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Group-Specific Diatom Silica Production in a Coastal Upwelling System

Group-Specific Diatom Silica Production in a Coastal Upwelling System
沿海上升流系统中特定族群硅藻二氧化硅的生产
批准号:
1155663
负责人:
Jeffrey Krause
金额:
$45.35万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2012
资助国家:
美国
项目状态:
已结题
起止时间:
2012-04-01 至 2017-03-31

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中文摘要
翻译
这项研究将使用现有方法的新组合来研究硅藻物种中二氧化硅产量的分布,以评估特定物种或属对硅藻二氧化硅产量的贡献。利用沿海上升流系统和低营养亚热带环流在硅藻群落结构和二氧化硅产量方面的强烈对比,将检验有关硅藻物种之间二氧化硅产量分布的具体假设。有几条证据支持这样的观点,即负责大部分二氧化硅生产的硅藻从沿海系统中数量最丰富的物种转移到近海贫营养环境中相对罕见但非常大的细胞。这种转变改变了硅藻在区域食物网中的作用,由于决定浮游植物群体在生物地球化学循环中作用的许多过程是细胞大小的函数,这种转变对硅藻对上层海洋碳循环和生物泵的贡献的区域差异具有强烈的影响。本研究还试图在物种水平上了解硅限制在调节硅藻二氧化硅生产中的作用。到目前为止,从南极的高硅水域到沿海上升流系统和少营养的亚热带环流,在所研究的每个系统中都检测到了硅对二氧化硅生产的限制。对硅限制的实地研究很少伴随着对存在的物种的检查。当研究确实有分类数据时,缺乏关于单个物种表现的信息,使得不可能在细胞之间分配测量的速率,这可能导致关于特定硅藻组对群落综合速率的贡献的错误结论。该项目将测试五个假说。每一项都与利用特定物种的数据以增进对调节硅藻在海洋食物网中作用的因素的了解这一总主题有关。通过将使用放射性同位素32Si的二氧化硅产量的批量测量与使用荧光探针2-(4-pyridyl)-5((4-(2-dimethylaminoethyl-aminocarbamoyl)-methoxy)phenyl)oxazole,或pDMPO的单个细胞的硅沉积速率的定量测量相结合,将确定以下内容:特定物种的硅藻对群落总二氧化硅产量的贡献,硅藻物种之间作为细胞大小函数的二氧化硅产量分布的区域差异,控制物种竞争溶解硅的能力的物种特定的动力学参数,以及是否可以通过了解硅藻利用硅的能力和数量丰度(而不是其他因素,如放牧或其他营养物质的限制)来解释特定硅藻组或物种的优势。更广泛的影响:来自田间组合的特定知识将提高对海洋硅藻产生有机碳和二氧化硅的主要生物和生态驱动因素的理解。这一数据集还将有助于确定可纳入沿海和低营养环流生态系统食物网和生物地球化学模型的关键物种,并测试实验室研究获得的硅藻养分吸收能力知识是否能代表实地混合群落中的硅藻。该项目还将为本科生提供实验室和现场环境下的研究经验,并将包括与UCSB海洋科学研究所海洋到课堂(O2C)计划的科学推广人员合作设计的K-12推广计划,供地区小学使用。O2C目前每年接触到800个区域K-12教室的18,000多名学生,使用UCSB PIs的海洋研究的真实例子为学生们带来海洋科学。
英文摘要
This study will examine the distribution of silica production among diatom species, using a novel combination of existing approaches, to evaluate the contributions of specific species or genera to total diatom silica production. Specific hypotheses regarding the distribution of silica production among species of diatoms will be tested by exploiting the strong contrasts in diatom community structure and silica production between a coastal upwelling system and in an oligotrophic subtropical gyre. Several lines of evidence support the idea that the diatoms responsible for the majority of silica production shifts from the most numerically abundant species in coastal systems to relatively rare, but very large, cells in offshore oligotrophic environments. This shift alters the role of diatoms in regional food webs and because many processes determining the role of phytoplankton groups in biogeochemical cycles are a function of cell size, such a shift has strong implications for regional differences in the contribution of diatoms to upper-ocean carbon cycling and the biological pump. This study also seeks to understand of the role of silicon limitation in regulating diatom silica production at the species level. Si limitation of silica production has been detected in every system examined to date, ranging from the high Si waters of the Antarctic, to coastal upwelling systems and the oligotrophic subtropical gyres. Field studies of Si limitation are rarely accompanied by examination of the species present. When studies do have taxonomic data the lack of information on the performance of individual species makes it impossible to allocate the measured rates among cells, potentially leading to erroneous conclusions about the contribution of specific diatom groups to community composite rates.The project will test five hypotheses. Each is related to the general theme of using species-specific data to improve understanding of the factors regulating diatoms' role in marine food webs. By combining bulk measures of silica production using the radioisotope 32Si with quantitative measures of silicon deposition rates by individual cells using the fluorescent probe 2-(4-pyridyl)-5((4-(2-dimethylaminoethyl-aminocarbamoyl)-methoxy)phenyl)oxazole, or PDMPO, the following will be determined: species-specific diatom contributions to total community silica production, regional differences in the distribution of silica production among diatom species as a function of cell size, species-specific kinetic parameters governing the ability of species to compete for dissolved silicon, and whether dominance of a particular diatom group or species can be explained by knowledge of their capacity to utilize Si and their numerical abundance (as opposed to other factors such as grazing or limitation by other nutrients).Broader impacts:Specific-specific knowledge from field assemblages will improve the understanding of the major biological and ecological drivers of organic carbon and silica production by diatoms in the sea. This dataset will also help identify key species for inclusion in food-web and biogeochemical models in coastal and oligotrophic gyre ecosystems, and test whether knowledge of diatom nutrient uptake capacity from laboratory studies are representative of diatoms in mixed communities in the field. This project will also provide research experiences for undergraduates in both the laboratory and field settings, and will include a K-12 outreach program designed in collaboration with scientific-outreach personnel from UCSB's Marine Science Institute's Oceans to Classroom (O2C) program for use in regional elementary schools. O2C currently reaches over 18,000 students in 800 regional K-12 classrooms annually bringing marine science to life for students using real-life examples of marine research by UCSB PIs.
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Quantifying the effect of sediment microbial activity in facilitating silica sequestration during early diagenesis (QUALIFIED)
Collaborative Research: RAPID: Extreme disturbances/perturbations to coastal deposition systems
Collaborative Research: Understanding substrate limitation and Lithium and Silicon isotope fractionation during secondary clay formation in marine systems
RII Track-4: Peering into Nature's Glass Boxes - using nano-Raman Spectroscopy to answer Novel Questions in Diatom-focused Environmental Research
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