El registro costero de los cambios del nivel del mar en el litoral mediterráneo español durante los periodos interglaciares de los últimos 450ka.

Zazo, Caridad ¹
Goy, José Luis ²
Bardají , Teresa ³
Dabrio, Cristino-José ⁴
Lario, Javier ⁵
Sánchez-Moral, Sergio ¹

1 Museo Nacional de Ciencias Naturales

Museo Nacional de Ciencias Naturales
Madrid, España

ROR https://ror.org/02v6zg374
2 Universidad de Salamanca

Universidad de Salamanca
Salamanca, España

ROR https://ror.org/02f40zc51
3 Universidad de Alcalá

Universidad de Alcalá
Alcalá de Henares, España

ROR https://ror.org/04pmn0e78
4 Universidad Complutense de Madrid

Universidad Complutense de Madrid
Madrid, España

ROR https://ror.org/02p0gd045
5 Universidad Nacional de Educación a Distancia

Universidad Nacional de Educación a Distancia
Madrid, España

ROR https://ror.org/02msb5n36

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Revista :

Estudios geológicos

ISSN : 0367-0449

Año de publicación : 2025

Volumen : 81

Número : 2

Tipo : Artículo

DOI: 10.3989/EGEOL.45715.1133 DIALNET GOOGLE SCHOLAR Acceso abierto editor

Otras publicaciones en : Estudios geológicos

Resumen

Se analiza el registro de los cambios del nivel del mar a lo largo de los interglaciares ocurridos en los últimos 450 ka, correspondientes a los MIS-5, MIS-7, MIS-9 y MIS-11. A partir del conocimiento obtenido a lo largo de los últimos 40 años, se comparan las secuencias estudiadas en el litoral mediterráneo peninsular e insular, con las curvas del nivel del mar establecidas, lo que permite calcular tasas de movimiento vertical para cada zona. La comparación de estas tasas con las obtenidas en otras zonas de la península ibérica indica que las mayores tasas de levantamiento se registran en el estrecho de Gibraltar disminuyendo tanto hacia el este como hacia el oeste, con un nuevo máximo en el Cabo de San Vicente. Esta tendencia al levantamiento está condicionada por la cercanía al límite entre la microplaca ibérica y la nubia. Las mayores tasas de levantamiento en la costa mediterránea se registran en secuencias afectadas localmente por fallas activas asociadas a la zona de desgarre de las béticas orientales y, en concreto, a sus aperturas terminales meridional y septentrional. Las tasas calculadas en las costas mediterráneas peninsulares para los MIS-5, 9 y 11 muestran un levantamiento moderado, con máximos que nunca sobrepasan los 0,1 mm/año. Los valores calculados para el MIS-7 por lo general muestran valores más altos (<0,2 mm/año) incongruentes con los calculados para cada secuencia. Las tasas calculadas para Mallorca (Campo de Tiro, Cala Blava) muestran un ligero levantamiento o estabilidad.

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