Mechanisms controlling the suboxic layer of the black sea
The Black Sea is a classic anoxic ocean basin resembling the earth's ancient oceanic conditions. Its present structure has evolved during the last 2.5 billion years, and is characterized by a well-defined sub-oxic zone at the interface between the oxic and sulfidic layers where many important b...
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| Langue: | English |
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Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción
2006
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| Accès en ligne: | http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382006000300012 |
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