Emissions of Fe(II) due to the undersea volcano of El Hierro

The Fe(II) is an essential micronutrient for the phytoplankton grow, and due to its low solubility in seawater it is found in the 0.2-2 nM range for the north Atlantic ocean. However the eruptive stage process and the subsequent hydrothermal stage occurred in the undersea volcano at the southeast of...

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Bibliographic Details
Main Authors: Santana González, Carolina, Santana Casiano, Juana Magdalena, González Dávila, Melchor
Other Authors: BU-BAS
Format: Conference Object
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/10553/114074
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author Santana González, Carolina
Santana Casiano, Juana Magdalena
González Dávila, Melchor
author2 BU-BAS
author_facet Santana González, Carolina
Santana Casiano, Juana Magdalena
González Dávila, Melchor
author_sort Santana González, Carolina
collection Universidad de Las Palmas de Gran Canaria: Acceda
description The Fe(II) is an essential micronutrient for the phytoplankton grow, and due to its low solubility in seawater it is found in the 0.2-2 nM range for the north Atlantic ocean. However the eruptive stage process and the subsequent hydrothermal stage occurred in the undersea volcano at the southeast of the El Hierro Island, Spain has risen the concentration of TFe(II) in the waters nearest to the main cone. Two cruises were carried out on March and October 2013, inside the VULCANO project, in order to detect any variation in concentrations of TFe(II) due to emissions after the eruptive process. Flow injection chemiluminescence using luminol as reagent was used to determine the concentrations of TFe(II). The results confirm an important positive anomalies in TFe(II) which coincide with negative anomalies in pH located in a secondary cone, during October cruise. It is also observed maximum values in TFe(II) at the surface associated to chlorophyll a maximum and to the sea bottom, showing the important influence of surface runoff, organic complexation and particle re-suspension processes. Temporal study in the station located over the secondary cone with positively anomalies in pH was carried out during 4 days. It showed an important variability in both pH and TFe(II) concentrations that indicated the volcanic area was affected by intermittent events of hydrothermal fluids in vent that remains in the volcano cone one and a half year after the eruptive phase has ceased. The increased TFe(II) concentrations and the low associated pH values may be acting as an important fertilization event in the seawater around the volcano at the Island of El Hierro providing optimal conditions for the regeneration of the area. 207 207 1
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op_relation IV Congress of Marine Sciences
http://hdl.handle.net/10553/114074

op_source Book of Abstracts submitted to the IV Congress of Marine Sciences. Las Palmas de Gran Canaria, June 11th to 13th 2014, p. 207
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spelling ftunivlaspalmas:oai:accedacris.ulpgc.es:10553/114074 2025-04-20T14:41:55+00:00 Emissions of Fe(II) due to the undersea volcano of El Hierro Santana González, Carolina Santana Casiano, Juana Magdalena González Dávila, Melchor BU-BAS 2014 http://hdl.handle.net/10553/114074 eng eng IV Congress of Marine Sciences http://hdl.handle.net/10553/114074 Sí Book of Abstracts submitted to the IV Congress of Marine Sciences. Las Palmas de Gran Canaria, June 11th to 13th 2014, p. 207 2510 Oceanografía 251001 Oceanografía biológica 251002 Oceanografía química 250621 Vulcanología info:eu-repo/semantics/conferenceobject ConferenceObject 2014 ftunivlaspalmas 2025-03-21T05:46:07Z The Fe(II) is an essential micronutrient for the phytoplankton grow, and due to its low solubility in seawater it is found in the 0.2-2 nM range for the north Atlantic ocean. However the eruptive stage process and the subsequent hydrothermal stage occurred in the undersea volcano at the southeast of the El Hierro Island, Spain has risen the concentration of TFe(II) in the waters nearest to the main cone. Two cruises were carried out on March and October 2013, inside the VULCANO project, in order to detect any variation in concentrations of TFe(II) due to emissions after the eruptive process. Flow injection chemiluminescence using luminol as reagent was used to determine the concentrations of TFe(II). The results confirm an important positive anomalies in TFe(II) which coincide with negative anomalies in pH located in a secondary cone, during October cruise. It is also observed maximum values in TFe(II) at the surface associated to chlorophyll a maximum and to the sea bottom, showing the important influence of surface runoff, organic complexation and particle re-suspension processes. Temporal study in the station located over the secondary cone with positively anomalies in pH was carried out during 4 days. It showed an important variability in both pH and TFe(II) concentrations that indicated the volcanic area was affected by intermittent events of hydrothermal fluids in vent that remains in the volcano cone one and a half year after the eruptive phase has ceased. The increased TFe(II) concentrations and the low associated pH values may be acting as an important fertilization event in the seawater around the volcano at the Island of El Hierro providing optimal conditions for the regeneration of the area. 207 207 1 Conference Object North Atlantic Universidad de Las Palmas de Gran Canaria: Acceda
spellingShingle 2510 Oceanografía
251001 Oceanografía biológica
251002 Oceanografía química
250621 Vulcanología
Santana González, Carolina
Santana Casiano, Juana Magdalena
González Dávila, Melchor
Emissions of Fe(II) due to the undersea volcano of El Hierro
title Emissions of Fe(II) due to the undersea volcano of El Hierro
title_full Emissions of Fe(II) due to the undersea volcano of El Hierro
title_fullStr Emissions of Fe(II) due to the undersea volcano of El Hierro
title_full_unstemmed Emissions of Fe(II) due to the undersea volcano of El Hierro
title_short Emissions of Fe(II) due to the undersea volcano of El Hierro
title_sort emissions of fe(ii) due to the undersea volcano of el hierro
topic 2510 Oceanografía
251001 Oceanografía biológica
251002 Oceanografía química
250621 Vulcanología
topic_facet 2510 Oceanografía
251001 Oceanografía biológica
251002 Oceanografía química
250621 Vulcanología
url http://hdl.handle.net/10553/114074