“…Given the temperature and pH dependence of brGDGT indices in soils and peats, they are used as proxies for these parameters in loess-palaeosol, peat and sedimentary records (e.g. Weijers et al, 2007;Schouten et al, 2008;Rueda et al, 2009;Ballantyne et al, 2010;Bendle et al, 2010;Tyler et al, 2010;Fawcett et al, 2011;Peterse et al, 2011;Gao et al, 2012;Niemann et al, 2012;Zech et al, 2012;Ajioka et al, 2014b;Sanchi et al, 2014;Cao et al, 2017;Wang et al, 2017a). However, brGDGTs are also argued to be produced in situ within the water column or the sediments of aquatic settings (e.g.…”