“…Since studies first demonstrated the presence of organic matter (OM) entrapped in calcite (Baker et al, 1996;Ramseyer et al, 1997), a number of organic components of speleothems being used as proxies for investigating changes in soils, vegetation, and climate (e.g., Baker et al, 1998;Blyth & Schouten 2013;Blyth et al 2011;Blyth et al, 2014;Bosle et al, 2014;Li et al, 2014;Perrette et al, 2005, Perrette et al, 2008Webb et al, 2014).…”