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Millennial-Scale Rhythms in Peatlands in the Western Interior of Canada and in the Global Carbon Cycle

Published online by Cambridge University Press:  20 January 2017

Ian D. Campbell ,
Celina Campbell ,
Zicheng Yu ,
Dale H. Vitt  and
Michael J. Apps
Ian D. Campbell
Affiliation:
Canadian Forest Service, 5320-122 Street, Edmonton, Alberta, T6H 3S5, Canada
Celina Campbell
Affiliation:
Department of Biological Sciences, University of Alberta, Edmonton, Alberta, T6G 2E9 Canada
Zicheng Yu
Affiliation:
Canadian Forest Service, 5320-122 Street, Edmonton, Alberta, T6H 3S5 Canada
Dale H. Vitt
Affiliation:
Department of Biological Sciences, University of Alberta, Edmonton, Alberta, T6G 2E9 Canada
Michael J. Apps
Affiliation:
Canadian Forest Service, 5320-122 Street, Edmonton, Alberta, T6H 3S5 Canada
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Abstract

A natural ∼1450-yr global Holocene climate periodicity underlies a portion of the present global warming trend. Calibrated basal radiocarbon dates from 71 paludified peatlands across the western interior of Canada demonstrate that this periodicity regulated western Canadian peatland initiation. Peatlands, the largest terrestrial carbon pool, and their carbon-budgets are sensitive to hydrological fluctuations. The global atmospheric carbon-budget experienced corresponding fluctuations, as recorded in the Holocene atmospheric CO2 record from Taylor Dome, Antarctica. While the climate changes following this ∼1450-yr periodicity were sufficient to affect the global carbon-budget, the resultant atmospheric CO2 fluctuations did not cause a runaway climate–CO2 feedback loop. This demonstrates that global carbon-budgets are sensitive to small climatic fluctuations; thus international agreements on greenhouse gasses need to take into account the natural carbon-budget imbalance of regions with large climatically sensitive carbon pools.

Keywords

peatcarbonHolocenecyclesperiodicitiesCO2Canada
Type
Short Paper
Information
Quaternary Research , Volume 54 , Issue 1 , July 2000 , pp. 155 - 158
Copyright
University of Washington

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References

Berger, A, Loutre, M.F (1991). Insolation values for the climate of the last 10 million years. Quaternary Science Reviews,10, 297–317., CrossRefGoogle Scholar
Bianchi, G.G, McCave, I.N (1999). Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland. Nature,397, 515–517., CrossRefGoogle Scholar
Bond, G, Showers, W, Cheseby, M, Lotti, R, Almasi, P, deMenocal, P, Priore, P, Cullen, H, Hajdas, I, Bonani, G (1997). A pervasive millenial-scale cycle in North Atlantic Holocene and glacial climates. Science,278, 1257–1266., CrossRefGoogle Scholar
Campbell, I.D, McAndrews, J.H (1993). Forest disequilibrium caused by Little Ice Age cooling. Nature,366, 336–338., CrossRefGoogle Scholar
Campbell, C, Campbell, I.A (1997). Calibration, review, and geomorphic implications of postglacial radiocarbon ages in southeastern Alberta, Canada. Quaternary Research,47, 37–44., CrossRefGoogle Scholar
Campbell, C (1998). Late Holocene lake sedimentology and climate change in southern Alberta, Canada. Quaternary Research,49, 96–101., CrossRefGoogle Scholar
Campbell, I.D, Campbell, C, Apps, M.J, Rutter, N.W, Bush, A.B.G (1998). Late Holocene ∼1500 yr climatic periodicities and their implications. Geology,26, 471–473., 2.3.CO;2>CrossRefGoogle Scholar
Dyke, A.S, Prest, V.K (1987). Late Wisconsinan and Holocene retreat of the Laurentide ice sheet. Géographie physique et Quaternaire,41, 237–263., CrossRefGoogle Scholar
Gorham, E (1991). Northern Peatlands: Role in the carbon cycle and probable responses to climatic warming. Ecological Applications,1, 182–195., CrossRefGoogle ScholarPubMed
Grove, J.M (1988). The Little Ice Age. Methuen, New York.Google Scholar
Halsey, L.A, Vitt, D.H, Bauer, I.E (1998). Peatland initiation during the Holocene in continental western Canada. Climatic Change,40, 315–342., CrossRefGoogle Scholar
Hogg, E.H (1997). Temporal scaling of moisture and the forest–grassland boundary in western Canada. Agricultural and Forest Meteorology,84, 115–122., CrossRefGoogle Scholar
Houghton, J.T, Jenkins, G.J, Ephraums, J.J (1990). Climate Change: The IPCC Scientific Assessment. Cambridge Univ. Press, Cambridge.Google Scholar
Hutton, M.J, MacDonald, G.M, Mott, R.J (1994). Postglacial vegetation history of the Mariana Lake region, Alberta. Canadian Journal of Earth Sciences,31, 418–425., CrossRefGoogle Scholar
Indermühle, A, Stocker, T.F, Joos, F, Fischer, H, Smith, H.J, Wahlen, M, Deck, B, Mastroianni, D, Tschumi, J, Blunier, T, Meyer, R, Stauffer, B.A (1999). Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome, Antarctica. Nature,398, 121–126., CrossRefGoogle Scholar
Ladurie, E.L.R (1971). Times of Feast, Times of Famine: A History of Climate Since the Year 1000. Doubleday, Garden City.Google Scholar
Mathewes, R.W, Heusser, L.E, Patterson, R.T (1993). Evidence for a Younger Dryas-like cooling event on the British Columbia coast. Geology,21, 101–104., 2.3.CO;2>CrossRefGoogle Scholar
Mayewski, P.A, Meeker, L.D, Twickler, M.S, Whitlow, S, Yang, Q, Prentice, M (1997). Major features and forcing of high-latitude northern hemisphere atmospheric circulation using a 110,000 year long glaciochemical series. Journal of Geophysical Research,102, 26345–26366., CrossRefGoogle Scholar
Pestiaux, P, Van der Mersch, I, Berger, A, Duplessy, J.C (1988). Paleoclimatre variability at frequencies ranging from 1 cycle per 10000 years to 1 cycle per 1000 years: Evidence for non-linear behaviour of the climate system. Climatic Change,12, 9–37., CrossRefGoogle Scholar
Schulz, M, Stattegger, K (1997). SPECTRUM: Spectral analysis of unevenly spaced paleoclimatic time series. Computers & Geosciences,23, 929–945., CrossRefGoogle Scholar
Shane, L.C.K (1987). Late-glacial vegetational and climatic history of the Allegheny Plateau and the till plains of Ohio and Indiana. Boreas,16, 1–20., CrossRefGoogle Scholar
Sirocko, F, Garbe-Schonberg, D, McIntyre, A, Molfino, B (1996). Teleconnections between the subtropical monsoons and high-latitude climates during the last deglaciation. Science,272, 526–529., CrossRefGoogle Scholar
Stuiver, M, Reimer, P.J (1993). Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon,35, 215–230., CrossRefGoogle Scholar
Stuiver, M, Braziunas, T.F, Grootes, P.M, Zielinski, G.A (1997). Is there evidence for solar forcing of climate in the GISP2 oxygen isotope record?. Quaternary Research,48, 259–266., CrossRefGoogle Scholar
Woodwell, G.M, MacKenzie, F.T (1995). Biotic Feedbacks in the Global Climatic System. Will the Warming Feed the Warming?. Oxford Univ. Press, New York.Google Scholar