This thesis presents the first description of the geographic and depth distributions of pelagic decapod shrimps in the area located around the Deepwater Horizon oil spill, based on the NOAA (National Oceanic and Atmospheric Administration) NRDA (National Resource Damage Assessment) trawl samples collected from April – June, 2011. This information is important in ecosystem models investigating trophic effects of the spill because pelagic decapod shrimp are consumed by a variety of organisms occupying higher trophic levels. One of the most abundant and diverse groups of decapods is the Family Oplophoridae. Their roles in pelagic food webs in the Gulf of Mexico (GOM) and other deep-sea ecosystems makes them ideal candidates for study; however, only a limited amount of research has been conducted on their distribution and reproductive biology. In the northeastern GOM, all previous studies have been conducted at Standard Station in the eastern Gulf (27°N, 86°W) (Hopkins and Lancraft, 1984; Hopkins et al., 1989; Hopkins and Gartner, 1992; Hopkins et al., 1994). The current study is unique because 1) it provides data from regions of the Gulf where oplophorids have never been studied, 2) allows for comparisons of distributions and abundances of oplophorid species in both the mesopelagic and bathypelagic zones by using a continuous data set, and 3) compares assemblages from two distinct bathymetric environments in the northeastern GOM: continental slope (200-1000 m bottom depth) and offshore (>1000 m). As the study site also encompasses the region most strongly impacted by the Deepwater Horizon oil spill, these data represent the first quantification of any component of the decapod crustacean assemblage in this location after the oil spill, and will be used for comparison with data obtained during future DEEPEND Consortium (Deep Pelagic Nekton Dynamics of the Gulf of Mexico) cruises to monitor changes, or lack thereof, in the assemblage after exposure to Deepwater Horizon oil and dispersants in the water column.

No description available.

No description available.

In 2010, the largest oil spill in U.S history occurred off the coast of Louisiana from April 20th to September 19th, when the well was declared officially sealed by the U.S Coast Guard, after releasing more than 4.4 million barrels of crude oil into the Gulf of Mexico (GOM) (McNutt et al., 2012). This spill was unique because it occurred in deep water approximately 1500 m below the ocean surface. Virtually nothing is known about the effects of oil spills on marine life in the deep sea, and there are limited data on mesopelagic and bathypelagic animals in the GOM before the Deepwater Horizon oil spill (DWHOS). The study presented here focuses on one of the most abundant and diverse groups of pelagic decapod crustaceans in the GOM – the family Oplophoridae and also includes one species from the family Pandalidae. Past studies on pelagic decapod crustaceans have been limited on both spatial and temporal scales. This study is unique because 1) it covers a large temporal range with data collected in 2011 and from 2015-2017, allowing for a more in-depth look at crustacean assemblage patterns, 2) it allows analysis of seasonality in reproduction, about which little is known for any deep-sea species, and 3) it assesses the potential effects of the Loop Current on species distribution and abundances, about which little is known. This information is important in understanding how the DWHOS may have affected the GOM ecosystem because pelagic decapod crustacean are intermediate components of the food web, and are in turn preyed upon by higher trophic levels. Unfortunately, there were little data on the mesopelagic ecosystem from this region before the spill, with the exception of a site in the eastern GOM (Standard Station, Hopkins et al., 1989; Hopkins et al., 1994). Therefore, these data, which incorporate samples taken one, five, six and seven years after the DWHOS, were analyzed with respect to year and season to determine if any trends were present. Results indicate that both biomass and abundance were significantly higher in 2011, than in subsequent years, indicating that the ecosystem has been declining since 2011. These two parameters were also lower in Loop Current water when compared to Common Water at all depths up to 1200 m, indicating that the Loop Current does have effects on deeper waters. The information obtained from this thesis will also act as a reference state for future studies in the GOM to monitor changes, or lack thereof, in the assemblage of deep-sea oplophorid and pandalid crustaceans.

