Geochemical and isotopic characterization of trace fossil infillings: New insights on tracemaker activity after the K/Pg impact event
文摘

The infilling of trace fossils from the K–Pg boundary transition has been analyzed.

Geochemical proxy evidence material from the ejecta layer infilling trace fossils.

Trace fossils distribution evidences a rapid recovery of the macrobenthic community.

Bioturbational disturbance should be considered for the K–Pg event reconstruction.

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