Fate of ocean oxygenation in a warming world

变暖世界中海洋氧化的命运

• 批准号: MR/S034293/1
• 负责人: Babette Hoogakker
• 金额: $ 124.52万
• 依托单位: Heriot-Watt University
• 依托单位国家: 英国
• 项目类别: Fellowship
• 财政年份: 2019
• 资助国家: 英国
• 起止时间: 2019 至 无数据
• 项目状态: 已结题
• 来源: https://gtr.ukri.org/projects?ref=MR%2FS034293%2F1
• 关键词: Fate; ocean; oxygenation; warming; world

Oxygen is critical to the health of all higher life. In the oceans dissolved oxygen concentrations have declined by 2% since 1960, and are expected to continue to decline into the future in relation to man-made climate change. Future deoxygenation, along with overfishing, threatens the sustainability of economically important fisheries and marine ecosystems and will impact global biogeochemical cycles. It is therefore crucial that we obtain a well-informed view about what the future may hold.Current model simulations that predict the future carry considerable uncertainties; they do not all agree and grossly underestimate the document decrease of the last 50 years. This suggests the models are missing key interactions, calling for urgent action and a dedicated and inclusive scientific approach. FARGO provides such an approach by addressing why, and to what extent, seawater dissolved oxygen concentrations may change in a warming world. FARGO will study dissolved oxygen concentrations in the Pacific Ocean, the largest low-oxic water body in the current ocean, through an innovative and dedicated research programme incorporating a novel multi-proxy approach feeding IPCC-type climate model simulations across key warm time intervals:i- warmer climates across the closure of the American sea-way (4-15 million years);ii- warmer climates as future analogue (mid-Pliocene Warm Period, 3.3 to 3 million years ago);iii- Pleistocene warm intervals (interglacials of the last ca. 800,000 years). FARGO is structured into two phases: Phase I (years 1-4), and Phase II (years 5-7). The focus of the first four years is analytical, to advance method development and reconstruct time-series of oxygen concentrations and associated processes that drive changes (seawater warming, stratification, productivity, ventilation). The material FARGO will use to create these time-series involves the shells of microorganisms called foraminifera. Some species float near the ocean surface, called planktonic foraminifera, and can be used to assess the presence of subsurface oxygen minimum zones, seawater temperatures, etc. Species that live on or in sediments at the bottom of the ocean are termed benthic foraminifera and can be used to reconstruct bottom water oxygen concentrations and ventilation. FARGO will use sediments from the International Ocean Discovery Program to determine if there have been changes in the natural extent and intensity of the shallow Pacific Ocean OMZ oxygen minimum, or 'dead', zones (e.g. areas where oxygen levels are too low to support aerobic life), during the key warm intervals. The original time-series will feed the IPCC-type climate model simulations and provide robust tests to investigate if the simulations are realistic and correct for the specific time periods, and identify routes to improve the model simulations. Utilizing these improvements, FARGO will carry out simulations for future, including 1.5 and 2 degree warming scenarios.To raise awareness of ocean deoxygenation FARGO plans several bespoke impact and engagement activities aimed at scientific peers, policy makers, and the general public. To slow/reduce deoxygenation and protect our marine environment FARGO plans to work with government (Scottish and UK) to develop regional legislation to manage nutrient inputs from aquaculture and agriculture of UK waters.

氧气对所有高等生物的健康至关重要。自1960年以来，海洋中的溶解氧浓度下降了2%，而且由于人为的气候变化，预计未来还会继续下降。未来的脱氧与过度捕捞一起，威胁着具有重要经济意义的渔业和海洋生态系统的可持续性，并将影响全球生物地球化学循环。因此，至关重要的是，我们要对未来可能会发生什么有一个充分的了解。目前预测未来的模式模拟具有相当大的不确定性；他们并不都同意并严重低估了过去50年的文件减少。这表明这些模型缺少关键的相互作用，呼吁采取紧急行动和专门的、包容性的科学方法。FARGO提供了这样一种方法，它解决了海水溶解氧浓度在变暖的世界中可能发生变化的原因和程度。FARGO将通过一项创新和专门的研究计划，研究太平洋的溶解氧浓度，太平洋是目前海洋中最大的低氧水体，该研究计划结合了一种新的多代理方法，为ipcc型气候模型模拟提供关键温暖时间间隔：i-美国海路关闭期间（400万至1500万年）的温暖气候；ii-较暖气候作为未来的类似物（上新世中期暖期，330万至300万年前）；iii-更新世暖期（最近约80万年的间冰期）。法戈项目分为两个阶段：第一阶段（1-4年）和第二阶段（5-7年）。前四年的重点是分析，以推进方法开发和重建氧浓度的时间序列和驱动变化的相关过程（海水变暖，分层，生产力，通风）。FARGO将用于创建这些时间序列的材料涉及被称为有孔虫的微生物的外壳。有些物种漂浮在海面附近，被称为浮游有孔虫，可以用来评估地下氧气最低带的存在，海水温度等。生活在海底沉积物上或沉积物中的物种被称为底栖有孔虫，可以用来重建底部水的氧气浓度和通风。FARGO将使用来自国际海洋发现计划的沉积物来确定在关键的温暖间隔期间，太平洋浅层OMZ氧最小值或“死亡”区域（例如氧气水平过低而无法支持有氧生命的区域）的自然范围和强度是否发生了变化。原始的时间序列将为ipcc型气候模式模拟提供数据，并提供可靠的测试，以调查模拟在特定时间段内是否真实和正确，并确定改进模式模拟的途径。利用这些改进，FARGO将对未来进行模拟，包括1.5度和2度的变暖情景。为了提高人们对海洋脱氧的认识，FARGO计划了一些针对科学界同行、政策制定者和公众的定制影响和参与活动。为了减缓/减少脱氧和保护我们的海洋环境，FARGO计划与政府（苏格兰和英国）合作，制定区域立法来管理英国水域水产养殖和农业的营养投入。

项目成果

Planktonic foraminifera organic carbon isotopes as archives of upper ocean carbon cycling.

• DOI: 10.1038/s41467-022-32480-0
• 发表时间: 2022-08-17
• 期刊: Nature communications
• 影响因子: 16.6

Supplementary material to "Reviews and syntheses: Review of proxies for low-oxygen paleoceanographic reconstructions "

“审查和综合：低氧古海洋学重建代理审查”的补充材料

• DOI: 10.5194/egusphere-2023-2981-supplement
• 发表时间: 2024
• 作者: Hoogakker B

Effect of an Open Central American Seaway on Ocean Circulation and the Oxygen Minimum Zone in the Tropical Pacific From Model Simulations

• DOI: 10.1029/2023gl103728
• 发表时间: 2023-10
• 期刊: Geophysical Research Letters
• 影响因子: 5.2
• 作者: V. Khon;B. Hoogakker;B. Schneider;J. Segschneider;W. Park

Editorial: Facing Marine Deoxygenation

社论：面临海洋脱氧

• DOI: 10.3389/fmars.2020.00046
• 发表时间: 2020
• 期刊: Frontiers in Marine Science
• 影响因子: 3.7
• 作者: Capet A

Evolution of the tropical Pacific oxygen minimum zone during the Miocene-Pliocene from model simulations: A role of the Panama Isthmus closure 

模型模拟中中新世-上新世期间热带太平洋氧气最低区的演化：巴拿马地峡闭合的作用

• DOI: 10.5194/egusphere-gc10-pliocene-65
• 发表时间: 2022
• 作者: Khon V