Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei
Abstract
Mg/Ca ratios of planktic foraminifera are commonly used to reconstruct past ocean temperatures. However, intrashell Mg/Ca ratios exhibit a pattern of alternating high and low Mg-bands in many species. Whereas mechanisms controlling Mg variability are poorly constrained, recent experiments demonstrate that it is paced by the diurnal light/dark cycle in Orbulina universa, which forms a terminal shell of simple spherical geometry. It is unknown whether Mg-heterogeneity is diurnally paced in species with complex shell morphologies, or is the result of growth processes. Here, we show that high Mg/Ca-calcite also forms at night in cultured specimens of the multi-chambered planktic foraminifera Neogloboquadrina dutertrei. Our results demonstrate that N. dutertrei adds a significant amount of calcite, and nearly all Mg-bands, after the final chamber forms. Furthermore, these results have implications for interpreting patterns of calcification in N. dutertrei, and possibly other foraminifera species, and suggests diurnal Mg-banding is an intrinsic component of biomineralization in planktic foraminifera.
- Authors:
-
[2];
- Oregon State Univ., Corvallis, OR (United States); Univ. of California, Davis, CA (United States)
- Univ. of California, Davis, CA (United States)
- Univ. of Washington, Seattle, WA (United States)
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
- Indianapolis, IN (United States)
- Publication Date:
- Research Org.:
- Pacific Northwest National Laboratory (PNNL), Richland, WA (United States). Environmental Molecular Sciences Laboratory (EMSL)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1358475
- Report Number(s):
- PNNL-SA-123433
Journal ID: ISSN 2041-1723; 48564; KP1704020
- Grant/Contract Number:
- AC05-76RL01830
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Nature Communications
- Additional Journal Information:
- Journal Volume: 8; Journal ID: ISSN 2041-1723
- Publisher:
- Nature Publishing Group
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 59 BASIC BIOLOGICAL SCIENCES; Environmental Molecular Sciences Laboratory; biogeochemistry; marine biology; palaeoceanography
Citation Formats
Fehrenbacher, Jennifer S., Russell, Ann D., Davis, Catherine V., Gagnon, Alexander C., Spero, Howard J., Cliff, John B., Zhu, Zihua, and Martin, Pamela. Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei. United States: N. p., 2017.
Web. doi:10.1038/ncomms15441.
Fehrenbacher, Jennifer S., Russell, Ann D., Davis, Catherine V., Gagnon, Alexander C., Spero, Howard J., Cliff, John B., Zhu, Zihua, & Martin, Pamela. Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei. United States. https://doi.org/10.1038/ncomms15441
Fehrenbacher, Jennifer S., Russell, Ann D., Davis, Catherine V., Gagnon, Alexander C., Spero, Howard J., Cliff, John B., Zhu, Zihua, and Martin, Pamela. Mon .
"Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei". United States. https://doi.org/10.1038/ncomms15441. https://www.osti.gov/servlets/purl/1358475.
@article{osti_1358475,
title = {Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei},
author = {Fehrenbacher, Jennifer S. and Russell, Ann D. and Davis, Catherine V. and Gagnon, Alexander C. and Spero, Howard J. and Cliff, John B. and Zhu, Zihua and Martin, Pamela},
abstractNote = {Mg/Ca ratios of planktic foraminifera are commonly used to reconstruct past ocean temperatures. However, intrashell Mg/Ca ratios exhibit a pattern of alternating high and low Mg-bands in many species. Whereas mechanisms controlling Mg variability are poorly constrained, recent experiments demonstrate that it is paced by the diurnal light/dark cycle in Orbulina universa, which forms a terminal shell of simple spherical geometry. It is unknown whether Mg-heterogeneity is diurnally paced in species with complex shell morphologies, or is the result of growth processes. Here, we show that high Mg/Ca-calcite also forms at night in cultured specimens of the multi-chambered planktic foraminifera Neogloboquadrina dutertrei. Our results demonstrate that N. dutertrei adds a significant amount of calcite, and nearly all Mg-bands, after the final chamber forms. Furthermore, these results have implications for interpreting patterns of calcification in N. dutertrei, and possibly other foraminifera species, and suggests diurnal Mg-banding is an intrinsic component of biomineralization in planktic foraminifera.},
doi = {10.1038/ncomms15441},
journal = {Nature Communications},
number = ,
volume = 8,
place = {United States},
year = {Mon May 15 00:00:00 EDT 2017},
month = {Mon May 15 00:00:00 EDT 2017}
}
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Planktonic foraminiferal spine versus shell carbonate Na incorporation in relation to salinity
posted_content, October 2018
- Mezger, Eveline M.; de Nooijer, Lennart J.; Bertlich, Jacqueline
- Biogeosciences Discussions
Impact of salinity on element incorporation in two benthic foraminiferal species with contrasting Magnesium contents
posted_content, December 2017
- Geerken, Esmee; de Nooijer, Lennart Jan; van Dijk, Inge
- Biogeosciences Discussions