Somosaguas fossil site
The Somosaguas fossil site is located in the Community of Madrid, in the Somosaguas campus, within the municipality of Pozuelo de Alarcón. The fossils found belong to the fauna of the Aragonian continental stage, about 14 million years ago. The sediments where the remains are found were deposited in an alluvial fan sedimentary environment. The site itself is formed by two zones with fossil presence, separated by : Somosaguas Norte, which occupies an upper stratigraphic position, and Somosaguas Sur.
The site was discovered in 1989 by a geology student near the Faculty of Political Sciences of the Complutense University, when he observed bone fragments in the ground. The student reported the discovery to Professor Nieves López Martínez, who verified that the remains were fossils, and in turn reported it to the Department of Paleobiology of the Museo Nacional de Ciencias Naturales.
History
In 1989 a geology student at the Complutense University of Madrid, Francisco Hernández Arteaga, was waiting for his girlfriend next to the Faculty of Political Science at the Somosaguas campus when he discovered skeletal remains on the ground. He did not report the discovery until 1996. Once the discovery was reported, members of the Paleobiology Department of the National Museum of Natural Sciences carried out prospections in the area, the results of which were included in a report presented to the Ministry of Culture of the Community of Madrid, and the site was included in the paleontological chart. The first paleontological excavation took place in 1998, in which Professor Nieves López led a team of students from the Faculty of Geological Sciences of Madrid, with the financial support of the Rector's Office of the Complutense University, and with the collaboration of the National Museum of Natural Sciences.Since then, excavations have been carried out regularly by students and since 2000 a fortnightly work period has been established in April or May, in addition to open days, workshops and exhibitions.
Geology
The site is located on Miocene materials that were deposited by a system of alluvial fans, which were formed due to the erosion suffered by the granitic and metamorphic rocks of the Central System. These sediments outcrop from the south of the urban area of Madrid to the contact with the plutonic and metamorphic materials of the sierra.The sediments present in the deposit have a potency of 6 m and consist of arkoses with clayey matrix and rock fragments with intercalations of brown clays and micaceous sands, distinguishing three sections.
- Section 1 : it forms the wall of the series and is thick. It is formed by arkoses with a clayey matrix, and in this section of the Somosaguas Sur deposit there are a large number of micro and macrovertebrate fossils.
- Section 2 : alternating levels of micaceous sands and brown clays, with a maximum thickness of.
- Section 3 : At the top of the series, it has a thickness of more than, formed by arkoses with clayey matrix. The macrovertebrate fossils of Somosaguas Norte are found in this section.
Fossils
The Somosaguas Sur site has a great richness of micromammal fossils that have allowed us to assign it to the Middle Aragonian E biozone. The taxa identified belong to different groups: Gliridae, Sciuridae, Cricetidae, Insectivora, Lagomorpha and Reptilia. Among the macrovertebrates, remains of the mastodon Gomphotherium angustidens have been recovered; from the family Rhinocerotidae, the taxon Alicornops ''simorrense has been identified; from the family Equidae, remains of Anchitherium have been found; and among the ruminants, there are fossils of the genera Heteroprox, Micromeryx and Tethytragus. There is also a suid, Conohyus.The fossils present in Somosaguas Norte correspond mostly to macrovertebrates, although microvertebrates have also been found, such as the lagomorphs Lagopsis and Prolagus oeningensis and the cricetid Democricetodoninae. As for macrovertebrates, remains of the mastodon Gomphotherium angustidens have been documented; fossils of the carnivores Hemicyon, Amphicyon, Pseudaelurus and an undetermined mustelid; the equid Anchitherium; the rhinoceros Prosantorhinus douvillei; the ruminants Heteroprox, Tethytragus and Micromeryx and the suid Conohyus simorrensis''. Bird and chelonian remains have also been recovered.
Taphonomy, paleoclimatology and paleoecology
Based on the taphonomic study of the Somosaguas Norte site, the following observations have been made: there are a large number of splinters from two different types of bone: cancellous bone splinters and compact bone, and they seem to indicate that the bone remains have undergone intense weathering processes. The presence of some fragile remains and intact surfaces has also been documented, as well as the presence of very altered remains that form powdery masses. In addition, signs of abrasion and mineral replacement have been observed in the remains. It seems that the main processes that have occurred in the deposit from the taphonomic point of view are:- Presence of different thanatoceonosis with different degrees of preservation.
- Concentration of the remains.
- Compaction of the sediment during fossildiagenesis.
- Mineralization of the bones.
- Cementation, cavity filling, decalcification and decomposition of bones.
- Differential compaction causing fractures in certain remains.