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Quantitative assessment of precipitation seasonality and summer surface wetness using ombrotrophic sediments from an Arctic Norwegian peatland

Published online by Cambridge University Press:  20 January 2017

Jonathan E. Nichols ,
Marie Walcott ,
Raymond Bradley ,
Jon Pilcher  and
Yongsong Huang
Jonathan E. Nichols
Affiliation:
Department of Geological Sciences, Brown University, Providence, RI, USA
Marie Walcott
Affiliation:
Department of Geological Sciences, Brown University, Providence, RI, USA
Raymond Bradley
Affiliation:
Department of Geosciences, University of Massachusetts, Amherst, Amherst, MA, USA
Jon Pilcher
Affiliation:
Palaeoecology Centre, Queen's University, Belfast, Belfast, Northern Ireland, UK
Yongsong Huang*
Affiliation:
Department of Geological Sciences, Brown University, Providence, RI, USA
*
⁎Corresponding author. E-mail address: yongsong_huang@brown.edu (Y. Huang).
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Abstract

Seasonality of precipitation is an important yet elusive climate parameter in paleoclimatological reconstructions. This parameter can be inferred qualitatively from pollen and other paleoecological methods, but is difficult to assess quantitatively. Here, we have assessed seasonality of precipitation and summer surface wetness using compound specific hydrogen and carbon isotope ratios of vascular plant leaf waxes and Sphagnum biomarkers extracted from the sediments of an ombrotrophic peatland, Bøstad Bog, Nordland, Norway. Our reconstructed precipitation seasonality and surface wetness are consistent with regional vegetation reconstructions. During the early Holocene, 11.5–7.5 ka, Fennoscandia experienced a cool, moist climate. The middle Holocene, 7.5–5.5 ka, was warm and dry, transitioning towards cooler and wetter conditions from the mid-Holocene to the present. Changes in seasonality of precipitation during the Holocene show significant coherence with changes in sea surface temperature in the Norwegian Sea, with higher SST corresponding to greater percentage of winter precipitation. Both high SST in the Norwegian Sea and increased moisture delivery to northern Europe during winter are correlated with a strong gradient between the subpolar low and subtropical high over the North Atlantic (positive North Atlantic Oscillation).

Keywords

Stable isotopesPeat bogsPaleoclimateLeaf waxesPrecipitation seasonalityNorth AtlanticArctic climateNorth Atlantic Oscillation

Information

Type
Research Article
Information
Quaternary Research , Volume 72 , Issue 3 , November 2009 , pp. 443 - 451
Copyright
University of Washington

