Leibniz Institute for Baltic Sea Research Warnemünde, Rostock, Germany.
Leibniz Institute for Plasma Science and Technology e.V. (INP Greifswald), Greifswald, Germany.
Glob Chang Biol. 2018 Nov;24(11):5031-5043. doi: 10.1111/gcb.14424. Epub 2018 Sep 26.
Ocean acidification (OA), arising from the influx of anthropogenically generated carbon, poses a massive threat to the ocean ecosystems. Our knowledge of the effects of elevated anthropogenic CO in marine waters and its effect on the performance of single species, trophic interactions, and ecosystems is increasing rapidly. However, our understanding of the biogeochemical cycling of nutrients such as nitrogen is less advanced and lacks a comprehensive overview of how these processes may change under OA. We conducted a systematic review and meta-analysis of eight major nitrogen transformation processes incorporating 49 publications to synthesize current scientific understanding of the effect of OA on nitrogen cycling in the future ocean by 2100. The following points were identified by our meta-analysis: (a) Diazotrophic nitrogen fixation is likely enhanced by 29% ± 4% under OA; (b) species- and strain-specific responses of nitrogen fixers to OA were detectable, which may result in alterations in microbial community composition in the future ocean; (c) nitrification processes were reduced by a factor of 29% ± 10%; (d) declines in nitrification rates were not reflected by nitrifier abundance; and (e) contrasting results in unispecific culture experiments versus natural communities were apparent for nitrogen fixation and denitrification. The net effect of the nitrogen cycle process responses also suggests there may be a shift in the relative nitrogen pools, with excess ammonium originating from CO -fertilized diazotrophs. This regenerated inorganic nitrogen may recycle in the upper water column increasing the relative importance of the ammonium-fueled regenerated production. However, several feedback mechanisms with other chemical cycles, such as oxygen, and interaction with other climate change stressors may counteract these findings. Finally, our review highlights the shortcomings and gaps in current understanding of the potential changes in nitrogen cycling under future climate and emphasizes the need for further ecosystem studies.
海洋酸化(OA)是由于人为产生的碳涌入而产生的,对海洋生态系统构成了巨大威胁。我们对海洋水中人为升高的 CO 的影响及其对单一物种、营养相互作用和生态系统的性能的影响的了解正在迅速增加。然而,我们对氮等营养物质的生物地球化学循环的理解还不够先进,也缺乏对这些过程在 OA 下可能发生变化的全面了解。我们对八项主要氮转化过程进行了系统回顾和荟萃分析,纳入了 49 篇出版物,以综合当前对未来海洋中 OA 对氮循环影响的科学认识。我们的荟萃分析确定了以下几点:(a)在 OA 下,固氮作用可能增强 29%±4%;(b)对固氮生物对 OA 的种和菌株特异性反应是可检测的,这可能导致未来海洋中微生物群落组成的改变;(c)硝化过程减少了 29%±10%;(d)硝化速率的下降并没有反映在硝化生物的丰度上;(e)氮固定和反硝化作用在单一培养实验与自然群落中的结果相反。氮循环过程响应的净效应还表明,相对氮库可能会发生转移,过量的铵来自 CO 施肥的固氮生物。这种再生无机氮可能在上层水柱中循环,增加了以铵为燃料的再生产量的相对重要性。然而,与其他化学循环(如氧气)的几个反馈机制以及与其他气候变化胁迫因素的相互作用可能会抵消这些发现。最后,我们的综述强调了当前对未来气候下氮循环潜在变化的理解的不足之处和差距,并强调了需要进一步进行生态系统研究。