21 citations as recorded by crossref.

1. Evidence for Low Dissolved Silica in mid-Mesozoic Oceans J. Yager et al. 10.2475/001c.122691
2. Diversity and structure of the deep-sea sponge microbiome in the equatorial Atlantic Ocean S. Williams et al. 10.1099/mic.0.001478
3. Silicon isotopic systematics of deep-sea sponge grounds in the North Atlantic K. Hendry et al. 10.1016/j.quascirev.2019.02.017
4. 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
5. 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
6. 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
7. Utilizing sponge spicules in taxonomic, ecological and environmental reconstructions: a review M. Łukowiak 10.7717/peerj.10601
8. 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
9. Diatom silicon isotope ratios in Quaternary research: Where do we stand? P. Frings et al. 10.1016/j.quascirev.2024.108966
10. 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
11. Extreme silicon isotope fractionation due to Si organic complexation: Implications for silica biomineralization F. Stamm et al. 10.1016/j.epsl.2020.116287
12. Silica–Biomacromolecule Interactions: Toward a Mechanistic Understanding of Silicification C. McCutchin et al. 10.1021/acs.biomac.4c00674
13. 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
14. Constraints on Earth System Functioning at the Paleocene‐Eocene Thermal Maximum From the Marine Silicon Cycle G. Fontorbe et al. 10.1029/2020PA003873
15. A New Method for Silicon Triple Isotope Analysis With Application to Siliceous Sponge Spicules A. Pack et al. 10.1029/2023GC011243
16. Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans E. Trower et al. 10.1111/gbi.12449
17. Linking silicon isotopic signatures with diatom communities K. Schmidtbauer et al. 10.1016/j.gca.2022.02.015
18. Silicon isotopic compositions of dissolved silicic acid in pre- and post-diatom oceans C. Andrade et al. 10.1016/j.gca.2022.11.021
19. Using Stable Isotopes to Disentangle Marine Sedimentary Signals in Reactive Silicon Pools R. Pickering et al. 10.1029/2020GL087877
20. Sponge-rich sediment recycling in a Paleozoic continental arc driven by mélange melting H. Liu et al. 10.1130/G50395.1
21. Silicon Isotope Signatures of Radiolaria Reveal Taxon-Specific Differences in Isotope Fractionation K. Doering et al. 10.3389/fmars.2021.666896