angiopteris chauliodonta/chlorine

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The distinctive isotopic signature of plant-derived chloromethane: possible application in constraining the atmospheric chloromethane budget.

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Chloromethane (CH(3)Cl) is the most abundant halocarbon in the atmosphere. Although largely of natural origin it is responsible for around 17% of chlorine-catalysed ozone destruction. Sources identified to date include biomass burning, oceanic emissions, wood-rotting fungi, higher plants and most

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