Journal of Paleolimnology

, Volume 54, Issue 1, pp 71–86 | Cite as

Spatial variability of recent macroscopic charcoal deposition in a small montane lake and implications for reconstruction of watershed-scale fire regimes

  • Colin J. Courtney Mustaphi
  • Emma L. Davis
  • Joelle T. Perreault
  • Michael F. J. Pisaric
Original paper


Sediment and subfossil deposition can vary spatially within a lake because of multiple taphonomic influences. Paleofire reconstructions are commonly based on stratigraphic analysis of macroscopic charcoal in a single core from the central basin of a lake. We investigated the influence of core location on paleofire interpretations. Our approach was to: (1) examine the spatial distribution of recent charcoal deposition in a lake, (2) evaluate the effects of different subsample volumes on charcoal counts, and (3) explore the influence of sediment water content on charcoal concentration values. We retrieved short sediment cores from eight locations, including central, profundal and sublittoral depths, across a small montane lake located in southeastern British Columbia, Canada, to examine the effect of core location on macroscopic charcoal-based reconstructions of fire history. A long sediment core was also collected from the centre of the lake. The pattern of charcoal accumulation in the short cores was compared to the record collected from the lake’s centre, which spans the Holocene. Each short core was stratigraphically matched with the long core using a discrete tephra marker to form a continuous record and examine the influence of core location on the interpretation of long-term fire regimes. We also examined how sample volume (1 vs. 5 cm3) from a single core affected macroscopic charcoal analysis and paleofire interpretation. Finally, we compared paleofire reconstructions generated from charcoal accumulation rates from wet sediment volume (CHAR) and dry sediment weight. Results were generally similar, but differed slightly in uppermost unconsolidated sediments. Even in small lakes with simple bathymetry, bulk sedimentation rates and charcoal accumulation rates may vary throughout the basin. The best record of past fires is preserved in sediment cores from the flattest and deepest area of the basin. These findings suggest that lake-bottom topography is an important consideration when targeting coring locations and interpreting charcoal data. Understanding how coring location, core sampling strategies and data processing affect paleofire inferences is important for generating robust quantitative paleoecological interpretations.


Fire ecology Fire history Lake sediments Paleofire Taphonomy Wildfire 



Part of this study comprised an honours dissertation project by JTP that was supported by a Natural Sciences and Engineering Research Council of Canada (NSERC) Undergraduate Summer Research Award (USRA). This research was funded by a Jeletzky Memorial Award given to CJCM, an Ontario Graduate Scholarship (OGS) awarded to ELD, and a NSERC Supplemental Strategic Grant and a NSERC Discovery Grant to MFJP. John Little facilitated the use of the Canadian National Fire Database. We thank Alexa D’Addario for help in the laboratory; Dirk Verschuren and Gijs de Cort for useful discussions on sediment-charcoal metrics; Virginia Iglesias, Jennifer Marlon, Simon Brewer and participants of the October 2013 Global Paleofire Working Group meeting in Frasne, France, for fruitful discussions on spatial charcoal data. We also thank Sarah L. Quann, Joshua R. Thienpont, and Esther N. Githumbi, for commenting on earlier drafts of this manuscript. The comments of editor Mark Brenner and two anonymous reviewers greatly improved the manuscript.


