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Fremont, P.

Publications and source records attributed to Fremont, P..

11 recordsLinked to original sources

Particle-based representation of phytoplankton modulates emergent coexistence and biogeography in a model ocean

Phytoplankton communities sustain the marine food web through primary productivity. These communities sustain a high diversity of species, all of which must draw from the same finite nutrient supply. The mechanisms driving phytoplankton biogeography and succession, as well as those enabling high diversity, remain incompletely understood. Here, we compare emerging patterns of biogeography, richness, and diversity in a size-structured phytoplankton community as it is advected and diffused within an idealized North Atlantic double-gyre circulation, using both Eulerian and Lagrangian (particle-based) modeling (PBM) frameworks. When a sufficient number of particles is modeled, the PBM, which resolves mortality at the particle level, produces stronger seasonal variability in biomass in the northern gyre and less stable and higher biomass in the southern gyre, while reproducing large-scale chlorophyll patterns observed by satellite. These contrasting dynamics are accompanied by distinct regional diversity patterns: local richness and diversity are generally higher in the PBM than in the Eulerian model in the northern gyre, with differences depending on the mortality threshold, whereas in the oligotrophic southern gyre, PBM local richness increases with particle number, while Eulerian richness is more sensitive to the mortality threshold. The PBM also produces a dynamic and emergent biogeographical structure that is more robust to the mortality threshold than the Eulerian model. Finally, Lagrangian variability in environmental conditions experienced by particles shows a stronger impact compared to the local Eulerian variability in the Northern gyre and stresses variable sensitivity to environmental histories. Together, these results suggest that the discrete representation of biomass fundamentally alters mortality, biogeography, and emergent coexistence patterns in model plankton ecosystems.

ecology↗

Slower-than-exponential viral decay is prevalent and can reshape virus-microbe dynamics

Viral population dynamics are shaped by production and loss. For viruses of microbes, high standing levels of viral abundances are interpreted as evidence of high rates of viral-induced cellular loss and viral production, followed by rapid extracellular viral decay. Here we reassess assumptions of rapid extracellular decay in 17 curated datasets, finding that biphasic decay either fits better or is statistically indistinguishable from exponential decay in approximately half the datasets. In addition to intrinsic heterogeneity in decay rates, biphasic decay at population scales can arise generically through aggregation mechanisms, where single virions decay and viral aggregates are protected. Integrating aggregation-induced biphasic decay into a virus-host model reveals that accounting for aggregation can recapitulate joint observations of high virion abundances and low infection prevalence, without assuming significant levels of uniformly inefficient infection. Together, our results suggest that durable extracellular virion persistence is environmentally relevant in shaping virus-microbe population dynamics.

ecology↗

Implicit representation of viruses fails to capture impacts of virus-induced mortality in global marine ecosystem models

Virus-induced mortality influences plankton biogeography, community structure, and ocean elemental cycles. However, quantification of virus-induced impacts remains challenging and often limited in scope. An alternative to explicit inclusion of viral dynamics in biogeochemical models is to represent viral effects implicitly, by assuming that mortality increases quadratically with cell or biomass density. Using 1D and 3D configurations of a nutrient-phytoplankton-zooplankton-virus-detritus (NPZVD) model, we ask whether the implicit quadratic mortality assumption captures patterns of virus-induced mortality, and its impact on biomass and primary production. The 1D water-column configuration shows that, at the onset of the spring bloom, the quadratic, implicit representation imposes viral losses on phytoplankton density instantaneously, which limits spring bloom formation. This is in contrast to the explicit representation, which allows initial bloom formation to proceed unhampered initially, but imposes a far stronger viral mortality later in the year driven by high rates of host-virus contact due to high phytoplankton and viral densities that take time to accumulate. By comparison to the implicit model, explicit resolution of viruses within the 3D global model shows strong potential for viruses to prematurely terminate phytoplankton blooms. Biogeochemical models would therefore benefit from explicit representation of viral infection insofar as models can be developed that adequately recapitulate in situ observations. Key PointsO_LIGlobal model reveals significant spatial heterogeneity arising from explicit, rather than implicit, representation of viruses C_LIO_LIImplicit representation of viral dynamics fails to capture the potential for viruses to terminate phytoplankton blooms C_LIO_LIBiogeochemical models require explicit representation of viruses to adequately simulate their effect on marine systems C_LI

microbiology↗

Viral impacts on plankton standing stocks, primary productivity, and biogeochemistry in a model ocean

Viral lysis fuels the microbial loop by enhancing organic matter recycling (via the viral shunt) and can redirect organic matter toward export (via the viral shuttle). However, the global impact of viral infection mediated by shunt and shuttle pathways remains unclear. Here, we implemented viral infection and lysis processes in a global ocean ecosystem model, including a single phytoplankton (representing Prochlorococcus), virus (representing cyanophage), and nanozooplankton. Despite low but plausible levels of viral infection, high shunt efficiencies generated enhanced-productivity regions covering up to approximately one-half of the global ocean. For lower viral shunt efficiencies, the enhanced-productivity regions contracted abruptly, accompanied by steady declines in productivity. Viral-mediated increases in primary productivity reduced the extent of tropical oligotrophic regions at high shunt efficiencies, while lower efficiencies expanded oligotrophic areas. These results provide a path forward to developing predictive models of how viral infection and the fate of cellular lysates shape global ocean ecosystems.

