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

Abstract Based on the Baltic Earth Assessment Reports of this thematic issue in Earth
System Dynamics and recent peer-reviewed literature, current knowledge of the effects of …

The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …

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 The Coexistence Approach was established by Mosbrugger and Utescher (1997)
as a plant-based method to reconstruct palaeoclimate by considering recent climatic …

Multi-proxy studies are becoming increasingly common in palaeolimnology. Eight basic
requirements and challenges for a multi-proxy study are outlined in this essay–definition of …

The mid-Cretaceous period was one of the warmest intervals of the past 140 million years,,,–
, driven by atmospheric carbon dioxide levels of around 1,000 parts per million by volume. In …

The examination of more than 1500 paleohydrological dated records collected between 10
and 28° N during the last 50 years have been used to improve our knowledge and …