The effect of different biological soil crusts on soil organic carbon in the AjiGol wetland

Rashin  Mohammadi; Mohsen  Hosseinalizadeh; Ali  Mohammadian Behbahani; Vahedberdi  Sheikh; Narges  Kariminejad; Jahangir  Mohammadi

نویسندگان

Rashin Mohammadi Department of Arid Zone Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran نویسنده
Mohsen Hosseinalizadeh Department of Arid Zone Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran نویسنده
Ali Mohammadian Behbahani Department of Arid Zone Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran نویسنده
Vahedberdi Sheikh Department of Watershed Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran نویسنده
Narges Kariminejad Department of Arid Zone Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran نویسنده
Jahangir Mohammadi Department of forest science, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran نویسنده

کلمات کلیدی:

Soil organic carbon, biological crusts, AjiGol wetland, soil stability

چکیده

The objective of this study was to investigate the role of biocrusts on the soil organic carbon characteristic in the AjiGol wetland of Golestan province (Iran). In the study area, three soil samples under the surface of biocrusts and no crust were taken at the depth of 0-2 and 2-5cm. Also, soil organic carbon factor was analyzed for all soil samples. The results showed that the presence of biocrusts compared to the no crust improved the soil quality. From the no crust to the moss biocrust, the content of organic carbon (OC) was significantly increased at two depths of soil (0-2 and 2-5cm). Therefore, the presence of biological soil crusts can increase the quality of soil as well as stability of it.

دانلودها

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بیوگرافی نویسندگان

Rashin Mohammadi، Department of Arid Zone Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran
Mohsen Hosseinalizadeh، Department of Arid Zone Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran
Ali Mohammadian Behbahani، Department of Arid Zone Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran
Vahedberdi Sheikh، Department of Watershed Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran
Narges Kariminejad، Department of Arid Zone Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran
Jahangir Mohammadi، Department of forest science, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran

مراجع

[1] Adessi A, De Philippis R, Rossi F (2021) Drought-tolerant cyanobacteria and mosses as biotechnological tools to attain land degradation neutrality. Web Ecol. 21: 65-78. https://doi.org/10.5194/we-21-65-2021.

[2] Armstrong, RA. (2017) Adaptation of lichens to extreme conditions. Plant Adaptation Strategies in Changing Environment. Springer. 1-27. https://doi.org/10.1007/978-981-10-6744-0_1.

[3] Belnap J, Weber B, Büdel B (2016) Biological Soil Crusts: An Organizing Principle in Drylands. Ecology study, Springer. 3–13. http://dx.doi.org/10.1007/978-3-319-30214-0.

[4] Hu P, Zhang W, Xiao L, Yang R, Xiao D, Zhao J, Wang W, Chen H, Wang K (2019) Moss-dominated biological soil crusts modulate soil nitrogen following vegetation restoration in a subtropical karst region. Geoderma. 352: 70-79. http://dx.doi.org/10.1016/j.geoderma.2019.05.047.

[5] Maestre FT, Bowker MA, Cantón Y, Castillo-Monroy AP, Cortina J, Escolar C, Escudero A, Lázaro R, Martínez I (2011) Ecology and functional roles of biological soil crusts in semi-arid ecosystems of Spain. J. Arid Environ. 75: 1282-1291. https://doi.org/10.1016/j.jaridenv.2010.12.008.

[6] Poeplau C, Don A (2013) Sensitivity of soil organic carbon stocks and fractions to different land-use changes across Europe. Geoderma. 192: 189-201. https://doi.org/10.1016/j.geoderma.2012.08.003.

[7] Rodríguez-Caballero E, Cantón Y, Chamizo S, Lázaro R, Escudero A (2013) Soil loss and runoff in semiarid ecosystems: a complex interaction between biological soil crusts, micro-topography, and hydrological drivers. Ecosyst. 16: 529-546. http://dx.doi.org/10.1007/s10021-012-9626-z.

[8] Rodriguez-Caballero E, Stanelle T, Egerer S, Cheng Y, Su H, Canton Y, Belnap J, Andreae MO, Tegen I, Reick CH (2022) Global cycling and climate effects of aeolian dust controlled by biological soil crusts. Nat. Geosci.: 1-6. http://dx.doi.org/10.1038/s41561-022-00942-1.

[9] Torres-Cruz TJ, Howell AJ, Reibold RH, McHugh TA, Eickhoff MA, Reed SC (2018) Species-specific nitrogenase activity in lichen-dominated biological soil crusts from the Colorado Plateau, USA. Plant Soil. 429: 113-125. https://doi.org/10.1007/s11104-018-3580-2.

[10] Walkley A, Black IA (1934) An examination of the Degtjareff method for determining soil organic matter, and a proposed modification of the chromic acid titration method. Soil Sci. 37: 29-38. http://dx.doi.org/10.1097/00010694-193401000-00003.

[11] Zhao L, Liu Y, Wang Z, Yuan S, Qi J, Zhang W, Wang Y, Li X (2020) Bacteria and fungi differentially contribute to carbon and nitrogen cycles during biological soil crust succession in arid ecosystems. Plant Soil. 447: 379-392. https://link.springer.com/article/10.1007/s11104-019-04391-5.