Diatom Physiology Controls Silicic Acid Leakage in Response to Iron Fertilization
Abstract
We explore how the iron dependence of the Si:P uptake ratio R Si:P of diatoms controls the response of the global silicon cycle and phytoplankton community structure to Southern Ocean iron fertilization. We use a data‐constrained model of the coupled Si‐P‐Fe cycles that features a mechanistic representation of nutrient colimitations for three phytoplankton classes and that is embedded in a data‐assimilated global ocean circulation model. We consider three parameterizations of the iron dependence of R Si:P , all of which are consistent with the available field data and allow equally good fits to the observed nutrient climatology but result in very different responses to iron fertilization: Depending on how sharply R Si:P decreases with increasing iron concentration, iron fertilization can either cause enhanced silicic acid leakage from the Southern Ocean or strengthened Southern Ocean silicon trapping. Enhanced silicic acid leakage occurs if decreases in R Si:P win over increases in diatom growth, while the converse causes strengthened Southern Ocean silicon trapping. Silicic acid leakage drives a floristic shift in favor of diatoms in the subtropical gyres and stimulates increased low‐latitude opal export. The diatom contribution to global phosphorus export increases, but the lower diatom silicon requirement under iron‐replete conditions reducesmore »
- Authors:
-
- Department of Applied Mathematics, School of Mathematics and Statistics University of New South Wales Sydney New South Wales Australia
- Department of Earth System Sciences University of California Irvine CA USA
- Earth Research Institute and Department of Geography University of California Santa Barbara CA USA
- Department of Ecology, Evolution and Marine Biology, The Marine Science Institute University of California Santa Barbara CA USA
- Publication Date:
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1577927
- Grant/Contract Number:
- SC0016539
- Resource Type:
- Publisher's Accepted Manuscript
- Journal Name:
- Global Biogeochemical Cycles
- Additional Journal Information:
- Journal Name: Global Biogeochemical Cycles Journal Volume: 33 Journal Issue: 12; Journal ID: ISSN 0886-6236
- Publisher:
- American Geophysical Union (AGU)
- Country of Publication:
- United States
- Language:
- English
Citation Formats
Holzer, Mark, Pasquier, Benoit, DeVries, Timothy, and Brzezinski, Mark. Diatom Physiology Controls Silicic Acid Leakage in Response to Iron Fertilization. United States: N. p., 2019.
Web. doi:10.1029/2019GB006460.
Holzer, Mark, Pasquier, Benoit, DeVries, Timothy, & Brzezinski, Mark. Diatom Physiology Controls Silicic Acid Leakage in Response to Iron Fertilization. United States. https://doi.org/10.1029/2019GB006460
Holzer, Mark, Pasquier, Benoit, DeVries, Timothy, and Brzezinski, Mark. Tue .
"Diatom Physiology Controls Silicic Acid Leakage in Response to Iron Fertilization". United States. https://doi.org/10.1029/2019GB006460.
@article{osti_1577927,
title = {Diatom Physiology Controls Silicic Acid Leakage in Response to Iron Fertilization},
author = {Holzer, Mark and Pasquier, Benoit and DeVries, Timothy and Brzezinski, Mark},
abstractNote = {We explore how the iron dependence of the Si:P uptake ratio R Si:P of diatoms controls the response of the global silicon cycle and phytoplankton community structure to Southern Ocean iron fertilization. We use a data‐constrained model of the coupled Si‐P‐Fe cycles that features a mechanistic representation of nutrient colimitations for three phytoplankton classes and that is embedded in a data‐assimilated global ocean circulation model. We consider three parameterizations of the iron dependence of R Si:P , all of which are consistent with the available field data and allow equally good fits to the observed nutrient climatology but result in very different responses to iron fertilization: Depending on how sharply R Si:P decreases with increasing iron concentration, iron fertilization can either cause enhanced silicic acid leakage from the Southern Ocean or strengthened Southern Ocean silicon trapping. Enhanced silicic acid leakage occurs if decreases in R Si:P win over increases in diatom growth, while the converse causes strengthened Southern Ocean silicon trapping. Silicic acid leakage drives a floristic shift in favor of diatoms in the subtropical gyres and stimulates increased low‐latitude opal export. The diatom contribution to global phosphorus export increases, but the lower diatom silicon requirement under iron‐replete conditions reduces the global opal export. Regardless of R Si:P parameterization, the global response of the biological phosphorus and silicon pumps is dominated by the Southern Ocean. The Si isotope signature of opal flux becomes systematically lighter with increasing iron‐induced silicic acid leakage, consistent with sediment records from iron‐rich glacial periods.},
doi = {10.1029/2019GB006460},
journal = {Global Biogeochemical Cycles},
number = 12,
volume = 33,
place = {United States},
year = {Tue Dec 10 00:00:00 EST 2019},
month = {Tue Dec 10 00:00:00 EST 2019}
}
https://doi.org/10.1029/2019GB006460
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