Hostname: page-component-78c5997874-94fs2 Total loading time: 0 Render date: 2024-11-05T04:26:27.525Z Has data issue: false hasContentIssue false
  • English
  • Français

Alpine lake sediment records of the impact of glaciation and climate change on the biogeochemical cycling of soil nutrients

Published online by Cambridge University Press:  20 January 2017

Gabriel M. Filippelli ,
Catherine Souch ,
Brian Menounos ,
Sara Slater-Atwater ,
A.J. Timothy Jull  and
Olav Slaymaker
Gabriel M. Filippelli
Affiliation:
Department of Geology, Indiana University-Purdue University, Indianapolis (IUPUI), IN 46202-5132, USA
Catherine Souch*
Affiliation:
Department of Geography, Indiana University-Purdue University, Indianapolis, IN 46202, USA
Brian Menounos
Affiliation:
Geography Program, University of Northern British Columbia, 3333 University Way, Prince George, BC, Canada V2N 4Z9
Sara Slater-Atwater
Affiliation:
Department of Geology, Indiana University-Purdue University, Indianapolis (IUPUI), IN 46202-5132, USA
A.J. Timothy Jull
Affiliation:
NSF Arizona AMS Laboratory, University of Arizona, Tucson, AZ 85721, USA
Olav Slaymaker
Affiliation:
Department of Geography, The University of British Columbia, 1984 West Mall, Vancouver, BC, Canada V6T 1Z2
*
⁎Corresponding author. Fax: +1 317 278 2525. E-mail addresses:[email protected] (G.M. Filippelli), [email protected] (C. Souch).
Get access Rights & Permissions [Opens in a new window]

Abstract

Lake sediment cores from the Coast Mountains of British Columbia were analyzed using chemical sequential extractions to partition the dominant geochemical fractions of phosphorus (P). The P fractions include mineral P (the original source of bioavailable P), occluded P (bound to soil oxides), and organic P (remains of organic matter). By comparing P fractions of soil and recent lake sediment samples, these fractions are shown to be a valid proxy for landscape-scale nutrient status. Changes in soil development for an alpine watershed (Lower Joffre Lake) are inferred from the P fractions in the basin's outlet lake sediments. Glacially sourced mineral P dominates at the base of the core, but several rapid shifts in P geochemistry are evident in the first ∼3000 yr of the record. The latter indicates an interval of early and rapid soil nutrient maturation from ∼9600 to 8500 cal yr BP and a significant influx of slope-derived material into Lower Joffre Lake. A substantial increase in mineral P occurs at ca. 8200 cal yr BP, consistent with the cold event in the vicinity of the North Atlantic at that time. The more recent record reveals a continual increase in the proportion of mineral P from glacial sources to the lake, indicating a trend toward cooler conditions in the Coast Mountains.

