The discovery of these very primitive marine vertebrates has helped scientists to reconstruct the palaeogeography of the Cordillera Bética mountain range. Their study shows that the mountain system in the south of the Iberian Peninsula was located alongside the Alps at that time.
In 2006, a group of Andalusian geologists found the oldest fossils in the Cordillera Bética, dating from the late Ordovician period between 446 and 444 million years ago, in the Maláguide Complex in Ardales (Malaga). This was also the first solid evidence of Ordovician rocks in the Bética range.
"The importance of this finding stems not only from the age of the fossils and the fact they make it possible to date the age of the materials they contain, but also from the valuable information they provide to help us reconstruct the tectonic history, the palaeogeography, and the geological history of the Cordillera Bética", Rosario Rodríguez-Cañero, lead author of the study and a researcher at the Department of Stratigraphy and Palaeontology of the University of Granada, tells SINC.
The study, which has been published in the latest issue of the journal Terra Nova, says that the fossils of conodonts, which are very rare and difficult to find, are "an essential tool" for unravelling the geological history of the Bética mountains and learning about the features of the environment in which they developed and the thermal history of the rocks in which they are found.
The researchers analysed the characteristics of the conodont remains they found, the presence of certain species, and the absence of others, and compared these with others of a similar age found in the macizo ibérico (essentially the western half of the Iberian Peninsula) and other ranges in the area.
The results of the study show that, during the late Ordovician period, the Maláguide Complex was not to be found with the rest of the Iberian Peninsula along the edge of the palaeo-continent of Gondwana, "but was rather at a much lower latitude much closer to the Alps, with its Ordovician conodont fauna showing much closer similarities to the fauna of this area", says Rodríguez-Cañero.
Tiny and essential fossils
The conodonts were small, eel-shaped animals without any vertebral column, which measured a few tenths of a millimetre in length, and inhabited the seas during the Palaeozoic era and became extinct at the end of the Triassic (around 205 million years ago).
The fossilised remains usually found are not complete conodonts, but rather pieces of less than one millimetre in size, with a phosphate composition similar to that of vertebrate teeth. The conodonts had these in the cephalic region and used them to catch and grind up their food.
"These teeth were the only mineralised pieces of conodonts, meaning they are generally the only remains to have fossilised, although complete conodont fossils have been found in other parts of the world", the geologist explains.
The fossils found by the research team are not only the oldest in the Cordillera Bética, but are also the first remains of Ordovidician conodonts found in the entire western Mediterranean, from Gibraltar to the south of Italy.
Rodriguez-Canero, R.; Martín-Algarra, A.; Sarmiento, G.N.; Navas-Parejo, P. "First Late Ordovician conodont fauna in the Betic Cordillera (South Spain): a palaeobiogeographical contribution" Terra Nova 22(5): 330-340, octubre de 2010.
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