Abstract
In the last decades, many studies were addressed focusing on soil protection that helps sequestration and stabilization of organic carbon in soil aggregates. Soil aggregates are an association of primary soil particles, bacteria, fungi, plant root and soil organic matter. Plant root provides a carbon source for arbuscular mycorrhizal fungi (AMF) present in soil aggregates. AMF produces a glycoprotein glomalin which is hydrophobic, insoluble, and recalcitrant in nature. Glomalin plays a vital role in the stabilization of soil aggregates. Greater stability of soil aggregates leads to a larger amount of protected organic carbon in the soil. Thus, glomalin-related soil protein can be considered as a potential contributor in the stabilization of soil organic carbon. In the present chapter, the different aspects of glomalin composition, production, role in soil, recalcitrant nature, potential role in soil carbon locking up and stabilization are summarized and discussed.
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Abbreviations
- AMF:
-
Arbuscular Mycorrhizal Fungi
- BRSP:
-
Bradford Reactive Soil Protein
- GRSP:
-
Glomalin-Related Soil Protein
- HSP60:
-
Heat Shock Protein 60
- OM:
-
Organic Matter
- SOC:
-
Soil Organic Carbon
- SOM:
-
Soil Organic Matter
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Acknowledgements
The work was supported by the project of Technology Agency of the Czech Republic TH02030169: “Effect of biologically transformed organic matter and biochar application on the stability of productive soil properties and reduction of environmental risks” and by the Ministry of Education, Youth and Sports of the Czech Republic, grant number FCH-S-20-6446.
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Holatko, J. et al. (2021). Glomalin: A Key Indicator for Soil Carbon Stabilization. In: Datta, R., Meena, R.S. (eds) Soil Carbon Stabilization to Mitigate Climate Change. Springer, Singapore. https://doi.org/10.1007/978-981-33-6765-4_2
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