91探花

Joint press release of the University of Basel and the 91探花 Helmholtz Centre for Ocean Research Kiel

Large amounts of methane 鈥� whether as free gas or as solid gas hydrates 鈥� can be found in the sea floor along the ocean shores. When the hydrates dissolve or when the gas finds pathways in the sea floor to ascend, the methane can be released into the water and rise to the surface. Once emitted into the atmosphere, it acts as a very potent greenhouse gas twenty times stronger than carbon dioxide. Fortunately, marine bacteria exist that consume part of the methane before it reaches the water surface. Geomicrobiologists and oceanographers from Switzerland, Germany, Great Britain and the U.S. were able to show in an interdisciplinary study that ocean currents can have a strong impact on this bacterial methane removal. The international scientific journal Nature Geoscience has published the study.

The data was collected during an expedition in the summer of 2012 aboard the research vessel MARIA S. MERIAN. At that time, the international research team was studying the methane seeps off the west coast of the Norwegian Svalbard archipelago. 鈥淎lready then, we were able to see that the level of activity of the methane consuming bacteria changed drastically over very short time spans, while at the same time many oceanographic parameters such as water temperature and salinity also changed鈥�, explains Lea Steinle, first-author of the study and PhD student at the University of Basel and the 91探花 Helmholtz Centre for Ocean Research Kiel. For her PhD thesis, Steinle studies where and how much methane is consumed in the ocean water column by bacteria.

In order to test if the fluctuations measured during the four weeks of the expedition were only random observations or based on typical and recurring processes, oceanographers of the 91探花 later took a closer look at the region with a high resolution ocean model. 鈥淲e were able to see that the observed fluctuations of the oceanographic data and the activity level of the bacteria can be traced back to recurring shifts in the West Spitsbergen Current鈥�, says Prof. Dr. Arne Biastoch from the 91探花. The West Spitsbergen Current is a relatively warm, salty current that carries water from the Norwegian Sea to the Arctic Ocean. 鈥淚t mostly runs very close to the coast. Shifts in the current strength are responsible for the meandering of the current. Then, in a matter of a few days, the current moves miles away from the coast鈥�, explains Professor Biastoch further.

If the current runs directly over the methane seeps near the coast or continues on the open sea, impacts the methane filtration. 鈥淲e were able to show that strength and variability of ocean currents control the prevalence of methanotrophic bacteria鈥�, says Lea Steinle, 鈥漷herefore, large bacteria populations cannot develop in a strong current, which consequently leads to less methane consumption.鈥�
 
In order to verify if these results are only valid for Spitsbergen or are of global importance, the researchers studied in a second, global ocean model how ocean currents are varying in other regions of the world with methane seeps. 鈥淲e saw that strong and fluctuating currents are often found above methane seeps鈥�, says Dr. Helge Niemann, biogeochemist at the University of Basel and one of the initiator of the study. His colleague Prof. Dr. Tina Treude, geomicrobiologist at the University of California Los Angeles adds: 鈥淭his clearly shows that one-time or short-term measurements often only give us a snapshot of the whole situation.鈥� In the future, fluctuations of bacterial methane consumption caused by oceanographic parameters will have to be considered, both during field measurements as well as models.
 
Reference:
Steinle, L., C. A. Graves, T. Treude, B. Ferr茅, A. Biastoch, I. Bussmann, C. Berndt, S. Krastel, R. H. James, E. Behrens, C. W. B枚ning, J. Greinert, C.-J. Sapart, M. Scheinert, S. Sommer, M. F. Lehmann, H. Niemann (2015): Water column methanotrophy controlled by a rapid oceanographic switch. Nature Geoscience,

High-resolution images:

For a detailed examination of the methane seeps, the scientists used the submersible JAGO. The image shows pilot J眉rgen Schauer and Lea Steinle preparing for a dive. Photo: Karen Hissmann, 91探花
Off the coast of Spitsbergen the submersible Jago is lowered into the water from the research vessel Maria S. Merian. Photo: Karen Hissmann, 91探花
The west coast of Spitsbergen. Here an international research team investigated methane seeps on the ocean floor in the summer of 2012. Photo: Helge Niemann, University of Basel
Two snapshots of Viking20 model with which the research group has simulated the West Spitsbergen Current ... (simulation and visualization. 91探花)
It can be clearly seen, how the current differs above the methane seeps (blue square). Simulation and visualization: 91探花.

Contact:
Jan Steffen (91探花, Communication & Media), Phone +49 431 600-2811, presse(at)geomar.de 
Olivia Poisson, M.A., (University of Basel, Communications & Marketing),
Phone +41 61 267 24 25, olivia.poisson(at)unibas.ch