<?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>Matt McCarthy</dc:contributor>
  <dc:contributor>Hilary G. Close</dc:contributor>
  <dc:contributor>Amanda Demopoulos</dc:contributor>
  <dc:contributor>Nancy G. Prouty</dc:contributor>
  <dc:creator>Natasha Vokhshoori</dc:creator>
  <dc:date>2021</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;In order to reconstruct the ecosystem structure of chemosynthetic environments in the fossil record, geochemical proxies must be developed. Here, we present a suite of novel compound-specific isotope parameters for tracing chemosynthetic production with a focus on understanding nitrogen dynamics in deep-sea cold seep environments. We examined the chemosymbiotic bivalve&amp;nbsp;&lt;/span&gt;&lt;i&gt;Bathymodiolus childressi&lt;/i&gt;&lt;span&gt;&amp;nbsp;from three geographically distinct seep sites on the NE Atlantic Margin and compared isotope data to non-chemosynthetic littoral mussels to test whether water depth, seep activity, and/or mussel bed size are linked to differences in chemosynthetic production. The bulk isotope analysis of carbon (δ&lt;/span&gt;&lt;sup&gt;13&lt;/sup&gt;&lt;span&gt;C) and nitrogen (δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N), and δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N values of individual amino acids (δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N&lt;/span&gt;&lt;sub&gt;AA&lt;/sub&gt;&lt;span&gt;) in both gill and muscle tissues, as well as δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N&lt;/span&gt;&lt;sub&gt;AA-&lt;/sub&gt;&lt;span&gt;derived parameters including trophic level (TL), baseline δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N value (δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N&lt;/span&gt;&lt;sub&gt;Phe&lt;/sub&gt;&lt;span&gt;), and a microbial resynthesis index (Σ&lt;/span&gt;&lt;i&gt;V&lt;/i&gt;&lt;span&gt;), were used to investigate specific geochemical signatures of chemosynthesis. Our results show that δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N&lt;/span&gt;&lt;sub&gt;AA&lt;/sub&gt;&lt;span&gt;&amp;nbsp;values provide a number of new proxies for relative reliance on chemosynthesis, including TL, ∑V, and both δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N values and molar percentages (Gly/Glu mol% index) of specific AA. Together, these parameters suggested that relative chemoautotrophy is linked to both degree of venting from seeps and mussel bed size. Finally, we tested a Bayesian mixing model using diagnostic AA δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N values, showing that percent contribution of chemoautotrophic versus heterotrophic production to seep mussel nutrition can be directly estimated from δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N&lt;/span&gt;&lt;sub&gt;AA&lt;/sub&gt;&lt;span&gt;&amp;nbsp;values. Our results demonstrate that δ&lt;/span&gt;&lt;sup&gt;15&lt;/sup&gt;&lt;span&gt;N&lt;/span&gt;&lt;sub&gt;AA&lt;/sub&gt;&lt;span&gt;&amp;nbsp;analysis can provide a new set of geochemical tools to better understand mixotrophic ecosystem function and energetics, and suggest extension to the study of ancient chemosynthetic environments in the fossil record.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/gbi.12458</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley</dc:publisher>
  <dc:title>New geochemical tools for investigating resource and energy functions at deep-sea cold seeps using amino-acid δ15N in chemosymbiotic mussels (Bathymodiolus childressi)</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>