Mg, Sr and Sr isotope geochemistry of a Belgian Holocene speleothem: implications for paleoclimate reconstructions

In this study, variations in Mg/Ca, Sr/Ca and Sr-87/Sr-86 ratios in a Holoc ene Belgian speleothem (cave secondary carbonate deposit) are interpreted i n terms of changes in water residence time and changes in weathering proces ses, possibly induced by changes in West European climate. A stalagmite fro m the Pere Noel cave (Belgium) was dated with the TIMS U/Th method and was deposited between similar to 13 and similar to 2 ka BP. The 1000 Mg/Ca rati o varies between 4.9 and 26, and displays short-term changes but no signifi cant long-term trend. The 1000 Sr/Ca ratio varies between 0.09 and 0.31 and displays both short-term changes and a long-term decreasing trend from 12. 9 to 3.5 ka. In parallel, the Sr isotopic composition of the speleothem dec reases from 0.7090 at 12.9 ka to 0.7088 at 3.5 ka. The Sr isotope ratio is higher than expected from the overlying limestone (Sr-87/Sr-86 = 0.7081) wh ich implies an external source of radiogenic Sr, most probably from a silic ate phase. Short-term and long-term changes in Mg/Ca, Sr/Ca as well as long -term changes of Sr-87/Sr-86 ratios can be explained by changes in the diss olution and precipitation processes of the host limestone. These processes are controlled by changes in water residence times linked to changes in the water excess (precipitation minus evapo-transpiration). (C) 2000 Elsevier Science B.V. All rights reserved.