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Size and spatial structure of the soil and lacustrine charcoal pool across a boreal forest watershed

Published online by Cambridge University Press:  20 January 2017

Mikael Ohlson ,
Isabella Kasin ,
Anveig Nordtug Wist  and
Anne E. Bjune
Mikael Ohlson*
Affiliation:
Department of Ecology and Natural Resource Management, Norwegian University of Life Sciences, P.O. Box 5003, NO-1432 Ås, Norway
Isabella Kasin
Affiliation:
Department of Ecology and Natural Resource Management, Norwegian University of Life Sciences, P.O. Box 5003, NO-1432 Ås, Norway
Anveig Nordtug Wist
Affiliation:
Department of Ecology and Natural Resource Management, Norwegian University of Life Sciences, P.O. Box 5003, NO-1432 Ås, Norway
Anne E. Bjune
Affiliation:
Uni Climate, Allégaten 55, NO-5007 Bergen, Norway Bjerknes Centre for Climate Research, Allégaten 55, NO-5007 Bergen, Norway
*
*Corresponding author. E-mail address:[email protected] (M. Ohlson).
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Abstract

Forest fires convert a proportion of the burning vegetation into charcoal that is stored in forest soils and lake sediments. In this paper we use a geostatistical approach to present a detailed analysis of the size of the charcoal pool and its spatial variation in a boreal forest watershed including its lake sediment. The amount of soil charcoal averaged 179 g/m2 and ranged from 0 to 3600 g/m2 in the watershed. There was an extreme variation in the size of the charcoal pool over fine (cm) spatial scales. For example, the amount of charcoal in the soil could range from 34 to 1646 g/m2 within a distance of 10 cm. Individually dated soil charcoal particles had radiocarbon ages that varied from 630 to 2930 cal yr BP. The lake sediment began accumulating at 10,600 cal yr BP and charcoal accumulation has been practically continuous ever since then, with the largest peak occurring at 6900 cal yr BP. The lake sediment contained more charcoal, 360 g/m2, than the average for forest soil. We interpret this as an indication of a relatively rapid degradation of charcoal in boreal forest soils.

Keywords

Charcoal degradationCharcoal massFire historyNorway spruceScots pineSoil charcoalWildfire
Type
Original Articles
Information
Quaternary Research , Volume 80 , Issue 3 , November 2013 , pp. 417 - 424
Copyright
University of Washington

