Elemental anomalies at the Cretaceous-Tertiary boundary, Woodside Creek, New Zealand

Details Elemental anomalies at the Cretaceous-Tertiary boundary, Woodside Creek, New Zealand Elemental anomalies at the Cretaceous-Tertiary boundary, Woodside Creek, New Zealand

Nov 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984sci...226..539b&link_type=abstract

Science (ISSN 0036-8075), vol. 226, Nov. 2, 1984, p. 539-542.

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21

Asteroids, Elements, Geochemistry, Anomalies, Extinction, Iridium, New Zealand

Scientific paper

Iridium and 26 other elements were determined in shale from the Cretaceous-Tertiary boundary at the locus classicus (for iridium anomalies) at Woodside Creek, New Zealand. Iridium, gold, copper, cobalt, chromium, nickel, arsenic, molybdenum, and iron were enriched in the basal 2 millimeters of the 8-millimeter shale parting as compared with the rest of the stratigraphic column. No other shale partings in the column had anomalous concentrations of any element when the data were expressed on a carbonate-free basis. The boundary material showed striking compositional similarities with the Stevns Klint Danish boundary shale. Elemental concentrations were in general much higher in the New Zealand material than in nonboundary shales from elsewhere in the world. The high concentration of iridium (153 nanograms per gram) in the basal layer of the boundary, together with the enrichment of other siderophile elements supports the idea of an exterrestrial source for much of the material. The iridium/gold ratio of 2.1 is also in accordance with such a source. The iridium content of the basal layer is higher than for any other marine boundary shale obtained on land. The integrated iridium value is 187 nanograms per square centimeter of boundary surface.

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