<?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>Jennifer A. Flannery</dc:contributor>
  <dc:contributor>Lauren T. Toth</dc:contributor>
  <dc:creator>Philip M. Gravinese</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;p&gt;The larvae of the Florida stone crab, &lt;i&gt;Menippe mercenaria&lt;/i&gt;, migrate through a variety of habitats as they develop and, therefore, experience a broad range of environmental conditions through ontogeny. Environmental variability experienced by the larvae may result in distinct elemental signatures within the exoskeletons, which could provide a tool for tracking the environmental history of larval stone crab populations. A method was developed to examine trace-element ratios, specifically magnesium-to-calcium (Mg/Ca) and strontium-to-calcium (Sr/Ca) ratios, in the exoskeletons of &lt;i&gt;M. mercenaria&lt;/i&gt; larvae. Two developmental stages of stone crab larvae were analyzed—stage III and stage V. Specimens were reared in a laboratory environment under stable conditions to quantify the average ratios of Mg/Ca and Sr/Ca of larval stone crab exoskeletons and to determine if the ratios differed through ontogeny. The elemental compositions (Ca, Mg, and Sr) in samples of stage III larvae (n = 50 per sample) from 11 different broods (mean Sr/Ca = 5.916 ± 0.161 millimole per mole [mmol mol&lt;sup&gt;−1&lt;/sup&gt;]; mean Mg/Ca = 218.275 ± 59.957 mmol mol&lt;sup&gt;−1&lt;/sup&gt;) and stage V larvae (n = 10 per sample) from 12 different broods (mean Sr/Ca = 6.110 ± 0.300 mmol mol&lt;sup&gt;−1&lt;/sup&gt;; mean Mg/Ca = 267.081 ± 67.211 mmol mol&lt;sup&gt;–1&lt;/sup&gt;) were measured using inductively coupled plasma optical emission spectrometry (ICP–OES). The ratio of Sr/Ca significantly increased from stage III to stage V larvae, suggesting an ontogenic shift in Sr/Ca ratios between larval stages. The ratio of Mg/Ca did not change significantly between larval stages, but variability among broods was high. The method used to examine the trace-element ratios provided robust, highly reproducible estimates of Sr/Ca and Mg/Ca ratios in the larvae of &lt;i&gt;M. mercenaria&lt;/i&gt;, demonstrating that ICP–OES can be used to determine the trace-element composition of chitinous organisms like the Florida stone crab.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20161148</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>A methodology for quantifying trace elements in the exoskeletons of Florida stone crab (&lt;i&gt;Menippe mercenaria&lt;/i&gt;) larvae using inductively coupled plasma optical emission spectrometry (ICP–OES) </dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>