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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>J. Joseph Giersch</dc:contributor>
  <dc:contributor>Debra S. Finn</dc:contributor>
  <dc:contributor>Lusha M. Tronstad</dc:contributor>
  <dc:contributor>Steve Jordan</dc:contributor>
  <dc:contributor>Larry Serpa</dc:contributor>
  <dc:contributor>Ronald Call</dc:contributor>
  <dc:contributor>Clint C. Muhlfeld</dc:contributor>
  <dc:contributor>David W. Weisrock</dc:contributor>
  <dc:creator>Scott Hotaling</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description>&lt;ol class=""&gt;&lt;li&gt;Comparative population genetic studies provide a powerful means for assessing the degree to which evolutionary histories may be congruent among taxa while also highlighting the potential for cryptic diversity within existing species.&lt;/li&gt;&lt;li&gt;In the Rocky Mountains, three confamilial stoneflies (&lt;i&gt;Zapada glacier&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;,&lt;i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;Lednia tumana&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;, and&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Lednia tetonica&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;; Plecoptera, Nemouridae) occupy cold alpine streams that are primarily fed by melting ice.&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Lednia tumana&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;and&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;L.&amp;nbsp;tetonica&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;are sister species diagnosed from systematic morphological differences, and they are endemic to areas surrounding Glacier National Park and Grand Teton National Park, respectively, in the U.S. Rocky Mountains.&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Zapada glacier&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;is also present in alpine streams from Glacier National Park to the Teton Range, sometimes co‐occurring with either&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Lednia&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;species.&lt;/li&gt;&lt;li&gt;We used mitochondrial sequence data to clarify species boundaries, compare population genetic patterns, and test demographic models in a coalescent framework for the three stoneflies. We addressed four questions: (1) Is there genetic support for the morphology‐based species boundaries in&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Lednia&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;? (2) Is there genetic support for cryptic, or as‐yet undescribed, diversity within&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Z.&amp;nbsp;glacier&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;? (3) Do similar geographic distributions and ecological requirements yield spatial congruence of genetic structure between high‐elevation&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Lednia&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;and&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Z.&amp;nbsp;glacier&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;populations? (4) Is there evidence for contemporary gene flow among isolated populations in either group?&lt;/li&gt;&lt;li&gt;Our results supported the existing taxonomy with&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Z.&amp;nbsp;glacier&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;and the two&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Lednia&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;species differing in their depths of divergence among study regions (e.g. maximum sequence divergence within&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Z.&amp;nbsp;glacier&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;&amp;nbsp;=&amp;nbsp;1.2% versus 5% between&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;L.&amp;nbsp;tumana&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;and&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;L.&amp;nbsp;tetonica&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;). However, spatial population genetic patterns were broadly congruent, indicating stonefly populations isolated on mountaintop islands. Coalescent modelling supported the possibility of rare, extremely limited contemporary gene flow among&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Z.&amp;nbsp;glacier&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;populations, with no support for gene flow between&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;L.&amp;nbsp;tumana&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;and&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;L.&amp;nbsp;tetonica&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;/i&gt;.&lt;/li&gt;&lt;li&gt;The focal stoneflies and associated assemblages occupy the highest elevation, coldest permanent alpine streams in the study region. This lotic habitat type faces an uncertain future under a diminishing alpine cryosphere. Given spatial congruence of genetic structure demonstrating unique biodiversity associated with individual alpine islands, we encourage conservation management strategies be developed and applied at corresponding spatial scales.&lt;/li&gt;&lt;/ol&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/fwb.13223</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>Congruent population genetic structure but differing depths of divergence for three alpine stoneflies with similar ecology and geographic distributions</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>