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production is limited by both iron and silicic acid in the Southern Ocean, which affect their potential to take up and export carbon to the deep ocean via complex coupling between biogeochemical cycles
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latitude continental margins are associated with complex geological and physical transformations (e.g. erosion, sedimentation, glacial isostatic adjustments, fracturing, pressure and temperature variations
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of cold adaptation at the atomic level. These groundbreaking results have however up to this point never been validated experimentally. In the current project we aim to bridge the gap between theory and
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