Iridium profiles and delivery across the Cretaceous/Paleogene boundary
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文摘

Concentration and profile shape of Ir are not uniform in closely spaced K/Pg sites.

The Lagrangian advection–diffusion model explains Ir profile shapes quantitatively.

Ir profiles were determined primarily by sediment mixing via bioturbation.

The depth-integrated Ir inventory is similar in the majority of the cores studied.

Total Ir delivery at time of the K/Pg event was spatially uniform in the region.

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