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Reply

Reply to Hrudey: Tracking the extent of oil sands airborne pollution

Joshua Kurek, Jane L. Kirk, Derek C. G. Muir, Xiaowa Wang, Marlene S. Evans, and John P. Smol
  1. aPaleoecological Environmental Assessment and Research Laboratory, Department of Biology, Queen’s University, Kingston, ON, Canada K7L 3N6;
  2. bEnvironment Canada, Aquatic Contaminants Research Division, Burlington, ON, Canada L7R 4A6; and
  3. cEnvironment Canada, Aquatic Contaminants Research Division, Saskatoon, SK, Canada S7N 3H5

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PNAS July 23, 2013 110 (30) E2749; https://doi.org/10.1073/pnas.1307696110
Joshua Kurek
aPaleoecological Environmental Assessment and Research Laboratory, Department of Biology, Queen’s University, Kingston, ON, Canada K7L 3N6;
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Jane L. Kirk
bEnvironment Canada, Aquatic Contaminants Research Division, Burlington, ON, Canada L7R 4A6; and
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Derek C. G. Muir
bEnvironment Canada, Aquatic Contaminants Research Division, Burlington, ON, Canada L7R 4A6; and
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Xiaowa Wang
bEnvironment Canada, Aquatic Contaminants Research Division, Burlington, ON, Canada L7R 4A6; and
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Marlene S. Evans
cEnvironment Canada, Aquatic Contaminants Research Division, Saskatoon, SK, Canada S7N 3H5
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John P. Smol
aPaleoecological Environmental Assessment and Research Laboratory, Department of Biology, Queen’s University, Kingston, ON, Canada K7L 3N6;
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  • For correspondence: smolj@queensu.ca
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We welcome Hrudey’s comments (1) regarding “the most noteworthy findings” of Kurek et al. (2) and have thus focused our response to discuss “several features” of the polycyclic aromatic hydrocarbon (PAH) data (and related dibenzothiophenes, DBTs) from Namur Lake.

First, historic forest fires cannot adequately explain the overall increasing trends of ΣPAHs, C1–C4 alkylated PAHs, and DBTs at Namur (Fig. 1 and figure 1A in ref. 2). Retene, a characteristic marker of conifer fires (3), is very low throughout the sediment record, and there is no significant correlation between the percentage of retene and ΣPAH flux (r2adj = 0.06, F = 2.3, P = 0.15). In addition, PAH ratios of retene to unsubstituted and C1–C4 alkylated PAHs have declined toward modern times at Namur (figure S3 in ref. 2), which is inconsistent with forest fires being a major contributor to the overall PAH trends. Second, all of our study sites located west of the bitumen upgraders and major open-pit mining areas show variable PAH trends. This finding can be attributed to their greater distance from the upgraders and to prevailing winds, which will deliver pollutants in pulses and may contribute to the observed variation. Additionally, the quality-control data for the sedimentary PAH analysis from Namur were very good and generally met laboratory performance standards in terms of blanks, recoveries of spiked unsubstituted and alkylated PAHs, and of deuterated internal standards. Thus, we are confident that the “oscillations” are reliable measurements. Third, apart from only two intervals, Namur ΣPAH flux values are comparable to four of our five near-field study lakes, except NE20 (figure S2 in ref. 2). The average sedimentation rate at Namur (0.027 g⋅cm−2⋅yr−1) and its temporal pattern are also similar to our near-field study lakes (except NE20), and other mid-latitude boreal forest lakes (4). It is possible that winter snowpack sampling from one season may underestimate the true spatial deposition pattern of PAHs, as priority pollutants were recorded as far as 85 km from the upgraders (5). These multiple lines of evidence suggest a detectable, although variable, PAH pollution signal at Namur. Finally, Hrudey notes (1) “the striking concordance” between sedimentary PAHs and inferred chlorophyll a (VRS-chla). Our study was not the first to recognize increased primary production driven by climatic warming; notable shifts in production are a hallmark of paleolimnological studies from the greater region (2). Unfortunately, we have only limited organic carbon data for Namur, although extensive data indicate that VRS-chla (available for near-field lakes) tracks primary production patterns well (6). We are also continuing to investigate historic PAH deposition patterns under the Joint Canada Alberta Oil Sands Monitoring Plan and will soon have additional data to address the issue of deposition in distant lakes.

Fig. 1.
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Fig. 1.

Flux of ΣPAH and DBT from the Namur Lake sediment record. (Inset) Retene as a percentage of total C1–C4 alkylated PAHs.

Although government funding of oil sands environmental monitoring before 1997 did provide some baseline data (e.g., condition and mercury levels in Athabasca River fish), it did not focus on temporal patterns in PAH deposition or the long-term ecological conditions in small lakes receiving emissions from nearby upgraders. Instead, the focus has been on variable river environments and downstream impacts. Reviews of previous monitoring programs have also largely been critical of their past monitoring approaches.

Footnotes

  • ↵1To whom correspondence should be addressed. E-mail: smolj{at}queensu.ca.
  • Author contributions: J.K., J.L.K., D.C.G.M., X.W., M.S.E., and J.P.S. wrote the paper.

  • The authors declare no conflict of interest.

References

  1. ↵
    1. Hrudey SE
    (2013) Valuable oil sands environmental research raises several questions. Proc Natl Acad Sci USA 110:E2748.
    OpenUrlFREE Full Text
  2. ↵
    1. Kurek J,
    2. et al.
    (2013) Legacy of a half century of Athabasca oil sands development recorded by lake ecosystems. Proc Natl Acad Sci USA 110(5):1761–1766.
    OpenUrlAbstract/FREE Full Text
  3. ↵
    1. Ramdahl T
    (1983) Retene—A molecular marker of wood combustion in ambient air. Nature 306:580–582.
    OpenUrlCrossRef
  4. ↵
    1. Muir DCG,
    2. et al.
    (2009) Spatial trends and historical deposition of mercury in eastern and northern Canada inferred from lake sediment cores. Environ Sci Technol 43(13):4802–4809.
    OpenUrlPubMed
  5. ↵
    1. Kelly EN,
    2. et al.
    (2010) Oil sands development contributes elements toxic at low concentrations to the Athabasca River and its tributaries. Proc Natl Acad Sci USA 107(37):16178–16183.
    OpenUrlAbstract/FREE Full Text
  6. ↵
    1. Michelutti N,
    2. et al.
    (2010) Do spectrally inferred determinations of chlorophyll a reflect trends in lake trophic status? J Paleolimnol 43:205–217.
    OpenUrlCrossRef
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Kurek et al. reply to Hrudey
Joshua Kurek, Jane L. Kirk, Derek C. G. Muir, Xiaowa Wang, Marlene S. Evans, John P. Smol
Proceedings of the National Academy of Sciences Jul 2013, 110 (30) E2749; DOI: 10.1073/pnas.1307696110

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Kurek et al. reply to Hrudey
Joshua Kurek, Jane L. Kirk, Derek C. G. Muir, Xiaowa Wang, Marlene S. Evans, John P. Smol
Proceedings of the National Academy of Sciences Jul 2013, 110 (30) E2749; DOI: 10.1073/pnas.1307696110
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