IMIS | Flanders Marine Institute
 

Flanders Marine Institute

Platform for marine research

IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Printer-friendly version

Significant discharge of CO2 from hydrothermalism associated with the submarine volcano of El Hierro Island
Santana-Casiano, J.M.; Fraile-Nuez, E.; Gonzalez-Davila, M.; Baker, E.T.; Resing, J.A.; Walker, S.L. (2016). Significant discharge of CO2 from hydrothermalism associated with the submarine volcano of El Hierro Island. NPG Scientific Reports 6(25686): 9 pp. http://hdl.handle.net/10.1038/srep25686
In: Scientific Reports (Nature Publishing Group). Nature Publishing Group: London. ISSN 2045-2322, more
Peer reviewed article  

Available in  Authors 

Keyword
    Marine

Authors  Top 
  • Santana-Casiano, J.M.
  • Fraile-Nuez, E.
  • Gonzalez-Davila, M.
  • Baker, E.T.
  • Resing, J.A.
  • Walker, S.L.

Abstract
    The residual hydrothermalism associated with submarine volcanoes, following an eruption event, plays an important role in the supply of CO2 to the ocean. The emitted CO2 increases the acidity of seawater. The submarine volcano of El Hierro, in its degasification stage, provided an excellent opportunity to study the effect of volcanic CO2 on the seawater carbonate system, the global carbon flux, and local ocean acidification. A detailed survey of the volcanic edifice was carried out using seven CTD-pH-ORP tow-yo studies, localizing the redox and acidic changes, which were used to obtain surface maps of anomalies. In order to investigate the temporal variability of the system, two CTD-pH-ORP yo-yo studies were conducted that included discrete sampling for carbonate system parameters. Meridional tow-yos were used to calculate the amount of volcanic CO2 added to the water column for each surveyed section. The inputs of CO2 along multiple sections combined with measurements of oceanic currents produced an estimated volcanic CO2 flux = 6.0 10(5) +/- 1.1 10(5) kg d(-1) which is similar to 0.1% of global volcanic CO2 flux. Finally, the CO2 emitted by El Hierro increases the acidity above the volcano by similar to 20%.

All data in IMIS is subject to the VLIZ privacy policy Top | Authors