Collaborative Proposal: Coupled C, N and S cycling in coastal plain wetlands: how will climate change and salt water intrusion alter ecosystem dynamics?

合作提案：沿海平原湿地耦合的碳、氮和硫循环：气候变化和咸水入侵将如何改变生态系统动态？

• 批准号: 1021149
• 负责人: Emily Bernhardt
• 金额: $ 50.98万
• 依托单位: Duke University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2010
• 资助国家: 美国
• 起止时间: 2010-10-01 至 2013-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1021149&HistoricalAwards=false
• 关键词: Collaborative; Proposal; Coupled; cycling; coastal

Coastal plain wetlands occupy a critical landscape position at the intersection of terrestrial and aquatic and fresh and salt waters. Like all wetlands, coastal wetlands are disproportionately valuable in terms of services provided compared to the area they comprise including nutrient transformation, water purification, and flood control. Humans have drained wetlands throughout much of the southeastern coastal plain for agriculture and forestry, thus diminishing their capacity to provide critical ecosystem services such as nutrient and carbon sequestration. At the same time, fertilizer use and manure from intensive meat and poultry production have dramatically increased nutrient loading to coastal ecosystems. Increased loading and decreased retention of nutrients has caused eutrophication of downstream freshwater and coastal ecosystems, with the associated degradation in water quality and decline in coastal fisheries. Climate change may further exacerbate these trends: higher temperatures and increasingly sporadic precipitation may further diminish the spatial extent of perennially flooded wetlands and is already leading to seasonal salt water intrusion during drought. Predicting the likely ecosystem carbon and nutrient cycling of coastal plain freshwaters into a saltier and increasingly uncertain hydrologic future requires significant improvements to our current understanding of freshwater ecosystems. This proposal focuses strategically on two aspects of this problem: first, incorporating sulfur (~from sea salt) dynamics into our understanding of how microbes alter carbon and nutrient cycling and second, utilizing simulation modeling to mesh dynamic hydrology together with microbial biogeochemistry. Adaptive simulation modeling together with targeted empirical work will allow us to rapidly test and refine current models of wetland carbon and nutrient cycling and to formalize the emerging conceptual understanding of wetland biogeochemistry into a flexible, easily adjusted modeling framework. The focal field site is a formerly ditched and drained agricultural field in North Carolina's coastal plain that was restored to riverine wetland hydrology in 2007, becoming the largest privately owned mitigation bank in the southeast. The site has very little topographic relief (-1 to +1 m elevation); experiences significant salt water intrusion via surface water mixing during summer droughts; and has wind tide driven hydrology that generates large gradients in sulfur concentrations in both time and space. The field site is representative of large areas of SE coastal plain agricultural landscapes that are being actively restored or abandoned. The economic and ecological "success" of this project will be closely watched by regulators and practitioners throughout the region. This research program will directly affect the potential for site owners to sell validated carbon and nutrient credits in emerging ecosystem service markets. Resulting research findings (together with their economic implications) will influence future patterns of mitigation and conservation investment throughout the southeastern coastal plain and will provide critical information that will facilitate climate adaptation planning throughout the region.

滨海平原湿地在陆地与水生、淡水与咸水的交汇处占据着重要的景观位置。与所有湿地一样，沿海湿地在提供的服务方面与它们所包括的区域相比价值不成比例，包括养分转化、水净化和防洪。人类已经排干了东南部沿海平原大部分地区的湿地，用于农业和林业，从而削弱了它们提供营养和碳固存等关键生态系统服务的能力。与此同时，集约化肉类和家禽生产产生的化肥和粪便极大地增加了沿海生态系统的营养负荷。负荷的增加和营养物质保留量的减少造成了下游淡水和沿海生态系统的富营养化，从而导致水质恶化和沿海渔业的衰退。气候变化可能会进一步加剧这些趋势：更高的气温和越来越零星的降水可能会进一步缩小常年洪水泛滥的湿地的空间范围，并已导致干旱期间季节性咸水入侵。预测沿海平原淡水可能的生态系统碳和养分循环进入盐度更高和日益不确定的水文未来，需要对我们目前对淡水生态系统的理解有重大改进。这一建议战略性地集中在这一问题的两个方面：第一，将硫(~来自海盐)的动力学纳入我们对微生物如何改变碳和养分循环的理解中；第二，利用模拟模型将动态水文学与微生物生物地球化学结合起来。自适应模拟建模和有针对性的实证工作将使我们能够快速测试和完善当前的湿地碳和养分循环模型，并将对湿地生物地球化学的新兴概念理解正式化为灵活、易于调整的建模框架。焦点场地位于北卡罗来纳州沿海平原，以前是一片被沟渠和排水的农田，2007年恢复为河岸湿地水文，成为东南部最大的私人拥有的缓解银行。该遗址的地形起伏很小(海拔-1至+1米)；在夏季干旱期间，通过地表水混合经历了显著的咸水入侵；风潮驱动的水文产生了硫磺浓度在时间和空间上的巨大梯度。该场地代表了正在积极恢复或废弃的东南部沿海平原农业景观的大片区域。整个地区的监管机构和从业者将密切关注该项目在经济和生态方面的“成功”。这项研究计划将直接影响网站所有者在新兴生态系统服务市场销售经过验证的碳和营养信用的潜力。由此产生的研究结果(及其经济影响)将影响整个东南沿海平原缓解和保护投资的未来模式，并将提供关键信息，促进整个区域的气候适应规划。