Articles | Volume 14, issue 21
https://doi.org/10.5194/bg-14-4905-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-14-4905-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The influence of environmental variability on the biogeography of coccolithophores and diatoms in the Great Calcite Belt
Helen E. K. Smith
CORRESPONDING AUTHOR
National Oceanography Centre, European Way, Southampton, SO14 3ZH,
UK
Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, SO14 3ZH, UK
Alex J. Poulton
National Oceanography Centre, European Way, Southampton, SO14 3ZH,
UK
presently at: The Lyell Centre, Heriot-Watt University, Edinburgh,
EH14 4AS, UK
Rebecca Garley
Bermuda Institute of Ocean Sciences, 17 Biological Station, Ferry
Reach, St. George's GE 01, Bermuda
Jason Hopkins
Bigelow Laboratory for Ocean Sciences, 60 Bigelow Drive, P.O. Box 380,
East Boothbay, Maine 04544, USA
Laura C. Lubelczyk
Bigelow Laboratory for Ocean Sciences, 60 Bigelow Drive, P.O. Box 380,
East Boothbay, Maine 04544, USA
Dave T. Drapeau
Bigelow Laboratory for Ocean Sciences, 60 Bigelow Drive, P.O. Box 380,
East Boothbay, Maine 04544, USA
Sara Rauschenberg
Bigelow Laboratory for Ocean Sciences, 60 Bigelow Drive, P.O. Box 380,
East Boothbay, Maine 04544, USA
Ben S. Twining
Bigelow Laboratory for Ocean Sciences, 60 Bigelow Drive, P.O. Box 380,
East Boothbay, Maine 04544, USA
Nicholas R. Bates
Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, SO14 3ZH, UK
Bermuda Institute of Ocean Sciences, 17 Biological Station, Ferry
Reach, St. George's GE 01, Bermuda
William M. Balch
Bigelow Laboratory for Ocean Sciences, 60 Bigelow Drive, P.O. Box 380,
East Boothbay, Maine 04544, USA
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31 citations as recorded by crossref.
- Two Production Stages of Coccolithophores in Winter as Revealed by Sediment Traps in the Northern South China Sea X. Jin et al. 10.1029/2019JG005070
- Remote sensing algorithms for particulate inorganic carbon (PIC) and the global cycle of PIC W. Balch & C. Mitchell 10.1016/j.earscirev.2023.104363
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- Factors controlling coccolithophore biogeography in the Southern Ocean C. Nissen et al. 10.5194/bg-15-6997-2018
- Haplo-diplontic life cycle expands coccolithophore niche J. de Vries et al. 10.5194/bg-18-1161-2021
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- Environmental Drivers of Coccolithophore Growth in the Pacific Sector of the Southern Ocean H. Oliver et al. 10.1029/2023GB007751
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- The role of biota in the Southern Ocean carbon cycle P. Boyd et al. 10.1038/s43017-024-00531-3
- Enhanced Carbonate Counter Pump and upwelling strengths in the Indian sector of the Southern Ocean during MIS 11 M. Brandon et al. 10.1016/j.quascirev.2022.107556
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- The Phenomenon Of Emiliania Huxleyi In Aspects Of Global Climate And The Ecology Of The World Ocean D. Pozdnyakov et al. 10.24057/2071-9388-2020-214
- Distribution of coccoliths in surface sediments across the Drake Passage and calcification of <i>Emiliania huxleyi</i> morphotypes N. Vollmar et al. 10.5194/bg-19-585-2022
- Distribution of planktonic biogenic carbonate organisms in the Southern Ocean south of Australia: a baseline for ocean acidification impact assessment T. Trull et al. 10.5194/bg-15-31-2018
- The Earth‐Observing Aqua Satellite Mission: 20 Years and Counting C. Parkinson 10.1029/2022EA002481
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Discussed (final revised paper)
Latest update: 03 Oct 2024
Short summary
The Great Calcite Belt (GCB), a region of high calcite concentration from coccolithophores, covers 60 % of the Southern Ocean area. We examined the influence of temperature, macronutrients, and carbonate chemistry on the distribution of mineralizing phytoplankton in the GCB. Coccolithophores occupy a niche in the Southern Ocean after the diatom spring bloom depletes silicic acid. No single environmental variable holds a dominant influence over phytoplankton biogeography in summer GCB conditions.
The Great Calcite Belt (GCB), a region of high calcite concentration from coccolithophores,...
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