Multiproxy palaeohydrological records from three raised bogs in Northern Ireland indicate
that a major shift to wetter/cooler climatic conditions postdated the rapid decrease in solar …

This paper investigates evidence for palaeoclimatic changes during the period ca. 1500–
500 cal. yr BC through peat humification studies on seven Irish ombrotrophic bogs. The sites …

A proxy climate record from a raised bog in County Fermanagh, Northern Ireland, is
presented. The record spans the interval between 2850 cal. yr BC and cal. yr AD 1000 and …

Recent research has shown that ombrotrophic mires can yield a proxy climate signal based
on changes in the degree of peat humification [1, 2], and that oceanic margin sites show the …

The influence of solar variability on the climate of the Lateglacial and Holocene periods has
been the subject of increasing discussion during the last decade. In the Mid-Holocene …

Understanding the ecohydrological responses of peatlands to climate change is particularly
challenging over the late Holocene owing to the confounding influence of anthropogenic …

Two 14C accelerator mass spectrometry (AMS) wiggle‐match dated peat sequences from
Denmark and northern England record changes in mire surface wetness reconstructed …

Peatland palaeoclimate sequences produce bog surface wetness (BSW) reconstructions
which are commonly interpreted as changes in summer effective precipitation, ie the net …

Analyses of pollen, tephra, mineral input and degree of peat humification from three
neighbouring raised peat profiles at Corlea, central Ireland, covering the period of the …

Mid-Holocene tephra layers have been located and geochemically analysed from seven
ombrotrophic bogs in Scotland. The tephras found in these Scottish peats occur as …