“…The sulfide spring populations from the Puyacatengo and Tacotalpa drainages show evidence for recent divergence between ecotypes, estimated at ~10,000 years ago in Tacotalpa and ~300 years ago in Puyacatengo (Brown et al, 2018). In contrast, sulfide spring populations in the Pichucalco and Ixtapangajoya drainages are hypothesized to have diverged earlier, with estimates from the Pichucalco drainage suggesting a timing of divergence of ~19,000 years ago (Greenway et al, 2021). Sulfide spring populations are locally adapted and exhibit convergent phenotypes related to morphology (Greenway et al, 2019; Riesch et al, 2016; Tobler & Hastings, 2011), life history traits (Riesch et al, 2010, 2014) and physiology (Greenway et al, 2020; Pfenninger et al, 2014; Plath et al, 2013; Tobler et al, 2011, 2016).…”