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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.
JM | Articles | Volume 40, issue 1
J. Micropalaeontol., 40, 15–35, 2021
https://doi.org/10.5194/jm-40-15-2021
J. Micropalaeontol., 40, 15–35, 2021
https://doi.org/10.5194/jm-40-15-2021

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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Latest update: 28 Jul 2021
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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.
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