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Data · dataset · 1993

Major and trace element abundance in sediment samples from ODP Hole 121-758B (Table 1)

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Major and trace element analyses of 30 sediment samples from ODP Core 758B across the Brunhes-Matuyama geomagnetic polarity reversal and the Australasian microtektite-bearing layer show a small but significant anomaly in the elemental abundances of Ir, Co and Ni.

Description

The maximum of the anomaly between 10.89 and 11.00 m below seafloor correlates with the maximum abundance of microtektites. Iridium abundances, which show the most significant anomaly, reach 0.16 ppb, which is evidence for an extraterrestrial component.

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Geochemistry 74% · Tabular 65%
Provenance · 1 source records, 8 field assertions
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DataCite10.1594/pangaea.71213115 d agoJSON v1
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concepts[field].anzsrc:group:3703enrichment · DataCitetaxonomy-embedding@1.1.0title+keywords+description (74%)
concepts[modality].local:modality:tabularenrichment · DataCitekeyword-concept-rules@1.0.0title+description (65%)
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