Center for Marine Environmental Ecology, School of Environmental Science and Engineering, Tianjin Universitygrid.33763.32, Tianjin, China.
School of Marine and Atmospheric Sciences, Stony Brook Universitygrid.36425.36, Stony Brook, New York, USA.
Microbiol Spectr. 2022 Jun 29;10(3):e0014422. doi: 10.1128/spectrum.00144-22. Epub 2022 May 3.
Labyrinthulomycetes protists are an important heterotrophic component of microeukaryotes in the world's oceans, but their distribution patterns and ecological roles are poorly understood in pelagic waters. This study employed flow cytometry and high-throughput sequencing to characterize the abundance, diversity, and community structure of Labyrinthulomycetes in the pelagic Eastern Indian Ocean. The total Labyrinthulomycetes abundance varied much more among stations than did the abundance of prokaryotic plankton, reaching over 1,000 cells mL at a few "bloom" stations. The total Labyrinthulomycetes abundance did not decline with depth throughout the whole water column (5 to 2,000 m) like the abundance of prokaryotic plankton did, and the Labyrinthulomycetes average projected biomass over all samples was higher than that of the prokaryotic plankton. However, Labyrinthulomycetes diversity showed obvious vertical variations, with richness, Shannon diversity, and evenness greatest in the upper epipelagic, lower epipelagic, and deep waters, respectively. Many abundant phylotypes were detected across multiple water layers, which aligned with the constant vertical Labyrinthulomycetes biomass, suggesting potential sinking and contribution to the biological pump. Hierarchical clustering revealed distinct ecotypes partitioning by vertical distribution patterns, suggesting their differential roles in the carbon cycle and storage processes. Particularly, most phylotypes showed patchy distributions (occurring in only few samples) as previously found in the coastal waters, but they were less associated with the Labyrinthulomycetes blooms than the prevalent phylotypes. Overall, this study revealed distinct patterns of Labyrinthulomycetes ecotypes and shed light on their importance in the pelagic ocean carbon cycling and sequestration relative to that of the prokaryotic plankton. While prokaryotic heterotrophic plankton are well accepted as major players in oceanic carbon cycling, the ecological distributions and functions of their microeukaryotic counterparts in the pelagic ocean remain largely unknown. This study focused on an important group of heterotrophic (mainly osmotrophic) protistan microbes, the Labyrinthulomycetes, whose biomass can surpass that of the prokaryotic plankton in many marine ecosystems, including the bathypelagic ocean. We found patchy horizontal but persistent vertical abundance profiles of the Labyrinthulomycetes protists in the pelagic waters of the Eastern Indian Ocean, which were distinct from the spatial patterns of the prokaryotic plankton. Moreover, multiple Labyrinthulomycetes ecotypes with distinct vertical patterns were detected and, based on the physiologic, metabolic, and genomic understanding of their cultivated relatives, were inferred to play multifaceted key roles in the carbon cycle and sequestration, particularly as contributors to the vertical carbon export from the surface to the dark ocean, i.e., the biological pump.
裂殖菌类原生动物是世界海洋中微真核生物的重要异养成分,但它们在远洋水域中的分布模式和生态角色还知之甚少。本研究采用流式细胞术和高通量测序技术,描述了东印度洋远洋水域中裂殖菌类原生动物的丰度、多样性和群落结构。裂殖菌类原生动物的总丰度在站位之间的变化比原核浮游生物的丰度大得多,在几个“爆发”站位达到了超过 1000 个细胞/mL。裂殖菌类原生动物的总丰度并没有像原核浮游生物那样随深度在整个水柱(5 至 2000 米)下降,而所有样本的裂殖菌类原生动物平均预测生物量都高于原核浮游生物。然而,裂殖菌类原生动物的多样性表现出明显的垂直变化,在上层真光层、中层真光层和深海中分别具有较高的丰富度、香农多样性和均匀度。许多丰富的类群在多个水层中被检测到,这与裂殖菌类原生动物的垂直生物量一致,表明它们有潜在的下沉和对生物泵的贡献。层次聚类揭示了不同的生态型通过垂直分布模式的分区,表明它们在碳循环和储存过程中具有不同的作用。特别是,与流行的类群相比,大多数类群表现出斑块状分布(仅在少数样本中出现),这与以前在沿海水域中发现的情况一致。总的来说,本研究揭示了裂殖菌类原生动物生态型的明显模式,并阐明了它们在海洋碳循环和固碳方面相对于原核浮游生物的重要性。虽然原核异养浮游生物被认为是海洋碳循环的主要参与者,但它们在远洋海洋中微真核生物对应体的生态分布和功能在很大程度上仍然未知。本研究集中于一类重要的异养(主要是渗透营养)原生微生物,即裂殖菌类,它们的生物量在许多海洋生态系统中可以超过原核浮游生物,包括深海。我们在东印度洋的远洋水域中发现了裂殖菌类原生动物的水平分布具有斑块状但垂直分布具有持续性的特征,这与原核浮游生物的空间模式不同。此外,检测到多个具有不同垂直模式的裂殖菌类原生动物生态型,并根据对其培养相关物的生理、代谢和基因组的了解,推断它们在碳循环和固碳中发挥多方面的关键作用,特别是作为从表面向黑暗海洋(即生物泵)垂直输送碳的贡献者。
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