Daniel Abel-Schaad

TL;DR: The combined pollen and speleothems proxy data indicate that this montane rainforest expansion during Heinrich Stadial 1 Event was triggered mainly by a less seasonal rainfall regime from the subtropics to the equatorial region.

TL;DR: A review of the available Holocene pollen records from the Spanish Central System (113 sites and 150 14 C dates) was presented in this paper, where Palynological data obtained from pollen analyses of peatbogs, lakes and archaeological sites, as well as radiocarbon dating, were used to infer the human impact on vegetation and landscape during the last 9 millennia.

TL;DR: In this paper, the authors examined landscape changes in a mountainous area in central Spain through the analysis of pollen at Pena Negra mire (Caceres), since its formation during the transition period between the third and second millennium cal bc.

TL;DR: In this article, the results show a strong relationship between altitude, temperature, rainfall, arboreal cover and variations in pollen taxa percentages, and the statistic discrimination of some of these forest communities has allowed them to propose three new associations.

TL;DR: In this paper, the patterns and processes of vegetation change and fire history in the Late Holocene (c. 2400 calendar year BP) palaeoecological sequence of Lanzahita, Sierra de Gredos in central Spain, and provides the first Iberian pollen sequence undertaken within a monospecific Pinus pinaster woodland.