Early Holocene vigorous Black Sea outflow and the onset of sluggish Aegean deep-water convection
Abstract The Eastern Mediterranean Sea underwent profound hydrographic changes from the late glacial to the Early Holocene, culminating in deep-water stagnation and the deposition of the most recent organic-rich sediment layer (sapropel S1). While this event has traditionally been attributed to rive...
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| Principais autores: | , , , , , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Portfolio
2026-06-01
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| coleção: | Communications Earth & Environment |
| Acesso em linha: | https://doi.org/10.1038/s43247-026-03730-6 |
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