Abstract
Two major patterns of shell morphogenesis occurring in varying proportions among species were identified by examining skeletons from five species of living collosphaerid, colonial Radiolaria: Collosphaera huxleyi, Acrosphaera cyrtodon, Acrosphaera spinosa, Siphonosphaera tubulosa and Siphonosphaera socialis. Skeletons possessing large open-lattice structures characterized by ellipsoidal to polygonal pores separated by narrow bars are produced by repeated subdivision of large pores into smaller pores. A bridge-like bar grows across the pore and subdivides it into two or more smaller pores. In skeletons with small, nearly circular pores and occasionally elongated tubular rims, the pores appear to be developed by rim thickening. Silica is deposited at the perimeter of the pore, thus decreasing its diameter and increasing the bar width between pores. In some species exhibiting intermediate types of skeletal morphology, there appears to be varying amounts of both bridge growth and rim growth. These data are used to explore possible phylogenetic pathways for a variety of collosphaerid species and to elucidate the processes of skeletal deposition in Radiolaria.
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