Scripps Institution of Oceanography, University of California, San Diego, California, USA.
Microbial and Environmental Genomics Group, J. Craig Venter Institute, La Jolla, California, USA.
mSystems. 2022 Oct 26;7(5):e0072922. doi: 10.1128/msystems.00729-22. Epub 2022 Aug 29.
Nearly half of carbon fixation and primary production originates from marine phytoplankton, and much of it occurs in episodic blooms in upwelling regimes. Here, we simulated blooms limited by nitrogen and iron by incubating Monterey Bay surface waters with subnutricline waters and inorganic nutrients and measured the whole-community transcriptomic response during mid- and late-bloom conditions. Cell counts revealed that centric and pennate diatoms (largely Pseudo-nitzschia and Chaetoceros spp.) were the major blooming taxa, but dinoflagellates, prasinophytes, and prymnesiophytes also increased. Viral mRNA significantly increased in late bloom and likely played a role in the bloom's demise. We observed conserved shifts in the genetic similarity of phytoplankton populations to cultivated strains, indicating adaptive population-level changes in community composition. Additionally, the density of single nucleotide variants (SNVs) declined in late-bloom samples for most taxa, indicating a loss of intraspecific diversity as a result of competition and a selective sweep of adaptive alleles. We noted differences between mid- and late-bloom metabolism and differential regulation of light-harvesting complexes (LHCs) under nutrient stress. While most LHCs are diminished under nutrient stress, we showed that diverse taxa upregulated specialized, energy-dissipating LHCs in low iron. We also suggest the relative expression of compared to the expression of as a marker of cellular nitrogen status and the relative expression of iron starvation-induced protein genes (, , and ) compared to the expression of the thiamine biosynthesis gene () as a marker of iron status in natural diatom communities. Iron and nitrogen are the nutrients that most commonly limit phytoplankton growth in the world's oceans. The utilization of these resources by phytoplankton sets the biomass available to marine systems and is of particular interest in high-nutrient, low-chlorophyll (HNLC) coastal fisheries. Previous research has described the biogeography of phytoplankton in HNLC regions and the transcriptional responses of representative taxa to nutrient limitation. However, the differential transcriptional responses of whole phytoplankton communities to iron and nitrogen limitation has not been previously described, nor has the selective pressure that these competitive bloom environments exert on major players. In addition to describing changes in the physiology of diverse phytoplankton, we suggest practical indicators of cellular nitrogen and iron status for future monitoring.
近一半的碳固定和初级生产来自海洋浮游植物,其中大部分发生在上升流区的间歇性浮游植物爆发中。在这里,我们通过用亚营养层水和无机养分孵育蒙特雷湾表层水来模拟受氮和铁限制的浮游植物爆发,并在中晚期爆发期间测量整个群落的转录组响应。细胞计数表明,中心纲和羽纹纲硅藻(主要是假菱形藻和角毛藻属)是主要的爆发类群,但甲藻、原绿藻和金藻也有所增加。病毒 mRNA 在晚期爆发时显著增加,可能在爆发结束中发挥作用。我们观察到浮游植物种群与培养株的遗传相似性发生保守变化,表明群落组成的种群水平适应性变化。此外,大多数分类群在晚期爆发样本中的单核苷酸变异 (SNV) 密度下降,表明由于竞争和适应性等位基因的选择清除,种内多样性丧失。我们注意到中晚期代谢之间的差异以及在养分胁迫下对光收集复合物 (LHC) 的差异调控。虽然大多数 LHC 在养分胁迫下减少,但我们表明,在低铁条件下,多种分类群上调了专门的、能量耗散 LHC。我们还建议将 与细胞氮状态的表达相比作为标记,并将铁饥饿诱导蛋白基因( 、 、和 )的相对表达与硫胺素生物合成基因( )的表达相比作为天然硅藻群落中铁状态的标记。铁和氮是世界海洋中最常见的限制浮游植物生长的营养物质。浮游植物对这些资源的利用决定了海洋系统中可用的生物量,这在高营养、低叶绿素 (HNLC) 沿海水域渔业中尤为重要。先前的研究描述了 HNLC 区域浮游植物的生物地理学以及代表性分类群对养分限制的转录响应。然而,整个浮游植物群落对铁和氮限制的差异转录响应尚未被描述,也没有描述这些竞争爆发环境对主要参与者施加的选择压力。除了描述不同浮游植物的生理学变化外,我们还建议为未来的监测提供细胞氮和铁状态的实用指标。