“…In general, changes in the pigment composition and stratigraphy reflect variations in the phytoplankton structure and abundance (Leavitt and Hodgson, 2001), which in turn reflects changes in light availability, temperature, nutrients, lake stratification, food web and some other factors (Wetzel, 2001). Several studies across the world have demonstrated that sedimentary pigments can be used to infer past climate changes in Scandinavia and Central Europe (Lami et al, 2000), Antarctica (Hodgson et al, 2005;Chen et al, 2013), Mongolia (Nara et al, 2005), Chile (von Gunten et al, 2009a) and Nepal (Lami et al, 2010) or to document changes in the trophic levels of lakes in Florida (Waters et al, 2005), Chile (von Gunten et al, 2009b), Sweden (Reuss et al, 2010), Hungary (Korponai et al, 2011) and Estonia (Leeben et al, 2013) among others.…”