Department of Geography, University of Hawaii, Honolulu, Hawaii, United States of America.
PLoS Biol. 2013 Oct;11(10):e1001682. doi: 10.1371/journal.pbio.1001682. Epub 2013 Oct 15.
Ongoing greenhouse gas emissions can modify climate processes and induce shifts in ocean temperature, pH, oxygen concentration, and productivity, which in turn could alter biological and social systems. Here, we provide a synoptic global assessment of the simultaneous changes in future ocean biogeochemical variables over marine biota and their broader implications for people. We analyzed modern Earth System Models forced by greenhouse gas concentration pathways until 2100 and showed that the entire world's ocean surface will be simultaneously impacted by varying intensities of ocean warming, acidification, oxygen depletion, or shortfalls in productivity. In contrast, only a small fraction of the world's ocean surface, mostly in polar regions, will experience increased oxygenation and productivity, while almost nowhere will there be ocean cooling or pH elevation. We compiled the global distribution of 32 marine habitats and biodiversity hotspots and found that they would all experience simultaneous exposure to changes in multiple biogeochemical variables. This superposition highlights the high risk for synergistic ecosystem responses, the suite of physiological adaptations needed to cope with future climate change, and the potential for reorganization of global biodiversity patterns. If co-occurring biogeochemical changes influence the delivery of ocean goods and services, then they could also have a considerable effect on human welfare. Approximately 470 to 870 million of the poorest people in the world rely heavily on the ocean for food, jobs, and revenues and live in countries that will be most affected by simultaneous changes in ocean biogeochemistry. These results highlight the high risk of degradation of marine ecosystems and associated human hardship expected in a future following current trends in anthropogenic greenhouse gas emissions.
持续的温室气体排放会改变气候过程,导致海洋温度、pH 值、含氧量和生产力发生变化,进而可能改变生物和社会系统。在这里,我们对未来海洋生物地球化学变量在海洋生物群系中的同步变化进行了综合全球评估,并探讨了其对人类的更广泛影响。我们分析了受温室气体浓度路径驱动的现代地球系统模型直至 2100 年的数据,并表明整个海洋表面将同时受到不同强度的海洋变暖、酸化、缺氧或生产力下降的影响。相比之下,只有世界海洋表面的一小部分,主要在极地地区,将经历增氧和生产力增加,而几乎没有任何地方会出现海洋降温或 pH 值升高。我们汇编了全球 32 个海洋生境和生物多样性热点的分布情况,并发现它们都将同时面临多种生物地球化学变量变化的影响。这种叠加突出了协同生态系统响应的高风险、应对未来气候变化所需的一系列生理适应,以及全球生物多样性格局可能发生重组的可能性。如果同时发生的生物地球化学变化影响海洋货物和服务的提供,那么它们也可能对人类福利产生相当大的影响。世界上大约有 4.7 亿至 8.7 亿最贫困人口严重依赖海洋获取食物、工作和收入,并且生活在受海洋生物地球化学变化影响最大的国家。这些结果突显了在当前人为温室气体排放趋势下,海洋生态系统退化和相关人类困境的高风险。