TY - JOUR
AU1 - Mauquoy, Dmitri
AU2 - Barber, Keith
AB - Quantitative plant macrofossil and colorimetric humification analyses have been used to reconstruct proxy‐climate from two paired ombrotrophic bogs in northern England (Coom Rigg Moss and Felecia Moss). Detrended correspondence analysis was used to transform the raw floral data into indices of mire surface wetness. The chronology of each peat profile was determined by radiocarbon assay, supported by pollen correlations. Palaeoclimatic reconstructions have been made by linking documented historical changes in climate, and other proxy‐climate records, to those inferred from the sites investigated in the study region. Both sites contain a sensitive palaeoclimatic record, as ten periods of increased effective precipitation have been detected between ca. cal. ad 1770–1800, ad 1400–1470, ad 1110–1260, ad 920–1060, ad 550–670, ad 210–360, 30 bc to ad 80, 180–130 bc, 590–520 bc and 760–710 bc. Copyright © 1999 John Wiley & Sons, Ltd.
TI - A replicated 3000 yr proxy‐climate record from Coom Rigg Moss and Felecia Moss, the Border Mires, northern England
JF - Journal of Quaternary Science
DO - 10.1002/(SICI)1099-1417(199905)14:3<263::AID-JQS445>3.0.CO;2-W
DA - 1999-05-01
UR - https://www.deepdyve.com/lp/wiley/a-replicated-3000-yr-proxy-climate-record-from-coom-rigg-moss-and-loW8LPES3d
SP - 263
EP - 275
VL - 14
IS - 3
DP - DeepDyve