Oxygen isotope fractionation between biogenic silica and ocean water

Details Oxygen isotope fractionation between biogenic silica and ocean water Oxygen isotope fractionation between biogenic silica and ocean water

Nov 1971

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1971gecoa..35.1185m&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 35, Issue 11, pp.1185-1187

Physics

6

Scientific paper

The suitability of siliceous radiolaria skeletons in deep sea sediments
for oxygen isotope investigations was determined. The notation used in
this report is defined as: O 18 = [( O 18 / O 16 ) Sampale /( O
18 / O 16 ) smow -1] × 1000 Where SMOW is standard mean ocean
water.

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