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Marine snow is an important part of the biological pump and marine food web, and although previous research has provided a thorough understanding of the underlying mechanisms of marine snow dynamics in general, there is still a knowledge gap concerning extreme conditions, such as storm events. Storms are predicted to increase in magnitude and frequency in the future, and could potentially have a large impact on marine snow dynamics. For these reasons, we assessed the effects of storm events on marine snow dynamics in the Baltic Sea, an area chosen due to its well-studied and stable stratified conditions outside of meteorologically extreme events. The combination of in-situ imaging and biogeochemical environmental data from three different years facilitates an assessment of storm event impacts, while simultaneously excluding the possibility that patterns in particle distribution and abundances were due to other environmental influences. The results show that extreme meteorological events such as storms can increase the abundance of marine snow in stratified marine environments by a factor of 10 or more. The particles are distributed more widely and are larger, brighter, rounder and less complexly shaped. In non-extreme conditions, particles have been observed to deposit along the density gradients in thin-layer aggregations. This study indicates that storms can episodically disrupt these formations, thereby altering vertical flux and export potentials across stratification boundaries. In addition, we observed that marine snow abundances are drastically higher in the aftermath of storm events than under calm conditions, potentially due to the disaggregation of larger particles and lateral import of resuspended matter from shallower areas. In light of the increased frequency and magnitude of storms in the future due to climate change, our findings indicate that marine snow dynamics in stratified environments might be altered permanently. • Storms cause higher marine snow abundances and a more even vertical distribution. • The combination of higher abundances and smaller particles indicates disaggregation. • Resuspension of particulates from shallow areas is a likely contributor to the increased abundance. [ABSTRACT FROM AUTHOR]

Predators not only have direct impact on biomass but also indirect, non-consumptive effects on the behavior their prey organisms. A characteristic response of zooplankton in aquatic ecosystems is predator avoidance by diel vertical migration (DVM), a behavior which is well studied on the population level. A wide range of behavioral diversity and plasticity has been observed both between- as well as within-species and, hence, investigating predator–prey interactions at the individual level seems therefore essential for a better understanding of zooplankton dynamics. Here we applied an underwater imaging instrument, the video plankton recorder (VPR), which allows the non-invasive investigation of individual, diel adaptive behavior of zooplankton in response to predators in the natural oceanic environment, providing a finely resolved and continuous documentation of the organisms' vertical distribution. Combing observations of copepod individuals observed with the VPR and hydroacoustic estimates of predatory fish biomass, we here show (i) a small-scale DVM of ovigerous Pseudocalanus acuspes females in response to its main predators, (ii) in-situ observations of a direct short-term reaction of the prey to the arrival of the predator and (iii) in-situ evidence of pronounced individual variation in this adaptive behavior with potentially strong effects on individual performance and ecosystem functioning. [ABSTRACT FROM AUTHOR]

Zooplankton consumption of sinking aggregates affects the quality and quantity of organic carbon exported to the deep ocean. Increasing laboratory evidence shows that small particle‐associated copepods impact the flux attenuation by feeding on sinking particles, but this has not been quantified in situ. We investigated the impact of an abundant particle‐colonizing copepod, Microsetella norvegica, on the attenuation of the vertical carbon flux in a sub‐Arctic fjord. This study combines field measurements of vertical carbon flux, abundance, and size‐distribution of marine snow and degradation rates of fecal pellets and algal aggregates. Female M. norvegica altered their feeding behavior when exposed to aggregates, and ingestion rates were 0.20 μg C ind.−1 d−1 on marine snow and 0.11 μg C ind.−1 d−1 on intact krill fecal pellets, corresponding to 48% and 26% of the females' body carbon mass. Due to high sea surface abundance of up to ~ 50 ind. L−1, the population of M. norvegica had the potential to account for almost all the carbon removal in the upper 50 m of the water column, depending on the type of the aggregate. Our observations highlight the potential importance of abundant small‐sized copepods for biogeochemical cycles through their impact on export flux and its attenuation in the twilight zone. [ABSTRACT FROM AUTHOR]

