Representative Diatom and Coccolithophore Species Exhibit Divergent Responses throughout Simulated Upwelling Cycles

Meta-analysis reveals responses of coccolithophores and diatoms to warming

A meta-analysis was conducted to explore the effects of warming on the physiological processes of coccolithophores and diatoms by synthesizing a large number of published literatures. A total of 154 studies consisting 301 experiments were synthesized in this study. Under a projected temperature increase of 3-5 °C by IPCC AR6 at the end of this century, our results suggest that the growth and photosynthetic rate of coccolithophores were significantly enhanced by the rising temperature, while the calcification of coccolithophores was only slightly promoted. Warming also had significantly positive effects on the growth but not photosynthesis of diatoms. In comparison, the effect size of warming on the growth rate of coccolithophores was larger than that of diatoms. However, there was no significant effect of warming on either the ratio of particulate inorganic carbon to particulate organic carbon (PIC:POC) of coccolithophores or the ratio of biogenic silica to carbon (BSi:C) of diatoms. Furthermore, the results reveal latitudinal and size-specific patterns of the effect sizes of warming. For diatoms, the effects of warming on growth were more prominent in high latitudes, specifically for the Southern Hemisphere species. In addition, the effect size of warming on the small-sized diatoms was larger than that of the large-sized diatoms. For coccolithophores, the growth of the Southern Hemisphere temperate strains was significantly promoted by warming. Overall, the results based on the meta-analysis indicate that the projected warming of the end of this century will be more favor to the growth of coccolithophores than that of diatoms, thus potentially affect the competitive advantages of coccolithophores over diatoms; while the mid-to high latitude species/strains of both coccolithophores and diatoms will benefit more than their counterparts in the lower latitudes. Therefore, this study offers novel insights into predicting both the inter- and intra-group competitive advantages of diatoms and coccolithophores under the future warming climate change scenario.

Diminished carbon and nitrate assimilation drive changes in diatom elemental stoichiometry independent of silicification in an iron-limited assemblage

In the California Current Ecosystem, upwelled water low in dissolved iron (Fe) can limit phytoplankton growth, altering the elemental stoichiometry of the particulate matter and dissolved macronutrients. Iron-limited diatoms can increase biogenic silica (bSi) content >2-fold relative to that of particulate organic carbon (C) and nitrogen (N), which has implications for carbon export efficiency given the ballasted nature of the silica-based diatom cell wall. Understanding the molecular and physiological drivers of this altered cellular stoichiometry would foster a predictive understanding of how low Fe affects diatom carbon export. In an artificial upwelling experiment, water from 96 m depth was incubated shipboard and left untreated or amended with dissolved Fe or the Fe-binding siderophore desferrioxamine-B (+DFB) to induce Fe-limitation. After 120 h, diatoms dominated the communities in all treatments and displayed hallmark signatures of Fe-limitation in the +DFB treatment, including elevated particulate Si:C and Si:N ratios. Single-cell, taxon-resolved measurements revealed no increase in bSi content during Fe-limitation despite higher transcript abundance of silicon transporters and silicanin-1. Based on these findings we posit that the observed increase in bSi relative to C and N was primarily due to reductions in C fixation and N assimilation, driven by lower transcript expression of key Fe-dependent genes.

Composition change and decreased diversity of microbial eukaryotes in the coastal upwelling waters of South China Sea

Upwelling plays an important role in marine ecosystems and potentially reshapes microbial communities by enhanced dispersal and distinct environmental drivers. Relative to that of bacterioplankton, however, the response of eukaryotic microbes to upwelling is largely unknown. Here, we investigated the influence of coastal upwelling in South China Sea on the microbial eukaryotic communities. Unlike several folds of increase in the cell abundance of bacterioplankton in upwelling than non-upwelling stations at corresponding water layers, no significant difference was detected for the total microbial eukaryotic 18S rRNA gene abundance. Moreover, the microbial eukaryotes in the upwelling stations exhibited increasing 18S rRNA gene abundance from the surface to the deep, contrasting the vertical cell abundance pattern of the bacterioplankton; but their vertical abundance patterns were similar in non-upwelling stations. Importantly, the coastal upwelling significantly reduced the community evenness of the microbial eukaryotes and slightly reduced their Shannon diversity. Their community composition also varied obviously especially between the surface waters of upwelling and non-upwelling stations. Among the dominant supergroups, Alveolata was found to be less abundant while Stramenopiles, particularly thraustochytrids and diatoms, to be more abundant in the surface water of upwelling than non-upwelling stations. Temperature was identified as the most important factor of the microbial eukaryotic community composition, suggesting potential effects of the cold upwelling water masses on specific taxa. Overall, our results reveal significant and distinct impacts of coastal upwelling on the abundance, diversity, and community structure of microbial eukaryotes, filling the knowledge gap about the microbial responses to this important marine phenomenon.