The Colombian state officially recognizes limits in the Caribbean Basin that enclose an area of approximately 589,302 \(km^2\), while the Pacific Basin covers an area of 332,129 \(km^2\). As of the present study, seven protected areas are recognized in the Caribbean Exclusive Economic Zone (EEZ) and six protected areas in the Pacific

**Figure 1.** Study area with the location of marine protected areas and main ports in the Colombian Exclusive Economic Zone (EEZ).

Figure 1. Study area with the location of marine protected areas and main ports in the Colombian Exclusive Economic Zone (EEZ).

The Colombian Caribbean is typically oligotrophic, except for some coastal regions such as Puerto Bolívar (La Guajira department) and Santa Marta (Magdalena department), where seasonal upwelling events increase coastal productivity, allowing for the presence of top predators such as cetaceans (Gordon 1967; Fajardo 1979; Andrade et al. 2003; Andrade and Barton 2005; Criales Hernández et al. 2006; Lonin et al. 2010; Paramo et al. 2011; Rueda-Roa and Muller-Karger 2013; Gutiérrez et al. 2015; Farías-Curtidor et al. 2017; Barragán-Barrera et al. 2019).). On the other hand, the Colombian Pacific is influenced by year-round coastal upwelling events, particularly during the months of February to April and November to December, as reported by Villegas (1997, 2003) and Díaz and Gusmao (2008). This leads to high productivity in coastal areas, particularly in the Gorgona Island National Natural Park (NNP) (Pineda 1995).

**Figure S1.** Contour lines of the bathymetry of the study area.

Figure S1. Contour lines of the bathymetry of the study area.

Both the Caribbean and Pacific areas in Colombia are influenced by tourism-related vessel activities. However, the main tourist attractions are different in each region. In the Caribbean, water tourism is focused mainly on cruise ships and diving activities, while in the Pacific, tourist vessel traffic is primarily for nature activities such as diving and whale-watching (Aguilera-Díaz et al. 2006; Sánchez and Jaramillo-Hurtado 2010; Brida et al. 2012; Trujillo and Ávila 2013 ). These differences are reflected in the tourist infrastructure, which is highly developed in the Colombian Caribbean with cities like Cartagena de Indias having a large hotel development (Aguilera-Díaz et al. 2006; Sánchez-Fernández et al. 2010; Brida et al. 2012). On the other hand, the Pacific region is more pristine and ecotourism and whale-watching activities are predominant, as the region is highly biodiverse and part of the breeding zone for stock G humpback whales (Flórez-González et al. 2007; Sánchez and Jaramillo-Hurtado 2010; Aguayo Lobo et al. 2011; Trujillo and Ávila 2013; Acevedo et al. 2017; Fagua and Ramsey 2019).

