Abstract
An understanding of the main controls on carbon accumulation in naturally saline peatlands can be useful for furthering peatland reclamation in the Athabasca Oil Sands Region where salinization complicates construction of sustainable peatland ecosystems. As such, the long-term apparent rate of carbon accumulation (LARCA) within a naturally saline fen situated near Fort McMurray, Alberta was studied using two peat cores. Changes in LARCA in less saline part of the fen coincide with water table fluctuations and seem not to be affected by low salinity (soil EC <5 mS cm−1). The highest LARCA values were associated with wet conditions; however, prolonged inundations coupled with high salinity (soil EC >10 mS cm−1) appear to have had a negative effect on LARCA. In the more saline part, salinity seem to have a notable effect on LARCA – hydrology links. Mean LARCA of the site (19.7 g−2 yr.−1) is lower than in western continental fens. The northern less saline part of the fen (soil EC <5 mS cm−1) has LARCA of 29.67 g−2 yr.−1 that is close to LARCA in continental fens, but LARCA in the southern part (soil EC >10 mS cm−1) is considerably lower (9.79 g−2 yr.−1).
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References
Alberta Environment (2008) Guideline for wetland establishment on reclaimed oil sands leases (2nd edition). Prepared by Harris ML of Lorax Environmental for the Wetlands and Aquatics Subgroup of the Reclamation Working Group of the Cumulative Environmental Management Association. Fort McMurray
Andriashek LD (2003) Quaternary geological setting of the Athabasca oil sands (in situ) area, northeast Alberta; Alberta energy and utilities board, EUB/AGS earth sciences report 2002-03, p 295. Available at: http://ags.aer.ca/publications/ESR_2002_03.html#citation. Accessed 20 Nov 2017
Biagi K (2015) Understanding flow pathways, major chemical transformations and water sources using hydrochemical data in a constructed fen, Alberta. M.Sc. Thesis, McMaster University
Bu Z, Hans J, Li H, Zhao G, Zheng X, Ma J, Zeng J (2011) The response of peatlands to climate warming: a review. Acta Ecologica Sinica 31:157–162. https://doi.org/10.1016/j.chnaes.2011.03.006
Campbell ID, Campbell C, Yu Z, Vitt DH, Apps MJ (2000) Millennial-scale rhythms in peatlands in the western interior of Canada and in the global carbon cycle. Quaternary Research 54:155–158. https://doi.org/10.1006/qres.2000.2134
Carrière S (2002) Photographic key for the microhistological identification of some Arctic vascular plants. Arctic 55:247–268. 10.14430/arctic709
Chymko N (2000) Guideline for wetland establishment on reclaimed oil sands leases. Oil SandsWetlands Working Group, Alberta Environment, Environmental Service, Edmonton, Canada, Report #ESD/LM/00-1, T/517
Clymo RS, Turunen J, Tolonen K (1998) Carbon accumulation in peatland. Oikos 81:368–388. https://doi.org/10.2307/3547057
Cooper A (1982) The effects of salinity and waterlogging on the growth and cation uptake of salt marsh plants. New Phytologist 90:263–275. https://doi.org/10.1111/j.1469-8137.1982.tb03258.x
Egan TP, Ungar IA (2000) Mortality of the salt marsh species Salicornia Europaea and Atriplex Prostrata (Chenopodiaceae) in response to inundation. Ohio. Journal of Science 100:24–27
Environment and Parks (2015) Reclamation Criteria for Wellsites and Associated Facilities for Peatlands, October, 2015, Edmonton, Alberta, PP 142. Available at http://aep.alberta.ca. Assessed 19 May 2016
Environment Canada (2015) Calculation Information for 1981 to 2010 Canadian Normals Data. Fort McMuray. Available http://climate.weather.gc.ca/climate_normals/station_metadata_e.html?StnId=2519. Accessed 22 Nov 2015
Halsey LA, Vitt DH, Bauer IE (1998) Peatland initiation during the Holocene in continental western Canada. Climatic Change 40:315–342
Hammer Ø, Harper DAT, Ryan PD (2001) PAST: paleontological statistics software package for education and data analysis. Palaeontologia Electronica 4:9
Heiri O, Lotter AF, Lemcke G (2001) Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results. Journal of Paleolimnology 25:101–110. https://doi.org/10.1023/A:1008119611481
Holmquist J, MacDonald GM (2014) Peatland succession and long-term apparent carbon accumulation in central and northern Ontario, Canada. The Holocene 24:1075–1089. https://doi.org/10.1177/0959683614538074
Hutton MJ, MacDonald GM, Mott RJ (1994) Postglacial vegetation history of the Mariana Lake region, Alberta. Canadian Journal of Earth Sciences 31:418–425. https://doi.org/10.1139/e94-038
