47 research outputs found

    Fussy Feeders: Phyllosoma Larvae of the Western Rocklobster (Panulirus cygnus) Demonstrate Prey Preference

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    The Western Rocklobster (Panulirus cygnus) is the most valuable single species fishery in Australia and the largest single country spiny lobster fishery in the world. In recent years a well-known relationship between oceanographic conditions and lobster recruitment has become uncoupled, with significantly lower recruitment than expected, generating interest in the factors influencing survival and development of the planktonic larval stages. The nutritional requirements and wild prey of the planktotrophic larval stage (phyllosoma) of P. cygnus were previously unknown, hampering both management and aquaculture efforts for this species. Ship-board feeding trials of wild-caught mid-late stage P. cygnus phyllosoma in the eastern Indian Ocean, off the coast of Western Australia, were conducted in July 2010 and August-September 2011. In a series of experiments, phyllosoma were fed single and mixed species diets of relatively abundant potential prey items (chaetognaths, salps, and krill). Chaetognaths were consumed in 2–8 times higher numbers than the other prey, and the rate of consumption of chaetognaths increased with increasing concentration of prey. The highly variable lipid content of the phyllosoma, and the fatty acid profiles of the phyllosoma and chaetognaths, indicated they were from an oligotrophic oceanic food chain where food resources for macrozooplankton were likely to be constrained. Phyllosoma fed chaetognaths over 6 days showed significant changes in some fatty acids and tended to accumulate lipid, indicating an improvement in overall nutritional condition. The discovery of a preferred prey for P. cygnus will provide a basis for future oceanographic, management and aquaculture research for this economically and ecologically valuable species

    Biogeochemical and ecological impacts of boundary currents in the Indian Ocean

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    Monsoon forcing and the unique geomorphology of the Indian Ocean basin result in complex boundary currents, which are unique in many respects. In the northern Indian Ocean, several boundary current systems reverse seasonally. For example, upwelling coincident with northward-flowing currents along the coast of Oman during the Southwest Monsoon gives rise to high productivity which also alters nutrient stoichiometry and therefore, the species composition of the resulting phytoplankton blooms. During the Northeast Monsoon most of the northern Indian Ocean boundary currents reverse and favor downwelling. Higher trophic level species have evolved behavioral responses to these seasonally changing conditions. Examples from the western Arabian Sea include vertical feeding migrations of a copepod (Calanoides carinatus) and the reproductive cycle of a large pelagic fish (Scomberomorus commerson). The impacts of these seasonal current reversals and changes in upwelling and downwelling circulations are also manifested in West Indian coastal waters, where they influence dissolved oxygen concentrations and have been implicated in massive fish kills. The winds and boundary currents reverse seasonally in the Bay of Bengal, though the associated changes in upwelling and productivity are less pronounced. Nonetheless, their effects are observed on the East Indian shelf as, for example, seasonal changes in copepod abundance and zooplankton community structure. In contrast, south of Sri Lanka seasonal reversals in the boundary currents are associated with dramatic changes in the intensity of coastal upwelling, chlorophyll concentration, and catch per unit effort of fishes. Off the coast of Java, monsoon-driven changes in the currents and upwelling strongly impact chlorophyll concentrations, seasonal vertical migrations of zooplankton, and sardine catch in Bali Strait. In the southern hemisphere the Leeuwin is a downwelling-favorable current that flows southward along western Australia, though local wind forcing can lead to transient near shore current reversals and localized coastal upwelling. The poleward direction of this eastern boundary current is unique. Due to its high kinetic energy the Leeuwin Current sheds anomalous, relatively high chlorophyll, warm-core, downwelling eddies that transport coastal diatom communities westward into open ocean waters. Variations in the Leeuwin transport and eddy generation impact many higher trophic level species including the recruitment and fate of rock lobster (Panulirus cygnus) larvae. In contrast, the transport of the Agulhas Current is very large, with sources derived from the Mozambique Channel, the East Madagascar Current and the southwest Indian Ocean sub-gyre. Dynamically, the Agulhas Current is upwelling favorable; however, the spatial distribution of prominent surface manifestations of upwelling is controlled by local wind and topographic forcing. Meanders and eddies in the Agulhas Current propagate alongshore and interact with seasonal changes in the winds and topographic features. These give rise to seasonally variable localized upwelling and downwelling circulations with commensurate changes in primary production and higher trophic level responses. Due to the strong influence of the Agulhas Current, many neritic fish species in southeast Africa coastal waters have evolved highly selective behaviors and reproductive patterns for successful retention of planktonic eggs and larvae. For example, part of the Southern African sardine (Sardinops sagax) stock undergoes a remarkable northward migration enhanced by transient cyclonic eddies in the shoreward boundary of the Agulhas Current. There is evidence from the paleoceanographic record that these currents and their biogeochemical and ecological impacts have changed significantly over glacial to interglacial timescales. These changes are explored as a means of providing insight into the potential impacts of climate change in the Indian Ocean

