Biology subjects

Dugenne, M.

Publications and source records attributed to Dugenne, M..

5 recordsLinked to original sources

bioRxiv2026

Virus-grazer interplay enhances virus production, particle aggregation, and trophic efficiency during infection of Prochlorococcus

Viruses and grazers are fundamental agents of mortality in the oceans, impacting phytoplankton populations and organic matter cycling. Although viruses and grazers co-occur in nature, they are typically studied in isolation in laboratory experiments, limiting our understanding of their combined ecosystem impacts. Here, using a simplified ecosystem approach, we investigated individual and combined effects of the T7-like cyanopodovirus, P-SSP7, and the protistan grazer, Paraphysomonas bandaiensis, on the abundant marine cyanobacterium, Prochlorococcus MED4, and co-occurring non-photosynthetic heterotrophic bacteria (bacteria from here on). We observed that, individually, viruses and grazers caused substantial Prochlorococcus mortality. Viral lysis also triggered increases in damaged Prochlorococcus cells, dissolved organic matter release, and bacterial growth, while grazing reduced bacterial abundances. When grazers and viruses were combined, Prochlorococcus mortality was lower than expected from the sum of their individual effects. Contrary to expectations, this reduced Prochlorococcus mortality did not result in fewer viruses or grazers. Instead, virus-grazer-Prochlorococcus interplay resulted in greater virus production, maintenance of grazer growth, and a dramatic increase in particle aggregation. Our results reveal trophic cooperation and efficiency in which competition between viruses and grazers was likely mitigated, with virus progeny production enhanced by grazers, and grazer growth sustained through a shift to alternative food sources (bacteria, damaged cells, aggregates) secondarily derived from Prochlorococcus following viral lysis. The synergistic enhancement of particle aggregation via grazer-virus-phytoplankton interplay observed with the small buoyant Prochlorococcus phytoplankter underscores the importance of food web interactions for the flow of phytoplankton-fixed carbon within, and export from, the photic zone. SignificanceViruses and grazers both use phytoplankton as a resource for reproduction. In a simplified experimental system with Prochlorococcus, an important primary producer in the oceans, we found that the interplay between viruses and grazers led to reduced mortality of Prochlorococcus. Despite this reduced mortality, virus-grazer interactions resulted in elevated virus production and a dramatic increase in organic matter aggregation. Furthermore, grazer abundance was not affected by this interplay, likely due to the transfer of organic matter from Prochlorococcus to bacteria and aggregates, which the grazers could consume as alternative food sources. These findings provide insights into the complexity of ecosystem interactions and how they impact the fate of organic matter fixed by phytoplankton in the oceans.

microbiology↗

bioRxiv2024

Key link between iron and the size structure of three main mesoplanktonic groups (Crustaceans, Rhizarians, and colonial N2-fixers) in the Global Ocean.

In marine ecosystems, critical services like fish production, carbon export, or the delivery of nutrients through N2-fixation rely heavily on the size spectrum of pelagic organisms, particularly mesoplankton (200-20,000 {micro}m). However, how environmental factors shape mesoplankton spectral biogeography remains largely unresolved, as so far only limited datasets exist to understand the large-scale shifts in mesoplankton size. Using global compilations of Rhizarian, colonial N2-fixer, and Crustacean images, we reveal the paramount role of iron in shaping the size structure and related biogeography of these groups. Our findings underscore the importance of atmospheric sources of iron for N2-fixers and Rhizarians while total iron, accounting for organic and inorganic compounds, appeared to explain most of the variance in Crustacean size structure via apparent recycling. With a comprehensive set of explanatory variables, our models reached high R2 (0.93, 0.61, and 0.69 respectively), providing robust predictions of mesoplankton size structure related to elemental cycling and ecosystem services. Our results suggest that future increases in global temperatures will have negative effects on mesoplankton size, possibly limiting carbon export from the productive layers to sequestration depth, that can be offset by expected increases in iron inputs that benefit N2-fixers, Rhizarians, and eventually Crustaceans.

ecology↗

bioRxiv2023

Complete zooplankton size spectra re-constructed from in situ imaging and Multinet data in the global ocean

