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M.Sc. Christian Breuer

Name:

M.Sc. Christian Breuer

Abteilung:

Geochemie & Hydrogeologie

Funktionen:

PhD-student

Telefon:

0421 218 - 65106

Fax:

0421 218 - 65105

E-Mail:

E-Mail-Adresse

 

E-Mail: breuer"@"uni-bremen.de


University of Bremen
Department of Geosciences
Klagenfurter Straße
GEO Building - Room 3040
28334 Bremen
PO Box 330440
Germany

CV:

2010 - todayPh.D. student MARUM Bremen
2007 - 2010M.Sc. Geosciences, Westfälische Wilhelms-Universität Münster & IFM Geomar Kiel

M.Sc.-Thesis: The role of magmatic volatiles in the formation of sulfates and sulfides in the off-shore area of Panarea, Äolian Island-arc, Italy

Supervisor: Prof. Dr. Harald Strauss & Dr. Sven Petersen
2004 - 2007B.Sc. Geosciences, Westfälische Wilhelms- Universität Münster

B.Sc.-Thesis: Genese von Phosphatschichten in der Upwelling-Zone vor Peru

Supervisor: Prof. Klaus Mezger & Dr. Nikolaus Gussone

PhD-Project:

Abundance and speciation of As, Sb, and Se in hydrothermal fluids


Metalloids such as arsenic, antimony and selenium are ubiquitously present in the aquatic environment and occur as dissolved species in different oxidation states depending on the redox potential (Eh), pH, adsorption, light, temperature and biological activity. They are important due to their toxicity, and so significant to human and animal health. Concentrations in the environment can vary markedly because of the geology and human activity (e.g. mining, industrial activity).

Hydrothermal systems have come into the focus of interest in the last 30 years because of their unknown and uncertain role in the global ocean system. They form from seawater penetrating into the upper crust through cracks and fissures and creating a convection cell by heating up the seawater, with the heat resulting from magmatic activity. The chemistry of the host rock and of the heated fluids change due to water-rock interaction.

For my thesis, I study hydrothermal fluids from different settings and systems like the Menez Gwen hydrothermal system at the MAR but also back-arc basins systems like in the Manus Basin. I want to find out how much arsenic is carried by hydrothermal activity to the worldwide ocean systems and also additional if vent organisms can embed arsenic.

- under construction -

Expeditions:

29.08. - 20.09.2006M 69/2CARBMED / WESTMEDCartagena - Malta
07.01. - 16.02.2008SO 195TOTALFiji - Tonga - Fiji
01.04. - 12.05.2009M 78/2 MAR-SÜD VTrinidad & Tobago - Rio de Janeiro
13.01. - 25.01.2010 POS 393TOPO-MEDMalaga - Faro
09.04. - 30.04.2010RV Urania TYRRHENISBari - Messina
11.06. - 15.07.2011SO 216BAMBUSTownsville - Madang
05.02. - 22.02.2012M 86/4AUVINTYSDubrovnik - Palma de Mallorca

Research interests:

- marine geochemistry
- submarine hydrothermal systems
- transport of metalloids in hydrothermal systems
- hydrothermal fluid geochemistry with emphasis on metalloids as well as δ2H and δ18O
- unstable isotope geochemistry and geochronology

Teaching:

SS 2011:
Laborübungen aquatische Geochemie

Publications:

Arning, E.T., Lückge, A., Breuer, C., Gussone, N., Birgel, D., Peckmann, J., (2009) Genesis of phosphorite crusts off Peru. Marine Geology, 262, 68 - 81.

Talks:

Breuer, C., Ruiz-Chancho, M., Pichler, T.: On the fate of arsenic in the Menez Gwen hydrothermal system, MAR: AGU Fall Meeting 2011, San Francisco, CA.


     
    Impressum | © marum | Diese Seite wurde zuletzt aktualisiert von: M.Sc. Christian Breuer. Datum: 23.02.2012, 13:45 Uhr