Articles | Volume 12, issue 8
https://doi.org/10.5194/bg-12-2411-2015
© Author(s) 2015. 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-12-2411-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
24 Apr 2015
Research article |
| 24 Apr 2015
Reconciling single-chamber Mg / Ca with whole-shell δ18O in surface to deep-dwelling planktonic foraminifera from the Mozambique Channel
J. Steinhardt
CORRESPONDING AUTHOR
Department of Geology and Chemical Oceanography, NIOZ Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790 AB Den Burg, the Netherlands
C. Cléroux
Department of Geology and Chemical Oceanography, NIOZ Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790 AB Den Burg, the Netherlands
L. J. de Nooijer
Department of Geology and Chemical Oceanography, NIOZ Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790 AB Den Burg, the Netherlands
G.-J. Brummer
Department of Geology and Chemical Oceanography, NIOZ Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790 AB Den Burg, the Netherlands
Faculty of Earth- and Life Sciences, VU University Amsterdam, de Boelelaan 1085, 1081 HV Amsterdam, the Netherlands
R. Zahn
Institució Catalana de Recerca i Estudis Avançats (ICREA) and Institut de Ciència i Tecnologia Ambientals, Departament de Física, Universitat Autònoma de Barcelona, Cerdanyola del Vallès, Spain
G. Ganssen
Faculty of Earth- and Life Sciences, VU University Amsterdam, de Boelelaan 1085, 1081 HV Amsterdam, the Netherlands
G.-J. Reichart
Department of Geology and Chemical Oceanography, NIOZ Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790 AB Den Burg, the Netherlands
Department of Earth Sciences, Faculty of Geosciences, Utrecht University, P.O. Box 80021, 3508TA Utrecht, the Netherlands
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Cited
12 citations as recorded by crossref.
- 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
- Stable oxygen isotopes in planktonic foraminifera from surface sediments in the California Current system A. Sánchez et al. 10.1016/j.marmicro.2022.102127
- Calcification depth of deep-dwelling planktonic foraminifera from the eastern North Atlantic constrained by stable oxygen isotope ratios of shells from stratified plankton tows A. Rebotim et al. 10.5194/jm-38-113-2019
- Assessing the impact of diagenesis on foraminiferal geochemistry from a low latitude, shallow-water drift deposit S. Stainbank et al. 10.1016/j.epsl.2020.116390
- High‐Resolution Mg/Ca and δ18O Patterns in Modern Neogloboquadrina pachyderma From the Fram Strait and Irminger Sea C. Livsey et al. 10.1029/2020PA003969
- The vertical calcification mode of planktonic foraminifera in the Western Pacific Warm Pool Z. Yu et al. 10.1016/j.palaeo.2024.112454
- Mg∕Ca, Sr∕Ca and stable isotopes from the planktonic foraminifera <i>T. sacculifer</i>: testing a multi-proxy approach for inferring paleotemperature and paleosalinity D. Dissard et al. 10.5194/bg-18-423-2021
- Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei J. Fehrenbacher et al. 10.1038/ncomms15441
- Individual Migration Pathways of Modern Planktic Foraminifers: Chamber-by-Chamber Assessment of Stable Isotopes H. Takagi et al. 10.2517/2015PR036
- Stable Oxygen Isotope Composition Is Biased by Shell Calcification Intensity in Planktonic Foraminifera M. Weinkauf et al. 10.1029/2020PA003941
- Horizontal and vertical distributions of planktic foraminifera in the subarctic Pacific S. Iwasaki et al. 10.1016/j.marmicro.2016.12.001
- 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
12 citations as recorded by crossref.
- 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
- Stable oxygen isotopes in planktonic foraminifera from surface sediments in the California Current system A. Sánchez et al. 10.1016/j.marmicro.2022.102127
- Calcification depth of deep-dwelling planktonic foraminifera from the eastern North Atlantic constrained by stable oxygen isotope ratios of shells from stratified plankton tows A. Rebotim et al. 10.5194/jm-38-113-2019
- Assessing the impact of diagenesis on foraminiferal geochemistry from a low latitude, shallow-water drift deposit S. Stainbank et al. 10.1016/j.epsl.2020.116390
- High‐Resolution Mg/Ca and δ18O Patterns in Modern Neogloboquadrina pachyderma From the Fram Strait and Irminger Sea C. Livsey et al. 10.1029/2020PA003969
- The vertical calcification mode of planktonic foraminifera in the Western Pacific Warm Pool Z. Yu et al. 10.1016/j.palaeo.2024.112454
- Mg∕Ca, Sr∕Ca and stable isotopes from the planktonic foraminifera <i>T. sacculifer</i>: testing a multi-proxy approach for inferring paleotemperature and paleosalinity D. Dissard et al. 10.5194/bg-18-423-2021
- Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei J. Fehrenbacher et al. 10.1038/ncomms15441
- Individual Migration Pathways of Modern Planktic Foraminifers: Chamber-by-Chamber Assessment of Stable Isotopes H. Takagi et al. 10.2517/2015PR036
- Stable Oxygen Isotope Composition Is Biased by Shell Calcification Intensity in Planktonic Foraminifera M. Weinkauf et al. 10.1029/2020PA003941
- Horizontal and vertical distributions of planktic foraminifera in the subarctic Pacific S. Iwasaki et al. 10.1016/j.marmicro.2016.12.001
- 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
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Short summary
In this paper we present, for the first time, results from single-chamber Mg/Ca analyses combined with single-shell δ18O and δ13C for four planktonic foraminiferal species from a sediment trap in the Mozambique Channel. Eddy-induced hydrographic variability is reflected in test carbonate chemistry of these different species. A species-specific depth-resolved mass balance model confirms distinctive migration and calcification patterns for each species as a function of hydrography.
In this paper we present, for the first time, results from single-chamber Mg/Ca analyses...
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