  1. Adam GC, Brown BE, Jones CD (1985) Natural selection. Hydrobiologia 150:301–331Google Scholar
  2. Aleman JC, Blarquez O, Bentaleb I, Bonté P, Brossier B, Carcaillet C, Gond V, Gourlet-Fleury S, Kpolita A, Lefèvre I, Oslisly R, Power MJ, Yongo O, Bremond L, Favier C (2013) Tracking land-cover changes with sedimentary charcoal in the Afrotropics. Holocene 23:1853–1862CrossRefGoogle Scholar
  3. Bamber RN (1982) Sodium hexametaphosphate as an aid in benthic sample sorting. Mar Environ Res 7:251–255CrossRefGoogle Scholar
  4. Birks HJB, Birks HH (2004) Quaternary paleoecology. The Blackburn Press, CaldwellGoogle Scholar
  5. Blair JM, Kalff J (1995) The influence of lake morphometry on sediment focusing. Limnol Oceanogr 40:582–588CrossRefGoogle Scholar
  6. Blott SJ, Pye K (2001) GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments. Earth Surf Proc Land 26:1237–1248CrossRefGoogle Scholar
  7. Bradbury JP (1996) Charcoal deposition and redeposition in Elk Lake, Minnesota, USA. Holocene 6:339–344CrossRefGoogle Scholar
  8. Canadian Forest Service (2010) National fire database—agency fire data. Natural Resources Canada, Canadian Forest Service, Northern Forestry Centre, Edmonton, Alberta.
  9. Carcaillet C, Bergeron Y, Richard PJH, Fréchette B, Gauthier S, Prairie YT (2001a) Change of fire frequency in the eastern Canadian boreal forests during the Holocene: does vegetation composition or climate trigger the fire regime? J Ecol 89:930–946CrossRefGoogle Scholar
  10. Carcaillet C, Bouvier M, Fréchette B, Larouche AC, Richard PJH (2001b) Comparison of pollen-slide and sieving methods in lacustrine charcoal analyses for local and regional fire history. Holocene 11:467–476CrossRefGoogle Scholar
  11. Clark JS, Royall PD (1995) Particle-size evidence for source areas of charcoal accumulation in late Holocene sediments of Eastern North American Lakes. Quat Res 43:80–89CrossRefGoogle Scholar
  12. Conedera M, Tinner W, Neff C, Meurer M, Dickens AF, Krebs P (2009) Reconstructing past fire regimes: methods, applications, and relevance to fire management and conservation. Quat Sci Rev 28:555–576CrossRefGoogle Scholar
  13. Courtney Mustaphi CJ, (2013) A landscape-scale assessment of Holocene fire regime controls in south-eastern British Columbia, Canada. (PhD thesis) Carleton University, Ottawa, Ontario, CanadaGoogle Scholar
  14. Courtney Mustaphi CJ, Pisaric MFJ (2013) Synchronous forest fire regimes between watersheds with similar aspect during the late Holocene, southeastern British Columbia, Canada. J Biogeogr 40:1983–1996Google Scholar
  15. Courtney Mustaphi CJ, Pisaric MFJ (2014a) A classification for macroscopic charcoal morphologies found in Holocene lacustrine sediments. Prog Phys Geogr 38:734–754CrossRefGoogle Scholar
  16. Courtney Mustaphi CJ, Pisaric MFJ (2014b) Holocene climate-fire-vegetation interactions at a subalpine watershed in southeastern British Columbia, Canada. Quat Res 81:228–239CrossRefGoogle Scholar
  17. Daly C, Neilson RP, Phillips DL (1994). A statistical-topographic model for mapping climatological precipitation over mountainous terrain. J Appl Meteorol 3:140–158Google Scholar
  18. Dean WE (1974) Determination of carbonate and organic matter in calcareous sediments and sedimentary rocks by loss on ignition: comparison with other methods. J Sediment Petrol 44:242–248Google Scholar
  19. Dearing JA (1999) Magnetic susceptibility. In: Walden J, Oldfield F, Smith J (eds) Environmental magnetism: a practical guide. Technical Guide No. 6. Quaternary Research Association, London, pp 35–62Google Scholar
  20. Edwards KJ, Whittington G (2000) Multiple charcoal profiles in a Scottish lake: taphonomy, fire ecology, human impact and inference. Palaeogeogr Palaeoclimatol Palaeoecol 164:67–86CrossRefGoogle Scholar
  21. Gavin DG, Hu FS, Lertzman K, Corbett P (2006) Weak climatic control of stand-scale fire history during the late Holocene. Ecology 87:1722–1732CrossRefGoogle Scholar
  22. Gedalof Z (2011) Climate and spatial patterns of wildfire. In: McKenzie D, Falk D, Miller C (eds) The landscape ecology of fire. Springer, New York, pp 89–116CrossRefGoogle Scholar
  23. Glew JR (1988) A portable extruding device for close interval sectioning of unconsolidated core samples. J Paleolimnol 1:235–239CrossRefGoogle Scholar
