Gradual changes in upwelled seawater conditions (redox, pH) from the late Cretaceous through early Paleogene at the northwest coast of Africa: Negative Ce anomaly trend recorded in fossil bio-apatite
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文摘

We investigated Maastrichtian–Eocene phosphorite deposits in Morocco.

Archive dependent REE contents are observed in bioapatite fossils.

The main REE source in the fossils is associated with seawater.

Age-related Ce/Ce* drops indicate redox and/or pH changes of upwelled seawater.

Link to extended oceanic circulation is proposed here.

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