Proceedings of the Royal Society of London. Series B, Biological sciences · 1986 · 17 citations · 13 references
Life SciencesBiologyEvolutionary BiologyEvolutionary PaleontologyMacroevolutionSystematic PaleontologyFunctional MorphologyMorphological SystematicsCiliary BiologyCiliary StructureColonial OrganismsFossil Developmental MorphologyLong-term Evolutionary Trends
Abstract Graptolites were ciliary-feeding, colonial animals; their small (1‒3 mm) zooids were supported by tubular periderm. Bush- or tree-like colonies attached to the sea floor gave rise to planktonic colonies held in suspension by their ciliary currents. Adaptation to automobility led to a reversal of the evolutionary trends that characterize most colonial organisms; the outreaching branching patterns of the sessile colonies became gradually simplified, and this led to the evolution of small, active, streamlined superindividuals. Constructed of ‘collagenous’ increments made up of three or four fibrillar fabrics, graptolite periderm appears to be unique and almost indestructible. Whether graptolites became extinct or returned neotenously to individuality, losing their characteristic periderm, is discussed in this paper.
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