A new sediment core from Padul, Padul-15-05, provides a long and continuous sedimentary
and paleoenvironmental record of the last∼ 200 kyr. Here we present a detailed …

Pollen from deep-sea sedimentary sequences provides an integrated regional
reconstruction of vegetation and climate (temperature, precipitation, and seasonality) on the …

Sedimentation in most glacial lakes and wetlands in the Sierra Nevada (southern Iberian
Peninsula) began after the last deglaciation and since the Younger Dryas (YD)-Early …

Introduction and objectives Although the Iberian Peninsula is a key area for understanding
the Middle to Upper Paleolithic transition and the demise of the Neandertals, valuable …

Past vegetation and biodiversity dynamics, reconstructed using palaeoecological methods,
can contribute to assessing the magnitude of the current biodiversity crisis and anticipating …

A new record from a long sediment core (S3) in Navamuño (1505 m asl, western Iberian
Central System) provides the reconstruction of the vegetation history and environmental …

Climatic variability of Marine Isotope Stage (MIS) 11 is examined using a new high-
resolution direct land—sea comparison from the SW Iberian margin Site U1385. This study …

Overlying a palustrine deposit of unknown age (complex FP), and protected from weathering
and erosion inside a large cave/rock-shelter cavity, the sedimentary fill of Cueva Antón, a …

The study of modern vegetation–pollen relationships has long been recognized as crucial
for the proper interpretation of fossil pollen records. Despite the quickly growing number of …

The settlement of cold and arid environments by Pleistocene hunter-gatherers has been a
heated topic in Paleolithic Archaeology and the Quaternary Sciences for years. In the Iberian …