Abstract
Beaver are well known to influence the geomorphology and geochemistry of boreal waters, in addition to being prominent vectors in the selective import of deciduous coarse woody debris (CWD). Because the stable carbon isotope ratios of deciduous trees are lower than those of coniferous trees, the possibility exists that the δ13C values of particulate organic matter near beaver lodges may differ from those characteristic for littoral regions without beaver activity. In agreement with this supposition, δ13C was found to significantly increase in progressively smaller size fractions of CWD collected from near lodges, probably due to the more rapid breakdown, decomposition and disappearance of deciduous material.
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Benner, R., M. L. Fogel, E. Sprague & R. E. Hodson, 1987. Depletion of 13C in lignin and its implications for stable isotope studies. Nature 329: 708–710.
Blais, J. M., R. L. France, L. E. Kimpe & R. J. Cornett, 1998. Climatic changes in northwestern Ontario have had a greater effect on erosion and sediment accumulation than logging and fire: evidence form 210Pb chronology in lake sediments. Biogeochemistry 43: 235–252.
Brunskill, G. J., D. Povoledo, B. W. Graham & M. P. Stainton, 1971. Chemistry of surface sediments of 16 lakes in the Experimental Lakes Area, northwestern Ontario. J. Fish. Res. Bd Can. 28: 277–294.
Ertel, J. R. & J. I. Hedges, 1985. Sources of sedimentary humic substances: vascular plant detritus. Geochim. Cosmochim. Acta 49: 2097–2107.
Ford, T. E. & R. J. Naiman, 1988. Alteration of carbon cycling by beaver: methane evasion rates from boreal forest streams and rivers. Can. J. Zool. 66: 529–533.
France, R. L., 1995. Macroinvertebrate standing crop in littoral regions of allochthonous detritus accumulation: implications for forest management. Biol. Conserv. 71: 35–39.
France, R. L., 1996. Carbon isotope ratios in logged and unlogged boreal forests: examination of the potential for determining wildlife habitat use. Envir. Manag. 20: 249–255.
France, R. L., 1997a. The importance of beaver lodges in structuring littoral communities in boreal headwater lakes. Can. J. Zool. 75: 1009–1013.
France, R. L., 1997b. Macroinvertebrate colonization of woody debris in Canadian Shield lakes following clearcutting. Conserv. Biol. 11: 513–517.
France, R. & R. Peters, 1995. Predictive model of the effects on lake metabolism of decreased airborne litterfall through riparian deforestation. Conserv. Biol. 9: 1578–1586.
France, R., R. Peters & L. McCabe, 1998. Spatial relationships among boreal riparian trees, litterfall and soil erosion potential with reference to buffer strip management and coldwater fisheries. Ann. bot. Fenn. 35: 1–9.
Gorham, E. & J. E. Sanger, 1975. Fossil pigments in Minnesota lake sediments and their bearing upon the balance between terrestrial and aquatic inputs to sedimentary organic matter. Verh. int. Ver. Limnol. 19: 2267–2273.
Harmon, M. E., 1986. Ecology of coarse woody debris in temperate ecosystems. Adv. Ecol. Res. 15: 133–302.
Hedges, J. I., G. I. Cowie, J. R. Ertel, R. J. Barbour & P. G. Hatcher, 1985. Degradation of carbohydrates and ligins in buried woods. Geochim. Cosmochim. Acta 49: 701–711.
Hodkinson, I. D., 1975. A community analysis of the benthic insect fauna of an abandoned beaver pond. J. anim. Ecol. 44: 533–552.
Johnston, C. A. & R. J. Naiman, 1987. Boundary dynamics at the aquatic-terrestrial interface: the influence of beaver and geomorphology. Land. Ecol. 1: 47–57.
Johnston, C. A. & R. J. Naiman, 1990a. Aquatic patch creation in relation to beaver population trends. Ecology 71: 1617–1621.
Johnston, C. A. & R. J. Naiman, 1990b. Browse selection by beaver: effects on riparian forest composition. Can. J. For. Res. 20: 1036–1043.
LaZerte, B. D., 1983. Stable carbon isotope ratios: implications for the source of sediment carbon and for phytoplankton carbon assimilation in Lake Meemphremagog, Quebec. Can. J. Fish. aquat. Sci. 40: 1658–1666.
Leavitt, S. W., 1993. Seasonal 13C/12C changes in tree rings: species and site coherence, and a possible drought influence. Can. J. For. Res. 23: 210–218.
Makereth, F. J. H., 1965. Chemical investigation of lake sediments and their interpretation. Proc. Roy. Soc. B. 161: 295–303.
McDowell, D. M. & R. J. Naiman, 1986. Structure and function of a benthic invertebrate stream community as influenced by beaver (Castor canadensis). Oecologia 68: 481–489.
Naiman, R. J., 1982. Characteristics of sediment and organic carbon export from pristine boreal forest watersheds. Can. J. Fish. aquat. Sci. 39: 1699–1718.
Naiman, R. J., C. A. Johnston & J. C. Kelley, 1988. Alteration of North American streams by beaver. BioScience 38: 753–762.
Naiman, R. J., G. Pinay, C. A. Johnston & J. Pastor, 1990. Beaver influences on the long-term biogeochemical characteristics of boreal forest drainage networks. Ecology 75: 905–921.
Northcott, T. H., 1971. Feedings habits of beaver in Newfoundland. Oikos 22: 407–410.
Ritchie, J. C., 1989. Carbon content of sediments of small reservoirs. Wat. Res. Bull. 25: 301–308.
Schallenberg, M. & J. Kalff, 1993. Constraints on hypolimnetic metabolism in lakes: a stable isotope study. Unpubl. report. Dept. Biol., McGill Univ., Montreal.
Smith, M. E., C. T. Driscoll, B. J. Wyskowski, C. M. Brooks & C. C. Cosentini, 1991. Modification of stream ecosystem structure and function by beaver (Castor canadensis) in the Adirondack Mountains, New York. Can. J. Zool. 69: 55–61.
Ward, G. M. & N. G. Aumen, 1986. Woody debris as a source of fine particulate organic matter in coniferous forest stream ecosystems. Can. J. Fish. aquat. Sci. 43: 1635–1642.
Wedin, D. A., L. L. Tieszen, B. Dewey & J. Pastor, 1995. Carbon isotope dynamics during grass decomposition and soil organic matter formation. Ecology 76: 1383–1392.
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France, R.L. Beaver alter stable carbon isotope ratios of benthic particulate organic matter. Hydrobiologia 441, 237–240 (2000). https://doi.org/10.1023/A:1017512100132
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DOI: https://doi.org/10.1023/A:1017512100132