Hostname: page-component-78c5997874-dh8gc Total loading time: 0 Render date: 2024-11-19T10:46:15.909Z Has data issue: false hasContentIssue false
  • English
  • Français

A dinoflagellate cyst record of Holocene climate and hydrological changes along the southeastern Swedish Baltic coast

Published online by Cambridge University Press:  20 January 2017

Shi-Yong Yu  and
Björn E. Berglund
Shi-Yong Yu*
Affiliation:
Large Lakes Observatory, University of Minnesota Duluth, 2205 East 5th Street, Duluth, MN 55812, USA GeoBiosphere Science Center, Department of Geology/Quaternary Sciences, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden
Björn E. Berglund
Affiliation:
GeoBiosphere Science Center, Department of Geology/Quaternary Sciences, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden
*
⁎Corresponding author. Large Lakes Observatory, University of Minnesota Duluth, 2205 East 5th Street, Duluth, MN 55812, USA. Fax: +1 218 726 6979. E-mail address:[email protected] (S.-Y. Yu).
Get access Rights & Permissions [Opens in a new window]

Abstract

A high-resolution, well-dated dinoflagellate cyst record from a lagoon of the southeastern Swedish Baltic Sea reveals climate and hydrological changes during the Holocene. Marine dinoflagellate cysts occurred initially at about 8600 cal yr BP, indicating the onset of the Littorina transgression in the southeastern Swedish lowland associated with global sea level rise, and thus the opening of the Danish straits. Both the species diversity and the total accumulation rates of dinoflagellate cysts continued to increase by 7000 cal yr BP and then decreased progressively. This pattern reveals the first-order change in local sea level as a function of ice-volume-equivalent sea level rise versus isostatic land uplift. Superimposed upon this local sea level trend, well-defined fluctuations of the total accumulation rates of dinoflagellate cysts occurred on quasi-1000- and 500-yr frequency bands particularly between 7500 and 4000 cal yr BP, when the connection between the Baltic basin and the North Atlantic was broader. A close correlation of the total accumulation rates of dinoflagellate cysts with GISP2 ice core sea-salt ions suggests that fluctuations of Baltic surface conditions during the middle Holocene might have been regulated by quasi-periodic variations of the prevailing southwesterly winds, most likely through a system similar to the dipole oscillation of the modern North Atlantic atmosphere.

Keywords

HoloceneBaltic SeaDinoflagellate cystsLittorina transgressionClimate changesNorth Atlantic storminess
Type
Research Article
Information
Quaternary Research , Volume 67 , Issue 2 , March 2007 , pp. 215 - 224
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

Andersson, H.C. Influence of long-term regional and large-scale atmospheric circulation on the Baltic sea level. Tellus Series A 54, (2002). 76–88.CrossRefGoogle Scholar
Andrén, E., Andrén, T., and Kunzendorf, H. Holocene history of the Baltic Sea as a background for assessing records of human impact in the sediments of the Gotland Basin. The Holocene 10, (2000). 621–636.CrossRefGoogle Scholar
Andrén, E., Andrén, T., and Sohlenius, G. The Holocene history of the southwestern Baltic Sea as reflected in a sediment core from the Bornholm Basin. Boreas 29, (2000). 233–250.Google Scholar
Andrews, J.T., Hardadottir, J., Stoner, J.S., Mann, M.E., Kristjansdottir, G.B., and Koç, N. Decadal to millennial-scale periodicities in North Iceland shelf sediments over the last 12000 cal yr: long-term North Atlantic oceanographic variability and solar forcing. Earth and Planetary Science Letters 210, (2003). 453–465.Google Scholar
