Modern MT: A New Open-Source Machine Translation Platform for the Translation Industry

Modern MT (www.modernmt.eu) is a three-year Horizon 2020 innovation action (2015–2017) to develop new open-source machine translation technology for use in translation production environments, both fully automatic and as a back-end in interactive post-editing scenarios. Led by Translated srl, the project consortium also includes the Fondazione Bruno Kessler (FBK), the University of Edinburgh, and TAUS B.V. Modern MT has received funding from the European Union’s Horizon 2020 research and innovation programme under Grant Agreement No 645487 (call ICT-17-2014)

The Skeletal Organic Matrix from Mediterranean Coral Balanophyllia europaea Influences Calcium Carbonate Precipitation

Scleractinian coral skeletons are made mainly of calcium carbonate in the form of aragonite. The mineral deposition occurs in a biological confined environment, but it is still a theme of discussion to what extent the calcification occurs under biological or environmental control. Hence, the shape, size and organization of skeletal crystals from the cellular level through the colony architecture, were attributed to factors as diverse as mineral supersaturation levels and organic mediation of crystal growth. The skeleton contains an intra-skeletal organic matrix (OM) of which only the water soluble component was chemically and physically characterized. In this work that OM from the skeleton of the Balanophyllia europaea, a solitary scleractinian coral endemic to the Mediterranean Sea, is studied in vitro with the aim of understanding its role in the mineralization of calcium carbonate. Mineralization of calcium carbonate was conducted by overgrowth experiments on coral skeleton and in calcium chloride solutions containing different ratios of water soluble and/or insoluble OM and of magnesium ions. The precipitates were characterized by diffractometric, spectroscopic and microscopic techniques. The results showed that both soluble and insoluble OM components influence calcium carbonate precipitation and that the effect is enhanced by their co-presence. The role of magnesium ions is also affected by the presence of the OM components. Thus, in vitro, OM influences calcium carbonate crystal morphology, aggregation and polymorphism as a function of its composition and of the content of magnesium ions in the precipitation media. This research, although does not resolve the controversy between environmental or biological control on the deposition of calcium carbonate in corals, sheds a light on the role of OM, which appears mediated by the presence of magnesium ions

Variations in growth and skeletal characteristics of a temperate non-zooxanthellate colonial coral naturally living at CO2 vents

Ocean acidification may impact ecosystems reliant on calcifying organisms, potentially reducing thesocioeconomic benefits these habitats provide. This study investigates the response of growth and skeletalproperties of the non-zooxanthellate stony coral Astroides calycularis living in naturally acidified seawater ata Mediterranean CO2 vent (Ischia, Italy). Unexpectedly, contrasting patterns of calcification were found atpolyp and colony levels. Polyp linear extension rate, bulk skeletal density and net calcification rate increasedwith acidification (i.e., skeletal porosity decreased). At the colony level, a decrease of net calcification ratewas observed in acidified conditions, with colonies that extended less, were smaller, and were composed byfewer polyps, thus partitioning the available energy among less polyps. As a result, the single polyps had ahigher amount of resources available for calcification than in control conditions, and all their growthparameters had higher values. This unforeseen pattern of response to acidification was observed in this studyfor the first time, and contrasts with what previously observed in the Mediterranean solitary coralBalanophyllia europaea,whose polyps invest the calcification resources in linear extension rate to reach thesize at sexual maturity at the expenses of skeletal resistance (i.e. bulk skeletal density). In the colonial A.calycularis asexual reproduction is possible and corals may invest more on skeletal resistance without theurge to reach sexual maturity

Effects of ocean acidification on skeletal characteristics of a temperate coral at a CO2 vent system

Ocean Acidification (OA) is predicted to have profound impacts on marine ecosystems because carbonate ions are an essential substrate for the biomineralization of shells and skeletons of calcifying marine organisms, from phytoplankton and corals to fishes1,2,3. Volcanic CO2 vent systems, where seawater is naturally acidified, offer a unique opportunity to investigate the response of benthic organisms and habitats to OA. The Ischia Island (Tyrrhenian Sea, Italy) offers a natural laboratory for OA studies, allowing us to investigate how a suite of habitats and species responds to acidification. A. calycularis is a Mediterranean endemic azooxanthellate coral. It is long-lived species and commonly found in dim light shallow rocky habitats of the south-western Mediterranean Sea4. It broods its larvae5 and thus has relatively low dispersal capacities and high potential for local adaptation. This coral is reported as vulnerable in the IUCN red list6. There is one population of A. calycularis that naturally occurs in a semi-submersed cave (Grotta del Mago) affected by CO2 venting, where is highly abundant (70% cover at 1 m depth). Here, we assess population structure and the skeletal characteristics of A. calycularis originating from different sites (naturally acidified and ambient pH sites) along the coast of Ischia Island . We hypothesize that the population thriving under naturally acidified conditions shows higher population dynamics and differences in biomineralization process than the populations studied from other reference sites with ambient pH.Colonies in the Grotta del Mago have encrusting morphology, with smaller size and consequent, lower weight and lower number of polyps compared to conspecifics from sites at normal pH conditions. With increasing acidification (lower pH), the skeletal porosity decreased while the bulk and micro- density increased. Given the reduced calcification rate that may be expected in acidified waters, the observed increase in skeletal density may be counterbalanced by a strong decrease in linear extension rate

Patterns in microbiome composition differ with ocean acidification in anatomic compartments of the Mediterranean coral Astroides calycularis living at CO2 vents

Coral microbiomes, the complex microbial communities associated with the different anatomic compartments of the coral, provide important functions for the host's survival, such as nutrient cycling at the host's surface, prevention of pathogens colonization, and promotion of nutrient uptake. Microbiomes are generally referred to as plastic entities, able to adapt their composition and functionality in response to environmental change, with a possible impact on coral acclimatization to phenomena related to climate change, such as ocean acidification. Ocean sites characterized by natural gradients of pCO2 provide models for investigating the ability of marine organisms to acclimatize to decreasing seawater pH. Here we compared the microbiome of the temperate, shallow water, non-symbiotic solitary coral Astroides calycularis that naturally lives at a volcanic CO2 vent in Ischia Island (Naples, Italy), with that of corals living in non-acidified sites at the same island. Bacterial DNA associated with the different anatomic compartments (mucus, tissue and skeleton) of A. calycularis was differentially extracted and a total of 68 samples were analyzed by 16S rRNA gene sequencing. In terms of phylogenetic composition, the microbiomes associated with the different coral anatomic compartments were different from each other and from the microbial communities of the surrounding seawater. Of all the anatomic compartments, the mucus-associated microbiome differed the most between the control and acidified sites. The differences detected in the microbial communities associated to the three anatomic compartments included a general increase in subdominant bacterial groups, some of which are known to be involved in different stages of the nitrogen cycle, such as potential nitrogen fixing bacteria and bacteria able to degrade organic nitrogen. Our data therefore suggests a potential increase of nitrogen fixation and recycling in A. calycularis living close to the CO2 vent system