Dr Jotis Baronas jotis.baronas@durham.ac.uk
Assistant Professor
Germanium–silicon fractionation in a river-influenced continental margin: The Northern Gulf of Mexico
Baronas, J. Jotautas; Hammond, Douglas E.; Berelson, William M.; McManus, James; Severmann, Silke
Authors
Douglas E. Hammond
William M. Berelson
James McManus
Silke Severmann
Abstract
In this study we have sampled the water column and sediments of the Gulf of Mexico to investigate the effects of high riverine terrigenous load and sediment redox conditions on the cycling of Ge and Si. Water column Ge/Si ratios across the Gulf of Mexico continental shelf range from 1.9 to 25 μmol/mol, which is elevated compared to the global ocean value of 0.7 μmol/mol. The Ge enrichment in the Gulf of Mexico seawater is primarily due to anthropogenic contamination of the Mississippi river, which is the main Ge and Si source to the area, and to a smaller extent due to discrimination against Ge during biogenic silica (bSi) production (Ge/Si = 1.2–1.8 μmol/mol), especially by radiolarians and siliceous sponges (Ge/Si = 0.6–1.1 μmol/mol). Most sediment pore waters (Ge/Si = 0.3–4.5 μmol/mol) and sediment incubation experiments (benthic flux Ge/Si = 0.9–1.2 μmol/mol) indicate precipitation of authigenic phases that sequester Ge from pore waters (non-opal sink). This process appears to be independent of oxidation–reduction reactions and suggests that authigenic aluminosilicate formation (reverse weathering) may be the dominant Ge sink in marine sediments. Compilation of previously published data shows that in continental margins, non-opal Ge burial flux is controlled by bSi supply, while in open ocean sediments it is 10–100 times lower and most likely limited by the supply of lithogenic material. We provide a measurement-based estimate of the global non-opal Ge burial flux as 4–32 Mmol yr−1, encompassing the 2–16 Mmol yr−1 needed to keep the global marine Ge cycle at steady state.
Citation
Baronas, J. J., Hammond, D. E., Berelson, W. M., McManus, J., & Severmann, S. (2016). Germanium–silicon fractionation in a river-influenced continental margin: The Northern Gulf of Mexico. Geochimica et Cosmochimica Acta, 178, 124-142. https://doi.org/10.1016/j.gca.2016.01.028
Journal Article Type | Article |
---|---|
Acceptance Date | Jan 3, 2016 |
Online Publication Date | Feb 2, 2016 |
Publication Date | Apr 1, 2016 |
Deposit Date | Dec 19, 2023 |
Journal | Geochimica et Cosmochimica Acta |
Print ISSN | 0016-7037 |
Electronic ISSN | 1872-9533 |
Publisher | Meteoritical Society |
Peer Reviewed | Peer Reviewed |
Volume | 178 |
Pages | 124-142 |
DOI | https://doi.org/10.1016/j.gca.2016.01.028 |
Public URL | https://durham-repository.worktribe.com/output/2048465 |
You might also like
Vegetal Undercurrents—Obscured Riverine Dynamics of Plant Debris
(2022)
Journal Article
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2024
Advanced Search