Biology subjects

Thamatrakoln, K.

Publications and source records attributed to Thamatrakoln, K..

3 recordsLinked to original sources

bioRxiv2026

RNA virus-mediated metabolic reprogramming in a bloom-forming, marine diatom

Diatoms are a widespread group of phytoplankton that disproportionately influence the global carbon cycle through substantial contributions to primary production and carbon export in the ocean. Marine viruses are major drivers of host metabolic reprogramming and mortality and it is increasingly clear that RNA viruses, which primarily infect eukaryotes, are abundant and distributed throughout the global ocean. Using an integrated, multi-omics approach, we characterized the molecular and metabolic response of the model, bloom-forming, centric diatom Chaetoceros tenuissimus to RNA virus infection. Time-resolved transcriptomics revealed coordinated, differential regulation of more than a third of host genes prior to host lysis, eliciting a cascade of metabolic responses that included early shifts in sulfur and lipid metabolism, induction of nitrogen assimilation pathways, and late-stage activation of stress, signaling and death-related genes. Lipidomics revealed substantial cellular enrichment of phosphatidylethanolamine, ceramide and triacylglycerol during RNA virus infection, as well as an infection-specific shift in fatty acid composition. Collectively, these findings provide insight into the intracellular requirements for RNA virus replication and illustrate a fundamental shift in resource partitioning in infected diatoms, advancing our understanding of how RNA virus infection transforms diatom host metabolic function and downstream ecosystem dynamics.

microbiology↗

bioRxiv2025

Viral infection induces oxylipin chemical signaling at the end of a summer upwelling bloom: implications for carbon cycling.

Abstract/SummaryDiatoms are large phytoplankton that form the base of the marine food web and often bloom first when nutrients are injected into the surface ocean through upwelling or deep ocean mixing1,2. Diatoms contribute 20% of global photosynthesis3 while disproportionately representing 40% of carbon export4, with most export occurring along the continental margins5. Oxylipin chemical signaling by diatoms has been extensively studied in the Mediterranean Sea where oxylipins are linked to grazing with subsequent insidious effects on copepod reproduction6-13. Culture studies with diatoms have shown that stress, growth phase, and viral infection also impact oxylipin production14-16. This study provides insight into the role of oxylipins as biomarkers and chemical signals during viral infection of diatoms in natural communities. Biomarkers for lysis and senescence were identified in laboratory experiments and observed at elevated concentrations in meta-lipidomes collected in the California Coastal Ecosystem (CCE) where diatoms had recently been lysed by viruses17. Deck-board incubations with natural communities show that oxylipins stimulate sinking particle-attached and surface-ocean microbes in a dose and community-dependent manner, while inhibiting microzooplankton grazing and phytoplankton growth rates. Carbon export was two times higher at the Post-lytic site than elsewhere along the transect consistent with the viral shuttle, whereby viruses facilitate carbon export. We previously reported enhanced enzymatic activity at the Post-lytic site17, suggestive of the viral shunt, whereby carbon is remineralized or attenuated into non-sinking dissolved organic matter. Here we layer geochemical evidence to show that lysis of oxylipin producing diatoms amplified the vertical flux of carbon from the surface ocean even in the presence of viral shunt processes. The remineralization length scale and community composition have been hypothesized as controls on shunt vs. shuttle18-20; our analysis provides another example of how community interactions may toggle a system between favoring shunt or shuttle.

ecology↗

bioRxiv2018

Divergent gene expression among phytoplankton taxa in response to upwelling

Frequent blooms of phytoplankton occur in coastal upwelling zones creating hotspots of biological productivity in the ocean. As cold, nutrient-rich water is brought up to sunlit layers from depth, phytoplankton are also transported upwards to seed surface blooms that are often dominated by diatoms. The physiological response of phytoplankton to this process, commonly referred to as shift-up, is characterized by rapid growth rates and increases in nitrate assimilation. To examine the molecular underpinnings behind this phenomenon, metatranscriptomics was applied to a simulated upwelling experiment using natural phytoplankton communities from the California Upwelling Zone. An increase in diatom growth following five days of incubation was attributed to the genera Chaetoceros and Pseudo-nitzschia. Here we show that certain bloom-forming diatoms exhibit a distinct transcriptional response that coordinates shift-up where diatoms exhibited the greatest transcriptional change following upwelling; however, comparison of coexpressed genes exposed overrepresentation of distinct sets within each of the dominant phytoplankton groups. The analysis revealed that diatoms frontload genes involved in nitrogen assimilation likely in order to outcompete other groups for available nitrogen during upwelling events. We speculate that the evolutionary success of diatoms may be due, in part, to this proactive response to frequently encountered changes in their environment.

microbiology↗