Fossil pollen records are well-established indicators of past vegetation changes. The
prevalence of pollen across environmental settings including lakes, wetlands, and marine …

This synthesis paper summarizes published proxy climate evidence showing the spatial and
temporal pattern of climate change through the Holocene in Arctic Canada and Greenland …

The origin of the temperature divergence between Holocene proxy reconstructions and
model simulations remains controversial, but it possibly results from potential biases in 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 …

Subfossil pollen and plant macrofossil data derived from 14 C-dated sediment profiles can
provide quantitative information on glacial and interglacial climates. The data allow climate …

The importance of reconstructing past environments quantitatively in palaeoecology is
reviewed by showing that many ecological questions asked of palaeoecological data …

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

Current interest and debate on pollen-assemblage richness as a proxy for past plant
richness have prompted us to review recent developments in assessing whether modern …

Plants will experience considerable changes in climate within their geographic ranges over
the next several decades. They may respond by exhibiting niche flexibility and adapting to …

Aim Our aims were to provide new pollen data for establishing a sub‐continental surface
pollen database (East Asian Pollen Database, EAPD) and to study relationships between …