Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/151174
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dc.contributor.authorTanzil, Jani Thuaibah Isaen_US
dc.contributor.authorGoodkin, Nathalie Fairbanken_US
dc.contributor.authorSin, T. M.en_US
dc.contributor.authorChen, Menglien_US
dc.contributor.authorFabbro, Gareth Nicholasen_US
dc.contributor.authorBoyle, E. A.en_US
dc.contributor.authorLee, A. C.en_US
dc.contributor.authorToh, K. B.en_US
dc.date.accessioned2021-06-09T08:28:28Z-
dc.date.available2021-06-09T08:28:28Z-
dc.date.issued2019-
dc.identifier.citationTanzil, J. T. I., Goodkin, N. F., Sin, T. M., Chen, M., Fabbro, G. N., Boyle, E. A., Lee, A. C. & Toh, K. B. (2019). Multi-colony coral skeletal Ba/Ca from Singapore’s turbid urban reefs : relationship with contemporaneous in-situ seawater parameters. Geochimica et Cosmochimica Acta, 250, 191-208. https://dx.doi.org/10.1016/j.gca.2019.01.034en_US
dc.identifier.issn0016-7037en_US
dc.identifier.other0000-0001-5334-2010-
dc.identifier.urihttps://hdl.handle.net/10356/151174-
dc.description.abstractThe ratio of barium to calcium in coral skeletons (Ba/Cacoral) is broadly used as a proxy for tracking terrestrial/river runoff. There are, however, inconsistencies in Ba/Cacoral records that have prompted caution in its reliability as an environmental proxy. Direct comparisons between in-situ seawater measurements and coral Ba/Ca are therefore needed to ensure accurate proxy calibration and interpretation. The current study represents the first to test Ba/Cacoral against years-long monthly-resolution contemporaneous measurements of several in-situ seawater parameters i.e. dissolved seawater barium (BaSW), temperature, salinity, suspended sediments, sedimentation rate and photosynthetically active radiation. We analysed the Ba/Cacoral of six Porites lutea corals sampled from two turbid reefs in Singapore, and explored relationships with in-situ seawater parameters over the period 2008–2015. Our study found poor agreement in Ba/Cacoral from replicate corals sampled from the same reef, and only one of the six colonies analysed showed significant but weak Ba/Cacoral–BaSW and Ba/Cacoral–Ba/CaSW relationships. There was also no clear relationship between Ba/Cacoral and skeletal luminescence G/B (a coral proxy strongly linked with salinity and river runoff). This implies that (1) the incorporation of terrestrially derived humic-like substances into the coral is independent of Ba, and (2) it is likely factors other than freshwater discharge/flood events are driving the poor reproducibility of Ba/Cacoral and disconnect with BaSW at our study sites. We found a positive relationship between Ba/Cacoral and organic suspended solids for 4 of the 6 colonies analysed that suggests biological mechanisms such as feeding could be driving skeletal Ba incorporation. A negative relationship between Ba/Cacoral and total sedimentation rate was also found, suggesting that within reef sediment fluxes may be influencing spatio-temporal variability of the Ba-supply. Ba incorporation into coral skeleton, especially in dynamic, turbid settings such as those found in Singapore, is likely more complex than previously thought. Our results highlight the possibility of high heterogeneity in coral responses to environmental conditions, and the need for careful selection of colonies and a site-specific, replicated approach when attempting to apply Ba/Cacoral as a trace element proxy.en_US
dc.description.sponsorshipMinistry of Education (MOE)en_US
dc.description.sponsorshipNational Research Foundation (NRF)en_US
dc.description.sponsorshipSingapore-MIT Alliance for Research and Technology (SMART)en_US
dc.language.isoenen_US
dc.relationMSRDP-03en_US
dc.relationM4430139en_US
dc.relation.ispartofGeochimica et Cosmochimica Actaen_US
dc.rights© 2019 Elsevier Ltd. All rights reserved.en_US
dc.subjectEngineering::Environmental engineeringen_US
dc.titleMulti-colony coral skeletal Ba/Ca from Singapore’s turbid urban reefs : relationship with contemporaneous in-situ seawater parametersen_US
dc.typeJournal Articleen
dc.contributor.schoolAsian School of the Environmenten_US
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.contributor.researchSingapore-MIT Alliance Programmeen_US
dc.identifier.doi10.1016/j.gca.2019.01.034-
dc.identifier.scopus2-s2.0-85061809719-
dc.identifier.volume250en_US
dc.identifier.spage191en_US
dc.identifier.epage208en_US
dc.subject.keywordsBariumen_US
dc.subject.keywordsCalciumen_US
dc.description.acknowledgementThis paper is dedicated to the memory of our colleague, friend and mentor, Dr. Sin Tsai Min (1970–2017). Many thanks to the Singapore National Parks for allowing us to conduct this research (permit no. NP/RP16-156-1). Thanks also to Miss Rosabelle Ong for her assistance in the lab and in the field. Funding was provided by the Singapore National Research Foundation (NRF), Prime Minister’s Office, under the Marine Science Research and Development Programme (Project MSRDP-03 “Adaptation and resilience of coral reefs to environmental change in Singapore”). We also thank the NRF for the St. John’s Island National Marine Laboratory. A portion of the research described in this project was funded by the NRF through the Singapore-MIT Alliance for Research and Technology (SMART) Center for Environmental Sensing and Modeling (CENSAM) and by the Singapore Ministry of Education under the Research Centres of Excellence initiative (Grant Number M4430139). We thank the Public Utilities Board (PUB), Singapore, for granting us the use of their long-term marine water quality monitoring data.en_US
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item.grantfulltextnone-
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