Shi Penglan, Wang Huan, Feng Mingjun, Cheng Haowu, Yang Qian, Yan Yifeng, Xu Jun, Zhang Min
Hubei Provincial Engineering Laboratory for Pond Aquaculture, Engineering Research Center of Green Development for Conventional Aquatic Biological Industry in the Yangtze River Economic Belt, Ministry of Education, College of Fisheries, Huazhong Agricultural University, Wuhan 430070, China.
State Key Laboratory of Marine Resource Utilization in South China Sea, Hainan University, Haikou 570228, China.
Microorganisms. 2022 Jun 30;10(7):1327. doi: 10.3390/microorganisms10071327.
Increased decomposition rates in shallow lakes with global warming might increase the release of atmospheric greenhouse gases, thereby producing positive feedback for global warming. However, how climate warming affects litter decomposition is still unclear in lake ecosystems. Here, we tested the effects of constant and variable warming on the bacterial metabolic potential of typically submerged macrophyte ( L.) litters during decomposition in 18 mesocosms (2500 L each). The results showed that warming reduced main chemoheterotrophic metabolic potential but promoted methylotrophy metabolism, which means that further warming may alter methane-cycling microbial metabolism. The nitrate reduction function was inhibited under warming treatments, and nitrogen fixation capability significantly increased under variable warming in summer. The changes in dissolved oxygen (DO), pH, conductivity and ammonium nitrogen driven by warming are the main environmental factors affecting the bacteria's metabolic potential. The effects of warming and environmental factors on fermentation, nitrate reduction and ammonification capabilities in stem and leaf litter were different, and the bacterial potential in the stem litter were more strongly responsive to environmental factors. These findings suggest that warming may considerably alter bacterial metabolic potential in macrophyte litter, contributing to long-term positive feedback between the C and N cycle and climate.
随着全球变暖,浅水湖泊中分解速率的增加可能会导致大气温室气体排放增加,从而对全球变暖产生正反馈。然而,在湖泊生态系统中,气候变暖如何影响凋落物分解仍不清楚。在此,我们在18个中型生态系统(每个2500升)中测试了恒定变暖和波动变暖对典型沉水植物(L.)凋落物在分解过程中细菌代谢潜力的影响。结果表明,变暖降低了主要化学异养代谢潜力,但促进了甲基营养代谢,这意味着进一步变暖可能会改变甲烷循环微生物代谢。在变暖处理下,硝酸盐还原功能受到抑制,夏季波动变暖下固氮能力显著增加。变暖驱动的溶解氧(DO)、pH值、电导率和铵态氮的变化是影响细菌代谢潜力的主要环境因素。变暖和环境因素对茎叶凋落物中发酵、硝酸盐还原和氨化能力的影响不同,茎凋落物中的细菌潜力对环境因素的响应更强。这些发现表明,变暖可能会显著改变大型植物凋落物中的细菌代谢潜力,从而导致碳氮循环与气候之间的长期正反馈。