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Potential Pitfalls of Pollen Dating

Published online by Cambridge University Press:  09 February 2016

Thomas Neulieb
Affiliation:
Geography Department and Global Environmental and Climate Change Centre, McGill University, 805 Sherbrooke Street West, Montreal, Quebec H3A 0B9, Canada
Elisabeth Levac*
Affiliation:
Geography Department and Global Environmental and Climate Change Centre, McGill University, 805 Sherbrooke Street West, Montreal, Quebec H3A 0B9, Canada Department of Environmental Studies, Bishop's University, 2600 College Street, Sherbrooke, Quebec J1M 1Z7, Canada
John Southon
Affiliation:
Earth System Science Department, University of California, B321 Croul Hall, Irvine, California 92697-3100, USA
Michael Lewis
Affiliation:
Geological Survey of Canada Atlantic, Natural Resources Canada, Bedford Institute of Oceanography, Box 1006, Dartmouth, Nova Scotia B2Y 4A2, Canada
I Florin Pendea
Affiliation:
Department of Interdisciplinary Studies, Lakehead University – Orillia Campus, 500 University Avenue, Orillia, Ontario L3V0B9, Canada
Gail L Chmura
Affiliation:
Geography Department and Global Environmental and Climate Change Centre, McGill University, 805 Sherbrooke Street West, Montreal, Quebec H3A 0B9, Canada
*
Corresponding author. Email: [email protected].

Abstract

Pollen extracted from ocean and wetland sediments cored from the eastern Canadian Margin, James Bay region, and Atlantic provinces of Canada have been radiocarbon dated and results are reported here. Pollen dates from ocean sediments were compared with marine carbonate (mollusk shells or foraminifera) dates from the same core levels, dates for which validity was assessed via correlations with other cores, and for which reworking has been excluded. Pollen samples from 3 tidal wetlands were taken from levels dated with 137Cs and 210Pb profiles. Pollen dates from 2 additional wetlands were compared with 14C dates of botanical macrofossils. Most pollen dates disagree with 14C dates based on macrofossils or carbonates, with age differences typically exceeding 250 yr and reaching 4000 yr in one instance. In some cores, pollen dates show age reversals. Significant proportions of reworked pollen grains in ocean and wetland samples are associated with pollen dates that are too old. Prolonged core storage could result in pollen 14C ages that are too young, possibly because of growth of fungi or other microbes, but more work is needed to verify this hypothesis. Despite the problems we encountered, some pollen dates are consistent with other 14C dates from the same core levels, suggesting this dating method can work, but at present, more work is needed to understand the conflicting results obtained.

Type
Radiocarbon Reservoir Effects
Copyright
Copyright © 2013 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

