Articles | Volume 12, issue 6
https://doi.org/10.5194/bg-12-1733-2015
© 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-12-1733-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Oxygen and carbon isotope composition of modern planktic foraminifera and near-surface waters in the Fram Strait (Arctic Ocean) – a case study
T. Pados
CORRESPONDING AUTHOR
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
R. F. Spielhagen
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
Academy of Sciences, Humanities, and Literature Mainz, Mainz, Germany
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
M. Segl
MARUM – Center for Marine Environmental Sciences, Bremen, Germany
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Cited
16 citations as recorded by crossref.
- Sea surface density gradients in the Nordic Seas during the Holocene as revealed by paired microfossil and isotope proxies N. Van Nieuwenhove et al. 10.1002/2015PA002815
- A solution for constraining past marine Polar Amplification A. Morley et al. 10.1038/s41467-024-53424-w
- Upper-ocean flux of biogenic calcite produced by the Arctic planktonic foraminiferaNeogloboquadrina pachyderma F. Tell et al. 10.5194/bg-19-4903-2022
- Ice-ocean interactions at the Northeast Greenland Ice stream (NEGIS) over the past 11,000 years J. Lloyd et al. 10.1016/j.quascirev.2023.108068
- Episodic Atlantic Water Inflow Into the Independence Fjord System (Eastern North Greenland) During the Holocene and Last Glacial Period N. Van Nieuwenhove et al. 10.3389/feart.2020.565670
- Marine deposits of the Chuy Formation (Late Pleistocene) and isostatic readjustments in the area of Laguna de Rocha (Uruguay) E. Castiglioni et al. 10.31285/AGRO.26.799
- Deep ocean 14C ventilation age reconstructions from the Arctic Mediterranean reassessed M. Ezat et al. 10.1016/j.epsl.2019.04.027
- Modern planktic foraminifers in the high-latitude ocean R. Schiebel et al. 10.1016/j.marmicro.2017.08.004
- Upper ocean variability off NE Greenland (79°N) since the last glacial maximum reconstructed from stable isotopes in planktic foraminifer morphotypes R. Spielhagen & A. Mackensen 10.1016/j.quascirev.2021.107070
- Development, Productivity, and Seasonality of Living Planktonic Foraminiferal Faunas and Limacina helicina in an Area of Intense Methane Seepage in the Barents Sea S. Ofstad et al. 10.1029/2019JG005387
- The role of Arctic Ocean freshwater during the past 200 ky R. Spielhagen & H. Bauch 10.1007/s41063-015-0013-9
- Environmental variability off NE Greenland (western Fram Strait) during the past 10,600 years M. Zehnich et al. 10.1177/0959683620950393
- Large Sea Surface Temperature, Salinity, and Productivity‐Preservation Changes Preceding the Onset of the Messinian Salinity Crisis in the Eastern Mediterranean Sea I. Vasiliev et al. 10.1029/2018PA003438
- Paleocirculation and Ventilation History of Southern Ocean Sourced Deep Water Masses During the Last 800,000 Years T. Williams et al. 10.1029/2018PA003472
- A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) J. Kim et al. 10.1029/2021GC009750
- The last two millennia: climate, ocean circulation and palaeoproductivity inferred from planktic foraminifera, south-western Svalbard margin K. Zamelczyk et al. 10.33265/polar.v39.3715
16 citations as recorded by crossref.
- Sea surface density gradients in the Nordic Seas during the Holocene as revealed by paired microfossil and isotope proxies N. Van Nieuwenhove et al. 10.1002/2015PA002815
- A solution for constraining past marine Polar Amplification A. Morley et al. 10.1038/s41467-024-53424-w
- Upper-ocean flux of biogenic calcite produced by the Arctic planktonic foraminiferaNeogloboquadrina pachyderma F. Tell et al. 10.5194/bg-19-4903-2022
- Ice-ocean interactions at the Northeast Greenland Ice stream (NEGIS) over the past 11,000 years J. Lloyd et al. 10.1016/j.quascirev.2023.108068
- Episodic Atlantic Water Inflow Into the Independence Fjord System (Eastern North Greenland) During the Holocene and Last Glacial Period N. Van Nieuwenhove et al. 10.3389/feart.2020.565670
- Marine deposits of the Chuy Formation (Late Pleistocene) and isostatic readjustments in the area of Laguna de Rocha (Uruguay) E. Castiglioni et al. 10.31285/AGRO.26.799
- Deep ocean 14C ventilation age reconstructions from the Arctic Mediterranean reassessed M. Ezat et al. 10.1016/j.epsl.2019.04.027
- Modern planktic foraminifers in the high-latitude ocean R. Schiebel et al. 10.1016/j.marmicro.2017.08.004
- Upper ocean variability off NE Greenland (79°N) since the last glacial maximum reconstructed from stable isotopes in planktic foraminifer morphotypes R. Spielhagen & A. Mackensen 10.1016/j.quascirev.2021.107070
- Development, Productivity, and Seasonality of Living Planktonic Foraminiferal Faunas and Limacina helicina in an Area of Intense Methane Seepage in the Barents Sea S. Ofstad et al. 10.1029/2019JG005387
- The role of Arctic Ocean freshwater during the past 200 ky R. Spielhagen & H. Bauch 10.1007/s41063-015-0013-9
- Environmental variability off NE Greenland (western Fram Strait) during the past 10,600 years M. Zehnich et al. 10.1177/0959683620950393
- Large Sea Surface Temperature, Salinity, and Productivity‐Preservation Changes Preceding the Onset of the Messinian Salinity Crisis in the Eastern Mediterranean Sea I. Vasiliev et al. 10.1029/2018PA003438
- Paleocirculation and Ventilation History of Southern Ocean Sourced Deep Water Masses During the Last 800,000 Years T. Williams et al. 10.1029/2018PA003472
- A Pulse of Meteoric Subsurface Fluid Discharging Into the Chukchi Sea During the Early Holocene Thermal Maximum (EHTM) J. Kim et al. 10.1029/2021GC009750
- The last two millennia: climate, ocean circulation and palaeoproductivity inferred from planktic foraminifera, south-western Svalbard margin K. Zamelczyk et al. 10.33265/polar.v39.3715
Saved (final revised paper)
Latest update: 21 Nov 2024
Short summary
Fossil planktic foraminifera and their geochemical composition are commonly used proxies in palaeoceanography. Our study with living specimens revealed that in the Fram Strait both Neogloboquadrina pachyderma and Turborotalita quinqueloba from the water column have lower δ18O and δ13C values than inorganically precipitated calcite/fossil tests from the sediment surface. These offsets indicate biological influence during calcification and a change of water column properties in the recent past.
Fossil planktic foraminifera and their geochemical composition are commonly used proxies in...
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