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View - Kowalewski, M. - Virginia Tech

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PALEONTOLOGICAL SOCIETY PAPERS, V. 8, 2002lack a significant fossil record—or by theectoparasitism of leeches. A second route is throughsmall size and inconspicuousness in free-livingforms, exemplified by rotifers, turbellarianflatworms, and some nemerteans that occur as soiland litter meiofauna. Third, there has been thedevelopment of an external, mineralized, protectiveshell, as in the vast majority of pulmonategastropods. Fourth, terrestrialization has beenaccompanied by infaunalization within soils andother moist habitats, as typified by relatively largeanimals such as oligochaetes and some nemerteans.The only large, free-living exceptions to the aboveoptions are the shelless pulmonates, or slugs, whichare rarely predaceous, exude copious amounts ofslime, and probably are defended by noxiouscompounds in their tissues (Greene, 1975).1. Acanthocephalans. Acanthocephalans areobligate endoparasites of the alimentary tract ofvertebrates, especially teleost fish, although aminority of species infect arthropods such asterrestrial crustaceans and insects as intermediatehosts (Conway Morris and Crompton 1982).Historically, acanthocephalans have beenconsidered to have their origin among thepseudocoelmate “aschelminth” phyla, although ithas been suggested that they are closely related tothe Priapulida; both of these groups were diverseduring the Cambrian (Conway Morris, 1981; butsee Barnes et al., 1993). Unlike the arthropod-likeonychophorans, tardigrades, and pentastomes (seebelow), acanthocephalans lack a continental or pre-Cenozoic fossil record. It has been speculated(Brusca and Brusca, 1990) that they may have hadan evolutionary trajectory similar to thepentastomes—endoparasitism of primitive marinevertebrates and subsequent evolution parallellingvertebrate phylogeny, including terrestrializationalong with an early, land-based, tetrapod stock(Brusca and Brusca, 1990).2. Rotifers. Of the continental phyla, the onewith the smallest individuals is the Rotifera, mostof which are less than a millimeter long. Rotifersfrequently occur in marine and especially freshwaterhabitats, as well as in moist soils and on the wetsurfaces of mosses. Approximately 1,800 specieshave been described, distinguished by the structureof their oral corona—the metrachronally beatingband of cilia encircling the mouth—and the type oftheir mouthpart-like mastax. They are variouslydetritivorous filter feeders, raptorial predators thtingest small animals, or piercers-and-suckers thatfluid-feed on larger prey. A few are parasitic on othermeiofauna, whereas others have entered intomutualistic associations with crustaceans (Bruscaand Brusca, 1990). With regard to the evolution ofvarious carnivorous feeding strategies, the fossilrecord is uninformative, except inasmuch as it candocument the presence of particular clades, such asthe Monogonta in the Eocene (Lutetian) of SouthAustralia (Southcott and Lange, 1971), and theBdelloidea in the Miocene (Aquitanian) ofDominican amber (Poinar and Ricci, 1992).3. Platyhelminths. The Platyhelminthes, orflatworms, include approximately 20,000 namedspecies and constitute one of the simplestmorphological grades of bilaterian metazoans; theyare triploblastic, acoelomate, and dorsoventrallyflattened. The class Turbellaria is free living andgenerally predaceous, although some species aresymbiotic with other invertebrates; by contrast, theclasses Monogenea (single-host flukes), Trematoda(multiple-host flukes), and Cestoda (tapeworms) areall ecto- or endoparasitic on vertebrates and, to alesser extent, cephalopods and crustaceans (Bruscaand Brusca, 1990). One group of flatworms, theAcoela, were once included in the Turbellaria, butnow are considered to be very basal bilateriansunrelated to the lophotrochozoic Platyhelminthes(Ruiz-Trillo et al., 1999). Feeding amongturbellarians is diverse and involves structuralvariations of a well-musculated pharynx for suction,release of mucus for external prey entrapment,capture of small prey by adoral ciliary action, oruse of a copulatory stylet or oral hooks forimpalement of victims. The fossil record of flukesand tapeworms is nonexistent, and that ofturbellarians is confined to the Neogene, with theirearliest occurrence in the late Miocene of California(Pierce, 1960). Resistant egg capsules and cocoonshave been documented from the European Pleistocene(Frey, 1964). A putative turbellarian from the late222

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