权益分类	功能权益	普通用户	{{item.name}}会员
{{category.name}}	{{benefitItem.name}}

Collaborative Research: Regional variation of phytoplankton diversity and biogeochemical functioning in the subtropical Indian Ocean

合作研究：副热带印度洋浮游植物多样性和生物地球化学功能的区域变化

基本信息

批准号：
1559002
负责人：
Adam Martiny
金额：
$ 29.42万
依托单位：
University of California-Irvine
依托单位国家：
美国
项目类别：
Standard Grant
财政年份：
2016
资助国家：
美国
起止时间：
2016-02-15 至 2018-12-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1559002&HistoricalAwards=false
关键词：
Collaborative Research Regional variation phytoplankton

项目摘要

The Indian Ocean accounts for nearly a fifth of global ocean photosynthesis and is likely a key component in global ocean nutrient and carbon cycles. However, the Indian Ocean may be the least studied major marine body on the planet. Our limited understanding suggests extensive variations in physical and chemical environmental conditions, but how this variation influences biodiversity, nutrient stress, and more broadly regional differences in the functioning of phytoplankton is unknown. To help address these gaps, the investigators will conduct a study by joining an already-funded major research cruise to this region. It will cover a northern region with some of the highest temperatures recorded in open ocean waters, an area around 10°S of predicted (but not tested in situ) iron stress, and a southern subtropical gyre with unique nitrogen to phosphorous(or N:P) ratios. The focus of this project is to quantify and synthesize the interconnectedness of environmental conditions, phytoplankton diversity and genome content, and nutrient biogeochemistry, with the goal of understanding how these may lead to unique biogeochemical regions in Indian Ocean. The research will have broader impacts on many levels. First, it will increase public awareness of the role of phytoplankton on ocean functioning, climate, and people's lives through a new partnership with the Aquarium of the Pacific (AOP), which is the fourth most-attended aquarium in the nation. Secondly, the project will train a postdoctoral scholar as well as a graduate and undergraduate students. Third, the research will dramatically increase our basic knowledge ocean biogeochemistry and in many cases will be the first measurements of their kind made in the Indian Ocean.This project will address two major questions: How do environmental conditions, phytoplankton diversity, phytoplankton physiology, and biogeochemistry vary across the central Indian Ocean? Are there distinct biogeochemical regimes in the central IO? The researchers hypothesize that environmental conditions, including the relative availability of nitrogen (N) and iron (Fe), lead to three distinct phytoplankton communities and biogeochemical regimes. They will employ a series of advanced analytical tools including high sensitivity measurements of dissolved and particulate nutrients (nitrogen, phosphorus, and iron), genomics, bioassays to test for nutrient stress, and cell-sorting of specific taxa followed by measures of nutrient content and uptake. A focus of this project is to quantify and synthesize the interconnectedness of environmental conditions, phytoplankton diversity and genome content, and nutrient biogeochemistry, and how these lead to unique biogeochemical regions in Indian Ocean. This extensive set of observations can ultimately be linked to ocean models and satellite data to provide a comprehensive view of regional differences in chemistry, biodiversity and phytoplankton biogeochemical functioning in the Indian Ocean.

印度洋占全球海洋光合作用的近五分之一，可能是全球海洋养分和碳循环的关键组成部分。然而，印度洋可能是地球上研究最少的主要海洋。我们有限的了解表明物理和化学环境条件存在广泛的变化，但这种变化如何影响生物多样性，营养压力以及浮游植物功能的更广泛的区域差异尚不清楚。为了帮助解决这些差距，调查人员将通过加入一个已经资助的主要研究巡航到该地区进行研究。它将覆盖北方地区，其中一些地区的最高温度记录在开放的海洋沃茨，一个地区约10°S的预测（但未在现场测试）铁应力，以及一个南亚热带环流与独特的氮磷（或N：P）比。该项目的重点是量化和综合环境条件、浮游植物多样性和基因组含量以及营养物地球化学之间的相互联系，目的是了解这些因素如何导致印度洋独特的地球化学区域。这项研究将在许多层面上产生更广泛的影响。首先，它将通过与太平洋水族馆（AOP）建立新的伙伴关系，提高公众对浮游植物对海洋功能，气候和人们生活的作用的认识，该水族馆是全国第四大最受欢迎的水族馆。第二，培养一名博士后，一名研究生和一名本科生。第三，这项研究将极大地增加我们对海洋生物地球化学的基本知识，在许多情况下，这将是在印度洋进行的第一次此类测量。该项目将解决两个主要问题：环境条件、浮游植物多样性、浮游植物生理学和海洋生物地球化学在印度洋中部是如何变化的？在IO中心是否存在不同的地球化学机制？研究人员假设，环境条件，包括氮（N）和铁（Fe）的相对可用性，导致三种不同的浮游植物群落和生物地球化学体系。他们将采用一系列先进的分析工具，包括溶解和颗粒营养物质（氮，磷和铁）的高灵敏度测量，基因组学，生物测定，以测试营养胁迫，以及特定分类群的细胞分选，然后测量营养含量和吸收。该项目的一个重点是量化和综合环境条件，浮游植物多样性和基因组含量，以及营养盐地球化学的相互联系，以及这些如何导致印度洋独特的地球化学区域。这套广泛的观测数据最终可以与海洋模型和卫星数据联系起来，以全面了解印度洋化学、生物多样性和浮游植物生物地球化学功能的区域差异。