankfurt/Main, Germany
| | - Karin Hohberg
- Senckenberg Museum of Natural History Görlitz, Görlitz, Germany
| | - Ricarda Lehmitz
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
- Senckenberg Museum of Natural History Görlitz, Görlitz, Germany
| | - Yannick Pauchet
- Insect Symbiosis, Max Planck Institute for Chemical Ecology, Jena, Germany
| | - Markus Pfenninger
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
- Senckenberg Biodiversity and Climate Research Centre, Frankfurt am Main, Germany
- Institute for Molecular and Organismic Evolution, Johannes Gutenberg University, Mainz, Germany
| | - Anton Potapov
- Senckenberg Museum for Natural History Görlitz, Görlitz, Germany
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Leipzig, Germany
- International Institute Zittau, TUD Dresden University of Technology, Zittau, Germany
| | - Juliane Romahn
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
- Senckenberg Biodiversity and Climate Research Centre, Frankfurt am Main, Germany
- Institute of Insect Biotechnology, Justus-Liebig University, Giessen, Germany
| | - Ina Schaefer
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
- Senckenberg Biodiversity and Climate Research Centre, Frankfurt am Main, Germany
- Animal Ecology, University of Goettingen, Goettingen, Germany
| | - Stefan Scheu
- J.F. Blumenbach Institute of Zoology and Anthropology, University of Goettingen, Goettingen, Germany
| | - Clément Schneider
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
- Senckenberg Museum of Natural History Görlitz, Görlitz, Germany
| | - Ingo Ebersberger
- Applied Bioinformatics Group, Inst. of Cell Biology and Neuroscience, Goethe University, Frankfurt am Main, Germany
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
- Senckenberg Biodiversity and Climate Research Centre, Frankfurt am Main, Germany
| | - Miklós Bálint
- LOEWE Centre for Translational Biodiversity Genomics, Frankfurt am Main, Germany
- Senckenberg Biodiversity and Climate Research Centre, Frankfurt am Main, Germany
- Institute of Insect Biotechnology, Justus-Liebig University, Giessen, Germany
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Zubkova EV, Frolov PV, Bykhovets SS, Nadporozhskaya MA, Frolova GG. Bilberry and Lingonberry Cenopopulation Mosaic Structures and Soil Organic Matter Dynamics in Southern Moscow Region Pine Stands. CONTEMP PROBL ECOL+ 2022. [DOI: 10.1134/s199542552207023x] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/29/2022]
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Chertov O, Kuzyakov Y, Priputina I, Frolov P, Shanin V, Grabarnik P. Modelling the Rhizosphere Priming Effect in Combination with Soil Food Webs to Quantify Interaction between Living Plant, Soil Biota and Soil Organic Matter. PLANTS (BASEL, SWITZERLAND) 2022; 11:2605. [PMID: 36235471 PMCID: PMC9572548 DOI: 10.3390/plants11192605] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 07/15/2022] [Revised: 09/26/2022] [Accepted: 09/29/2022] [Indexed: 06/16/2023]
Abstract
A model of rhizosphere priming effect under impact of root exudate input into rhizosphere soil was developed as an important process of the plant-soil interaction. The model was based on the concept of nitrogen (N) mining, compensating for the N scarcity in exudates for microbial growth by accelerating SOM mineralisation. In the model, N deficiency for microbial growth is covered ("mined") by the increased SOM mineralisation depending on the C:N ratio of the soil and exudates. The new aspect in the model is a food web procedure, which calculates soil fauna feeding on microorganisms, the return of faunal by-products to SOM and mineral N production for root uptake. The model verification demonstrated similar magnitude of the priming effect in simulations as in the published experimental data. Model testing revealed high sensitivity of the simulation results to N content in exudates. Simulated CO2 emission from the priming can reach 10-40% of CO2 emission from the whole Ah horizon of boreal forest soil depending on root exudation rates. This modeling approach with including food web activity allows quantifying wider aspects of the priming effect functioning including ecologically important available N production.