Keywords

Lake sedimentP geochemistryWatershed nutrient statusBritish Columbia
Type
Research Article
Information
Quaternary Research , Volume 66 , Issue 1 , July 2006 , pp. 158 - 166
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Alley, R., Mayewski, P., Sowers, T., Stuiver, M., Taylor, K., and Clark, P. Holocene climate instability a prominent widespread event 8200 yr ago. Geology 25, (1997). 483–486.Google Scholar
Anderson, L.D., and Delaney, M.L. Sequential extraction and analysis of phosphorus in marine sediments Streamlining of the SEDEX procedure. Limnology Oceanography 45, (2000). 509–515.Google Scholar
Barber, D., Dyke, A., Hillaire-Marcel, C., Jennings, A., Andrews, J., Kerwin, M., Bilodeau, G., McNeely, R., Southon, J., Morehead, M., and Gagnon, J. Forcing of the cold event of 8200 years ago by catastrophic draining of Laurentide lakes. Nature 200, (1999). 344–348.Google Scholar
Bradley, R.S. Paleoclimatology: Reconstructing Climates of the Quaternary. Second Edition (1999). Harcourt Academic Press, San Diego, CA. 613 Google Scholar
Chadwick, O.A., Derry, L.A., Vitousek, P.M., Hubert, B.J., and Hedin, L.O. Changing sources of nutrients during four million years of ecosystem development. Nature 397, (1999). 491–497.Google Scholar
Clague, J.J. Quaternary Geology of the Canadian Cordillera Chapter 1 in Quaternary Geology of Canada and Greenland. Fulton, R.J. Geology of Canada vol. 1, (1989). Geological Survey of Canada, 17–98.Google Scholar
Clague, J., and Mathewes, R. Early Holocene thermal maximum in western North America new evidence from Castle Peak British Columbia. Geology 17, (1989). 277–280.2.3.CO;2>CrossRefGoogle Scholar
Clague, J.J., Evans, S.G., Rampton, V.N., and Woodsworth, G.J. Improved age estimates for the White River and Bridge River tephras, Western Canada. Canadian Journal of Earth Science 32, (1995). 1172–1179.CrossRefGoogle Scholar
Crews, T.E., Kitayama, K., Fownes, J.H., Riley, R.H., Herbert, D.A., Mueller-Dombois, D., and Vitousek, P.M. Changes in soil phosphorus fractions and ecosystem dynamics across a long chronosequence in Hawaii. Ecology 76, (1995). 1407–1424.Google Scholar
Cross, M. compiler. (1997). Greenland summit ice cores. Boulder, CO National Snow and Ice Data Center in association with the World Data Center for Paleoclimatology at NOAA-NGDC, and the Institute of Arctic and Alpine Research. CD-ROM.Google Scholar
Cross, A.F., and Schlesinger, W.H. A literature review and evaluation of the Hedley fractionation applications to the biogeochemical cycle of soil phosphorus in natural ecosystems. Geoderma 64, (1995). 197–214.CrossRefGoogle Scholar
Desloges, J.R., and Gilbert, R. Sediment source and hydroclimatic inferences from glacial lake sediments the postglacial sedimentary record of Lillooet Lake British Columbia. Journal of Hydrology 159, (1994). 375–393.CrossRefGoogle Scholar
Engstrom, D.R., Fritz, S.C., Almendinger, J.E., and Juggins, S. Chemical and biological trends during lake evolution in recently deglaciated terrain. Nature 408, (2000). 161–166.CrossRefGoogle ScholarPubMed
Filippelli, G.M. The global phosphorus cycle. Kohn, M., Rakovan, J., Hughes, J. Reviews in Mineralogy and Geochemistry vol. 48, (2002). 391–425.Google Scholar
Filippelli, G.M., and Delaney, M.L. Phosphorus geochemistry of equatorial Pacific sediments. Geochimica et Cosmochimica Acta 60, (1996). 1479–1495.CrossRefGoogle Scholar
Filippelli, G.M., and Souch, C. Effects of climate and landscape development on the terrestrial phosphorus cycle. Geology 27, (1999). 171–174.Google Scholar
Gardner, L.R. The role of rock weathering in the phosphorus budget of terrestrial watersheds. Biogeochemistry 11, (1990). 97–110.CrossRefGoogle Scholar
Gavin, D.G., McLachlan, J.S., Brubaker, L.B., and Young, K.A. Postglacial history of subalpine forests Olympic Peninsula, WA, U. S. A.. The Holocene (2001). 11177–11188.Google Scholar
Hebda, R. British Columbia vegetation and climate history with focus on 6 KA BP. Geographie Physique et Quaternaire 49, (1995). 55–79.CrossRefGoogle Scholar
Leonard, E. Use of sedimentary sequences as indicators of Holocene glacial history Banff National Park, Alberta. Quaternary Research 26, (1986). 218–231.CrossRefGoogle Scholar
Lian, B., and Huntley, D.J. Optical dating studies of post-glacial aeolian deposits from the south-central interior of British Columbia Canada. Quaternary Science Reviews 18, (1999). 1453–1466.Google Scholar