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References

Benedict, J.B., (2002). Eolian deposition of forest-fire charcoal above tree limit, Colorado Front Range, U.S.A.: potential contamination of AMS radiocarbon samples. Arctic, Antarctic, and Alpine Research 34, 33–37.Google Scholar
Birks, H.H., (2001). Plant macrofossils. Smol, J.P., Birks, H.J.B., Last, W.M. Tracking Environmental Change Using Lake Sediments. Volume 3: Terrestrial, Algal, and Siliceous Indicators Kluwer, Dordrecht.49–74.Google Scholar
Blaauw, M., (2010). Methods and code for ‘classical’ age-modelling of radiocarbon sequences. Quaternary Geochronology 5, 512–518.Google Scholar
Blanck, Y.L., Rolstad, J., Storaunet, K.O., (2013). Low- to moderate-severity historical fires promoted high tree growth in a boreal Scots pine forest of Norway. Scandinavian Journal of Forest Research 28, 126–135.Google Scholar
Clark, J.S., (1988). Particle motion and the theory of charcoal analysis: source area, transport, deposition and sampling. Quaternary Research 30, 67–80.CrossRefGoogle Scholar
Clark, J.S., Lynch, J., Stocks, B.J., Goldammer, J.G., (1998). Relationships between charcoal particles in air and sediments in west-central Siberia. The Holocene 8, 19–29.CrossRefGoogle Scholar
de Lafontaine, G., Asselin, H., (2011). Soil charcoal stability over the Holocene across boreal northeastern North America. Quaternary Research 76, 196–200.CrossRefGoogle Scholar
de Lafontaine, G., Asselin, H., (2012). Soil charcoal stability over the Holocene—response to comments by Mikael Ohlson. Quaternary Research 78, 155–156.Google Scholar
de Lafontaine, G., Payette, S., (2012). Long-term fire and forest history of subalpine balsam fir (Abies balsamea) and white spruce (Picea glauca) stands in eastern Canada inferred from soil charcoal analysis. The Holocene 22, 191–201.Google Scholar
Gardner, J.J., Whitlock, C., (2001). Charcoal accumulation following a recent fire in the Cascade Range, northwestern USA, and its relevance for fire-history studies. The Holocene 11, 541–549.CrossRefGoogle Scholar
Gavin, D.G., (2003). Forest soil disturbance intervals inferred from soil charcoal radiocarbon dates. Canadian Journal of Forest Research 33, 2514–2518.Google Scholar
Gavin, D.G., Brubaker, L.B., Lertzman, K.P., (2003a). Holocene fire history of a coastal temperate rain forest based on soil charcoal radiocarbon dates. Ecology 84, 186–201.Google Scholar
Gavin, D.G., Brubaker, L.B., Lertzman, K.P., (2003b). An 1800-year record of the spatial and temporal distribution of fire from the west coast of Vancouver Island, Canada. Canadian Journal of Forest Research 33, 573–586.Google Scholar
Higuera, P.E., Peters, M.E., Brubaker, L.B., Gavin, D.G., (2007). Understanding the origin and analysis of sediment–charcoal records with a simulation model. Quaternary Science Reviews 26, 1790–1809.Google Scholar
Higuera, P.E., Whitlock, C., Gage, J.A., (2010). Linking tree-ring and sediment charcoal records to reconstruct fire occurrence and area burned in subalpine forests of Yellowstone National Park, USA. The Holocene 21, 327–341.CrossRefGoogle Scholar
Hockaday, W.C., Grannas, A.M., Kim, S., Hatcher, P.G., (2007). The transformation and mobility of charcoal in a fire-impacted watershed. Geochimica et Cosmochimica Acta 71, 3432–3445.Google Scholar
Hörnberg, G., Ohlson, M., Zackrisson, O., (1995). Stand dynamics, regeneration patterns and long-term continuity in boreal old-growth Picea abies swamp-forests. Journal of Vegetation Science 6, 291–298.Google Scholar
Kane, E.S., Hockaday, W.C., Turetsky, M.R., Masiello, C.A., Valentine, D.W., Finney, B.P., (2010). Topographic controls on black carbon accumulation in Alaskan black spruce forest soils: implications for organic matter dynamics. Biogeochemistry 100, 39–56.Google Scholar
Kasin, I., Blanck, Y.L., Rolstad, J., Storaunet, K.O., Ohlson, M., (2013). The charcoal record in peat and mineral soil across a boreal landscape and possible linkages to climate change and recent fire history. The Holocene 23, 1052–1065.CrossRefGoogle Scholar
Larsen, C.P.S., MacDonald, G.M., (1993). Lake morphometry, sediment mixing and the selection of sites for fine-resolution palaeoecological studies. Quaternary Science Reviews 12, 781–792.Google Scholar
Lehmann, J., Sohi, S., (2008). Comment on “Fire-derived charcoal causes loss of forest humus”. Science 321, 1295.Google Scholar
Lehmann, J., Rillig, M.C., Thies, J., Masiello, C.M., Hockaday, W.C., Crowley, D., (2011). Biochar effects on soil biota – a review. Soil Biology and Biochemistry 43, 1812–1836.CrossRefGoogle Scholar
Lie, M.H., Josefsson, T., Storaunet, K.O., Ohlson, M., (2012). A refined view on the “Green lie”: forest structure and composition succeeding early twentieth century selective logging in SE Norway. Scandinavian Journal of Forest Research 27, 270–284.Google Scholar
Long, C.J., Whitlock, C., Bartlein, P.J., Millspaugh, S.H., (1998). A 9000-year fire history from the Oregon Coast Range, based on a high-resolution charcoal study. Canadian Journal of Forest Research 28, 774–787.CrossRefGoogle Scholar
Lynch, J.A., Hollis, J.L., Hu, F.S., (2004). Climatic and landscape controls of the boreal forest fire regime: Holocene records from Alaska. Journal of Ecology 92, 477–489.Google Scholar
