The origin of suspended particulate matter in the Great Barrier Reef

River run-off has long been regarded as the largest source of organic-rich suspended particulate matter (SPM) in the Great Barrier Reef (GBR), contributing to high turbidity, pollutant exposure and increasing vulnerability of coral reef to climate change. However, the terrestrial versus marine origi...

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Published inNature communications Vol. 14; no. 1; pp. 5629 - 11
Main Authors Bahadori, Mohammad, Chen, Chengrong, Lewis, Stephen, Wang, Juntao, Shen, Jupei, Hou, Enqing, Rashti, Mehran Rezaei, Huang, Qiaoyun, Bainbridge, Zoe, Stevens, Tom
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group UK 12.09.2023
Nature Publishing Group
Nature Portfolio
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Summary:River run-off has long been regarded as the largest source of organic-rich suspended particulate matter (SPM) in the Great Barrier Reef (GBR), contributing to high turbidity, pollutant exposure and increasing vulnerability of coral reef to climate change. However, the terrestrial versus marine origin of the SPM in the GBR is uncertain. Here we provide multiple lines of evidence ( 13 C NMR, isotopic and genetic fingerprints) to unravel that a considerable proportion of the terrestrially-derived SPM is degraded in the riverine and estuarine mixing zones before it is transported further offshore. The fingerprints of SPM in the marine environment were completely different from those of terrestrial origin but more consistent with that formed by marine phytoplankton. This result indicates that the SPM in the GBR may not have terrestrial origin but produced locally in the marine environment, which has significant implications on developing better-targeted management practices for improving water quality in the GBR. This multidisciplinary fingerprinting study, using isotopic, structural and genetic fingerprints, has shown that the suspended particulate matter in the Great Barrier Reef does not have terrestrial origin but produced locally by marine phytoplankton
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ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-023-41183-z