Goldberg S J, Nelson C E, Viviani D A, Shulse C N, Church M J
Center for Microbial Oceanography: Research and Education, Department of Oceanography, School of Ocean and Earth Science and Technology, University of Hawai'i at Mānoa, 1950 East West Road, Honolulu, HI 96822, USA.
Center for Microbial Oceanography: Research and Education, Department of Oceanography and Sea Grant College Program, School of Ocean and Earth Science and Technology, University of Hawai'i at Mānoa, 1950 East West Road, Honolulu, HI 96822, USA.
Environ Microbiol. 2017 Sep;19(9):3450-3464. doi: 10.1111/1462-2920.13825. Epub 2017 Aug 14.
Nitrogen frequently limits oceanic photosynthesis and the availability of inorganic nitrogen sources in the surface oceans is shifting with global change. We evaluated the potential for abrupt increases in inorganic N sources to induce cascading effects on dissolved organic matter (DOM) and microbial communities in the surface ocean. We collected water from 5 m depth in the central North Pacific and amended duplicate 20 liter polycarbonate carboys with nitrate or ammonium, tracking planktonic carbon fixation, DOM production, DOM composition and microbial community structure responses over 1 week relative to controls. Both nitrogen sources stimulated bulk phytoplankton, bacterial and DOM production and enriched Synechococcus and Flavobacteriaceae; ammonium enriched for oligotrophic Actinobacteria OM1 and Gammaproteobacteria KI89A clades while nitrate enriched Gammaproteobacteria SAR86, SAR92 and OM60 clades. DOM resulting from both N enrichments was more labile and stimulated growth of copiotrophic Gammaproteobacteria (Alteromonadaceae and Oceanospirillaceae) and Alphaproteobacteria (Rhodobacteraceae and Hyphomonadaceae) in weeklong dark incubations relative to controls. Our study illustrates how nitrogen pulses may have direct and cascading effects on DOM composition and microbial community dynamics in the open ocean.
氮素常常限制海洋光合作用,且随着全球变化,海洋表层无机氮源的可利用性正在发生改变。我们评估了无机氮源突然增加对海洋表层溶解有机物(DOM)和微生物群落产生级联效应的可能性。我们从北太平洋中部5米深处采集海水,并在20升的重复聚碳酸酯大玻璃瓶中添加硝酸盐或铵盐,相对于对照组,追踪浮游植物碳固定、DOM产生、DOM组成和微生物群落结构在1周内的响应。两种氮源均刺激了浮游植物、细菌的大量繁殖以及DOM的产生,并使聚球藻属和黄杆菌科富集;铵盐使贫营养放线菌OM1和γ-变形菌KI89A进化枝富集,而硝酸盐使γ-变形菌SAR86、SAR92和OM60进化枝富集。与对照组相比,两种氮添加导致的DOM在为期一周的黑暗培养中更不稳定,并刺激了富营养γ-变形菌(交替单胞菌科和海螺旋菌科)和α-变形菌(红杆菌科和生丝微菌科)的生长。我们的研究表明,氮脉冲如何可能对开阔海洋中的DOM组成和微生物群落动态产生直接和级联效应。