Plankton size spectra are important indicators of the ecosystem state, as they illustrate the quantity of organisms available for higher marine food web and reflect multiple size-dependent processes. Yet, such measurements are typically biased by the available sampling methods, either disrupting fragile organisms or lacking good resolution (in size and/or time and space). In this study, we combined two of the most common approaches to measure zooplankton Normalized Biomass/Biovolume Size Spectra (NBSS) to calculate a complete zooplankton distribution for organisms larger than 1 mm. The reconstructed NBSS slopes appeared steeper and closer to those measured by the UVP5 (+7.6%) and flatter than those of the Multinet (- 20%) particularly in tropics and temperate latitudes. The overall gain in polar biomass was relatively small for reconstructed biomass compared to bulk estimates from Multinet (+0.24 mgC/m3 or +4.25%) and high from the UVP5 (+2.0 mgC/m3 or +53%). In contrast, in the tropical and temperate ecosystems, the gain in biomass was small for UVP5 (+0.67 mgC/m3 or +30.44% and +0.74 mgC/m3 or +19.59% respectively) and high for Multinet (+1.66 mgC/m3 or +136% and +3.4 mgC/m3 or +309% respectively). Given these differences, we suggest here to combine in situ imaging sensors and net data in any comprehensive study exploring key living players in the ocean ecosystem and their contributions to the biological pump.

ecology↗

bioRxiv2021

Diel population dynamics and mortality of Prochlorococcus in the North Pacific Subtropical Gyre

Photosynthesis fuels primary production at the base of marine food webs. Yet, in many surface ocean ecosystems, diel-driven primary production is tightly coupled to daily loss. This tight coupling raises the question: which top-down drivers predominate in maintaining persistently stable picocyanobacterial populations over longer time scales? Motivated by high-frequency surface water measurements taken in the North Pacific Subtropical Gyre (NPSG), we developed multitrophic models to investigate bottom-up and top-down mechanisms underlying the balanced control of Prochlorococcus populations. We find that incorporating photosynthetic growth with viral- and predator-induced mortality is sufficient to recapitulate daily oscillations of Prochlorococcus abundances with baseline community abundances. In doing so, we infer that grazers function as the primary top-down factor despite high standing viral particle densities while identifying the potential for light-dependent viral traits and non-canonical loss factors to shape the structure and function of marine microbial communities.

ecology↗

bioRxiv2021

Nitrogen fixation in mesoscale eddies of the North Pacific Subtropical Gyre: patterns and mechanisms

1.Mesoscale eddies have been shown to support elevated dinitrogen (N2) fixation rates (NFRs) and abundances of N2-fixing microorganisms (diazotrophs), but the mechanisms underlying these observations are not well understood. We explored relationships among NFRs and cyanobacterial diazotroph abundances in eddy pairs of opposite polarity sampled in the North Pacific Subtropical Gyre and compared our observations to seasonal trends from the Hawaii Ocean Time-series (HOT) program. Consistent with previous reports, we found that NFRs were anomalously high for this region (up to 3.7-fold above previous monthly HOT observations) in the centers of the sampled anticyclones, coinciding with elevated abundances of Crocosphaera in the summertime. We then coupled our field-based observations, together with transcriptomic analyses of nutrient stress marker genes and ecological models, to evaluate potential mechanisms controlling diazotroph abundance and activity at the mesoscale. Specifically, we evaluated the role of biological (via estimates of growth and grazing rates) and physical controls on populations of Crocosphaera, Trichodesmium, and diatom symbionts. Our results suggest that increased Crocosphaera abundances associated with summertime anticyclones resulted from the alleviation of phosphate limitation, allowing cells to grow at rates exceeding grazing losses. In contrast, distributions of larger, buoyant taxa (Trichodesmium and diatom symbionts) appeared less affected by eddy-driven biological controls. Instead, they appeared driven by physical dynamics along frontal boundaries that separate cyclonic and anticyclonic eddies. Together, the interplay of eddy-specific changes in bottom-up control, top-down control, and the physical accumulation of cells likely explains the elevated diazotroph abundances and NFRs associated with anticyclones and eddy fronts.

ecology↗