“…In the current global warming phase, alpine glaciers at global scale are experiencing a severe reduction but also an increase of supraglacial stony debris, due to freeze-thaw processes delivering large volumes of debris from the surrounding slopes to the glacier surface (Azzoni et al, 2018; Janke et al, 2015; Kirkbride, 1993; Kraaijenbrink et al, 2017; Tielidze et al, 2020). The role of glacier forelands and supraglacial debris as potential habitat and refugium for high altitude organisms, such as plants (Caccianiga et al, 2011; Fickert et al, 2022; Losapio et al, 2021; Tampucci et al, 2015) and arthropods (Gobbi, 2020a; Hågvar et al, 2020; Valle et al, 2020) is increasingly recognized. However, it is still not clear how many cryophilic species – being both cold-adapted and hygrophilous (Deharveng et al, 2008; Fjellberg, 2010; Jurekova et al, 2021) – can live in glacial habitats and how much they are directly related to the presence of ice (Stibal et al, 2020).…”