El registro fósil como una herramienta en cicloestratigrafía. Incidencia de los cambios paleoambientales a escala de Milankovitch sobre las paleo-comunidades
DOI:
https://doi.org/10.21701/bolgeomin.124.2.002Palabras clave:
ciclo, fósil, Milankovitch, paleontología, plantónicoResumen
Tradicionalmente, el análisis cicloestratigráfico a escala de los ciclos de Milankovitch se ha realizado a partir del estudio del registro estratigráfico/sedimentológico. Sin embargo, los datos paleontológicos (registro fósil) poseen un gran potencial para caracterizar ciclos orbitales de precesión, oblicuidad y excentricidad. Cambios climáticos orbitalmente inducidos determinan variaciones paleoambientales en los medios marino y terrestre a los que responden de manera variable las comunidades que los habitan; fundamentalmente alteraciones y, en menor medida, cambios evolutivos, incluyendo fenómenos de especiación y extinción. Son numerosos los trabajos que ponen de manifiesto variaciones a nivel de comunidad o de algunos taxones concretos en respuesta a cambios cíclicos orbitalmente inducidos sobre el medio marino. La mayor información procede del medio plantónico como lo revelan los estudios sobre paleo-comunidades cretácicas de foraminíferos, radiolarios y nanofósiles, frente al ambiente bentónico comparativamente menos conocido, cuya respuesta proviene del estudio de foraminíferos bentónicos y trazas fósiles. La caracterización de ciclos de Milankovitch en el medio terrestre es relativamente escasa y fundamentalmente se debe al estudio de asociaciones de polen del Plioceno-Mioceno. Cambios climáticos orbitalmente inducidos han sido ampliamente reconocidos en el medio terrestre a partir de variaciones en la distribución de la vegetación, pero también afectan a la comunidad animal, con una especial atención a la respuesta de las poblaciones de homínidos (migración, dispersión, colonización).
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