Evaluating climate indices and their geochemical proxies measured in corals

R. G. Fairbanks; M. N. Evans; J. L. Rubenstone; R. A. Mortlock; K. Broad; M. D. Moore; C. D. Charles

doi:10.1007/s003380050245

Evaluating climate indices and their geochemical proxies measured in corals

R. G. Fairbanks, M. N. Evans, J. L. Rubenstone, R. A. Mortlock, K. Broad, M. D. Moore, C. D. Charles

Research output: Contribution to journal › Review article › peer-review

167 Scopus citations

Abstract

Standard ocean/climate indices such as the Niño-3 sea surface temperature (SST) index, based on sparse instrumental data, and atmospheric indices such as the Southern Oscillation Index (SOI), may now be substituted and/or extended by coral-based indices. Several elements or their isotopes are incorporated in coral aragonitic skeletons at predictable concentrations, some of which are temperature or salinity dependent. The availability of century-old corals, at key oceanographic sites, permits the establishment of a network of proxy climate indices.

Original language	English (US)
Pages (from-to)	S93-S100
Journal	Coral Reefs
Volume	16
Issue number	SUPPL. 1
DOIs	https://doi.org/10.1007/s003380050245
State	Published - 1997
Externally published	Yes

ASJC Scopus subject areas

Aquatic Science

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

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10.1007/s003380050245

Cite this

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title = "Evaluating climate indices and their geochemical proxies measured in corals",

abstract = "Standard ocean/climate indices such as the Ni{\~n}o-3 sea surface temperature (SST) index, based on sparse instrumental data, and atmospheric indices such as the Southern Oscillation Index (SOI), may now be substituted and/or extended by coral-based indices. Several elements or their isotopes are incorporated in coral aragonitic skeletons at predictable concentrations, some of which are temperature or salinity dependent. The availability of century-old corals, at key oceanographic sites, permits the establishment of a network of proxy climate indices.",

author = "Fairbanks, {R. G.} and Evans, {M. N.} and Rubenstone, {J. L.} and Mortlock, {R. A.} and K. Broad and Moore, {M. D.} and Charles, {C. D.}",

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T1 - Evaluating climate indices and their geochemical proxies measured in corals

AU - Fairbanks, R. G.

AU - Evans, M. N.

AU - Rubenstone, J. L.

AU - Mortlock, R. A.

AU - Broad, K.

AU - Moore, M. D.

AU - Charles, C. D.

PY - 1997

Y1 - 1997

N2 - Standard ocean/climate indices such as the Niño-3 sea surface temperature (SST) index, based on sparse instrumental data, and atmospheric indices such as the Southern Oscillation Index (SOI), may now be substituted and/or extended by coral-based indices. Several elements or their isotopes are incorporated in coral aragonitic skeletons at predictable concentrations, some of which are temperature or salinity dependent. The availability of century-old corals, at key oceanographic sites, permits the establishment of a network of proxy climate indices.

AB - Standard ocean/climate indices such as the Niño-3 sea surface temperature (SST) index, based on sparse instrumental data, and atmospheric indices such as the Southern Oscillation Index (SOI), may now be substituted and/or extended by coral-based indices. Several elements or their isotopes are incorporated in coral aragonitic skeletons at predictable concentrations, some of which are temperature or salinity dependent. The availability of century-old corals, at key oceanographic sites, permits the establishment of a network of proxy climate indices.

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M3 - Review article

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SP - S93-S100

JO - Coral Reefs

JF - Coral Reefs

SN - 0722-4028

IS - SUPPL. 1

ER -

Evaluating climate indices and their geochemical proxies measured in corals

Abstract

ASJC Scopus subject areas

UN SDGs

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