Linking oceanographic processes and marine resources in the western Caribbean Sea Large Marine Ecosystem Subarea

被引:23
|
作者
Carrillo, L. [1 ]
Lamkin, J. T. [2 ]
Johns, E. M. [3 ]
Vasquez-Yeomans, L. [1 ]
Sosa-Cordero, F. [1 ]
Malca, E. [2 ,4 ]
Smith, R. H. [3 ]
Gerard, T. [2 ]
机构
[1] El Colegio Frontera Sur, Dept Sistemat & Ecol Acuat, Av Centenario Km 5-5, Chetmal 77014, Quintana Roo, Mexico
[2] NOAA, Natl Marine Fisheries Serv, Southeast Fisheries Sci Ctr, 75 Virginia Beach Dr, Miami, FL 33149 USA
[3] NOAA, Atlantic Oceanog & Meteorol Lab, 4301 Rickenbacker Causeway, Miami, FL 33149 USA
[4] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Cooperat Inst Marine & Atmospher Studies, 4600 Rickenbacker Causeway, Miami, FL 33149 USA
关键词
Marine resources; Oceanographic processes; Mesoscale; Large marine ecosystem; Mesoamerican reef; Caribbean; BARRIER-REEF SYSTEM; POPULATION CONNECTIVITY; LARVAL DISPERSAL; VARIABILITY; MANAGEMENT; FISHERIES; MEXICO; MODEL; CONSERVATION; HYDROGRAPHY;
D O I
10.1016/j.envdev.2017.01.004
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The western Caribbean, a subarea of the Caribbean Sea Large Marine Ecosystem, includes the Mesoamerican Barrier Reef System, the Yucatan Basin, the Cayman Basin and the Yucatan Channel. Here we discuss the main oceanographic features of the western Caribbean Sea and present some examples of marine resources distributed throughout the western Caribbean Sea LME subarea along different spatial scales. Particular attention is given to their planktonic stages when physical oceanographic features (such as eddies and gyres, or current systems) can operate either as forces that promote larval dispersal or as barriers enhancing larval retention, as this determines their connectivity. Bluefin tuna, the early life stages (eggs and larvae) of reef fish, the Caribbean Spiny lobster, and the Queen conch are presented as examples. Dispersal distances depend on the oceanographic phenomena, with larger dispersals expected where intense currents occur, such as in the Yucatan Current. Conversely, retention can be expected in the presence of gyres such as the Honduras Gyre and Yucatan Basin eddies. There is a growing body of evidence supporting the need for a multi-scale approach in order to understand the complexity of LMEs. Moreover, the connectivity between regions in the western Caribbean Sea LME subarea, as shown by the exchange of marine resources and physical oceanographic processes, requires an international policy that supports collaborative efforts to monitor the dynamics of coastal and oceanic habitats together with marine resources.
引用
收藏
页码:84 / 96
页数:13
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