Marlon, J.R., Bartlein, P.J., Daniau, A.-L., Harrison, S.P., Maezumi, S.Y., Power, M.J., Tinner, W., Vanniére, B., (2013). Global biomass burning: a synthesis and review of Holocene paleofire records and their controls. Quaternary Science Reviews 65, 5–25.Google Scholar
Molinari, C., Bradshaw, R.H.W., Risbøl, O., Lie, M., Ohlson, M., (2005). Long-term vegetational history of a Picea abies stand in south-eastern Norway: implications for the conservation of biological values. Biological Conservation 126, 155–165.Google Scholar
Nesje, A., (1992). A piston corer for lacustrine and marine-sediments. Arctic and Alpine Research 24, 257–259.Google Scholar
Niklasson, M., (1998). Dendroecological studies in forest and fire history. Acta Universitatis Agriculturae Sueciae, Silvestria 52, Google Scholar
Niklasson, M., Granström, A., (2000). Number and sizes of fires: long-term spatially explicit fire history in a Swedish boreal landscape. Ecology 81, 1484–1499.Google Scholar
Ohlson, M., (2012). Soil charcoal stability over the Holocene — comment to the paper published by de Lafontaine and Asselin. Quaternary Research 76, 196–200.(2011, Quaternary Research 78, 154).Google Scholar
Ohlson, M., Tryterud, E., (2000). Interpretation of the charcoal record in forest soils: forest fires and their production and deposition of macroscopic charcoal. The Holocene 10, 519–525.Google Scholar
Ohlson, M., Korbøl, A., Økland, R.H., (2006). The macroscopic charcoal record in boreal forested peatlands in South-east Norway. The Holocene 16, 731–741.Google Scholar
Ohlson, M., Dahlberg, B., Økland, T., Brown, K.J., Halvorsen, R., (2009). The charcoal carbon pool in boreal forest soils. Nature Geoscience 2, 692–695.Google Scholar
Ohlson, M., Brown, K.J., Birks, H.J.B., Grytnes, J.-A., Hörnberg, G., Niklasson, M., Seppä, H., Bradshaw, R.H.W., (2011). Invasion of Norway spruce diversifies the fire regime in boreal European forests. Journal of Ecology 99, 395–403.Google Scholar
Payette, S., Filion, L., Delwaide, A., (2008). Spatially explicit fire-climate history of the boreal forest-tundra (Eastern Canada) over the last 2000 years. Philosophical Transactions of the Royal Society B 363, 2301–2316.Google Scholar
Pedersen, L.E., Heaman, L.M., Holm, R.M., (1995). Further constraints on the temporal evolution of the Oslo Rift from precise U–Pb zircon dating in the Siljan–Skrim area. Lithos 34, 301–315.CrossRefGoogle Scholar
Peters, M.E., Higuera, P.E., (2007). Quantifying the source area of macroscopic charcoal with a particle dispersal model. Quaternary Research 67, 304–310.Google Scholar
Pingree, M.R.A., Homann, P.S., Morrissette, B., Darbyshire, R., (2012). Long and short-term effects of fire on soil charcoal of conifer forest in Southwest Oregon. Forests 3, 353–369.CrossRefGoogle Scholar
Preston, C.M., (2009). Fire's black legacy. Nature Geoscience 2, 674–675.Google Scholar
Preston, C.M., Schmidt, M.W.I., (2006). Black (pyrogenic) carbon: a synthesis of current knowledge and uncertainties with special consideration of boreal regions. Biogeosciences 3, 397–420.Google Scholar
R Core Team, . (2013). R: A Language and Environment for Statistical Computing. R Foundation for Statistical Computing, Vienna, Austria.(URL http://www.R-project.org/ ).Google Scholar
Reimer, P.J., (2009). IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51, 1111–1150.CrossRefGoogle Scholar
Ribeiro jr., P.J., Diggle, P.J., (2001). geoR: a package for geostatistical analysis. R-NEWS 1, 2.Google Scholar
Rossi, R.E., (1992). Geostatistical tools for modeling and interpreting ecological spatial dependence. Ecological Monographs 62, 277–314.Google Scholar
Scott, A.C., (2010). Charcoal recognition, taphonomy and uses in palaeoenvironmental analysis. Palaeogeography, Palaeoclimatology, Palaeoecology 291, 11–39.Google Scholar
Singh, N., Abiven, S., Tom, M.S., Schmidt, M.W.I., (2012). Fire-derived organic carbon in soil turns over on a centennial scale. Biogeosciences 9, 2847–2857.Google Scholar
Tinner, W., Hofstetter, S., Zeugin, F., Zimmermann, L., Zweifel, R., (2006). Long-distance transport of macroscopic charcoal by an intensive crown fire in the Swiss Alps — implications for fire history reconstruction. The Holocene 16, 287–292.Google Scholar
Touflan, P., Talon, B., (2009). Spatial reliability of soil charcoal analysis: the case of subalpine forest soils. Ecoscience 16, 23–27.Google Scholar
Whitlock, C., Millspaugh, S.H., (1996). Testing the assumptions of fire-history studies: an examination of modern charcoal accumulation in Yellowstone National Park, USA. The Holocene 6, 7–15.Google Scholar
Whitlock, C., Bardbury, J.P., Millspaugh, S.H., (1997). Controls on charcoal distribution in lake sediments: case studies from Yellowstone National Park and northwestern Minnesota. Clark, J.S., Cachier, H., Goldammer, J.G., Stocks, B. Sediment Records of Biomass Burning and Global Change. Springer, Berlin.367–386.Google Scholar
Wist, A.N., (2008). Spatial structure of the charcoal record in a boreal landscape — a quantitative study of a lake sediment and the surrounding forest soil. Master ThesisDepartment of Ecology and Natural Resource Management, Norwegian University of Life Sciences, .Google Scholar
Zackrisson, O., (1977). Influence of forest fires on the North Swedish boreal forest. Oikos 29, 22–32.Google Scholar
Zackrisson, O., Nilsson, M.-C., Wardle, D.A., (1996). Key ecological function of charcoal from wildfire in the boreal forest. Oikos 77, 10–19.Google Scholar
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