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Depositional environment and climate changes during the Holocene in Grande Valley, Fildes Peninsula, King George Island, Antarctica

Published online by Cambridge University Press:  13 September 2017

Zhuding Chu ,
Liguang Sun ,
Yuhong Wang ,
Tao Huang  and
Xin Zhou
Zhuding Chu
Affiliation:
School of Earth and Space Sciences & Anhui Province Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei 230026, China
Liguang Sun*
Affiliation:
School of Earth and Space Sciences & Anhui Province Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei 230026, China
Yuhong Wang
Affiliation:
National Institutes of Health, Bethesda, MD 20892, USA
Tao Huang
Affiliation:
School of Earth and Space Sciences & Anhui Province Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei 230026, China
Xin Zhou
Affiliation:
School of Earth and Space Sciences & Anhui Province Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei 230026, China
*
*Corresponding author: slg@ustc.edu.cn
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Abstract

A 9.24 m sediment core, GA-2, was collected on the coastal platform of Grande Valley, a relatively narrow and shallow fjord in Fildes Peninsula, King George Island, Antarctica. The sediment was formed between 6600 and 2000 cal. yr bp according to accelerator mass spectrometry (AMS) 14C dating of five bulk sediment samples. The comprehensive proxy indicators (grain size, loss on ignition at 550°C, magnetic susceptibility, elements) were analysed, and three separate depositional environments and an alternating climate change pattern were identified. Grande Valley experienced a warm marine environment between 6600 and 5800 cal. yr bp, a minor cooling between 5800 and 4800 cal. yr bp, the transition from cool to warm during 4800–4400 cal. yr bp, a mid-Holocene climatic optimum between 4400 and 2700 cal. yr bp, and the onset of the Neoglacial at 2700 cal. yr bp. This study reconstructed the environmental history of Grande Valley during the mid–late Holocene, provides the missing marine record of historical climate for the western coast of Fildes Peninsula and lays the foundation for further study of the climate and environment changes therein. Our finding that the sea level was c. 12 m a.m.s.l. at 2000 cal. yr bp allows for detailed reconstruction of Holocene sea level variations.

Keywords

climate historyfjord sedimentgrain sizemarine environment
Type
Earth Sciences
Information
Antarctic Science , Volume 29 , Issue 6 , December 2017 , pp. 545 - 554
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Copyright
© Antarctic Science Ltd 2017 

