Plant-microbe-soil interactions in the rhizosphere: an evolutionary perspective
Soils are the product of the activities of plants, which supply organic matter and play a pivotal role in weathering rocks and minerals. Many plant species have a distinct ecological amplitude that shows restriction to specific soil types. In the numerous interactions between plants and soil, micro-...
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| Published in | Plant and soil Vol. 321; no. 1/2; pp. 83 - 115 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article Conference Proceeding |
| Language | English |
| Published |
Dordrecht
Springer
01.08.2009
Springer Netherlands Springer Nature B.V Springer Verlag |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Soils are the product of the activities of plants, which supply organic matter and play a pivotal role in weathering rocks and minerals. Many plant species have a distinct ecological amplitude that shows restriction to specific soil types. In the numerous interactions between plants and soil, micro-organisms also play a key role. Here we review the existing literature on interactions between plants, microorganisms and soils, and include considerations of evolutionary time scales, where possible. Some of these interactions involve intricate systems of communication, which in the case of symbioses such as the arbuscular mycorrhizal symbiosis are several hundreds of millions years old; others involve the release of exudates from roots, and other products of rhizodeposition that are used as substrates for soil microorganisms. The possible reasons for the survival value of this loss of carbon over tens or hundreds of millions of years of evolution of higher plants are discussed, taking a cost-benefit approach. Coevolution of plants and rhizosphere microorganisms is discussed, in the light of known ecological interactions between various partners in terrestrial ecosystems. Finally, the role of higher plants, especially deep-rooted plants and associated microorganisms in the weathering of rocks and minerals, ultimately contributing to pedogenesis, is addressed. We show that rhizosphere processes in the long run are central to biogeochemical cycles, soil formation and Earth history. Major anticipated discoveries will enhance our basic understanding and allow applications of new knowledge to deal with nutrient deficiencies, pests and diseases, and the challenges of increasing global food production and agroecosystem productivity in an environmentally responsible manner. |
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| AbstractList | Soils are the product of the activities of plants, which supply organic matter and play a pivotal role in weathering rocks and minerals. Many plant species have a distinct ecological amplitude that shows restriction to specific soil types. In the numerous interactions between plants and soil, microorganisms also play a key role. Here we review the existing literature on interactions between plants, microorganisms and soils, and include considerations of evolutionary time scales, where possible. Some of these interactions involve intricate systems of communication, which in the case of symbioses such as the arbuscular mycorrhizal symbiosis are several hundreds of millions years old; others involve the release of exudates from roots, and other products of rhizodeposition that are used as substrates for soil microorganisms. The possible reasons for the survival value of this loss of carbon over tens or hundreds of millions of years of evolution of higher plants are discussed, taking a cost-benefit approach. Co-evolution of plants and rhizosphere microorganisms is discussed, in the light of known ecological interactions between various partners in terrestrial ecosystems. Finally, the role of higher plants, especially deep-rooted plants and associated microorganisms in the weathering of rocks and minerals, ultimately contributing to pedogenesis, is addressed. We show that rhizosphere processes in the long run are central to biogeochemical cycles, soil formation and Earth history. Major anticipated discoveries will enhance our basic understanding and allow applications of new knowledge to deal with nutrient deficiencies, pests and diseases, and the challenges of increasing global food production and agroecosystem productivity in an environmentally responsible manner. Soils are the product of the activities of plants, which supply organic matter and play a pivotal role in weathering rocks and minerals. Many plant species have a distinct ecological amplitude that shows restriction to specific