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Aaglacrinus
''Aaglacrinus'' is an extinct species of crinoidea in the ''Cladia'' order.〔http://paleobackup.nceas.ucsb.edu:8090/cgi-bin/bridge.pl〕〔http://www.paleodb.org/cgi-bin/bridge.pl?action=displayTaxonomicNamesAndOpinions&reference_no=6930&display=opinions〕〔http://paleodb.org/cgi-bin/bridge.pl?action=displayTaxonomicNamesAndOpinions&reference_no=6930&display=authorities〕〔New crinoids from the Naco Formation (middle Pennsylvanian) of Arizona and a revision of the family Cromyocrinidae. Journal of Paleontology, 55(6) 1981: 1176-1199. (Record Volume 118 )〕〔http://www.ubio.org/browser/details.php?namebankID=6942808〕 It has been proposed that it was a stationary (attached) suspension feeder the hard parts of which were composed of magnesium calcite.〔http://paleobackup.nceas.ucsb.edu:8090/cgi-bin/bridge.pl〕〔http://paleobackup.nceas.ucsb.edu:8090/cgi-bin/bridge.pl?action=displayReference&reference_no=9940〕
==Species==
There are currently 2 species in this genus, both of which are under the name ''Aaglaocrinus'':
*''Aaglaocrinus bowsheri'' (Webster & Kues, 2006)〔Pennsylvanian crinoids of New Mexico. New Mexico Geology, 28(1), February 2006: 3-37. (Record Volume 143 )〕〔http://www.organismnames.com/details.htm?lsid=1889131〕
*''Aaglaocrinus sphaeri'' (Strimple 1949)〔http://www.ubio.org/browser/details.php?namebankID=6942813〕〔http://www.ubio.org/browser/details.php?namebankID=6942814〕〔http://www.organismnames.com/details.htm?lsid=234197〕
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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