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Affiliation(s)
- Oleg Chertov
- Department of Natural Sciences, Bingen University of Applied Sciences, Berlin Str. 109, 55411 Bingen, Germany
| | - Yakov Kuzyakov
- Department of Soil Science of Temperate Ecosystems, Department of Agricultural Soil Science, Georg-August-Universität Göttingen, Büsgenweg 2, 37077 Göttingen, Germany
- Agro-Technological Institute, RUDN University, 117198 Moscow, Russia
| | - Irina Priputina
- Institute of Physicochemical and Biological Problems in Soil Science, Pushchino Scientific Center for Biological Research of the Russian Academy of Sciences, Institutskaya 2, 142290 Pushchino, Russia
| | - Pavel Frolov
- Institute of Physicochemical and Biological Problems in Soil Science, Pushchino Scientific Center for Biological Research of the Russian Academy of Sciences, Institutskaya 2, 142290 Pushchino, Russia
| | - Vladimir Shanin
- Institute of Physicochemical and Biological Problems in Soil Science, Pushchino Scientific Center for Biological Research of the Russian Academy of Sciences, Institutskaya 2, 142290 Pushchino, Russia
- Center for Forest Ecology and Productivity of the Russian Academy of Sciences, Profsoyuznaya st., 84/32, bld. 14, 117997 Moscow, Russia
| | - Pavel Grabarnik
- Institute of Physicochemical and Biological Problems in Soil Science, Pushchino Scientific Center for Biological Research of the Russian Academy of Sciences, Institutskaya 2, 142290 Pushchino, Russia
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Potapov AM. Multifunctionality of belowground food webs: resource, size and spatial energy channels. Biol Rev Camb Philos Soc 2022; 97:1691-1711. [PMID: 35393748 DOI: 10.1111/brv.12857] [Citation(s) in RCA: 16] [Impact Index Per Article: 8.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/21/2021] [Revised: 03/25/2022] [Accepted: 03/28/2022] [Indexed: 01/17/2023]
Abstract
The belowground compartment of terrestrial ecosystems drives nutrient cycling, the decomposition and stabilisation of organic matter, and supports aboveground life. Belowground consumers create complex food webs that regulate functioning, ensure stability and support biodiversity both below and above ground. However, existing soil food-web reconstructions do not match recently accumulated empirical evidence and there is no comprehensive reproducible approach that accounts for the complex resource, size and spatial structure of food webs in soil. Here I build on generic food-web organisation principles and use multifunctional classification of soil protists, invertebrates and vertebrates, to reconstruct a 'multichannel' food web across size classes of soil-associated consumers. I infer weighted trophic interactions among trophic guilds using feeding preferences and prey protection traits (evolutionarily inherited traits), size and spatial distributions (niche overlaps), and biomass-dependent feeding. I then use food-web reconstruction, together with assimilation efficiencies, to calculate energy fluxes assuming a steady-state energetic system. Based on energy fluxes, I propose a number of indicators, related to stability, biodiversity and multiple ecosystem-level functions such as herbivory, top-down control, translocation and transformation of organic matter. I illustrate this approach with an empirical example, comparing it with traditional resource-focused soil food-web reconstruction. The multichannel reconstruction can be used to assess 'trophic multifunctionality' (analogous to ecosystem multifunctionality), i.e. simultaneous support of multiple trophic functions by the food web, and compare it across communities and ecosystems spanning beyond the soil. With further empirical validation of the proposed functional indicators, this multichannel reconstruction approach could provide an effective tool for understanding animal diversity-ecosystem functioning relationships in soil. This tool hopefully will inspire more researchers to describe soil communities and belowground-aboveground interactions comprehensively. Such studies will provide informative indicators for including consumers as active agents in biogeochemical models, not only locally but also on regional and global scales.
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Affiliation(s)
- Anton M Potapov
- Johann Friedrich Blumenbach Institute of Zoology and Anthropology, Animal Ecology, University of Göttingen, Untere Karspüle 2, 37073, Göttingen, Germany.,A.N. Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Leninsky Prospect 33, 119071, Moscow
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Deckmyn G, Flores O, Mayer M, Domene X, Schnepf A, Kuka K, Van Looy K, Rasse DP, Briones MJ, Barot S, Berg M, Vanguelova E, Ostonen I, Vereecken H, Suz LM, Frey B, Frossard A, Tiunov A, Frouz J, Grebenc T, Öpik M, Javaux M, Uvarov A, Vindušková O, Henning Krogh P, Franklin O, Jiménez J, Curiel Yuste J. KEYLINK: towards a more integrative soil representation for inclusion in ecosystem scale models. I. review and model concept. PeerJ 2020; 8:e9750. [PMID: 32974092 PMCID: PMC7486829 DOI: 10.7717/peerj.9750] [Citation(s) in RCA: 14] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/11/2020] [Accepted: 07/27/2020] [Indexed: 11/20/2022] Open
Abstract
The relatively poor simulation of the below-ground processes is a severe drawback for many ecosystem models, especially when predicting responses to climate change and management. For a meaningful estimation of ecosystem production and the cycling of water, energy, nutrients and carbon, the integration of soil processes and the exchanges at the surface is crucial. It is increasingly recognized that soil biota play an important role in soil organic carbon and nutrient cycling, shaping soil structure and hydrological properties through their activity, and in water and nutrient uptake by plants through mycorrhizal processes. In this article, we review the main soil biological actors (microbiota, fauna and roots) and their effects on soil functioning. We review to what extent they have been included in soil models and propose which of them could be included in ecosystem models. We show that the model representation of the soil food web, the impact of soil ecosystem engineers on soil structure and the related effects on hydrology and soil organic matter (SOM) stabilization are key issues in improving ecosystem-scale soil representation in models. Finally, we describe a new core model concept (KEYLINK) that integrates insights from SOM models, structural models and food web models to simulate the living soil at an ecosystem scale.