Israelsen KR, Ransom CV, Waldron BL (2011) Salinity tolerance of foxtail barley (Hordeum jubatum) and desirable pasture grasses. Weed Sciences 59:500–505. https://doi.org/10.1614/WS-D-10-00164.1
Juggins S (2011) C2 version 1.7: software for ecological and paleoecological data analysis and visualisation. University of Newcastle, Newcastle upon Tyne. Available https://www.staff.ncl.ac.uk/stephen.juggins/software/code/C2.pdf. Assessed 12 Mar 2016
Kessel E (2016) The hydrogeochemistry of a constructed fen peatland in a post-mined landscape in the Athabasca Oil Sands region, Alberta, Canada. M.Sc. Thesis, University of Waterloo
Ketcheson SJ, Price JS, Carey SK, Petrone RM, Mendoza CA, Devito KJ (2016) Constructing fen peatlands in post-mining oil sands landscapes: challenges and opportunities from a hydrological perspective. Earth-Science Reviews 161:130–139. https://doi.org/10.1016/j.earscirev.2016.08.007
Loisel J, Garneau M (2010) Late Holocene paleoecohydrology and carbon accumulation estimates from two boreal peat bogs in eastern Canada: potential and limits of multi-proxy archives. Palaeogeography, Palaeoclimatology, Palaeoecology 291:493–533. https://doi.org/10.1177/0959683614538073
Mauquoy D, Hughes P, Van Geel B (2010) A protocol for plant macrofossil analysis of peat deposits. Mires and Peat 7:1–5
Montemayor MB, Price JS, Rochefort L, Boudreau S (2008) Temporal variations and spatial patterns in saline and waterlogged peat fields. 1. Survival and growth of salt marsh graminoids. Environmental and Experimental Botany 62:333–342. https://doi.org/10.1016/j.envexpbot.2007.10.004
Montemayor MB, Price JS, Rochefort L, Boudreau S (2010) Temporal variations and spatial patterns in saline and waterlogged peat fields: II. Ion accumulation in transplanted salt marsh graminoids. Environmental and Experimental Botany 69:87–94. https://doi.org/10.1016/j.envexpbot.2010.03.012
Montemayor MB, Price JS, Rochefort L (2015) The importance of pH and sand substrate in the revegetation of saline non-waterlogged peat fields. Journal of Environmental Management 163:87–97. https://doi.org/10.1016/j.jenvman.2015.07.052
Necajeva J, Ievinsh G (2008) Seed germination of six coastal plant species of the Baltic region: effect of salinity and dormancy-breaking treatments. Seed Science Research 18:173–177. https://doi.org/10.1017/S0960258508040403
Nelson DW, Sommers LE (1996) Total carbon, organic carbon, and organic matter. In: Sparks DL, Page AL, Helmke PA, Loeppert RH, Soltanpour PN, Tabatabai MA, Johnston CT, Sumner ME (eds) Methods of Soil Analysis. Part 3, Chemical Methods. Soil Science Society of America– American Society of Agronomy, Madison, pp 961–1010
Phillips T, Petrone RM, Wells CM, Price JS (2016) Characterizing dominant controls governing evapotranspiration within a natural saline fen in the Athabasca Oil Sands of Alberta, Canada. Ecohydrology 9:817–829. https://doi.org/10.1002/eco.1685
von Post L, Granlund E (1926) Södra Sveriges Torvtillgångar I (peat resources in southern Sweden I). Sveriges Geologiska Undersökning C 335(19):1–128
Pouliot R, Rochefort L, Graf MD (2012) Impacts of oil sands process water on fen plants: implications for plant selection in required reclamation projects. Environmental Pollution 167:132–137. https://doi.org/10.1016/j.envpol.2012.03.050
Pouliot R, Rochefort L, Graf MD (2013) Fen mosses can tolerate some saline conditions found in oil sands process water. Environmental and Experimental Botany 89:44–50. https://doi.org/10.1016/j.envpol.2012.03.050
Pribyl DW (2010) A critical review of the conventional SOC to SOM conversion factor. Geoderma 156:75–83
Purdy BG, Macdonald SE, Lieffers VJ (2005) Naturally saline boreal communities as models for reclamation of saline oil sand tailings. Restoration Ecology 13:667–677. https://doi.org/10.1111/j.1526-100X.2005.00085.x
Rayment GE, Higginson FR (1992) Australian laboratory handbook of soil and water chemical methods. Inkata Press, Port Melbourne
Rooney RC, Bayley SE, Schindler DW (2012) Oil sands mining and reclamation cause massive loss of peatland and stored carbon. Proceedings of the National Academy of Sciences 109:4933–4937. https://doi.org/10.1073/pnas.1117693108
Roulet NT, Lafleur PM, Richard PJH, Moore TR, Humphreys ER, Bubier J (2007) Contemporary carbon balance and late Holocene carbon accumulation in a northern peatland. Global Change Biology 13:397–411. https://doi.org/10.1111/j.1365-2486.2006.01292.x
