<?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>Erica L. Ashe</dc:contributor>
  <dc:contributor>Ryan P. Moyer</dc:contributor>
  <dc:contributor>Andrew C. Kemp</dc:contributor>
  <dc:contributor>Simon E. Engelhart</dc:contributor>
  <dc:contributor>Matthew J. Brain</dc:contributor>
  <dc:contributor>Lauren T. Toth</dc:contributor>
  <dc:contributor>Amanda R. Chappel</dc:contributor>
  <dc:contributor>Margaret Christie</dc:contributor>
  <dc:contributor>Robert E. Kopp</dc:contributor>
  <dc:contributor>Benjamin P. Horton</dc:contributor>
  <dc:creator>Nicole S. Khan</dc:creator>
  <dc:date>2022</dc:date>
  <dc:description>&lt;div id="abstracts" class="Abstracts u-font-serif"&gt;&lt;div id="ab0005" class="abstract author" lang="en"&gt;&lt;div id="as0005"&gt;&lt;p id="sp0070"&gt;&lt;span&gt;A paucity of detailed relative sea-level (RSL) reconstructions from low latitudes hinders efforts to understand the global, regional, and local processes that cause&amp;nbsp;RSL change. We reconstruct RSL change during the past ~5&amp;nbsp;ka using cores of&amp;nbsp;mangrove&amp;nbsp;&lt;/span&gt;peat&lt;span&gt;&amp;nbsp;at two sites (Snipe Key and Swan Key) in the Florida Keys.&amp;nbsp;Remote sensing&amp;nbsp;and field surveys established the relationship between peat-forming mangroves and tidal elevation in South Florida. Core chronologies are developed from age-depth models applied to 72 radiocarbon dates (39 mangrove wood macrofossils and 33 fine-fraction bulk peat). RSL rose 3.7&amp;nbsp;m at Snipe Key and 5.0&amp;nbsp;m at Swan Key in the past 5&amp;nbsp;ka, with both sites recording the fastest century-scale rate of&amp;nbsp;RSL rise&amp;nbsp;since ~1900&amp;nbsp;CE (~2.1&amp;nbsp;mm/a). We demonstrate that it is feasible to produce near-continuous reconstructions of RSL from mangrove peat in regions with a microtidal regime and accommodation space created by millennial-scale RSL rise. Decomposition of RSL trends from a network of reconstructions across South Florida using a spatio-temporal model suggests that Snipe Key was representative of regional RSL trends, but Swan Key was influenced by an additional local-scale process acting over at least the past five millennia. Geotechnical analysis of modern and buried mangrove peat indicates that sediment compaction is not the local-scale process responsible for the exaggerated RSL rise at Swan Key. The substantial difference in RSL between two nearby sites highlights the critical need for within-region replication of RSL reconstructions to avoid misattribution of sea-level trends, which could also have implications for geophysical modeling studies using RSL data for model tuning and validation.&lt;/span&gt;&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.gloplacha.2022.103902</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Relative sea-level change in South Florida during the past ~5000 years</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>