Articles | Volume 16, issue 2
https://doi.org/10.5194/bg-16-643-2019
© 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-16-643-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth
Hilde Pracht
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Sciences, Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV,
Amsterdam, the Netherlands
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Sciences, Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV,
Amsterdam, the Netherlands
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA-CNRS-UVSQ, Université Paris-Saclay, 91191 Gif-sur-Yvette, France
Frank J. C. Peeters
Earth and Climate Cluster, Department of Earth Sciences, Faculty of
Sciences, Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV,
Amsterdam, the Netherlands
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16 citations as recorded by crossref.
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- New Calcium Carbonate Nano‐particulate Pressed Powder Pellet (NFHS‐2‐NP) for LA‐ICP‐OES, LA‐(MC)‐ICP‐MS and µXRF W. Boer et al. 10.1111/ggr.12425
- Seasonal and vertical distribution of living planktonic foraminifera in the western tropical Pacific Ocean R. Kim et al. 10.1016/j.dsr.2023.104159
- 2D geochemical imaging of biogenic marine carbonates using LA-TOF-ICP-MS at 1 and 2 μm pixel resolution C. Standish et al. 10.1016/j.chemgeo.2024.122438
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- Population dynamics and reproduction strategies of planktonic foraminifera in the open ocean J. Meilland et al. 10.5194/bg-18-5789-2021
- 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
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- Molluscan isotope sclerochronology in marine palaeoclimatology: Taxa, technique and timespan issues A. Johnson et al. 10.1016/j.quascirev.2024.109068
- The in situ Mg/Ca ratios of planktonic foraminifera shells in the northeastern South China Sea: an attempt to get efficient and reliable proxies G. Zhang et al. 10.1016/j.dsr.2025.104553
- Field Testing the Fidelity of δ18O and δ13C in Reconstructing Upper Ocean Hydrography F. Mekik & I. Winkelstern 10.1029/2020PA003880
- Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth H. Pracht et al. 10.5194/bg-16-643-2019
15 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
- Leeuwin current dynamics in the SE Indian Ocean and implications for regional surface hydrography since the latest Miocene: Results from ODP Site 763A R. Palei et al. 10.1016/j.gloplacha.2024.104459
- New Calcium Carbonate Nano‐particulate Pressed Powder Pellet (NFHS‐2‐NP) for LA‐ICP‐OES, LA‐(MC)‐ICP‐MS and µXRF W. Boer et al. 10.1111/ggr.12425
- Seasonal and vertical distribution of living planktonic foraminifera in the western tropical Pacific Ocean R. Kim et al. 10.1016/j.dsr.2023.104159
- 2D geochemical imaging of biogenic marine carbonates using LA-TOF-ICP-MS at 1 and 2 μm pixel resolution C. Standish et al. 10.1016/j.chemgeo.2024.122438
- Relationship between individual chamber and whole shell Mg/Ca ratios in Trilobatus sacculifer and implications for individual foraminifera palaeoceanographic reconstructions G. Rustic et al. 10.1038/s41598-020-80673-8
- Testing the effect of bioturbation and species abundance upon discrete-depth individual foraminifera analysis B. Lougheed & B. Metcalfe 10.5194/bg-19-1195-2022
- The Influence of Geochemical Variation Among Globigerinoides ruber Individuals on Paleoceanographic Reconstructions L. Kearns et al. 10.1029/2022PA004549
- Oxygen Isotope Variability of Planktonic Foraminifera Provide Clues to Past Upper Ocean Seasonal Variability B. Metcalfe et al. 10.1029/2018PA003475
- Population dynamics and reproduction strategies of planktonic foraminifera in the open ocean J. Meilland et al. 10.5194/bg-18-5789-2021
- 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
- The vertical calcification mode of planktonic foraminifera in the Western Pacific Warm Pool Z. Yu et al. 10.1016/j.palaeo.2024.112454
- Molluscan isotope sclerochronology in marine palaeoclimatology: Taxa, technique and timespan issues A. Johnson et al. 10.1016/j.quascirev.2024.109068
- The in situ Mg/Ca ratios of planktonic foraminifera shells in the northeastern South China Sea: an attempt to get efficient and reliable proxies G. Zhang et al. 10.1016/j.dsr.2025.104553
- Field Testing the Fidelity of δ18O and δ13C in Reconstructing Upper Ocean Hydrography F. Mekik & I. Winkelstern 10.1029/2020PA003880
Discussed (final revised paper)
Latest update: 29 Jul 2025
Short summary
In palaeoceanography the shells of single-celled foraminifera are routinely used as proxies to reconstruct the temperature, salinity and circulation of the ocean in the past. Traditionally a number of specimens were pooled for a single stable isotope measurement; however, technical advances now mean that a single shell or chamber of a shell can be measured individually. Three different hypotheses regarding foraminiferal biology and ecology were tested using this approach.
In palaeoceanography the shells of single-celled foraminifera are routinely used as proxies to...
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