A new photodegradable molecule as a low impact ballast water biocide: efficacy screening on marine organisms from different trophic levels

2006 ◽  
Vol 149 (1) ◽  
pp. 7-16 ◽  
Author(s):  
M. Faimali ◽  
F. Garaventa ◽  
E. Chelossi ◽  
V. Piazza ◽  
O.D. Saracino ◽  
...  
1991 ◽  
Vol 1991 (59) ◽  
pp. 14-16 ◽  
Author(s):  
Madeleine M. Jones

2021 ◽  
Author(s):  
Jerome Pinti ◽  
Tim DeVries ◽  
Tommy Norin ◽  
Camila Serra-Pompei ◽  
Roland Proud ◽  
...  

<p>Diel Vertical Migration (DVM) is a key feature of pelagic and mesopelagic ecosystems, mainly driven by predator-prey interactions along a time-varying vertical gradient of light. Marine organisms including meso-zooplankton and fish typically hide from visual predators at depth during daytime and migrate up at dusk to feed in productive near-surface waters during nighttime. Specific migration patterns, however, vary tremendously, for instance in terms of residency depth during day and night. In addition to environmental parameters such as light intensity and oxygen concentration, the migration pattern of each organism is intrinsically linked to the patterns of its conspecifics, its prey, and its predators through feedbacks that are hard to understand—but important to consider.</p><p>DVM not only affects trophic interactions, but also the biogeochemistry of the world’s oceans.  Organisms preying at the surface and actively migrating vertically transport carbon to depth, contributing to the biological carbon pump, and directly connecting surface production with mesopelagic and demersal ecosystems.</p><p>Here, we present a method based on a game-theoretic trait-based mechanistic model that enables the optimal DVM patterns for all organisms in a food-web to be computed simultaneously. The results are used to investigate the contributions of the different food-web pathways to the active component of the biological carbon pump. We apply the method to a modern pelagic food-web (comprised of meso- and macro-zooplankton, forage fish, mesopelagic fish, large pelagic fish and gelatinous organisms), shedding light on the direct effects that different trophic levels can have on the DVM behaviours of each other. The model is run on a global scale to assess the carbon export mediated by different functional groups, through fecal pellet production, carcasses sinking and respiration.</p><p>Finally, the model output is coupled to an ocean inverse circulation model to assess the carbon sequestration potential of the different export pathways. Results indicate that the carbon sequestration mediated by fish is much more important than presently recognised in global assessments of the biological carbon pump. The work we present relates to contemporary ecosystems, but we also explain how it can be adapted to fit any pelagic food-web structure to assess the contribution of the active biological pump to the global carbon cycle in past ecosystems.</p>


PLoS ONE ◽  
2017 ◽  
Vol 12 (3) ◽  
pp. e0172468 ◽  
Author(s):  
Katharine J. Carney ◽  
Mark S. Minton ◽  
Kimberly K. Holzer ◽  
A. Whitman Miller ◽  
Linda D. McCann ◽  
...  

2008 ◽  
Vol 8 (2) ◽  
pp. 74-79 ◽  
Author(s):  
Luigi Pane ◽  
Elisabetta Giacco ◽  
Christian Corrà ◽  
Giuliano Greco ◽  
Gian Luigi Mariottini ◽  
...  

Author(s):  
S.A.M.A.I.K. Senanayake ◽  
R.R.M.P.K. Ranathunga ◽  
A.J.M. Gunasekara ◽  
N. Priyadarshana

Chemosphere ◽  
2020 ◽  
Vol 238 ◽  
pp. 124592 ◽  
Author(s):  
David Nos ◽  
Joan Navarro ◽  
Enric Saiz ◽  
Juan C. Sanchez-Hernandez ◽  
Montserrat Solé

2018 ◽  
Vol 35 (1-2) ◽  
pp. 31-36
Author(s):  
M.T. Babu ◽  
K Sudheesh ◽  
P Vethamony ◽  
S Anuvindha

Aquatic organisms and pathogens may become major threats to the coastal and marine environment when introduced into a region beyond their natural distributions through ballast water (BW). Coastal currents induced by tides and winds, especially ebb currents, may facilitate the spread of these marine organisms along nearshore and inshore areas. Numerical modelling of hydrodynamics is an effective tool to track the dispersion of these organisms in the receiving water body through BW release. Particle transport models can be used to track the advection and dispersion of these organisms. Alternatively, the difference in salinity of the BW and coastal waters can be used as a tracer to estimate the dispersion pattern. Tides and winds present in the region at the time of BW release are responsible for the dispersal of the particles present in BW discharge. Based on advection and dispersion processes, the transport of the marine organisms present in the BW can be studied using numerical models. Numerical modelling studies were carried out using the 2-D hydrodynamic model MIKE21 HD, to understand the pattern of BW dispersion at select bioregions along the east and west coasts of India. Mangalore Port located along the west coast in Bioregion-I (CIO-I) and Chennai Port on the east coast in Bioregion-II (CIO-II) were selected for the modelling study. Results obtained from ballast water dispersion modelling studies will be useful for developing and assisting port-based ballast water management programmes for CIO-I and CIO-II regions. The currents are predominantly tide driven near the ports situated along the west coast and the circulation exhibited reversals associated with the tidal currents. However, along the east coast of India, the particles largely followed coastal currents - advected either southward or northward under the influence of prevailing coastal currents in the offshore region and tidal reversals showed had less impact. This information proved useful for determining suitable locations for BW discharge and monitoring points for field sampling in connection with BW release.


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