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Affiliation(s)
- Gaby Deckmyn
- Department of Biology, Plants and Ecosystems (PLECO), Universiteit Antwerpen, Antwerpen, Belgium
| | - Omar Flores
- Department of Biology, Plants and Ecosystems (PLECO), Universiteit Antwerpen, Antwerpen, Belgium
- Biogeography and Global Change, National Museum of Natural Sciences-Spanish National Research Council (MNCN-CSIC), Madrid, Spain
| | - Mathias Mayer
- Institute of Forest Ecology, Department of Forest and Soil Sciences, University of Natural Resources and Life Sciences (BOKU), Vienna, Austria
- Biogeochemistry Group, Forest Soils and Biogeochemistry, Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
| | - Xavier Domene
- CREAF, Cerdanyola del Vallès, Spain
- Universitat Autònoma de Barcelona, Cerdanyola del Vallès, Spain
| | - Andrea Schnepf
- Agrosphere Institute, IBG, Forschungszentrum Jülich GmbH, Jülich, Germany
| | - Katrin Kuka
- Institute for Crop and Soil Science, Julius Kühn-Institut (JKI), Braunschwei, Germany
| | - Kris Van Looy
- OVAM, Flemish Institute for Materials and Soils, Mechelen, Belgium
| | - Daniel P. Rasse
- Department of Biogeochemistry and Soil Quality, Norwegian Institute of Bioeconomy Research (NIBIO), Aas, Norway
| | - Maria J.I. Briones
- Departamento de Ecología y Biología Animal, Universidad de Vigo, Vigo, Spain
| | - Sébastien Barot
- Institute of Ecology and Environmental Sciences, IRD, UPEC, CNRS, INRA, Sorbonne Université, Paris, France
| | - Matty Berg
- Department of Ecological Science, Vrije Universiteit Amsterdam, Amsterdam, Netherlands
- Groningen Institute for Evolutionary Life Sciences, University of Groningen, Groningen, Netherlands
| | | | - Ivika Ostonen
- Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia
| | - Harry Vereecken
- Agrosphere Institute, IBG, Forschungszentrum Jülich GmbH, Jülich, Germany
| | - Laura M. Suz
- Comparative Plant and Fungal Biology, Royal Botanic Gardens, Kew, London, UK
| | - Beat Frey
- Forest Soils and Biogeochemistry, Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
| | - Aline Frossard
- Forest Soils and Biogeochemistry, Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
| | - Alexei Tiunov
- A.N. Severtsov Institute of Ecology and Evolution RAS, Moscow, Russia
| | - Jan Frouz
- Institute for Environmental Studies, Charles University, Prague, Czech Republic
| | - Tine Grebenc
- Slovenian Forestry Institute, Ljubljana, Slovenia
| | - Maarja Öpik
- Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia
| | - Mathieu Javaux
- Agrosphere Institute, IBG, Forschungszentrum Jülich GmbH, Jülich, Germany
- Earth and Life Institute, UCLouvain, Louvain-la-Neuve, Belgium
| | - Alexei Uvarov
- A.N. Severtsov Institute of Ecology and Evolution RAS, Moscow, Russia
| | - Olga Vindušková
- Department of Biology, Plants and Ecosystems (PLECO), Universiteit Antwerpen, Antwerpen, Belgium
| | | | - Oskar Franklin
- Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umeå, Sweden
- International Institute for Applied Systems Analysis IIASA, Laxenburg, Austria
| | - Juan Jiménez
- Department of Biodiversity Conservation and Ecosystem Restoration, ARAID/IPE-CSIC, Jaca, Spain
| | - Jorge Curiel Yuste
- BC3-Basque Centre for Climate Change, Scientific Campus of the University of the Basque Country, Bilbao, Bizkaia, Spain
- IKERBASQUE, Basque Foundation for Science, Bilbao, Spain
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Frolov P, Zubkova E, Shanin V, Bykhovets S, Mäkipää R, Salemaa M. CAMPUS-S – The model of ground layer vegetation populations in forest ecosystems and their contribution to the dynamics of carbon and nitrogen. II. Parameterization, validation and simulation experiments. Ecol Modell 2020. [DOI: 10.1016/j.ecolmodel.2020.109183] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/24/2022]
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CAMPUS-S – The model of ground layer vegetation populations in forest ecosystems and their contribution to the dynamics of carbon and nitrogen. I. Problem formulation and description of the model. Ecol Modell 2020. [DOI: 10.1016/j.ecolmodel.2020.109184] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/19/2022]
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Rinne‐Garmston KT, Peltoniemi K, Chen J, Peltoniemi M, Fritze H, Mäkipää R. Carbon flux from decomposing wood and its dependency on temperature, wood N 2 fixation rate, moisture and fungal composition in a Norway spruce forest. GLOBAL CHANGE BIOLOGY 2019; 25:1852-1867. [PMID: 30767385 PMCID: PMC6849867 DOI: 10.1111/gcb.14594] [Citation(s) in RCA: 17] [Impact Index Per Article: 3.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/01/2018] [Accepted: 01/21/2019] [Indexed: 05/23/2023]
Abstract
