2002
DOI: 10.1080/14634980290031875
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Status of water quality at Holbox Island, Quintana Roo State, Mexico

Abstract: Holbox Island (with its coastal lagoon, Yalahau Lagoon) located in the littoral zone at the north-eastern tip of the Yucatan Peninsula, Gulf of Mexico, is a relatively undisturbed ecosystem that is currently under threat from unplanned and intensive urban development. Although other ecosystems in this littoral zone have been studied to determine the basic requirements for sustainable development, little information about Holbox Island exists. Thus far, no data concerning coastal pollution in Yalahau Lagoon hav… Show more

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Cited by 14 publications
(17 citation statements)
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“…1). In the Yalahau lagoon and its adjacent inshore sublittoral zone (<2 km from the shoreline; <2 m depth) euhaline conditions prevail (salinity between 35 and 40) throughout the year with little seasonal variation (Tran et al, 2002). Three main weather seasons are recognized in this region: (1) dry, with low rainfall and high air temperatures (March-May, 0-30 mm/month, 36-38°C);…”
Section: Methodsmentioning
confidence: 95%
“…1). In the Yalahau lagoon and its adjacent inshore sublittoral zone (<2 km from the shoreline; <2 m depth) euhaline conditions prevail (salinity between 35 and 40) throughout the year with little seasonal variation (Tran et al, 2002). Three main weather seasons are recognized in this region: (1) dry, with low rainfall and high air temperatures (March-May, 0-30 mm/month, 36-38°C);…”
Section: Methodsmentioning
confidence: 95%
“…Es la laguna costera más extensa en la región, con longitud de 30 km, anchura de 8 a 10 km y área de 275 km 2 . El intervalo de marea es micromareal (< 1 m), la profundidad promedio del agua es de 2 m (intervalo: 0.3 a 4 m) y no existe estratificación de la columna de agua (Tran et al, 2002a). Se encuentra rodeada por bosques de manglar, principalmente Rhizophora mangle Linnaeus y Avicennia germinans (Linnaeus) Linnaeus (García-Beltrán, 2006).…”
Section: Introductionunclassified
“…El intercambio de agua entre el mar y la laguna Yalahau ocurre principalmente a través de una boca natural de 5 km de anchura localizada al oeste. La salinidad tiende a incrementarse hacia el interior pasando de condiciones mixoeuhalinas en la boca de comunicación mar-laguna a condiciones hiperhalinas en la zona norte, que presenta una escasa comunicación con el resto de la Laguna, lo que ocasiona menor circulación y alta evaporación (Tran et al, 2002a(Tran et al, , 2002bAguilar-Salazar et al, 2003). En sitios cercanos a la boca de comunicación mar-laguna, el sedimento se compone principalmente de arena (> 80%), mientras que en la zona norte, el limo y la arcilla representan hasta un 50% (Tran et al, 2002b).…”
Section: Introductionunclassified
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