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Resumen del producto

Gilly, W., U., Markaida, P., Daniels, T., Frawley, C.J., Robinson, J., Gómez-Gutiérrez, D., Hyun, J., Soliman & P., Pandey (2022). Long-term hydrographic changes in the Gulf of California and Ecological Impacts: A Crack in the World’s Aquarium. Enrique Curchitser (Eds.), Progress in Oceanography. 206: 102857. DOI: 10.1016/j.pocean.2022.102857.

Long-term hydrographic changes in the Gulf of California and Ecological Impacts: A Crack in the World’s Aquarium

William Gilly 1, Unai Markaida 2, Patrick Daniels 3, Tim Frawley 4, Carlos J. Robinson 5, Jaime Gómez-Gutiérrez 6, Dylan Hyun 7, Jacob Soliman 7 y Punneta Pandey 8

1 Hopkins Marine Station of Stanford University, Pacific Grove, CA 93950, USA
2 El Colegio de la Frontera Sur, CONACyT, Campeche 24500, Mexico
3 University of California Santa Cruz, Santa Cruz, CA 95064, USA
4 Institute of Marine Science, University of California Santa Cruz, Santa Cruz, CA, USA
5 Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Mexico City, México
6 Instituto Politécnico Nacional, Centro Interdisciplinario de Ciencias Marinas
7 Stanford University, Stanford, CA 94305, USA
8 Terra Habitus, A.C., Garza García, Nuevo Leo ´n, Mexico

Although the Gulf of California is widely recognized as a region of high productivity and biodiversity, recent oceanographic and ecological changes have had asignificant impact on its overall health. We review the relevant history of the economically important fishery based on large Humboldt (jumbo flying) squid (Dosidicusgigas) (>50 cm mantle-length and 10 kg body weight) that existed in the Guaymas Basin from the 1990's until 2009, when a strong El Nin ~o was accompanied byprecocious spawning of squid at extremely small size (<30 cm mantle length and 0.1 kg). This short-lived phenotype is characteristic of the equatorial part of thespecies range and cannot be profitably fished. This phenomenon also occurred in conjunction with the strong 1997–1998 El Nin ~o. Although rapid recovery of squidsize and landings occurred after the 1997–1998 event, recovery after 2009–2010 El Nin ~o was still incomplete when another strong El Nin ~o occurred in 2015–2016.This last event has led to fixation of the small size-at-maturity phenotype in the Gulf of California — an effective poleward migration of the tropical phenotype. Wealso document years between El Nin ~o 2009–2010 and 2015–2016 as being characterized by significant subsurface warming, leading to decreased productivity andrestricted nighttime foraging opportunities for squid in the upper water column. These climatic trends have likely altered trophic webs throughout the Gulf ofCalifornia, impacting many other taxa, including small pelagic fishes that are ecologically vital and commercially harvested in large quantities, as well as a suite oflarger teleost fishes that are targeted by sport fishers. From these disparate data sources, collected and collated in coordination with regional resource users andenvironmental monitoring programs, an overall pattern emerges of long-term decline across multiple taxa. We also present evidence of a significant abatement ofsubsurface warming after 2015 and consider when – or if – the Gulf of California will return to a ‘normal’ state like that prior to 2010. Despite the potential forshifting to a cooler oceanic regime, the small phenotype for jumbo squid has persisted until present (2022), and the overall trajectory of ecological recovery isunclear. Integrated analyses of additional oceanographic and biological time-series, fisheries records, and other data will be necessary to identify critical processesand trajectories occurring in the Gulf of California.

Palabras clave: Jumbo squid; fishery; resilience; Gulf of California

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