Como resultado do seu passado evolutivo, a família dos camarões Palaemonidae reúne representantes de ambientes osmóticos dos mais variados. Sejam de ambientes marinhos, estuarinos ou dulcícolas, estáveis ou variáveis, as espécies destes camarões mantêm a concentração osmo-iônica da hemolinfa independente da concentração do meio. Essas espécies hiper-regulam a osmolalidade e íons da hemolinfa em meio diluído e água doce e hipo-regulam em meio concentrado ou água do mar. Um importante local de transporte iônico envolvido na regulação osmo-iônica é o epitélio brânquial, pois nas membranas de seus ionócitos constituintes encontra-se um conjunto de transportadores que efetuam o movimento transepitelial de íons. Dentre estes transportadores, o simportador Na+, K+, 2Cl- (NKCC) é considerado ter um papel na secreção de sal, objetivo primário dessa investigação. Espécies representativas de habitat marinho do gênero Palaemon foram coletadas em regiões de estuário e de poça de maré, e de habitat dulcícola do gênero Macrobrachium foram coletadas em rios que desembocam no mar e também em riachos continentais sem influência do aporte salobro. Avaliou-se os limites letais de salinidade superior (LSS50) das espécies marinhas P. northropi e P. pandaliformis e dulcícolas diádromas M. acanthurus, M. olfersi, M. amazonicum que dependem de água salobra para completo desenvolvimento larval, e hololimnéticas M. potiuna e M. brasiliense com ciclo reprodutivo completo em água doce. Objetivou-se aqui (i) caracterizar os mecanismos de hiperregulação (condição controle de 18 S P. northropi, 17 S P. pandaliformis, água doce <0,5 S nas espécies de Macrobrachium) e hiporegulação [a curto (24 h) e longo prazo (120 h) em salinidade correspondente a 80% da LSS50] da osmolalidade e [Cl-] da hemolinfa, da expressão gênica e proteica e a localização por imunofluorescência do NKCC nos ionócitos branquiais; (ii) da existência de um padrão filogenético nesses parâmetros; e (iii) testar as hipóteses de um efeito da salinidade na evolução da expressão gênica e proteica desse simportador. As espécies de Palaemon apresentaram os maiores limites de tolerância ao aumento da salinidade, assim como exibiram uma maior capacidade hiporegulatória a longo prazo (120 h) comparada aos representantes de Macrobrachium. Dentre as espécies de Macrobrachium, os limites de tolerância foram maiores nas espécies diádromas do que nas hololimnéticas. Os parâmetros LSS50, osmolalidade e [Cl-] da hemolinfa demonstraram-se estruturados na filogenia, sendo as semelhanças compartilhadas justificadas pela estreita proximidade entre as espécies. As análises filogenéticas revelaram que a capacidade hiper-regulatória da [Cl-] da hemolinfa foi correlacionada com a expressão gênica do simportador NKCC nas brânquias, enquanto que a síntese proteica do NKCC parece estar associada à hiper-regulação da osmolalidade da hemolinfa. A avaliação da localização do NKCC por imunofluorescência demonstrou que o simportador está distribuído em ambas as células que compõem o epitélio das brânquias, as células pilares e células do septo intralamelar. A localização na porção inferior das franjas e no corpo da célula pilar e por toda célula do septo não diferiu entre as espécies, e também não difereiu entre as condições controle e a curto e longo prazo em salinidade elevada. Esses resultados em conjunto sugerem a importância do NKCC também na captação de sal pelas brânquias. Houve um aumento da síntese proteica do NKCC nas brânquias dos representantes de Macrobrachium, exceto M. potiuna, quando em salinidade elevada. Observou-se que este aumento é explicado pela proximidade filogenética entre as espécies. Não houve mudança na transcrição de RNAm para o NKCC apesar do aumento na síntese proteica, o que sugere uma possível regulação pós-transcricional. A reconstrução da história evolutiva da osmorregulação, incorporando o conceito de filofisiologia, revelou a existência de mecanismos em nível molecular, celular e sistêmico que evoluíram acompanhando os eventos cladogenéticos