Articles | Volume 15, issue 22
https://doi.org/10.5194/bg-15-6959-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-15-6959-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Nov 2018
Research article |
| 21 Nov 2018
| 21 Nov 2018
Silicon isotopes of deep sea sponges: new insights into biomineralisation and skeletal structure
Lucie Cassarino
CORRESPONDING AUTHOR
University of Bristol, School of Earth Sciences, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK
Christopher D. Coath
University of Bristol, School of Earth Sciences, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK
Joana R. Xavier
CIIMAR – Interdisciplinary Centre of Marine and Environmental Research, University of Porto, Avenida General Norton de Matos, 4450-208 Matosinhos, Portugal
Department of Biological Sciences and K.G. Jebsen Centre for Deep Sea Research, University of Bergen, P.O. Box 7803, 5020 Bergen, Norway
Katharine R. Hendry
University of Bristol, School of Earth Sciences, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK
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Cited
21 citations as recorded by crossref.
- Evidence for Low Dissolved Silica in mid-Mesozoic Oceans J. Yager et al. 10.2475/001c.122691
- Diversity and structure of the deep-sea sponge microbiome in the equatorial Atlantic Ocean S. Williams et al. 10.1099/mic.0.001478
- Silicon isotopic systematics of deep-sea sponge grounds in the North Atlantic K. Hendry et al. 10.1016/j.quascirev.2019.02.017
- Technical note: The silicon isotopic composition of choanoflagellates: implications for a mechanistic understanding of isotopic fractionation during biosilicification A. Marron et al. 10.5194/bg-16-4805-2019
- Silicon isotopes reveal a decline in oceanic dissolved silicon driven by biosilicification: A prerequisite for the Cambrian Explosion? Y. Ye et al. 10.1016/j.epsl.2021.116959
- Nutrient utilization and diatom productivity changes in the low-latitude south-eastern Atlantic over the past 70 ka: response to Southern Ocean leakage K. Hendry et al. 10.5194/cp-17-603-2021
- Utilizing sponge spicules in taxonomic, ecological and environmental reconstructions: a review M. Łukowiak 10.7717/peerj.10601
- Nutrient availability in the North Pacific region not primarily driven by climate through the Quaternary A. Snelling et al. 10.1016/j.palaeo.2022.111109
- Diatom silicon isotope ratios in Quaternary research: Where do we stand? P. Frings et al. 10.1016/j.quascirev.2024.108966
- δ30Si and δ18O of multiple silica phases in chert: Implications for δ30Siseawater of Darriwilian seawater and sea surface temperatures K. Chen et al. 10.1016/j.palaeo.2020.109584
- Extreme silicon isotope fractionation due to Si organic complexation: Implications for silica biomineralization F. Stamm et al. 10.1016/j.epsl.2020.116287
- Silica–Biomacromolecule Interactions: Toward a Mechanistic Understanding of Silicification C. McCutchin et al. 10.1021/acs.biomac.4c00674
- Paragenesis of silicified mid-Paleozoic and mid-Cenozoic corals based on petrography and silicon isotopic analyses C. Andrade et al. 10.1016/j.chemgeo.2020.119483
- Constraints on Earth System Functioning at the Paleocene‐Eocene Thermal Maximum From the Marine Silicon Cycle G. Fontorbe et al. 10.1029/2020PA003873
- A New Method for Silicon Triple Isotope Analysis With Application to Siliceous Sponge Spicules A. Pack et al. 10.1029/2023GC011243
- Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans E. Trower et al. 10.1111/gbi.12449
- Linking silicon isotopic signatures with diatom communities K. Schmidtbauer et al. 10.1016/j.gca.2022.02.015
- Silicon isotopic compositions of dissolved silicic acid in pre- and post-diatom oceans C. Andrade et al. 10.1016/j.gca.2022.11.021
- Using Stable Isotopes to Disentangle Marine Sedimentary Signals in Reactive Silicon Pools R. Pickering et al. 10.1029/2020GL087877
- Sponge-rich sediment recycling in a Paleozoic continental arc driven by mélange melting H. Liu et al. 10.1130/G50395.1
- Silicon Isotope Signatures of Radiolaria Reveal Taxon-Specific Differences in Isotope Fractionation K. Doering et al. 10.3389/fmars.2021.666896
20 citations as recorded by crossref.