Andrews, J.T., Hardardo, R., Hardardottir, J., Kristjansdottir, G.B., Gronvold, K., and Stoner, J.S. A high-resolution Holocene sediment record from Hunafloaall, N Iceland margin: century-to millennial-scale variability since the Vedde tephra. The Holocene 13, (2003). 625–638.Google Scholar
Berglund, B.E. Littorina transgressions in Blekinge, south Sweden—A preliminary survey. Geologiska Föreningens Förhandlingar 93, (1971). 625–652.CrossRefGoogle Scholar
Berglund, B.E., Sandgren, P., Barnekow, L., Hannon, G., Jiang, H., Skog, G., and Yu, S.-Y. Early Holocene history of the Baltic Sea, as reflected in coastal sediments in Blekinge, southeastern Sweden. Quaternary International 130, (2005). 111–139.CrossRefGoogle Scholar
Björck, S. A review of the history of the Baltic Sea, 13.0–8.0 ka BP. Quaternary International 27, (1995). 19–40.CrossRefGoogle Scholar
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hadjas, I., and Bonani, G. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278, (1997). 1257–1266.Google Scholar
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M.N., Showers, W., Hoffmann, S., Lotti-Bond, R., Hajdas, I., and Bonani, G. Persistent solar influence on North Atlantic climate during the Holocene. Science 294, (2001). 2130–2136.CrossRefGoogle ScholarPubMed
Brenner, W.W. Distribution of organic walled microfossils within single laminae from Gotland Basin and their environmental evidence. Baltica 14, (2001). 34–39.Google Scholar
Brenner, W.W. Organic walled microfossils from the central Baltic Sea, indicators of environmental change and base for ecostratigraphic correlation. Baltica 14, (2001). 40–51.Google Scholar
Brenner, W.W. Holocene environmental history of the Gotland Basin (Baltic Sea)—A micropalaeontological model. Palaeogeography, Palaeoclimatology, Palaeoecology 220, (2005). 227–241.Google Scholar
Brenner, W.W., and Meemken, H.-J. Öko-und chronostratigraphische Korrelierung der Zentralen Ostsee mit der Kieler Bucht anhand organisch-wandiger Mikrofossilien. Meyniana 54, (2002). 17–40.Google Scholar
Brown, P., Kennett, J.P., and Ingram, B.L. Marine evidence for episodic Holocene megafloods in North America and the northern Gulf of Mexico. Paleoceanography 14, (1999). 498–510.Google Scholar
Brown, S.L., Bierman, P.R., Lini, A., and Southon, J.R. 10,000 yr record of extreme hydrologic events. Geology 28, (2000). 335–338.Google Scholar
Chapman, M.R., and Shackleton, N.J. Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene. The Holocene 10, (2000). 287–291.Google Scholar
Christensen, C. The Littorina transgression in Denmark. Fisher, A. Man and Sea in the Mesolithics, Coastal Settlements Above and Below Present Sea Level, Oxbow Monograph vol. 53, (1996). Oxbow Books, Oxford. 15–22.Google Scholar
Clemmensen, L.B., Andreasen, F., Heinemeier, J., and Murray, A. A Holocene coastal aeolian system, Vejers, Denmark: Landscape evolution and sequence stratigraphy. Terra Nova 13, (2001). 129–134.CrossRefGoogle Scholar
Dale, B., and Fjellsa, A. Dinoflagellate cysts as paleoproductivity indicators: state of the art, potential, and limits. Zahn, R., Pedersen, T.F., Kaminski, M.A., Labeyrie, L. Carbon Cycling in the Glacial Ocean: Constraints on the Ocean's Role in Global Change, NATO ASI Series I: Global Environmental Change vol. 17, (1994). 521–537.Google Scholar
Dawson, A.G., Elliott, L., Mayewski, P., Lockett, P., Noone, S., Hickey, K., Holt, T., Wadhams, P., and Foster, I. Late-Holocene North Atlantic climate ‘seesaws’, storminess changes and Greenland ice sheet (GISP2) palaeoclimates. The Holocene 13, (2003). 381–392.CrossRefGoogle Scholar
