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Global distribution of relative sea-level d
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Classroom Contents
Late Holocene Relative Sea-Level Change with Mangrove Sediments in the Western Pacific Ocean
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- 1 Intro
- 2 Why sea level is not level
- 3 Longer-term processes + future projectio
- 4 Global distribution of relative sea-level d
- 5 Sea-level proxy: mangrove sediment
- 6 Proxy sea-level reconstruction
- 7 Glacial-isostatic model predictions
- 8 Potential processes of regional subsiden
- 9 Absence of a mid-Holocene highstand
- 10 Future implications
- 11 Sea level & the peopling of Remote Ocea
- 12 Implications for cultural heritage
- 13 Key points
- 14 Acknowledgements
