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)|
|Number of pages||4|
|Journal||Cave and Karst Science|
|State||Published - Dec 2016|