soil types. In the numerous interactions between plants and soil, microorganisms also play a key role. Here we review the existing literature on interactions between plants, microorganisms and soils, and include considerations of evolutionary time scales, where possible. Some of these interactions involve intricate systems of communication, which in the case of symbioses such as the arbuscular mycorrhizal symbiosis are several hundreds of millions years old; others involve the release of exudates from roots, and other products of rhizodeposition that are used as substrates for soil microorganisms. The possible reasons for the survival value of this loss of carbon over tens or hundreds of millions of years of evolution of higher plants are discussed, taking a cost-benefit approach. Co-evolution of plants and rhizosphere microorganisms is discussed, in the light of known ecological interactions between various partners in terrestrial ecosystems. Finally, the role of higher plants, especially deep-rooted plants and associated microorganisms in the weathering of rocks and minerals, ultimately contributing to pedogenesis, is addressed. We show that rhizosphere processes in the long run are central to biogeochemical cycles, soil formation and Earth history. Major anticipated discoveries will enhance our basic understanding and allow applications of new knowledge to deal with nutrient deficiencies, pests and diseases, and the challenges of increasing global food production and agroecosystem productivity in an environmentally responsible manner Issue Title: Special Issue: Rhizosphere: achievements and challenges/Guest Edited by Yves Dessaux, Philippe Hinsinger and Philippe Lemanceau Soils are the product of the activities of plants, which supply organic matter and play a pivotal role in weathering rocks and minerals. Many plant species have a distinct ecological amplitude that shows restriction to specific soil types. In the numerous interactions between plants and soil, microorganisms also play a key role. Here we review the existing literature on interactions between plants, microorganisms and soils, and include considerations of evolutionary time scales, where possible. Some of these interactions involve intricate systems of communication, which in the case of symbioses such as the arbuscular mycorrhizal symbiosis are several hundreds of millions years old; others involve the release of exudates from roots, and other products of rhizodeposition that are used as substrates for soil microorganisms. The possible reasons for the survival value of this loss of carbon over tens or hundreds of millions of years of evolution of higher plants are discussed, taking a cost-benefit approach. Co-evolution of plants and rhizosphere microorganisms is discussed, in the light of known ecological interactions between various partners in terrestrial ecosystems. Finally, the role of higher plants, especially deep-rooted plants and associated microorganisms in the weathering of rocks and minerals, ultimately contributing to pedogenesis, is addressed. We show that rhizosphere processes in the long run are central to biogeochemical cycles, soil formation and Earth history. Major anticipated discoveries will enhance our basic understanding and allow applications of new knowledge to deal with nutrient deficiencies, pests and diseases, and the challenges of increasing global food production and agroecosystem productivity in an environmentally responsible manner. [PUBLICATION ABSTRACT] Soils are the product of the activities of plants, which supply organic matter and play a pivotal role in weathering rocks and minerals. Many plant species have a distinct ecological amplitude that shows restriction to specific soil types. In the numerous interactions between plants and soil, micro-organisms also play a key role. Here we review the existing literature on interactions between plants, microorganisms and soils, and include considerations of evolutionary time scales, where possible. Some of these interactions involve intricate systems of communication, which in the case of symbioses such as the arbuscular mycorrhizal symbiosis are several hundreds of millions years old; others involve the release of exudates from roots, and other products of rhizodeposition that are used as substrates for soil microorganisms. The possible reasons for the survival value of this loss of carbon over tens or hundreds of millions of years of evolution of higher plants are discussed, taking a cost-benefit approach. Coevolution of plants and rhizosphere microorganisms is discussed, in the light of known ecological interactions between various partners in terrestrial ecosystems. Finally, the role of higher plants, especially deep-rooted plants and associated microorganisms in the weathering of rocks and minerals, ultimately contributing to pedogenesis, is addressed. We show that rhizosphere processes in the long run are central to biogeochemical cycles, soil formation and Earth history. Major anticipated discoveries will enhance our basic understanding and allow applications of new knowledge to deal with nutrient deficiencies, pests and diseases, and the challenges of increasing global food production and agroecosystem productivity in an environmentally responsible manner. |
