“…Alkane sources and distributions in McMurdo Dry Valleys were discussed in great detail by Matsumoto et al, (1990aMatsumoto et al, ( , 2010, where odd/even predominance was reported. Furthermore, Matsumoto et al (2010) provided stable isotope signatures (d 13 C) of alkanes, inferring the erosion of Beacon Supergroup sedimentary rocks and endolithic environments as major sources of these lipids in McMurdo Dry Valley paleosols. Alkane abundances in deeper horizons (828-Cox2, 10-20 cm; 828-Cox3, 20-30 cm) are even 4-fold higher, 62.3% and 51.4%, respectively, than in the surface horizons (828-Cox1, 0-10 cm; 829-Cox, 0-7 cm), where they account for 15.4% and 27.1% of total alkanes, respectively.…”