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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Didier de Bakker</dc:contributor>
  <dc:contributor>Alice Webb</dc:contributor>
  <dc:contributor>Steeve Comeau</dc:contributor>
  <dc:contributor>Ben Harvey</dc:contributor>
  <dc:contributor>Chris Cornwall</dc:contributor>
  <dc:contributor>Lorenzo Alvarez-Filip</dc:contributor>
  <dc:contributor>Esmerelda Perez-Cervantes</dc:contributor>
  <dc:contributor>John T Morris</dc:contributor>
  <dc:contributor>Ian C. Enochs</dc:contributor>
  <dc:contributor>Lauren T. Toth</dc:contributor>
  <dc:contributor>Aaron O'Dea</dc:contributor>
  <dc:contributor>Erin M. Dillon</dc:contributor>
  <dc:contributor>Erik H, Meesters</dc:contributor>
  <dc:contributor>William F. Precht</dc:contributor>
  <dc:creator>Chris T. Perry</dc:creator>
  <dc:date>2025</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Coral reefs form complex physical structures that can help to mitigate coastal flooding risk&lt;/span&gt;&lt;sup&gt;1,2&lt;/sup&gt;&lt;span&gt;. This function will be reduced by sea-level rise (SLR) and impaired reef growth caused by climate change and local anthropogenic stressors&lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;. Water depths above reef surfaces are projected to increase as a result, but the magnitudes and timescales of this increase are poorly constrained, which limits modelling of coastal vulnerability&lt;/span&gt;&lt;sup&gt;4,5&lt;/sup&gt;&lt;span&gt;. Here we analyse fossil reef deposits to constrain links between reef ecology and growth potential across more than 400 tropical western Atlantic sites, and assess the magnitudes of resultant above-reef increases in water depth through to 2100 under various shared socioeconomic pathway (SSP) emission scenarios. Our analysis predicts that more than 70% of tropical western Atlantic reefs will transition into net erosional states by 2040, but that if warming exceeds 2 °C (SSP2–4.5 and higher), nearly all reefs (at least 99%) will be eroding by 2100. The divergent trajectories of reef growth and SLR will thus magnify the effects of SLR; increases in water depth of around 0.3–0.5 m above the present are projected under all warming scenarios by 2060, but depth increases of 0.7–1.2 m are predicted by 2100 under scenarios in which warming surpasses 2 °C. This would increase the risk of flooding along vulnerable reef-fronted coasts and modify nearshore hydrodynamics and ecosystems. Reef restoration offers one pathway back to higher reef growth&lt;/span&gt;&lt;sup&gt;6,7&lt;/sup&gt;&lt;span&gt;, but would dampen the effects of SLR in 2100 only by around 0.3–0.4 m, and only when combined with aggressive climate mitigation.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1038/s41586-025-09439-4</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Nature</dc:publisher>
  <dc:title>Reduced Atlantic reef growth past 2 °C warming amplifies sea-level impacts</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>