dos Palaemonidae durante a irradiação e ocupação de diferentes nichos osmóticos. / Owing to their evolutionary history, the shrimp family Palaemonidae includes species from widely distinct osmotic environments. Whether from marine, estuarine, or fresh waters, inhabiting stable or variable osmotic niches, these shrimps maintain the osmotic-ionic concentration of their hemolymph independently of the concentration of the external medium. These species hyper-regulate hemolymph osmolality and ions in dilute medium and fresh water and hypo-regulate this fluid in concentrated medium or seawater. The gill epithelium constitutes an important interface of ion transport, and its constituent ionocytes express an ensemble of ion transporters that enable active transepithelial ion movements. The Na+, K+, 2Cl- cotransporter (NKCC) is thought to play a significant role in compensatory salt secretion. Species representative of the marine habitat (Palaemon) were collected from estuaries and tidal pools; diadromous species from the fresh water habitat (Macrobrachium) were collected near the mouths of rivers that flow into the sea, while hololimnetic species were collected in continental streams lacking the influence of brackish waters. The critical upper salinity limits (LSS50) of the marine species P. northropi and P. pandaliformis and the diadromous freshwater species M. acanthurus, M. olfersi, M. amazonicum that depend on brackish water for complete larval development, and the hololimnetic M. potiuna and M. brasiliense that complete their reproductive cycle entirely in fresh water were established. Our objectives were to characterize the mechanisms of hyper-regulation (control condition 18 S P. northropi, 17 S P. pandaliformis, fresh water <0.5 S for Macrobrachium) and hypo-regulation [short-term (24 h) and long-term 120 h) at salinities corresponding to 80% of LSS50] of hemolymph osmolality and [Cl-], gene and protein expression, and NKCC localization for immunofluorescence in the gill ionocytes; (ii) the existence of a phylogenetic pattern in these parameters; and (iii) to test hypotheses for a salinity effect on the evolution of the gene and protein expression of this symporter. The species of Palaemon had the highest tolerance limits to increased salinity, and also exhibited a greater hypo-regulatory capacity for long-term acclimation compared to the species of Macrobrachium. Among the Macrobrachium species, the LSS50 were higher in the diadromous species than in the hololimnetic species. The parameters LSS50 and osmolality and [Cl-] of the hemolymph were phylogenetically structured, similarities being shared by closely related species. The hyper-regulatory capacity of hemolymph [Cl-] correlated with NKCC gene expression in the gills, while NKCC protein synthesis appears to be associated with hyper-regulation of hemolymph osmolality. Immunofluorescence analysis showed that the NKCC was located in both cell types that constitute the gill epithelium, the pillar cells and the septal cells. The location of the NKCC in the lower flanges and perikarya of the pillar cells and throughout the septal cells, did not differ among species, and also did not differ among control conditions or short and long-term exposure at high salinity. These results together also suggest the importance of the NKCC in salt uptake by the gills. When in high salinity there was an increase in NKCC protein synthesis in the gills of the Macrobrachium species, except for M. potiuna. This increase can be explained by the phylogenetic proximity among those species, which excludes adaptive inferences. There was no change in NKCC mRNA transcription, which suggests possible post-transcriptional regulation. The reconstruction of the evolutionary history of osmoregulation, incorporating the concept of phylophysiology, revealed the existence of mechanisms at the molecular, cellular and systemic levels that have evolved accompanying the cladogenetic events of the Palaemonidae during their radiation and occupation of different osmotic niches.

