“…For example, the chloroform flux through the environment is estimated at 660 ± 220 × 10 9 g yr −1 with 90 % of natural origin (McCulloch, 2003), and that of bromoform at ∼ 220 × 10 9 g yr −1 with 70 % from macroalgae (Carpenter and Liss, 2000). Abiotically, aliphatic volatile organohalogens were released from senescent and dead leaves (Hamilton et al, 2003), Fe-oxyhydroxide and halide containing soil or sediment (or with H 2 O 2 ; Fahimi et al, 2003;Huber et al, 2009), and emissions from savannah fires, volcanoes, hydrothermal sources, and salt mines (Weissflog et al, 2005;Gribble, 2010). Biotically, enzymes like haloperoxidases and halogenases widespread in soils and oceans are thought to contribute the major sources of environmental organohalogens (Nightingale et al, 1995;Hoekstra et al, 1998;Öberg, 2002;Reddy et al, 2002;Ortiz-Bermudez et al, 2007;Blasiak and Drennan, 2009;Wagner et al, 2009).…”