Eastern Mediterranean Sea circulation inferred from the conditions of S1 sapropel deposition
Holocene eastern Mediterranean Sea sediments contain an organic-rich sapropel S1 layer that was formed in oxygen-depleted waters. The spatial distribution of this layer revealed that during S1 deposition, deep waters were anoxic below a depth of 1800 m. However, whether this boundary permanently exi...
| Main Authors: | , , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2015-06-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/11/855/2015/cp-11-855-2015.pdf |