A 2023 study expanded the halite fluid-inclusion archive from individual geologic intervals into a roughly 550-million-year reconstruction of seawater strontium.
You can explore related material in the Rock Salt Chemistry section.
131 Halite Samples
Researchers chemically analysed 1,371 fluid inclusions in 131 halite samples that had marine 87Sr/86Sr values.
The dataset covered Phanerozoic and Neoproterozoic seawater.
Seven-Fold Variation
The paper reported roughly seven-fold variation in seawater strontium concentration over about 550 million years.
Strontium oscillated twice between high and low concentrations.
Plate-Tectonic Link
The authors linked these strontium changes with intervals of calcium-rich, sulfate-poor paleoseawater and calcite–aragonite sea cycles.
The study interprets the long-term pattern within a plate-tectonic control framework.
Related article: Why Is Halite a Chemical Archive of Ancient Oceans?.
Sources
- Geochimica et Cosmochimica Acta 2023 – Plate tectonic control of strontium concentration in seawater
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