An orthonectid parasitizing the sabellariid polychaete Sabellaria cementarium Moore has been studied with the aid of a method of impregnation with activated silver albumose (Protargol). This technique differentiates the boundaries of many of the cells, and also brings out the kinetosomes of cilia, thereby permitting a precise analysis of the pattern of ciliation. In adult individuals, the cells of the outer jacket are arranged in rings around the axial mass. Certain of the jacket cells are characterized by presence of conspicuous granules and at least one transverse row of cilia, whereas others have neither obvious granules nor cilia. In both sexes, the first three rings of jacket cells bear three transverse rows of cilia; all other ciliated cells have either one row of cilia near the posterior margins or a row near both the anterior and posterior margins. In typical males, there are 26 or 27 rings, of which rings 6, 10, 12, 15, 17, 20, and 22 are unciliated. In typical females, there are 36 or 37 rings, of which rings 6, 8, 10, 12, 14, 16, and 18 are unciliated. In the male, the mass of gametes or prospective gametes occupies the posterior half of the axial mass. In the female, there is a column of 9 to 12 oocytes occupying the posterior four-fifths of the axial mass. The name Ciliocincta sabellariae gen. n., sp. n. is proposed for this orthonectid. The type locality is near Dot Rock (long 122047.8/ W; lat 48?29.5' N), San Juan Archipelago, Washington. Of 88 worms of the host species examined from this locality, only two (both males) were infected. The few known species of orthonectid mesozoans are parasites of acoel, rhabdocoel, and polyclad turbellarians, nemerteans, polychaete annelids, gastropod and pelecypod molluscs, and ophiuroid echinoderms. Except for one report of an orthonectid parasitizing a nemertean collected near Woods Hole, Massachusetts (Meinkoth, 1956), all published accounts deal with species occurring in the Mediterranean Sea or in the Atlantic waters of Europe. That these interesting organisms will eventually be found in a variety of hosts in North America and elsewhere may confidently be predicted, but attempts to find them on the Pacific coast in invertebrates of the same taxonomic groups as those which they are known to parasitize have until recently been unsuccessful. My discovery of orthonectids, at the Friday Harbor Laboratories of the University of Washington, came about in a nearly fortuitous manner. On 14 July 1962 I collected a large number of brittle stars (Ophiura sarsi) with a view to examining them for orthonectids. After disReceived for publication 31 August 1964. 37 secting over 80 specimens with negative results, I liberated the rest of the catch. Returning to the laboratory, I decided to examine a few specimens of the polychaete Sabellaria cementarium Moore (Sabellariidae) which had been collected on the same dredging trip. From previous experience, I knew that this species was regularly infected by a so-called schizogregarine of the genus Selenidium. As the first worm was opened, hundreds of male and female orthonectids emerged from the tissue of the body wall. Over a period of several days, I examined a total of 88 worms (47 males, 41 females) from the same locality. The sixtysixth specimen to be opened also was infected. Both of the parasitized worms were mature males carrying sperm, and before examination appeared to be completely normal. The orthonectid from S. cementarium, for which I propose the name Ciliocincta sabellariae gen. n., sp. n., resembles certain species of Rhopalura. However, its precise pattern of ciliation is decidedly different from that described by any of the European investigators. It is possible that if the morphology of other This content downloaded from 207.46.13.114 on Thu, 26 May 2016 06:30:46 UTC All use subject to http://about.jstor.org/terms 38 THE JOURNAL OF PARASITOLOGY, VOL. 51, NO. 1, FEBRUARY 1965 orthonectids were investigated carefully, some of them would be found to have an organization similar to that of C. sabellariae. The type locality for C. sabellariae is near Dot Rock (long 122o47.8' W; lat 48?29.5' N), San Juan Archipelago, Washington. The material was collected at a depth of 7 fathoms. Syntype slides have been deposited in the United States National Museum (USNM No. 23734).