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  • Gulf of Mexico - an overview | ScienceDirect Topics
    The continental slope of the northern Gulf of Mexico margin (Texas–Louisiana slope) displays a bathymetrically complex morphology that terminates abruptly in the Sigsbee escarpment in the central Gulf, and is filled in by the head of the Mississippi fan to the east (Steffens et al , 2003) The hallmark of the central Gulf continental slope is the presence of numerous closed to partially
  • The Gulf of Mexico - ScienceDirect
    The Gulf of Mexico (GOM) is a marginal sea of the Atlantic Ocean bordered by five states of the United States on the northern and the eastern border, five Mexican states on its western and southern border, and Cuba to the southeast (Fig 18 1)
  • The economic significance of the Gulf of Mexico related to population . . .
    Mexico and Cuba are two other notable nations that utilize the fisheries resources of the Gulf of Mexico Mexico and Cuba landed 259,156 and 51,400 mt in 2001, respectively, from the Western Atlantic region [9] This region (FAO region 31) contains the Gulf of Mexico and the western, central Atlantic Ocean
  • Mangrove forests in a rapidly changing world: Global change impacts and . . .
    The Gulf of Mexico is a valuable region for advancing understanding of global change impacts to mangrove forests because, in addition to a rich legacy of ecological research, coastal wetlands in the region are abundant and span multiple ecologically-relevant abiotic gradients (López-Portillo and Ezcurra, 2002; Méndez-Alonzo et al , 2008; Day et al , 2013; Yáñez-Arancibia et al , 2014
  • Structure, age, and tectonic evolution of the Gulf of Mexico
    The Gulf of Mexico is an isolated oceanic basin whose nature, structure and age are not fully elucidated, mostly because seafloor spreading isochrons have not been identified in this basin so far We compiled and processed all publicly available marine magnetic data to produce a new magnetic anomaly map of the Gulf of Mexico
  • The Gulf of Mexico: towards an integration of coastal management with . . .
    The Gulf of Mexico is a shared resource at risk, with the following major problems: (a) freshwater use and shortage, (b) pollution, (c) habitat modification, (d) unsustainable exploitation of living resources, (e) global change (sea level rise, temperature increase and change in rainfall patterns), (f) public education, and (g) lack of
  • Ocean acidification in the Gulf of Mexico: Drivers, impacts, and . . .
    Ocean acidification (OA) has resulted in global-scale changes in ocean chemistry, which can disturb marine organisms and ecosystems Despite its extensively populated coastline, many marine-dependent communities, and valuable economies, the Gulf of Mexico (GOM) remains a relatively understudied region with respect to acidification
  • Gulf Stream - an overview | ScienceDirect Topics
    After entering the Gulf of Mexico, the western boundary current, now named the Loop Current, flows northward to the middle of the Gulf and turns east toward the Straits of Florida Loops, characterized by high sea surface temperature (SST), frequently pinch off, forming anticyclonic eddies that propagate westward, often ending their existence on the shelf of the eastern Texas coast ( Figure 9
  • Spatiotemporal dynamics of coastal dead zones in the Gulf of Mexico . . .
    The Gulf of Mexico, as illustrated in Fig 1, harbors the most extensive hypoxic zone in North America and ranks as the second largest human-caused coastal hypoxic zone globally In addition, it was selected as the study area due to the availability of abundant and temporally consistent dissolved oxygen (DO) observations, which are critical for robust model training and validation
  • Gulf of Mexico sediment sources and sediment transport trends from . . .
    The trends we see in the MS and ARM data for the Gulf of Mexico indicate coherent transport of detrital particles from near-shore to deep Gulf areas These surface sediment distributions appear to describe integrated and long-term high-stand transport pathways within the Gulf, both long-shore in association with nepheloid layers and into the deep Gulf as part of the current system within the Gulf





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