Coral reefs in the Bay of Cartagena, Colombia, have been heavily disturbed by anthropogenic perturbations since the founding of Cartagena in 1533. A prominent perturbation was the construction of Canal del Dique, a channel built by the Spaniards to shorten the access to the Magdalena River, a major waterway used by Colombian authorities for colonization and later for commercial purposes. Canal del Dique turned the clear waters of Cartagena Bay into a seasonally fluctuating, highly turbid, and eutrophied body of water with high sedimentation, and most coral reefs within the Bay disappeared (Restrepo et al. 2006). Even reefs outside the Bay, like those of Rosario Islands, were negatively affected. Only a few reefs remained, though they were also severely affected by human activities, such as the dredging of one of the natural mouths of the bay for seaport access.
Fig. 1 Coral reef at Varadero: a, b massive corals (Orbicella spp.) reach sizes of >3 m in diameter and exhibit flattened growing forms, despite being at shallow depths (3–5 m). c Some areas the reef exhibit high species richness and coral cover (coral species shown include O. faveolata, Millepora alcicornis, Colpophyllia natans, Porites astreoides, Agaricia tenuifolia, and Montastraea cavernosa)
https://link.springer.com/article/10.1007/s00338-014-1246-y