  24. Glew JR, Smol JP, Last WM (2001) Sediment core collection and extrusion. In: Last WM, Smol JP (eds) Tracking environmental change using lake sediments, vol 1., Basin Analysis, Coring, and Chronological TechniquesKluwer Academic Publishers, Dordrecht, pp 73–105CrossRefGoogle Scholar
  25. Grissino-Mayer HD (1999) Modeling fire interval data from the American Southwest with the Weibull distribution. Int J Wildland Fire 9:37–50CrossRefGoogle Scholar
  26. Hallett DJ, Hills LV (2006) Holocene vegetation dynamics, fire history, lake level and climate change in the Kootenay Valley, southeastern British Columbia, Canada. J Paleolimnol 35:351–357CrossRefGoogle Scholar
  27. Hallett D, Walker R (2000) Paleoecology and its application to fire and vegetation management in Kootenay National Park, British Columbia. J Paleolimnol 24:401–414Google Scholar
  28. Hebda RJ (1995) British Columbia vegetation and climate history with focus on 6 ka BP. Géogr Phys Quat 49:55–79Google Scholar
  29. 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. J Paleolimnol 25:101–110CrossRefGoogle Scholar
  30. Higuera PE (2009) CharAnalysis 0.9: diagnostic and analytical tools for sediment-charcoal analysis [User’s Guide].
  31. Higuera PE, Brubaker LB, Anderson PM, Hu FS, Brown TA (2009) Vegetation mediated the impacts of postglacial climate change on fire regimes in the south-central Brooks Range, Alaska. Ecol Monogr 79:201–219CrossRefGoogle Scholar
  32. Higuera PE, Gavin DG, Bartlein PJ, Hallett DJ (2010) Peak detection in sediment-charcoal records: impacts of alternative data analysis methods on fire-history interpretations. Int J Wildland Fire 19:996–1014CrossRefGoogle Scholar
  33. Higuera PE, Barnes JL, Chipman MU, Hu FS (2011) The burning tundra: a look back at the last 6,000 years of fire in the Noatak National Preserve, Northwestern Alaska. Alsk Park Sci 10:36–41Google Scholar
  34. Hilton J (1985) A conceptual framework for predicting the occurrence of sediment focusing and sediment redistribution in small lakes. Limnol Oceanogr 30:1131–1143CrossRefGoogle Scholar
  35. Johnson EA, Wowchuk DR (1993) Wildfires in the southern Canadian Rocky Mountains and their relationship to mid-tropospheric anomalies. Can J Forest Res 23:1213–1222Google Scholar
  36. Journeay JM, Williams SP, Wheeler JO (2000) Tectonic assemblage map, Kootenay Lake, British Columbia-Alberta-USA. Geological Survey of Canada, Open File 2948b. 1:1,000,000Google Scholar
  37. Jungen JR (1980) Soil resources of the Nelson map area (82F). British Columbia Soil Survey. Province of British Columbia, Ministry of Environment, Resource Analysis Branch. Victoria, BC, RAB Bulletin 20, report no. 28, 217 pp + 4 mapsGoogle Scholar
  38. Kelly RF, Higuera PE, Barrett CM, Hu FS (2011) A signal-to-noise-index to quantify the potential for peak detections in sediment-charcoal records. Quat Res 75:11–17CrossRefGoogle Scholar
  39. Koff T, Vandel E (2008) Spatial distribution of macrofossil assemblages in surface sediments of two small lakes in Estonia. Est J Ecol 57:5–20CrossRefGoogle Scholar
  40. Larsen CPS, MacDonald GM (1998) Fire and vegetation dynamics in a jack pine and black spruce forest reconstructed using fossil pollen and charcoal. J Ecol 86:815–828CrossRefGoogle Scholar
  41. Little HW (1960) Nelson (West Half) Kootenay and Similkameen Districts, BC [map]. Geology Map 1090 A. 1:253 440. Geological Survey of Canada, Surveys and Mapping BranchGoogle Scholar
  42. Long CJ, Whitlock C, Bartlein PJ, Millspaugh SH (1998) A 9000-year fire history from the Oregon Coast Range, based on a high-resolution charcoal study. Can J For Res 28:774–787CrossRefGoogle Scholar
  43. Lowe DJ (2008) Tephrochronology and its application: a review. Quat Geochronol 6:107–153CrossRefGoogle Scholar
  44. MacDonald GM, Larsen CP, Szeicz JM, Moser KA (1991) The reconstruction of boreal forest fire history from lake sediments: a comparison of charcoal, pollen, sedimentological, and geochemical indices. Quat Sci Rev 10:53–71CrossRefGoogle Scholar
  45. Mullineaux DR (1996) Pre-1980 tephra-fall deposits erupted from Mount St. Helens, Washington, US Geological Survey Professional Paper 1563, pp 1–99Google Scholar
