Articles | Volume 12, issue 15
https://doi.org/10.5194/bg-12-4781-2015
© 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-12-4781-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
07 Aug 2015
Research article |
| 07 Aug 2015
Late Pleistocene glacial–interglacial shell-size–isotope variability in planktonic foraminifera as a function of local hydrography
Earth and Climate Cluster, Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV, the Netherlands
W. Feldmeijer
Earth and Climate Cluster, Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV, the Netherlands
M. de Vringer-Picon
Earth and Climate Cluster, Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV, the Netherlands
G.-J. A. Brummer
Department of Geology and Chemical Oceanography, NIOZ Royal Netherlands Institute for Sea Research, Landsdiep 4, 1797 SZ t' Horntje, Texel, the Netherlands
Earth and Climate Cluster, Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV, the Netherlands
F. J. C. Peeters
Earth and Climate Cluster, Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV, the Netherlands
G. M. Ganssen
Earth and Climate Cluster, Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV, the Netherlands
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Cited
15 citations as recorded by crossref.
- Temperature-dependent ocean–atmosphere equilibration of carbon isotopes in surface and intermediate waters over the deglaciation J. Lynch-Stieglitz et al. 10.1016/j.epsl.2018.11.024
- Marine sediment cores database for the Mediterranean Basin: a tool for past climatic and environmental studies I. Alberico et al. 10.1515/geo-2017-0019
- SEAMUS (v1.20): a Δ<sup>14</sup>C-enabled, single-specimen sediment accumulation simulator B. Lougheed 10.5194/gmd-13-155-2020
- High‐precision stable isotope analysis of <5 μg CaCO3 samples by continuous‐flow mass spectrometry H. Vonhof et al. 10.1002/rcm.8878
- Oxygen Isotope Variability of Planktonic Foraminifera Provide Clues to Past Upper Ocean Seasonal Variability B. Metcalfe et al. 10.1029/2018PA003475
- 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
- 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
- Productivity Evolution in the South Brazilian Bight During the Last 40,000 Years L. Pereira et al. 10.1029/2018PA003406
- Moving beyond the age–depth model paradigm in deep-sea palaeoclimate archives: dual radiocarbon and stable isotope analysis on single foraminifera B. Lougheed et al. 10.5194/cp-14-515-2018
- The Miocene Climatic Optimum at the interface of epicontinental sea and large continent: A case study from the Middle Miocene of the Eastern Paratethys Y. Vernyhorova et al. 10.1016/j.marmicro.2023.102231
- Advances in planktonic foraminifer research: New perspectives for paleoceanography R. Schiebel et al. 10.1016/j.revmic.2018.10.001
- Mg ∕ Ca and <i xmlns="">δ</i><sup>18</sup>O in living planktic foraminifers from the Caribbean, Gulf of Mexico and Florida Straits A. Jentzen et al. 10.5194/bg-15-7077-2018
- Deciphering the Variability in Mg/Ca and Stable Oxygen Isotopes of Individual Foraminifera J. Groeneveld et al. 10.1029/2018PA003533
- Tracing shifts of oceanic fronts using the cryptic diversity of the planktonic foraminifera Globorotalia inflata R. Morard et al. 10.1002/2016PA002977
14 citations as recorded by crossref.
- Temperature-dependent ocean–atmosphere equilibration of carbon isotopes in surface and intermediate waters over the deglaciation J. Lynch-Stieglitz et al. 10.1016/j.epsl.2018.11.024
- Marine sediment cores database for the Mediterranean Basin: a tool for past climatic and environmental studies I. Alberico et al. 10.1515/geo-2017-0019
- SEAMUS (v1.20): a Δ<sup>14</sup>C-enabled, single-specimen sediment accumulation simulator B. Lougheed 10.5194/gmd-13-155-2020
- High‐precision stable isotope analysis of <5 μg CaCO3 samples by continuous‐flow mass spectrometry H. Vonhof et al. 10.1002/rcm.8878
- Oxygen Isotope Variability of Planktonic Foraminifera Provide Clues to Past Upper Ocean Seasonal Variability B. Metcalfe et al. 10.1029/2018PA003475
- 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
- 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
- Productivity Evolution in the South Brazilian Bight During the Last 40,000 Years L. Pereira et al. 10.1029/2018PA003406
- Moving beyond the age–depth model paradigm in deep-sea palaeoclimate archives: dual radiocarbon and stable isotope analysis on single foraminifera B. Lougheed et al. 10.5194/cp-14-515-2018
- The Miocene Climatic Optimum at the interface of epicontinental sea and large continent: A case study from the Middle Miocene of the Eastern Paratethys Y. Vernyhorova et al. 10.1016/j.marmicro.2023.102231
- Advances in planktonic foraminifer research: New perspectives for paleoceanography R. Schiebel et al. 10.1016/j.revmic.2018.10.001
- Mg ∕ Ca and <i xmlns="">δ</i><sup>18</sup>O in living planktic foraminifers from the Caribbean, Gulf of Mexico and Florida Straits A. Jentzen et al. 10.5194/bg-15-7077-2018
- Deciphering the Variability in Mg/Ca and Stable Oxygen Isotopes of Individual Foraminifera J. Groeneveld et al. 10.1029/2018PA003533
Saved (preprint)
Latest update: 24 Apr 2024
Short summary
Iron biogeochemical budgets during the natural ocean fertilisation experiment KEOPS-2 showed that complex circulation and transport pathways were responsible for differences in the mode and strength of iron supply, with vertical supply dominant on the plateau and lateral supply dominant in the plume. The exchange of iron between dissolved, biogenic and lithogenic pools was highly dynamic, resulting in a decoupling of iron supply and carbon export and controlling the efficiency of fertilisation.
Iron biogeochemical budgets during the natural ocean fertilisation experiment KEOPS-2 showed...
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