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Why Was Cretaceous Seawater Different? Chemical Records from Brazilian, Congo and Thai Halites

The 2006 reconstruction of calcium-rich, sulfate-poor Cretaceous seawater from halite fluid inclusions.

A 2006 Geochimica et Cosmochimica Acta study used halite fluid inclusions to show that Cretaceous seawater had markedly different major-ion chemistry from the modern ocean.

More information on this topic is available in the Rock Salt Chemistry section.

Three Evaporite Regions

Researchers analysed Early Cretaceous halites from the Sergipe Basin in Brazil, Congo Basin and Khorat Plateau in Laos/Thailand.

These deposits allowed comparison across different intervals of Cretaceous seawater.

Calcium-Rich, Sulfate-Poor

The paper reported higher calcium but lower sodium, magnesium and sulfate than modern seawater.

The Mg/Ca ratio was also lower than in today’s ocean.

Tachyhydrite Connection

This chemistry may help explain rare CaCl2-bearing tachyhydrite in some Cretaceous evaporites of Brazil, Congo and Thailand.

The absence of typical modern-seawater Mg-sulfate salts in these deposits is also consistent with the reconstructed paleochemistry.

Sources

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