News archive for Department of Earth Science
Headlines for a researcher at the Center after EGU presentation
When we look at the sky and think "Are we alone?", there is no need to look only for planets receiving sun light.
A new project for the Center for Deep Sea Research financed by the Norwegian Research Council.
A new study from researchers from the Center for Deep Sea Research tells about a 80 000 year long powernap on the seafloor.
Two PhD students from the Center for Deep Sea Research have written an article for Aftenposten on the search for the origins of life.
Kikki Kleiven follows Tore Furevik as the direcor of Bjernes Centre, and will lead 200 climate researchers the coming four years.
Alma Dzozlic Bradaric completed her master's degree at GEO in 2020. Now she has received the first prize: Earth Model Award Winner from Halliburton for her brilliantly executed master's project.
The effect of increased mantle temperature at wide volcanic margins is likely overestimated. Large volumes of magmatism at volcanic rifted margin can be explained by depth-dependent extension and very moderate excess mantle potential temperature.
Mighty floods have carved out deep canyons on Earth. New research suggests this may have required less power than previously thought. Collecting such data, however, may be demanding.
The UN Ocean Science Decade gets off to a flying start through the University of Bergen’s new interdisciplinary SEAS Fellowship Programme.
For the next 5 years, UiB will be training a new generation of marine research leaders and decision makers to ensure sustainable oceans.
Modeling and inversion of seismic data using multiple scattering, renormalization and homotopy methods.
Temperature in the Southern Ocean was more tightly linked to the extent of Antarctic glaciation during past greenhouse climates than previously thought.
The effects of magmatic intrusions on temperature history and diagenesis in sedimentary basins and petroleum systems.
The Jebsen Centre has a new PhD candidate starting today!
Near the end of the last ice age, the global sea level rose 12–14 meters in less than 350 years. Most of the meltwater has been thought to have come from North America and Antarctica. A new study shows that the ice over coastal Norway and the Barents Sea may have contributed almost as much.
Last month Andreas Beinlich had a publication in Nature Geoscience, and this month we are happy to announce that a new publication from Jebsen Centre researchers is out in Nature Geoscience: Today Jo Brendryen, Bjarte Hannisdal, and Kristian Agasøster Haaga published “Eurasian Ice Sheet collapse was a major source of Meltwater Pulse 1A 14,600 years ago”.
The world’s sea level was at one time ten meters higher than today. Researchers have now discovered where the water came from.
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