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An irrigation experiment to compare soil, water and speleothem tetraether membrane lipid distributions

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Authors
Baker, A.
Jex, C.
Rutlidge, H.
Woltering, M.
Blyth, Alison
Andersen, M.
Cuthbert, M.
Marjo, C.
Markowska, M.
Rau, G.
Khan, S.
Date
2016
Type
Journal Article

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Baker, A. and Jex, C. and Rutlidge, H. and Woltering, M. and Blyth, A. and Andersen, M. and Cuthbert, M. et al. 2016. An irrigation experiment to compare soil, water and speleothem tetraether membrane lipid distributions. Organic Geochemistry. 94: pp. 12-20.
Source Title
Organic Geochemistry
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Department of Applied Geology
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Abstract

© 2016 Elsevier Ltd. Measurement of glycerol dialkyl glycerol tetraethers (GDGTs) preserved in speleothems offers a potential proxy for past temperature but, in general, their origin is unknown. To understand the source of speleothem GDGTs, we undertook an irrigation experiment to activate drip sites within a hydrogeochemically well characterised cave. The cave drip water was analysed for GDGTs, inorganic elements (major ions and trace elements), stable isotopes and dissolved organic matter concentration and character. Published speleothem GDGT records from the site have been observed to be dominated by isoprenoid GDGTs and interpreted as deriving from in situ microbial communities within the cave or vadose zone. The drip water in our irrigation experiment had a GDGT distribution distinct from that of soil and speleothem samples, providing direct evidence that the distinctive GDGT signature in speleothems is derived from a subsurface source. Analysis of GDGTs in this context allowed further elucidation of their source and transport in cave systems, enhancing our understanding of how they might be used as a temperature proxy.