de Vernal, A., Henry, M., Matthiessen, J., Mudie, P.J., Rochon, A., Boessenkool, K.P., Eynaud, F., Grosfjeld, K., Guiot, J., Hamel, D., Harland, R., Head, M.J., Kunz-Pirrung, M., Levac, E., Loucheur, V., Peyron, O., Pospelova, V., Radi, T., Turon, J.L., and Voronina, E. Dinoflagellate cyst assemblages as tracers of sea-surface conditions in the northern North Atlantic, Arctic and sub-Arctic seas: the new ‘n = 677’ data base and its application for quantitative palaeoceanographic reconstruction. Journal of Quaternary Science 16, (2001). 681–698.CrossRefGoogle Scholar
Devillers, R., and de Vernal, A. Distribution of dinoflagellate cysts in surface sediments of the northern North Atlantic in relation to nutrient content and productivity in surface waters. Marine Geology 166, (2000). 103–124.Google Scholar
Digerfeldt, G. A standard profile for Littorina transgression in western Skåne, South Sweden. Boreas 4, (1975). 125–142.Google Scholar
Döös, K., Meier, H.E.M., and Döscher, R. The Baltic haline conveyor belt or the overturning circulation and mixing in the Baltic. Ambio 33, (2004). 261–266.CrossRefGoogle ScholarPubMed
Ekman, M. A common pattern for interannual and periodical sea level variations in the Baltic Sea and adjacent waters. Geophysica 32, (1996). 261–272.Google Scholar
Ekman, M. Secular change of the seasonal sea level variability in the Baltic Sea and secular change of the winter climate. Geophysica 34, (1998). 131–140.Google Scholar
Emeis, K.C., Struck, U., Blanz, T., Kohly, A., and Voss, M. Salinity changes in the central Baltic Sea (NW Europe) over the last 10 000 years. The Holocene 13, (2003). 411–421.Google Scholar
Fischer, H. Imprint of large-scale atmospheric transport patterns on sea-salt records in northern Greenland ice cores. Journal of Geophysical Research 106, (2001). 23977–23984.CrossRefGoogle Scholar
Fonselius, S., and Valderrama, J. One hundred years of hydrographic measurements in the Baltic Sea. Journal of Sea Research 49, (2003). 229–241.CrossRefGoogle Scholar
Glueck, M.F., and Stockton, C.W. Reconstruction of the North Atlantic Oscillation, 1429–1983. International Journal of Climatology 21, (2001). 1453–1465.Google Scholar
Grimm, E.C. CONISS: a FORTRAN 77 program for stratigraphical constrained cluster analysis by the method of incremental sum of squares. Computers and Geosciences 13, (1987). 13–35.Google Scholar
Gundersen, N., (1988). En palynologisk undersøkelse av dinoflagellatcyster langs en synkende salinitetsgradient i recente sedimenter fra Østersjø-området. PhD Dissertation, Geologisk Institutt, Universitetet i Oslo, 96 pp.Google Scholar
Gustafsson, B.G., and Westman, P. On the causes for salinity variations in the Baltic Sea during the last 8500 years. Paleoceanography 17, (2002). 1–14.Google Scholar
Hammarlund, D., Barnekow, L., Birks, H.J.B., Buchardt, B., and Edwards, T.W.D. Holocene changes in atmospheric circulation recorded in the oxygen-isotope stratigraphy of lacustrine carbonates from northern Sweden. The Holocene 12, (2002). 339–351.CrossRefGoogle Scholar
Hanninen, J., Vuorinen, I., and Hjelt, P. Climatic factors in the Atlantic control the oceanographic and ecological changes in the Baltic Sea. Limnology and Oceanography 45, (2000). 703–710.Google Scholar
Harland, R. Distribution maps of recent dinoflagellate cysts in bottom sediments from the North Atlantic Ocean and adjacent seas. Palaeontology 26, (1983). 321–387.Google Scholar
Head, M., Seidenkrantz, M., Janczyk-Kopikowa, Z., Marks, L., and Gibbard, P. Last Interglacial (Eemian) hydrographic conditions in the southeastern Baltic Sea, NE Europe, based on dinoflagellate cysts. Quaternary International 130, (2005). 3–30.Google Scholar
Heegaard, E., Birks, H.J.B., and Telford, R.J. Relationships between calibrated ages and depth in stratigraphical sequences: an estimation procedure by mixed-effect regression. The Holocene 15, (2005). 612–618.Google Scholar
