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The continental Si cycle and its impact on the ocean Si isotope budget

Frings, Patrick J. LU ; Clymans, Wim LU ; Fontorbe, Guillaume LU ; De La Rocha, Christina L. LU and Conley, Daniel J. LU (2016) In Chemical Geology 425. p.12-36
Abstract

The silicon isotope composition of biogenic silica (δ30SiBSi) in the ocean is a function of the δ30Si of the available dissolved Si (DSi; H2SiO4), the degree of utilisation of the available DSi, and, for some organisms, the concentration of DSi. This makes δ30SiBSi in sediment archives a promising proxy for past DSi concentrations and utilisation. At steady-state, mean δ30SiBSi must equal a weighted average of the inputs, the majority of which are of continental origin. Variation in the functioning of the continental Si cycle on timescales similar to the residence time of DSi in the ocean (~10 ka) may therefore contribute to downcore... (More)

The silicon isotope composition of biogenic silica (δ30SiBSi) in the ocean is a function of the δ30Si of the available dissolved Si (DSi; H2SiO4), the degree of utilisation of the available DSi, and, for some organisms, the concentration of DSi. This makes δ30SiBSi in sediment archives a promising proxy for past DSi concentrations and utilisation. At steady-state, mean δ30SiBSi must equal a weighted average of the inputs, the majority of which are of continental origin. Variation in the functioning of the continental Si cycle on timescales similar to the residence time of DSi in the ocean (~10 ka) may therefore contribute to downcore variability in δ30SiBSi on millennial or longer timescales. The direction and magnitude of change in published δ30SiBSi records over the last few glacial cycles is consistent among ocean basins and between groups of silicifiers. They document glacial values that are typically 0.5 to 1.0‰ lower than interglacial values and together hint at coherent and predictable glacial-interglacial variability in whole-ocean δ30Si driven by a change in mean δ30Si of the inputs. In this contribution, we review the modern inputs of DSi to the ocean and the controls on their isotopic composition, and assess the evidence for their variability on millennial-plus timescales.Today, 9.55 × 1012 mol yr-1 DSi enters the ocean, of which roughly 64% and 25% are direct riverine inputs of DSi, and DSi from dissolution of aeolian and riverborne sediment, respectively. The remainder derives from alteration or weathering of the ocean crust. Each input has a characteristic δ30Si, with our current best estimate for a weighted mean being 0.74‰, although much work remains to be done to characterise the individual fluxes. Many aspects of the continental Si cycle may have differed during glacial periods that together can cumulatively substantially lower the mean δ30Si of DSi entering the ocean. These changes relate to i) a cooler, drier glacial climate, ii) lowered sea level and the exposure of continental shelves, iii) the presence of large continental ice-sheets, and iv) altered vegetation zonation. Using a simple box-model with a Monte-Carlo approach to parameterisation, we find that a transition from a hypothesised glacial continental Si cycle to the modern Si cycle can drive an increase in whole ocean δ30Si of comparable rate and magnitude to that recorded in δ30SiBSi. This implies that we may need to revisit our understanding of aspects of the Si cycle in the glacial ocean. Although we focus on the transition from the last glacial, our synthesis suggests that the continental Si cycle should be seen as a potential contributory factor to any variability observed in ocean δ30SiBSi on millennial or longer timescales.

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organization
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Contribution to journal
publication status
published
subject
keywords
Biogenic silica, Biogeochemical cycling, Global silicon cycle, LGM, Palaeoceanography, Silicon isotopes
in
Chemical Geology
volume
425
pages
25 pages
publisher
Elsevier
external identifiers
  • Scopus:84957004931
  • WOS:000371130700002
ISSN
0009-2541
DOI
10.1016/j.chemgeo.2016.01.020
language
English
LU publication?
yes
id
4b0aa4dd-e1f8-466e-a0bd-5ddcdb30648b
date added to LUP
2016-05-10 09:40:43
date last changed
2016-12-04 04:51:28
@misc{4b0aa4dd-e1f8-466e-a0bd-5ddcdb30648b,
  abstract     = {<p>The silicon isotope composition of biogenic silica (δ<sup>30</sup>Si<sub>BSi</sub>) in the ocean is a function of the δ<sup>30</sup>Si of the available dissolved Si (DSi; H<sub>2</sub>SiO<sub>4</sub>), the degree of utilisation of the available DSi, and, for some organisms, the concentration of DSi. This makes δ<sup>30</sup>Si<sub>BSi</sub> in sediment archives a promising proxy for past DSi concentrations and utilisation. At steady-state, mean δ<sup>30</sup>Si<sub>BSi</sub> must equal a weighted average of the inputs, the majority of which are of continental origin. Variation in the functioning of the continental Si cycle on timescales similar to the residence time of DSi in the ocean (~10 ka) may therefore contribute to downcore variability in δ<sup>30</sup>Si<sub>BSi</sub> on millennial or longer timescales. The direction and magnitude of change in published δ<sup>30</sup>Si<sub>BSi</sub> records over the last few glacial cycles is consistent among ocean basins and between groups of silicifiers. They document glacial values that are typically 0.5 to 1.0‰ lower than interglacial values and together hint at coherent and predictable glacial-interglacial variability in whole-ocean δ<sup>30</sup>Si driven by a change in mean δ<sup>30</sup>Si of the inputs. In this contribution, we review the modern inputs of DSi to the ocean and the controls on their isotopic composition, and assess the evidence for their variability on millennial-plus timescales.Today, 9.55 × 10<sup>12</sup> mol yr<sup>-1</sup> DSi enters the ocean, of which roughly 64% and 25% are direct riverine inputs of DSi, and DSi from dissolution of aeolian and riverborne sediment, respectively. The remainder derives from alteration or weathering of the ocean crust. Each input has a characteristic δ<sup>30</sup>Si, with our current best estimate for a weighted mean being 0.74‰, although much work remains to be done to characterise the individual fluxes. Many aspects of the continental Si cycle may have differed during glacial periods that together can cumulatively substantially lower the mean δ<sup>30</sup>Si of DSi entering the ocean. These changes relate to i) a cooler, drier glacial climate, ii) lowered sea level and the exposure of continental shelves, iii) the presence of large continental ice-sheets, and iv) altered vegetation zonation. Using a simple box-model with a Monte-Carlo approach to parameterisation, we find that a transition from a hypothesised glacial continental Si cycle to the modern Si cycle can drive an increase in whole ocean δ<sup>30</sup>Si of comparable rate and magnitude to that recorded in δ<sup>30</sup>Si<sub>BSi</sub>. This implies that we may need to revisit our understanding of aspects of the Si cycle in the glacial ocean. Although we focus on the transition from the last glacial, our synthesis suggests that the continental Si cycle should be seen as a potential contributory factor to any variability observed in ocean δ<sup>30</sup>Si<sub>BSi</sub> on millennial or longer timescales.</p>},
  author       = {Frings, Patrick J. and Clymans, Wim and Fontorbe, Guillaume and De La Rocha, Christina L. and Conley, Daniel J.},
  issn         = {0009-2541},
  keyword      = {Biogenic silica,Biogeochemical cycling,Global silicon cycle,LGM,Palaeoceanography,Silicon isotopes},
  language     = {eng},
  month        = {05},
  pages        = {12--36},
  publisher    = {ARRAY(0x8205e18)},
  series       = {Chemical Geology},
  title        = {The continental Si cycle and its impact on the ocean Si isotope budget},
  url          = {http://dx.doi.org/10.1016/j.chemgeo.2016.01.020},
  volume       = {425},
  year         = {2016},
}