Tyrosine, octopamine, tryptophan, serotonin, putrescine, spermidine, spermine, norepinephrine, epinephrine, and dopamine were measured by means of high performance liquid chromatography (HPLC) in gills (anterior and posterior) and haemolymph extracts of the freshwater Chinese mitten crab, Eriocheir sinensis. These results may be considered as basic data to be used as control physiological doses, to which to refer for injection or for in vitro perfusion experiments.No signi cant difference has been detected between anterior respiratory and posterior salttransporting gills.After 10 days acclimation to sea water, a signi cant increase of haemolymph norepinephrine and dopamine has been observed. Exposure to hydrostatic pressure (101 ATA for 5 hours) also results in an octopamine increase in the haemolymph. In addition, there is a tryptophan increase in both the anterior and the posterior gills. Results are discussed in terms of possible correlations of the concentrations of polyamines, indoleamines, and catecholamines with osmoregulation and behaviour.

The Gulf Stream and Deep Western Boundary Current (DWBC) shape the distribution of heat and carbon in the North Atlantic, with consequences for global climate. This thesis employs a combination of theory, observations and models to probe the dynamics of these two western boundary currents.First, to diagnose the dynamical balance of the Gulf Stream, a depth-averaged vorticity budget framework is developed. This framework is applied to observations and a state estimate in the subtropical North Atlantic. Budget terms indicate a primary balance of vorticity between wind stress forcing and dissipation, and that the Gulf Stream has a significant inertial component.The next chapter weighs in on an ongoing debate over how the deep ocean is filled with water from high latitude sources. Measurements of the DWBC at Line W, on the continental slope southeast of New England, reveal water mass changes that are consistent with changes in the Labrador Sea, one of the sources of deep water thousands of kilometers upstream. Coherent patterns of change are also found along the path of the DWBC. These changes are consistent with an advective-diffusive model, which is used to quantify transit time distributions between the Labrador Sea and Line W. Advection and stirring are both found to play leading order roles in the propagation of water mass anomalies in the DWBC.The final study brings the two currents together in a quasi-geostrophic process model, focusing on the interaction between the Gulf Stream's northern recirculation gyre and the continental slope along which the DWBC travels. We demonstrate that the continental slope restricts the extent of the recirculation gyre and alters its forcing mechanisms. The recirculation gyre can also merge with the DWBC at depth, and its adjustment is associated with eddy fluxes that stir the DWBC with the interior. This thesis provides a quantitative description of the structure of the overturning circulation in the western North Atlantic, which is an important step towards understanding its role in the climate system.

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