On October 10th 2011 a shallow submarine volcanic eruption south of El Hierro (Canary Islands) gave rise to a drastic physical-chemical change in the water column. The initial eruptive phase affected a wide area south of the island, along with a plume that was observed to be transported north-westwards during November 2011. From March 2012 the volcanic activity shifted towards a degasification stage, during which the emissions affected a smaller area surrounding Tagoro submarine volcano and quite close to the seabed. Periodic multidisciplinary oceanographic cruises were carried out in order to monitor the impacts of these emissions. Discrete water samples were collected for analysis of inorganic macronutrients (NO2 - +NO3 -, PO4 3-, and SiO4 4-). Here, we present the spatial and temporal distribution of these nutrients from November 2011 to March 2014 with the data of 9 different cruises and more than 2450 samples in the area affected by the volcano. Our results highlight the significant nutrient emissions for both the eruptive / degasification stages, with maximum concentrations of 8.14 / 6.20, 0.78 / 0.29 and 21.63 / 18.56 μmol kg-1 of nitrite+nitrate, phosphate and silicate, respectively. Comparing the mean concentrations of the emissions with reference values, remarkably large percentages of nutrient enrichments have been obtained, quantified as 152% / 136%, 1118% / 377% and 2002% / 1534%, respectively. Furthermore, in the area affected by the volcano, N:P ratios of 4.28 for the eruptive and 12.36 for the degasification phase have been obtained, lower than the approximately 16:1 Redfield ratio that characterized the reference stations. Similarly, N:Si ratios found were 0.25 and 0.22 (reference: 3.40), and P:Si ratios were 0.02 and 0.01 (reference: 0.12), highlighting the large proportion in which silicate was emitted respect to the other nutrients. Finally, significant positive concentrations of chlorophyll-a respect to the reference were observed with data from several yo-yo and tow-yo studies, suggesting the possibility of a natural fertilization process that could have an important impact on the marine ecosystem surrounding Tagoro submarine volcano.

Máster en Oceanografía ; 2017-2018