Rare earth elements and yttrium (REY) are essential to modern technologies, yet we know little about how they concentrate at the Earth’s surface, particularly in marine sediments, which hold vast reserves.
REY are enriched in deep-sea mud by several billion times compared to seawater, and, from a fundamental perspective, determining the chemical forms of REY is critical to understanding one of the highest levels of metal partitioning on Earth.
The sedimentary component hosting REY consists of biogenic and authigenic fluorapatite (FAp, Ca5(PO4)3F). When fish die, their bones and teeth accumulate on the seafloor, allowing biogenic FAp to adsorb REY from seawater and pore fluids over extensive periods, ranging from hundreds of thousands to millions of years, during the diagenesis process. Until now, scientists thought cerium just replaced calcium atoms in the bone structure. However, scientists led by the ESRF have found otherwise.
ESRF scientist Alain Manceau and his team, in the framework of his ERC Advanced Grant Deep-SEE, analysed several tens of fossil bones and teeth handpicked at 1.94 and 4.70 meters depth below the seafloor in a sediment core (16GC) collected in the Pacific Ocean’s Clarion-Clipperton Fracture Zone. They found that cerium actually forms a completely different local structure within the fish remains, separate from that of calcium. This structure is a new kind of cerium-phosphate compound precipitated in an amorphous phase at the surface of FAp nanocrystals.
The team used the techniques of X-ray fluorescence mapping, to see the location of cerium, and high-energy-resolution fluorescence-detected X-ray absorption spectroscopy (HERFD-XAS), to track how the cerium atoms bond to other atoms nearby, in the newly built ID24-DCM.
Read more on ESRF website