0000000000384738
AUTHOR
Gary Tarbuck
Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum.
Description
Seasonal variability in silicate weathering signatures recorded by Li isotopes in cave drip-waters
Abstract Silicate weathering is a critical process in Earth’s carbon cycle, but the fundamental controls on weathering are poorly understood and its response to future climate change is uncertain. In particular, the potential for changes in seasonality or extreme weather events to control silicate weathering rates or mechanisms has been little studied. Here, we use lithium (Li) isotope measurements in bimonthly sampled drip-waters from two caves in the Yorkshire Dales (U.K.) to assess the response of silicate weathering processes to changes in temperature and hydrology over seasonal timescales. While the caves are contained in limestone bedrock, the drip-water Li isotope signal predominantl…