Ciclos de Milankovitch del Rhaetiense (Triásico Superior) en las formaciones Tethyan Dachstein Limstone y Laurentian Passaic Formation vinculadas por el metrónomo astronómico g2-g5
DOI:
https://doi.org/10.21701/bolgeomin.131.2.004Palabras clave:
ciclotemas Lofer, Alpes julianos, Cuenca Newark, cicloestratigrafía, TriásicoResumen
Se ha venido sospechando desde hace mucho que los ciclos de Milankovitch se han registrado en los ciclotemas Lofer correspondientes a un ambiente marino somero de la Rhaetian Dachstein Limestone de las zonas norte y sur de los European Northern and Southern Calcareous Alps. Sin embargo, la evidencia no ha sido todavía suficiente para demostrar de modo inequívoco el control de Milankovitch sobre los ciclotemas. Al mismo tiempo, hay una evidencia abrumadoramente fuerte de que los ciclos de Milankovitch influenciaron los paleoclimas de Rhaetian Laurentia y los depósitos húmedo-seco de playa-lake de la Passaic Formation (Newark Basin, USA). Los ciclos más claros en estos depósitos, los ciclos McLaughlin, se han asociado al metrónomo g2-g5, o ciclo orbital de excentricidad de 405 ka.
De este modo, los ciclos de Milankovitch estuvieron operando a lo largo del Rhaetiense, y siendo de naturaleza global, es muy factible que jugaran un papel en la génesis de los ciclotemas Lofer coetáneos. La Dachstein Limestone en los Julian Alps, relativamente no muy alterados por la tectónica, exhiben una fuerte ciclicidad de tipo Milankovitch, incluyendo evidencia de ciclicidad g2-g5. La formación marina somera Dachstein y la continental Passaic proporcionan evidencia para mecanismos complementarios de impulso y acuífero-limno-eustasia activa: el nivel del mar bajo en las facies emergidas Lofer es un reflejo de los depósitos Passaic húmedos de playa-lake, y nivel del mar alto en las facies subtidales Lofer en depósitos Passaic de playa-lake secos. Las formaciones Dachstein y Passaic están además asociadas por el metrónomo g2-g5; se propone una correlación provisional, sujeto a una validación futura con adicional, aunque todavía no desarrolladas restricciones cronoestratigráficas.
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