Department of Marine Ecology, University of Bremen, Bremen, Germany.
Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Netherlands Institute for Sea Research, Texel, Netherlands.
mSystems. 2024 Nov 19;9(11):e0083224. doi: 10.1128/msystems.00832-24. Epub 2024 Oct 22.
High molecular weight (HMW; >1 kDa) carbohydrates are a major component of dissolved organic matter (DOM) released by benthic primary producers. Despite shifts from coral to algae dominance on many reefs, little is known about the effects of exuded carbohydrates on bacterioplankton communities in reef waters. We compared the monosaccharide composition of HMW carbohydrates exuded by hard corals and brown macroalgae and investigated the response of the bacterioplankton community of an algae-dominated Caribbean reef to the respective HMW fractions. HMW coral exudates were compositionally distinct from the ambient, algae-dominated reef waters and similar to coral mucus (high in arabinose). They further selected for opportunistic bacterioplankton taxa commonly associated with coral stress (i.e., , , , and ) and significantly increased the predicted energy-, amino acid-, and carbohydrate-metabolism by 28%, 44%, and 111%, respectively. In contrast, HMW carbohydrates exuded by algae were similar to those in algae tissue extracts and reef water (high in fucose) and did not significantly alter the composition and predicted metabolism of the bacterioplankton community. These results confirm earlier findings of coral exudates supporting efficient trophic transfer, while algae exudates may have stimulated microbial respiration instead of biomass production, thereby supporting the microbialization of reefs. In contrast to previous studies, HMW coral and not algal exudates selected for opportunistic microbes, suggesting that a shift in the prevalent DOM composition and not the exudate type (i.e., coral vs algae) , may induce the rise of opportunistic microbial taxa.
Dissolved organic matter (DOM) released by benthic primary producers fuels coral reef food webs. Anthropogenic stressors cause shifts from coral to algae dominance on many reefs, and resulting alterations in the DOM pool can promote opportunistic microbes and potential coral pathogens in reef water. To better understand these DOM-induced effects on bacterioplankton communities, we compared the carbohydrate composition of coral- and macroalgae-DOM and analyzed the response of bacterioplankton from an algae-dominated reef to these DOM types. In line with the proposed microbialization of reefs, coral-DOM was efficiently utilized, promoting energy transfer to higher trophic levels, whereas macroalgae-DOM likely stimulated microbial respiration over biomass production. Contrary to earlier findings, coral- and not algal-DOM selected for opportunistic microbial taxa, indicating that a change in the prevalent DOM composition, and not DOM type, may promote the rise of opportunistic microbes. Presented results may also apply to other coastal marine ecosystems undergoing benthic community shifts.
高分子量(HMW;>1 kDa)碳水化合物是底栖初级生产者释放的溶解有机物质(DOM)的主要成分。尽管许多珊瑚礁的优势从珊瑚转变为藻类,但对于渗出的碳水化合物对珊瑚礁水中的细菌浮游生物群落的影响知之甚少。我们比较了硬珊瑚和褐藻分泌的 HMW 碳水化合物的单糖组成,并研究了藻类占主导地位的加勒比海珊瑚礁的细菌浮游生物群落对各自 HMW 分数的反应。HMW 珊瑚分泌物的组成与环境中以藻类为主的珊瑚礁水不同,与珊瑚黏液相似(阿拉伯糖含量高)。它们进一步选择了与珊瑚压力相关的机会主义细菌分类群(即 、 、 、和 ),并分别显著增加了预测的能量、氨基酸和碳水化合物代谢 28%、44%和 111%。相比之下,藻类分泌的 HMW 碳水化合物与藻类组织提取物和珊瑚礁水相似(岩藻糖含量高),并没有显著改变细菌浮游生物群落的组成和预测的代谢。这些结果证实了先前的发现,即珊瑚分泌物支持有效的营养转移,而藻类分泌物可能刺激微生物呼吸而不是生物量产生,从而支持珊瑚礁的微生物化。与以前的研究不同,HMW 珊瑚而不是藻类分泌物选择了机会主义微生物,这表明 DOM 组成的变化而不是外泌体类型(即珊瑚与藻类)可能导致机会主义微生物分类群的增加。
底栖初级生产者释放的溶解有机物质(DOM)为珊瑚礁食物网提供燃料。人为压力导致许多珊瑚礁从珊瑚转变为藻类占主导地位,DOM 池的这种变化可能会促进珊瑚礁水中的机会主义微生物和潜在的珊瑚病原体。为了更好地了解这些 DOM 对细菌浮游生物群落的影响,我们比较了珊瑚和大型藻类 DOM 的碳水化合物组成,并分析了藻类占主导地位的珊瑚礁中细菌浮游生物对这些 DOM 类型的反应。与提出的珊瑚礁微生物化一致,珊瑚 DOM 被有效地利用,促进了能量向更高营养级别的转移,而大型藻类 DOM 可能刺激了微生物呼吸而不是生物量的产生。与早期的发现相反,珊瑚 DOM 而不是藻类 DOM 选择了机会主义微生物分类群,这表明流行的 DOM 组成的变化,而不是 DOM 类型,可能促进了机会主义微生物的出现。提出的结果也可能适用于其他正在经历底栖群落变化的沿海海洋生态系统。