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Evaluation of oxygen isotope and Sr/Ca ratios from a Maldivian Scleractinian coral for reconstruction of climate variability in the NW Indian Ocean.
Storz, D., Gischler, E., Fiebig, J., Eisenhauer, Anton and Garbe-Schönberg, Dieter (2013) Evaluation of oxygen isotope and Sr/Ca ratios from a Maldivian Scleractinian coral for reconstruction of climate variability in the NW Indian Ocean. Palaios, 28 (1). pp. 42-55. DOI 10.2110/palo.2012.p12-034r.
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Abstract
Corals are important marine archives for high-resolution reconstructions of low-latitude climate variability in preinstrumental and historical periods. Herein, we present monthly-resolved records of delta O-18 and Sr/Ca for the 20th century (1917-2007) from a Porites lutea colony from the Maldives (northwestern Indian Ocean). Previous studies of annual mean extension rates of this coral revealed a distinct dependency of coral growth on variations of sea surface temperature (SST) and hydraulic energy, driven by El Nino-Southern Oscillation (ENSO) and southwestern Indian monsoon forcing. This enables the investigation of coral delta O-18 and Sr/Ca ratios from the Maldives as archives of historical ENSO and Indian monsoon variability. Unlike other locations in the Indian Ocean, correlation of delta O-18 and SST is weak (r = -0.42; p < 0.001), suggesting interferences of SST and seawater delta O-18 at the location. These interferences probably caused significantly weaker interannual ENSO signatures in delta O-18 as evident in the extension rates of our coral and in geochemical proxies measured at other sites in the northwestern Indian Ocean. Sr/Ca ratios show bias by nontemperature effects, and were not used to estimate seawater delta O-18 and salinity. Strong decadal variability (10-14 years) in delta O-18, indicative of a Pacific ENSO signal, is not found in instrumental SST, and could be explained by variations in salinity. Interannual and decadal monsoon variability (6-7 yrs and 18-19 yrs), found in the extension rates, was not found in delta O-18, suggesting, in agreement with other studies, that geochemical coral proxy records from the northwestern Indian Ocean do not capture temporal variations of the Indian monsoon strength.
Document Type: | Article |
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Additional Information: | WOS:000317248200006 |
Keywords: | SEA-SURFACE TEMPERATURE; SOUTH CHINA SEA; CHAGOS ARCHIPELAGO; ASIAN MONSOON; EL-NINO; PALEOTEMPERATURE PROXY; DELTA-O-18 RECORDS; SEAWATER STRONTIUM; MARINE CARBONATES; TROPICAL PACIFIC |
Research affiliation: | OceanRep > The Future Ocean - Cluster of Excellence > FO-R09 Kiel University OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems OceanRep > The Future Ocean - Cluster of Excellence |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | SEPM |
Projects: | Future Ocean |
Date Deposited: | 10 May 2013 06:04 |
Last Modified: | 23 Sep 2019 22:16 |
URI: | https://oceanrep.geomar.de/id/eprint/21212 |
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