Seagrass sediments reveal the long-term deterioration of an estuarine ecosystem
KAUST DepartmentRed Sea Research Center (RSRC)
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Abstract© 2016 John Wiley & Sons Ltd. The study of a Posidonia australis sediment archive has provided a record of ecosystem dynamics and processes over the last 600 years in Oyster Harbour (SW Australia). Ecosystem shifts are a widespread phenomenon in coastal areas, and this study identifies baseline conditions and the time-course of ecological change (cycles, trends, resilience and thresholds of ecosystem change) under environmental stress in seagrass-dominated ecosystem. The shifts in the concentrations of chemical elements, carbonates, sediments <0.125 mm and stable carbon isotope signatures (δ13C) of the organic matter were detected between 1850s and 1920s, whereas the shift detected in P concentration occurred several decades later (1960s). The first degradation phase (1850s-1950s) follows the onset of European settlement in Australia and was characterized by a strong increase in sediment accumulation rates and fine-grained particles, driven primarily by enhanced run-off due to land clearance and agriculture in the catchment. About 80% of total seagrass area at Oyster Harbour was lost during the second phase of environmental degradation (1960s until present). The sharp increase in P concentration and the increasing contribution of algae and terrestrial inputs into the sedimentary organic matter pool around 1960s provides compelling evidence of the documented eutrophication of the estuary and the subsequent loss of seagrass meadows. The results presented demonstrate the power of seagrass sedimentary archives to reconstruct the trajectories of anthropogenic pressures on estuarine ecosystem and the associated regime shifts, which can be used to improve the capacity of scientists and environmental managers to understand, predict and better manage ecological change in these ecosystems.
CitationSerrano O, Lavery P, Masque P, Inostroza K, Bongiovanni J, et al. (2016) Seagrass sediments reveal the long-term deterioration of an estuarine ecosystem. Global Change Biology 22: 1523–1531. Available: http://dx.doi.org/10.1111/gcb.13195.
SponsorsThis work was supported by the ECU Faculty Research Grant Scheme, the ECU Early Career Research Grant Scheme, and the CSIRO Flagship Marine & Coastal Carbon Biogeochemical Cluster (Coastal Carbon Cluster) with funding from the CSIRO Flagship Collaboration Fund. PM was partially funded by the Generalitat de Catalunya (MERS) (2014 SGR-1356) and through a Gledden Visiting Fellowship awarded by the Institute of Advanced Studies at The University of Western Australia. The authors are grateful to N. Marba, G. Bastyan, G. Davis, M. Rozaimi and D. Kyrwood for their help in field and/or laboratory tasks.
JournalGlobal Change Biology
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