“…While positive carbon isotope excursions have been described in Paleoproterozoic (Knoll et al, 1986;Baker and Fallick, 1989;Buick et al, 1998;Melezhik et al, 1999;Lindsay and Brassier, 2002) and Neoproterozoic (Iyer et al, 1995;Kaufman and Knoll, 1995;Magaritz et al, 1986;Santos et al, 2000) carbonate sequences worldwide, Mesoproterozoic carbonate sequences usually have d 13 C PDB values similar to Phanerozoic sequences (Veizer et al, 1980;Buick et al, 1995;Kha et al, 1999). In most instances, these carbon isotope variations have been attributed to global processes, such as glaciation events or other mechanisms that disturb the inorganic and organic carbon reservoirs.…”