Elsevier

Plant Science

Volume 264, November 2017, Pages 48-56
Plant Science

Review article
Agricultural practices to improve nitrogen use efficiency through the use of arbuscular mycorrhizae: Basic and agronomic aspects

https://doi.org/10.1016/j.plantsci.2017.08.004Get rights and content

Highlights

  • Nitrogen cycling in agroecosystems is heavily dependent upon arbuscular mycorrhizal fungi present in the soil.

  • It is necessary to investigate which agricultural practices could be favorable to maximize the benefits of AMF in order to improve crop nitrogen use efficiency.

  • We describe how improving colonization by AMF though the reduction of soil perturbation could be helpful for increasing crop nitrogen use efficiency.

Abstract

Nitrogen cycling in agroecosystems is heavily dependent upon arbuscular mycorrhizal fungi (AMF) present in the soil microbiome. These fungi develop obligate symbioses with various host plant species, thus increasing their ability to acquire nutrients. However, AMF are particularly sensitive to physical, chemical and biological disturbances caused by human actions that limit their establishment. For a more sustainable agriculture, it will be necessary to further investigate which agricultural practices could be favorable to maximize the benefits of AMF to improve crop nitrogen use efficiency (NUE), thus reducing nitrogen (N) fertilizer usage. Direct seeding, mulch-based cropping systems prevent soil mycelium disruption and increase AMF propagule abundance. Such cropping systems lead to more efficient root colonization by AMF and thus a better establishment of the plant/fungal symbiosis. In addition, the use of continuous cover cropping systems can also enhance the formation of more efficient interconnected hyphal networks between mycorrhizae colonized plants. Taking into account both fundamental and agronomic aspects of mineral nutrition by plant/AMF symbioses, we have critically described, how improving fungal colonization through the reduction of soil perturbation and maintenance of an ecological balance could be helpful for increasing crop NUE.

Section snippets

The contribution of mycorrhizal fungi to plant nitrogen nutrition

Mineral fertilizers such as nitrogen (N) are presently the main source of nutrients applied to soils, even if the contribution of animal manure remains important in areas where there are livestock nearby. Following the Green Revolution in the 1960s, N fertilizers synthesized by the Haber–Bosch process have been used extensively to increase crop yield, allowing the production of food for nearly half of the world population [1].

Despite an almost ten-fold increase in the application of mineral N

The complexity of nutrient uptake in a plant-fungal symbiosis

Many excellent reviews have described extensively our current knowledge of the role of mycorrhizal fungi in the uptake of nutrients by plants, notably N [23] and P [24]. In these reviews it has been emphasized that AMF play an essential role in the nutrient uptake of the majority of land plants, including many important crop species. The contribution of the AMF symbiosis to P nutrition has focused on the interplay between direct P uptake via the roots and uptake via the AMF pathway.

Whether AMF

The roles of arbuscular mycorrhizal fungi in agroecosystems

The association between AMF and host plants is an ancient symbiosis that arose on the earth more than 400 million years ago [36]. Such associations are based upon a succession of biological events that can lead to a number of beneficial effects in both natural and agricultural ecosystems [37]. Mycorrhizal fungi can be involved in seedling growth [38], litter decomposition [39], and soil aggregation [40]. In this section, we will discuss the three main requirements necessary for the successful

Improving plant N uptake and utilization with arbuscular mycorrhizal fungi

The ability of AMF to increase nutrient uptake through the hyphal network offers an interesting strategy to limit the rather inefficient use of applied N by crops. AMF could play a useful role in the recycling of soil N by varying the availability of soil mineral N, through changes in the composition of the rhizosphere microbial community by modifying the development of denitrifying, nitrifying and diazotrophic symbiotic or free-living bacteria. This could be due to the changes in resources and

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