“…Lipid biomarkers from aquatic sediments, which are used as paleoclimate and paleoenvironment proxies, mainly consist of alkanes, alkenes, alkanols, sterols, ketones, fatty acids, GDGTs and so forth. These biomarkers are derived from a wide variety of origins, including but not limit to (1) upland terrestrial plants (Street et al, 2013;Vogts et al, 2009), (2) emergent macrophytes (Cranwell, 1973(Cranwell, , 1974Cranwell et al, 1987;Eglinton and Hamilton, 1967;Street et al, 2013;Wiesenberg and Schwark, 2006), (3) floating and submerged macrophytes (Seki et al, 2009;Street et al, 2013), (4) algae (Cranwell et al, 1987;Guo et al, 2015), (5) fauna (Fulco, 1983;Volkman et al, 1980a), (6) bacteria (including archaea) (Horikawa et al, 2010;Vogts et al, 2009), and moss (Nott et al, 2000).…”