A first evaluation of the spatial gradients in δ18O recorded by European Holocene speleothems. / McDermott, F.; Atkinson, T.C.; Fairchild, I.J.; Baldini, L.M.; Mattey, D.P.

In: Global and Planetary Change, Vol. 79 , No. 3-4, 12.2011, p. 275–287.

Research output: Contribution to journalArticlepeer-review

  • F. McDermott
  • T.C. Atkinson
  • I.J. Fairchild
  • L.M. Baldini
  • D.P. Mattey


Oxygen isotope ratios in Holocene stalagmites decrease systematically in an easterly direction across Europe, reflecting zonal flow and progressive rainout. ► Speleothem δ18O longitudinal gradients decrease gradually during the course of the Holocene. ► Speleothems from Mediterranean-influenced cave sites exhibit higher δ18O values than those predicted by the regional longitudinal trends. ► δ18O in speleothems deposited in high elevation sites are lower than those predicted by the regional longitudinal trends. ► The first-order δ18O variability in European Holocene speleothems can be predicted from time-dependent linear regression models.

Original languageEnglish
Pages (from-to)275–287
JournalGlobal and Planetary Change
Issue number3-4
Early online date5 Feb 2011
Publication statusPublished - Dec 2011
This open access research output is licenced under a Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License.

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