Articles | Volume 16, issue 6
Clim. Past, 16, 2401–2414, 2020
https://doi.org/10.5194/cp-16-2401-2020
Clim. Past, 16, 2401–2414, 2020
https://doi.org/10.5194/cp-16-2401-2020

Research article 30 Nov 2020

Research article | 30 Nov 2020

Evaluation of oxygen isotopes and trace elements in planktonic foraminifera from the Mediterranean Sea as recorders of seawater oxygen isotopes and salinity

Linda K. Dämmer et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (17 Aug 2020) by Alessio Rovere
AR by Linda Dämmer on behalf of the Authors (11 Sep 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (17 Sep 2020) by Alessio Rovere
AR by Linda Dämmer on behalf of the Authors (25 Sep 2020)  Author's response    Manuscript
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Short summary
The compositions of foraminifera shells often vary with environmental parameters such as temperature or salinity; thus, they can be used as proxies for these environmental variables. Often a single proxy is influenced by more than one parameter. Here, we show that while salinity impacts shell Na / Ca, temperature has no effect. We also show that the combination of different proxies (Mg / Ca and δ18O) to reconstruct salinity does not seem to work as previously thought.