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The science of tectonics is linked to climate change and sea-level rise in the most unexpected ways. When an earthquake occurs, for example, a tectonic fault ruptures and causes short-term deformations, such as vertical land motion – a shift in the earth that influences sea-level rise by literally raising or lowering the seabed – it forms a link to climate change that is not immediately apparent.
The past sea levels of the Holocene period can be reconstructed via the use of paleo-proxies, including the use of mangrove sediments, which contain organic materials that can be carbon-dated and serve as age markers.