Ozone-Activated Halogenation of Mono- and Dimethylbipyrrole in

Dec 6, 2016 - The relative abundances of the halogenated isomers were calculated by peak area analysis using the Agilent software Integrator, ChemStat...
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Ozone-Activated Halogenation of Mono- and Dimethylbipyrrole in Seawater Abdhesh Kumar, Miles Borgen, Lihini I. Aluwihare, and William Fenical Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.6b03601 • Publication Date (Web): 06 Dec 2016 Downloaded from http://pubs.acs.org on December 7, 2016

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Environmental Science & Technology

Environmental Science and Technology

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Ozone-Activated Halogenation of Mono- and Dimethylbipyrrole in Seawater

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Abdhesh Kumar†,‡, Miles Borgen†§, Lihini I. Aluwihare†§, William Fenical†,‡

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Scripps Center for Oceans and Human Health, ‡Center for Marine Biotechnology and Biomedicine, §Geoscience Research Division, Scripps Institution of Oceanography, University of California at San Diego, La Jolla, California 92093, United States ABSTRACT: Polyhalogenated N-methylbipyrroles of two different structure classes have been detected worldwide in over 100 environmental samples including seawater, bird eggs, fish, dolphin blubber, and in the breast milk of humans that consume seafood. These molecules are concentrated in the fatty tissues in comparable abundance to some of the most important anthropogenic contaminants, such as the halogenated flame-retardants and pesticides. Although the origin of these compounds is still unknown, we present evidence that the production of these materials can involve the direct ozone activated seawater halogenation of N-methylbipyrrole precursors. This observation shows that environmental polyhalogenated bipyrroles can be produced via an abiotic process, and implies that the ozone activated halogenation of a variety of natural and anthropogenic seawater organics may be a significant process occurring in surface ocean waters.

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INTRODUCTION

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More than 5000 naturally-occurring organohalogen compounds are currently known.1,2 These

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compounds comprise a large number of structure types including halogenated terpenoids,

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alkaloids, polyketides, peptides, and others. Halogenation is a known biochemical process in

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some terrestrial organisms, but it is particularly pronounced in marine plants, animals and

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bacteria, by virtue of their access to the halogens in seawater as building blocks. However, very

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few, if any of the biosynthetically-produced organohalogens are found to accumulate in marine

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life, presumably due to their naturally-evolved biodegradation pathways. Among the molecules

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that are being accumulated in marine food webs world-wide are a large diversity of conspicuous

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polyhalogenated N-methylbipyrroles, containing randomly mixed bromine and chlorine

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substituents.3-16 These compounds have received focused attention because they have been found

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in over 100 environmental samples, including air samples,4 fish11 and sharks,13 dolphin12 and

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dugong blubber7 and, remarkably, human breast milk4 where they are among the most abundant,

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non-PCB and non-DDT contaminants that bio-accumulate in fatty tissues.

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absence in freshwater sources, except one report of their occurrence in Lake Baikal seals, has

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been taken as strong evidence of a marine origin.6

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Their general

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Polyhalogenated N-methylbipyrroles are of two types, polyhalo-1,1'-dimethyl-2,2'-bipyrroles

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(DMBPs) and polyhalo- 1'-methyl-1,2'-bipyrroles (MBPs), which are related structures in which

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two pyrrole rings are linked by either a carbon-carbon (C1-C1) bond or a carbon-nitrogen (C1-N)

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bond (Figure 1). Both classes of polyhalobipyrroles are found in Nature with bromine and

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chlorine in various ratios and at various substitution sites on the bipyrrole skeletons.

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Figure 1. Chemical compositions of the major polyhalogenated-N-methylbipyrroles observed

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world-wide that accumulate in marine fatty tissues and human breast milk.

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Subsequent to the first observation of these compounds, natural abundance radiocarbon

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measurements by Reddy and co-workers have provided significant support for a natural rather

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than anthropogenic origin of the carbon skeletons in the polyhalobipyrroles.19 Further, the

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presence of these contaminants has been observed in archived whale oil produced prior to the

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industrial era.20 Radiocarbon measurements, however, can only identify a biosynthetic origin of

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carbon, not how and when halogenation occurs. One unique feature of these two classes of

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bipyrroles is their random halogenation patterns ranging from 1 to 7 halogen isomers at various

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positions on the bipyrrole rings.14,17,18 Another significant feature is that these compounds are

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always N-methylated. To date, no industrial materials even closely related to these bipyrroles can

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be identified. The consistent presence of chlorine and bromine, and the completely random

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regiochemistry of halogen substitution, is inconsistent with known biosynthetic halogenation

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processes which largely target bromination. These processes involve a variety of brominating

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enzymes that function in a regio- and stereo-chemically specific manner.1,2 Bacteria of the

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common genus Pseudoalteromonas, for example, are known to brominate, but to not chlorinate

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pyrroles in natural biosynthetic processes.21-23 Numerous other halogenation products such as the

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halomethanes CH3I, CH3Br, CH2I2, CH2ICl are known to occur at ppb concentrations in seawater

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by photochemical halogenation of unknown dissolved organic matter.24-29 Other halogenation

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reactions, involve the production of halomethanes by seaweeds, albeit also at ppm and ppb

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levels.25 These observations of very low levels of photochemical halogenation reaction products

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do not explain the world-wide bioaccumulation of the polyhalo-N-methylbipyrroles. That these

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bipyrrole contaminants are produced in significant amounts, and bio-concentrated in such a vast

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diversity of marine life, suggests a prolific and potentially dynamic source in ocean systems.

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The exchange of gases across the air-sea interface provides a primary relationship between the

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chemistry of the ocean and atmosphere. Many gases (CO, CH4, N2O, H2, O3, methyl halides etc,)

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and numerous shorter-lived species (