Abstract
This study investigates the influence of organic matter (OM) on the historical variations of Hg in sediments from two closely-situated Canadian Arctic lakes, prior to the advent of Hg pollution inputs. Because of variable landscape evolution in the Mackenzie River Delta over the past 1–3 millennia, the lakes provide distinctly different histories of OM sources, types, and degree of aquatic productivity (i.e., depositional environments). They also differ significantly in their pre-1900 Hg concentration profiles. When labile, kerogen-like carbon (“S2”) from aquatic sources (diatoms and other unicellular algae) increased between 750 and 1900 A.D. in the more productive lake (Nesbitt), Hg concentrations also increased by ca. 50%. In contrast, S2 carbon concentrations in the nearby organic-poor lake (Big Lake) were several-times lower than in Nesbitt and decreased over the past millennium, while Hg concentrations showed no trend probably reflecting the stable input of clastic material from tundra soils. The contrast between lakes suggests that OM derived from unicellular algae is more effective at scavenging Hg than OM from terrestrial plants or aquatic macrophytes, possibly because of a higher content of labile, sulphur-rich compounds, high particle surface area and its dispersion throughout the water column. The results indicate that, in the absence of anthropogenic Hg inputs, increasing phytoplankton productivity and Hg scavenging alone can lead to significant increases in the Hg content of lake sediments. This finding is consistent with the hypothesis that increasing lake productivity because of climate warming during the twentieth century has confounded the interpretation of recently increasing Hg levels in northern lake sediments as being unequivocally due to anthropogenic Hg deposition. This study also suggests that sedimentary TOC by itself is a poor and sometimes misleading indicator of possible changes in the source and quality of OM in aquatic systems, which can have a major impact on Hg concentrations in sediments.
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References
AMAP (2005) AMAP Assessment 2002: heavy metals in the Arctic. Arctic Monitoring and Assessment Programme, Oslo
Antoniades D, Hamilton PB, Douglas MSV, Smol JP (2008) Diatoms of North America: the freshwater floras of Prince Patrick, Ellef Ringnes and northern Ellesmere Islands from the Canadian Arctic Archipelago. Iconogr Diatomol 14:1–649
Carrie J, Sanei H, Goodarzi F et al (2008) Characterization of organic matter in surface sediments of the Mackenzie River basin, Canada. Int J Coal Geol 77:416–423
Carrie J, Wang F, Sanei H et al (2009) Increasing contaminant burdens in an Arctic fish, burbot (Lota lota), in a warming climate. Environ Sci Technol. doi:10.1021/es902582y
Dallimore A, Schröder-Adams CJ, Dallimore SR (2000) Holocene environmental history of thermokarst lakes on Richards Island N.W.T.: thecamoebians as paleolimnoloical indicators. J Paleolimnol 23:261–283
Espitalié J, Laporte J-L, Madec M et al (1977) Méthode rapide de caractéristique des roches mères, de leur potentiel pétrolier et de leur degré d’évolution. Revue de l’Institut français du Pétrole 32:23–42
Faïn X, Ferraria CP, Dommergue A et al (2009) Polar firn air reveals large-scale impact of anthropogenic mercury emissions during the 1970s. Proc Natl Acad Sci USA. doi:10.1073/pnas.0905117106
Gasper JD, Aiken GR, Ryan JN (2007) A critical review of three methods used for the measurement of mercury (Hg2+)-dissolved organic matter constants. Appl Geochem 22:1583–1597
Jackson TA (1986) Methyl mercury levels in a polluted prairie river-lake system: seasonal and site-specific variations, and the dominant influence of trophic conditions. Can J Fish Aquat Sci 43:1873–1887
Kainz M, Lucotte M, Parrish CC (2003) Relationships between organic matter composition and methyl mercury content of offshore and carbon-rich littoral sediments in an oligotrophic lake. Can J Fish Aquat Sci 60:888–896
Lafargue E, Espitalité J, Marquis F et al (1998) Rock-Eval 6 applications in hydrocarbon exploration, production and soil contamination studies. Rev L’inst Franc Petr 53:421–437
Langford FF, Blanc-Valleron MM (1990) Interpreting Rock-Eval pyrolysis data using graphs of pyrolyzable hydrocarbons vs total organic carbon. Am Assoc Pet Geol Bull 74:799–804
Larter SR, Horsfield B (1993) Determination of structural components of kerogens by the use of analytical pyrolysis. In: Engel MH, Macko SA (eds) Organic geochemistry, chap 13. Plenum Press, New York, pp 271–287