Hofmann, W. Distribution of Cladocera remains in two sediment cores from the central Baltic Sea. Baltica 14, (2001). 52–57.Google Scholar
Huckriede, H., Clasen, S., and Meischner, D. Hydrographic and climatic changes recorded in Holocene sediments of the central Baltic Sea. Baltica 9, (1995). 76–91.Google Scholar
Jacobi, C., and Beckmann, B.R. On the connection between upper atmospheric dynamics and tropospheric parameters: correlations between mesopause region winds and the North Atlantic Oscillation. Climatic Change 43, (1999). 629–643.CrossRefGoogle Scholar
Lass, H.U., and Matthäus, W. On temporal wind variations forcing salt water inflows into the Baltic Sea. Tellus Series A 48, (1996). 663–671.Google Scholar
Lehmann, A., Krauss, W., and Hinrichsen, H.H. Effects of remote and local atmospheric forcing on circulation and upwelling in the Baltic Sea. Tellus Series A 54, (2002). 299–316.Google Scholar
Lewis, J., and Hallett, R. Lingulodinium polyedrum (Gonyaulax polyedra) a blooming dinoflagellate. Ansell, A.D., Gibson, R.N., Barnes, M. Oceanography and Marine Biology: An Annual Review vol. 35, (1997). 97–161.Google Scholar
Luterbacher, J., Xoplaki, E., Dietrich, D., Jones, P.D., Davies, T.D., Portis, D., Gonzalez-Rouco, J.F., von Storch, H., Gyalistras, D., Casty, C., and Wanner, H. Extending North Atlantic Oscillation reconstructions back to 1500. Atmospheric Science Letters 2, (2002). 114–124.CrossRefGoogle Scholar
Marret, F., and Zonneveld, K.A.F. Atlas of modern organic-walled dinoflagellate cyst distribution. Review of Palaeobotany and Palynology 125, (2003). 1–200.Google Scholar
Matsuoka, K. Holocene dinoflagellate cyst assemblages in shallow water sediments of the Tsushima Islands, west Japan. Review of Palaeobotany and Palynology 84, (1994). 155–168.CrossRefGoogle Scholar
Mayewski, P.A., Meeker, L.D., Twickler, M.S., Whitlow, S.I., Yang, Q., Lyons, W.B., and Prentice, M. Major features and forcing of high-latitude northern hemisphere atmospheric circulation using a 110,000-year-long glaciochemical series. Journal of Geophysical Research 102, (1997). 26345–26366.Google Scholar
Miettinen, A. Holocene sea-level changes and glacio-isostasy in the Gulf of Finland, Baltic Sea.. Quaternary International 120, (2004). 91–104.Google Scholar
Müller, A. Late- and postglacial sea-level change and paleoenvironments in the Order Estuary, southern Baltic Sea. Quaternary Research 55, (2001). 86–96.Google Scholar
Nordberg, K., Gustafsson, M., and Krantz, A.-L. Decreasing oxygen concentrations in the Gullmar Fjord, Sweden, as confirmed by benthic foraminifera, and the possible association with NAO. Journal of Marine Systems 23, (2000). 303–316.Google Scholar
Noren, A.J., Bierman, P.R., Steig, E.J., Lini, A., and Southon, J. Millennial-scale storminess variability in the northeastern United States during the Holocene epoch. Nature 419, (2002). 821–824.Google Scholar
O'Brien, S.R., Mayewski, P.A., Meeker, L.D., Meese, D.A., Twickler, M.S., and Whitlow, S.I. Complexity of Holocene climate as reconstructed from a Greenland ice core. Science 270, (1995). 1962–1964.Google Scholar
Oppo, D.W., McManus, J.F., and Cullen, J.L. Deepwater variability in the Holocene epoch. Nature 422, (2003). 277–278.Google Scholar
Orford, J.D., Murdy, J.M., and Wintle, A.G. Prograded Holocene beach ridges with superimposed dunes in north-east Ireland: mechanisms and timescales of fine and coarse beach sediment decoupling and deposition. Marine Geology 194, (2003). 47–64.Google Scholar
Orvik, K.A., Skagseth, O., and Mork, M. Atlantic inflow to the Nordic Seas: current structure and volume fluxes from moored current meters, VM-ADCP and SeaSoar-CTD observations, 1995–1999. Deep-Sea Research Part I 48, (2001). 937–957.Google Scholar