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References

Baas, M., Pancost, R., van Geel, B., and Sinninghe Damsté, J.S. A comparative study of lipids in Sphagnum species. Organic Geochemistry 31, (2000). 535–541.Google Scholar
Barber, K.E., Maddy, D., Rose, N., Stevenson, A.C., Stoneman, R., and Thompson, R. Replicated proxy-climate signals over the last 2000 yr from two distant UK peat bogs: new evidence for regional palaeoclimate teleconnections. Quaternary Science Reviews 19, (2000). 481–487.CrossRefGoogle Scholar
Birks, C., and Koç, N. A high-resolution diatom record of late-Quaternary sea-surface temperatures and oceanographic conditions from the eastern Norwegian Sea. Boreas 31, (2002). 323–344.Google Scholar
Blackford, J. Paleoclimatic records from peat bogs. Trends in Ecology and Evolution 15, (2000). 193–198.Google Scholar
Blackford, J.J., and Chambers, F.M. Proxy climate record for the last 1000 years from Irish blanket peat and a possible link to solar variability. Earth and Planetary Science Letters 133, (1995). 145–150.Google Scholar
Blodau, C., and Moore, T.R. Micro-scale CO2 and CH4 dynamics in a peat soil during a water fluctuation and sulfate pulse. Soil Biology & Biogeochemistry 35, (2003). 535–547.Google Scholar
Booth, R.K. Testate amoebae as palioindicators of surface-moisture changes on Michigan peatlands: modern ecology and hydrological calibration. Journal of Paleolimnology 28, (2002). 329–348.CrossRefGoogle Scholar
Bowen, G.J., and Revenaugh, J. Interpolating the isotopic composition of modern meteoric precipitation. Water Resources Research 39, (2003). 1299 Google Scholar
Bowen, G.J., and Wilkinson, B. Spatial distribution of δ18O in meteoric precipitation. Geology 30, (2002). 315–318.2.0.CO;2>CrossRefGoogle Scholar
Bowen, G.J., Wassenaar, L.I., and Hobson, K.A. Global application of stable hydrogen and oxygen isotopes to wildlife forensics. Oecologia 143, (2005). 337–348.Google Scholar
Calvo, E., Grimalt, J., and Jansen, E. High resolution U37K sea surface temperature reconstruction in the Norwegian Sea during the Holocene. Quaternary Science Reviews 21, (2002). 1385–1394.CrossRefGoogle Scholar
Caseldine, C., Baker, A., Charman, D., and Hendon, D. A comparative study of optical properties of NaOH peat extracts: implications for humification studies. The Holocene 10, (2000). 649–658.CrossRefGoogle Scholar
Charman, D. Peatlands and Environmental Change. (2002). John Wiley and Sons Ltd, Chichester.Google Scholar
Clark, I., and Fritz, P. Environmental Isotopes in Hydrogeology. (1997). CRC Press, Boca Raton.Google Scholar
Collister, J.W., Rieley, G., Stern, B., Eglinton, G., and Fry, B. Compound specific 13C analyses of leaf lipids from plants with differing carbon dioxide metabolism. Organic Geochemistry 21, (1994). 619–628.CrossRefGoogle Scholar
Davis, R., and Anderson, D. Classification and distribution of freshwater peatlands in Maine. Northeastern Naturalist 8, (2001). 1–50.Google Scholar
Flatau, M., Talley, L., and Niiler, P. The North Atlantic oscillation, surface current velocities, and SST changes in the subpolar North Atlantic. Journal of Climate 16, (2003). 2355–2369.CrossRefGoogle Scholar
Frankignoul, C., de Coëtlogon, G., Joyce, T., and Dong, S. Gulf Stream variability and ocean–atmosphere interactions. Journal of Physical Oceanography 31, (2001). 3516–3529.2.0.CO;2>CrossRefGoogle Scholar
Fritz, S. Paleolimnological records of climatic change in North America. Limnology and Oceanography 41, (1996). 882–889.Google Scholar
Glaser, P.H., Siegel, D.I., Romanowicz, E.A., and Shen, Y.P. Regional linkages between raised bogs and the climate, groundwater, and landscape of north-western Minnesota. Journal of Ecology 85, (1997). 3–16.Google Scholar
Halsey, L., Vitt, D., and Gignac, L. Sphagnum-dominated peatlands in North America since the last glacial maximum: their occurrence and extent. The Bryologist 103, (2000). 334–352.Google Scholar
Hou, J., Huang, Y., Wang, Y., Shuman, B., Oswald, W.W., Faison, E., and Foster, D.R. Postglacial climate reconstruction based on compound-specific D/H ratios of fatty acids from Blood Pond, New England, 2006. Geochemistry Geophysics Geosystems (2006). 7 Google Scholar
Hou, J., Huang, Y., Oswald, W.W., Foster, D.R., and Shuman, B. Centennial scale compound-specific hydrogen isotope record of Pleistocene–Holocene climate transition from southern New England. Geophysical Research Letters (2007). 34 Google Scholar
Hou, J., D'andrea, W., and Huang, Y. Can sedimentary leaf waxes record D/H ratios of continental precipitation? Field, model, and experimental assessments. Geochimica et Cosmochimica Acta 72, (2008). 3503–3517.Google Scholar
Huang, Y., Eglinton, G., Ineson, P., Latter, P.M., Bol, R., and Douglas, D.D. Absence of carbon isotope fractionation of individual n-alkanes in a 23 year field decomposition experiment with Calluna vulgaris . Organic Geochemistry 26, (1997). 497–501.CrossRefGoogle Scholar
Huang, Y., Shuman, B., Wang, Y., Webb, T. III Hydrogen isotope ratios of palmitic acid in lacustrine sediments record late Quaternary climate variations. Geology 30, (2002). 1103–1106.2.0.CO;2>CrossRefGoogle Scholar
Huang, Y., Shuman, B., Wang, Y., Webb, T. III Hydrogen isotope ratios of individual lipids in lake sediments as novel tracers of climatic and environmental change: a surface sediment test. Journal of Paleolimnology 31, (2004). 363–375.Google Scholar
