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Microbial carbon cycling in marine shallow-water hydrothermal systems

Subject Area Mineralogy, Petrology and Geochemistry
Term from 2011 to 2020
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 185573157
 
Final Report Year 2020

Final Report Abstract

Within these so far poorly explored ecosystems, we were able to gain pervasive knowledge especially on: (1) the imprint of environmental parameters on spatial microbial diversity, (2) the importance of dark carbon fixation within these light-exposed shallow water hydrothermal systems, (3) membrane adaptation mechanisms to extreme conditions, (4) the molecular composition of the dissolved organic carbon from the hydrothermal fluids and underlying transformation processes, and (5) first proof of arsenic being released as nanoparticles from shallow water hydrothermal systems. To date, 27 presentations, 8 peer-reviewed publications and one book chapter and six that are close to submission have resulted from this research. The group studied four shallow-water hydrothermal systems, gained insights into their unique geochemistry, and into the diversity, lipid adaptations and function of their microbial communities. We have developed methods to sample hydrothermal sediments and fluids and proved the applicability of stable isotope probing (SIP) for these systems. As a spin-off of this Emmy Noether project, a cruise proposal has just been granted that will investigate hydrothermal systems in the Aegean Sea off Milos in a transect from shallow to deep, in order to remove the arbitrary boundary between these two phenomena and to investigate marine hydrothermal systems as a continuum.

Publications

 
 

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