Alldredge, AL, Silver, MW. 1988. Characteristics, dynamics and significance of marine snow. Progress in Oceanography 20(1):4182.Google Scholar
Anderson, DM. 2001. Attenuation of millennial-scale events by bioturbation in marine sediments. Paleoceanography 16(4):352–7.Google Scholar
Anderson, TW, Levac, E, Lewis, CFM. 2007. Cooling in the Gulf of St. Lawrence and estuary region at 9.7 to 7.2 14C ka (11.2–8.0 cal ka): palynological response to the PBO and 8.2 cal ka cold events, Laurentide Ice Sheet air-mass circulation and enhanced freshwater runoff. Palaeogeography, Palaeoclimatology, Palaeoecology 246(1):75100.Google Scholar
Anderson, TW, Lewis, CFM. 1992. Climatic influences of deglacial drainage changes in southern Canada at 10 to 8 ka suggested by pollen evidence. Géographie Physique et Quaternaire 46(3):255–72.Google Scholar
Bard, E. 1988. Correction of accelerator mass spectrometry 14C ages measured in planktonic foraminifera: paleoceanographic implications. Palaeogeography 3(6):635–5.Google Scholar
Bard, E. 2001. Paleoceanographic implications of the difference in deep sea sediment mixing between large and fine particles. Palaeogeography 16(3):235–9.Google Scholar
Bard, E, Arnold, M, Mangerud, J, Paterne, M, Labeyrie, L, Duprat, J, Melieres, MA, Sonstegaard, E, Duplessy, JC. 1994. The North Atlantic atmosphere-sea surface 14C gradient during the Younger Dryas climatic event. Earth and Planetary Science Letters 126(4):275–87.Google Scholar
Beecher, CB, Chmura, GL. 2004. Pollen-vegetation relationships in Bay of Fundy salt marshes. Canadian Journal of Botany 82(5):663–70.Google Scholar
Birks, HJ, Birks, HH. 1980. Quaternary Paleoecology. Baltimore: University Park Press.Google Scholar
Blaauw, M, van der Plicht, J, van Geel, B. 2004. Radiocarbon dating of bulk peat samples from raised bogs: non-existence of a previously reported ‘reservoir effect’? Quaternary Science Reviews 23(14–15):1537–42.Google Scholar
Bourgeois, JC, Koerner, RM, Alt, BT. 1985. Airborne pollen: a unique air mass tracer, its influx to the Canadian High Arctic. Annals of Glaciology 7:109–16.Google Scholar
Bowman, S. 1990. Radiocarbon Dating (Interpreting the Past. Berkeley: University of California Press.Google Scholar
Brown, TA, Nelson, DE, Mathewes, RW, Vogel, JS, Southon, JR. 1989. Radiocarbon dating of pollen by accelerator mass spectrometry. Quaternary Research 32(2):205–12.Google Scholar
Brown, TA, Farwell, GW, Grootes, PM, Schmidt, FH. 1992. Radiocarbon dating of pollen extracted from peat samples. Radiocarbon 34(3):550–6.Google Scholar
Chmura, GL. 2001. The fate of salt marshes in Atlantic Canada. Climate Change Action Fund, Natural Resources Canada. 18 p.Google Scholar
Chmura, GL, Eisma, D. 1995. A palynological study of surface and suspended sediments on a tidal flat: implications for pollen transport and deposition in coastal waters. Marine Geology 128(3–4):183200.Google Scholar
Chmura, GL, Hung, GA. 2004. Controls on salt marsh accretion: a test in salt marshes of Eastern Canada. Estuaries 27:7081.Google Scholar
Dale, CT, Haworth, RT. 1979. High resolution seismology studies on late Quaternary sediments of the northeast Newfoundland continental shelf. Current Research, Part B, Geological Survey of Canada, Paper 79-1B. p 357–64.Google Scholar
Dyer, AK. 1986. A palynological investigation of the late Quaternary vegetational history of the Baie Verte Peninsula, northcentral Newfoundland [Master's thesis]. Department of Geography, Memorial University of Newfoundland. 182 pages.Google Scholar
Grimm, EC, Maher, LJ, Nelson, DM. 2009. The magnitude of error in conventional bulk-sediment radiocarbon dates from central North America. Quaternary Research 72:301–8.Google Scholar
Higham, T. 2006. C14 dating: corrections [online]. Available: www.c14dating.com/corr.html [accessed September 6, 2012].Google Scholar
Hinga, KR, Sieburth, J, Heath, GR. 1979. The supply and use of organic matter at the deep-sea floor. Journal of Marine Research 37:357579.Google Scholar
Hodder, TJ. 2009. Sediment analysis of three piston cores from the Labrador Inner Marginal Trough. Coop report to Geological Survey of Canada Atlantic/Natural Resources Canada/Bedford Institute of Oceanography.Google Scholar
Hua, Q, Barbetti, M. 2004. Review of tropospheric bomb 14C data for carbon cycle modeling and age calibration purposes. Radiocarbon 46(3):1273–98.Google Scholar
Josenhans, HW, Fader, GBJ. 1989. A comparison of models of glacial sedimentation along the Eastern Canadian Margin. Marine Geology 84(2–4):273300.CrossRefGoogle Scholar
Josenhans, H, Zevenhuizen, J, Klassen, RA. 1986. The Quaternary geology of the Labrador Shelf. Canadian Journal of Earth Sciences 23:1190–213.Google Scholar
Kilian, MR, van der Plicht, J, van Geel, B, Goslar, T. 2002. Problematic 14C-AMS dates of pollen concentrates from Lake Gościąż (Poland). Quaternary International 88:21–6.Google Scholar
Levac, E. 2002. High resolution palynological records from Atlantic Canada: regional Holocene paleoceanographic and paleoclimatic history [PhD dissertation]. Department of Earth Sciences, Dalhousie University, Halifax. 465 pages.Google Scholar
Levac, E. 2003. Palynological records from Bay of Islands, Newfoundland: direct correlation Holocene paleoceanographic and climatic changes. Palynology 27:135–54.Google Scholar
