This paper examines the Late Quaternary (c. 20,300–< 505calyr BP) environmental history
of Siles, a lake situated at 1320m in the Segura mountains of southern Spain, with the goal …

In the long term (glacial/interglacial sequences), river development follows general climatic
evolution. However, at the scale of one cold-warm cycle, it appears that the …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

It is a widely held belief that a climax vegetation of closed forest systems covered the
lowlands of Central and Western Europe before humans intervened in prehistoric times to …

In pollen preparations other microfossils of various origin are often preserved. Among the
microfossils that attracted the attention of palynologists are a variety of organisms, eg, algae …

A palaeo-environmental reconstruction from the Roman Period settlement site Uitgeest-
Dorregeest (northwestern Netherlands) based on samples of old soil horizons derived from …

Remains of various ascomycetes, mainly ascospores, have been detected during
palynological studies of lake sediments, peat deposits and samples from archaeological …

Recent, high-resolution palaeoecological records are changing the traditional picture of post-
glacial vegetation succession in the Iberian Peninsula. In addition to the influence of …

ABSTRACT Quaternary (last 2.6 million years) botany involves studying plant megafossils
(eg tree stumps), macrofossils (eg seeds, leaves), and microfossils (eg pollen, spores) …

The Younger Dryas (YD) was a period of rapid climate cooling that occurred at the end of the
last glaciation. Here, we present the first palaeoglacier-derived reconstruction of YD …