| Literature DB >> 32448964 |
Manoj Parihar1, Amitava Rakshit2, Vijay Singh Meena3, Vijai Kumar Gupta4, Kiran Rana5, Mahipal Choudhary3, Gopal Tiwari6, Pankaj Kumar Mishra3, Arunava Pattanayak3, Jaideep Kumar Bisht3, Surendra Singh Jatav2, Priyanka Khati3, Hanuman Singh Jatav2.
Abstract
Arbuscular mycorrhizal fungi (AMF) contribute predominantly to soil organic matter by creating a sink demand for plant C and distributing to below-ground hyphal biomass. The extra-radical hyphae along with glomalin-related soil protein significantly influence the soil carbon dynamics through their larger extent and turnover period need to discuss. The role of AMF is largely overlooked in terrestrial C cycling and climate change models despite their greater involvement in net primary productivity augmentation and further accumulation of this additional photosynthetic fixed C in the soil. However, this buffering mechanism against elevated CO2 condition to sequester extra C by AMF can be described only after considering their potential interaction with other microbes and associated mineral nutrients such as nitrogen cycling. In this article, we try to review the potential of AMF in C sequestration paving the way towards a better understanding of possible AMF mechanism by which C balance between biosphere and atmosphere can be moved forward in more positive direction.Entities:
Keywords: Carbon sequestration; Glomalin; Net primary productivity; Nutrient exchange; Soil nitrifiers
Year: 2020 PMID: 32448964 DOI: 10.1007/s00203-020-01915-x
Source DB: PubMed Journal: Arch Microbiol ISSN: 0302-8933 Impact factor: 2.552