The condition at settlement of the western rock lobster pueruli presumably reflects both their energetic condition in reaching the near shore and subsequent recruitment into adult populations. In recruiting to the near shore the pueruli swim across the continental shelf where oceanographic conditions are complex and likely influence the success of recruitment. The results from the biochemical studies are interpreted in light of the oceanography off the coast of Western Australia. I investigated the nutritional condition of larval phyllosomata, post-larval puerulus and first instar post-pueruli juveniles of the spiny lobster, Panulirus cygnus, to determine energy use during the non-feeding transitional puerulus stage. Biochemical analyses of lipid, fatty acid (FA) and protein revealed that lipid, in particular phospholipids, is primarily used for energy during the nonfeeding puerulus stage. Monounsaturated FA showed the greatest decline with development, whereas the polyunsaturated FA showed a high degree of sparing, suggesting these FA are not used as a substrate for energy production. The knowledge gained on the biochemistry of energy use in P. cygnus was then used to investigate the spatial and temporal variability in the nutritional condition, in particular lipid condition, of puerulus collected at three near shore locations (Alkimos, Jurien Bay and Dongara) along the Western Australia coast, and one offshore location (Houtman Abrolhos Islands). The one offshore location was chosen as I hypothesised that arriving pueruli are likely to be in a better state of nutrition than those arriving at more coastal locations where the potential journey from offshore larval feeding grounds to the near shore is considerably greater. This element of my research showed lipid levels to be inversely related, generally, to shelf width but were variable, suggesting pueruli may travel complex trajectories to reach nearshore settlement. The lipid and FA composition of pueruli was also consistent with spatial and seasonal variation in Leeuwin Current and coastal productivity regimes.

Como resultado do seu passado evolutivo, a família dos camarões Palaemonidae reúne representantes de ambientes osmóticos dos mais variados. Sejam de ambientes marinhos, estuarinos ou dulcícolas, estáveis ou variáveis, as espécies destes camarões mantêm a concentração osmo-iônica da hemolinfa independente da concentração do meio. Essas espécies hiper-regulam a osmolalidade e íons da hemolinfa em meio diluído e água doce e hipo-regulam em meio concentrado ou água do mar. Um importante local de transporte iônico envolvido na regulação osmo-iônica é o epitélio brânquial, pois nas membranas de seus ionócitos constituintes encontra-se um conjunto de transportadores que efetuam o movimento transepitelial de íons. Dentre estes transportadores, o simportador Na+, K+, 2Cl- (NKCC) é considerado ter um papel na secreção de sal, objetivo primário dessa investigação. Espécies representativas de habitat marinho do gênero Palaemon foram coletadas em regiões de estuário e de poça de maré, e de habitat dulcícola do gênero Macrobrachium foram coletadas em rios que desembocam no mar e também em riachos continentais sem influência do aporte salobro. Avaliou-se os limites letais de salinidade superior (LSS50) das espécies marinhas P. northropi e P. pandaliformis e dulcícolas diádromas M. acanthurus, M. olfersi, M. amazonicum que dependem de água salobra para completo desenvolvimento larval, e hololimnéticas M. potiuna e M. brasiliense com ciclo reprodutivo completo em água doce. Objetivou-se aqui (i) caracterizar os mecanismos de hiperregulação (condição controle de 18 S P. northropi, 17 S P. pandaliformis, água doce <0,5 S nas espécies de Macrobrachium) e hiporegulação [a curto (24 h) e longo prazo (120 h) em salinidade correspondente a 80% da LSS50] da osmolalidade e [Cl-] da hemolinfa, da expressão gênica e proteica e a localização por imunofluorescência do NKCC nos ionócitos branquiais; (ii) da existência de um padrão filogenético nesses parâmetros; e (iii) testar as hipóteses de um efeito da salinidade na evolução da expressão gênica e proteica desse simportador. As espécies de Palaemon apresentaram os maiores limites de tolerância ao aumento da salinidade, assim como exibiram uma maior capacidade hiporegulatória a longo prazo (120 h) comparada aos representantes de Macrobrachium. Dentre as espécies de Macrobrachium, os limites de tolerância foram maiores nas espécies diádromas do que nas hololimnéticas. Os parâmetros LSS50, osmolalidade e [Cl-] da hemolinfa demonstraram-se estruturados na filogenia, sendo as semelhanças compartilhadas justificadas pela estreita proximidade entre as espécies. As análises filogenéticas revelaram que a capacidade hiper-regulatória da [Cl-] da hemolinfa foi correlacionada com a expressão gênica do simportador NKCC nas brânquias, enquanto que a síntese proteica do NKCC parece estar associada à hiper-regulação da osmolalidade da hemolinfa. A avaliação da localização do NKCC por imunofluorescência demonstrou que o simportador está distribuído