On board of RV Meteor in the Eastern Tropical South Pacific Ocean
Congratulations to Jasmine Berg...
...on the successful defense of her doctoral dissertation on November 11th in Geosciences at the University of Bremen. Her doctoral dissertation was entitled:
The microbial impact on Fe & S cycling at oxic-anoxic interfaces: a single cell view
Research in the Biogeochemistry Group focuses on microbiological and geochemical processes that control bioactive element cycling in the marine environment. We employ geochemical, microbiological, modeling, molecular and single-cell techniques to study the environmental regulation of these processes, and their effects on the global biogeochemical cycles.
Our goal is to provide fundamental insights into microbial mediated processes in the Ocean that ultimately affect Ocean chemistry, biology and climate, and vital input for models used to predict potential future changes resulting from human activities.
25. April 2017
Our colleagues Clarissa Karthäuser, Laura Bristow and Gaute Lavik are sailing on board RV Meteor investigating microbial processes responsible for nitrogen loss and nutrient regeneration in oxygen-deficient waters. This cruise is supported by the Collaborative Research Centre 754: Climate - Biogeochemistry Interactions in the Tropical Ocean. You can find the weekly cruise reports HERE.
4. April 2017
Glacier bacteria’s contribution to carbon cycling
A new study published in the journal Nature Geoscience by Dr. Heidi Smith (Montana State University) and colleagues shows how microbial communities in melting glaciers contribute to the Earth’s carbon cycle, a finding that has global implications as the bulk of Earth’s glaciers shrink in response to a warming climate. See full MPI press release HERE.
29. March 2017
Phosphorus cycling in the dark ocean
A new study by Dr. Sarah Sokoll and colleagues is coming out in Geophysical Research Letters. This study describes experiments using radiolabeled phosphate that show the rapid uptake of phosphate into particles in sub-euphotic waters off the coasts of Mauritania and Namibia. The experiments and analyses demonstrate that this uptake is biologically mediated, and thus P cycling in the dark ocean is more intense than originally thought. In other words, P associated with sinking organic matter in the ocean is not simply degraded and released into the water column, but cycles several times through a microbial loop. Such intensified P cycling in sinking particles may have implications for the composition of phosphorus bearing organic matter reaching the seafloor, and for global ocean biogeochemical models.
This work was conducted as cooperation between the University Bremen (Marum) and the Max Planck Institute for Marine Microbiology (MPIMM) in Bremen.