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Evaluation of oxygen isotopes and trace elements in planktonic foraminifera from the Mediterranean Sea as recorders of seawater oxygen isotopes and salinity
- Source :
- Climate of the Past, Vol 16, Pp 2401-2414 (2020), Climate of the Past, 16(6), 2401. European Geosciences Union
- Publication Year :
- 2020
- Publisher :
- Copernicus Publications, 2020.
-
Abstract
- The Mediterranean Sea is characterized by a relatively strong west to east salinity gradient, which makes it an area suitable for testing the effect of salinity on foraminiferal shell geochemistry. We collected living specimens of the planktonic foraminifer Globigerinoides ruber albus to analyse the relation between element ∕ Ca ratios, stable oxygen isotopes of their shells, and surface seawater salinity, isotopic composition and temperature. The oxygen isotopes of sea surface water also correlate with salinity in the Mediterranean during winter, which is when sampling for this study took place. Seawater oxygen and hydrogen isotopes are positively correlated in both the eastern and western Mediterranean Sea, although the relationship differs from previously reported values, especially in the eastern region. The slope between salinity and seawater oxygen isotopes is lower than previously published results. Still, despite the rather modest slope, seawater and foraminiferal carbonate oxygen isotopes are correlated in our dataset, albeit with large residuals and high residual variability. This scatter could be due to either biological variability in vital effects or environmental variability. Numerical models backtracking particles show that ocean-current-driven mixing of particles of different origins might dampen sensitivity and could result in an offset caused by horizontal transport. Results show that Na ∕ Ca is positively correlated with salinity and independent of temperature. As expected, foraminiferal Mg ∕ Ca increases with temperature, which is in line with earlier calibrations, and in the high salinity environment. By using living foraminifera during winter, the previously established Mg ∕ Ca–temperature calibration is extended to temperatures below 18 ∘C, which is a fundamental prerequisite of using single foraminifera for reconstructing past seasonality.
- Subjects :
- lcsh:GE1-350
Global and Planetary Change
biology
Stratigraphy
lcsh:Environmental protection
Ocean current
Paleontology
Plankton
biology.organism_classification
Isotopes of oxygen
Foraminifera
Salinity
Oceanography
Mediterranean sea
lcsh:Environmental pollution
lcsh:TD172-193.5
Environmental science
Seawater
lcsh:TD169-171.8
Globigerinoides
lcsh:Environmental sciences
Subjects
Details
- Language :
- English
- ISSN :
- 18149332 and 18149324
- Volume :
- 16
- Database :
- OpenAIRE
- Journal :
- Climate of the Past
- Accession number :
- edsair.doi.dedup.....60bc341bb79671bec1c9700aca77aa66