Long-Term Warming of Baltic Sea Coastal Waters Affects Bacterial Communities in Bottom Water and Sediments Differently

被引:12
|
作者
Seidel, Laura [1 ]
Broman, Elias [1 ,2 ]
Stahle, Magnus [1 ]
Nilsson, Emelie [1 ]
Turner, Stephanie [1 ]
Hendrycks, Wouter [1 ,3 ]
Sachpazidou, Varvara [1 ]
Forsman, Anders [1 ]
Hylander, Samuel [1 ]
Dopson, Mark [1 ]
机构
[1] Linnaeus Univ, Ctr Ecol & Evolut Microbial Model Syst EEMiS, Kalmar, Sweden
[2] Stockholm Univ, Dept Ecol Environm & Plant Sci, Stockholm, Sweden
[3] Univ Antwerp, Dept Biol, Evolutionary Ecol, Antwerp, Belgium
基金
瑞典研究理事会;
关键词
climate change; marine waters; cyanobacteria; 16S rRNA gene amplicon sequencing; seasonal shifts; DIVERSITY; ASSIMILATION; TEMPERATURE; WARMER; OXYGEN;
D O I
10.3389/fmicb.2022.873281
中图分类号
Q93 [微生物学];
学科分类号
071005 ; 100705 ;
摘要
Coastal marine ecosystems are some of the most diverse natural habitats while being highly vulnerable in the face of climate change. The combination of anthropogenic influence from land and ongoing climate change will likely have severe effects on the environment, but the precise response remains uncertain. This study compared an unaffected "control" Baltic Sea bay to a "heated" bay that has undergone artificial warming from cooling water release from a nuclear power plant for ~50 years. This heated the water in a similar degree to IPCC SSP5-8.5 predictions by 2100 as natural systems to study temperature-related climate change effects. Bottom water and surface sediment bacterial communities and their biogeochemical processes were investigated to test how future coastal water warming alters microbial communities; shifts seasonal patterns, such as increased algae blooming; and influences nutrient and energy cycling, including elevated respiration rates. 16S rRNA gene amplicon sequencing and geochemical parameters demonstrated that heated bay bottom water bacterial communities were influenced by increased average temperatures across changing seasons, resulting in an overall Shannon's H diversity loss and shifts in relative abundances. In contrast, Shannon's diversity increased in the heated surface sediments. The results also suggested a trend toward smaller-sized microorganisms within the heated bay bottom waters, with a 30% increased relative abundance of small size picocyanobacteria in the summer (June). Furthermore, bacterial communities in the heated bay surface sediment displayed little seasonal variability but did show potential changes of long-term increased average temperature in the interplay with related effects on bottom waters. Finally, heated bay metabolic gene predictions from the 16S rRNA gene sequences suggested raised anaerobic processes closer to the sediment-water interface. In conclusion, climate change will likely alter microbial seasonality and diversity, leading to prolonged and increased algae blooming and elevated respiration rates within coastal waters.
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收藏
页数:19
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