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17 páginas, 2 tablas, 16 figuras, Semi-enclosed bays in upwelling regions are exposed to forcing related to winds, currents and buoyancy over the shelf. The influence of this external forcing is moderated by factors such as connectivity to the open ocean, shelter by surrounding topography, dimensions of the bay, and freshwater outflows. Such bays, preferred locations for ports, mariculture, marine industry, recreational activities and coastal settlement, present a range of characteristics, understanding of which is necessary to their rational management. Observations in such a semi-enclosed bay, the Ria de Vigo in Spain, are used to characterize the influence of upwelling and downwelling pulses on its circulation. In this location, near the northern limit of the Iberian upwelling system, upwelling events dominate during a short summer season and downwelling events the rest of the year. The ria response to the external forcing is central to nutrient supply and resultant plankton productivity that supports its high level of cultured mussel production. Intensive field studies in September 2006 and June 2007 captured a downwelling event and an upwelling event, respectively. Data from eight current profiler moorings and boat-based MiniBat/ADCP surveys provided an unprecedented quasi-synoptic view of the distribution of water masses and circulation patterns in any ria. In the outer ria, circulation was dominated by the introduction of wind-driven alongshore flow from the external continental shelf through the ria entrances and its interaction with the topography. In the middle ria, circulation was primarily related to the upwelling/downwelling cycle, with a cool, salty and dense lower layer penetrating to the inner ria during upwelling over the shelf. A warmer, lower salinity and less dense surface layer of coastal waters flowed inward during downwelling. Without external forcing, the inner ria responded primarily to tides and buoyancy changes related to land runoff. Under both upwelling and downwelling conditions, the flushing of the ria involved shelf responses to wind pulses. Their persistence for a few days was sufficient to allow waters from the continental shelf to penetrate the innermost ria. Longer term observations supported by numerical modeling are required to confirm the generality of such flushing events in the ria and determine their typical frequency, while comparative studies should explore how these scenarios fit into the range of conditions experienced in other semi-enclosed bays, Field project supported by Xunta de Galicia under project PDIGIT05RMA40201PR. Writing up was supported under Interreg-Poctep project 0313_RAIA_CO_I_E

The identification of the natural ligand for growth hormone secretagogue receptor 1a (GHSR1a) added a new element to the complex machinery of the physiological regulators for both growth hormone (GH) secretion and food intake. Initially, the incorporation of this "novel system" contributes to clarify some aspects of the regulation of GH that previously were not fully understood. However, this system is not as simple as it was thought at first. Ghrelin and its receptor became recognized not only for stimulating GH release but also by the discovery that this system appeared to exert an important role on several aspects of energy homeostasis. In this way, GHSR1a becomes a potential therapeutic target for the treatment of wasting syndromes. One of the important features of GHSR1a is the basal activity in the absence of an agonist, resulting in a high degree of receptor internalization as well as of signaling activity. This constitutive activity seems to provide a tonic signal required for the development of normal height, probably through an effect on the GH axis. Additionally, GHSR1a might function as homo- or heteromeric complexes in living cells which introduce a key concept that could have significant implications in different aspects of receptor biogenesis and function. At molecular level, GHSR1a regulates the activation of the downstream mitogen-activated protein kinase, Akt, nitric oxide synthase, and AMPK cascades in different cellular systems. Added to this complexity, the idea that GHSR1a is not the single receptor for ghrelin has been progressively more recognized. In this sense, the available data are quite ambiguous and many fundamental questions need to be clarified. The purpose of this chapter is to summarize the most recent characteristics of GHSR1a as the features to define the action of ghrelin and its physiological implication.