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  4. Morphotype and Crust Effects on the Geochemistry of Globorotalia inflata
 
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Morphotype and Crust Effects on the Geochemistry of Globorotalia inflata

Journal
Paleoceanography and Paleoclimatology
Journal Volume
36
Journal Issue
4
Date Issued
2021
Author(s)
Jonkers L
Gopalakrishnan A
Weßel L
Chiessi C.M
JEROEN GROENEVELD  
Monien P
Lessa D
Morard R.
DOI
10.1029/2021PA004224
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85105834545&doi=10.1029%2f2021PA004224&partnerID=40&md5=91b826e05ff5b8935dda8f52e0509bab
https://scholars.lib.ntu.edu.tw/handle/123456789/624736
Abstract
Sedimentary specimens of the planktonic foraminifera Globorotalia inflata can provide information on subsurface conditions of past oceans. However, interpretation of their geochemical signal is complicated by possible effects of cryptic diversity and encrustation. Here we address these issues using plankton tow and sediment samples from the western South Atlantic, where two genotypes of G. inflata occur. To separate the genotypes, we analyzed shells from the extreme ends of the morphospace of G. inflata. The δ18O and δ13C of encrusted specimens from both morphotypes are indistinguishable. However, we do find a large influence of encrustation on δ18O and Mg/Ca. Whereas crust Mg/Ca ratios are at all locations lower than lamellar calcite, the crust effect on δ18O is less consistent in space. Plankton tows show that encrusted specimens occur at any depth and that even close to the surface crust Mg/Ca ratios are lower than in lamellar calcite. This is inconsistent with formation of the crust at lower temperature at greater depth. Instead we suggest that the difference between the crust and lamellar calcite Mg/Ca ratio is temperature-independent and due to the presence of high Mg/Ca bands only in the lamellar calcite. The variable crust effect on δ18O is more difficult to explain, but the higher incidence of crust-free specimens in warmer waters and the observation that a crust effect is clearest in the confluence zone, hint at the possibility that the difference reflects advective mixing of specimens from warmer and colder areas, rather than vertical migration. © 2021. The Authors.
Subjects
cryptospecies; encrustation; geochemistry; ontogenic migration; planktonic foraminifera
SDGs

[SDGs]SDG14

Other Subjects
calcite; confluence; encrustation; genotype; morphotype; planktonic foraminifera; sediment analysis; shell; Atlantic Ocean; Atlantic Ocean (South); Atlantic Ocean (South); Foraminifera; Globorotalia inflata
Type
journal article

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