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Signori, C. N.

Publications and source records attributed to Signori, C. N..

3 recordsLinked to original sources

A Multidomain Lens on the Temporal Dynamics of Surface Microbial Communities in the Southern Ocean (2013-2019)

Marine microorganisms are vital to biogeochemical cycles and food web dynamics, with their community structure shaped by environmental factors such as temperature, light, and salinity. While microbial dynamics in the western Antarctic Peninsula are relatively well- studied, the northwestern region remains underexplored, particularly in long-term, multidomain analyses. To fill this gap, we investigated microbial communities encompassing all three domains of life (Bacteria, Archaea, and Eukarya) in the Northwestern Antarctic Peninsula. Using the universal primer set 515Y/926R, we sequenced unfractionated seawater from ten sites over a six-year period (2013-2019). Environmental parameters, temperature and salinity, showed minimal variation across the study. However, microbial diversity and composition, especially among eukaryotic phytoplankton, displayed significant temporal changes among seasons and years. The prokaryotic community, by contrast, was relatively stable, with Gammaproteobacteria-- particularly the Nitrincolaceae family--maintaining high relative abundance throughout all sampling periods, but a few distinct ASVs. In contrast, no eukaryotic group exhibited consistently high relative abundance across sampling periods. The summer of 2016, marked by a strong El Nino event, presented the most distinct microbial community structure, underscoring the sensitivity of these communities to extreme climatic conditions. These results highlight the importance of integrated, long-term studies to better understand the dynamics, interactions, and resilience of microbial ecosystems in the rapidly changing Antarctic environment. IMPORTANCEThis study provides a unique long-term perspective on microbial community dynamics in the Northwestern Antarctic Peninsula, a region still poorly explored through a multidomain lens. By investigating the temporal variability of Bacteria, Archaea, and Eukaryotes over six years, we reveal distinct stability patterns between these groups, with phytoplankton showing the highest variability and prokaryotes remaining relatively stable. The strong response of the microbial community to the 2016 El Nino event highlights its sensitivity to extreme climate conditions, reinforcing the importance of understanding how Antarctic ecosystems will respond to future climate shifts. The consistent presence of Nitrincolaceae, a key bacterial taxon, suggests its ecological relevance in the region, while fluctuations in phytoplankton composition may impact food web dynamics. These findings emphasize the need for continued long-term monitoring to predict how microbial communities will adapt to environmental changes, which is crucial for assessing the future functioning of polar marine ecosystems.

microbiology↗

Spatial Patterns of Microbial Diversity, Composition and Community Structure in Fe-Mn Deposits and Associated Sediments in the Atlantic and Pacific Oceans

Mining of deep-sea Fe-Mn deposits will remove crusts and nodules in large areas from the seafloor. The growth of a few millimeters of these minerals by Fe and Mn oxides precipitation takes millions of years, and yet little is known about their microbiome. Besides being key elements of the biogeochemical cycles and essential links of food and energy to deep-sea trophic webs, microbes have been identified to affect manganese oxide formation. Hence, polymetallic crusts and nodules may present unique habitats that deserve better understanding. In this study, we determined the composition and diversity of Bacteria and Archaea in deep-sea Fe-Mn crusts, nodules, and associated sediments from two oceanic elevations in the Atlantic Ocean, the Tropic Seamount in the northeast and the Rio Grande Rise (RGR) in the southwest. Sequencing of the 16S rRNA gene was performed using the Illumina MiSeq platform and statistical analyses using environmental data were performed in R. Additionally, we included public domain environmental DNA data of Fe-Mn crusts, nodules, and associated sediments from Clarion-Clipperton Zone and Takuyo-Daigo Seamount in the Pacific Ocean to compare microbial diversity in Fe-Mn deposits from different ocean basins. Our results indicated that Atlantic seamounts harbor an unusual and unknown Fe-Mn deposit microbiome with lower diversity and richness compared to deposits from Pacific areas. Crusts and nodules from Atlantic seamounts revealed the presence of unique taxa (Alteromonadales, Nitrospira, and Magnetospiraceae) and a higher relative abundance of sequences related to potential metal-cycling bacteria, such as Betaproteobacteriales and Pseudomonadales. The microbial beta-diversity from Atlantic seamounts was clearly grouped into microhabitats according to crusts, nodules, and sediments geochemical composition. Furthermore, community structure analysis using principal coordinate analysis also showed that the microbial communities of all seamounts were significantly divided into ocean basins and sampling areas. Despite the time scale of million years for these deposits to grow, a combination of environmental settings (temperature, salinity, depth, substrate geochemistry, nutrient, and organic matter availability) played a significant role in shaping the crusts and nodules microbiome, which was distinct between the Atlantic and Pacific Fe-Mn deposits. Our results suggest that the microbial community inhabiting Fe-Mn deposits participate in biogeochemical reactions indispensable to deep-sea ecosystems, which implies that understanding the microbial community is of utmost importance for any baseline environmental study in areas of potential deep-sea mining. Graphical abstract O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=98 SRC="FIGDIR/small/485154v1_ufig1.gif" ALT="Figure 1"> View larger version (49K): org.highwire.dtl.DTLVardef@1214ccorg.highwire.dtl.DTLVardef@1139796org.highwire.dtl.DTLVardef@144f967org.highwire.dtl.DTLVardef@151f069_HPS_FORMAT_FIGEXP M_FIG C_FIG HighlightsO_LIAtlantic deposits showed lower diversity and richness compared to Pacific deposits C_LIO_LIFe-Mn crusts and nodules are a potential specific ecological niche C_LIO_LIAtlantic Fe-Mn deposits harbor an unusual and unknown microbiome C_LIO_LITemperature, salinity, depth, and substrate geochemistry at Atlantic Fe-Mn deposits may drive community composition C_LI

microbiology↗

BATHYARCHAEOTA OCCURRENCE IN SHALLOW MARINE METHANE-RICH SEDIMENTS (SACO DO MAMANGUA, RIO DE JANEIRO, BRAZIL)

Methane gas (CH4) reservoirs have previously been reported in tropical marine sediments of Saco do Mamangua ria (Rio de Janeiro, Brazil). It is known that a methane microbiome can be established in methane seeps sites; however, they are still poorly characterised. In this study, we aimed to investigate the spatial and vertical distribution of the bacterial and archaeal composition and the community structure in the sediments of Saco do Mamangua ria. For this purpose, we collected sediment samples through 100 cm long gravity corer at three different sites and performed community analysis based on 16S rRNA gene sequencing, quantification of the methyl coenzyme M reductase-encoding gene (mcrA) and geochemical analysis, including CH4 stable isotope. Our results revealed a biogenic trend for CH4 isotopic signature and a high proportion of archaeal sequences assigned as Bathyarchaeota, with a spatial distribution throughout the inner areas of the channel and the deepest strata. OTUs classified within Bathyarchaeota and Chloroflexi (Dehalococcoidia) showed positive correlation with methane concentrations, sediment depth and oxidation-reduction potential. Due to their prevalence in the microbial community, we also performed phylogenetic analysis to understand the closeness of our Bathyarchaeota OTUs with Bathyarchaeota subgroups, and the results demonstrated a close relationship particularly with Bathy-8 and Bathy-13, which possess genes for acetogenesis and methanogenesis. Although direct relations between microbial populations and the biogenic methane emissions in Saco do Mamangua cannot be assured, our results emphasize the importance of further investigations about the potential role of Bathyarchaeota in the carbon cycling in methane-rich tropical shallow ecosystems.

microbiology↗