2015
DOI: 10.1016/j.csr.2015.09.014
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Pathways and Hydrography in the Mesoamerican Barrier Reef System Part 1: Circulation

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Cited by 53 publications
(49 citation statements)
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References 36 publications
(52 reference statements)
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“…The Gulf of Honduras also acts as a geographic barrier promoting a pattern of counterclockwise circular currents that keeps larvae near the coast and restricts migration to adjacent areas. Our results agree with the patterns of the currents of the Mesoamerican Reef System hydrography and with the flow pattern's cyclonic circulation known as the Honduras Gyre (Carrillo et al, ). Still, the finding of P. miles in Banco Chinchorro (Guzmán‐Méndez, Rivera‐Madrid, Díaz‐Jaimes, García‐Rivas, et al, ) evidence that the dispersion process of both species ( P. miles and P. volitans ) is constant and increasing.…”
Section: Discussionsupporting
confidence: 89%
“…The Gulf of Honduras also acts as a geographic barrier promoting a pattern of counterclockwise circular currents that keeps larvae near the coast and restricts migration to adjacent areas. Our results agree with the patterns of the currents of the Mesoamerican Reef System hydrography and with the flow pattern's cyclonic circulation known as the Honduras Gyre (Carrillo et al, ). Still, the finding of P. miles in Banco Chinchorro (Guzmán‐Méndez, Rivera‐Madrid, Díaz‐Jaimes, García‐Rivas, et al, ) evidence that the dispersion process of both species ( P. miles and P. volitans ) is constant and increasing.…”
Section: Discussionsupporting
confidence: 89%
“…This species has a similar life cycle as L. griseus, therefore the results of this project support the findings by these authors. The Yucatan current (average speed of 1.5 m/s), which later becomes the Loop Current (Athié et al, 2011), can export fish larvae from the Caribbean up to the Gulf of Mexico (Carrillo et al, 2015). Possibly these ocean dynamics favor the dispersion of L. griseus larvae.…”
Section: Discussionmentioning
confidence: 99%
“…According to Carrillo et al (2015), the general pattern of surface water currents along the Quintana Roo coast is from south to north, as is the Yucatán Current (Figure 6.68). Although reversals in longshore transport south of Cancú n occur in the nearshore reef between rock headlands, the Yucatán Current, coupled with wave refraction, produces a net northward current for all littoral areas along the northeast coast of Quintana Roo (Krutak and Gío-Argáez 1994).…”
Section: Caribbean Sea Marine Ecoregion: Cabo Catoche To Cancú Nmentioning
confidence: 99%