Articles | Volume 16, issue 17
https://doi.org/10.5194/bg-16-3425-2019
© 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-16-3425-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Depth habitat of the planktonic foraminifera Neogloboquadrina pachyderma in the northern high latitudes explained by sea-ice and chlorophyll concentrations
MARUM – Center for Marine Environmental Sciences, Leobener Str. 8,
28359, Bremen, Germany
Lukas Jonkers
MARUM – Center for Marine Environmental Sciences, Leobener Str. 8,
28359, Bremen, Germany
Kerstin Kretschmer
MARUM – Center for Marine Environmental Sciences, Leobener Str. 8,
28359, Bremen, Germany
Jelle Bijma
Section Marine Biogeosciences, Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, Germany
Michal Kucera
MARUM – Center for Marine Environmental Sciences, Leobener Str. 8,
28359, Bremen, Germany
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44 citations as recorded by crossref.
- Life on the ice-edge: Paleoenvironmental significance of the radiolarian species Amphimelissa setosa in the northern hemisphere I. Hernández-Almeida et al. 10.1016/j.quascirev.2020.106565
- Multiproxy investigation of the last 2,000 years BP marine paleoenvironmental record along the western Spitsbergen margin F. Torricella et al. 10.1080/15230430.2022.2123859
- Morphotypical and Geochemical Variations of Planktic Foraminiferal Species in Siberian and Central Arctic Ocean Core Tops M. Prabhakar et al. 10.2113/gsjfr.54.1.1
- Ocean surface and bottom water conditions, iceberg drift and sediment transport on the North Iceland margin during MIS 3 and MIS 2 J. Andrews et al. 10.1016/j.quascirev.2020.106722
- Revisiting Oxygen‐18 and Clumped Isotopes in Planktic and Benthic Foraminifera M. Daëron & W. Gray 10.1029/2023PA004660
- Preferential Loss of High Trace Element Bearing Inner Calcite in Foraminifera During Physical and Chemical Cleaning T. Fritz‐Endres & J. Fehrenbacher 10.1029/2020GC009419
- Are Past Sea-Ice Reconstructions Based on Planktonic Foraminifera Realistic? Study of the Last 50 ka as a Test to Validate Reconstructed Paleohydrography Derived from Transfer Functions Applied to Their Fossil Assemblages F. Eynaud et al. 10.3390/geosciences11100409
- The FORCIS database: A global census of planktonic Foraminifera from ocean waters S. Chaabane et al. 10.1038/s41597-023-02264-2
- Variability in <i>Neogloboquadrina pachyderma</i> stable isotope ratios from isothermal conditions: implications for individual foraminifera analysis L. Jonkers et al. 10.5194/cp-18-89-2022
- Geochemical Differences Between Alive, Uncrusted and Dead, Crusted Shells of Neogloboquadrina pachyderma: Implications for Paleoreconstruction B. Hupp & J. Fehrenbacher 10.1029/2023PA004638
- Population dynamics and reproduction strategies of planktonic foraminifera in the open ocean J. Meilland et al. 10.5194/bg-18-5789-2021
- Increased Productivity in the Equatorial Pacific During the Deglaciation Inferred From the Ba/Ca Ratios of Non‐Spinose Planktic Foraminifera T. Fritz‐Endres et al. 10.1029/2022PA004506
- Planktonic Biota Constituents Responses to Global Sea-Level Changes Recorded in the Uppermost Albian to Middle Cenomanian Deep-Water Facies of the Outer Carpathians Z. Górny et al. 10.3390/min12020152
- 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
- Planktonic foraminifera genomic variations reflect paleoceanographic changes in the Arctic: evidence from sedimentary ancient DNA J. Pawłowska et al. 10.1038/s41598-020-72146-9
- Shell density of planktonic foraminifera and pteropod species Limacina helicina in the Barents Sea: Relation to ontogeny and water chemistry S. Ofstad et al. 10.1371/journal.pone.0249178
- Uncovering hidden structures: previously undescribed pseudopodia and ectoplasmic structures in planktonic foraminifera M. Greco et al. 10.1093/plankt/fbad031
- Stratigraphic and paleoceanographic alternations within a Mediterranean semi-enclosed, syn-rift basin during Marine Isotope Stage 5: The Gulf of Corinth, Greece S. Sergiou et al. 10.1016/j.margeo.2024.107340
- A multi-decadal record of oceanographic changes of the past ~165 years (1850-2015 AD) from Northwest of Iceland M. Simon et al. 10.1371/journal.pone.0239373
