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Ten Years of Intense Physical-Chemical, Geological and Biological Monitoring Over the Tagoro Submarine Volcano Marine Ecosystem (Eruptive and Degassing Stages)

Authors :
Agencia Estatal de Investigación (España)
Fraile-Nuez, Eugenio
Santana-Casiano, Juana Magdalena
González-Dávila, Melchor
González-Vega, Alba
Vázquez, Juan Tomás
Sotomayor García, Ana
Ferrera, Isabel
Santana-González, Carolina
Eugenio, Francisco
Marcello, Javier
Hernández León, Santiago
Bakalis, Evangelos
Rueda, José Luis
Gómez-Ballesteros, María
Álvarez-Valero, Antonio M.
Sánchez-Guillamón, Olga
Palomino, Desirée
Tello-Antón, María Olvido
Presas-Navarro, Carmen
Escánez, José
González-Porto, Marcos
Fernández de Puelles, María Luz
Olivé Abelló, Anna
Vinha, Beatriz
Machín, Francisco
Martín-Diaz, Juan Pablo
Arrieta López de Uralde, Jesús M.
Agencia Estatal de Investigación (España)
Fraile-Nuez, Eugenio
Santana-Casiano, Juana Magdalena
González-Dávila, Melchor
González-Vega, Alba
Vázquez, Juan Tomás
Sotomayor García, Ana
Ferrera, Isabel
Santana-González, Carolina
Eugenio, Francisco
Marcello, Javier
Hernández León, Santiago
Bakalis, Evangelos
Rueda, José Luis
Gómez-Ballesteros, María
Álvarez-Valero, Antonio M.
Sánchez-Guillamón, Olga
Palomino, Desirée
Tello-Antón, María Olvido
Presas-Navarro, Carmen
Escánez, José
González-Porto, Marcos
Fernández de Puelles, María Luz
Olivé Abelló, Anna
Vinha, Beatriz
Machín, Francisco
Martín-Diaz, Juan Pablo
Arrieta López de Uralde, Jesús M.
Publication Year :
2023

Abstract

The shallow Tagoro submarine volcano monitoring represents a unique opportunity not only for improving our sparse understanding of submarine volcanic processes in specific scientific fields as physical and chemical oceanography or marine geology but also its interactions over the marine biology in one of the richest marine ecosystems in Europe. This chapter aims to summarize the most relevant physical–chemical, geological and biological changes that occurred in the marine ecosystem of El Hierro island, at the Marine Reserve Punta de La Restinga—El Mar de Las Calmas, due to the genesis of the new underwater volcano Tagoro (27º37′07″N–017º59′28″W) in October 2011. During the first six months of the eruption, extreme physical–chemical perturbations caused by this event, comprising thermal increase from up to + 18.8 °C, water acidification with a pH decrease of 2.9 units, deoxygenation to anoxic levels and extremely high metal enrichment among others, resulted in significant and dramatic alterations of the marine ecosystem. After March 2012, once the eruptive phase was finished, the new submarine volcano entered an active hydrothermal phase involving the release of heat with smaller but still significant and important thermal anomalies of up to + 2.55 °C around the craters, density decrease of − 1.43 kg m−3, pH decrease of − 1.25 units, and high concentrations of metals and inorganic nutrients similar to upwelling zones. These enrichments are still active up to date, producing clear signs of marine recovery not only in the benthonic strata but also in the whole water column compared with pre-eruptive data. Since its eruption ten years ago, an unprecedented monitoring effort has turned into the longest and most complete multidisciplinary time-series for the study of a shallow submarine volcano, with the realization of 31 oceanographic multidisciplinary expeditions that systematically measure more than 40 different physical–chemical and biological variables. All this info

Details

Database :
OAIster
Notes :
English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1416000282
Document Type :
Electronic Resource