Utilization and degradation of laminarin-based substrates by marine yeasts suggests their niche-specific role in microbial loop dynamics.

Berin Arslan-Gatz, Mikkel Schultz-Johansen, Tom-Niklas Hollwedel, Sofie Niggemeier, Rolf Nimzyk, Antje Wichels, Gunnar Gerdts, Jan-Hendrik Hehemann, Tilmann Harder, Marlis Reich
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Abstract

In the oceans, the diversity of phytoplankton primary products supports a wide range of microbial heterotrophs, including bacteria and fungi. The organic substrate dynamics within pelagic microbial communities are strongly controlled by microorganismal interactions, resulting in a dense interactome. While the role of bacteria in the microbial loop is well documented, the degradation capacity and substrate specificity of marine fungi, as well as their role and function in metabolic guilds with bacteria, is comparatively less understood. We chose the polysaccharide laminarin, a major product of marine primary production, as well as oligomeric laminarin subunits and monomeric glucose, to study the degradation capacity of eleven marine yeast isolates from the pelagic microbial community of Helgoland Roads. Our aim was to measure yeast growth and correlate degradation yields and putative intermediate degradation products with the size of laminarin-based organic precursor substrates. We developed a reproducible, temporally resolved, high-throughput growth protocol to measure resource-specific yeast growth. Measurement of temporally fine-scaled growth kinetic models of isolates were accompanied with qualitative and quantitative chemical analyses of substrates and degradation intermediates. Our data showed that yeast growth was negatively correlated with oligomer length. Fluorophore-assisted carbohydrate electrophoresis suggested the lack of enzymatic endo-activity for laminarin in yeasts under investigation, suggesting they may occupy a niche in the microbial loop, benefitting from extracellular hydrolysis of carbohydrates by other microorganisms. In terrestrial environments, namely forest soil ecosystems, yeasts have been assigned a similar niche, supporting a prominent role of yeasts in microbial interactomes.
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海洋酵母菌利用和降解以层皮素为基础的底物,表明它们在微生物环路动力学中发挥着特定的生态位作用。
在海洋中,浮游植物初级产品的多样性为包括细菌和真菌在内的各种微生物异养生物提供了支持。浮游微生物群落中的有机基质动态受到微生物相互作用的强烈控制,从而形成了一个密集的相互作用组。虽然细菌在微生物循环中的作用已被充分记录,但人们对海洋真菌的降解能力和底物特异性,以及它们在与细菌的代谢行会中的作用和功能的了解却相对较少。我们选择了海洋初级生产的主要产物--多糖层粘菌素以及低聚层粘菌素亚基和单体葡萄糖,来研究赫尔戈兰路浮游微生物群落中 11 个海洋酵母分离物的降解能力。我们的目的是测量酵母的生长情况,并将降解产量和推测的中间降解产物与基于层素的有机前体底物的大小联系起来。我们开发了一种可重复的、时间分辨率高的高通量生长方案来测量特定资源的酵母生长。在测量分离物的时间微尺度生长动力学模型的同时,还对底物和降解中间产物进行了定性和定量化学分析。我们的数据显示,酵母的生长与寡聚体的长度呈负相关。荧光团辅助碳水化合物电泳表明,所研究的酵母菌对层粘蛋白缺乏酶内活性,这表明它们可能在微生物循环中占据了一个位置,从其他微生物对碳水化合物的胞外水解中获益。在陆地环境(即森林土壤生态系统)中,酵母菌也被赋予了类似的生态位,这支持了酵母菌在微生物相互作用组中的突出作用。
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