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References

Ball, D.F. 1964. Loss‐on‐ignition as an estimate of organic matter and organic carbon in non‐calcareous soils. European Journal of Soil Science, 15, 84–92.Google Scholar
Barnard, A., Wellner, J.S. & Anderson, J.B. 2014. Late Holocene climate change recorded in proxy records from a Bransfield Basin sediment core, Antarctic Peninsula. Polar Research, 33, 10.3402/polar.v33.17236.CrossRefGoogle Scholar
Bentley, M.J., Hodgson, D., Smith, J., Cofaigh, C.Ó., Domack, E., Larter, R., Roberts, S., Brachfeld, S., Leventer, A., Hjort, C., Hillenbrand, C.D. & Evans, J. 2009. Mechanisms of Holocene palaeoenvironmental change in the Antarctic Peninsula Region. Holocene, 19, 51–69.CrossRefGoogle Scholar
Björck, S., Håkansson, H., Olsson, S., Barnekow, L. & Janssens, J. 1993. Palaeoclimatic studies in South Shetland 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. 1991. A late Holocene lake sediment sequence from Livingston Island, South Shetland Islands, with palaeoclimatic implications. Antarctic Science, 3, 61–72.Google Scholar
Björck, S., Olsson, S., Ellis-Evans, C., Håkansson, H., Humlum, O. & deLirio, J.M. 1996. Late Holocene palaeoclimatic records from lake sediments on James Ross Island, Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 121, 195–220.Google Scholar
Bloemendal, J. 1983. Paleoenvironmental implications of the magnetic characteristics of sediments from deep-sea drilling project site-514, southeast argentine basin. Initial Reports of the Deep-Sea Drilling Project, 71, 1097–1108.Google Scholar
Brachfeld, S.A., Banerjee, S.K., Guyodo, Y. & Acton, G.D. 2002. A 13 200 year history of century to millennial-scale paleoenvironmental change magnetically recorded in the Palmer Deep, western Antarctic Peninsula. Earth and Planetary Science Letters, 194, 311–326.Google Scholar
Chen, Z.Y., Chen, Z.L. & Zhang, W.G. 1997. Quaternary stratigraphy and trace-element indices of the Yangtze Delta, eastern China, with special reference to marine transgressions. Quaternary Research, 47, 181–191.Google Scholar
Chu, Z.D., Sun, L.G., Huang, W., Huang, T. & Zhou, X. 2016. On selecting bulk fjord sediment samples for radiocarbon dating in Fildes Peninsula, Antarctica. Quaternary International, 425, 173–182.Google Scholar
Ciais, P., Jollzel, J., Petit, J.R., Lipenkov, V. & White, J.W.C. 1994. Holocene temperature variations inferred from six Antarctic ice cores. Annals of Glaciology, 20, 427–436.CrossRefGoogle Scholar
Domack, E.W. & Williams, C.R. 1990. Fine structure and suspended sediment transport in three Antarctic fjords. Antarctic Research Series, 50, 71–89.Google Scholar
Heiri, O., Lotter, A.F. & Lemcke, G. 2001. Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results. Journal of Paleolimnology, 25, 101–110.Google Scholar
Hjort, C., Ingólfsson, Ó., Möller, P. & Lirio, J.M. 1997. Holocene glacial history and sea-level changes on James Ross Island, Antarctic Peninsula. Journal of Quaternary Science, 12, 259–273.Google Scholar
Jones, V.J., Hodgson, D.A. & Chepstow-Lusty, A. 2000. Palaeolimnological evidence for marked Holocene environmental changes on Signy Island, Antarctica. Holocene, 10, 43–60.Google Scholar
Kirby, M.E., Domack, E.W. & McClennen, C.E. 1998. Magnetic stratigraphy and sedimentology of Holocene glacial marine deposits in the Palmer Deep, Bellingshausen Sea, Antarctica: implications for climate change? Marine Geology, 152, 247–259.Google Scholar
Liu, X.D., Zhao, S.P., Sun, L.G., Luo, H.H., Yin, X.B., Xie, Z.Q., Wang, Y.H., Liu, K.X., Wu, X.H., Ding, X.F. & Fu, D.P. 2006. Geochemical evidence for the variation of historical seabird population on Dongdao Island of the South China Sea. Journal of Paleolimnology, 36, 259–279.Google Scholar
Majewski, W., Wellner, J.S., Szczuciński, W. & Anderson, J.B. 2012. Holocene oceanographic and glacial changes recorded in Maxwell Bay, West Antarctica. Marine Geology, 326, 67–79.Google Scholar
Mäusbacher, R., Muller, J. & Schmidt, R. 1989. Evolution of postglacial sedimentation in Antarctic lakes (King-George-Island). Zeitschrift Fur Geomorphologie, 33, 219–234.CrossRefGoogle Scholar