- Evidence for Low Dissolved Silica in mid-Mesozoic Oceans J. Yager et al. 10.2475/001c.122691
- Diversity and structure of the deep-sea sponge microbiome in the equatorial Atlantic Ocean S. Williams et al. 10.1099/mic.0.001478
- Silicon isotopic systematics of deep-sea sponge grounds in the North Atlantic K. Hendry et al. 10.1016/j.quascirev.2019.02.017
- Technical note: The silicon isotopic composition of choanoflagellates: implications for a mechanistic understanding of isotopic fractionation during biosilicification A. Marron et al. 10.5194/bg-16-4805-2019
- Silicon isotopes reveal a decline in oceanic dissolved silicon driven by biosilicification: A prerequisite for the Cambrian Explosion? Y. Ye et al. 10.1016/j.epsl.2021.116959
- Nutrient utilization and diatom productivity changes in the low-latitude south-eastern Atlantic over the past 70 ka: response to Southern Ocean leakage K. Hendry et al. 10.5194/cp-17-603-2021
- Utilizing sponge spicules in taxonomic, ecological and environmental reconstructions: a review M. Łukowiak 10.7717/peerj.10601
- Nutrient availability in the North Pacific region not primarily driven by climate through the Quaternary A. Snelling et al. 10.1016/j.palaeo.2022.111109
- Diatom silicon isotope ratios in Quaternary research: Where do we stand? P. Frings et al. 10.1016/j.quascirev.2024.108966
- δ30Si and δ18O of multiple silica phases in chert: Implications for δ30Siseawater of Darriwilian seawater and sea surface temperatures K. Chen et al. 10.1016/j.palaeo.2020.109584
- Extreme silicon isotope fractionation due to Si organic complexation: Implications for silica biomineralization F. Stamm et al. 10.1016/j.epsl.2020.116287
- Silica–Biomacromolecule Interactions: Toward a Mechanistic Understanding of Silicification C. McCutchin et al. 10.1021/acs.biomac.4c00674
- Paragenesis of silicified mid-Paleozoic and mid-Cenozoic corals based on petrography and silicon isotopic analyses C. Andrade et al. 10.1016/j.chemgeo.2020.119483
- Constraints on Earth System Functioning at the Paleocene‐Eocene Thermal Maximum From the Marine Silicon Cycle G. Fontorbe et al. 10.1029/2020PA003873
- A New Method for Silicon Triple Isotope Analysis With Application to Siliceous Sponge Spicules A. Pack et al. 10.1029/2023GC011243
- Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans E. Trower et al. 10.1111/gbi.12449
- Linking silicon isotopic signatures with diatom communities K. Schmidtbauer et al. 10.1016/j.gca.2022.02.015
- Silicon isotopic compositions of dissolved silicic acid in pre- and post-diatom oceans C. Andrade et al. 10.1016/j.gca.2022.11.021
- Using Stable Isotopes to Disentangle Marine Sedimentary Signals in Reactive Silicon Pools R. Pickering et al. 10.1029/2020GL087877
- Sponge-rich sediment recycling in a Paleozoic continental arc driven by mélange melting H. Liu et al. 10.1130/G50395.1
1 citations as recorded by crossref.
Discussed (final revised paper)
Latest update: 02 Apr 2025
Short summary
Using a simple model, we show that the silicon isotopic composition of sponges can be used to estimate the silicic acid concentration of seawater, a key parameter linked to nutrient and carbon cycling. However, our data illustrate that skeletal type and growth rate also control silicon isotopic composition of sponges. Our study demonstrates the paleoceanographic utility of sponges as an archive for ocean silica content provided that suitable skeleton types are selected.
Using a simple model, we show that the silicon isotopic composition of sponges can be used to...
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