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Chronostratigraphy of the sedimentary record of Limnopolar Lake, Byers Peninsula, Livingston Island, Antarctica

Published online by Cambridge University Press:  20 March 2013

Manuel Toro ,
Ignacio Granados ,
Sergi Pla ,
Santiago Giralt ,
Dermot Antoniades ,
Luis Galán ,
Antonio Martínez Cortizas ,
Hyoun Soo Lim  and
Peter G. Appleby
Manuel Toro*
Affiliation:
Centro de Estudios Hidrográficos (CEDEX), Paseo Bajo Virgen del Puerto, 3, 28005 Madrid, Spain
Ignacio Granados
Affiliation:
Parque Natural de Peñalara, Centro de Investigación y Gestión Puente del Perdón, Ctr. M-604, Km 27.6, 28740 Rascafría, Spain
Sergi Pla
Affiliation:
CSIC-CEAB, Biogeodynamics and Biodiversity Group, C/ Carrer Acces Cala St. Francesc 14, 17300 Blanes, Spain
Santiago Giralt
Affiliation:
Institute of Earth Sciences, Jaume Almera (CSIC), Lluís Solé i Sabarís s/n, 08028 Barcelona, Spain
Dermot Antoniades
Affiliation:
Centre d’études Nordiques, Pavillon Abitibi-Price, Université Laval, Québec, Québec G1V 0A6, Canada
Luis Galán
Affiliation:
Instituto Geológico y Minero de España - IGME, Ríos Rosas 23, 28003 Madrid, Spain
Antonio Martínez Cortizas
Affiliation:
Departamento de Edafoloxía e Química Agrícola, Facultade de Bioloxía - Rúa Lope Gómez de Marzoa, s/n, Campus Vida, 15782 Santiago de Compostela, Spain
Hyoun Soo Lim
Affiliation:
Department of Geological Sciences, Pusan National University, Pusan 609-735, Korea
Peter G. Appleby
Affiliation:
Department of Mathematical Sciences, University of Liverpool, Liverpool L69 3BX, UK
*
[email protected]
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Abstract

The chronostratigraphy of the sedimentary record of Limnopolar Lake, located on Byers Peninsula (Livingston Island, South Shetland Islands, Maritime Antarctica), is described based on radionuclides and radiocarbon age dating. The oldest moss macrofossil age was 6700±50 yr bp (7510±80 cal yr bp) from which the age/depth model estimates a basal age for the sedimentary record of c. 8300 cal yr bp, suggesting an earlier deglaciation of Byers Peninsula than reported in previous studies. Lithological units and other stratigraphic zones are described throughout the sediment core, showing different mineralogical composition and a fine alternation of clays and silty clays and moss layers of Drepanocladus longifolius. Based on magnetic susceptibility analyses, a number of probable primary and reworked tephra layers were identified, seven of them confirmed by SEM observations, and most of them in agreement with the regional tephrachronology stratigraphy for the north-west Antarctic Peninsula. Sedimentation rates showed no significant changes during the last 5000 years with the exception of an abrupt event that took place around 5400 cal yr bp, which implied the sedimentation of c. 30 cm of clays in a very short time, probably related to a period of glacial re-advance that caused abrupt changes in geomorphological processes in the catchment.

Keywords

137Cs datingdeglaciationDrepanocladus longifolius210Pb datingradiocarbon datingtephrachronology
Type
Research Articles
Information
Antarctic Science , Volume 25 , Issue 2: Byers Peninsula – A New Reference Site For The Maritime Antarctic , April 2013 , pp. 198 - 212
Copyright
Copyright © Antarctic Science Ltd 2013

