Mitigation of Greenhouse Gas Emissions from Rice via Manipulation of Key Root Traits

• Published in: Rice (New York, N.Y.) Vol. 16; no. 1; p. 24
• Main Authors: Jiménez, Juan de la Cruz, Pedersen, Ole
• Format: Journal Article
• Language: English
• Published: New York Springer US 10.05.2023; Springer Nature B.V; SpringerOpen
• Subjects: Aerenchyma; Agricultural practices; Agriculture; Anthropogenic factors; barrier to radial O2 loss; Biomedical and Life Sciences; Carbon dioxide; CH4; CO2; Crop production; Crop yield; Diffusion; Diffusion barriers; Emissions; Emissions control; Exploitation; Farm buildings; Fertilization; Gas production; Gas tightness; Greenhouse gases; Irrigation practices; Life Sciences; Methane; Methanotrophic bacteria; Microorganisms; Mitigation; N2O; Nitrification; Nitrous oxide; Oil and gas production; Oxidation; Plant Breeding/Biotechnology; Plant Ecology; Plant Genetics and Genomics; Plant nutrition; Plant Sciences; Review; Rhizosphere; Rice; Rice fields; Roots; loss; barrier to radial O; CH; oxidation; Aerenchyma; CO; N; O; N2O; barrier to radial O2 loss; CH4; CO2
• ISSN: 1939-8425; 1939-8433; 1934-8037
• DOI: 10.1186/s12284-023-00638-z

Rice production worldwide represents a major anthropogenic source of greenhouse gas emissions. Nitrogen fertilization and irrigation practices have been fundamental to achieve optimal rice yields, but these agricultural practices together with by-products from plants and microorganisms, facilitate the production, accumulation and venting of vast amounts of CO 2 , CH 4 and N 2 O. We propose that the development of elite rice varieties should target root traits enabling an effective internal O 2 diffusion, via enlarged aerenchyma channels. Moreover, gas tight barriers impeding radial O 2 loss in basal parts of the roots will increase O 2 diffusion to the root apex where molecular O 2 diffuses into the rhizosphere. These developments result in plants with roots penetrating deeper into the flooded anoxic soils, producing higher volumes of oxic conditions in the interface between roots and rhizosphere. Molecular O 2 in these zones promotes CH 4 oxidation into CO 2 by methanotrophs and nitrification (conversion of NH 4 + into NO 3 - ), reducing greenhouse gas production and at the same time improving plant nutrition. Moreover, roots with tight barriers to radial O 2 loss will have restricted diffusional entry of CH 4 produced in the anoxic parts of the rhizosphere and therefore plant-mediated diffusion will be reduced. In this review, we describe how the exploitation of these key root traits in rice can potentially reduce greenhouse gas emissions from paddy fields.