Levac, E. 2012. Eolian pollen transport towards Sable Island, Nova Scotia, Canada. IPC/IOPC 2012 Conference, August 23–30, Tokyo, Japan. Japanese Journal of Palynology 58:125.Google Scholar
Levac, E, Lewis, CFM, Miller, AAL. 2011. The impact of the final Lake Agassiz flood recorded in northeast Newfoundland and northern Scotian shelves based on century-scale palynological data. In: Rashid, H, Polyak, L, Mosley-Thompson, E, editors. Abrupt Climate Change: Mechanisms, Patterns, and Impacts. Geophysical Monograph Series 193. Washington, DC: American Geological Union. p 139–59.Google Scholar
Lewis, CFM, Miller, AAL, Levac, E, Piper, DJW, Sonnichsen, GV. 2012. Lake Agassiz outburst age and routing by Labrador Current and the 8.2 cal ka cold event. Quaternary International 260:8397.Google Scholar
Long, A, Davis, OK, DeLanois, J. 1992. Separation and 14C dating of pure pollen from lake sediments: nannofossil AMS dating. Radiocarbon 34(3):557–60.CrossRefGoogle Scholar
McNeely, R, Dyke, AS, Southon, JR. 2006. Canadian marine reservoir ages, preliminary data assessment: Open file 5049. Geological Survey of Canada. 3 p.Google Scholar
Mensing, SA, Southon, JR. 1999. A simple method to separate pollen for AMS radiocarbon dating and its application to lacustrine and marine sediments. Radiocarbon 41(1):18.Google Scholar
Mudie, PJ. 1982. Pollen distribution in recent marine sediment, eastern Canada. Canadian Journal of Earth Science 19:729–47.Google Scholar
Mudie, PJ, McCarthy, FMG 1994. Late Quaternary pollen transport processes, western North Atlantic: data from box models cross-margin and N-S transects. Marine Geology 118(1–2):79105.Google Scholar
Pendea, IF. 2011. Mid to late Holocene coastal landscape change in Eastern James Bay [PhD dissertation]. Department of Geography, McGill University, Montreal 154 p.Google Scholar
Pendea, IF, Chmura, GL. 2012. High resolution record of carbon accumulation rates during boreal peatland initiation. Biogeosciences 9:2711–7.Google Scholar
Pendea, IF, Costopoulos, A, Nielsen, C, Chmura, GL. 2010. A new shoreline displacement model for the last 7 ka from eastern James Bay, Canada. Quaternary Research 73(3):474–84.Google Scholar
Regnell, J, Everitt, E. 1996. Preparative centrifugation: a new method for preparing concentrates suitable for radiocarbon dating by AMS. Vegetation History and Archaeobotany 5:201–5.Google Scholar
Reimer, PJ, Reimer, R. 2005. CALIBomb Radiocarbon Calibration [online]. Available: http://calib.qub.ac.uk/CALIBomb/. Accessed 23 February 2013.Google Scholar
Reimer, PJ, Brown, TA, Reimer, RW. 2004. Discussion: reporting and calibration of post-bomb 14C data. Radiocarbon 46(3):1299–304.Google Scholar
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, T, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, McCormac, FG, Manning, SW, Reimer, RW, Richards, DA, 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(4):1111–50.Google Scholar
Richardson, F, Hall, VA. 1994. Pollen concentrate preparation from highly organic Holocene peat and lake deposits for AMS dating. Radiocarbon 36(3):407–12.Google Scholar
Roe, HM, van de Plassche, O. 2005. Modern pollen distribution in a Connecticut saltmarsh: implications for studies of sea-level change. Quaternary Science Reviews 24(18–19):2030–49.Google Scholar
Sandercombe, S. 2011. The marine record of abrupt climate change at Bay of Islands, Newfoundland [MSc thesis]. Department of Geography, McGill University, Montreal. 65 p.Google Scholar
Santos, GM, Southon, JR, Griffin, S, Beaupré, SR, Druffel, ERM. 2007. Ultra small-mass AMS 14C sample preparation and analyses at KCCAMS/UCI Facility. Nuclear Instruments and Methods in Physics Research B 259(1):293302.CrossRefGoogle Scholar
Shotyk, W. 1996. Peat bog archives of atmospheric metal deposition: Geochemical evaluation of peat profiles, natural variations in metal concentrations, and metal enrichment factors. Environmental Reviews 4:149–83.Google Scholar
Southon, J, Santos, G Druffel-Rodriguez, K, Druffel, E, Trumbore, S, Xu, XM, Griffin, S, Ali, S, Mazon, M. 2004. The Keck Carbon Cycle AMS laboratory, University of California, Irvine: initial operation and a background surprise. Radiocarbon 46(1):41–9.Google Scholar
Stuiver, M, Polach, HA. 1977. Discussion: reporting of 14C data. Radiocarbon 19(3):355–63.Google Scholar
Stuiver, M, Reimer, P, Reimer, R. 2005. CALIB Manual [online]. Available: http://calib.qub.ac.uk/calib/manual/. Accessed 15 January 2013.Google Scholar
Stuiver, M, Reimer, PJ, Reimer, R. 2012. Marine Reservoir Correction Database [online]. Available: http://calib.qub.ac.uk/marine/. Accessed 15 January 2013.Google Scholar
Vasil'chuk, AK. 2004. Radiocarbon dating of pollen and spores from ice wedges of the Yamal and Kolyma regions. Biology Bulletin 31:182–92.Google Scholar
Vasil'chuk, AC, Kim, JC, Vasil'chuk, YK. 2004. The AMS dating of pollen from syngenetic ice-wedge ice. Nuclear Instruments and Methods in Physics Research B 223–224:645–9.Google Scholar
Wohlfarth, B, Skog, G, Possnert, G, Holmquist, B. 1998. Pitfalls in the AMS radiocarbon-dating of terrestrial macrofossils. Journal of Quaternary Science 13(2): 137–45.Google Scholar
Zhou, W, Zhou, J, Xiao, JDD, Jull, AJT. 1999. Preliminary study on radiocarbon AMS dating of pollen. Science in China Series D 42:524–30.Google Scholar