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dc.contributor.authorMartin, Patricken_US
dc.contributor.authorMoynihan, Molly A.en_US
dc.contributor.authorChen, Shuangen_US
dc.contributor.authorWoo, Oon Yeeen_US
dc.contributor.authorZhou, Yonglien_US
dc.contributor.authorNichols, Robert S.en_US
dc.contributor.authorChang, Kristy Y. W.en_US
dc.contributor.authorTan, Ashleen S. Y.en_US
dc.contributor.authorChen, Ying-Hsuanen_US
dc.contributor.authorRen, Haojiaen_US
dc.contributor.authorChen, Menglien_US
dc.identifier.citationMartin, P., Moynihan, M. A., Chen, S., Woo, O. Y., Zhou, Y., Nichols, R. S., Chang, K. Y. W., Tan, A. S. Y., Chen, Y., Ren, H. & Chen, M. (2022). Monsoon-driven biogeochemical dynamics in an equatorial shelf sea: time-series observations in the Singapore Strait. Estuarine, Coastal and Shelf Science, 270, 107855-.
dc.description.abstractCoastal tropical waters are experiencing rapid increases in anthropogenic pressures, yet coastal biogeochemical dynamics in the tropics are poorly studied. We present a multi-year biogeochemical time series from the Singapore Strait in Southeast Asia's Sunda Shelf Sea. Despite being highly urbanised and a major shipping port, the strait harbours numerous biologically diverse habitats and is a valuable system for understanding how tropical marine ecosystems respond to anthropogenic pressures. We observed strong seasonality driven by the semi-annual reversal of ocean currents: dissolved inorganic nitrogen (DIN) and phosphorus varied from ≤0.05 μmol l−1 during the intermonsoons to ≥4 μmol l−1 and ≥0.25 μmol l−1, respectively, during the southwest monsoon. Si(OH)4 exceeded DIN year-round. Based on nutrient concentrations, their relationships to salinity and coloured dissolved organic matter, and the isotopic composition of NOx−, we infer that terrestrial input from peatlands is the main nutrient source. This input delivered dissolved organic carbon (DOC) and nitrogen, but was notably depleted in dissolved organic phosphorus. In contrast, particulate organic matter showed little seasonality, and the δ13C of particulate organic carbon (−21.0 ± 1.5‰) is consistent with a primarily autochthonous origin. The seasonal pattern of the diel changes in dissolved O2 suggests that light availability controls primary productivity more than nutrient concentrations. However, diel changes in pH were greater during the southwest monsoon, when remineralisation of terrestrial DOC lowers the seawater buffer capacity. We conclude that terrestrial input results in mesotrophic conditions, and that the strait might undergo further eutrophication if nutrient inputs increase during seasons when light availability is high. Moreover, the remineralisation of terrestrial DOC within the Sunda Shelf Sea may enhance future ocean acidification.en_US
dc.description.sponsorshipNational Research Foundation (NRF)en_US
dc.relation.ispartofEstuarine, Coastal and Shelf Scienceen_US
dc.rights© 2022 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (
dc.titleMonsoon-driven biogeochemical dynamics in an equatorial shelf sea: time-series observations in the Singapore Straiten_US
dc.typeJournal Articleen
dc.contributor.schoolAsian School of the Environmenten_US
dc.contributor.schoolInterdisciplinary Graduate School (IGS)en_US
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.description.versionPublished versionen_US
dc.subject.keywordsMarine Biogeochemistryen_US
dc.subject.keywordsNutrient Dynamicsen_US
dc.description.acknowledgementThis research was funded by the National Research Foundation, Singapore, Prime Minister’s Office, through the Marine Science Research and Development Programme and the Marine Environment Sensing Network (grants MSRDP-P11, MSRDP-P32, and NRF-NRI-2020-MESN), and was carried out under research permit NP/RP17-044-3 from the Singapore National Parks Board.en_US
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