In this study, we combine erosion and anthropogenic proxies (Ti, Pb) from calibrated
portable XRF with pollen and radiocarbon chronologies in peat from mires of the …

Abstract Microscopic tephra layers ('cryptotephras') represent important age-equivalent
stratigraphic markers utilised in many palaeoenvironmental reconstructions. When used in …

Pollen analysis and radiocarbon dating of a core from northern Iran enable reconstructing
the past three millennia of vegetation dynamics of the Caspian lowlands and Alborz foothills …

Coeval changes in the reconstructed bog surface wetness and the pollen record of a peat
sequence extracted from an ombrothropic bog (Calul de Piatră, 1630 m, Apuseni Mountains) …

To understand peatland carbon-cycling processes ultimately requires the ability to track
changes occurring on the molecular-level. In this study, we profile a peat core taken from the …

This study provides a multi‐year (2017–2022) Net Ecosystem Carbon Balance (NECB) of a
Pyrenean mountainous peatland through the integration of field data, satellite imagery, and …

There have been few detailed studies into the tephrostratigraphy of southern Britain. We
report the tephrostratigraphy of two sites, one in southern England (Rough Tor, Cornwall) …

Peatlands in Canaan Valley National Wildlife Refuge hold a pedomemory of Pleistocene
and Holocene climatic fluctuations in the central Appalachian Mountains of the eastern …

The response of peatland carbon accumulation to climate can be complex, with internal
feedbacks and processes that can dampen or amplify responses to external forcing …

The Little Ice Age (LIA) is a well-recognised palaeoclimatic phenomenon, although its
causes, duration and severity have been matters of debate and dispute. Data from a wide …