Articles | Volume 11, issue 9
https://doi.org/10.5194/gmd-11-3587-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-11-3587-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model description paper
| 
03 Sep 2018
Model description paper |
| 03 Sep 2018
| 03 Sep 2018
FAME (v1.0): a simple module to simulate the effect of planktonic foraminifer species-specific habitat on their oxygen isotopic content
Didier M. Roche
CORRESPONDING AUTHOR
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France
Vrije Universiteit Amsterdam, Faculty of Science, Cluster Earth and Climate, de Boelelaan 1085, Amsterdam, the Netherlands
Invited contribution by Didier M. Roche, recipient of the EGU CL Division Outstanding Young Scientists Award 2012.
Claire Waelbroeck
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France
Brett Metcalfe
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France
Vrije Universiteit Amsterdam, Faculty of Science, Cluster Earth and Climate, de Boelelaan 1085, Amsterdam, the Netherlands
Thibaut Caley
EPOC, UMR 5805, CNRS, University Bordeaux, Pessac, France
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Cited
15 citations as recorded by crossref.
- On the combination of the planktonic foraminiferal Mg/Ca, clumped (Δ47) and conventional (δ18O) stable isotope paleothermometers in palaeoceanographic studies M. Peral et al. 10.1016/j.gca.2022.10.030
- Assessing the impact of bioturbation on sedimentary isotopic records through numerical models D. Hülse et al. 10.1016/j.earscirev.2022.104213
- Sedproxy: a forward model for sediment-archived climate proxies A. Dolman & T. Laepple 10.5194/cp-14-1851-2018
- Empirical estimate of the signal content of Holocene temperature proxy records M. Reschke et al. 10.5194/cp-15-521-2019
- Modal shift in North Atlantic seasonality during the last deglaciation G. Brummer et al. 10.5194/cp-16-265-2020
- 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
- Testing the effect of bioturbation and species abundance upon discrete-depth individual foraminifera analysis B. Lougheed & B. Metcalfe 10.5194/bg-19-1195-2022
- Oxygen Isotope Variability of Planktonic Foraminifera Provide Clues to Past Upper Ocean Seasonal Variability B. Metcalfe et al. 10.1029/2018PA003475
- The Foraminiferal Response to Climate Stressors Project: Tracking the Community Response of Planktonic Foraminifera to Historical Climate Change T. de Garidel-Thoron et al. 10.3389/fmars.2022.827962
- Deciphering the Variability in Mg/Ca and Stable Oxygen Isotopes of Individual Foraminifera J. Groeneveld et al. 10.1029/2018PA003533
- Testing the reliability of global surface temperature reconstructions of the Last Glacial Cycle with pseudo-proxy experiments J. Baudouin et al. 10.5194/cp-21-381-2025
- 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
- Revisiting Oxygen‐18 and Clumped Isotopes in Planktic and Benthic Foraminifera M. Daëron & W. Gray 10.1029/2023PA004660
- SEAMUS (v1.20): a Δ14C-enabled, single-specimen sediment accumulation simulator B. Lougheed 10.5194/gmd-13-155-2020
- USING SEDIMENTOLOGICAL PRIORS TO IMPROVE 14C CALIBRATION OF BIOTURBATED SEDIMENT ARCHIVES B. Lougheed 10.1017/RDC.2021.116
15 citations as recorded by crossref.
- On the combination of the planktonic foraminiferal Mg/Ca, clumped (Δ47) and conventional (δ18O) stable isotope paleothermometers in palaeoceanographic studies M. Peral et al. 10.1016/j.gca.2022.10.030
- Assessing the impact of bioturbation on sedimentary isotopic records through numerical models D. Hülse et al. 10.1016/j.earscirev.2022.104213
- Sedproxy: a forward model for sediment-archived climate proxies A. Dolman & T. Laepple 10.5194/cp-14-1851-2018
- Empirical estimate of the signal content of Holocene temperature proxy records M. Reschke et al. 10.5194/cp-15-521-2019
- Modal shift in North Atlantic seasonality during the last deglaciation G. Brummer et al. 10.5194/cp-16-265-2020
- 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
- Testing the effect of bioturbation and species abundance upon discrete-depth individual foraminifera analysis B. Lougheed & B. Metcalfe 10.5194/bg-19-1195-2022
- Oxygen Isotope Variability of Planktonic Foraminifera Provide Clues to Past Upper Ocean Seasonal Variability B. Metcalfe et al. 10.1029/2018PA003475
- The Foraminiferal Response to Climate Stressors Project: Tracking the Community Response of Planktonic Foraminifera to Historical Climate Change T. de Garidel-Thoron et al. 10.3389/fmars.2022.827962
- Deciphering the Variability in Mg/Ca and Stable Oxygen Isotopes of Individual Foraminifera J. Groeneveld et al. 10.1029/2018PA003533
- Testing the reliability of global surface temperature reconstructions of the Last Glacial Cycle with pseudo-proxy experiments J. Baudouin et al. 10.5194/cp-21-381-2025
- 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
- Revisiting Oxygen‐18 and Clumped Isotopes in Planktic and Benthic Foraminifera M. Daëron & W. Gray 10.1029/2023PA004660
- SEAMUS (v1.20): a Δ14C-enabled, single-specimen sediment accumulation simulator B. Lougheed 10.5194/gmd-13-155-2020
- USING SEDIMENTOLOGICAL PRIORS TO IMPROVE 14C CALIBRATION OF BIOTURBATED SEDIMENT ARCHIVES B. Lougheed 10.1017/RDC.2021.116
Latest update: 09 May 2025
Short summary
The oxygen-18 signal recorded in fossil planktonic foraminifers has been used for over 50 years in many geoscience applications. However, different planktonic foraminifer species from the same sediment core generally yield distinct oxygen-18 signals, as a consequence of their specific living habitat in the water column and along the year. To explicitly take into account this variability for five common planktonic species, we developed the portable module FAME (Foraminifers As Modeled Entities).
The oxygen-18 signal recorded in fossil planktonic foraminifers has been used for over 50 years...
