Collaborative Research: How are estuarine carbon and alkalinity dynamics influenced by macrobiota?

合作研究：河口碳和碱度动态如何受到宏观生物群的影响？

• 批准号: 2148950
• 负责人: Ryan Woodland
• 金额: $ 62.57万
• 依托单位: University of Maryland Center for Environmental Sciences
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2022
• 资助国家: 美国
• 起止时间: 2022-07-01 至 2025-06-30
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2148950&HistoricalAwards=false
• 关键词: Collaborative; Research; How; estuarine; carbon

The global carbon cycle consists of the processes that transform and transport carbon on Earth. Interest in the global carbon cycle stems from its intimate connection with ecological processes and its control on atmospheric carbon dioxide, an extremely important greenhouse gas. A key feature of the global carbon cycle is the transport of carbon from land to the open ocean. Before reaching the open ocean, the carbon carried by rivers must past through estuaries, where significant transformations take place, including the interconversion of organic forms (such as carbohydrates, proteins, and lipids) and inorganic forms (carbon dioxide, bicarbonate, and carbonate) through photosynthesis and respiration. In addition to carbon, alkalinity is another important chemical quantity that is relevant to climate and life on Earth. The alkalinity is the capacity of a water body to neutralize acid and determines the extent to which carbon dioxide reacts with water to create chemical species that do not interact directly with the atmosphere. While many transformations of carbon and alkalinity in the ocean are dominated by microscopic life, like phytoplankton and bacteria, these transformations are also influenced by macroscopic life (macrobiota), such as oysters, clams, salt marshes, mangroves, and seagrasses. However, macrobiota are generally ignored in conceptual and computational models of carbon transformations in estuaries. The overall objective of this project is to improve understanding of the role that macrobiota play in estuarine carbon and alkalinity dynamics. The research will also support numerous undergraduate students, two graduate students and three post-doctoral scholars.The proposed research will be carried out through a coordinated program of field measurements, laboratory experiments, historical data analysis, and numerical modeling. Two contrasting tidal tributaries of the Chesapeake Bay, the Potomac River Estuary and the York River Estuary, will be sampled because they span much of the range of carbon and alkalinity dynamics found in estuaries worldwide and hence will facilitate the generalization of the project findings. The interdisciplinary research team will evaluate four hypotheses: (1) Tidal wetlands, such as marshes and mangroves, are a source of alkalinity to estuaries and this source increases with salinity, tidal wetland productivity, and tidal range. (2) Alkalinity sinks in estuaries are favored when riverine alkalinity is high and when benthic fauna (e.g., clams and oysters) or submerged aquatic vegetation (e.g., seagrasses) are present in sufficient quantities. (3) Alkalinity sources and sinks in estuaries are highly seasonal, with summer fluxes dominated by net calcification (due to benthic fauna and submerged aquatic vegetation, an alkalinity sink) and sulfate reduction (due to tidal wetlands, an alkalinity source) and winter fluxes due to net CaCO3 dissolution (an alkalinity source). (4) Estuaries with high-alkalinity rivers and low tidal marsh areas are sinks of alkalinity and sources of atmospheric carbon dioxide while those with low-alkalinity rivers and high tidal marsh areas are sources of alkalinity and sinks of atmospheric carbon dioxide. The research plan includes seven main elements: (1) carbonate system measurements, (2) benthic fauna distribution measurements, (3) measurements of macrobiota carbon and alkalinity fluxes, (4) development of macrobiota carbon and alkalinity flux maps, (5) historical analysis of carbonate system measurements, (6) 3-D numerical modeling, and (7) a meta-analysis that extend findings to other systems. Mentoring and inclusion will occur through the development of a research affinity group of at least eight students that will connect existing regional undergraduate research programs. Students will present their research to managers and policy makers from the Chesapeake Bay Program during annual summits and we will engage estuarine managers through presentations on macrobiota influence on biogeochemistry. This research will advance the understanding of how macrobiota influence estuarine carbon and alkalinity dynamics and, ultimately, the large-scale marine cycles of carbon and alkalinity.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

全球碳循环包括在地球上转化和运输碳的过程。对全球碳循环的关注源于其与生态过程的密切联系及其对大气二氧化碳这一极其重要的温室气体的控制。全球碳循环的一个关键特征是碳从陆地运输到公海。在到达开阔的海洋之前，河流携带的碳必须通过河口，在那里发生重要的转化，包括通过光合作用和呼吸作用进行有机形式（如碳水化合物，蛋白质和脂质）和无机形式（二氧化碳，碳酸氢盐和碳酸盐）的相互转化。除了碳，碱度是另一个与地球上的气候和生命有关的重要化学量。碱度是水体中和酸的能力，并决定了二氧化碳与水反应产生不直接与大气相互作用的化学物质的程度。虽然海洋中的许多碳和碱度的转化都是由浮游植物和细菌等微观生命主导的，但这些转化也受到牡蛎、蛤蜊、盐沼、红树林和海草等宏观生命（大型生物群）的影响。然而，大型生物群通常被忽略的概念和计算模型的碳转化在河口。该项目的总体目标是提高对大型生物群在河口碳和碱度动态中所起作用的理解。该研究还将支持众多的本科生，两名研究生和三名博士后学者。拟议的研究将通过现场测量，实验室实验，历史数据分析和数值模拟的协调计划进行。将对切萨皮克湾的两条对比鲜明的潮汐支流波托马克河河口和约克河河口进行采样，因为它们跨越了世界各地河口中发现的碳和碱度动态范围，因此将有助于推广项目结果。跨学科研究小组将评估四个假设：（1）潮汐湿地，如沼泽和红树林，是河口碱度的来源，这种来源随着盐度，潮汐湿地生产力和潮差的增加而增加。 (2)当河流碱度高时，当底栖动物（例如，蛤和牡蛎）或水下水生植物（例如，海草）以足够的量存在。(3)河口的碱度源和汇是高度季节性的，夏季通量主要由净钙化（由于底栖动物和沉水水生植被，碱度汇）和硫酸盐还原（由于潮汐湿地，碱度源）和冬季通量由于净CaCO3溶解（碱度源）。(4)具有高碱度河流和低潮沼泽区的河口是碱度的汇和大气CO2的源，而具有低碱度河流和高潮沼泽区的河口是碱度的源和大气CO2的汇。研究计划包括七个主要内容：（1）碳酸盐系统测量，（2）底栖动物分布测量，（3）大型生物群碳和碱度通量测量，（4）大型生物群碳和碱度通量地图的开发，（5）碳酸盐系统测量的历史分析，（6）三维数值建模，以及（7）将研究结果扩展到其他系统的荟萃分析。指导和包容性将通过至少八名学生的研究亲和组的发展发生，将连接现有的区域本科研究计划。学生将在年度峰会期间向切萨皮克湾计划的管理人员和政策制定者展示他们的研究，我们将通过大型生物群对海洋地球化学影响的演讲来吸引河口管理人员。这项研究将促进对大型生物群如何影响河口碳和碱度动态的理解，并最终影响碳和碱度的大规模海洋循环。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。