REFERENCES

Acevedo J, Aguayo-Lobo A, Allen J, et al (2017) Migratory preferences of humpback whales between feeding and breeding grounds in the eastern South Pacific. Marine Mammal Science 33:1035–1052. https://doi.org/10.1111/mms.12423
Aguayo Lobo A, Acevedo J, Cornejo S (2011) La ballena jorobada Conservación en el Parque Marino Francisco Coloane. Ocho Libros Editores., Santiago de Chile
Aguilera-Díaz MM, Bernal-Mattos C, Quintero-Puentes P (2006) Turismo y desarrollo en el Caribe colombiano. Documentos de Trabajo Sobre Economía Regional y Urbana; No 79
Andrade CA, Barton ED (2005) The Guajira upwelling system. Continental Shelf Research 25:1003–1022. https://doi.org/10.1016/j.csr.2004.12.012
Andrade CA, Barton ED, Mooers CNK (2003) Evidence for an eastward flow along the Central and South American Caribbean Coast. Journal of Geophysical Research: Oceans 108:
Barragán-Barrera DC, Luna-Acosta A, May-Collado LJ, et al (2019) Foraging habits and levels of mercury in a resident population of bottlenose dolphins (Tursiops truncatus) in Bocas del Toro Archipelago, Caribbean Sea, Panama. Marine pollution bulletin 145:343–356. https://doi.org/doi.org/10.1016/j.marpolbul.2019.04.076
Brida JG, Pulina M, Riaño E, Zapata-Aguirre S (2012) Cruise passengers’ experience embarking in a Caribbean home port. The case study of Cartagena de Indias. Ocean and Coastal Management 55:135–145. https://doi.org/10.1016/j.ocecoaman.2011.10.003
Criales Hernández MI, B. García C, Wolff M (2006) Flujos de biomasa y estructura de un ecosistema de surgencia tropical en La Guajira, Caribe colombiano. Revista de Biología Tropical 54: https://doi.org/10.15517/rbt.v54i4.3103
Díaz X, Gusmao LM de O (2008) Influencia de los eventos climáticos El Niño y La Niña en la comunidad de Chaetognatha de las aguas superficiales del océano pacífico Colombiano. Revista Brasileira de Engenharia de Pesca 3:30–50
Fagua JC, Ramsey RD (2019) Geospatial modeling of land cover change in the Chocó-Darien global ecoregion of South America; One of most biodiverse and rainy areas in the world. PloS one 14:e0211324
Fajardo GE (1979) Surgencia costera en las proximidades de la península colombiana de la Guajira. Boletín Científico CIOH 7–19. https://doi.org/10.26640/22159045.6
Farías-Curtidor N, Barragán-Barrera DC, Chávez-Carreño PA, et al (2017) Range extension for the common dolphin (Delphinus sp.) to the Colombian Caribbean, with taxonomic implications from genetic barcoding analysis. PLoS ONE 12:
Flórez-González L, Ávila IC, Capella JJ, et al (2007) Estrategia para la conservación de la Ballena Jorobada del Pacífico Sudeste. Lineamientos para un Plan de Acción Regional e Iniciativas Nacionales. Fundación Yubarta, Cali
Gordon AL (1967) Circulation of the Caribbean Sea. J Geophys Res 72:6207–6223
Gutiérrez GA, Correa MA, Hormazabal SE (2015) Análisis de la variabilidad espacio-temporal del sistema de surgencia de La Guajira en el dominio espacio-frecuencia, empleando el MTM-SVD (Multi Taper Method Singular Value Decomposition). Bol Cient CIOH 33:87–106
Lonin SA, Hernández JL, Palacios DM (2010) Atmospheric events disrupting coastal upwelling in the southwestern Caribbean. Journal of Geophysical Research: Oceans 115:
Paramo J, Correa M, Núñez S (2011) Evidencias de desacople físico-biológico en el sistema de surgencia en La Guajira, Caribe colombiano. Rev Biol Mar Oceanogr 46:421–430
Pineda AR (1995) Condiciones hidrológicas en la cuenca del Pacífico colombiano. Bol Cient CCCP 73–97
Rueda-Roa DT, Muller-Karger FE (2013) The southern Caribbean upwelling system: Sea surface temperature, wind forcing and chlorophyll concentration patterns. Deep Sea Research Part I: Oceanographic Research Papers 78:102–114
Sánchez CI, Jaramillo-Hurtado ME (2010) Policies for enhancing sustainability and competitiveness in tourism in Colombia. Worldwide Hospitality and Tourism Themes
Sánchez-Fernández D, Lobo JM, Hernández-Manrique OL (2010) Species distribution models that do not incorporate global data misrepresent potential distributions: a case study using Iberian diving beetles. Diversity and Distributions no–no. https://doi.org/10.1111/j.1472-4642.2010.00716.x
Trujillo F, Ávila IC (2013) “Uso no letal de cetáceos: el turismo de observación de delfines y ballenas como estrategia de conservación en Colombia,”. In: F. A. Trujillo DC A. Gärtner, Diazgranados MC (eds) Diagnóstico del estado de conocimiento y conservación de los mamíferos acuáticos en Colombia. Ministerio de Ambiente y Desarrollo Sostenible / Fundación Omacha / Conservación Internacional / WWF, Bogotá D. C. Colombia., pp 232–251
Villegas NL (1997) Estudio del movimiento vertical de las aguas en la región Este de la Cuenca del Pacífico colombiano. Bol Cient CCCP 6:71–80
Villegas NL (2003) Evolución mensual de las corrientes verticales y zonas de surgencia en la Cuenca del Pacífico colombiano CPC. Bol Cient CCCP 9:34–44