Ozone-Activated Halogenation of Mono- and Dimethylbipyrrole in

Dec 6, 2016 - PDF. es6b03601_si_001.pdf (3.48 MB). Citing Articles; Related Content. Citation data is made available by participants in CrossRef's Cit...
3 downloads 11 Views 713KB Size
Subscriber access provided by GAZI UNIV

Article

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

Just Accepted “Just Accepted” manuscripts have been peer-reviewed and accepted for publication. They are posted online prior to technical editing, formatting for publication and author proofing. The American Chemical Society provides “Just Accepted” as a free service to the research community to expedite the dissemination of scientific material as soon as possible after acceptance. “Just Accepted” manuscripts appear in full in PDF format accompanied by an HTML abstract. “Just Accepted” manuscripts have been fully peer reviewed, but should not be considered the official version of record. They are accessible to all readers and citable by the Digital Object Identifier (DOI®). “Just Accepted” is an optional service offered to authors. Therefore, the “Just Accepted” Web site may not include all articles that will be published in the journal. After a manuscript is technically edited and formatted, it will be removed from the “Just Accepted” Web site and published as an ASAP article. Note that technical editing may introduce minor changes to the manuscript text and/or graphics which could affect content, and all legal disclaimers and ethical guidelines that apply to the journal pertain. ACS cannot be held responsible for errors or consequences arising from the use of information contained in these “Just Accepted” manuscripts.

Environmental Science & Technology is published by the American Chemical Society. 1155 Sixteenth Street N.W., Washington, DC 20036 Published by American Chemical Society. Copyright © American Chemical Society. However, no copyright claim is made to original U.S. Government works, or works produced by employees of any Commonwealth realm Crown government in the course of their duties.

Page 1 of 20

1

Environmental Science & Technology

Environmental Science and Technology

2 3

Ozone-Activated Halogenation of Mono- and Dimethylbipyrrole in Seawater

4 5

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

*

6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29



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.

30 31

INTRODUCTION

32

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

33

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

34

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

35

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

36

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

37

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

38

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

ACS Paragon Plus Environment

1

Environmental Science & Technology

Page 2 of 20

39

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

40

polyhalogenated N-methylbipyrroles, containing randomly mixed bromine and chlorine

41

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

42

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

43

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

44

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

45

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

46

been taken as strong evidence of a marine origin.6

17,18

Their general

47 48

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

49

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

50

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

51

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

52

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

53

54 55

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

56

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

57 58

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

59

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

60

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

61

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

62

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

63

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

64

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

65

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

ACS Paragon Plus Environment

2

Page 3 of 20

Environmental Science & Technology

66

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

67

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

68

regiochemistry of halogen substitution, is inconsistent with known biosynthetic halogenation

69

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

70

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

71

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

72

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

73

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

74

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

75

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

76

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

77

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

78

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

79

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

80 81

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

82

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

83

and numerous shorter-lived species (