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References

Anisimov, O.A., Vaughan, D.G., Callaghan, T.V., Furgal, C., Marchant, H., Prowse, T.D., Vilhjálmsson, H.Walsh, J.E. 2007. Polar regions (Arctic and Antarctic). In Parry, M.L., Canziani, O.F., Palutikof, J.P., van Der Linden, P.J. & Hanson, C.E., eds. Climate change 2007: impacts, adaptation and vulnerability. Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 653–685.Google Scholar
Appleby, P.G.Oldfield, F. 1978. The calculation of 210Pb dates assuming a constant rate of supply of unsupported 210Pb to the sediment. Catena, 5, 1–8.CrossRefGoogle Scholar
Appleby, P.G., Richardson, N.Nolan, P.J. 1992. Self-absorption corrections for well-type germanium detectors. Nuclear Instruments and Methods in Physics Research B, 71, 228–233.CrossRefGoogle Scholar
Appleby, P.G., Nolan, P.J., Gifford, D.W., Godfrey, M.J., Oldfield, F., Anderson, N.J.Battarbee, R.W. 1986. 210Pb dating by low background gamma counting. Hydrobiologia, 141, 21–27.CrossRefGoogle Scholar
Baker, P.E., McReath, I., Harvey, M.R., Rooboi, M.J.Davies, T.G. 1975. The geology of the South Shetland Islands: V. Volcanic evolution of Deception Island. British Antarctic Survey Scientific Reports, No. 78, 81 pp.Google Scholar
Bentley, M.J., Hodgson, D.A., Smith, J.A., Ó Cofaigh, C., Domack, E.W., Larter, R.D., Roberts, S.J., Brachfeld, S., Leventer, A., Hjort, C., Hillenbrand, C.D.Evans, J. 2009. Mechanisms of Holocene palaeoenvironmental change in the Antarctic Peninsula region. The Holocene, 19, 51–69.CrossRefGoogle Scholar
Björck, S.Zale, R. 1996. Late Holocene tephrochronology and palaeoclimate, based on lake sediment studies. In López-Martínez, J., Thomson, M.R.A. et al., eds. Geomorphological map of Byers Peninsula, Livingston Island. BAS GEOMAP Series, Sheet 5-A. Cambridge: British Antarctic Survey, 43–48.Google Scholar
Björck, S., Sandgren, P.Zale, R. 1991a. Late Holocene tephrochronology of the northern Antarctic Peninsula. Quaternary Research, 36, 322–328.CrossRefGoogle Scholar
Björck, S., Hjort, C., Ingólfsson, Ó.Skog, G. 1991b. Radiocarbon dates from the Antarctic Peninsula - problems and potential. In Lowe, J.J., ed. Radiocarbon dating: recent applications and future potential. Quaternary Proceedings, 1, 55–65.Google Scholar
Björck, S., Håkansson, H., Olsson, S., Barnekow, L.Janssens, J. 1993. Palaeoclimatic studies in South Shetlands Islands, Antarctica, based on numerous stratigraphic variables in lake sediments. Journal of Paleolimnology, 8, 233–272.CrossRefGoogle Scholar
Björck, S., Håkansson, H., Zale, R., Karlén, W.Jönsson, B.L. 1991c. A late Holocene lake sediment sequence from Livingston Island, South Shetland Islands, with palaeoclimatic implications. Antarctic Science, 3, 61–72.CrossRefGoogle Scholar
Björck, S., Hjort, C., Ingólfsson, Ó., Zale, R.Ising, J. 1996. Holocene deglaciation chronology from lake sediments. In López-Martínez, J., Thomson, M.R.A. et al., eds. Geomorphological map of Byers Peninsula, Livingston Island. BAS GEOMAP Series, Sheet 5-A. Cambridge: British Antarctic Survey, 49–51.Google Scholar
Blaauw, M.Christen, J.A. 2011. Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Analysis, 6, 457–474.CrossRefGoogle Scholar
Chung, F.H. 1974. Quantitative interpretation of X-ray diffraction patterns of mixtures. Journal of Applied Crystallography, 7, 519–531.CrossRefGoogle Scholar
Fretzdorff, S.Smellie, J.L. 2002. Electron microprobe characterization of ash horizons in sediments from the central Bransfield basin (Antarctic Peninsula): evidence for at least two volcanic sources. Antarctic Science, 14, 412–421.CrossRefGoogle Scholar
Galán, L., Vegas, J.García-Cortés, A. 2007. Caracterización de las propiedades físicas en registros lacustres mediante GEOTEK Multisensor Core Logger. Aplicación para el estudio paleoclimático del maar de Fuentillejo. In Lario, J. & Silva, P.G., eds. Contribuciones al estudio del periodo Cuaternario. Sección de Publicaciones de la Escuela Técnica Superior de Ingenieros Industriales, Universidad Politécnica de Madrid, 187–188.Google Scholar
