PRF/J: Effects of Geothermal Phosphorus Inputs on Microbes, Litter, Decomposition, and Higher Trophic Levels in a Tropical Stream

PRF/J：地热磷输入对热带溪流中微生物、凋落物、分解和较高营养水平的影响

• 批准号: 9403292
• 负责人: Amy Rosemond
• 金额: $ 6.96万
• 依托单位: GA Fellowships
• 依托单位国家: 美国
• 项目类别: Fellowship Award
• 财政年份: 1995
• 资助国家: 美国
• 起止时间: 1995-01-01 至 1997-02-28
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9403292&HistoricalAwards=false
• 关键词: PRF; Effects; Geothermal; Phosphorus; Inputs

9403292 Rosemond Although nutrients in aquatic food webs may control growth rates of primary producers (which are consumed by higher trophic levels), few investigations have directly probed the role of nutrients in detrital systems. Landscape - scale volcanic activity in Central America results in prominent changes to surface water chemistry, including dramatic increases in soluble reactive phosphorus (P) concentrations, with appreciable localized effects on stream biota. This research will examine whether geothermal P inputs enhance microbial biomass, nutrient content, and leaf litter decomposition rates. Effects of P variation on higher trophic levels will be assessed by comparing drift and trap densities, and size of detritivorous shrimp. High and low P site comparisons of leaf litter quality will be performed using measures of detritivore growth and fat content. The relative importance of microbial versus macroconsumer processes in leaf decomposition will be determined using in situ manipulations of nutrient levels. Both bottom - up (nutrient) control and top - down (detritivory) control will be examined. %%% The role of detritus in trophic dynamics hasn't been well studied, particularly in lotic (flowing water) ecosystems. But beyond fundamental research aspects, this project's importance derives our need to know how aquatic systems operate, as human population pressures place increasing burdens on the natural environment, in the United States, Latin America, and around the world. ***

小行星9403292 虽然水生食物网中的营养物质可能控制初级生产者的生长速度（被更高的营养级消耗），但很少有调查直接探讨营养物质在碎屑系统中的作用。 中美洲景观规模的火山活动导致地表水化学的显著变化，包括可溶性活性磷（P）浓度的急剧增加，对河流生物群产生了明显的局部影响。 本研究将探讨是否地热磷输入提高微生物生物量，养分含量和落叶分解率。 磷的变化对更高的营养水平的影响将通过比较漂移和陷阱的密度，和大小的食虫虾进行评估。 高和低P站点比较落叶质量将进行食草动物的生长和脂肪含量的措施。 微生物与宏消费过程中的叶分解的相对重要性将确定使用原位操作的营养水平。 自下而上（营养）控制和自上而下（摄食）控制都将被检查。 碎屑在营养动力学中的作用还没有得到很好的研究，特别是在流动的水生态系统中。 但是，除了基础研究方面，这个项目的重要性源于我们需要知道水生系统是如何运作的，因为人口压力给美国，拉丁美洲和世界各地的自然环境带来了越来越大的负担。 ***