U-Pb geochronology reveals that hydrothermal dolomitization was coeval to the deposition of the Burgess Shale lagerstätte

• Published in: Communications earth & environment Vol. 5; no. 1; pp. 318 - 13
• Main Authors: McCormick, Cole A, Corlett, Hilary, Roberts, Nick M. W, Johnston, Paul A, Collom, Christopher J, Stacey, Jack, Koeshidayatullah, Ardiansyah, Hollis, Cathy
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group 01.12.2024; Nature Portfolio
• Subjects: Cambrian; Cathedrals; Clinochlore; Deep water; Deposition; Fossils; Geochronology; Lead; Magnesite; Magnesium carbonate; Mineralization; Offshore platforms; Ordovician; Paleozoic; Radiometric dating; Rifting; Sedimentary basins; Shale; Shales; Shallow water; Canada
• ISSN: 2662-4435
• DOI: 10.1038/s43247-024-01429-0

Fault-controlled, hydrothermal dolomitization often occurs at margins between shallow-water carbonate platforms and deep-water sedimentary basins. In western Canada, for example, the platform margin between the Cathedral Formation and the Burgess Shale Formation has been dolomitized at temperatures up to ~200 °C, with local magnesite, talc, and clinochlore mineralization. At the same time, the Burgess Shale Formation includes exceptional fossils that provide key evidence of the radiation of the animal phyla during the Cambrian Period (541 to 485.4 Ma). This lagerstätte and Mg-rich minerals within the adjacent and underlying strata, however, have been critically understudied. Here we show, using carbonate U-Pb geochronology, that western Canada was tectonically active and subject to hydrothermal dolomitization during the Middle Cambrian (Miaolingian Epoch) to Middle Ordovician (488.1 ± 18.8 Ma). These results extend the latest stages of rifting along the western margin of Laurentia into the Paleozoic, while also suggesting that the dolomitization of the Cathedral Formation occurred at the same time as the deposition of the Burgess Shale lagerstätte.U-Pb geochronology indicates that the western margin of Laurentia was tectonically active and subject to hydrothermal dolomitization during the Middle Cambrian (Miaolingian Epoch) to Middle Ordovician, coeval to the deposition of the Burgess Shale lagerstätte.