Luckman, B. The little ice age in the Canadian Rockies. Geomorphology 32, (2000). 358–384.CrossRefGoogle Scholar
Luckman, B., and Osborn, G.D. Holocene glacier fluctuations in the middle Canadian Rocky Mountains. Quaternary Research 11, (1979). 52–77.CrossRefGoogle Scholar
Luckman, B., Holdsworth, G., and Osborn, G.D. Neoglacial glacial fluctuations in the Canadian Rockies. Quaternary Research 39, (1993). 144–153.CrossRefGoogle Scholar
Mayewski, P.A., Rohling, E., Stager, J.C., Karlen, W., Maasch, K.A., Meeker, L.D., Meyerson, E.A., Gasse, F., van Kreveld, S., Holmgren, K., Lee-Thorp, J., Rosqvist, G., Rack, F., Staubwasser, M., Schneider, R.R., and Steig, E.J. Holocene climate variability. Quaternary Research 62, (2004). 243–255.CrossRefGoogle Scholar
Menounos, B., (2002). Climate, fine-sediment transport linkages, Coast Mountains, British Columbia. PhD thesis, The University of British Columbia, Vancouver, Canada., 259 pp.Google Scholar
Menounos, B., Koch, J., Osborn, G., Clague, J.J., and Mazzucchi, D. Early Holocene glacier advance, southern Coast Mountains British Columbia, Canada. Quaternary Science Reviews 23, (2004). 1543–1550.CrossRefGoogle Scholar
Morrill, C., and Jacobsen, R.M. How widespread were climate anomalies 8200 years ago?. Geophysical Research Letters 32, (2005). L19701 http://dx.doi.org/10.1029/2005GL023536CrossRefGoogle Scholar
Oldfield, F. Lakes and their drainage basins as units of sediment based ecological study. Progress in Physical Geography 1, (1977). 460–504.CrossRefGoogle Scholar
Osborn, G., and Luckman, B. Holocene glacier fluctuations in the Canadian Cordillera. Quaternary Science Reviews 7, (1988). 115–128.Google Scholar
Pellatt, M.G., and Mathewes, R.W. Holocene tree line and climate change on the Queen Charlotte Islands Canada. Quaternary Research 48, (1997). 88–99.Google Scholar
Ruttenberg, K.C. Development of a sequential extraction method for different forms of phosphorus in marine sediments. Limnology and Oceanogaph. 37, (1992). 1460–1482.CrossRefGoogle Scholar
Ryder, J.M. Geomorphology of the southern part of the Coast Mountains of British Columbia. Zeitscrift fur Geomorphologue 37, (1981). 120–147.Google Scholar
Ryder, J.M., and Thompson, B. Neoglaciation in the southern Coast Mountains of British Columbia chronology prior to the late-neoglacial maximum. Canadian Journal of Earth Science 23, (1986). 273–287.CrossRefGoogle Scholar
Schlesinger, W.H. Biogeochemistry an Analysis of Global Change. (1997). Acad. Press, San Diego.Google Scholar
Schlesinger, W.H., Bruijnzeel, L.A., Bush, M.B., Klein, E.M., Mace, K.A., Raikes, J.A., and Whittaker, R.J. The biogeochemistry of phosphorus after the first century of soil development on Rakata Island Krakatau, Indonesia. Biogeochemistry 40, (1998). 37–55.CrossRefGoogle Scholar
Slater-Atwater, S., (2004). The effects of climate and weathering on terrestrial phosphorus cycling in an alpine system, Coast Mountains, British Columbia. MS Thesis, Department of Geology, Indiana University-Indianapolis, 111 pp.Google Scholar
Souch, C. A methodology to interpret downvalley lake sediments as records of neoglacial activity Coast Mountains British Columbia, Canada. Geografiska Annaler 76A, (1994). 169–186.CrossRefGoogle Scholar
Strickland, J.D.H., and Parsons, T.R. A practical handbook of seawater analysis. Fisheries Research Board Canada Bulletin 167, (1972). 311 Google Scholar
Stuiver, M., Reimer, P.J., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., van der Plicht, J., and Spurk, M. INTCAL98 radiocarbon age calibration 24,000 -0 cal BP. Radiocarbon 40, (1998). 1041–1083.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., and Braziunas, T.F. High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon 40, (1998). 1127–1151.Google Scholar
Tiessen, H., Moir, J.O. Carter, M. Characterization of Available P by Sequential Extraction, in Soil Sampling and Methods of Analysis. (1993). Lewis, Boca Raton, FL. 75–86.Google Scholar
Vitousek, P.M., Chadwick, O.A., Crews, T.E., Fownes, J.H., Hendricks, D.M., and Herbert, D. Soil and ecosystem development across the Hawaiian Islands. GSA Today 7, (1997). 1–8.Google Scholar
Walker, T.W., and Syers, J.K. The fate of phosphorus during pedogenesis. Geoderma 15, (1976). 1–19.CrossRefGoogle Scholar