Department of Biological & Environmental Sciences - Tjärnö, University of Gothenburg, Sweden.
Ambio. 2012 Sep;41(6):637-44. doi: 10.1007/s13280-012-0326-x.
Increasing partial pressure of atmospheric CO₂ is causing ocean pH to fall-a process known as 'ocean acidification'. Scenario modeling suggests that ocean acidification in the Baltic Sea may cause a ≤ 3 times increase in acidity (reduction of 0.2-0.4 pH units) by the year 2100. The responses of most Baltic Sea organisms to ocean acidification are poorly understood. Available data suggest that most species and ecologically important groups in the Baltic Sea food web (phytoplankton, zooplankton, macrozoobenthos, cod and sprat) will be robust to the expected changes in pH. These conclusions come from (mostly) single-species and single-factor studies. Determining the emergent effects of ocean acidification on the ecosystem from such studies is problematic, yet very few studies have used multiple stressors and/or multiple trophic levels. There is an urgent need for more data from Baltic Sea populations, particularly from environmentally diverse regions and from controlled mesocosm experiments. In the absence of such information it is difficult to envision the likely effects of future ocean acidification on Baltic Sea species and ecosystems.
大气中二氧化碳分压的增加导致海洋 pH 值下降——这一过程被称为“海洋酸化”。情景模型表明,到 2100 年,波罗的海的海洋酸化可能导致酸度增加≤3 倍(降低 0.2-0.4 个 pH 单位)。大多数波罗的海生物对海洋酸化的反应仍知之甚少。现有数据表明,波罗的海食物网中的大多数物种和生态重要群体(浮游植物、浮游动物、大型底栖动物、鳕鱼和鲱鱼)将能够适应预期的 pH 值变化。这些结论来自(主要)单一物种和单一因素的研究。然而,很少有研究使用多种胁迫因素和/或多个营养水平来确定海洋酸化对生态系统的综合影响。迫切需要来自波罗的海种群的更多数据,特别是来自环境多样的地区和受控的中观实验。在缺乏这些信息的情况下,很难想象未来海洋酸化对波罗的海物种和生态系统的可能影响。