Kellogg Christina A, Griffin Dale W
US Geological Survey, 600 4th St S, St Petersburg, FL 33701, USA.
Trends Ecol Evol. 2006 Nov;21(11):638-44. doi: 10.1016/j.tree.2006.07.004. Epub 2006 Jul 14.
Desert winds aerosolize several billion tons of soil-derived dust each year, including concentrated seasonal pulses from Africa and Asia. These transoceanic and transcontinental dust events inject a large pulse of microorganisms and pollen into the atmosphere and could therefore have a role in transporting pathogens or expanding the biogeographical range of some organisms by facilitating long-distance dispersal events. As we discuss here, whether such dispersal events are occurring is only now beginning to be investigated. Huge dust events create an atmospheric bridge over land and sea, and the microbiota contained within them could impact downwind ecosystems. Such dispersal is of interest because of the possible health effects of allergens and pathogens that might be carried with the dust.
每年,沙漠风会使数十亿源自土壤的沙尘形成气溶胶,其中包括来自非洲和亚洲的季节性集中沙尘脉冲。这些跨洋和跨大陆的沙尘事件会将大量微生物和花粉注入大气,因此可能在通过促进远距离扩散事件来传播病原体或扩大某些生物的生物地理范围方面发挥作用。正如我们在此所讨论的,此类扩散事件是否正在发生直到现在才开始得到研究。巨大的沙尘事件在陆地和海洋上空架起了一座大气桥梁,其中所含的微生物群可能会影响顺风方向的生态系统。这种扩散之所以受到关注,是因为沙尘可能携带的过敏原和病原体可能对健康产生影响。