Penélope González-Sampériz

TL;DR: In addition to the influence of Lateglacial and Early Holocene climatic changes, other factors are critical in the course of vegetation development and observe strong regional differences as discussed by the authors.

TL;DR: Palynological, sedimentological and stable isotopic analyses of carbonates and organic matter performed on the El Portalet sequence (1802m a.s.l., 42°48′00ʺN, 0°23′52ʺW) reflect the paleoclimatic evolution and vegetation history in the central-western Spanish Pyrenees over the last 30,000 yr, and provide a high-resolution record for the late glacial period as mentioned in this paper.

TL;DR: In this article, the authors presented a comprehensive regional paleoclimate reconstruction for the Medieval Climate Anomaly (MCA: 900-1300 AD) in the Mediterranean IP using multi-proxy and accurately dated marine and terrestrial records covering the past 2000 years.

TL;DR: A palaeobotanical analysis of the Pleistocene floras and vegetation in the Iberian Peninsula shows the existence of patched landscapes with Pinus woodlands, deciduous and mixed forests, parklands (savannah-like), shrublands, steppes and grasslands as discussed by the authors.

TL;DR: In this paper, a palynological sequence was used to examine the Holocene (8390-160 cal yr BP) environmental history of the Sierra de Baza (Granada, southeastern Spain) with the goal of establishing the mechanisms exerting control over vegetation change.