1902 Encyclopedia > Teredo

Teredo




TEREDO, a genus of Lamellibranchiate Mollusca, of the order Isomya, sub-order Sinupallia, family Pholadacea (see MOLLUSCA, vol. xvi. p. 685). The animals included in this genus are commonly known as " ship-worms," and are notorious for the destruction which they cause in ships' timbers, the woodwork of harbours, and piles or other wood immersed for a long period in the sea. They inhabit long cylindrical holes, which they excavate in the wood, and usually occur in great numbers, crowded together so that often only a very thin film remains between the adjacent burrows. Each burrow is lined with a layer of calcareous substance secreted. by the mollusc ; this lining is not usually complete, but stops short a little distance from the inner end of the burrow, where the boring process continues to take place. In some burrows, how-ever, the lining is complete, either because the animal has reached its full size or because some cause prevents it continuing its tunnel; in such cases the calcareous tube has a hemispherical termination. The burrows are usually driven in the direction of the grain of the wood, but not invariably so. When a knot or nail or the tube of a neighbour is reached, the course of the burrow is altered so as to bend round the obstruction. One burrow is never found to break into another.
The adult Teredo, when removed from its burrow and calcareous tube, is from a few inches to 3 feet in length, according to the species to which it belongs, and is cylindrical and worm-like in appearance. The anterior end, which lies at the bottom of the burrow, is somewhat enlarged and bears a pair of shells or valves, which are not connected by the usual ligament, but are widely-separated dorsally. The valves are triangular in shape and very concave on the side which is in contact with the animal. In front their edges are widely separated, and the mantle tube, which is elsewhere closed, has here a slight median aperture, through which the short sucker-like foot can be protruded. The next portion of the body behind the shell-bearing part is naked, except for the shelly lining of the burrow, which is secreted by this part. Anteriorly this portion contains part of the body proper; posteriorly it forms a tube divided internally by a horizontal partition into two chambers. In the lower chamber are the elongated gill plates, which have the typical lamellibranchiate structure. In the upper chamber anteriorly is the rectum. A thick muscular ring terminates this region of the body, and bears two calcareous plates shaped like spades or battledores. The expanded parts of these plates are free and project backwards; the handle is fixed in a deep socket or pit lined by epidermis. These calcareous plates are called pallets (Fr. palmules). Behind the pallets the tubular body bifurcates, forming two siphons similar to those of other Lamellibranchs ; the siphons can be contracted or expanded within wide limits of length. The principal organs of the body—stomach, heart, genera-tive organs, and nephridia—are situated in the anterior part of the body, forming a visceral mass, which extends some distance behind the valves. The heart is above the in-testine and not perforated by it. The two valves are connected by an anterior adductor muscle.
From its resemblance to Pholas, Teredo is placed by conchologists in the family Pholadidee, among the Isomya ; but it is still undecided which part of the body corresponds to the posterior adductor. According to Quatrefages, it is a muscular band passing transversely between the handles of the pallets. His discussion of this point is connected with another, namely, the nature of the long tubular portion of the body behind the valves. Deshayes limits the extent of the mantle to the part covered by the shell, and considers all the rest of the animal as formed by the siphons ; the branehife and part of the other viscera in this view are contained in the siphons. Quatrefages argues that the siphons commence at the point where their retractor muscles are inserted, namely, at the muscular ring corresponding to the pallets. This reasoning is plausible ; but it is difficult to accept the view that the retractor muscles of the siphons and the posterior adductor muscle are so closely connected as Quatrefages thinks; in other Isomya the retractors of the siphons and the posterior adductor are distinct and separate. Deshayes believes that the single adductor between the valves results from the fusion of the two muscles usually separate. Jeffreys believes that the posterior adductor is really present between the posterior parts of the valves; but the opinion of a conchologist on a question of morphology is not of very great weight. In other Isomya the visceral (parieto-splanchnic) ganglia are attached to the ventral surface of the posterior adductor. In Teredo these ganglia are situated at the posterior end of the body proper, some distance behind the shells, and immediately behind the generative organ. It is here probably that the rudiment of the posterior adductor, if it exists, is to be sought; or, if it does not exist, it is here that it originally was placed.
