Geoformas, malacofauna y evolución costera durante el holoceno en Ensenada Ferrer (Santa cruz, Patagonia, Argentina)
En este trabajo se propone un esquema evolutivo desde el Holoceno medio hasta el Presente del área costera de Ensenada Ferrer, ubicada al noreste de la Provincia de Santa Cruz, Argentina. Se aplicó el método morfocronológico para la definición de secuencias deposicionales cordoniformes, distinguiénd...
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| Published in | Revista de la Asociación Geológica Argentina Vol. 71; no. 1; pp. 69 - 81 |
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| Main Authors | , , , , |
| Format | Journal Article |
| Language | Portuguese |
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| Abstract | En este trabajo se propone un esquema evolutivo desde el Holoceno medio hasta el Presente del área costera de Ensenada Ferrer, ubicada al noreste de la Provincia de Santa Cruz, Argentina. Se aplicó el método morfocronológico para la definición de secuencias deposicionales cordoniformes, distinguiéndose dos sistemas y tres grupos, división que está avalada además por el contenido malacológico y características paleoambientales. Estos sistemas están separados entre sí por una superficie de truncamiento y desnivel asociado de 1,5 a 3 m. A su vez, se separan de un sistema más antiguo (Pleistoceno tardío?) por otra superficie de truncamiento con un desnivel asociado de 4 a 6 m. Se propone que estas discontinuidades se habrían originado entre ca. 6.000 y 1.000 años A.P. En relación con los sistemas de cordones identificados, se esboza un esquema evolutivo en tres fases, pasando el sector de ser una bahía abierta hacia el mar circundante (Fase 1), a una bahía semiprotegida (Fase 2), para finalmente alcanzar un alto grado de protección evidenciado por la conformación de la actual planicie de marea parcialmente ascendida (Fase 3). |
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| AbstractList | En este trabajo se propone un esquema evolutivo desde el Holoceno medio hasta el Presente del área costera de Ensenada Ferrer, ubicada al noreste de la Provincia de Santa Cruz, Argentina. Se aplicó el método morfocronológico para la definición de secuencias deposicionales cordoniformes, distinguiéndose dos sistemas y tres grupos, división que está avalada además por el contenido malacológico y características paleoambientales. Estos sistemas están separados entre sí por una superficie de truncamiento y desnivel asociado de 1,5 a 3 m. A su vez, se separan de un sistema más antiguo (Pleistoceno tardío?) por otra superficie de truncamiento con un desnivel asociado de 4 a 6 m. Se propone que estas discontinuidades se habrían originado entre ca. 6.000 y 1.000 años A.P. En relación con los sistemas de cordones identificados, se esboza un esquema evolutivo en tres fases, pasando el sector de ser una bahía abierta hacia el mar circundante (Fase 1), a una bahía semiprotegida (Fase 2), para finalmente alcanzar un alto grado de protección evidenciado por la conformación de la actual planicie de marea parcialmente ascendida (Fase 3). |
| Author | Mormeneo, Liliana Medina, Rubén A Codignotto, Jorge O Aguirre, Marina L Richiano, Sebastián M |
| AuthorAffiliation | Consejo Nacional de Investigaciones Científicas y Técnicas Comisión de Investigaciones Científicas de la Provincia de Buenos Aires Universidad Nacional de La Plata Universidad de Buenos Aires Centro de Investigaciones Geológicas Servicio Geológico Minero Argentino |
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| Author_xml | – sequence: 1 givenname: Rubén A surname: Medina fullname: Medina, Rubén A organization: Universidad de Buenos Aires – sequence: 2 givenname: Marina L surname: Aguirre fullname: Aguirre, Marina L organization: Universidad Nacional de La Plata – sequence: 3 givenname: Jorge O surname: Codignotto fullname: Codignotto, Jorge O organization: Servicio Geológico Minero Argentino – sequence: 4 givenname: Sebastián M surname: Richiano fullname: Richiano, Sebastián M organization: Consejo Nacional de Investigaciones Científicas y Técnicas – sequence: 5 givenname: Liliana surname: Mormeneo fullname: Mormeneo, Liliana organization: Universidad Nacional de La Plata |
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| Issue | 1 |
| Keywords | Nivel del mar Holoceno Palaeoenvironments Paleoambientes Santa Cruz Sea level Patagonia Holocene |
| Language | Portuguese |
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| Snippet | En este trabajo se propone un esquema evolutivo desde el Holoceno medio hasta el Presente del área costera de Ensenada Ferrer, ubicada al noreste de la... |
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| Title | Geoformas, malacofauna y evolución costera durante el holoceno en Ensenada Ferrer (Santa cruz, Patagonia, Argentina) |
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