Hall, B.L. 2010. Holocene relative sea-level changes and ice fluctuations in the South Shetland Islands. Global and Planetary Change, 74, 15–26.CrossRefGoogle Scholar
Hjort, C., Ingólfsson, Ó.Björck, S. 1992. The last major deglaciation in the Antarctic Peninsula region: a review of recent Swedish Quaternary research. In Yoshida, Y., Kaminuma, K. & Shiraishi, K., eds. Recent progress in Antarctic earth science. Tokyo: Terra Scientific Publishing Company, 741–743.Google Scholar
Hodgson, D.A., Doran, P.T., Roberts, D.McMinn, A. 2004. Paleolimnological studies from the Antarctic and Subantarctic islands. In Pienitz, R., Douglas, M.S.V. & Smol, J.P., eds. Long-term environmental change in Arctic and Antarctic lakes. Dordrecht: Springer, 419–474.CrossRefGoogle Scholar
Hodgson, D.A., Dyson, C.L., Jones, V.J.Smellie, J.L. 1998. Tephra analysis of sediments from Midge Lake (South Shetland Islands) and Sombre Lake (South Orkney Islands), Antarctica. Antarctic Science, 10, 13–20.CrossRefGoogle Scholar
Hodgson, D.A., Noon, P.E., Vyverman, W., Bryant, C.L., Gore, D.B., Appleby, P., Gilmour, M., Verleyen, E., Sabbe, K., Jones, V.J., Ellis-Evans, J.C.Wood, P.B. 2001. Were the Larsemann Hills ice-free through the Last Glacial Maximum? Antarctic Science, 13, 440–454.CrossRefGoogle Scholar
Ingólfsson, O. 2004. Quaternary glacial and climate history of Antarctica. In Ehlers, J. & Gibbard, P.L., eds. Quaternary glaciations - extent and chronology, Part III. New York: Elsevier, 3–43.Google Scholar
Ingólfsson, O., Hjort, C.Humlum, O. 2003. Glacial and climate history of the Antarctic Peninsula since the Last Glacial Maximum. Arctic, Antarctic, and Alpine Research, 35, 175–186.CrossRefGoogle Scholar
Keller, R.A., Fisk, M.R., White, W.M.Birkenmajer, K. 1991. Isotopic and trace element constraints on mixing and melting models of marginal basin volcanism, Bransfield Strait, Antarctica. Earth and Planetary Science Letters, 111, 287–303.CrossRefGoogle Scholar
Lee, Y.I., Lim, H.S., Yoon, H.I.Tatur, A. 2007. Characteristics of tephra in Holocene lake sediments on King George Island, West Antarctica: implications for deglaciation and paleoenvironment. Quaternary Science Reviews, 26, 3167–3178.CrossRefGoogle Scholar
Li, S.P., Ochyra, R., Wu, P.C., Seppelt, R.D., Cai, M.H., Wang, H.Y.Li, C.S. 2009. Drepanocladus longifolius (Amblystegiaceae), an addition to the moss flora of King George Island, South Shetland Islands, with a review of Antarctic benthic mosses. Polar Biology, 32, 1415–1425.CrossRefGoogle Scholar
López-Martínez, J., Serrano, E.Martínez de Pisón, E. 1996. Geomorphological features of the drainage system. In López-Martínez J., Thomson M.R.A. et al., eds. Geomorphological map of Byers Peninsula, Livingston Island. BAS GEOMAP Series, Sheet 5-A. Cambridge: British Antarctic Survey, 15–19.Google Scholar
López-Martínez, J., Serrano, E., Schmid, T., Mink, S.Linés, C. 2012. Periglacial processes and landforms in the South Shetland Islands (northern Antarctic Peninsula region). Geomorphology, 55, 62–79.CrossRefGoogle Scholar
Matthies, D., Mäusbacher, R.Storzer, D. 1990. Deception Island tephra: a stratigraphical marker for limnic and marine sediments in Bransfield Strait area, Antarctica. Zentralblatt für Geomorphologie und Paläontologie, 33, 219–234.Google Scholar
Mäusbacher, R., Muller, J., Munnich, M.Schmidt, R. 1989. Evolution of postglacial sedimentation in Antarctic lakes (King George Island). Zeitschrift für Geomorphologie, 33, 219–234.CrossRefGoogle Scholar
McCormac, F.G., Hogg, A.G., Blackwell, P.G., Buck, C.E., Higham, T.F.G.Reimer, P.J. 2004. SHCal04 Southern Hemisphere calibration 0–11.0 cal Kyr bp. Radiocarbon, 46, 1087–1092.CrossRefGoogle Scholar
