Susana Rubio, Joaquín Panera and Alfredo Pérez González, scientists at the Centro Nacional de Investigación sobre la Evolución Humana (CENIEH), have published a study in the journal Quaternary International of the changes to vegetation and climate over the last 400,000 years in the region of Madrid, a Mediterranean area subject to an important continental influence which is key to understanding global climate change, and especially for the Mediterranean region itself, due to its vulnerability.
Manzanares Valley today [Credit: Joaquín Panera] |
Pines and other conifers have been the most characteristic elements of a landscape, together with a mesophile and/or Mediterranean forest, which has been varying with the temperature and humidity. During the second half of the Middle Pleistocene, mesophile (humid) forests predominated, while the end of that period was characterized by a cold moment marked by a retreat of the forest during which oaks and holm-oaks disappeared.
In the Upper Pleistocene, an expansion of the Mediterranean species associated to those of the coastal areas of the southern Iberian Peninsula took place. Finally, at the start of the Holocene, 10,000 years ago, the record shows a drop in the diversity of the vegetation, which might be due not so much to climatic as anthropic factors.
Up to now, there were no data from the central region of the Iberian Peninsula, which is typified by being a Mediterranean area subject to an important continental influence. The record it presents is exceptional as there are hardly any continental records in southern Europe which furnish paleoecological information over such a wide timescale.
Source: CENIEH [May 09, 2018]