Do interactions between vertically and horizontally transported particles measurably affect particle composition and flux to the sediments? A mechanistic approach.

垂直和水平输送颗粒之间的相互作用是否会显着影响沉积物的颗粒组成和通量？

• 批准号: 1061128
• 负责人: David Black
• 金额: $ 159.71万
• 依托单位: SUNY at Stony Brook
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-04-01 至 2016-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1061128&HistoricalAwards=false
• 关键词: Do; interactions; between; vertically; horizontally

The export of many elements from the surface ocean to the deep sea is mediated by the flux of sinking particles; for example, sinking particles account for 50-80% of the vertical transport of organic carbon through the mesopelagic zone. Heterotrophic remineralization of particulate organic carbon (POC) in the open ocean is usually very efficient, as 90% of the POC produced in surface waters is returned to inorganic form in the euphotic zone or during transit through the upper water column. However, a small fraction of the organic matter produced in surface waters survives transit to the deep ocean or seafloor. Similarly, the flux and composition of inorganic material also vary during transport to the sea floor. Perhaps the most obvious example of such modification is the dissolution of carbonate and biogenic silica as they sink through the water column. However, the flux and composition of particulate organic and inorganic matter that reaches the deep sea and sediments depend not just on their source in the surface waters, but also on alteration, supplementation, and selective removal that occurs during vertical transit. In some regions, particularly near margins, lateral transport can also be extensive. Exchange between sinking material and suspended particles or dissolved organic matter via aggregation/disaggregation and solution/dissolution can also influence composition. In this project, a research team at the State University of New York at Stony Brook set out to develop a better mechanistic understanding of the ocean?s role in the global carbon cycle and the factors that influence the sedimentary record. Their work is developed around five interrelated hypotheses revolving around the themes of remineralization and exchange as particles sink to the sea floor, potential horizontal influences on sinking particles, and how vertical and horizontal transport potentially influence the interpretation of the sediment record. They will apply some of the tools developed during the recent MedFlux program to produce better quantitative models of sinking fluxes by incorporating explicit consideration of ballast minerals (including celestite and barite) and to define better the interactions among particles as they sink. They will also compare results of inorganic, organic and radiochemical analyses of particles sampled by traps and pumps with those of bottom sediments at our proposed site on the Bermuda Rise. While this is a modern process study, it is expected to have significant paleoceanographic implications. Quantifying the relative vertical and horizontal fluxes of key paleoceanographic proxies in combination with characterization of the seasonal fluxes will greatly enhance our understanding of the existing sediment record at the Bermuda Rise, and improve the quality of future reconstructions as well as lead to more robust interpretations from other sites with significant lateral input. Broader Impacts. The diversity of backgrounds represented by the PIs (organic geochemistry, radiochemistry, palaeoceanography, modeling) offers unique opportunities to train the next generation of marine scientists. Four graduate students will be involved in this project. All will receive training at sea, in the laboratory, and in modern data analysis. In addition to graduate students, a postdoctoral scholar will be involved in the present project at no additional cost to NSF. The PIs also participate in outreach activities that will include presentations of research results to lay persons and other community groups.

许多元素从表层海洋向深海的输出是通过下沉颗粒的通量来调节的；例如，下沉颗粒占中层区域有机碳垂直输送的 50-80%。公海中颗粒有机碳 (POC) 的异养再矿化通常非常有效，因为地表水中产生的 POC 90% 在富光带或通过上部水柱的过程中返回到无机形式。然而，地表水中产生的有机物的一小部分在转移到深海或海底时幸存下来。类似地，无机材料的通量和成分在运输到海底的过程中也会发生变化。也许这种改变最明显的例子是碳酸盐和生物二氧化硅在沉入水柱时的溶解。然而，到达深海和沉积物的颗粒有机物和无机物的通量和组成不仅取决于它们在表层水中的来源，还取决于垂直运输过程中发生的改变、补充和选择性去除。在某些地区，特别是靠近边缘地区，横向运输也可能很广泛。沉没物质与悬浮颗粒或溶解有机物之间通过聚集/分解和溶解/溶解进行的交换也会影响成分。在该项目中，纽约州立大学石溪分校的一个研究小组着手对海洋在全球碳循环中的作用以及影响沉积记录的因素进行更好的机械理解。他们的工作围绕五个相互关联的假设展开，这些假设围绕颗粒沉入海底时的再矿化和交换、对下沉颗粒的潜在水平影响以及垂直和水平运输如何潜在影响沉积物记录的解释等主题展开。他们将应用最近 MedFlux 计划中开发的一些工具，通过明确考虑压载矿物（包括天青石和重晶石）来生成更好的下沉通量定量模型，并更好地定义颗粒下沉时的相互作用。他们还将通过捕集器和泵采样的颗粒的无机、有机和放射化学分析结果与我们拟定的百慕大海隆地点的底部沉积物的分析结果进行比较。虽然这是一项现代过程研究，但预计将具有重大的古海洋学意义。量化关键古海洋代理的相对垂直和水平通量，结合季节性通量的表征，将极大地增强我们对百慕大海隆现有沉积物记录的理解，提高未来重建的质量，并从具有重要横向输入的其他地点得出更可靠的解释。更广泛的影响。 PI（有机地球化学、放射化学、古海洋学、建模）所代表的背景多样性为培养下一代海洋科学家提供了独特的机会。四名研究生将参与该项目。所有人都将接受海上、实验室和现代数据分析方面的培训。除了研究生之外，一名博士后学者也将参与本项目，无需向 NSF 支付额外费用。 PI 还参与外展活动，其中包括向非专业人士和其他社区团体介绍研究成果。