Towards a plant-based proxy for the isotope ratio of atmospheric water vapor

寻找基于植物的大气水蒸气同位素比代理

• 批准号: 0615501
• 负责人: Brent Helliker
• 金额: $ 35.04万
• 依托单位: University of Pennsylvania
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2006
• 资助国家: 美国
• 起止时间: 2006-07-15 至 2010-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0615501&HistoricalAwards=false
• 关键词: Towards; plant; based; proxy; isotope

The analysis of stable oxygen isotopes in natural systems allows for the elucidation of plant physiological responses to environmental change from the scales of enzymes up through whole plants and ecosystems to the planet. Plants modify the distinct regional and seasonal isotopic signals in environmental water yielding unique tracers in atmospheric CO2, O2 and plant organic material. These signals allow for the partitioning of gross CO2 fluxes on a variety of temporal and spatial scales, the reconstruction of growth environment from seasons to centuries and the estimation of global productivity over millennia. The isotope ratio of leaf-water is central to all of these applications, and is controlled by three physical factors: (i) relative humidity, (ii) the isotope ratio of plant root water and (iii) the isotope ratio of atmospheric water vapor. Our lack of knowledge of the isotope ratio of atmospheric water vapor at any spatial or temporal scale leads to large errors in the interpretation of stable isotope ratios of CO2, O2, and plant organics. This error would be minimized by obtaining integrated estimates of the isotope ratio of atmospheric water vapor through time and space. The objectives of the proposed research are to develop and test models to explain the observed oxygen isotope ratios of leaf water and cellulose of the epiphytic CAM plant Tillandsia usneoides. It is hypothesized that the isotope ratio of leaf water and consequently leaf organic material is controlled by and reflects the isotope ratio of atmospheric water vapor. These predictions will be tested through a combination of laboratory experiments and field campaigns. Contemporary values of the isotope ratio of atmospheric water vapor for annual and monthly timescales will be determined at two isotopically distinct locations in Virginia and Florida; historical values in these regions will be reconstructed using herbarium specimens.The broader impacts of this research represent a characterization of mean values for the oxygen isotope ratio of atmospheric water vapor on an unprecedented spatial and temporal scale. The realized final product of this leaf-level ecophysiological research would be a map of time-integrated atmospheric water vapor from Virginia, USA southwards through the tropics to Argentina. Such a product would benefit broad disciplines of scientific pursuits including ecosystem to global scale estimates of biological productivity, forensic applications, reconstruction of past climates and hydrological models. Additionally, this proposal will train a technician, a graduate student and several undergraduate students in the theory and applications of stable isotopes. These specialized analytical skills are highly marketable in both the public and private sectors.

对自然系统中稳定氧同位素的分析可以阐明植物对环境变化的生理反应，从酶的规模到整个植物和生态系统到地球。 植物改变了环境水中不同的区域和季节性同位素信号，在大气CO2，O2和植物有机物质中产生独特的示踪剂。 这些信号允许在各种时间和空间尺度上划分总CO2通量，重建从季节到世纪的生长环境，并估计千年的全球生产力。 叶水的同位素比是所有这些应用的核心，并由三个物理因素控制：（i）相对湿度，（ii）植物根水的同位素比和（iii）大气水蒸气的同位素比。 我们缺乏在任何空间或时间尺度上的大气水蒸气的同位素比的知识，导致在解释CO2，O2和植物有机物的稳定同位素比时出现很大的误差。通过对大气水蒸气的同位素比率进行时间和空间上的综合估计，可以将这种误差降到最低。 拟议的研究的目标是开发和测试模型来解释观察到的叶水和纤维素的附生CAM植物Tillandsia usneoides的氧同位素比值。 据推测，叶水的同位素比，从而叶有机物质的控制，并反映了大气水蒸气的同位素比。 这些预测将通过实验室实验和实地活动相结合的方式进行检验。 当代值的大气水蒸气的同位素比的年度和月度的时间尺度将确定在两个同位素不同的地点在弗吉尼亚州和佛罗里达;在这些地区的历史价值将重建使用植物标本标本。这项研究的更广泛的影响代表了表征的平均值的大气水蒸气的氧同位素比在一个前所未有的空间和时间尺度。 这一叶级生态生理学研究的最终成果将是一张从美国弗吉尼亚州向南通过热带到阿根廷的时间积分大气水汽图。这种产品将有利于科学研究的广泛学科，包括生态系统到全球规模的生物生产力估计、法医应用、过去气候和水文模型的重建。 此外，该提案将在稳定同位素的理论和应用方面培训一名技术员、一名研究生和几名本科生。这些专业的分析技能在公共和私营部门都很有市场。