Articles | Volume 16, issue 16
https://doi.org/10.5194/bg-16-3267-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-16-3267-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Temporal variability in foraminiferal morphology and geochemistry at the West Antarctic Peninsula: a sediment trap study
Anna Mikis
School of Earth and Ocean Sciences, Cardiff University, Main Building, Cardiff, CF10 3AT, UK
Katharine R. Hendry
CORRESPONDING AUTHOR
School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK
Jennifer Pike
School of Earth and Ocean Sciences, Cardiff University, Main Building, Cardiff, CF10 3AT, UK
Daniela N. Schmidt
School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK
Kirsty M. Edgar
School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Victoria Peck
British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK
Frank J. C. Peeters
Department of Earth Sciences, Faculty of Sciences, Vrije Universiteit Amsterdam, De Boelelaan 1085, 1081 HV, Amsterdam, the Netherlands
Melanie J. Leng
NERC Isotope Geosciences Facilities, British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK
Centre for Environmental Geochemistry, School of Biosciences, Sutton Bonington Campus, University of Nottingham, Loughborough, LE12 5RD, UK
Michael P. Meredith
British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK
Chloe L. C. Jones
School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK
previously published under the name Chloe L. Todd
Sharon Stammerjohn
Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO 80303, USA
Hugh Ducklow
Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY 10964-1000, USA
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12 citations as recorded by crossref.
- Modal shift in North Atlantic seasonality during the last deglaciation G. Brummer et al. 10.5194/cp-16-265-2020
- Last Glacial Maximum to Holocene paleoceanography of the northwestern Ross Sea inferred from sediment core geochemistry and micropaleontology at Hallett Ridge R. Melis et al. 10.5194/jm-40-15-2021
- Tracking Southern Ocean Sea Ice Extent With Winter Water: A New Method Based on the Oxygen Isotopic Signature of Foraminifera D. Lund et al. 10.1029/2020PA004095
- A proxy modelling approach to assess the potential of extracting ENSO signal from tropical Pacific planktonic foraminifera B. Metcalfe et al. 10.5194/cp-16-885-2020
- Environmental and Oceanographic Conditions at the Continental Margin of the Central Basin, Northwestern Ross Sea (Antarctica) Since the Last Glacial Maximum F. Torricella et al. 10.3390/geosciences11040155
- Antarctic Sea Ice Proxies from Marine and Ice Core Archives Suitable for Reconstructing Sea Ice over the Past 2000 Years E. Thomas et al. 10.3390/geosciences9120506
- The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal Z. Yu et al. 10.1016/j.gca.2022.04.014
- Developmental plasticity in deep time: a window to population ecological inference A. Brombacher et al. 10.1017/pab.2022.26
- Foraminifer and Ostracod Occurrence in a Cool-Water Carbonate Factory of the Cape Adare (Ross Sea, Antarctica): A Key Lecture for the Climatic and Oceanographic Variations in the Last 30,000 Years R. Melis & G. Salvi 10.3390/geosciences10100413
- Paleoenvironmental changes related to the variations of the sea-ice cover during the Late Holocene in an Antarctic fjord (Edisto Inlet, Ross Sea) inferred by foraminiferal association G. Galli et al. 10.5194/jm-42-95-2023
- Continuous reproduction of planktonic foraminifera in laboratory culture J. Meilland et al. 10.1111/jeu.13022
- The FORCIS database: A global census of planktonic Foraminifera from ocean waters S. Chaabane et al. 10.1038/s41597-023-02264-2
11 citations as recorded by crossref.
- Modal shift in North Atlantic seasonality during the last deglaciation G. Brummer et al. 10.5194/cp-16-265-2020
- Last Glacial Maximum to Holocene paleoceanography of the northwestern Ross Sea inferred from sediment core geochemistry and micropaleontology at Hallett Ridge R. Melis et al. 10.5194/jm-40-15-2021
- Tracking Southern Ocean Sea Ice Extent With Winter Water: A New Method Based on the Oxygen Isotopic Signature of Foraminifera D. Lund et al. 10.1029/2020PA004095
- A proxy modelling approach to assess the potential of extracting ENSO signal from tropical Pacific planktonic foraminifera B. Metcalfe et al. 10.5194/cp-16-885-2020
- Environmental and Oceanographic Conditions at the Continental Margin of the Central Basin, Northwestern Ross Sea (Antarctica) Since the Last Glacial Maximum F. Torricella et al. 10.3390/geosciences11040155
- Antarctic Sea Ice Proxies from Marine and Ice Core Archives Suitable for Reconstructing Sea Ice over the Past 2000 Years E. Thomas et al. 10.3390/geosciences9120506
- The influence of seasonal calcification depth change on the planktonic foraminiferal stable oxygen isotope signal Z. Yu et al. 10.1016/j.gca.2022.04.014
- Developmental plasticity in deep time: a window to population ecological inference A. Brombacher et al. 10.1017/pab.2022.26
- Foraminifer and Ostracod Occurrence in a Cool-Water Carbonate Factory of the Cape Adare (Ross Sea, Antarctica): A Key Lecture for the Climatic and Oceanographic Variations in the Last 30,000 Years R. Melis & G. Salvi 10.3390/geosciences10100413
- Paleoenvironmental changes related to the variations of the sea-ice cover during the Late Holocene in an Antarctic fjord (Edisto Inlet, Ross Sea) inferred by foraminiferal association G. Galli et al. 10.5194/jm-42-95-2023
- Continuous reproduction of planktonic foraminifera in laboratory culture J. Meilland et al. 10.1111/jeu.13022
1 citations as recorded by crossref.
Latest update: 10 Oct 2024
Short summary
Antarctic marine calcifying organisms are threatened by regional climate change and ocean acidification. Future projections of regional carbonate production are challenging due to the lack of historical data combined with complex climate variability. We present a 6-year record of flux, morphology and geochemistry of an Antarctic planktonic foraminifera, which shows that their growth is most sensitive to sea ice dynamics and is linked with the El Niño–Southern Oscillation.
Antarctic marine calcifying organisms are threatened by regional climate change and ocean...
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