Formation and evolution of the ocean floor
We combine models with data to study the geodynamic evolution of the ocean floor. For this purpose, we link findings from computer simulations with
Mid-ocean ridge dynamics
Fresh oceanic crust is generated at the axis of mid-ocean ridges and transported away with the oceanic lithosphere. Spreading velocities are highly variable and correlate
Research Submersible JAGO
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Technical Specifications | Logistics
Logistics
Transport: 1 x 20 ' standard sea
Modeling fluid-rock interactions within the oceanic lithosphere
The ageing and alteration of oceanic lithosphere is closely linked to fluid flow and the associated hydration and alteration reactions.
SONNE 225: ROV KIEL 6000 explores the Manihiki-Plateau
The SO 225 expedition with the German research vessel SONNE lead scientists to the 120 million-year-old Manihiki Plateau. The formation at the
Talks and Poster
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Talks
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Krause S, Liebetrau V, Joubert A, Jaramillo-Vogel D, Löscher CR, Böhm F, Grob S, Eisenhauer A, Treude T: Carbonate Matrix
Chrimp
CHatham RIse Methane Pockmarks
Mechanism of formation of pockmarks at the southern Chatham Rise and their influences on gashydrate stability, benthic habitat and climate
Duration:
Proxy Development and Application
Many environmental parameters (e.g. temperature, salinity, pH) influence the isotopic and elemental composition of shells formed by marine calcifiers. Consequently
Staff
Dr. Christophe Galerne
Forschungsbereich 2: Marine Biogeochemie FE Marine Geosysteme
Office: Room: 8E/103 Phone: +49 431 600-2105 Email: cgalerne(at)geomar.de
Address: GEOMAR |
Larval Ecology
Survival of fish eggs and larvae is crucial for the recruitment to fisheries and the bottleneck in production for aquaculture. The focus of the larval ecology group therefore is on
