<mets:mets LABEL="Eprints Item" xsi:schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-0.xsd" xmlns:xlink="http://www.w3.org/1999/xlink" OBJID="oai:utas.edu.au:3972" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:mods="http://www.loc.gov/mods/v3" xmlns:mets="http://www.loc.gov/METS/"><mets:metsHdr CREATEDATA="2009-01-08T01:32:20Z"><mets:agent TYPE="ORGANIZATION" ROLE="CUSTODIAN"><mets:name>UTas ePrints</mets:name></mets:agent></mets:metsHdr><mets:dmdSec ID="DMD_oai:utas.edu.au:3972_mods"><mets:mdWrap MDTYPE="mods"><mets:xmlData><mods:titleInfo><mods:title>Protists in the marine ice of the Amery Ice Shelf, East Antarctica</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">D</mods:namePart><mods:namePart type="family">Roberts</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">M</mods:namePart><mods:namePart type="family">Craven</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">M</mods:namePart><mods:namePart type="family">Cai</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">I</mods:namePart><mods:namePart type="family">Allison</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">G</mods:namePart><mods:namePart type="family">Nash</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>Samples of marine ice were collected from&#13;
the Amery Ice Shelf, a large embayed ice shelf in East&#13;
Antarctica, during the Austral summer of 2001–2002.&#13;
The samples came from a site ~90 km from the iceberg&#13;
calving front of the shelf, where the ice is 479 m thick&#13;
and the lower 203 m is composed of accreted marine&#13;
ice. Protists identified within the marine ice layer of the&#13;
Amery Ice Shelf include diatoms, chrysophytes, silicoflagellates&#13;
and dinoflagellates. The numerical dominance&#13;
of sea ice indicator diatoms such as&#13;
Fragilariopsis curta, Fragilariopsis cylindrus, Fragilariopsis&#13;
rhombica and Chaetoceros resting spores, and the&#13;
presence of cold open water diatoms such as Fragilariopsis&#13;
kerguelensis and species of Thalassiosira suggest&#13;
the protist composition of the Amery marine ice is&#13;
attributable to seeding from melting pack and/or fast&#13;
ice protist communities in the highly productive waters&#13;
of Prydz Bay to the north.</mods:abstract><mods:classification authority="lcc">260115 Glaciology</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2007</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>Springer-Verlag</mods:publisher></mods:originInfo><mods:genre>Article</mods:genre></mets:xmlData></mets:mdWrap></mets:dmdSec><mets:amdSec ID="TMD_oai:utas.edu.au:3972"><mets:rightsMD ID="rights_oai:utas.edu.au:3972_mods"><mets:mdWrap MDTYPE="mods"><mets:xmlData><mods:useAndReproduction>
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