Huang, Y., Alexandre, M., and Wang, Y. Structure and isotopic ratios of aliphatic side chains in the insoluble organic matter of the Murchison carbonaceous chondrite. Earth and Planetary Science Letters 259, (2007). 517–525.Google Scholar
Hurrell, J., and Dickson, R. Climate variability over the North Atlantic. Stensth, G.O., Ottersen, G., Hurrell, J., and Belgrano, A. Marine Ecosystems and Climate Variation. (2004). Oxford University Press, Oxford. 15–31.Google Scholar
Johansen, O.S., and Vorren, K.-D. The prehistoric expansion of farming into arctic Norway — a chronology based on C-14 dating. Radiocarbon 28, (1986). 739–747.Google Scholar
Kalnay, E. et al. The NCEP/NCAR 40-year reanalysis project. Bulletin of the American Meteorological Society 77, (1996). 437–470.Google Scholar
Kim, J., and Verma, S. Surface exchange of water vapour between an open Sphagnum fen and the atmosphere. Boundary-Layer Meteorology 79, (1996). 243–264.Google Scholar
Loisel, J., Garneau, M., and Hélie, J.-F. Modern Sphagnum δ13C signatures follow a surface moisture gradient in two boreal peat bogs, James Bay lowlands, Québec. Journal of Quaternary Science 24, (2009). 209–214.Google Scholar
Mauquoy, D., and Barber, K. Testing the sensitivity of the palaeoclimatic signal from ombrotrophic peat bogs in northern England. Review of Palaeobotany and Palynology 119, (2002). 219–240.Google Scholar
McMullen, J., Barber, K.E., and Johnson, B. A paleoecological perspective on vegetation succession on raised bog microforms. Ecological Monographs 74, (2004). 45–77.Google Scholar
Nichols, J.E., Booth, R.K., Jackson, S.T., Pendall, E.G., and Huang, Y. Palohydrologic reconstruction based on n-alkane distributions in ombrotrophic peat. Organic Geochemistry 37, (2006). 1505–1513.Google Scholar
Nott, C.J., Xie, S., Avsejs, L.A., MAddy, D., Chambers, F.M., and Evershed, R.P. N-Alkane distribution in ombrotrophic mires as indicators of vegetation change related to climatic variation. Organic Geochemistry 31, (2000). 231–235.Google Scholar
Pancost, R., Baas, M., van Geel, B., and Sinninghe Damste, J.S. Bioarkers as proxies for plant inputs to peats: an example from a sub-boreal ombrotrophic bog. Organic Geochemistry 33, (2002). 675–690.Google Scholar
Pilcher, J., Bradley, R., Francus, P., and Anderson, L. A Holocene tephra record from the Lofoten Islands, Arctic Norway. Boreas 34, (2005). 136–156.Google Scholar
Raghoebarsing, A., Smolders, A., and Schmid, M. Methanotrophic symbionts provide carbon for photosynthesis in peat bogs. Nature 436, (2005). 1153–1156.Google Scholar
Ripullone, F., Matsuo, N., Stuart-Williams, H., Wong, S., Borghetti, M., Tani, M., and Farquhar, G. Environmental effects on oxygen isotope enrichment of leaf water in cotton leaves. Plant Physiology 146, (2008). 729–736.Google Scholar
Roulet, N.T., LaFleur, P., Richard, P., Moore, T., Humphreys, E., and Bubier, J. Contemporary carbon balance and late Holocene carbon accumulation in a northern peatland. Global Change Biology 13, (2007). 397–411.Google Scholar
Sachse, D., Radke, J., and Gleixner, G. δD values of individual n-alkanes from terrestrial plants along a climatic gradient—implications for the sedimentary biomarker record. Organic Geochemistry 37, (2006). 469–483.Google Scholar
Seppä, H., and Hammarlund, D. Pollen-stratigraphic evidence of Holocene hydrological chane in northern Fennoscandia supported by independent isotopic data. Journal of Paleolimnology 24, (2000). 69–79.Google Scholar
Shuman, B., and Donnelly, J.P. The influence of seasonal precipitation and temperature regimes on lake levels in the northeastern United States during the Holocene. Quaternary Research 65, (2006). 44–56.Google Scholar
Shuman, B., Newby, P., Huang, Y., Webb, T. III Evidence for the close climatic control of New England vegetation history. Ecology 85, (2004). 1297–1310.Google Scholar
Snowball, I., Korhola, A., Briffa, K., and Koç, N. Holocene climate dynamics in Fennoscandia and the North Atlantic. Battarbee, R.W., Gasse, F., Stickley, C.E. Past Climate Variability through Europe and Africa Vol. 6, (2004). Springer, Dordrecht.Google Scholar
Xie, S., Nott, C., Avsejs, L., Volders, F., and Maddy, D. Palaeoclimate records in compound-specific δD values of a lipid biomarker in ombrotrophic peat. Organic Geochemistry 31, (2000). 1053–1057.Google Scholar
Xie, S., Nott, C., Avsejs, L., Maddy, D., and Chambers, F. Molecular and isotopic stratigraphy in an ombrotrophic mire for paleoclimate reconstruction. Geochimica et Cosmochimica Acta 68, (2004). 2849–2862.CrossRefGoogle Scholar
Vorren, K.-D. Anthropogenic influence on the natural vegetation in coastal North-Norway during the Holocene, development of farming and pastures. Norwegian Archaeological Review 2, (1979). 1–21.Google Scholar
Vorren, K.-D. The impact of early agriculture on the vegetation of Northern Norway — a discussion of the anthropogenic indicators in biostratigraphic data. Behre, K.E. Anthropogenic Indicators in Pollen Diagrams. (1986). A.A. Balkema, Rotterdam.Google Scholar
White, J.W.C., Cook, E.R., Lawrence, J.R., and Broecker, W.S. The D/H ratios of sap in trees — implications for water sources and tree-ring D/H ratios. Geochimica et Cosmochimica Acta 49, (1985). 237–246.Google Scholar
Williams, T., and Flannagan, L. Effect of changes in water content on photosynthesis, transpiration and discrimination against 13CO2 and C18O16O in Pleurozium and Sphagnum. Oecologia 108, (1996). 38–46.Google Scholar
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