Effects of the ocean temperature on organisms of the Galapagos Islands

Ocean temperature shapes marine life in ways both obvious and subtle — it affects metabolism, survival, and ultimately how many fish, invertebrates, and other organisms a stretch of ocean can support. Understanding that relationship is key to predicting how ecosystems respond as the ocean keeps warming.

The western Galapagos Archipelago comprises two islands: Isabela and Fernandina. Two distinct shallow water biological communities have been identified in these islands: the Elizabeth region in the Bolivar Channel and the western region elsewhere (Edgar et al, 2004). These distinct communities have different responses to temperature variability (Kuhn, 2010).

Early in my career, I studied how temperature shapes shallow-water marine life around Isabela and Fernandina, the westernmost Galápagos islands. This region is unusual: strong upwelling brings cold, nutrient-rich water to the surface, supporting cold-water species found nowhere else nearby, including penguins and flightless cormorants. I found that different parts of the region respond to temperature differently — communities in a deep channel were most sensitive to vertical temperature differences, while communities nearer the equatorial current responded more to seasonal swings.

Later, with colleagues, I looked at how temperature and fishing pressure together affected two economically important species, sea cucumber and spiny lobster. After accounting for fishing itself, we found warmer sea temperatures were followed, a year or two later, by higher catches of both — most visibly after the strong 1997–98 El Niño (Defeo et al., 2013).

Correlations between mean annual in situ sea surface temperature and lagged catch of spiny lobster and sea cucumber in the Galapagos Islands, Ecuador (Defeo et al., 2013). Catch series from 1995 to 2011 were linearly detrended and the residuals added to the mean, to account for the effect of fishing. Encircled triangles in B and D indicate the positive effect of 1997/1998 El Niño over spiny lobster (2000) and sea cucumber (2002–2003) catches. El Niño and La Niña events were defined based on the Oceanic Niño Index (ONI) estimated by the National Oceanic and Atmospheric Administration (NOAA). **: P < 0.05; ***: P < 0.001. Catch and SST time series were provided by Galápagos National Park and Charles Darwin Foundation. Content reproduced Creative Commons Attribution-NonCommercial 4.0 International License

Defeo, O., Castrejón, M., Ortega, L., Kuhn, A., Gutiérrez, N., & Castilla, J. C. (2013). Impacts of Climate Variability on Latin American Small-scale Fisheries. Ecology and Society, 18(4).
Edgar, G. J., Banks, S., Fariña, J. M., Calvopiña, M., & Martínez, C. (2004). Regional biogeography of shallow reef fish and macro‐invertebrate communities in the Galapagos archipelago. Journal of Biogeography, 31(7), 1107-1124.
Kuhn, A.M. (2010). Influencia de la temperatura del mar sobre comunidades rocosas submareales de la Reserva Marina de Galapagos. Tesis para la obtencion del titulo de Licenciatura en Oceanografia. Escuela Politecnica del Litoral. Guayaquil – Ecuador.