Last Glacial Maximum deep water masses in southwestern Gulf of Mexico: Clues from benthic foraminifera
The repercussions of climate change during the Last Glacial Maximun (LGM) associated with changes in the structure and chemistry of abyssal waters in the southwestern Gulf of Mexico were studied by numerical analysis of benthic foraminiferal data from three sediment cores (water depth 1988-2735 m)....
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| Gepubliceerd in: | Boletín de la Sociedad Geológica Mexicana |
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| Hoofdauteurs: | , , , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Sociedad Geológica Mexicana, A.C.
2010
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| Onderwerpen: | |
| Online toegang: | https://www.redalyc.org/articulo.oa?id=94319371010 |
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