Scarlett SJ, Price JS (2013) The hydrological and geochemical isolation of a freshwater bog within a saline fen in north-eastern Alberta. Mires and Peat 12:1–12
Simhayov R (2017) Chemical characterization of construction materials and solute transport in peat from the Nikanotee constructed fen watershed in the Athabasca oil sands region, Alberta, Canada. PhD Thesis, University of Waterloo
Stewart SA, Lemay TG (2011) Inorganic water chemistry of saline fens in north-eastern Alberta (NTS 74D). ERCB/AGS Open File Report 2011-09. Energy Resources Conservation Board and AGS, Edmonton, AB. Available at: http://ags.aer.ca/document/OFR/OFR_2011_09.PDF. Accessed 20 Sept 2016
Tolonen K, Turunen J (1996) Accumulation rates of carbon in mires in Finland and implications for climate change. Holocene 6:171–178
Trites M, Bayley SE (2009a) Organic matter accumulation in western boreal saline wetlands: a comparison of undisturbed and oil sands wetlands. Ecological Engineering 35:1734–1742. https://doi.org/10.1016/j.ecoleng.2009.07.011
Trites M, Bayley SE (2009b) Vegetation communities in continental boreal wetlands along a salinity gradient: implications for oil sands mining reclamation. Aquatic Botany 91:27–39. https://doi.org/10.1016/j.aquabot.2009.01.003
Turetsky M (2002) Current disturbance and the diminishing peatland carbon sink. Geophysical Research Letters 29:7–10. https://doi.org/10.1029/2001GL014000
Turetsky MR, St Louis VL (2006) Disturbance in boreal peatlands. In: Wieder RK, Vitt DH (eds) Boreal peatland ecosystems. Springer Berlin Heidelberg, Berlin, pp 359–379
Vitt DH, Halsey LA, Bauer IE, Campbell C (2000) Spatial and temporal trends in carbon storage of peatlands of continental western Canada through the Holocene. Canadian Journal of Earth Sciences 37:683–693. https://doi.org/10.1139/e99-097
Vitt DH, Wieder RK, Scott KD, Faller S (2009) Decomposition and peat accumulation in rich fens of boreal Alberta, Canada. Ecosystems 12:360–373. https://doi.org/10.1007/s10021-009-9228-6
Wells CM, Price JS (2015a) A hydrologic assessment of a saline-spring fen in the Athabasca oil sands region, Alberta, Canada – a potential analogue for oil sands reclamation. Hydrological Processes 29:4533–4548. https://doi.org/10.1002/hyp.10518
Wells CM, Price JS (2015b) The hydrogeologic connectivity of a low-flow saline-spring fen peatland within the Athabasca oil sands region, Canada. Hydrogeology Journal 23:1799–1816. https://doi.org/10.1007/s10040-015-1301-y
Yu Z (2006) Holocene carbon accumulation of fen peatlands in boreal western Canada: a complex ecosystem response to climate variation and disturbance. Ecosystems 9:1278–1288. https://doi.org/10.1007/s10021-006-0174-2
Yu ZC (2012) Northern peatland carbon stocks and dynamics: a review. Biogeosciences 9:4071–4085. https://doi.org/10.5194/bg-9-4071-2012
Yu Z, Campbell ID, Campbell C, Vitt DH, Bond GC, Apps MJ (2003) Carbon sequestration in western Canadian peat highly sensitive to Holocene wet-dry climate cycles at millennial timescales. The Holocene 13:801–808. https://doi.org/10.1191/0959683603hl667ft
Yu Z, Vitt DH, Wieder RK (2014) Continental fens in western Canada as effective carbon sinks during the Holocene. The Holocene 24:1090–1104. https://doi.org/10.1177/0959683614538075
Acknowledgments
We wish to thank Meaghan Quanz for help with field work; Volodymyr Sivkov, Tristan Gingras-Hill, and Adam Green for help with core collection; Carley Crann (A.E. Lalonde AMS Facility, University of Ottawa) for radiocarbon dating. We thank the editors of Wetlands and anonymous reviewers for comments on an early draft of this work. Funding provided by the Natural Science and Engineering Research Council (NSERC) of Canada, Collaborative Research and Development Program, co-funded by Suncor Energy Inc., Imperial Oil Resources Limited and Shell Canada Energy (Price, Petrone); NSERC Discovery Grant Program (Petrone); NSERC Northern Supplement (Petrone); and Northern Studies Training Program (Volik).
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Volik, O., Petrone, R.M., Wells, C.M. et al. Impact of Salinity, Hydrology and Vegetation on Long-Term Carbon Accumulation in a Saline Boreal Peatland and its Implication for Peatland Reclamation in the Athabasca Oil Sands Region. Wetlands 38, 373–382 (2018). https://doi.org/10.1007/s13157-017-0974-5
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DOI: https://doi.org/10.1007/s13157-017-0974-5