<?xml version='1.0' encoding='utf-8'?>
<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>Anastasios Stathakopoulos</dc:contributor>
  <dc:contributor>Ilsa B. Kuffner</dc:contributor>
  <dc:contributor>Robert R. Ruzicka</dc:contributor>
  <dc:contributor>Michael A. Colella</dc:contributor>
  <dc:contributor>Eugene A. Shinn</dc:contributor>
  <dc:creator>Lauren T. Toth</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Over the last half century, climate change, coral disease, and other anthropogenic disturbances have restructured coral-reef ecosystems on a global scale. The disproportionate loss of once-dominant, reef-building taxa has facilitated relative increases in the abundance of “weedy” or stress-tolerant coral species. Although the recent transformation of coral-reef assemblages is unprecedented on ecological timescales, determining whether modern coral reefs have truly reached a novel ecosystem state requires evaluating the dynamics of reef composition over much longer periods of time. Here, we provide a geologic perspective on the shifting composition of Florida's reefs by reconstructing the millennial-scale spatial and temporal variability in reef assemblages using 59 Holocene reef cores collected throughout the Florida Keys Reef Tract (FKRT). We then compare the relative abundances of reef-building species in the Holocene reef framework to data from contemporary reef surveys to determine how much Florida's modern reef assemblages have diverged from long-term baselines. We show that the composition of Florida's reefs was, until recently, remarkably stable over the last 8000&amp;nbsp;yr. The same corals that have dominated shallow-water reefs throughout the western Atlantic for hundreds of thousands of years,&amp;nbsp;&lt;/span&gt;&lt;i&gt;Acropora palmata&lt;/i&gt;&lt;span&gt;,&lt;/span&gt;&lt;i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;Orbicella&lt;/i&gt;&lt;span&gt;&amp;nbsp;spp., and other massive coral taxa, accounted for nearly 90% of Florida's Holocene reef framework. In contrast, the species that now have the highest relative abundances on the FKRT, primarily&amp;nbsp;&lt;/span&gt;&lt;i&gt;Porites astreoides&lt;/i&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;Siderastrea siderea&lt;/i&gt;&lt;span&gt;, were rare in the reef framework, suggesting that recent shifts in species assemblages are unprecedented over millennial timescales. Although it may not be possible to return coral reefs to pre-Anthropocene states, our results suggest that coral-reef management focused on the conservation and restoration of the reef-building species of the past, will optimize efforts to preserve coral reefs, and the valuable ecosystem services they provide into the future.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1002/ecy.2781</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Ecological Society of America</dc:publisher>
  <dc:title>The unprecedented loss of Florida's reef-building corals and the emergence of a novel coral-reef assemblage</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>