However, Cockell reported that on Cornwallis Island and Devon Island, 94-95% of a random sample of 850 opaquedolomitic rocks were colonized by hypoliths, and found that the communities were dominated by cyanobacteria. The rocks chosen were visually indistinguishable from those nearby, and were about 10 cm across; the hypolithon was visible as a greenish coloured band. Cockell proposed that rock sorting by periglacial action, including that during freeze–thaw cycles, improves light penetration around the edges of rocks (see granular material and Brazil nut effect).
Cockell and Stokes went on to estimate the productivity of the Arctic communities by monitoring the uptake of sodium bicarbonate labelled with Carbon-14 and found that (for Devon Island) productivity of the hypolithon was comparable to that of plants, lichens, and bryophytes combined (0.8 ± 0.3 g m−2 y−1 and 1 ± 0.4 g m−2 y−1 respectively) and concluded that the polar hypolithon may double previous estimates of the productivity of that region of the rocky polar desert.[2]
^Charles S. Cockell; M. Dale Stokes (August 2006). "Hypolithic Colonization of Opaque Rocks in the Arctic and Antarctic Polar Desert". Arctic, Antarctic, and Alpine Research. 38 (3): 335–342. doi:10.1657/1523-0430(2006)38[335:HCOORI]2.0.CO;2. S2CID140167789.