“…A few factors make reef‐building corals a particularly powerful archive of past climate variability: (1) annual density banding patterns (Knutson et al, 1972), relatively rapid growth (~0.3–2 cm/year, depending on the species), and fine‐scale milling techniques permit annual or even sub‐annual reconstructions of past climate (hereafter “high‐resolution”); (2) annual density banding patterns, combined with advances in radiometric dating techniques (see Section 3.6) permit chronological uncertainties on the order of only a few years or less for well‐dated chronologies; and (3) well‐preserved colonies of living (modern) and sub‐fossil (hereafter “fossil,” Figure 1) samples fill critical gaps in both the spatial and temporal coverage of climate information from the global tropics (Lough, 2010). Several reviews have discussed the rich history of coral paleoclimate studies, including an in‐depth discussion of the commonly utilized proxies for paleo‐temperature (δ 18 O, Sr/Ca) and coral growth (density, extension, and calcification) (Barnes & Lough, 1996; Corrège, 2006; Felis & Pätzold, 2003; Gagan et al, 2000; Grottoli & Eakin, 2007; Jones et al, 2009; Lough, 2004, 2008, 2010; Lough & Cantin, 2014; Lough & Cooper, 2011; Sadler et al, 2014; Williams, 2020), as well as novel geochemical proxies (Saha et al, 2016).…”