Globally 40-70 Pg of carbon (C) are stored in coarse woody debris on the forest floor. Climate change may reduce the function of this stock as a C sink in the future due to increasing temperature. However, current knowledge on the drivers of wood decomposition is inadequate for detailed predictions. To define the factors that control wood respiration rate of Norway spruce and to produce a model that adequately describes the decomposition process of this species as a function of time, we used an unprecedentedly diverse analytical approach, which included measurements of respiration, fungal community sequencing, N2 fixation rate, nifH copy number, 14 C-dating as well as N%, δ13 C and C% values of wood. Our results suggest that climate change will accelerate C flux from deadwood in boreal conditions, due to the observed strong temperature dependency of deadwood respiration. At the research site, the annual C flux from deadwood would increase by 27% from the current 117 g C/kg wood with the projected climate warming (RCP4.5). The second most important control on respiration rate was the stage of wood decomposition; at early stages of decomposition low nitrogen content and low wood moisture limited fungal activity while reduced wood resource quality decreased the respiration rate at the final stages of decomposition. Wood decomposition process was best described by a Sigmoidal model, where after 116 years of wood decomposition mass loss of 95% was reached. Our results on deadwood decomposition are important for C budget calculations in ecosystem and climate change models. We observed for the first time that the temperature dependency of N2 fixation, which has a major role at providing N for wood-inhabiting fungi, was not constant but varied between wood density classes due to source supply and wood quality. This has significant consequences on projecting N2 fixation rates for deadwood in changing climate.
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Affiliation(s)
| | | | - Janet Chen
- Natural Resources Institute Finland (Luke)HelsinkiFinland
| | | | - Hannu Fritze
- Natural Resources Institute Finland (Luke)HelsinkiFinland
| | - Raisa Mäkipää
- Natural Resources Institute Finland (Luke)HelsinkiFinland
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Mulder C, Maas R. Unifying the functional diversity in natural and cultivated soils using the overall body-mass distribution of nematodes. BMC Ecol 2017; 17:36. [PMID: 29183362 PMCID: PMC5706308 DOI: 10.1186/s12898-017-0145-9] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.1] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/27/2017] [Accepted: 11/02/2017] [Indexed: 11/10/2022] Open
Abstract
BACKGROUND Sustainable use of our soils is a key goal for environmental protection. As many ecosystem services are supported belowground at different trophic levels by nematodes, soil nematodes are expected to provide objective metrics for biological quality to integrate physical and chemical soil variables. Trait measurements of body mass carried out at the individual level can in this way be correlated with environmental properties that influence the performance of soil biota. RESULTS Soil samples were collected across 200 sites (4 soil types and 5 land-use types resulting in 9 combinations) during a long-term monitoring programme in the Netherlands and the functional diversity of nematode communities was investigated. Using three commonly used functional diversity indices applicable to single traits (Divergence, Evenness and Richness), a unified index of overall body-mass distribution is proposed to better illustrate the application of functional metrics as a descriptor of land use. Effects of land use and soil chemistry on the functional diversity of nematodes were demonstrated and a combination of environmental factors accounts for the low functional value of Scots Pine forest soils in comparison to the high functional value of heathland soils, whereas human factors account for the low functional and chemical values of arable fields. CONCLUSIONS These findings show an unexpected high functional vulnerability of nematodes inhabiting clay-rich soils in comparison to sandy soils and support the notion that soil C:N ratio is a major driver of biodiversity. The higher the C:N ratio, the higher the overall diversity, as soil nematodes cope better with nutrient-poor agroecosystems under less intense fertilization. A trait-based way focusing on size distribution of nematodes is proposed to maintain environmental health by monitoring the overall diversity in soil biota, keeping agriculture and forestry sustainable.
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Affiliation(s)
- Christian Mulder
- National Institute for Public Health and the Environment (RIVM), Bilthoven, The Netherlands.
| | - Rob Maas
- National Institute for Public Health and the Environment (RIVM), Bilthoven, The Netherlands
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