<?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>David A. Stonestrom</dc:contributor>
  <dc:contributor>Guntram von Kiparski</dc:contributor>
  <dc:contributor>Corey R. Lawrence</dc:contributor>
  <dc:contributor>C.A. Masiello</dc:contributor>
  <dc:contributor>Arthur F. White</dc:contributor>
  <dc:contributor>John Fitzpatrick</dc:contributor>
  <dc:creator>Marjorie S. Schulz</dc:creator>
  <dc:date>2011</dc:date>
  <dc:description>&lt;div id="aep-abstract-id15" class="abstract author" lang="en"&gt;&lt;div id="aep-abstract-sec-id16"&gt;&lt;p id="sp005"&gt;Concentrations of CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;in soil atmosphere and CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;efflux were measured across a marine terrace soil chronosequence near Santa Cruz, California. Soil development, specifically the formation of an argillic horizon, has created a two-tier soil gas profile in the older terrace soils. The soil above the argillic horizon has seasonal variations in soil CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;associated with plant respiration. The older soils with dense argillic horizons maintain a year round ∼1%CO&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;below the argillic horizon. The CO&lt;sub&gt;2&lt;/sub&gt;efflux during the growing season is higher on the older terraces.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.apgeochem.2011.03.048</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Elsevier </dc:publisher>
  <dc:title>Seasonal dynamics of CO2 profiles across a soil chronosequence, Santa Cruz, California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>