ecology↗

Epigenetic profile drives accurate survival prediction in breast cancer via a multi-omics machine learning model

Accurate overall survival (OS) prediction is key for personalized treatment in breast cancer, but mutation burden alone is insufficient. To improve prognostic accuracy, we integrated genomic, transcriptomic, proteomic, epigenetic, and clinical features from 802 breast cancer patients to develop BANDOL (Breast cancer Analysis with Neoplastic Data and Omics Learning), a Random Survival Forest model. BANDOL correctly predicted survival ranking in 73% of patient pairs and outperformed mutation-based models (time-dependent AUC: 0.9-1 vs. 0.4-0.9). Immune activation signatures correlated with a longer OS after therapy, while a shorter OS was linked to TREM2 myeloid cells, B cells, and leptin signaling. The transferability of the model was further explored in three independent TCGA cohorts from distinct cancer types (uterine, ovarian and lower-grade glioma), where moderate predictive performance was maintained despite biological differences between tumors. Epigenetic features were the strongest OS predictors for BANDOL. Current therapies may be combined with strategies to target the methylations of ME3, PPARG, OLIG3 and SLC25A22 genes. This study demonstrates that multi-omics integration via machine learning enhances survival prediction and reveals actionable biomarkers. O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=180 SRC="FIGDIR/small/667894v6_ufig1.gif" ALT="Figure 1"> View larger version (61K): org.highwire.dtl.DTLVardef@1f3efc6org.highwire.dtl.DTLVardef@2cff0org.highwire.dtl.DTLVardef@a1c3baorg.highwire.dtl.DTLVardef@392114_HPS_FORMAT_FIGEXP M_FIG C_FIG

cancer biology↗

Coexistence of Photosynthetic Marine Microorganisms, Viruses, and Grazers: Toward Integration in Ocean Ecosystem Models

Photosynthetic microorganisms are responsible for primary production at the base of the marine food web that impacts ocean biogeochemistry and ecological interactions. The growth of these microorganisms is balanced by mortality processes, including top-down losses from zooplankton grazing and infection and lysis by viruses. Multiple types of grazers and viruses often coexist despite apparent competition for the same (or similar) microorganisms. Here, we develop a community model of photosynthetic microorganisms, grazers, and viruses that accounts for molar cell and virion elemental quotas suitable for incorporation into ocean ecosystem models. Our aim is to investigate mechanisms that enable coexistence of a virus and a grazer with a single phytoplankton type. To do so, we evaluate the extent to which coexistence is facilitated by: (i) infected phytoplankton, potentially subject to non-preferential intraguild predation, where grazers feed on virally infected microorganisms; (ii) heterogeneity in susceptibility to infection, where microorganisms vary in their resistance to the virus either intracellularly or extracellularly; and (iii) the inclusion of higher-order mortality terms for the predators. We find evidence for a trade-off between the virus latent period and virulence in facilitating a coexistence regime. The inclusion of an explicit latent period can generate oscillations of all populations that facilitate coexistence by reducing the growth rate of the free virus, or lead to system collapse when oscillations become too large. Heterogeneity in phage susceptibility promotes coexistence through resource partitioning between the predators, while higher-order mortality terms widen the coexistence regime by stabilizing the system. We observe strong sensitivity of model outcomes to viral life history traits, including shifts in infected cell percentages and the balance between virally and zooplankton-induced mortality. Finally, taking advantage of algebraic calculation of model equilibria, we identify life history trait parameter combinations that yield realistic ecological properties in simplified oligotrophic and mesotrophic epipelagic environments. Importantly, our ecological models suggest that ongoing efforts to embed virus dynamics in large-scale ocean ecosystem models should likely include phytoplankton types that are moderately to strongly resistant to viral infection and lysis.

ecology↗

Changes in functional composition and gene expression in eukaryotic plankton at the Atlantic-Arctic Polar front

In the Arctic Ocean, phytoplankton communities, dominated by eukaryotes, sustain the marine food web and influence biogeochemical cycles. While many are endemic, some are transported by currents from the Atlantic Ocean along an environmental gradient that steepens at the polar front. Despite these distinct biogeographies, the functional characteristics of these communities remain poorly characterized. Here, we analyzed twenty metatranscriptomes from a North Atlantic-Arctic environmental gradient considering ocean currents transport times. Functions related to the regulation of gene expression and cold acclimation were more abundant in Arctic metatranscriptomes. Using the PHATE dimensionality reduction algorithm, reconstructed transcriptomes of Bacillariophyta, Mamiellales, Pelagophyceae, and Phaeocystales revealed different gene expression patterns, including photosynthesis regulation. All groups showed upregulation of numerous key temperature-associated functions and a subset of shared functions, supporting a convergence in transcriptomic changes under polar conditions. This study, based on a new resource of reconstructed transcriptomes, addressed the functional differentiation of eukaryotic phytoplankton across the North Atlantic and Arctic Ocean. It evidenced both differential and convergent changes in gene expression across the polar front in widespread phytoplankton types. These results advance our understanding of the functional dynamics of phytoplankton along environmental gradients.

