Glomalin and Contribution of Glomalin to Carbon Sequestration in Soil: A Review

Arbuscular mycorrhizal fungi (AMF) improves the uptake of nutrients and water to the plants through mutual symbiosis. Only AMF produces glomalin related soil protein (GRSP). Acaulospora morroaiae, Glomus luteum, Glomus verruculosum, Glomus versiforme are the effective glomalin producing AMFs. Mixed...

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Main Author: MD. Belal Hossain
Format: Article
Language:English
Published: Turkish Science and Technology Publishing (TURSTEP) 2021-01-01
Series:Turkish Journal of Agriculture: Food Science and Technology
Subjects:
Online Access:http://www.agrifoodscience.com/index.php/TURJAF/article/view/3803
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spelling doaj-744317e339d04fcd9b0b09e040f7dd182021-03-31T07:33:34ZengTurkish Science and Technology Publishing (TURSTEP)Turkish Journal of Agriculture: Food Science and Technology2148-127X2021-01-019119119610.24925/turjaf.v9i1.191-196.38031965Glomalin and Contribution of Glomalin to Carbon Sequestration in Soil: A ReviewMD. Belal Hossain0Soil Science Division, Bangladesh Institute of Nuclear Agriculture (BINA), Bangladesh Agricultural University campus, Mymensingh 2202Arbuscular mycorrhizal fungi (AMF) improves the uptake of nutrients and water to the plants through mutual symbiosis. Only AMF produces glomalin related soil protein (GRSP). Acaulospora morroaiae, Glomus luteum, Glomus verruculosum, Glomus versiforme are the effective glomalin producing AMFs. Mixed primary forest, tropical rainforest, soil organic matter, clay soil, no tillage, quality and quantity of fertilizers, crop rotation, and water stable aggregates are also suitable to increase glomalin production. Glomalin is a glycoprotein that contains 30–40% carbon (C) which is assumed to be stable and persistent in soil. The glomalin can sequestrate more carbon in the soil due to its high carbon and aggregate stability. Greater aggregate stability leads to high organic carbon protection in terrestrial ecosystems. The lowest glomalin content (0.007 mg per gram soil) was found in Antarctic region, and the highest glomalin content (13.50 mg per gram soil) was observed in tropical rainforest. In agricultural soil, glomalin content varies between 0.30 and 0.70 mg per gram soil. The GRSP containing soil organic carbon (SOC) in deeper soil layers was 1.34 to 1.50 times higher than in surface layers. Glomalin can sequestrate 0.24 Mg C ha-1 in soil when present at 1.10±0.04 mg g-1. At elevated CO2 (700 µmol mol-1) level, easily extractable glomalin (EEG) and total glomalin (TG) were 2.76 and 5.67% SOC in the surface soil layer over ambient carbon dioxide (CO2) level. This finding indicates the effective function of GRSP C sequestration in soil under global environmental change scenarios. Glomalin can also protect labile carbon that can help regulating nutrient supply to the plants. No tillage practice causes higher AMF hyphal length, GRSP and water stable aggregate (WSA) compared to that of conventional tillage practice. The current review demonstrated that GRSP is an important tool for carbon storage in deep soils. Glomalin mediates soil aggregates, improves soil quality, increases carbon sequestration and crop production, and mitigates climate change.http://www.agrifoodscience.com/index.php/TURJAF/article/view/3803mycorrhizal fungi speciesglomalinglomalin carbon poolssoil aggregate formationcarbon sequestration
collection DOAJ
language English
format Article
sources DOAJ
author MD. Belal Hossain
spellingShingle MD. Belal Hossain
Glomalin and Contribution of Glomalin to Carbon Sequestration in Soil: A Review
Turkish Journal of Agriculture: Food Science and Technology
mycorrhizal fungi species
glomalin
glomalin carbon pools
soil aggregate formation
carbon sequestration
author_facet MD. Belal Hossain
author_sort MD. Belal Hossain
title Glomalin and Contribution of Glomalin to Carbon Sequestration in Soil: A Review
title_short Glomalin and Contribution of Glomalin to Carbon Sequestration in Soil: A Review
title_full Glomalin and Contribution of Glomalin to Carbon Sequestration in Soil: A Review
title_fullStr Glomalin and Contribution of Glomalin to Carbon Sequestration in Soil: A Review
title_full_unstemmed Glomalin and Contribution of Glomalin to Carbon Sequestration in Soil: A Review
title_sort glomalin and contribution of glomalin to carbon sequestration in soil: a review
publisher Turkish Science and Technology Publishing (TURSTEP)
series Turkish Journal of Agriculture: Food Science and Technology
issn 2148-127X
publishDate 2021-01-01
description Arbuscular mycorrhizal fungi (AMF) improves the uptake of nutrients and water to the plants through mutual symbiosis. Only AMF produces glomalin related soil protein (GRSP). Acaulospora morroaiae, Glomus luteum, Glomus verruculosum, Glomus versiforme are the effective glomalin producing AMFs. Mixed primary forest, tropical rainforest, soil organic matter, clay soil, no tillage, quality and quantity of fertilizers, crop rotation, and water stable aggregates are also suitable to increase glomalin production. Glomalin is a glycoprotein that contains 30–40% carbon (C) which is assumed to be stable and persistent in soil. The glomalin can sequestrate more carbon in the soil due to its high carbon and aggregate stability. Greater aggregate stability leads to high organic carbon protection in terrestrial ecosystems. The lowest glomalin content (0.007 mg per gram soil) was found in Antarctic region, and the highest glomalin content (13.50 mg per gram soil) was observed in tropical rainforest. In agricultural soil, glomalin content varies between 0.30 and 0.70 mg per gram soil. The GRSP containing soil organic carbon (SOC) in deeper soil layers was 1.34 to 1.50 times higher than in surface layers. Glomalin can sequestrate 0.24 Mg C ha-1 in soil when present at 1.10±0.04 mg g-1. At elevated CO2 (700 µmol mol-1) level, easily extractable glomalin (EEG) and total glomalin (TG) were 2.76 and 5.67% SOC in the surface soil layer over ambient carbon dioxide (CO2) level. This finding indicates the effective function of GRSP C sequestration in soil under global environmental change scenarios. Glomalin can also protect labile carbon that can help regulating nutrient supply to the plants. No tillage practice causes higher AMF hyphal length, GRSP and water stable aggregate (WSA) compared to that of conventional tillage practice. The current review demonstrated that GRSP is an important tool for carbon storage in deep soils. Glomalin mediates soil aggregates, improves soil quality, increases carbon sequestration and crop production, and mitigates climate change.
topic mycorrhizal fungi species
glomalin
glomalin carbon pools
soil aggregate formation
carbon sequestration
url http://www.agrifoodscience.com/index.php/TURJAF/article/view/3803
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