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  4. Mg/Ca in the planktonic foraminifera Globorotalia inflata and Globigerinoides bulloides from Western Mediterranean plankton tow and core top samples
 
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Mg/Ca in the planktonic foraminifera Globorotalia inflata and Globigerinoides bulloides from Western Mediterranean plankton tow and core top samples

Journal
Marine Micropaleontology
Journal Volume
78
Journal Issue
44624
Pages
101-112
Date Issued
2011
Author(s)
van Raden U.J
JEROEN GROENEVELD  
Raitzsch M
Kucera M.
DOI
10.1016/j.marmicro.2010.11.002
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-79651473006&doi=10.1016%2fj.marmicro.2010.11.002&partnerID=40&md5=bbaefd1cfc789edd88315c52c0a11b63
https://scholars.lib.ntu.edu.tw/handle/123456789/624796
Abstract
Due to its strong gradient in salinity and small temperature gradient the Mediterranean provides an ideal setting to study the impact of salinity on the incorporation of Mg into foraminiferal tests. We have investigated tests of Globorotalia inflata and Globigerina bulloides in plankton tow and core top samples from the Western Mediterranean using ICP-OES for bulk analyses and LA-ICP-MS for analyses of individual chambers in single specimens. Mg/Ca observed in G. inflata are consistent with existing calibrations, whereas G. bulloides had significantly higher Mg/Ca than predicted, particularly in core top samples from the easterly stations. Scanning Electron Microscopy and Laser Ablation ICP-MS revealed secondary overgrowths on some tests, which could explain the observed high core top Mg/Ca. We suggest that the Mediterranean intermediate and deep water supersaturated with respect to calcite cause these overgrowths and therefore increased bulk Mg/Ca. However, the different species are influenced by diagenesis to different degrees probably due to different test morphologies. Our results provide new perspectives on reported anomalously high Mg/Ca in sedimentary foraminifera and the applicability of the Mg/Ca paleothermometry in high salinity settings, by showing that (1) part of the signal is generated by precipitation of inorganic calcite on the foraminifer test due to increased calcite saturation state of the water and (2) species with high surface-to-volume shell surfaces are potentially more affected by secondary Mg-rich calcite encrustation. © 2010 Elsevier B.V.
Subjects
Calcite saturation state; Habitat depth; Mediterranean; Mg/Ca paleothermometry; Paleoceanography; Planktonic foraminifera; Recent
SDGs

[SDGs]SDG14

Other Subjects
calcite; calcium; encrustation; magnesium; micropaleontology; paleoceanography; paleotemperature; planktonic foraminifera; sampling; saturation; sea surface salinity; Mediterranean Sea; Mediterranean Sea (West); Foraminifera; Globigerina bulloides; Globigerinoides; Globorotalia inflata
Type
journal article

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