- Tracking Southern Ocean Sea Ice Extent With Winter Water: A New Method Based on the Oxygen Isotopic Signature of Foraminifera D. Lund et al. 10.1029/2020PA004095
- The effect of an experimental decrease in salinity on the viability of the Subarctic planktonic foraminifera Neogloboquadrina incompta M. Greco et al. 10.33265/polar.v39.3842
- Southern Ocean sea surface temperature synthesis: Part 1. Evaluation of temperature proxies at glacial-interglacial time scales D. Chandler & P. Langebroek 10.1016/j.quascirev.2021.107191
- Morphotypical and Geochemical Variations of Planktic Foraminiferal Species in Siberian and Central Arctic Ocean Core Tops M. Prabhakar et al. 10.61551/gsjfr.54.1.1
- Seasonality of marine calcifiers in the northern Barents Sea: Spatiotemporal distribution of planktonic foraminifers and shelled pteropods and their contribution to carbon dynamics G. Anglada-Ortiz et al. 10.1016/j.pocean.2023.103121
- Planktic Foraminiferal and Pteropod Contributions to Carbon Dynamics in the Arctic Ocean (North Svalbard Margin) G. Anglada-Ortiz et al. 10.3389/fmars.2021.661158
- INTRATEST TRACE ELEMENT VARIABILITY IN POLAR AND SUBPOLAR PLANKTIC FORAMINIFERA: INSIGHTS INTO VITAL EFFECTS, ONTOGENY, AND BIOMINERALIZATION PROCESSES B. Hupp & J. Fehrenbacher 10.61551/gsjfr.54.4.355
- Planktic Foraminiferal Assemblages in Surface Sediments From the Subpolar North Atlantic Ocean N. Sahoo et al. 10.3389/fmars.2021.781675
- Paleoceanography of the Nw Greenland Sea and Return Atlantic Current Evolution, 35–4 Kyr BP D. Devendra et al. 10.2139/ssrn.4115797
- Environmental variability off NE Greenland (western Fram Strait) during the past 10,600 years M. Zehnich et al. 10.1177/0959683620950393
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- A 600 kyr reconstruction of deep Arctic seawater δ18O from benthic foraminiferal δ18O and ostracode Mg ∕ Ca paleothermometry J. Farmer et al. 10.5194/cp-19-555-2023
- Micropaleontological and Isotopic Perspective of Surface Water Mass Variability in the NE Atlantic from MIS 6 to 5e (188 to 115 ka) H. Rashid et al. 10.3390/geosciences13050149
- Large-scale culturing of Neogloboquadrina pachyderma, its growth in, and tolerance of, variable environmental conditions A. WestgÅrd et al. 10.1093/plankt/fbad034
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- Single-cell metabarcoding reveals biotic interactions of the Arctic calcifier Neogloboquadrina pachyderma with the eukaryotic pelagic community M. Greco et al. 10.1093/plankt/fbab015
- Paleoceanography of the Northwestern Greenland Sea and Return Atlantic Current evolution, 35–4 kyr BP D. Devendra et al. 10.1016/j.gloplacha.2022.103947
- Late Neogene evolution of modern deep-dwelling plankton F. Boscolo-Galazzo et al. 10.5194/bg-19-743-2022
- Dynamics of the subpolar gyre and transition zone of the North Atlantic during the last glacial cycle M. Zeng et al. 10.1016/j.quascirev.2023.108215
- Atlantic inflow and low sea-ice cover in the Nordic Seas promoted Fennoscandian Ice Sheet growth during the Last Glacial Maximum M. Simon et al. 10.1038/s43247-023-01032-9
- Population dynamics of modern planktonic foraminifera in the western Barents Sea J. Meilland et al. 10.5194/bg-17-1437-2020
- Upper-ocean flux of biogenic calcite produced by the Arctic planktonic foraminiferaNeogloboquadrina pachyderma F. Tell et al. 10.5194/bg-19-4903-2022
- A solution for constraining past marine Polar Amplification A. Morley et al. 10.1038/s41467-024-53424-w
Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
To be able to interpret the paleoecological signal contained in N. pachyderma's shells, its habitat depth must be known. Our investigation on 104 density profiles of this species from the Arctic and North Atlantic shows that specimens reside closer to the surface when sea-ice and/or surface chlorophyll concentrations are high. This is in contrast with previous investigations that pointed at the position of the deep chlorophyll maximum as the main driver of N. pachyderma vertical distribution.
To be able to interpret the paleoecological signal contained in N. pachyderma's shells, its...
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