“…For the past 20 years, sub-fossil chironomids preserved in lake sediments have started to be used in paleolimnology to quantitatively reconstruct various factors such as nutrients (Lotter et al, 1998), macrophytes (Langdon et al, 2010), salinity (Heinrichs et al, 1999), lake depth (Engels and Cwynar, 2011), anoxia (Quinlan et al, 1998) and temperature (Larocque-Tobler et al, 2011). As they are becoming accurate indicators (Brooks et al, 2012), their distribution is being studied in many parts of the world because new training sets are being developed for quantitative reconstruction.…”