Suchergebnisse

The Sahara in North Africa and the Gobi and Taklamakan deserts in Asia are the primary sources of mobilized dust in the atmosphere, with regional or global airborne transport estimated at 2 to 5 billion tonnes per year. Annual Asian dust plumes take about 7 to 10d to cross the Pacific Ocean, and often reach the northwest USA between late February and May. In contrast, the peak season for the movement of African dust storms to the southeastern USA is typically June to August, and dust plumes take about 5 to 7d to reach Florida. Although studies have documented that a wide range of bacteria, fungi, archaea, and viruses in dust plumes reach the USA each year, little is known about temporal and spatial variability in the microbial biodiversity in transoceanic dust plumes, or the effect on the deposition environments. A scoping study (called the Transoceanic Aerobiology Biodiversity Study) was conducted to develop field-based campaigns centered on examining the abundance, diversity, survival, and impact of microorganisms in transoceanic dust plumes arriving in the continental USA from Asia and Africa. This effort identified Science Questions (SQs) and Knowledge Gaps(KGs) that are highly relevant toward an understanding of the microbial diversity, transport, survival, and dispersal in transoceanic dusts. Science Questions were defined as broad science topics in transoceanic dust plume microbiology that were underexplored by the aerobiology community. Knowledge Gaps were defined as specific project-level research questions for each SQ that represented important topics in the study of transoceanic aerobiology. ; NASA's Biodiversity Office [NNX16AQ38G]; National Science Foundation grant from the Division of Environmental Biology [1241161, 1643288]; Earth and Biological Sciences Directorate Program Development Funds at Pacific Northwest National Laboratory; U.S. Geological Survey's Environmental Health Toxic Substances Hydrology and Contaminate Biology Programs ; The project was supported by a scoping study Grant from NASA's Biodiversity Office (Grant #NNX16AQ38G). Partial support to BC was provided by a National Science Foundation grant from the Division of Environmental Biology (1241161 and 1643288). Partial support to SB was funded by the Earth and Biological Sciences Directorate Program Development Funds at Pacific Northwest National Laboratory. DG was partially supported by the U.S. Geological Survey's Environmental Health Toxic Substances Hydrology and Contaminate Biology Programs. ; Public domain authored by a U.S. government employee