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Detection of phytoplankton blooms in Antarctic coastal water with an online mooring system during summer 2010/11

Published online by Cambridge University Press:  09 September 2013

Yuxin Ma ,
Fang Zhang ,
Haizhen Yang ,
Ling Lin  and
Jianfeng He
Yuxin Ma
Affiliation:
College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China The Key Laboratory for Polar Science of State Ocean Administration, Polar Research Institute of China, Shanghai 200136, China
Fang Zhang
Affiliation:
The Key Laboratory for Polar Science of State Ocean Administration, Polar Research Institute of China, Shanghai 200136, China
Haizhen Yang
Affiliation:
College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China
Ling Lin
Affiliation:
The Key Laboratory for Polar Science of State Ocean Administration, Polar Research Institute of China, Shanghai 200136, China
Jianfeng He*
Affiliation:
The Key Laboratory for Polar Science of State Ocean Administration, Polar Research Institute of China, Shanghai 200136, China
*
*Corresponding author: hejianfeng@pric.gov.cn
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Abstract

In order to continuously monitor the phytoplankton growth in Antarctic coastal waters, an online mooring system was deployed in Great Wall Bay (unofficial name), King George Island, and both chlorophyll a (chl a) concentrations and environmental variables were monitored in a period between December 2010 and March 2011. Water temperatures showed a significant increasing trend (0.27–2.52°C), whereas the salinities displayed a decreasing trend (34.19–33.86). In general, phytoplankton biomass accumulated from mid-December and two significant blooms developed in January (3.18 μg l-1 and 4.75 μg l-1) and were then maintained at a relatively high level, with a transient bloom in late February (4.93 μg l-1). Sea-ice meltwater and terrestrial freshwater input caused by the increase of temperature played an important role in inducing phytoplankton blooms in early summer. The variation and stratification of temperature and salinity signals in different water layers, without total mixing, suggested lateral intrusion of oceanic waters with alternating levels of temperature and salinity and, presumably, phytoplankton as well. Meanwhile, chl a concentrations initially decreased with an increase in irradiance, indicating the shade-adapted characteristic of phytoplankton in early summer, and then gradually adapted to the increasing irradiance. Our results demonstrated the effectiveness and reliability of the online coastal mooring system for the monitoring of Antarctic coastal phytoplankton bloom and environmental conditions.

Keywords

King George Islandphotosynthetically active radiation (PAR)South Shetland Islandstemperature
Type
Biological Sciences
Information
Antarctic Science , Volume 26 , Issue 3 , June 2014 , pp. 231 - 238
Copyright
Copyright © Antarctic Science Ltd 2013 

