Towards reconstructing ancient seawater Mg/Ca by combining porcelaneous and hyaline foraminiferal Mg/Ca-temperature calibrations

TitreTowards reconstructing ancient seawater Mg/Ca by combining porcelaneous and hyaline foraminiferal Mg/Ca-temperature calibrations
Type de publicationArticle de revue
AuteurWit, Johannes C., de Nooijer, Lennart Jan, Haig, J., Jorissen, Frans , Thomas, E., Reichart, Gert-Jan
EditeurElsevier
TypeArticle scientifique dans une revue à comité de lecture
Année2017
LangueAnglais
Date15 Août 2017
Pagination341-354
Volume211
Titre de la revueGeochimica et Cosmochimica Acta
ISSN00167037
Mots-clésbenthic foraminifera, Mg/Ca seawater, Proxy calibration, Temperature reconstructions
Résumé en anglais

The temperature of the deep ocean plays a vital role in the Earth’s climate system. Paleo-reconstructions of deep-sea temperatures have traditionally been based on the oxygen isotope composition of deep-sea benthic foraminiferal calcite shells, although this parameter depends upon polar ice volume as well as temperature. More recent reconstructions use Mg/Ca in these shells, with temperature calibrations based on empirical relationships observed in present-day oceans. Incorporation of Mg (DMg) into foraminiferal calcite is, however, not solely dependent on temperature, but also on seawater Mg/Ca. Due to its long oceanic residence time, Mg concentrations remained relatively constant over time scales of a few hundred thousand years, but varied significantly over longer geological time scales. Accurate reconstruction of past temperatures using foraminiferal Mg/Ca, therefore, hinges on our understanding of Mg/Ca seawater changes on geological timescales. We explore a novel, independent approach to reconstructing past seawater Mg/Ca using the temperature-dependent offset in DMg between porcelaneous (secreting intermediate- or high-Mg calcite, abbreviated as IMC or HMC, respectively) and hyaline (producing low-Mg calcite, abbreviated as LMC) benthic foraminifera. We calibrated the Mg/Ca-temperature dependence for Pyrgo spp. (one of the few common, large-sized porcelaneous taxa present in the deep-sea since the middle Miocene), and combined this with an existing calibration of hyaline Cibicidoides spp. to mathematically solve for changes in Mg/Ca seawater through time. We show that changes in Mg/Ca seawater can be reconstructed using the offset between porcelaneous and hyaline foraminifera, but absolute values are highly dependent on the species-specific offset between Mg/Ca seawater and Mg-partition coefficients.

URL de la noticehttp://okina.univ-angers.fr/publications/ua18605
DOI10.1016/j.gca.2017.05.036
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https://www.sciencedirect.com/science/article/pii/S0016703717303320?via%...

Titre abrégéGeochimica et Cosmochimica Acta