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Outputs (4)

Relative sea level response to mixed carbonate-siliciclastic sediment loading along the Great Barrier Reef margin (2023)
Journal Article
Lin, Y., Whitehouse, P. L., Hibbert, F. D., Woodroffe, S. A., Hinestrosa, G., & Webster, J. M. (2023). Relative sea level response to mixed carbonate-siliciclastic sediment loading along the Great Barrier Reef margin. Earth and Planetary Science Letters, 607, Article 118066. https://doi.org/10.1016/j.epsl.2023.118066

The continental shelf along northeastern Australia is the world’s largest mixed carbonate-siliciclastic passive margin and the location of the Great Barrier Reef (GBR). Following sea-level transgression during the last deglaciation, extensive sedimen... Read More about Relative sea level response to mixed carbonate-siliciclastic sediment loading along the Great Barrier Reef margin.

Stability of the Antarctic Ice Sheet during the pre-Industrial Holocene (2022)
Journal Article
Jones, R., Johnson, J., Lin, Y., Mackintosh, A., Sefton, J., Smith, J., Thomas, E., & Whitehouse, P. (2022). Stability of the Antarctic Ice Sheet during the pre-Industrial Holocene. Nature Reviews Earth & Environment, 3(8), 500-515. https://doi.org/10.1038/s43017-022-00309-5

The rate and magnitude of the Antarctic Ice Sheet (AIS) contribution to global sea-level rise beyond 2100 CE remains highly uncertain. Past changes of the AIS, however, offer opportunities to understand contemporary and future ice sheet behaviour. In... Read More about Stability of the Antarctic Ice Sheet during the pre-Industrial Holocene.

A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting (2021)
Journal Article
Lin, Y., Hibbert, F., Whitehouse, P., Woodroffe, S., Purcell, A., Shennan, I., & Bradley, S. (2021). A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting. Nature Communications, 12, Article 2015. https://doi.org/10.1038/s41467-021-21990-y

The most rapid global sea-level rise event of the last deglaciation, Meltwater Pulse 1A (MWP-1A), occurred ∼14,650 years ago. Considerable uncertainty regarding the sources of meltwater limits understanding of the relationship between MWP-1A and the... Read More about A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting.