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Stable isotope geochemistry of corals from Costa...
Journal article

Stable isotope geochemistry of corals from Costa Rica as proxy indicator of the EL Niño/southern Oscillation (ENSO)

Abstract

We analyzed the δ18O and δ13C time-series contained in coral skeletons collected from Isla del Caño, Costa Rica, that survived the 1982–1983 El Niño warming event. Coral δ18O give a record of thermal histories with a precision of ~0.5°C. For this locality, we have determined that the average Δδw effect in the coral skeletons is equivalent to 33% of the skeletal δ18O range. Therefore, if δw effects are not compensated for, the annual …

Authors

Carriquiry JD; Risk MJ; Schwarcz HP

Journal

Geochimica et Cosmochimica Acta, Vol. 58, No. 1, pp. 335–351

Publisher

Elsevier

Publication Date

January 1994

DOI

10.1016/0016-7037(94)90468-5

ISSN

0016-7037