Carbon and nitrogen accumulation rates in ombrotrophic peatlands of central and northern Alberta, Canada, during the last millennium

2020 ◽  
Vol 151 (2-3) ◽  
pp. 251-272
Author(s):  
Simon van Bellen ◽  
William Shotyk ◽  
Gabriel Magnan ◽  
Lauren Davies ◽  
Ted Nason ◽  
...  
Geoderma ◽  
2012 ◽  
Vol 183-184 ◽  
pp. 109-123 ◽  
Author(s):  
Markus Egli ◽  
Filippo Favilli ◽  
Rolf Krebs ◽  
Barbara Pichler ◽  
Dennis Dahms

The Holocene ◽  
2016 ◽  
Vol 27 (6) ◽  
pp. 811-821 ◽  
Author(s):  
Anna Larsson ◽  
Ulf Segerström ◽  
Hjalmar Laudon ◽  
Mats B Nilsson

2009 ◽  
Vol 44 (4) ◽  
pp. 313-322 ◽  
Author(s):  
Monalisa Elshayeb ◽  
Michael D. MacKinnon ◽  
D. George Dixon ◽  
Michael Power

Abstract One strategy for reclamation of oil sands leases in northern Alberta is the construction of lakes and wetlands by capping oil sands process-affected material (OSPM) with water. To assess this approach, experimental sites containing a range of OSPM have been constructed to monitor the evolution of the resulting aquatic habitats. Stable isotopes of carbon and nitrogen were used to assess the effects of OSPM on aquatic food webs. Carbon and nitrogen isotopic signatures of sediment, dissolved inorganic and organic carbon, particulate organic matter, periphyton, plants, plankton, aquatic invertebrates, and fish were used to assess differences related to the naphthenic acid (NA) concentration in OSPM and reference sites. NAs are a principal contaminant of concern in OSPM. Sites were grouped into low (0 to 4 mg/L), medium (4 to 15 mg/L), and high (>15 mg/L) NA concentrations. There were no significant differences in food web area or length among the three NA groupings. In most cases, carbon isotope analyses of samples from low, medium, and high NA concentration sites were not significantly different, suggesting that OSPM is not a significant contributor to food web carbon sources. Significant differences were found in nitrogen isotope signatures between low, medium, and high NA sites. Ammonia from OSPM is suggested as the main contributor to δ15N enrichment.


2012 ◽  
Vol 7 (11) ◽  
pp. 1498-1500 ◽  
Author(s):  
Thomas M. Arnold ◽  
Heidi M. Appel ◽  
Jack C. Schultz

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