“…In December of 1936, both C. fusca and C. polyspora appeared in great quantity, often attached to the same mass substrate, during a period of unseasonably warm weather (Kolk 1938). Although a possible correlation between the growth of these microorganisms in the artesian well and an increase of iron, calcium, magnesium, ammonia and nitrite levels in the water with a moderate decrease of pH values was suggested in our previous study (Vigliotta et al 2007), the link between the physical-chemical environmental parameters and the physiology of this microorganism remained elusive. In this study we associate the absolute requirement of high magnesium and calcium levels for growth of C. fusca to the absence, among its membrane lipids, of cardiolipin, a dimeric phospholipid derived from phosphatidylglycerol, generally abundant in Proteobacteria membranes (Cronan & Gelmann 1975, Dowhan 1997).…”