Unveiling the inherent physical-chemical dynamics: Direct measurements of hydrothermal fluid flow, heat, and nutrient outflow at the Tagoro submarine volcano (Canary Islands, Spain)

Tagoro is one of the few submarine volcanoes in the world that has been monitored since its early eruptive stage in 2011 to present day. After six multidisciplinary oceanographic cruises conducted between 2014 and 2023 to gather a comprehensive dataset of georeferenced video-imagery and in situ meas...

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Detalhes bibliográficos
Autores: Martín-Diaz, Juan Pablo, González-Vega, Alba, Barreyre, Thibaut, Cornide, B., Arrieta López de Uralde, Jesús M., Vázquez, Juan Tomás, Palomino, Desirée, Lozano Rodríguez, José Antonio, Escánez-Pérez, J., Presas-Navarro, Carmen, Fraile-Nuez, Eugenio
Formato: artículo
Fecha de publicación:2024
País:España
Recursos:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/352630
Acesso em linha:http://hdl.handle.net/10261/352630
Access Level:acceso abierto
Palavra-chave:Tagoro volcano
Hydrothermal vents
Hydrothermal fluxes
Heat flux
Nutrient fluxes
Descrição
Resumo:Tagoro is one of the few submarine volcanoes in the world that has been monitored since its early eruptive stage in 2011 to present day. After six multidisciplinary oceanographic cruises conducted between 2014 and 2023 to gather a comprehensive dataset of georeferenced video-imagery and in situ measurements of hydrothermal flow velocities and hydrothermal fluid samples, we provide a robust characterization of the ongoing hydrothermal fluid velocity, heat flux, and nutrient release, along with an accurate delimitation of the hydrothermal field area. Our results reveal that Tagoro hydrothermal system extends from the main hydrothermal crater up to the summit, covering an area of 7600 m2. This hydrothermal field comprises thousands of small individual vents, displaying diverse morphologies such as crevices and delicate chimney-like structures, irregularly scattered across the dominant diffuse venting surface. Hydrothermal fluid temperatures and velocities at the substratum level reveal a clustered spatial distribution, ranging from 21.0 to 33.3 ◦C and 1.6–26.8 cm min− 1, respectively.