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Journal of Micropalaeontology An open-access journal of The Micropalaeontological Society
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Integrated micropaleontological (planktic and benthic foraminifera, diatoms, and silicoflagellates) analysis, together with textural and geochemical results of a deep-sea core from the Hallett Ridge (northwestern Ross Sea), provides new data for late Quaternary (23–2 ka) paleoenvironmental and paleoceanographic reconstructions of this region. Results allow us to identify three time intervals: the glacial–deglacial transition, the deglacial period, and the interglacial period.
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JM | Articles | Volume 40, issue 1
JM | Articles | Volume 40, issue 1
J. Micropalaeontol., 40, 15–35, 2021
https://doi.org/10.5194/jm-40-15-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
J. Micropalaeontol., 40, 15–35, 2021
https://doi.org/10.5194/jm-40-15-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
JM | Articles | Volume 40, issue 1

Research article 10 Mar 2021

Research article | 10 Mar 2021

Last Glacial Maximum to Holocene paleoceanography of the northwestern Ross Sea inferred from sediment core geochemistry and micropaleontology at Hallett Ridge

Romana Melis et al.

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Short summary
Integrated micropaleontological (planktic and benthic foraminifera, diatoms, and silicoflagellates) analysis, together with textural and geochemical results of a deep-sea core from the Hallett Ridge (northwestern Ross Sea), provides new data for late Quaternary (23–2 ka) paleoenvironmental and paleoceanographic reconstructions of this region. Results allow us to identify three time intervals: the glacial–deglacial transition, the deglacial period, and the interglacial period.
Read more
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Journal of Micropalaeontology

An open-access journal of The Micropalaeontological Society

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