Variaciones de rango orbital en la dinámica de la Nutriclina/Termoclina en el Pacifíco Ecuatorial durante los últimos 500 Ka indicado por cocolitofóridos (Site 1240, Leg 202)
The ODP Site 1240 is located in the equatorial cold tongue in the Eastern Equatorial Pacific. The analysis of the calcareous nannofossil assemblages allow us to monitor fluctuations in the Nutricline/Thermocline over the last 500 Ka, using the relationship between the upper photic zone taxa (small p...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2005 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/8765 |
| Acceso en línea: | http://hdl.handle.net/10272/8765 |
| Access Level: | acceso abierto |
| Palabra clave: | Eastern Equatorial Pacific ENSO Coccolithophores Calcareous nannofossils Paleoproductivity Pleistocene |
| Sumario: | The ODP Site 1240 is located in the equatorial cold tongue in the Eastern Equatorial Pacific. The analysis of the calcareous nannofossil assemblages allow us to monitor fluctuations in the Nutricline/Thermocline over the last 500 Ka, using the relationship between the upper photic zone taxa (small placoliths) and the lower photic zone taxa (Florisphaera profunda), by means of the N ratio function. The variations in this N ratio pointed out two intervals with dominant higher relative abundances of small placoliths over Florisphaera profunda, and other interval with an abrupt increasing in the relative abundance of Florisphaera profunda over the small placoliths, controlled esentially by a precessional force, and during the last 177 Ka by a markedly excentricity component |
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