em ambas as células que compõem o epitélio das brânquias, as células pilares e células do septo intralamelar. A localização na porção inferior das franjas e no corpo da célula pilar e por toda célula do septo não diferiu entre as espécies, e também não difereiu entre as condições controle e a curto e longo prazo em salinidade elevada. Esses resultados em conjunto sugerem a importância do NKCC também na captação de sal pelas brânquias. Houve um aumento da síntese proteica do NKCC nas brânquias dos representantes de Macrobrachium, exceto M. potiuna, quando em salinidade elevada. Observou-se que este aumento é explicado pela proximidade filogenética entre as espécies. Não houve mudança na transcrição de RNAm para o NKCC apesar do aumento na síntese proteica, o que sugere uma possível regulação pós-transcricional. A reconstrução da história evolutiva da osmorregulação, incorporando o conceito de filofisiologia, revelou a existência de mecanismos em nível molecular, celular e sistêmico que evoluíram acompanhando os eventos cladogenéticos dos Palaemonidae durante a irradiação e ocupação de diferentes nichos osmóticos. / Owing to their evolutionary history, the shrimp family Palaemonidae includes species from widely distinct osmotic environments. Whether from marine, estuarine, or fresh waters, inhabiting stable or variable osmotic niches, these shrimps maintain the osmotic-ionic concentration of their hemolymph independently of the concentration of the external medium. These species hyper-regulate hemolymph osmolality and ions in dilute medium and fresh water and hypo-regulate this fluid in concentrated medium or seawater. The gill epithelium constitutes an important interface of ion transport, and its constituent ionocytes express an ensemble of ion transporters that enable active transepithelial ion movements. The Na+, K+, 2Cl- cotransporter (NKCC) is thought to play a significant role in compensatory salt secretion. Species representative of the marine habitat (Palaemon) were collected from estuaries and tidal pools; diadromous species from the fresh water habitat (Macrobrachium) were collected near the mouths of rivers that flow into the sea, while hololimnetic species were collected in continental streams lacking the influence of brackish waters. The critical upper salinity limits (LSS50) of the marine species P. northropi and P. pandaliformis and the diadromous freshwater species M. acanthurus, M. olfersi, M. amazonicum that depend on brackish water for complete larval development, and the hololimnetic M. potiuna and M. brasiliense that complete their reproductive cycle entirely in fresh water were established. Our objectives were to characterize the mechanisms of hyper-regulation (control condition 18 S P. northropi, 17 S P. pandaliformis, fresh water <0.5 S for Macrobrachium) and hypo-regulation [short-term (24 h) and long-term 120 h) at salinities corresponding to 80% of LSS50] of hemolymph osmolality and [Cl-], gene and protein expression, and NKCC localization for immunofluorescence in the gill ionocytes; (ii) the existence of a phylogenetic pattern in these parameters; and (iii) to test hypotheses for a salinity effect on the evolution of the gene and protein expression of this symporter. The species of Palaemon had the highest tolerance limits to increased salinity, and also exhibited a greater hypo-regulatory capacity for long-term acclimation compared to the species of Macrobrachium. Among the Macrobrachium species, the LSS50 were higher in the diadromous species than in the hololimnetic species. The parameters LSS50 and osmolality and [Cl-] of the hemolymph were phylogenetically structured, similarities being shared by closely related species. The hyper-regulatory capacity of hemolymph [Cl-] correlated with NKCC gene expression in the gills, while NKCC protein synthesis appears to be associated with hyper-regulation of hemolymph osmolality. Immunofluorescence analysis showed that the NKCC was located in both cell types that constitute the gill epithelium, the pillar cells and the septal cells. The location of the NKCC in the lower flanges and perikarya of the pillar cells and throughout the septal cells, did not differ among species, and also did not differ among control conditions or short and long-term exposure at high salinity. These results together also suggest the importance of the NKCC in salt uptake by the gills. When in high salinity there was an increase in NKCC protein synthesis in the gills of the Macrobrachium species, except for M. potiuna. This increase can be explained by the phylogenetic proximity among those species, which excludes adaptive inferences. There was no change in NKCC mRNA transcription, which suggests possible post-transcriptional regulation. The reconstruction of the evolutionary history of osmoregulation, incorporating the concept of phylophysiology, revealed the existence of mechanisms at the molecular, cellular and systemic levels that have evolved accompanying the cladogenetic events of the Palaemonidae during their radiation and occupation of different osmotic niches.

