Articles | Volume 16, issue 1
Clim. Past, 16, 141–160, 2020
https://doi.org/10.5194/cp-16-141-2020
Clim. Past, 16, 141–160, 2020
https://doi.org/10.5194/cp-16-141-2020
Research article
16 Jan 2020
Research article | 16 Jan 2020

Reconstructing seasonality through stable-isotope and trace-element analyses of the Proserpine stalagmite, Han-sur-Lesse cave, Belgium: indications for climate-driven changes during the last 400 years

Stef Vansteenberge et al.

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Cited articles

Allan, M., Fagel, N., Van Rampelbergh, M., Baldini, J., Riotte, J., Cheng, H., Edwards, R. L., Gillikin, D., Quinif, Y. and Verheyden, S.: Lead concentrations and isotope ratios in speleothems as proxies for atmospheric metal pollution since the industrial revolution, Chem. Geol., 401, 140–150, 2015. 
Baker, A., Genty, D., Dreybrodt, W., Barnes, W. L., Mockler, N. J., and Grapes, J.: Testing theoretically predicted stalagmite growth rate with recent annually laminated samples: Implications for past stalagmite deposition, Geochim. Cosmochim. Ac., 62, 393–404, 1998. 
Baker, A., Smith, C. L., Jex, C., Fairchild, I. J., Genty, D., and Fuller, L.: Annually laminated speleothems: a review, Int. J. Speleology, 37, 4, 193–206, 2008. 
Baker, A., Wilson, R., Fairchild, I. J., Franke, J., Spötl, C., Mattey, D., Trouet, V., and Fuller, L.: High resolution δ18O and δ13C records from an annually laminated Scottish stalagmite and relationship with last millennium climate, Global Planet. Change, 79, 303–311, 2011. 
Baldini, J. U., McDermott, F., and Fairchild, I. J.: Structure of the 8200 year cold event revealed by a speleothem trace element record, Science, 296, 2203–2206, 2002. 
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Short summary
We measured the chemical composition (trace-element concentrations and stable-isotope ratios) of a Belgian speleothem that deposited annual layers. Our sub-annual resolution dataset allows us to investigate how the chemistry of this speleothem recorded changes in the environment and climate in northwestern Europe. We then use this information to reconstruct climate change during the 16th and 17th century on the seasonal scale and demonstrate that environmental change drives speleothem chemistry.