genomics↗

Insights into biotic and abiotic modulation of ocean mesopelagic communities

For decades, marine plankton have been investigated for their capacity to modulate biogeochemical cycles and provide fishery resources. Between the sunlit (epipelagic) layer and the deep dark waters, lies a vast and heterogeneous part of the ocean: the mesopelagic zone. How plankton composition is shaped by environment has been well-explored in the epipelagic but much less in the mesopelagic ocean. Here, we conducted comparative analyses of trans-kingdom community assemblages thriving in the mesopelagic oxygen minimum zone (OMZ), mesopelagic oxic, and their epipelagic counterparts. We identified nine distinct types of intermediate water masses that correlate with variation in mesopelagic community composition. Furthermore, oxygen, NO - and particle flux together appeared as the main drivers governing these communities. Novel taxonomic signatures emerged from OMZ while a global co-occurrence network analysis showed that about 70% of the abundance of mesopelagic plankton groups is organized into three community modules. One module gathers prokaryotes, pico-eukaryotes and Nucleo-Cytoplasmic Large DNA Viruses (NCLDV) from oxic regions, and the two other modules are enriched in OMZ prokaryotes and OMZ pico-eukaryotes, respectively. We hypothesize that OMZ conditions led to a diversification of ecological niches, and thus communities, due to selective pressure from limited resources. Our study further clarifies the interplay between environmental factors in the mesopelagic oxic and OMZ, and the compositional features of communities.

ecology↗

Restructuring of genomic provinces of surface ocean plankton under climate change

The impact of climate change on diversity, functioning and biogeography of marine plankton remains a major unresolved issue. Here, niche theory is applied to plankton metagenomes of 6 size fractions, from viruses to meso-zooplankton, sampled during the Tara Oceans expedition. Niches are used to derive plankton size-dependent structuring of the oceans south of 60{degrees}N in climato-genomic provinces characterized by signature genomes. By 2090, assuming the RCP8.5 high warming scenario, provinces would be reorganized over half of the considered ocean area and quasi-systematically displaced poleward. Particularly, tropical provinces would expand at the expense of temperate ones. Sea surface temperature is identified as the main driver of changes (50%) followed by phosphate (11%) and salinity (10%). Compositional shifts among key planktonic groups suggest impacts on the nitrogen and carbon cycles. Provinces are linked to estimates of carbon export fluxes which are projected to decrease on average by 4% in response to biogeographical restructuring.

ecology↗

Functional repertoire convergence of distantly related eukaryotic plankton lineages revealed by genome-resolved metagenomics

Marine planktonic eukaryotes play a critical role in global biogeochemical cycles and climate. However, their poor representation in culture collections limits our understanding of the evolutionary history and genomic underpinnings of planktonic ecosystems. Here, we used 280 billion Tara Oceans metagenomic reads from polar, temperate, and tropical sunlit oceans to reconstruct and manually curate more than 700 abundant and widespread eukaryotic environmental genomes ranging from 10 Mbp to 1.3 Gbp. This genomic resource covers a wide range of poorly characterized eukaryotic lineages that complement long-standing contributions from culture collections while better representing plankton in the upper layer of the oceans. We performed the first comprehensive genome-wide functional classification of abundant unicellular eukaryotic plankton, revealing four major groups connecting distantly related lineages. Neither trophic modes of plankton nor its vertical evolutionary history could explain the functional repertoire convergence of major eukaryotic lineages that coexisted within oceanic currents for millions of years. CoverNavigating on the map of plankton genomics with Tara Oceans and anvio: a comprehensive genome-resolved metagenomic survey dedicated to eukaryotic plankton. O_FIG O_LINKSMALLFIG WIDTH=153 HEIGHT=200 SRC="FIGDIR/small/341214v2_ufig1.gif" ALT="Figure 1"> View larger version (82K): org.highwire.dtl.DTLVardef@536fe5org.highwire.dtl.DTLVardef@1d72cc9org.highwire.dtl.DTLVardef@1bd5281org.highwire.dtl.DTLVardef@739512_HPS_FORMAT_FIGEXP M_FIG C_FIG

microbiology↗

Genomic evidence for global ocean plankton biogeography shaped by large-scale current systems

Biogeographical studies have traditionally focused on readily visible organisms, but recent technological advances are enabling analyses of the large-scale distribution of microscopic organisms, whose biogeographical patterns have long been debated. Here we assessed the global structure of plankton geography and its relation to the biological, chemical and physical context of the ocean (the seascape) by analyzing metagenomes of plankton communities sampled across oceans during the Tara Oceans expedition, in light of environmental data and ocean current transport. Using a consistent approach across organismal sizes that provides unprecedented resolution to measure changes in genomic composition between communities, we report a pan-ocean, size-dependent plankton biogeography overlying regional heterogeneity. We found robust evidence for a basin-scale impact of transport by ocean currents on plankton biogeography, and on a characteristic timescale of community dynamics going beyond simple seasonality or life history transitions of plankton.

ecology↗