Mg/Ca-ΔCO3porewater2−–temperature calibration for Globobulimina spp.: A sensitive paleothermometer for deep-sea temperature reconstruction

Mg/Ca-ΔCO3porewater2−–temperature calibration for Globobulimina spp.: A sensitive... Existing benthic foraminiferal Mg/Ca–temperature calibrations are surrounded by substantial uncertainties mainly due to low temperature sensitivity of Mg/Ca in most benthic foraminifers and the effect of carbonate ion concentration on benthic foraminiferal Mg/Ca. Here we present Mg/Ca analysis of Rose Bengal stained and exceptionally well-preserved tests of the infaunal benthic foraminifer Globobulimina spp. from 39 eastern equatorial Atlantic core top samples. Mg/Ca in Globobulimina spp. varies between 2.5 mmol/mol and 9.1 mmol/mol corresponding to bottom water temperatures (BWT) between 1.8 °C and 19.1 °C and ΔCO3pore water2− between 33.7±4 and −34.3±4 μmol/kg in sediment depths between 1 and 10 cm. Mg/Ca and BWT are linearly correlated with a best fit of Mg/Ca [mmol/mol] = (0.36 ± 0.02) ⁎ BWT [°C] + 2.22 ± 0.19 (r2=0.92, p-value: 11⁎10−20, and n=39). Using total alkalinity and pH data of pore water samples from 64 Atlantic multi-corer sites, we obtained ΔCO3pore water2− data from the depth habitat range of Globobulimina spp. (≥1 cm ≤ 10 cm below sediment surface). We show that ΔCO3pore water2− is significantly lower than and linearly co-varies with the ΔCO2−3 of the overlying bottom water: ΔCO3pore water2−=(0.67±0.05)⁎ΔCO3bottom water2−−(39.84±1.98); r2=0.75, p-value: 6⁎10−20, n=64. We found a Mg/Ca sensitivity of 0.009±0.0044 mmol/mol per μmol/kg ΔCO3pore water2− and Mg/Ca temperature sensitivity of 0.32±0.06 mmol/mol/°C after a correction for the ΔCO3pore water2− effect. This study provides a robust Mg/Ca–temperature calibration, highlights that ΔCO3pore water2− is spatially and most likely temporally variable, and contradicts the notion that infaunal foraminiferal Mg/Ca is relatively immune from ΔCO2−3 changes in the overlying bottom water. Furthermore, comparison of down core Mg/Ca data of Cibicides pachyderma and Globobulimina spp. demonstrates that the high temperature sensitivity of Mg/Ca in Globobulimina spp. presents a more robust paleothermometer to reconstruct past changes in the thermal state of the deep ocean. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Earth and Planetary Science Letters Elsevier

Mg/Ca-ΔCO3porewater2−–temperature calibration for Globobulimina spp.: A sensitive paleothermometer for deep-sea temperature reconstruction

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Publisher
Elsevier
Copyright
Copyright © 2016 Elsevier B.V.
ISSN
0012-821X
eISSN
1385-013X
D.O.I.
10.1016/j.epsl.2016.01.009
Publisher site
See Article on Publisher Site

Abstract

Existing benthic foraminiferal Mg/Ca–temperature calibrations are surrounded by substantial uncertainties mainly due to low temperature sensitivity of Mg/Ca in most benthic foraminifers and the effect of carbonate ion concentration on benthic foraminiferal Mg/Ca. Here we present Mg/Ca analysis of Rose Bengal stained and exceptionally well-preserved tests of the infaunal benthic foraminifer Globobulimina spp. from 39 eastern equatorial Atlantic core top samples. Mg/Ca in Globobulimina spp. varies between 2.5 mmol/mol and 9.1 mmol/mol corresponding to bottom water temperatures (BWT) between 1.8 °C and 19.1 °C and ΔCO3pore water2− between 33.7±4 and −34.3±4 μmol/kg in sediment depths between 1 and 10 cm. Mg/Ca and BWT are linearly correlated with a best fit of Mg/Ca [mmol/mol] = (0.36 ± 0.02) ⁎ BWT [°C] + 2.22 ± 0.19 (r2=0.92, p-value: 11⁎10−20, and n=39). Using total alkalinity and pH data of pore water samples from 64 Atlantic multi-corer sites, we obtained ΔCO3pore water2− data from the depth habitat range of Globobulimina spp. (≥1 cm ≤ 10 cm below sediment surface). We show that ΔCO3pore water2− is significantly lower than and linearly co-varies with the ΔCO2−3 of the overlying bottom water: ΔCO3pore water2−=(0.67±0.05)⁎ΔCO3bottom water2−−(39.84±1.98); r2=0.75, p-value: 6⁎10−20, n=64. We found a Mg/Ca sensitivity of 0.009±0.0044 mmol/mol per μmol/kg ΔCO3pore water2− and Mg/Ca temperature sensitivity of 0.32±0.06 mmol/mol/°C after a correction for the ΔCO3pore water2− effect. This study provides a robust Mg/Ca–temperature calibration, highlights that ΔCO3pore water2− is spatially and most likely temporally variable, and contradicts the notion that infaunal foraminiferal Mg/Ca is relatively immune from ΔCO2−3 changes in the overlying bottom water. Furthermore, comparison of down core Mg/Ca data of Cibicides pachyderma and Globobulimina spp. demonstrates that the high temperature sensitivity of Mg/Ca in Globobulimina spp. presents a more robust paleothermometer to reconstruct past changes in the thermal state of the deep ocean.

Journal

Earth and Planetary Science LettersElsevier

Published: Mar 15, 2016

References

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