“…The sulfide cave ecosystems received attention with the studies of Sarbu et al (1996). The first studied cave containing a sulfide ecosystem was Movile Cave in Romania (Sarbu and Popa, 1992;Sarbu et al, 1996;Sarbu, 2000;Engel, 2012), followed by the Frasassi caves and Grotto Azzurra in Italy (Macalady et al, 2007;Peterson et al, 2013), Tito Bustillo and Maltravieso caves in Spain (Schabereiter-Gurtner, 2002;Arrozo et al, 1997), Fiume Coperto Cave in Italy (Latella et al, 1999), Melissotrypa Cave in Greece (Falniowski and Sarbu, 2015), El Hamma in Tunisia (Por, 1963), Ayalon Cave and the Tabgha Spring in Israel (Por, 1963;2011), Kugitangtou caves in Turkmenistan (Maltsev and Korshunov, 1998), Cueva de Villa Luz in Mexico (Hose et al, 2000;Engel, 2007), Bungonia and Nullarbor caves with Bunder Sinkhole in Australia (Holmes et al, 2001;Jaume et al, 2001), Lower Kane Cave in Wyoming, USA (Porter et al, 2002), Cesspool Cave in Virginia, USA (Engel et al, 2001), and the Mammoth and Parker Caves in North America (Hutchins et al, 2016).…”