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Norwegian margin outer shelf cracking: a consequence of climate-induced gas hydrate dissociation?
A series of en echelon cracks run nearly parallel to the outer shelf edge of the mid-Norwegian margin. The features can be followed in a *60-km-long and *5-km-wide zone in which up to 10-m-deep cracks developed in the ...
The potential of sedimentary ancient DNA for reconstructingpast sea ice evolution
(Springer Nature, 2019-06-24)
Sea ice is a crucial component of the Arctic climate system, yet the tools to document the evolution of sea ice conditions onhistorical and geological time scales are few and have limitations. Such records are essential ...