| Author | Lambers, Hans Mougel, Christophe Jaillard, Benoît Hinsinger, Philippe |
| Author_xml | – sequence: 1 givenname: Hans surname: Lambers fullname: Lambers, Hans – sequence: 2 givenname: Christophe surname: Mougel fullname: Mougel, Christophe – sequence: 3 givenname: Benoît surname: Jaillard fullname: Jaillard, Benoît – sequence: 4 givenname: Philippe surname: Hinsinger fullname: Hinsinger, Philippe |
| BackLink | http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=21938498$$DView record in Pascal Francis https://hal.inrae.fr/hal-02665203$$DView record in HAL |
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| ISSN | 0032-079X |
| IngestDate | Fri May 09 12:17:57 EDT 2025 Tue Aug 05 11:01:35 EDT 2025 Fri Jul 25 11:18:28 EDT 2025 Mon Jul 21 09:11:25 EDT 2025 Thu Apr 24 23:00:20 EDT 2025 Tue Jul 01 00:58:44 EDT 2025 Fri Feb 21 02:33:29 EST 2025 Sun Aug 24 12:10:21 EDT 2025 |
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| IsScholarly | true |
| Issue | 1/2 |
| Keywords | Pedogenesis Symbiosis Rhizosphere Biogeochemistry Rhizodeposition Weathering Evolution Nutrient acquisition Root exudation Rhizodeposit Root Acquisition Vegetative apparatus Soil genesis Nutrient Exudation Microorganism Soil plant relation WEATHERING ROOT EXUDATION NUTRIENT ACQUISITION EVOLUTION BIOGEOCHEMISTRY PEDOGENESIS RHIZODEPOSITION RHIZOSPHERE SYMBIOSIS RELATION PLANTE-SOL |
| Language | English |
| License | http://www.springer.com/tdm CC BY 4.0 Distributed under a Creative Commons Attribution 4.0 International License: http://creativecommons.org/licenses/by/4.0 |
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| MeetingName | Rhizosphere: achievements and challenges |
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| PublicationDate | 2009-08-01 |
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| PublicationPlace | Dordrecht |
| PublicationPlace_xml | – name: Dordrecht |
| PublicationSubtitle | An International Journal on Plant-Soil Relationships |
| PublicationTitle | Plant and soil |
| PublicationTitleAbbrev | Plant Soil |
| PublicationYear | 2009 |
| Publisher | Springer Springer Netherlands Springer Nature B.V Springer Verlag |
| Publisher_xml | – name: Springer – name: Springer Netherlands – name: Springer Nature B.V – name: Springer Verlag |
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| Snippet | Soils are the product of the activities of plants, which supply organic matter and play a pivotal role in weathering rocks and minerals. Many plant species... Issue Title: Special Issue: Rhizosphere: achievements and challenges/Guest Edited by Yves Dessaux, Philippe Hinsinger and Philippe Lemanceau Soils are the... |
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| SubjectTerms | Acid soils Agricultural ecosystems Agronomy. Soil science and plant productions Animal, plant and microbial ecology Biogeochemical cycles Biological and medical sciences Biomedical and Life Sciences carbon Clay soils communications technology Ecology ecosystems evolution Evolutionary biology Food production Forest soils Fundamental and applied biological sciences. Psychology General agronomy. Plant production Geochemistry Life Sciences Microorganisms Minerals nutrient deficiencies Nutrients Organic matter Pedogenesis pests Plant biology Plant Physiology Plant roots Plant Sciences Plant species Plants REVIEW ARTICLE rhizodeposition Rhizosphere Rocks roots Soil ecology Soil formation Soil genesis Soil microorganisms Soil science Soil Science & Conservation Soil surveys, classification and mapping, soil genesis Soil types Soil-plant relationships. Soil fertility Soil-plant relationships. Soil fertility. Fertilization. Amendments Symbiosis Terrestrial ecosystems Vegetal Biology vesicular arbuscular mycorrhizae Weathering |
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| Title | Plant-microbe-soil interactions in the rhizosphere: an evolutionary perspective |
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