Newman, L., Convey, P., Gibson, J.A.E.Linse, K. 2009. Antarctic paleobiology: glacial refugia and constraints on past ice-sheet reconstructions. PAGES news, 17(1), 22–24.CrossRefGoogle Scholar
Oksanen, J., Blanchet, F.G., Kindt, R., Legendre, P., Minchin, P.R., O'Hara, R.B., Simpson, G.L., Solymos, P., Henry, M., Stevens, H.Wagner, H. 2012. vegan: community ecology package. R package version 2.0-3. http://CRAN.R-project.org/package=veganGoogle Scholar
Pallàs, R., Smellie, J.L., Casas, J.M.Calvet, J. 2001. Using tephrochronology to date temperate ice: correlation between ice tephras on Livingston Island and eruptive units on Deception Island volcano (South Shetland Islands, Antarctica). The Holocene, 11, 149–160.CrossRefGoogle Scholar
Quayle, W.C., Peck, L.S., Peat, H., Ellis-Evans, J.C.Harrigan, P.R. 2002. Extreme responses to climate change in Antarctic lakes. Science, 295, 645–645.CrossRefGoogle ScholarPubMed
R Development Core Team. 2012. R: a language and environment for statistical computing. Vienna: Wirtschafts University, http://www.R-project.org/Google Scholar
Smellie, J.L. 1990. Graham Land and South Shetland Islands: summary. Antarctic Research Series, 48, 303–312.Google Scholar
Smellie, J.L. 1999. The upper Cenozoic tephra record in the south polar region: a review. Global and Planetary Change, 21, 51–70.CrossRefGoogle Scholar
Sterken, M., Roberts, S.J., Hodgson, D.A., Vyverman, W., Balbo, A.L., Sabbe, K., Moreton, S.G.Verleyen, E. 2012. Holocene glacial and climate history of Prince Gustav Channel, northeastern Antarctic Peninsula. Quaternary Science Reviews, 31, 93–111.CrossRefGoogle Scholar
Sugden, D.E.Clapperton, C.M. 1986. Glacial history of the Antarctic Peninsula and South Georgia. South African Journal of Science, 82, 508–509.Google Scholar
Tatur, A., del Valle, R.Barczuk, A. 1999. Discussion on the uniform pattern of Holocene tephrochronology in South Shetland Islands, Antarctica. Polish Polar Studies, XXVI Polar Symposium. Lublin: Maria Curie Sklodowska University Press, 303–321.Google Scholar
Toms, P.S., King, M., Zárate, M.A., Kemp, R.A.Foit, F.F. Jr 2004. Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina. Quaternary Research, 62, 60–75.CrossRefGoogle Scholar
Toro, M., Camacho, A., Rochera, C., Rico, E., Bañón, M., Fernández-Valiente, E., Marco, E., Justel, A., Avendaño, M.C., Ariosa, Y., Vincent, W.F.Quesada, A. 2007. Limnological characteristics of the freshwater ecosystems of Byers Peninsula, Livingston Island, in maritime Antarctica. Polar Biology, 30, 635–649.CrossRefGoogle Scholar
Turner, J., Colwell, S.R., Marshall, G.J., Lachlan-Cope, T.A., Carelton, A.M., Jones, P.D., Lagun, V., Reid, P.A.Iagovkina, S. 2005. Antarctic climate change during the last 50 years. International Journal of Climatology, 25, 279–294.CrossRefGoogle Scholar
Vaughan, D.G., Marshall, G., Connolley, W.M., Parkinson, C., Mulvaney, R., Hodgson, D.A., King, J.C., Pudsey, C.J., Turner, J.Wolff, E. 2003. Recent rapid regional climate warming on the Antarctic Peninsula. Climate Change, 60, 243–274.CrossRefGoogle Scholar
Watcham, E.P., Bentley, M.J., Hodgson, D.A., Roberts, S.J., Fretwell, P.T., Lloyd, J.M., Larter, R.D., Whitehouse, P.L., Leng, M.J., Monien, P.Moreton, S.G. 2011. A new relative sea level curve for the South Shetland Islands, Antarctica. Quaternary Science Reviews, 30, 3152–3170.CrossRefGoogle Scholar
Willmott, V., Domack, E.W., Canals, M.Brachfeld, S. 2006. A high resolution relative paleointensity record from the Gerlache–Boyd paleo-ice stream region, northern Antarctic Peninsula. Quaternary Research, 66, 1–11.CrossRefGoogle Scholar
Wolfe, A.P., Miller, G.H., Olsen, C.A., Forman, S.L., Doran, P.T.Holmgren, S.U. 2004. Geochronology of high latitude lake sediments. In Pienitz, R., Douglas, M.S.V. & Smol, J.P., eds. Long-term environmental change in Arctic and Antarctic lakes. Dordrecht: Springer, 19–52.CrossRefGoogle Scholar