School of Biological Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong SAR, China.
Nat Rev Microbiol. 2012 Jul 9;10(8):551-62. doi: 10.1038/nrmicro2831.
Drylands constitute the most extensive terrestrial biome, covering more than one-third of the Earth's continental surface. In these environments, stress limits animal and plant life, so life forms that can survive desiccation and then resume growth following subsequent wetting assume the foremost role in ecosystem processes. In this Review, we describe how these organisms assemble in unique soil- and rock-surface communities to form a thin veneer of mostly microbial biomass across hot and cold deserts. These communities mediate inputs and outputs of gases, nutrients and water from desert surfaces, as well as regulating weathering, soil stability, and hydrological and nutrient cycles. The magnitude of regional and global desert-related environmental impacts is affected by these surface communities; here, we also discuss the challenges for incorporating the consideration of these communities and their effects into the management of dryland resources.
干旱地区构成了最广泛的陆地生物群系,覆盖了地球大陆表面的三分之一以上。在这些环境中,压力限制了动植物的生命,因此能够在干燥后存活并在随后的湿润后恢复生长的生命形式在生态系统过程中起着最重要的作用。在这篇综述中,我们描述了这些生物是如何在独特的土壤和岩石表面群落中聚集在一起的,从而在炎热和寒冷的沙漠中形成一层主要由微生物生物量组成的薄薄的外壳。这些群落调节着来自沙漠表面的气体、养分和水的输入和输出,以及控制风化、土壤稳定性以及水文和养分循环。这些表面群落影响着与沙漠相关的区域和全球环境影响的规模;在这里,我们还讨论了将这些群落及其影响纳入干旱地区资源管理的考虑的挑战。