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References

Ahn, I.-Y., Chung, H., Kang, J.-S. Kang, S.-H. 1997. Diatom composition and biomass variability in nearshore waters of Maxwell Bay, Antarctica, during the 1992/1993 austral summer. Polar Biology, 17, 123–130.CrossRefGoogle Scholar
Annett, A.L., Carson, D.S., Croata, X., Clarke, A. Ganeshram, R.S. 2010. Seasonal progression of diatom assemblages in surface waters of Ryder Bay, Antarctica. Polar Biology, 33, 13–29.CrossRefGoogle Scholar
Bian, L.G., Ma, Y.F., Lu, C.G. Lu, L.H. 2010. Temperature variations at the Great Wall Station (1985–2008) and Zhongshan Station (1989–2008). Chinese Journal of Polar Research, 22, 1–9.Google Scholar
Chang, K.I., Jun, H.K., Park, G.T. Eo, Y.S. 1990. Oceanographic conditions of Maxwell Bay, King George Island, Antarctica (austral summer 1989). Korean Journal of Polar Research, 1, 27–46.Google Scholar
Clarke, A., Holmes, L.J. White, M.G. 1988. The annual cycle of temperature, chlorophyll and major nutrients at Signy Island, South Orkney Islands, 1969–1982. British Antarctic Survey Bulletin, No. 80, 65–86.Google Scholar
Clarke, A., Meredith, M.P., Wallance, M.I., Brandon, M.A. Thomas, D.N. 2008. Seasonal and interannual variability in temperature, chlorophyll and macronutrients in northern Marguerite Bay, Antarctica. Deep-Sea Research II, 55, 1988–2006.Google Scholar
Clarke, A., Murphy, E.J., Meredith, M.P., King, J.C., Peck, L.S., Barnes, D.K.A. Smith, R.C. 2007. Climate change and the marine ecosystem of the western Antarctic Peninsula. Philosophical Transaction of the Royal Society, B362, 149–166.Google Scholar
Fukuchi, M., Hattori, H., Sasaki, H. Hoshiai, T. 1988. A phytoplankton bloom and associated processes observed with a long-term moored system in Antarctic waters. Marine Ecology Progress Series, 45, 279–288.Google Scholar
Hansen, J., Ruedy, R., Glascoe, J. Sato, M. 1999. GISS analysis of surface temperature change. Journal of Geophysical Research: Atmospheres, 104, 30 997–31 022.Google Scholar
Hewes, C.D., Reiss, C.S. Holm-Hansen, O. 2009. A quantitative analysis of sources for summertime phytoplankton variability over 18 years in the South Shetland Islands (Antarctica) region. Deep-Sea Research I, 56, 1230–1241.Google Scholar
Lange, P.K., Tenenbaum, D.R., De Santis Braga, E. Campos, L.S. 2007. Microphytoplankton assemblages in shallow waters at Admiralty Bay (King George Island, Antarctica) during the summer 2002–2003. Polar Biology, 30, 1483–1492.Google Scholar
Li, B.H. 2004. The subaltern of chlorophyll a maxima in the Great Wall bay and adjacent sea, Antarctica. Chinese Journal of Polar Research, 16, 127–134.Google Scholar
Lips, U., Lips, I., Liblik, T., Kikas, V., Altoja, K., Buhhalko, N. Ruenk, N. 2011. Vertical dynamics of summer phytoplankton in a stratified estuary (Gulf of Finland, Baltic Sea). Ocean Dynamics, 61, 903–915.CrossRefGoogle Scholar
Lizotte, M.P. 2001. The contributions of sea ice algae to Antarctic marine primary production. American Zoologist, 41, 57–73.Google Scholar
Lizotte, M.P. Sullivan, C.W. 1991. Rates of photoadaptation in sea ice diatoms from McMurdo Sound, Antarctica. Journal of Phycology, 27, 367–373.CrossRefGoogle Scholar
Meredith, M.P. King, J.C. 2005. Rapid climate change in the ocean west of the Antarctic Peninsula during the second half of the 20th century. Geophysical Research Letters, 10.1029/2005GL024042.CrossRefGoogle Scholar
Moline, M.A., Claustre, H., Frazer, T., Schofield, O. Vernet, M. 2004. Alteration of the food web along the Antarctic Peninsula in response to a regional warming trend. Global Change Biology, 10, 1973–1980.CrossRefGoogle Scholar
Morgan-Kiss, R.M., Priscu, J.C., Pocock, T., Gudynaite-Savitch, L. Huncr, N.P.A. 2006. Adaptation and acclimation of photosynthetic microorganisms to permanently cold environments. Microbiology and Molecular Biology Reviews, 70, 222–252.CrossRefGoogle ScholarPubMed
Piquet, A.M.-T., Bolhuis, H., Meredith, M.P. Buma, A.G.J. 2011. Shifts in coastal Antarctic marine microbial communities during and after meltwater-related surface stratification. FEMS Microbiology Ecology, 76, 413–427.Google Scholar
Prezelin, B.B. Matlick, H.A. 1980. Time course of photoadaptation in the photosynthesis irradiance relationship of a dinoflagellates exhibiting photosynthetic periodicity. Marine Biology, 58, 85–96.Google Scholar
Reay, D.S., Priddle, J., Nedwell, D.B., Whitehouse, M.J., Ellis-Evans, J.C., Deubert, C. Connelly, D.P. 2001. Regulation by low temperature of phytoplankton growth and nutrient uptake in the Southern Ocean. Marine Ecology Progress Series, 219, 51–64.Google Scholar
Schloss, I.R., Ferreyra, G.A. Diana, R.-P. 2002. Phytoplankton biomass in Antarctic shelf zones: a conceptual model based on Potter Cove, King George Island. Journal of Marine Systems, 36, 129–143.Google Scholar
Smith, R.C., Baker, K.S. Vernet, M. 1998. Seasonal and interannual variability of phytoplankton biomass west of the Antarctic Peninsula. Journal of Marine Systems, 17, 229–243.CrossRefGoogle Scholar
Smith, W.O. Jr,, Asper, V. Tozzi, S., Liu, X. Stammerjohn, S.E. 2011. Surface layer variability in the Ross Sea, Antarctica as assessed by in situ fluorescence measurements. Progress in Oceanography, 88, 28–45.CrossRefGoogle Scholar
Stammerjohn, S.E., Martinson, D.G., Smith, R.C. Iannuzzi, R.A. 2008a. Sea ice in the western Antarctic Peninsula region: spatio-temporal variability from ecological and climate change perspectives. Deep Sea Research II, 55, 2041–2058.Google Scholar
Strutton, P.G., Martz, T.R., Degrandpre, M.D., McGillis, W.R., Drennan, W.M. Boss, E. 2011. Bio-optical observations of the 2004 Labrador Sea phytoplankton bloom. Journal of Geophysical Research: Oceans, 10.1029/2010JC006872.Google Scholar
Tanabe, Y., Kudoh, S., Imura, S. Fukuchi, M. 2008. Phytoplankton blooms under dim and cold conditions in freshwater lakes of East Antarctica. Polar Biology, 31, 199–208.Google Scholar
Thomas, D.N. Dieckmann, G.S. 2002. Antarctic sea ice: a habitat for extremophiles. Science, 295, 641–644.Google Scholar
Vaughan, D.G., Marshall, G.J., Connolley, W.M., Parkinson, C., Mulvaney, R., Hodgson, D.A., King, J.C., Pudsey, C.J. Turner, J. 2003. Recent rapid regional climate warming on the Antarctic Peninsula. Climate Change, 60, 243–274.Google Scholar
Yu, J.L., Li, R.X. Huang, F.P. 1992. A preliminary study on the ecology of the phytoplankton in Great Wall Bay, Antarctica. Antarctic Research, 4, 34–39.Google Scholar