Leitch DR, Carrie J, Lean D et al (2007) The delivery of mercury to the Beaufort Sea of the Arctic Ocean by the Mackenzie River. Sci Total Environ 373:178–195
Li C, Cornett J, Willie S et al (2009) Mercury in Arctic air: the long-term trend. Sci Total Environ 407:2756–2759
Lockhart WL, Wilkinson P, Billeck BN et al (1998) Fluxes of mercury to lake sediments in central and northern Canada inferred from dated sediment cores. Biogeochemistry 40:163–173
Michelutti N, Wolfe AP, Vinebrook RD et al (2005). Recent primary productivity increases in arctic lakes. Geophys Res Lett 32. doi:10.1029/2005GL023693
Muir DCG, Wang X, Yang F et al (2009) Spatial trends and historical deposition of mercury in eastern and northern Canada inferred from lake sediment cores. Environ Sci Technol 43:4802–4809
Outridge PM, Stern GA, Hamilton PB et al (2005) Trace metal profiles in the varved sediment of an Arctic lake. Geochim Cosmochim Acta 69:4881–4894
Outridge PM, Sanei H, Stern GA et al (2007) Evidence for control of mercury accumulation rates in Canadian High Arctic lake sediments by variations of aquatic primary productivity. Environ Sci Technol 41:5259–5265
Reimer PJ, Baillie MGL, Bard E et al (2002) IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 46:I029–I1058
Rydberg J, Klaminder J, Rosen P, Bindler R (2010) Climate driven release of carbon and mercury from permafrost mires increases mercury loading to sub-arctic lakes. Sci Total Environ 408:4778–4783
Sanei H, Goodarzi F (2006) Relationship between organic matter and mercury in recent lake sediments: the physical geochemical aspects. Appl Geochem 21:1900–1912
Sanei H, Goodarzi F, Snowdon LR et al (2000) Characterizing the recent sediments from Pigeon Lake Alberta as related to anthropogenic and natural fluxes. Environ Geosci (AAPG) 7:177–189
Sanei H, Goodarzi F, Van Der Flier-Keller E (2001) Historical variation of elements with respect to different geochemical fractions in recent sediments from Pigeon Lake, Alberta, Canada. J Environ Monit 3:27–36
Sanei H, Stasiuk LD, Goodarzi F (2006) Petrological changes occurring in organic matter from lacustrine sediments during thermal alteration by Rock-Eval pyrolysis. Org Geochem 36:1190–1203
Skyllberg U (2010) Mercury biogeochemistry in soils and sediments. Dev Soil Sci 34:379–410
Smol JP, Wolfe AP, Birks HJB et al (2005) Climate-driven regime shifts in the biological communities of Arctic lakes. Proc Natl Acad Sci USA 102:4397–4402
Stern GA, Sanei H, Roach P et al (2009) Historical interrelated variations of mercury and aquatic organic matter in lake sediment cores from a subarctic lake in Yukon, Canada: further evidence toward the algal-mercury scavenging hypothesis. Environ Sci Technol 43:7684–7690
Temme C, Blanchard P, Steffen A et al (2007) Trend, seasonal and multivariate analysis study of total gaseous mercury data from the Canadian atmospheric mercury measurement network (CAMNet). Atmos Environ 41:5423–5441
Tissot B, Durand B, Espitalié J et al (1974) Influence of the nature and diagenesis of organic matter in the formation of petroleum. Am Assoc Pet Geol Bull 58:499–506
Tyson RV (1995) Sedimentary organic matter organic facies and palynofacies. Chapman and Hall, London
Tyson RV (2001) Sedimentation rate, dilution, preservation and total organic carbon: some results of a modeling study. Org Geochem 32:333–339
Van Krevelen DW (1961) Coal: typology, chemistry, physics constitution. Elsevier, New York
Wolfe AP, Härtling JW (1997) Early Holocene trace metal enrichment in organic lake sediments, Baffin Island, Arctic Canada. Arct Alp Res 29:24–31
Acknowledgments
The sediment cores were retrieved by Mark Nixon, GSC Ottawa. Funding was provided by the Environment and Health Program, Earth Science Sector (Natural Resources Canada), and by ArcticNET. Radiocarbon dating was provided by John Southon (University of California, Irvine), and we particularly thank Roger McNeely for his help. RockEval analyses were carried out by Ross Stewart at GSC Calgary, and Hg determinations by Gail Boila, DFO Winnipeg.
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Sanei, H., Outridge, P.M., Dallimore, A. et al. Mercury–organic matter relationships in pre-pollution sediments of thermokarst lakes from the Mackenzie River Delta, Canada: the role of depositional environment. Biogeochemistry 107, 149–164 (2012). https://doi.org/10.1007/s10533-010-9543-1
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DOI: https://doi.org/10.1007/s10533-010-9543-1