Dégradés par plusieurs siècles d’endiguement et menacés par les effets du changement climatique, les marais intertidaux européens font aujourd’hui l’objet d’un nombre croissant de restaurations par rétablissement des marées sur d’anciennes zones endiguées, suivant une tendance générale appelée dépoldérisation. Cette thèse décrit la trajectoire de restauration des marais intertidaux à partir des communautés de necton (i.e., poissons et crustacés décapodes), sur la base de deux sites dépoldérisés accidentellement dans l’estuaire de la Gironde : le marais de Mortagne et l’île Nouvelle. L’évolution du necton dans les marais dépoldérisés est caractérisée à travers une approche synchronique à l’échelle de la mosaïque des habitats estuariens. La composition du necton dans les marais dépoldérisés est en grande partie similaire à celles des milieux intertidaux naturels et se différencie nette-ment des marais endigués, où les espèces exotiques d’eau douce prospèrent. Les marais restaurés apparaissent particulièrement attractifs pour le mulet porc, Liza ramada. La distribution des traits fonctionnels au sein des communautés de poissons révèle un changement de structure fonctionnelle au cours de la dépoldérisation, le temps de restauration étant inféré à partir d’un gradient de naturalité des habitats estuariens. En particulier, la spécialisation, la dispersion et la richesse fonctionnelle augmentent au cours de la restauration. Concernant l’évolution des règles d’assemblage, aucune tendance claire ne se dégage : les patrons diffèrent selon les traits fonctionnels.La dynamique temporelle de la composition des communautés de necton dans l’un des sites dépoldérisés montre une succession de trois phases au cours des quatre années suivant la restauration. Un changement plus abrupt concernant l’abondance de certaines espèces et la structure fonctionnelle des communautés est identifié au milieude la seconde phase, moins de deux ans après la dépoldérisation. La cinétique de transformation des communautés est probablement ralentie par le drainage incomplet du site dans les premiers temps de la dépoldérisation. Les résultats de cette thèse permettent de mieux comprendre la trajectoire de restauration des marais intertidaux, sans intervention humaine, tout en soulignant les atouts et les limites de certains modèles théoriques utilisés en écologie de la restauration. / European intertidal marshes have greatly declined during the past centuries because of land claim andhave recently been threatened by the effects of climate change. In recent years, an increasing number of tidal resto-ration projects have been implemented, following a global trend termed de-embankment. This thesis describes therestoration trajectory of tidally restored marshes from the response of nekton (i.e., fish and decapod crustaceans)based on two storm-breached study sites in the Gironde estuary : the Mortagne marsh and the Nouvelle island.Nekton assemblage composition of tidally restored marshes was described through a whole-estuary approach en-compassing natural, restored and dyked habitats. Nekton assemblages of tidally restored marshes showed highcompositional similarity with natural intertidal habitats and greatly departed from dyked marshes. Dyked marsheswere characterized by high occurrence of freshwater exotic taxa. Tidally restored marshes seemed particularly at-tractive for the thin-lipped grey mullet, Liza ramada. The functional traits’ distribution within fish communities revealeda change in functional structure in the course of restoration using the naturalness state of habitats as a proxy forrestoration time. Most notably, functional specialization, dispersion and richness increased with restoration time.No clear pattern of change was observed in community assembly over time ; trends chiefly varied with respect totraits. Temporal trends in one of the restored sites revealed three phases in the first four years of tide restoration.The abundance of several species and the community functional structure changed more steeply in the midst ofthe second phase, less than two years following tide restoration. Community turnover was probably delayed dueto incomplete drainage of the site in the early stages of restoration. The results of this thesis lead to a better un-derstanding of the restoration trajectory of tidal marshes without human intervention and highlight the strengths andweaknesses of some theoretical models used in restoration ecology.