The present interglacial, the Holocene, spans the period of the last 11,700 years. It has
sustained the growth and development of modern society. The millennial-scale decreasing …

Peat, especially from acidic mires (bogs), is a natural archive of past environmental change.
Reconstructions of past climate from bogs commenced in the 19th Century through …

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 …

The Holocene Thermal Maximum with peak temperatures prior to 7 ka BP is mostly
accentuated in the Northern Hemisphere, still visible in the Southern Hemisphere and …

The surface temperature changes for the last 4000years in northern inland Iberia (an area
particularly sensitive to climate change) are determined by a high resolution study of carbon …

Reconstruction of hydroclimate variability is an important part of understanding natural
climate change on decadal to millennial timescales. Peatland records reconstruct 'bog …

The impact of rapid climate change on contemporary human populations is of global
concern. To contextualize our understanding of human responses to rapid climate change it …

Seasonal sea-surface temperature variability for the Neoglacial (3300–2500BP) and Roman
Warm Period (RWP; 2500–1600BP), which correspond to the Bronze and Iron Ages …

In archaeology, the meta-analysis of scientific dating information plays an ever-increasing
role. A common thread among many recent studies contributing to this has been the …

Water‐table reconstructions from Holocene peatlands are increasingly being used as
indicators of terrestrial palaeoclimate in many regions of the world. However, the links …