<?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>Belle E. Philibosian</dc:contributor>
  <dc:contributor>Aron J. Meltzner</dc:contributor>
  <dc:contributor>Chung-Che Wu</dc:contributor>
  <dc:contributor>Chuan-Chou Shen</dc:contributor>
  <dc:contributor>R. Lawrence Edwards</dc:contributor>
  <dc:contributor>Chih-Kai Chuang</dc:contributor>
  <dc:contributor>Bambang W. Suwargadi</dc:contributor>
  <dc:contributor>Danny H. Natawidjaja</dc:contributor>
  <dc:creator>Hong-Wei Chiang</dc:creator>
  <dc:date>2023</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;One of the key factors in obtaining precise and accurate&amp;nbsp;&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th ages of corals, especially for corals with ages less than a few thousand years, is the correction for non-radiogenic&amp;nbsp;&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th based on an initial&amp;nbsp;&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th/&lt;/span&gt;&lt;sup&gt;232&lt;/sup&gt;&lt;span&gt;Th value (&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th/&lt;/span&gt;&lt;sup&gt;232&lt;/sup&gt;&lt;span&gt;Th&lt;/span&gt;&lt;sub&gt;0&lt;/sub&gt;&lt;span&gt;). Studies that consider coral&amp;nbsp;&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th/&lt;/span&gt;&lt;sup&gt;232&lt;/sup&gt;&lt;span&gt;Th&lt;/span&gt;&lt;sub&gt;0&lt;/sub&gt;&lt;span&gt;&amp;nbsp;values in intertidal environments are limited, and it is in these environments that corals have Th concentrations 100–1000 times greater than open-ocean corals. Here we present 66 reconstructed U–Th isochrons of modern and&amp;nbsp;Holocene&amp;nbsp;&lt;/span&gt;&lt;i&gt;Porites lutea&lt;/i&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;lobata&lt;/i&gt;&lt;span&gt;&amp;nbsp;corals from throughout the Sumatran forearc islands (SFI). Mean square of weighted deviates (&lt;/span&gt;&lt;i&gt;MSWD&lt;/i&gt;&lt;span&gt;) is used to evaluate the variabilities of 28 location-specific&amp;nbsp;&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th/&lt;/span&gt;&lt;sup&gt;232&lt;/sup&gt;&lt;span&gt;Th0 values before the regional mean. Results show no significant spatial difference between the means of 3.1&amp;nbsp;±&amp;nbsp;3.2&amp;nbsp;×&amp;nbsp;10&lt;/span&gt;&lt;sup&gt;−6&lt;/sup&gt;&lt;span&gt;&amp;nbsp;for the northern SFI and 4.7&amp;nbsp;±&amp;nbsp;1.3&amp;nbsp;×&amp;nbsp;10&lt;/span&gt;&lt;sup&gt;−6&lt;/sup&gt;&lt;span&gt;&amp;nbsp;for the southern SFI. Using the weighted mean of 4.3&amp;nbsp;±&amp;nbsp;2.5&amp;nbsp;×&amp;nbsp;10&lt;/span&gt;&lt;sup&gt;−6&lt;/sup&gt;&lt;span&gt;&amp;nbsp;for all islands has the advantage that no data need be subjectively excluded in the calculation of reliable&amp;nbsp;&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th ages, where a local initial value is unknown. There were no clear centennial to millennial time-scale changes in&amp;nbsp;&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th/&lt;/span&gt;&lt;sup&gt;232&lt;/sup&gt;&lt;span&gt;Th&lt;/span&gt;&lt;sub&gt;0&lt;/sub&gt;&lt;span&gt;&amp;nbsp;in the past 2500 years. This study, therefore, suggests a reliable value of initial&amp;nbsp;&lt;/span&gt;&lt;sup&gt;230&lt;/sup&gt;&lt;span&gt;Th/&lt;/span&gt;&lt;sup&gt;232&lt;/sup&gt;&lt;span&gt;Th ratio in intertidal environments.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.quascirev.2023.108005</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier</dc:publisher>
  <dc:title>Investigating spatio-temporal variability of initial 230Th/232Th in intertidal corals</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>