Abstract
Three uranium series dates from Warton Crag confirm a pre-last glacial maximum age for the draining of a phreatic cave fragment in the Morecambe Bay karst of northwest England. Preliminary δ18O and δ13C results appear to record millennial-scale climate variability.
Original language | English (US) |
---|---|
Pages (from-to) | 103-106 |
Number of pages | 4 |
Journal | Cave and Karst Science |
Volume | 43 |
Issue number | 3 |
State | Published - Dec 2016 |
Externally published | Yes |