<?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>C.E.G.R. Schaefer</dc:contributor>
  <dc:contributor>E.S. Mendonca</dc:contributor>
  <dc:contributor>I.R. Silva</dc:contributor>
  <dc:contributor>R.M. Santana</dc:contributor>
  <dc:contributor>A.S.S. Ribeiro</dc:contributor>
  <dc:creator>F.N.B. Simas</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>Recent works show that organic matter accumulation in some soils from coastal Antarctica is higher than 
previously expected. The objective of the present work was to estimate the organic C stocks for soils from maritime 
Antarctica. Cryosols from subpolar desert landscapes presented the lowest organic C stocks. Ornithogenic soils are the 
most important C reservoirs in terrestrial ecosystems in this part of Antarctica. Although these soils correspond to only 
2.5 % of the ice-free areas at Admiralty Bay, they contain approximately 20 % of the estimated C stock. Most of the 
organic C in the studied soils is stored in the active layer but in some cases the C is also stored in the permafrost.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20071047SRP076</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S Geological Survey</dc:publisher>
  <dc:title>Organic carbon stocks in permafrost-affected soils from Admiralty Bay, Antarctica</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>