• Deciding whether to include a new process in a model cannot be objective. • An open-access event allowed people to design a flowchart for making this decision. • The flowcharts created highlight many issues that the decision needs to account for. • Variability between flowcharts is used to illustrate subjectivity behind a decision. • There is no perfect flowchart - but creating one's own is itself valuable. Models are critical tools for environmental science. They allow us to examine the limits of what we think we know and to project that knowledge into situations for which we have little or no data. They are by definition simplifications of reality. There are therefore inevitably times when it is necessary to consider adding a new process to a model that was previously omitted. Doing so may have consequences. It can increase model complexity, affect the time a model takes to run, impact the match between the model output and observations, and complicate comparison to previous studies using the model. How a decision is made on whether to add a process is no more objective than how a scientist might design a laboratory experiment. To illustrate this, we report on an event where a broad and diverse group of marine biogeochemists were invited to construct flowcharts to support making the decision of when to include a new process in a model. The flowcharts are used to illustrate both the complexity of factors that modellers must consider prior to making a decision on model development and the diversity of perspectives on how that decision should be reached. The purpose of this paper is not to provide a definitive protocol for making that decision. Instead, we argue that it is important to acknowledge that there is no objectively "best" approach and instead we discuss the flowcharts created as a means of encouraging modellers to think through why and how they are doing something. This may also hopefully guide observational scientists to understand why it may not always be appropriate to include a process they are studying in a model. [ABSTRACT FROM AUTHOR]

A recent increase in the construction of Offshore Wind Farms (OWFs) has initiated numerous environmental impact assessments and monitoring programs. These focus on sea mammals, seabirds, benthos or demersal fish, but generally ignore any potential effects OWFs may have on the pelagic ecosystem. The only work on the latter has been through modelling analyses, which predict localised impacts like enhanced vertical mixing leading to a decrease in seasonal stratification, as well as shelf-wide changes of tidal amplitudes. Here we provide for the first-time empirical bio-physical data from an OWF. The data were obtained by towing a remotely operated vehicle (TRIAXUS ROTV) through two non-operating OWFs in the summer stratified North Sea. The undulating TRIAXUS transects provided high-resolution CTD data accompanied by oxygen and chlorophyll- a measurements. We provide empirical indication that vertical mixing is increased within the OWFs, leading to a doming of the thermocline and a subsequent transport of nutrients into the surface mixed layer (SML). Nutrients were taken up rapidly because underwater photosynthetically active radiation (PAR) enabled net primary production in the entire water column, especially within submesoscale chlorophyll- a pillars that were observed at regular intervals within the OWF regions. Video Plankton Recorder (VPR) images revealed distinct meroplankton distribution patterns in a copepod-dominated plankton community. Hydroacoustic records did not show any OWF effects on the distribution of pelagic fish. The results of a pre-OWF survey show however, that it is difficult to fully separate the anthropogenic impacts from the natural variability. [ABSTRACT FROM AUTHOR]

If some approaches have been developed for automated estimation of pigment groups (from scientist or companies), the data have not yet been hosted by a European data infrastructure, and data format and vocabulary still need to be better defined. Véronique Créach, Cefas (UK), veronique.creach@cefas.co.uk Luis Felipe Artigas, CNRS-LOG (France), felipe.artigas@univ-littoral.fr Alain Lefebvre, Ifremer (France), Alain.Lefebvre@ifremer.fr Markus Lindh, SMHI (Sweden), markus.lindh@smhi.se Fabien Lombard, CNRS-LOV (France), lombard@obs-vlfr.fr Klas Ove Möller, HZG (Germany), klas.moeller@hzg.de Lennert Schepers, VLIZ (Belgium), lennert.schepers@vliz.be Jukka Seppälä, SYKE (Finland), jukka.seppala@ymparisto.fi Melilotus Thyssen, CNRS-MIO (France), melilotus.thyssen@mio.osupytheas.fr JERICO-S3 is a new building-block in the "Joint European Research Infrastructure network of Coastal Observatories" concept. on-line automated flow cytometry: this single-cell/particle inflow technology becomes more and more popular for optically defining phytoplankton functional groups over the whole size range, due to the versatility and the autonomy of the instruments. [Extracted from the article]