  46. Nesbitt JH (2010) Quantifying forest fire variability using tree rings Nelson, British Columbia 1700–Present. MSc Thesis, University of British Columbia, VancouverGoogle Scholar
  47. Pellatt MG, Smith MJ, Mathewes RW, Walker IR, Palmer SL (2000) Holocene treeline and climate change in the subalpine zone near Stoyoma Mountain, Cascade Mountains, Southwestern British Columbia, Canada. Arct Antarct Alp Res 32:73–83CrossRefGoogle Scholar
  48. Reimer PJ, Baillie MGL, Bard E, Bayliss A, Beck JW, Blackwell PG, Bronk Ramsey C, Buck CE, Burr GS, Edwards RL, Friedrich M, Grootes PM, Guilderson TP, Hajdas I, Heaton TJ, Hogg AG, Hughen KA, Kaiser KF, Kromer B, McCormac FG, Manning SW, Reimer RW, Richards DW, Southon JR, Talamo S, Turney CSM, van der Plicht J, Weyhenmeyer CE (2009) IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51:1111–1150Google Scholar
  49. Smith MJ, Pellatt MG, Walker IR, Mathewes RW (1998) Postglacial changes in chironomid communities and inferred climate near treeline at Mount Stoyoma, Cascade Mountains, southwestern British Columbia, Canada. J Paleolimnol 20:277–293CrossRefGoogle Scholar
  50. Väliranta M (2006) Terrestrial plant macrofossil records; possible indicators of past lake-level fluctuations in north-eastern European Russia and Finnish Lapland? Acta Palaeobot 46:235–243Google Scholar
  51. Vermaire JC, Pisaric MFJ, Thienpont JR, Courtney Mustaphi CJ, Kokelj SV, Smol JP (2013) Arctic climate warming and sea ice declines lead to increased storm surge activity. Geophys Res Lett 40:1386–1390CrossRefGoogle Scholar
  52. Viau AE, Gajewski K (2001) Holocene variations in the global hydrological cycle quantified by objective gridding of lake level databases. J Geophys Res Atmos 106(D23):31703–31716CrossRefGoogle Scholar
  53. Walker IR, Pellatt MG (2008) Climate changes end ecosystem response in the northern Columbia River basin: a paleoenvironmental perspective. Environ Rev 16:113–140CrossRefGoogle Scholar
  54. Whitlock C, Larsen CPS (2001) Charcoal as a fire proxy. In: Smol JP, Birks HJB, Last WM, Bradley RS, Alverson K (eds) Tracking environmental change using lake sediments, vol 3., Terrestrial, Algal, and Siliceous IndicatorsKluwer Academic Publishers, Dordrecht, pp 75–97CrossRefGoogle Scholar
  55. Whitlock C, Millspaugh SH (1996) Testing the assumptions of fire history studies: an examination of modern charcoal accumulation in Yellowstone National Park, USA. Holocene 6:7–15CrossRefGoogle Scholar
  56. Whitlock C, Bradbury JP, Millspaugh SH (1997) Controls on charcoal distribution in lake sediments: case studies from Yellowstone National Park and Northwestern Minnesota. In: Clark JS, Cachier H, Goldammer JG, Stocks B (eds) Sediment records of biomass burning and global change. Springer, Heidelberg, pp 367–386CrossRefGoogle Scholar
  57. Whitlock C, Higuera PE, McWethy DB, Briles CE (2010) Paleoecological perspectives on fire ecology: revisiting the fire-regime concept. Open Ecol J 3:6–23CrossRefGoogle Scholar
  58. Wright HEJ, Mann DH, Glaser PH (1984) Piston corers for peat and lake sediments. Ecology 65:657–659CrossRefGoogle Scholar
  59. Yamaguchi DK (1983) New tree ring dates for recent eruptions of Mount St. Helens. Quat Res 20:246–250CrossRefGoogle Scholar
  60. Yamaguchi DK (1985) Tree-ring evidence for a two-year interval between recent prehistoric explosive eruptions of Mount St. Helens. Geology 13:554–557CrossRefGoogle Scholar
  61. Zdanowicz CM, Zielinski GA, Germani MS (1999) Mount Mazama eruption: calendrical age verified and atmospheric impact assessed. Geology 27:621–624CrossRefGoogle Scholar

Copyright information

© Springer Science+Business Media Dordrecht 2015

Authors and Affiliations

  • Colin J. Courtney Mustaphi
    • 1
    • 2
  • Emma L. Davis
    • 3
    • 4
  • Joelle T. Perreault
    • 3
  • Michael F. J. Pisaric
    • 3
    • 5
  1. 1.Department of Earth Sciences, Ottawa-Carleton Geoscience CentreCarleton UniversityOttawaCanada
  2. 2.Environment DepartmentUniversity of YorkHeslington, YorkUK
  3. 3.Department of Geography and Environmental StudiesCarleton UniversityOttawaCanada
  4. 4.Department of GeographyUniversity of GuelphGuelphCanada
  5. 5.Department of GeographyBrock UniversitySt. CatharinesCanada

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