Plag, H.P., and Tsimplis, M.N. Temporal variability of the seasonal sea-level cycle in the North Sea and Baltic Sea in relation to climate variability. Global and Planetary Change 20, (1999). 173–203.Google Scholar
R Development Core Team, (2005). R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. ISBN 3-900051-07-0, URL http://www.R-project.org.Google Scholar
Ram, M., and Stolz, M.R. Possible solar influences on the dust profile of the GISP2 ice core from Central Greenland. Geophysical Research Letters 26, (1999). 1043–1046.Google Scholar
Rochon, A., deVernal, A., Turon, J.L., Matthiessen, J., and Head, M.J. Distribution of recent dinoflagellate cysts in surface sediments from the North Atlantic Ocean and adjacent seas in relation to sea-surface parameters. American Association of Stratigraphic Palynologists Foundation (1999). 1–150.Google Scholar
Rodwell, M.J., Rowell, D.P., and Folland, C.K. Oceanic forcing of the wintertime North Atlantic Oscillation and European climate. Nature 398, (1999). 320–323.Google Scholar
Schinke, H., and Matthäus, W. On the causes of major Baltic inflows—An analysis of long time series. Continental Shelf Research 18, (1998). 67–97.CrossRefGoogle Scholar
Schrum, C. Regionalization of climate change for the North Sea and Baltic Sea. Climate Research 18, (2001). 31–37.Google Scholar
Sohlenius, G., Sternbeck, J., Andrén, E., and Westman, P. Holocene history of the Baltic Sea as recorded in a sediment core from the Gotland Deep. Marine Geology 134, (1996). 183–201.Google Scholar
Stenseth, N.C., Mysterud, A., Ottersen, G., Hurrell, J.W., Chan, K.S., and Lima, M. Ecological effects of climate fluctuations. Science 297, (2002). 1292–1296.CrossRefGoogle ScholarPubMed
Stuiver, M., and Braziunas, T.F. Sun, ocean climate and atmospheric 14CO2: an evaluation of causal and spectral relationships. The Holocene 3, (1993). 289–305.Google Scholar
Stuiver, M., Grootes, P.M., and Braziunas, T.F. The GISP2 δ18O climate record of the past 16,500 years and the role of the sun, ocean, and volcanoes. Quaternary Research 44, (1995). 341–354.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., Plicht, J., and Spurk, M. INTCAL98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40, (1998). 1041–1083.CrossRefGoogle Scholar
Torrence, C., and Compo, G.P. A practical guide to wavelet analysis. Bulletin of the American Meteorological Society 79, (1998). 61–78.Google Scholar
Wilson, P. Holocene coastal dune development on the South Erradale peninsula, Wester Ross, Scotland. Scottish Journal of Geology 38, (2002). 5–13.Google Scholar
Winsor, P., Rodhe, J., and Omstedt, A. Baltic Sea ocean climate: an analysis of 100 yr of hydrographic data with focus on the freshwater budget. Climate Research 18, (2001). 5–15.Google Scholar
Woolf, D.K., Shaw, A.G.P., and Tsimplis, M.N. The influence of the North Atlantic Oscillation on sea-level variability in the North Atlantic region. Global Atmosphere and Ocean System 9, (2003). 145–167.Google Scholar
Yu, S.-Y. centennial-scale cycles in middle Holocene sea level along the southeastern Swedish Baltic coast. Bulletin of the Geological Society of America 115, (2003). 1404–1409.Google Scholar
Yu, S.-Y., Berglund, B.E., Sandgren, P., and Fritz, S.C. Holocene palaeoecology along the Blekinge coast, SE Sweden, and implications for climate and sea-level changes. The Holocene 15, (2005). 278–292.Google Scholar
Zorita, E., and Laine, A. Dependence of salinity and oxygen concentrations in the Baltic Sea on large-scale atmospheric circulation. Climate Research 14, (2000). 25–41.CrossRefGoogle Scholar