Evolution of the Great Barrier Reef Halimeda carbonate factory in response to Holocene environmental changes, determined from radiocarbon and nitrogen isotope measurements

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dc.contributor.authorMcNeil, Men_AU
dc.contributor.authorHua, Qen_AU
dc.contributor.authorErler, DVen_AU
dc.contributor.authorNothdurft, LDen_AU
dc.contributor.authorWebster, JMen_AU
dc.contributor.authorMoss, Pen_AU
dc.date.accessioned2023-01-19T05:10:46Zen_AU
dc.date.available2023-01-19T05:10:46Zen_AU
dc.date.issued2021-11-17en_AU
dc.date.statistics2022-05-27en_AU
dc.description.abstractThe inter-reef Halimeda algal bioherms of the northern Great Barrier Reef (GBR) have accumulated up to 25 m of positive relief and up to four times greater volume of calcium carbonate than the nearby coral reefs during the Holocene. Covering > 6000 km² on the continental shelf, the Halimeda bioherms represent a significant contribution to the development of the northeast Australian neritic carbonate factory and sedimentary archive of post-glacial environmental changes. However, the geochronological record of initiation and development of the Halimeda bioherm carbonate factory throughout the Holocene was poorly constrained and based on very few radiocarbon dates, considering their vast area. Additionally, the main source of nitrogen (N) fuelling the productivity of these biogenic structures had not been traced geochemically, and there was no understanding of any temporal variation. A total of 63 samples of calcium carbonate Halimeda and foraminifera grains, mollusc shells, and bulk soil were dated by ¹⁴ C AMS using the VEGA facility at the ANSTO Centre for Accelerator Science. Changes in the terrestrial vegetation community were determined from palynological analysis at the University of Queensland. Nitrogen isotopes were measured on a subset of 27 Halimeda samples using isotope ratio mass spectrometry (IRMS) at the Centre for Coastal Biogeochemistry at Southern Cross University. Using the persulfate-denitrifier method previously developed for foraminifera and coral skeletal material, nitrogen bound within the Halimeda skeletal organic material (SOM) was targeted. This allowed for fossil samples down-core to be analysed, thus providing a 5000-year record of Halimeda δ¹⁵ N-SOM. A temporal sequence of facies transitions that record terrestrial and marine environmental changes over a full sea level cycle from the Last Interglacial, to Last Glacial Maximum (LGM) and deglacial, to transgressive estuarine sediments and shallow marine carbonates was reconstructed. Halimeda growth and carbonate deposition had established by 11,143 (+237/-277) cal. yr BP, just ~450 years after the marine transgression. The Halimeda carbonate factory was productive at least 2100 years earlier than Holocene coral reefs in the study area. Our results provide the first direct in-situ measurements of Halimeda bioherm ages from at or near the Holocene/Pleistocene boundary, recording the timing of bioherm initiation in response to post-glacial sea level rise. The average Halimeda skeletal δ¹⁵ N-SOM was 6.28 ± 0.26 ‰, consistent with δ¹⁵ N-NO₃ - from western tropical South Pacific (WTSP) thermocline waters, geochemically validating shelf-break upwelling of an oceanic N source. From 5000 to 2000 cal. yr BP, Halimeda δ¹⁵ N-SOM decreased by 1-2 ‰, reaching a minima of 5.5 ‰ that persisted for almost 1000 years. The Halimeda δ¹⁵ N-SOM variation reflects changes in regional climate and intensified El Niño activity and is consistent with other regional climate proxy records at this time. Thus, the inter-reef Halimeda algal bioherms of the GBR are an important carbonate ecosystem that record a >10,000-year near-continuous record of northeast Australian Holocene oceanographic and environmental changes in response to sea level and climatic drivers, potentially filling spatial and temporal gaps not covered by coral and other proxies. © The Authorsen_AU
dc.identifier.citationMcNeil, M., Hua, Q., Erler, D., Northdurft, L., Webster, J., Moss, P. (2021). Evolution of the Great Barrier Reef Halimeda carbonate factory in response to Holocene environmental changes, determined from radiocarbon and nitrogen isotope measurements. Paper presented to the 15th International Conference on Accelerator Mass Spectrometry. ANSTO Sydney, Australia. November 15th – 19th, (pp. 35). Retrieved from: https://ams15sydney.com/wp-content/uploads/2021/11/AMS-15-Full-Program-and-Abstract-Book-R-1.pdfen_AU
dc.identifier.conferenceenddate19 November 2021en_AU
dc.identifier.conferencename15th International Conference on Accelerator Mass Spectrometryen_AU
dc.identifier.conferenceplaceSydney, Australiaen_AU
dc.identifier.conferencestartdate15 November 2021en_AU
dc.identifier.pagination35en_AU
dc.identifier.urihttps://ams15sydney.com/wp-content/uploads/2021/11/AMS-15-Full-Program-and-Abstract-Book-R-1.pdfen_AU
dc.identifier.urihttps://apo.ansto.gov.au/dspace/handle/10238/14411en_AU
dc.language.isoenen_AU
dc.publisherAustralian Nuclear Science and Technology Organisationen_AU
dc.subjectReefsen_AU
dc.subjectCoral reefsen_AU
dc.subjectQueenslanden_AU
dc.subjectAustraliaen_AU
dc.subjectCalcium carbonatesen_AU
dc.subjectQuaternary perioden_AU
dc.subjectGlaciersen_AU
dc.subjectMolluscsen_AU
dc.subjectNitrogenen_AU
dc.subjectFossilsen_AU
dc.subjectSedimentsen_AU
dc.titleEvolution of the Great Barrier Reef Halimeda carbonate factory in response to Holocene environmental changes, determined from radiocarbon and nitrogen isotope measurementsen_AU
dc.typeConference Abstracten_AU
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