38 citations as recorded by crossref.

1. Comparing paleo-oxygenation proxies (benthic foraminiferal surface porosity, I/Ca, authigenic uranium) on modern sediments and the glacial Arabian Sea W. Lu et al. 10.1016/j.gca.2022.06.001
2. Planktic foraminifera iodine/calcium ratios from plankton tows H. Winkelbauer et al. 10.3389/fmars.2023.1095570
3. Reduced bottom water oxygenation in the northern Indian Ocean during the Last Glacial Maximum K. Nisha & S. Naik 10.1016/j.margeo.2024.107437
4. Mineralogy-based stepwise dissolution of dolomitic limestone reveals high iodine content in water-column precipitated calcite and well‑oxygenated shallow seawater during the ∼1.57 Ga oxygenation event H. Fang et al. 10.1016/j.chemgeo.2024.122052
5. Simultaneous Determination of I/Ca and Other Elemental Ratios in Foraminifera: Comparing Results From Acidic and Basic Solutions X. Zhou et al. 10.1029/2022GC010660
6. Iodate in calcite, aragonite and vaterite CaCO3: Insights from first-principles calculations and implications for the I/Ca geochemical proxy X. Feng & S. Redfern 10.1016/j.gca.2018.02.017
7. Iodine-to-calcium ratios in deep-sea scleractinian and bamboo corals Y. Sun et al. 10.3389/fmars.2023.1264380
8. Transient shallow-ocean oxidation associated with the late Ediacaran Nama skeletal fauna: Evidence from iodine contents of the Lower Nama Group, southern Namibia C. Uahengo et al. 10.1016/j.precamres.2020.105732
9. Oxygen depletion recorded in upper waters of the glacial Southern Ocean Z. Lu et al. 10.1038/ncomms11146
10. Iodine content of fish otoliths in species found in diverse habitats R. He et al. 10.1007/s10641-022-01228-6
11. High resolution I/Ca ratios of benthic foraminifera from the Peruvian oxygen-minimum-zone: A SIMS derived assessment of a potential redox proxy N. Glock et al. 10.1016/j.chemgeo.2016.10.025
12. The Peruvian oxygen minimum zone was similar in extent but weaker during the Last Glacial Maximum than Late Holocene N. Glock et al. 10.1038/s43247-022-00635-y
13. Mesoproterozoic oxygenation event: From shallow marine to atmosphere B. Xie et al. 10.1130/B36407.1
14. Incorporation Modes of Iodate in Calcite S. Kerisit et al. 10.1021/acs.est.8b00339
15. A New biological proxy for deep-sea paleo-oxygen: Pores of epifaunal benthic foraminifera A. Rathburn et al. 10.1038/s41598-018-27793-4
16. Iodine content of the carbonates from the Doushantuo Formation and shallow ocean redox change on the Ediacaran Yangtze Platform, South China H. Wei et al. 10.1016/j.precamres.2019.01.007
17. Foraminifera Iodine to Calcium Ratios: Approach and Cleaning H. Winkelbauer et al. 10.1029/2021GC009811
18. Calculating dissolved marine oxygen values based on an enhanced Benthic Foraminifera Oxygen Index M. Kranner et al. 10.1038/s41598-022-05295-8
19. Assessing oxygen depletion in the Northeastern Pacific Ocean during the last deglaciation using I/Ca ratios from multiple benthic foraminiferal species M. Taylor et al. 10.1002/2016PA003062
20. Bacterial diether lipids as a novel proxy to reconstruct past changes in sedimentary oxygenation B. Naafs et al. 10.1016/j.gca.2024.07.036
21. Expanded oxygen minimum zones during the late Paleocene‐early Eocene: Hints from multiproxy comparison and ocean modeling X. Zhou et al. 10.1002/2016PA003020
22. Early Diagenetic Controls on Sedimentary Iodine Release and Iodine‐To‐Organic Carbon Ratios in the Paleo‐Record F. Scholz et al. 10.1029/2023GB007919
23. Halogen and trace element analysis of carbonate-veins and Fe-oxyhydroxide by LA-ICPMS: Implications for seafloor alteration, Atlantis Bank, SW Indian Ridge M. Kendrick et al. 10.1016/j.chemgeo.2020.119668
24. Reconstructing the Oxygen Depth Profile in the Arabian Sea During the Last Glacial Period W. Lu et al. 10.1029/2023PA004632
25. Iodine stability as a function of pH and its implications for simultaneous multi-element ICP-MS analysis of marine carbonates for paleoenvironmental reconstructions M. Cook et al. 10.1016/j.marchem.2022.104148
26. Patterns of local and global redox variability during the Cenomanian–Turonian Boundary Event (Oceanic Anoxic Event 2) recorded in carbonates and shales from central Italy J. Owens et al. 10.1111/sed.12352
27. A Benthic Monitor for Coastal Water Dissolved Oxygen Variation: Mn/Ca Ratios in Tests of an Epifaunal Foraminifer X. Guo et al. 10.1029/2021JC017860
28. Refining the carbonate-associated iodine redox proxy with leaching experiments K. Zhang et al. 10.1016/j.chemgeo.2023.121896
29. The Mesoproterozoic Oxygenation Event S. Zhang et al. 10.1007/s11430-020-9825-x
30. A DOM regulation model for dolomite versus calcite precipitation in the Ediacaran ocean: Implications for the “dolomite problem” W. Wang et al. 10.1016/j.precamres.2022.106947
31. Reconstructing ocean oxygenation changes from U/Ca and U/Mn in foraminiferal coatings: Proxy validation and constraints on glacial oxygenation changes R. Hu et al. 10.1016/j.quascirev.2023.108028
32. A pulse of oxygen increase in the early Mesoproterozoic ocean at ca. 1.57–1.56 Ga M. Shang et al. 10.1016/j.epsl.2019.115797
33. Proxies for paleo-oxygenation: A downcore comparison between benthic foraminiferal surface porosity and I/Ca W. Lu et al. 10.1016/j.palaeo.2021.110588
34. Linking the Bitter Springs carbon isotope anomaly and early Neoproterozoic oxygenation through I/[Ca + Mg] ratios S. Wörndle et al. 10.1016/j.chemgeo.2019.06.015
35. Organic Heterogeneities in Foraminiferal Calcite Traced Through the Distribution of N, S, and I Measured With NanoSIMS: A New Challenge for Element-Ratio-Based Paleoproxies? N. Glock et al. 10.3389/feart.2019.00175
36. I/Ca in epifaunal benthic foraminifera: A semi-quantitative proxy for bottom water oxygen in a multi-proxy compilation for glacial ocean deoxygenation W. Lu et al. 10.1016/j.epsl.2019.116055
37. A transient oxygen increase in the Mesoproterozoic ocean at ∼1.44 Ga: Geochemical evidence from the Tieling Formation, North China Platform Y. Yu et al. 10.1016/j.precamres.2021.106527
38. Perspectives on Proterozoic surface ocean redox from iodine contents in ancient and recent carbonate D. Hardisty et al. 10.1016/j.epsl.2017.01.032