File:Loess formation in semi-arid environments.webp

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Loess formation in semi-arid environments

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Description
English: Biological loess crust formation in semi-arid environments

According to a hypothesis by Svirčev et al., 2013, loess sediment growth in arid and semi-arid regions is facilitated in the same manner, via trapping and accumulation of airborne dust particles by sticky exopolymeric substances during wet events. The particles are then processed through a series of weathering reactions, and translocated downward as cyanobacteria move up toward the light source. When biological activity halts during the dry period, the trapped particles remain immobilized and turn into constituents of cohesive biological loess crusts that resists wind erosion. The switch between the wet and dry conditions and associated processes represents one cycle of accumulation. The compilation of such cycles results in the initial growth of loess.

  • Reference: Svirčev Z, Marković SB, Stevens T, Codd GA, Simeunovć J, Obreht I, Dulić T, Pantelić D, Hambach U (2013) "Importance of biological loess crusts for loess formation in semi-arid environments". Quat Int, 296: 206–215.
Date
Source [1] doi:10.1007/s11104-019-04048-3
Author Zorica Svirčev, Tamara Dulić, Igor Obreht, Geoffrey A. Codd, Frank Lehmkuhl, Slobodan B. Marković, Ulrich Hambach & Jussi Meriluoto

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current22:56, 11 August 2021Thumbnail for version as of 22:56, 11 August 20211,916 × 827 (124 KB)Epipelagic (talk | contribs)adjust relative positions and recrop
20:49, 11 August 2021Thumbnail for version as of 20:49, 11 August 20211,890 × 837 (216 KB)Epipelagic (talk | contribs)Uploaded a work by Zorica Svirčev, Tamara Dulić, Igor Obreht, Geoffrey A. Codd, Frank Lehmkuhl, Slobodan B. Marković, Ulrich Hambach & Jussi Meriluoto from [https://link.springer.com/article/10.1007/s11104-019-04048-3] {{doi|10.1007/s11104-019-04048-3}} with UploadWizard

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