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Geomorphic controls of biological soil crust distribution, Mojave Desert (USA)

机译:莫哈韦沙漠(美国)生物土壳分布的地貌控制

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Biological soil crusts (BSCs) are vital features of arid regions. These crusts form living skin that mitigates erosion, influences soil fertility, manages soil moisture/temperature, and prevents desertification. BSCs are fragile resources, easily destroyed by physical disturbances and potentially impacted by climate change. Our investigation employs a novel, interdisciplinary approach to investigate BSC biotic potential (bridging gaps among biology, ecology, soils, hydrology, statistics, chemistry, geomorphology, remote sensing, and GIS). Our study documents important links among BSCs, soils, geomorphology, and land stability. Results indicate geomorphic stability and dust influx impact BSC composition and development. Soil stability ultimately controls biotic potential of cyanobacterial versus moss-lichen crust; however, dust influences both crust types through texturally enhanced water-holding capacity and increased soil fertility. Soil chemistry of moss-lichen substrates exhibit a potential dustsignature, with elevated Ca, K, Mg, B, Fe, Ni, Co, Mn, CI, and EC. While results indicate inherent geomorphic stability controls BSC development, we suggest BSCs enhance their propagation through dust capture and erosion mitigation. These soil-geomorphic relationships present insight into arid landscape evolution, providing tools to improve BSC mapping and land management.
机译:生物土壳(BSC)是干旱地区的重要特征。这些地壳形成活皮肤,减轻侵蚀,影响土壤肥力,管理土壤水分/温度,并防止荒漠化。 BSC是脆弱的资源,容易被物理干扰摧毁,并且可能受到气候变化的影响。我们的调查采用了一种新颖的跨学科方法来调查BSC生物潜力(生物学,生态,土壤,水文,统计,化学,地貌,遥感和GIS)的桥接空白。我们的研究记录了BSC,土壤,地貌和土地稳定性的重要环节。结果表明地貌稳定性和粉尘涌入影响BSC成分和发育。土壤稳定性最终控制蓝藻的生物潜力与苔藓 - 地衣壳;然而,灰尘通过纹理增强的水持能力和土壤肥力增加来影响地壳类型。苔藓 - 地衣底物的土壤化学表现出潜在的灰尘性,具有升高的Ca,K,Mg,B,Fe,Ni,Co,Mn,Ci和Ec。虽然结果表明了固有的地貌稳定性控制BSC开发,但我们建议BSC通过灰尘捕获和侵蚀缓解增强它们的传播。这些土壤 - 地貌关系存在洞察干旱景观演化,提供改善BSC测绘和土地管理的工具。

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