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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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factories”. This implies extensive cellular resource re-allocations which could lead to large changes and increases in greenhouse gas emissions from soils (including CO2, methane (CH4), and other greenhouse
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to propose novel system solutions that will lead to improved design and efficiency of the plant. We aim to achieve scientific advances that incorporates state of-the-art knowledge in several fields
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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