Regional climate change from peat stratigraphy for the mid- to late Holocene in central Ireland

At the millennial scale bog surface wetness (BSW) records show a clear Holocene climate event stratigraphy, with major phases comparable with other regional climate proxies such as chironomid inferred temperature records. Moving towards the centennial scale, however, and towards the limits of chronological certainty within the records, regional differences are apparent which likely reflect the more heterogeneous precipitation patterns which occur on shorter timescales. The BSW data presented in this paper are reconstructed from testate amoebae assemblages from central Ireland and are compared with other regional records. The results suggest that this region is in phase with the North of Ireland in terms of timings and durations of climate change, but the comparisons are less clear with a stacked and tuned record from Northern Britain that shows an apparent offset compared to the Irish records. This may reflect variations in past regional precipitation or be a function of the tuning and stacking process. The broad phases of comparison between the Irish records, and the extension of the central Irish record back to 6000 cal BP, allow comparisons with low frequency temperature reconstructions from chironomids, which also show a broad level of correlation, with cooler temperatures relating to wetter BSW at centennial to millennial timescales.