@article {1606,
	title = {Cupuladria canariensis (Busk) - portrait of a bryozoan},
	journal = {Palaeontology},
	volume = {6},
	year = {1963},
	month = {04/1963},
	chapter = {172},
	author = {Lagaaij, R.}
}
@article {562,
	title = {A new ichnogenus for etchings made by cheilostome bryozoans into calcareous substrates},
	journal = {Palaeontology},
	volume = {42},
	year = {1999},
	chapter = {595},
	author = {Taylor, P.D. and Wilson, M.A. and Bromley, R.G.}
}
@article {34,
	title = {Disarticulated bivalve shells as substrates for encrustation by the bryozoan Cribrilina puncturata in the Plio-Pleistocene Red Crag of Eastern England},
	journal = {Palaeontology},
	volume = {31},
	year = {1988},
	chapter = {237},
	abstract = {Cribrilina puncturata (Wood, 1844) forms small, patch-like colonies encrusting the concave (almost invariably lower) surface of disarticulated bivalve mollusc shells in the Plio-Pleistocene Red Crag of eastern England. The species is restricted to the deeper central part of each shell, away from the margin. Peripheral abrasion of the shell{\textquoteright}s surface, which might have removed marginal settlement, is rejected as the major agent in producing the observed distribution. A number of larval behaviour mechanisms that might have been responsible are therefore considered. All are discounted except one: that the larva crept up the slope of the shell{\textquoteright}s inner surface towards the highest point (geonegative movement) before fixation. This hypothesis seems to explain many details of the settlement pattern. C. puncturata apparently exploited the shell{\textquoteright}s major concavity as a refuge from physical disturbance in a high-energy environment, and its larval settlement behaviour appears to have been specialized for concavo-convex (bivalve) substrates. A second category of refuge, minor local concavities anywhere on the shell{\textquoteright}s surface, was occupied during the vulnerable early astogenetic stages of two other bryozoan species, both with a runner-like colony morphology.},
	author = {Bishop, J.D.D.}
}
@article {11,
	title = {Palaeobiology and systematics of large cyclostome bryozoans from the Pliocene Coralline Crag of Suffolk},
	journal = {Palaeontology},
	volume = {25},
	year = {1982},
	month = {07/1982},
	chapter = {529},
	abstract = {Bioclastic sands of the Coralline Crag are characterized by abundant bryozoans including large colonies of four cyclostomes: Blumenbachium globosum Koenig, Meandropora aurantium (Milne Edwards in Lyell), M. tubipora (Busk), and Multifascigera debenensis sp. nov. These species are systematically described and the relationships investigated between colony growth pattern, form, and inferred ecology. Colonies of each species are composed of numerous subcolonies bounded by exterior walls. Times of autonomous subcolony growth were punctuated by periods of subcolony anastomosis. Most colonies acquired a roughly hemispherical shape but others developed a subspheroidal form. The former apparently retained a stable attitude during growth whereas the latter either enveloped an unstable substrate (circumrotatory growth) or were attached to a perishable substrate which supported the colony above the sea-bed. Colonies are absent from the turbulent sandwave facies of the Coralline Crag but are present in other facies where mobile animals rather than currents may have been responsible for overturning circumrotatory colonies. Evolution of exterior wall-bounded subcolonies, known in many post-Palaeozoic cyclostomes, was possible because interzooidal pores allowed soft tissue connection between subcolonies beneath the colony surface when soft tissue was absent above it. The localization of coelomic damage may have been a factor in the success of this type of organization.},
	issn = {0031-0239},
	url = {http://palaeontology.palass-pubs.org/pdf/Vol\%2025/Pages\%20529-554.pdf},
	author = {Balson, Peter S. and Taylor, P.D.}
}
