“…Additionally, clone-library analyses have revealed a significant decrease in Acidobacteria representation with increasing latitude (Yergeau et al 2007b). Bacteroidetes, Firmicutes, Cyanobacteria, and Alphaproteobacteria were found to be more abundant relative to other taxa in soils of Fossil Bluff (71°19 0 S) and Coal Nunatak (72°03 0 ) on Alexander Island than at sites on the Falkland Islands, Signy Island, and Anchorage Island (51°76 0 S-67°34 0 S) (Yergeau et al 2009). Several phyla were significantly influenced by soil physicochemical factors, as the proportion of Chloroflexi and Betaproteobacteria were negatively (Yergeau et al 2007b); West Antarctic soil sequences (180) are from a study in the Ellsworth Mountains (Yergeau et al 2007b); Victoria Land soil sequences, a total of 426 clone sequences and 25976 pyrosequencing reads, were included from the McMurdo Dry Valleys, from studies in the Miers Valley Tiao et al 2012), Beacon Valley, Wright Valley, Battleship Promontory , Luther Vale (Niederberger et al 2008), and Bull Pass and Vanda in the Wright Valley ); ornithogenic soil sequences (514) are from Cape Hallett and Cape Bird in the Ross Sea region (Aislabie et al 2009); East Antarctic soil sequences (1396) were included from the Larsmann Hills (Bajerski and Wagner 2013) and Schirmacher Oasis (Shivaji et al 2004); and the Transantarctic Mountain soil sequences (361) were from the Darwin Mountains (Aislabie et al 2013).…”