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Journal of Paleontology; November 1961; v. 35; no. 6; p. 1113-1116
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Auloblastus, a new blastoid from the Mississippian Burlington limestone

Harold Hartman Beaver

Auloblastus clinei, a large spiraculate blastoid from the Upper Burlington of southwestern Missouri, differs from other blastoids in a combination of morphologic features, including the number of hydrospires, the radial-deltoid relationship, and the lack of a hydrospire plate. Two previously undescribed passageways, the lateral canals, are recognized; these canals parallel the median groove and are excavated into lancet and side-plate material along the lancet-side plate suture.

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