热带沿海海洋富营养化的扩散和二氧化碳通量的变化:里约热内卢的一些经验教训

G. Abril, Luiz C. Cotovicz Jr., A. Nepomuceno, Thaís Erbas, S. Costa, Vinicius V. Ramos, G. Moser, A. Fernandes, Eduardo Negri, Bastiaan A. Knoppers, N. Brandini, W. Machado, Marcelo Bernardes, V. Vantrepotte
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引用次数: 2

摘要

在巴西和许多其他热带国家,沿海地区的大城市和人口仍在增长,污水处理的覆盖范围远远不够理想。文化富营养化不仅仅是对沿海海洋的威胁;它现在是主要的生物地球化学和生态驱动力之一。在里约热内卢州沿海地区,城市化地区的半封闭海湾和泻湖水体和沉积物中叶绿素a、有机碳和营养物质浓度呈明显的时空上升趋势。作为缓冲,近岸生态系统已变得高度富营养化,其自养代谢已增强,产生强大的二氧化碳(CO2)汇。我们在这里汇编了最近在里约热内卢州的四个沿海海洋生态系统中收集的二氧化碳通量数据:瓜纳巴拉湾和阿鲁阿马、萨夸雷马和Jacarepagua泻湖。我们在污水负荷附近的限制区域观察到强烈的二氧化碳源,在那里微生物降解有机物占主导地位,在限制和近岸微咸、海洋和高咸水中观察到大量的二氧化碳汇,浮游植物大量繁殖。我们还报告了四个生态系统中水中CO2分压与Chl a浓度之间的相关性。沿着巴西海岸的卫星数据表明,由富营养化引起的二氧化碳汇可能发生在许多沿海生态系统中,包括海湾、泻湖和陆架水域,并可能造成额外的蓝碳。额外的有机碳一部分储存在沉积物中,一部分出口到近海。然而,这些额外的蓝碳会对环境产生巨大的影响,因为它会逐渐形成海洋死亡区,并可能导致甲烷(CH4)的产生,这是一种更强大的温室气体。我们强调迫切需要进行多学科研究,以同时促进大气碳的储存,保护热带富营养化沿海海洋的生物多样性和社会经济产品。关键词:热带沿海生态系统,人工富营养化,浮游植物大量繁殖,海洋死区,蓝碳
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SPREADING EUTROPHICATION AND CHANGING CO2 FLUXES IN THE TROPICAL COASTAL OCEAN: A FEW LESSONS FROM RIO DE JANEIRO
In Brazil and in many other tropical countries, large urban cities and populations are still growing on the coast and coverage in terms of sewage treatments is far from desirable. Cultural eutrophication is not solely a threat for the coastal ocean; it is now acting as one of its major biogeochemical and ecological driver. Along the littoral of the state of Rio de Janeiro, semi-enclosed marine bays and lagoons show clear spatial and temporal pattern of increasing concentrations of chlorophyll a (Chl a), organic carbon, and nutrients in their waters and sediments in urbanized regions. Acting as a buffer, the nearshore ecosystems have turned highly eutrophic and their autotrophic metabolism has been enhanced creating strong carbon dioxide (CO2) sinks. We compile here data of CO2fluxes recently gathered in four coastal marine ecosystems in the state of Rio de Janeiro: the Guanabara Bay and the Araruama, Saquarema and Jacarepagua lagoons. We observed intense CO2 sources in restricted areas at the vicinity of sewage loads, where microbial degradation of organic matter predominates, and large CO2 sinks in confined and nearshore brackish, marine and hypersaline waters, where phytoplankton blooms occur. We also report a correlation across the four ecosystems between the partial pressure of CO2 in waters and the Chl a concentration. Chl a satellite data all along the Brazilian coast suggest that the CO2 sink induced by eutrophication probably occurs in many coastal ecosystems including bays, lagoon and shelf waters, and could contribute to an additional blue carbon. Part of the additional organic carbon is stored in sediments, and part is exported offshore. However, this additional blue carbon has dramatic environment impacts as it would evolve toward the formation of marine dead zones, and could contribute to a production of methane (CH4) a more powerful greenhouse gas. We emphasize an urgent need for multidisciplinary research to promote simultaneously the storage of atmospheric carbon, and the preservation of biodiversity and socio-economic goods in the eutrophic tropical coastal ocean. Keywords: tropical coastal ecosystems, cultural eutrophication, phytoplankton blooms, marine dead zones, blue carbon
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