CO<sub>2</sub> maximum in the oxygen minimum zone (OMZ)
Oxygen minimum zones (OMZs), known as suboxic layers which are mainly localized in the Eastern Boundary Upwelling Systems, have been expanding since the 20th "high CO<sub>2</sub>" century, probably due to global warming. OMZs are also known to significantly contribute to the oc...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2011-02-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/8/239/2011/bg-8-239-2011.pdf |