McLaren, P. & Bowles, D. 1985. The effects of sediment transport on grain-size distributions. Journal of Sedimentary Petrology, 55, 457–470.Google Scholar
Michalchuk, B.R., Anderson, J.B., Wellner, J.S., Manley, P.L., Majewski, W. & Bohaty, S. 2009. Holocene climate and glacial history of the northeastern Antarctic Peninsula: the marine sedimentary record from a long SHALDRIL core. Quaternary Science Reviews, 28, 3049–3065.CrossRefGoogle Scholar
Milliken, K.T., Anderson, J.B., Wellner, J.S., Bohaty, S.M. & Manley, P.L. 2009. High-resolution Holocene climate record from Maxwell Bay, South Shetland Islands, Antarctica. Geological Society of America Bulletin, 121, 1711–1725.CrossRefGoogle Scholar
Minzoni, R.T., Anderson, J.B., Fernandez, R. & Wellner, J.S. 2015. Marine record of Holocene climate, ocean, and cryosphere interactions: Herbert Sound, James Ross Island, Antarctica. Quaternary Science Reviews, 129, 239–259.Google Scholar
Rosqvist, G.C. & Schuber, P. 2003. Millennial-scale climate changes on South Georgia, Southern Ocean. Quaternary Research, 59, 470–475.Google Scholar
Schmidt, R., Mäusbacher, R. & Müller, J. 1990. Holocene diatom flora and stratigraphy from sediment cores of two Antarctic lakes (King George Island). Journal of Paleolimnology, 3, 55–74.Google Scholar
Shevenell, A.E., Domack, E.W. & Kernan, G.M. 1996. Record of Holocene palaeoclimate change along the Antarctic Peninsula: evidence from glacial marine sediments, Lallemand Fjord. Papers and Proceedings of the Royal Society of Tasmania, 130, 55–64.Google Scholar
Simms, A.R., DeWitt, R., Kouremenos, P. & Drewry, A.M. 2011a. A new approach to reconstructing sea levels in Antarctica using optically stimulated luminescence of cobble surfaces. Quaternary Geochronology, 6, 50–60.Google Scholar
Simms, A.R., Milliken, K.T., Anderson, J.B. & Wellner, J.S. 2011b. The marine record of deglaciation of the South Shetland Islands, Antarctica since the Last Glacial Maximum. Quaternary Science Reviews, 30, 1583–1601.Google Scholar
Smith, L.M. & Andrews, J.T. 2000. Sediment characteristics in iceberg dominated fjords, Kangerlussuaq region, East Greenland. Sedimentary Geology, 130, 11–25.Google Scholar
Sun, L.G., Liu, X.D., Yin, X.B., Xie, Z.Q. & Zhao, J.L. 2005. Sediments in palaeo-notches: potential proxy records for palaeoclimatic changes in Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 218, 175–193.Google Scholar
Sun, L.G., Liu, X.D., Yin, X.B., Zhu, R.B., Xie, Z.Q. & Wang, Y.H. 2004. A 1,500-year record of Antarctic seal populations in response to climate change. Polar Biology, 27, 495–501.Google Scholar
Syvitski, J.P.M., Burrell, D.C. & Skei, J.M. 2012. Fjords: processes and products. New York, NY: Springer, 215 pp.Google Scholar
Tatur, A., del Valle, R., Barczuk, A. & Martinez-Macchiavello, J. 2004. Records of Holocene environmental changes in terrestrial sedimentary deposits on King George Island, Antarctica: a critical review. Ocean and Polar Research, 26, 531–537.Google Scholar
Thiry, M. 2000. Palaeoclimatic interpretation of clay minerals in marine deposits: an outlook from the continental origin. Earth-Science Reviews, 49, 201–221.Google Scholar
Udden, J.A. 1914. Mechanical composition of clastic sediments. Geological Society of America Bulletin, 25, 655–744.Google 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 Holocene relative sea level curve for the South Shetland Islands, Antarctica. Quaternary Science Reviews, 30, 3152–3170.Google Scholar
Wentworth, C.K. 1922. A scale of grade and class terms for clastic sediments. Journal of Geology, 30, 377–392.Google Scholar
Yan, Q. & Xu, S. 1987. Recent Yangtze Delta deposits. Shanghai: East China Normal University Press, 68–75.Google Scholar
Yoon, H.I., Park, B.-K., Kim, Y. & Kim, D. 2000. Glaciomarine sedimentation and its paleoceanographic implications along the fjord margins in the South Shetland Islands, Antarctica during the last 6000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 157, 189–211.Google Scholar
Zhou, X., Sun, L.G., Huang, W., Cheng, W.H. & Jia, N. 2012. Precipitation in the Yellow River drainage basin and East Asian monsoon strength on a decadal time scale. Quaternary Research, 78, 486–491.CrossRefGoogle Scholar