    Computing return times or return periods with rare event algorithms

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    The average time between two occurrences of the same event, referred to as its return time (or return period), is a useful statistical concept for practical applications. For instance insurances or public agencies may be interested by the return time of a 10 m flood of the Seine river in Paris. However, due to their scarcity, reliably estimating return times for rare events is very difficult using either observational data or direct numerical simulations. For rare events, an estimator for return times can be built from the extrema of the observable on trajectory blocks. Here, we show that this estimator can be improved to remain accurate for return times of the order of the block size. More importantly, we show that this approach can be generalised to estimate return times from numerical algorithms specifically designed to sample rare events. So far those algorithms often compute probabilities, rather than return times. The approach we propose provides a computationally extremely efficient way to estimate numerically the return times of rare events for a dynamical system, gaining several orders of magnitude of computational costs. We illustrate the method on two kinds of observables, instantaneous and time-averaged, using two different rare event algorithms, for a simple stochastic process, the Ornstein-Uhlenbeck process. As an example of realistic applications to complex systems, we finally discuss extreme values of the drag on an object in a turbulent flow. © 2018 IOP Publishing Ltd and SISSA Medialab srl

    Estimates of exploitation rates of the spiny lobster fishery for Panulirus argus from tagging within the BahĂ­a EspĂ­ritu Santa 'Sian Ka'an' Biosphere Reserve, Mexican Caribbean

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    The Caribbean spiny lobster (Panulirus argus) fishery is currently being assessed for a certification process. It is the main economic activity within the Biosphere Reserve of Sian Ka'an-Mexico (SK), which is a marine-protected area where restricted access fishing is allowed. In this study, commercial catch rates were examined, and lobsters over a wide size range were tagged throughout the 2010/2011 fishing season, to assess fishing mortality rates and movement patterns in Bahía Espíritu Santo-SK. Lobster tag recovery data were aggregated into 2-week periods and analysed using a modified Brownie model that was parameterized to account for lobster tag-reporting, and the lobster tag-retention rates. This allowed the estimation of instantaneous rates of natural and fishing mortality, considering catchability and fishing effort. Independent aquaria trials were conducted to better estimate lobster tag retention, tagging-induced mortality and interviews with fishermen were conducted to better estimate lobster tag reporting. Based mainly on legal-sized juveniles with fast growth rates found in casitas, the stock is subject to fishing to a maximum depth of 20 m, because of the prohibition of SCUBA diving and the use of other fishing gear. The Brownie model indicated that exploitation rates within this bay area were high,>0.94. Changes in catch per unit of effort and catchability throughout the season explain how the ‘casita/campo’ system allows for a seasonal replenishment of juveniles and adults, which has kept the landings relatively stable for the past decade

    Un nouveau systĂšme d’imagerie gamma portable dĂ©diĂ© Ă  la dĂ©tection et Ă  la visualisation des points chauds dans les centrales nuclĂ©aires

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    International audienceA new portable gamma imaging system dedicated to the detection and the direct visualisation of hot spots in nuclear power plants. In a nuclear power plant (NPP), the localization of radioactive hot spots is a major issue, as they are responsible for a significant part of the doses received by the workers, especially during maintenance operations. Since 2010, EDF and CEA havebeen adapting a new generation camĂ©ra gamma, GAMPIX, to have a dedicated portable tool available for this use. This system enables to superimpose a gamma image with a visible image, in order to locate radioactive sources in a given area. Onsitemeasurements at the Tricastin EDF NPP, combined with specific developments at CEA, have been carried out in order to meet the particular environmental and radiological conditions experienced in such industrial facilities: the relatively high energy of cobalt-60 (1.17 and 1.33 MeV) and the existence of an ubiquitous background. This article will present the specifications required, the corresponding improvements and the main results obtained during the on-site measurements campaigns. Even if they were dedicated to the qualification of the camera, the tests carried out showed useful results like the leakage lines along a lead protection and the displacement of a hot spot in a pipe (compared to its identified position). At the end, further developments are presented.Dans une centrale nuclĂ©aire (CNPE), la localisation des points chauds est une prĂ©occupation importante, car ils participent Ă  la dose que reçoivent les intervenants, en particulier lors des opĂ©rations de maintenance. Depuis 2010, EDF et le CEA ont entrepris d’adapter une nouvelle gĂ©nĂ©ration de camĂ©ra gamma, GAMPIX, pour disposer d’un instrument portable dĂ©diĂ© Ă  cet usage. Ce systĂšme permet de superposer une image gamma Ă  une image visible, afin de localiser les sources radioactives prĂ©-sentes dans un environnement. Des essais sur site au CNPE de Tricastin ont Ă©tĂ© associĂ©s aux dĂ©veloppements spĂ©cifiques rĂ©alisĂ©s par le CEA, afin d’apprĂ©hender les conditions particuliĂšres rencontrĂ©es en CNPE, Ă  la fois environnementales et radiologiques : l’énergie relativement Ă©levĂ©e des gamma du cobalt 60 (1,17 et 1,33 MeV) et la prĂ©sence d’un bruit de fond ambiant permanent. Cet article prĂ©sente les principaux axes du cahier des charges initial, les dĂ©veloppements rĂ©alisĂ©s pour y rĂ©pondre, et les rĂ©sultats obtenus lors des campagnes d’essais. MĂȘme s’ils Ă©taient uniquement dĂ©diĂ©s Ă  la qualification de la camĂ©ra gamma, les tests rĂ©alisĂ©s ont montrĂ© des rĂ©sultats trĂšs prometteurs, par exemple la mise en Ă©vidence de lignes de fuite le long d’une protection biologique ou le mouvement d’un point chaud dans une tuyauterie (par rapport Ă  sa position identifiĂ©e). En dernier lieu, les dĂ©veloppements futurs sont Ă©voquĂ©s
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