Yucatán Channel many of these died. Some recolonisation has since taken place. The Campeche Bank is a biodiverse area and it and other parts of the Yucatán Channel are heavily fished by artisan fishermen who converge on the area from along the coast of Mexico. The area is threatened by over exploitation. Yucatán Channel The Yucatán Channel or Straits of Yucatán (Spanish: "Canal de Yucatán") is a strait between Mexico and Cuba. It connects the Yucatán Basin of the Caribbean Sea with the Gulf of Mexico. It is just over wide and nearly deep at its deepest point near the coast of
Gulf of Mexico basin center active contemporaneously in regards to geologic time. The transform boundary caused two approximately 22° counterclockwise rotations of the Yucatan Block away from the North American plate. One rotation happened prior to seafloor spreading, and the second rotation happened while the basin spread, creating the current geographical shape of the Gulf of Mexico and the current placement of the Yucatan Peninsula. The active rifting of the Late-Triassic to Mid-Jurassic, and the stratigraphy which depended strongly on that tectonic development, is followed by a relatively calm tectonic period in the Late-Jurassic. The Late-Jurassic Gulf of Mexico is characterized mostly by prolonged