Bedoukian   RussellIPM   RussellIPM   Piezoelectric Micro-Sprayer


Home
Animal Taxa
Plant Taxa
Semiochemicals
Floral Compounds
Semiochemical Detail
Semiochemicals & Taxa
Synthesis
Control
Invasive spp.
References

Abstract

Guide

Alphascents
Pherobio
InsectScience
E-Econex
Counterpart-Semiochemicals
Print
Email to a Friend
Kindly Donate for The Pherobase

« Previous AbstractCoinfection with Pseudomonas aeruginosa and Aspergillus fumigatus in cystic fibrosis    Next AbstractNatural formation of vinyl chloride in the terrestrial environment »

Nature


Title:Halocarbons produced by natural oxidation processes during degradation of organic matter
Author(s):Keppler F; Eiden R; Niedan V; Pracht J; Scholer HF;
Address:"Institute of Environmental Geochemistry, Heidelberg University, Germany. fkeppler@ix.urz.uni-heidelberg.de"
Journal Title:Nature
Year:2000
Volume:403
Issue:6767
Page Number:298 - 301
DOI: 10.1038/35002055
ISSN/ISBN:0028-0836 (Print) 0028-0836 (Linking)
Abstract:"Volatile halogenated organic compounds (VHOC) play an important role in atmospheric chemical processes-contributing, for example, to stratospheric ozone depletion. For anthropogenic VHOC whose sources are well known, the global atmospheric input can be estimated from industrial production data. Halogenated compounds of natural origin can also contribute significantly to the levels of VHOC in the atmosphere. The oceans have been implicated as one of the main natural sources, where organisms such as macroalgae and microalgae can release large quantities of VHOC to the atmosphere. Some terrestrial sources have also been identified, such as wood-rotting fungi, biomass burning and volcanic emissions. Here we report the identification of a different terrestrial source of naturally occurring VHOC. We find that, in soils and sediments, halide ions can be alkylated during the oxidation of organic matter by an electron acceptor such as Fe(III): sunlight or microbial mediation are not required for these reactions. When the available halide ion is chloride, the reaction products are CH3Cl, C2H5Cl, C3H7Cl and C4H9Cl. (The corresponding alkyl bromides or alkyl iodides are produced when bromide or iodide are present.) Such abiotic processes could make a significant contribution to the budget of the important atmospheric compounds CH3Cl, CH3Br and CH3I"
Keywords:"Atmosphere/*chemistry Ferric Compounds/chemistry *Geologic Sediments/analysis Hydrocarbons, Halogenated/*analysis/chemistry Organic Chemicals/analysis/chemistry Oxidation-Reduction *Soil/analysis;"
Notes:"MedlineKeppler, F Eiden, R Niedan, V Pracht, J Scholer, H F eng England 2000/02/05 Nature. 2000 Jan 20; 403(6767):298-301. doi: 10.1038/35002055"

 
Back to top
 
Citation: El-Sayed AM 2024. The Pherobase: Database of Pheromones and Semiochemicals. <http://www.pherobase.com>.
© 2003-2024 The Pherobase - Extensive Database of Pheromones and Semiochemicals. Ashraf M. El-Sayed.
Page created on 16-11-2024