Disentangling marine microbial networks across space

Although microbial interactions underpin ocean ecosystem functions, they remain barely known. Different studies have analyzed microbial interactions using static association networks based on omics-data. However, microbial associations are dynamic and can change across physicochemical gradients and spatial scales, which needs to be considered to understand the ocean ecosystem better. We explored associations between archaea, bacteria, and picoeukaryotes along the water column from the surface to the deep ocean across the northern subtropical to the southern temperate ocean and the Mediterranean Sea by defining sample-specific subnetworks. Quantifying spatial association recurrence, we found the lowest fraction of global associations in the bathypelagic zone, while associations endemic of certain regions increased with depth. Overall, our results highlight the need to study the dynamic nature of plankton networks and our approach represents a step forward towards a better comprehension of the biogeography of microbial interactions across ocean regions and depth layers.

Associations between depth and micro-diversity within marine viral communities revealed through metagenomics

Viruses are extremely abundant and diverse biological entities that contribute to the functioning of marine ecosystems. Despite their recognized importance no studies have addressed trends of micro-diversity in marine viral communities across depth gradients. To fill this gap we obtained metagenomes from both the cellular and viral fractions of Mediterranean seawater samples spanning the epipelagic to the bathypelagic zone at 15, 45, 60 and 2000 meters deep. The majority of viral genomic sequences obtained were derived from bacteriophages of the order Caudovirales, and putative host assignments suggested that they infect some of the most abundant bacteria in marine ecosystems such as Pelagibacter, Puniceispirillum and Prochlorococcus. We evaluated micro-diversity patterns by measuring the accumulation of synonymous and non-synonymous mutations in viral genes. Our results demonstrated that the degree of micro-diversity differs among genes encoding metabolic, structural, and replication proteins and that the degree of micro-diversity increased with depth. These trends of micro-diversity were linked to the changes in environmental conditions observed throughout the depth gradient, such as energy availability, host densities and proportion of actively replicating viruses. These observations allowed us to generate hypotheses regarding the selective pressures acting upon marine viruses from the epipelagic to the bathypelagic zones.

Scottoecia villosa sp. nov., a new deep-sea species of halocyprid (Ostracoda, Myodocopa) from the northern Pacific

A new species of halocyprid ostracod, Scottoecia villosa sp. nov., from the bathypelagic zone of the Kurile-Kamchatka Trench, is described and illustrated. This species is closely similar to S. foveolata (Deevey, 1968), but differs by the shape of the postero-dorsal corners of the carapace, the carapace sculpture, the number of secondary filaments on the first antenna, and the setae on the first endopodite segment of the maxilla. A key to the species of the genus Scottoecia is presented.

Bathyconchoecia liui n. sp., a new species of ostracod (Myodocopa, Halocyprididae) from the South China Sea

A new species of halocyprid ostracod,Bathyconchoecia liui, from the bathypelagic zone of the Nansha Trough (North-West Borneo Trough, southern South China Sea) is described and illustrated. It is compared with the closely similar speciesB. angeliGeorge, 1977. The present species is easily distinguished fromB. angeliby the structures of the toothed edges of the mandibular basis and coxa, and by the segmentation of the fifth limb.

Swept under the carpet: the effect of organic matter burial in global biogeochemical ocean models

Although of substantial importance for marine tracer distributions and eventually global carbon, oxygen, and nitrogen fluxes, the interaction between sinking and remineralization of organic matter, benthic fluxes and burial is not always represented consistently in global biogeochemical models. We here aim to investigate the relationships between these processes with a suite of global biogeochemical models, each simulated over millennia, and compared against observed distributions of pelagic tracers and benthic and pelagic fluxes. We concentrate on the representation of sediment-water interactions in common numerical models, and investigate their potential impact on simulated global sediment-water fluxes and nutrient and oxygen distributions. We find that model configurations with benthic burial simulate global oxygen well over a wide range of possible sinking flux parameterizations, making the model more robust with regard to uncertainties about the remineralization length scale. On a global scale, burial mostly affects oxygen in the meso- to bathypelagic zone. While all model types show an almost identical fit to observed pelagic particle flux, and the same sensitivity to particle sinking speed, comparison to observational estimates of benthic fluxes reveals a more complex pattern and may be influenced by the data distribution and methodology. Still, evaluating model results against observed pelagic and benthic fluxes of organic matter can complement model assessments based on more traditional tracers such as nutrients or oxygen. Based on a combined metric of dissolved tracers and biogeochemical fluxes, we here identify two model descriptions of burial as suitable candidates for further experiments and eventual model refinements.

Randomly Amplified Polymorphic DNA Reveals Tight Links between Viruses and Microbes in the Bathypelagic Zone of the Northwestern Mediterranean Sea

ABSTRACT The study site located in the Mediterranean Sea was visited eight times in 2005 and 2006 to collect samples from the epipelagic (5 m), mesopelagic (200 m, 600 m), and bathypelagic (1,000 m, 2,000 m) zones. Randomly amplified polymorphic DNA PCR (RAPD-PCR) analysis was used to obtain fingerprints from microbial and viral size fractions using two different primers each. Depending on the primer used, the number of bands in the water column varied between 12 to 24 and 6 to 19 for the microbial size fraction and between 16 to 26 and 8 to 22 for the viral size fraction. The majority of sequences from the microbial fraction was related to Alphaproteobacteria, Cyanobacteria, Gammaproteobacteria, Firmicutes, and Eukaryota. Only 9% of sequences obtained from the viral fraction were of identifiable viral origin; however, 76% of sequences had no close relatives in the nr database of GenBank. Only 20.1% of complete phage genomes tested in silico resulted in potential RAPD-PCR products, and only 12% of these were targeted by both primers. Also, in silico analysis indicated that RAPD-PCR profiles obtained by the two different primers are largely representative of two different subsets of the viral community. Also, correlation analyses and Mantel tests indicate that the links between changes in the microbial and viral community were strongest in the bathypelagic. Thus, these results suggest a strong codevelopment of virus and host communities in deep waters. The data also indicate that virus communities in the bathypelagic zone can exhibit substantial temporal dynamics.