Export of calcium carbonate corrosive waters from the East Siberian Sea
The Siberian shelf seas are areas of extensive biogeochemical transformation of organic matter, both of marine and terrestrial origin. This in combination with brine production from sea ice formation results in a cold bottom water of relative high salinity and partial pressure of carbon dioxide (<...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2017-04-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/14/1811/2017/bg-14-1811-2017.pdf |