It is evident that the anatomy of Teredo has not yet been in-vestigated from the point of view of modern morphology; but as far as can be judged at present the body proper extends back some distance behind the shells, to the posterior limit of the visceral mass. The part between this and the pallets is a tubular prolonga-tion of the mantle chamber containing the extended gill lamina;, and beyond the pallets are the separate siphons. Besides the visceral ganglia a cerebral and a pedal pair are present. The stomach is provided with a large crystalline style. The function of the pallets is to form an operculum to the calcareous tube when the siphons are withdrawn into it. In some species the external or narrower end of the calcareous tube is provided with transverse laminse projecting into the lumen ; and in some the external aperture is divided by a horizontal partition into two, one for each siphon.
The Teredo, according to Quatrefages, is dioecious, though Gwyn Jeffreys believes it to be hermaphrodite. As in the case of the oyster, the ova are retained in the branchial chamber during the earl}' stages of their development. The segmentation of the ovum is unequal, and leads to the formation of a gastrula by opibole. By the growth of a preoral lobe provided with a ring of cilia, and by the formation of a mouth and an anus, the trochosphere stage is reached. A pair of thin shells then appear on the sides of the larva, connected by a hinge on the dorsal median line, and the foot grows out between mouth and anus. By the time the larva} "swarm," or leave the branchial cavity of the parent to live for a time as free-swimming pelagic larvae, the valves of the shell have grown so large as to cover the whole of the body when the velum is retracted; the foot is also long, cylindrical, and flexible, and can bo protruded far beyond the shell. The valves of the shell at this stage are hemi-spherical in shape, so that the whole larva when its organs are retracted is contained in a globular case.
Concerning the later changes of the larva and the method by which it bores into wood nothing or little is known from direct observation. Much has been written about the boring of this and other marine animals, but even yet the matter cannot be said to be satisfactorily elucidated. Osier, in a paper in Phil. Trans., 1826, argued that the Teredo bores by means of its shells, fixing itself by the surface of the foot, which it uses as a sucker, and then rasping the wood with the rough front edges of the shell-valves. This view was founded on the similarity of the arrangement of the shells and muscles in Teredo to those occurring in Photas, in which the method of boring described was actually observed. W. Thompson, in a paper in the Edinb. New Phil. Joum., 1835, supported the view that the excavation is due to the action of a solvent secreted from the surface of the animal. Albany Hancock, again (Ann. and Mag. Nat. Hist., vol. xv.), thinks that the excavating power of Teredo is due to silicious particles embedded in the anterior portion of the integument, in front of the valves. But the actual existence of either silicious particles or acid secretion has been denied by others. Jeffreys believes that the foot is the organ by which the animal burrows. In the larger number of Lamellibranehs the foot is doubtless a burrowing organ, and it is difficult to see how the limpet hollows out the rock to which it is attached if not by means of the surface of its foot. At the same time it is difficult to explain how the soft muscular foot can penetrate into hard wood. The process is of course slow, and Jeffreys supposes that particles are detached one by one from the moistened surface to which the foot is applied. In any case the valves are covered by an epidermis, which could scarcely be there if they were used in burrowing.
Teredo grows and burrows at an extremely rapid rate : spawning takes place in the spring and summer, and before the end of the year the animals are adult and their burrows of large size. Quatre-fages relates that at Guipuzcoa (N. Spain) a ferry-boat was sunk accidentally in the spring, and was raised four months afterwards, when its timbers were already rendered useless by T. pedieellata. How long the animals live is not accurately known, but Quatrefages found that they nearly all perished in the winter. This can-not be generally the case, as the size of the tubes varies so greatly. In Holland their greatest ravages are made in Jul}7 and August. Iron ships have nothing to fear from their attacks, and the copper sheathing now almost universally used protects wooden hulls. A great deal of loss is, however, caused by Teredo in harbour works and shipping stages, and the embankments in Holland are con-tinually injured by it. The most efficient protection is afforded by large-headed nails driven in in close proximity. Soaking wood in creasote is not a certain safeguard ; Jeffreys found at Christiania in 1863 that a large number of harbour piles previously soaked in creasote had been completely destroyed by T. navalis. Coal tar and the silicate of lime, used for coating stonework, have been sug-gested as protective coverings, but they do not seem to have been adequately tested.
Species of Teredo occur in all seas. The animal was known to the ancients and is mentioned by Theophrastus, Pliny, and Ovid. In 1715 it is mentioned by Valisnieri, in 1720 by Deslandes. In 1733 great attention was drawn to it on account of the discovery that the wooden dykes of Holland were being rapidly destroyed, by ship-worms, and that the country was in danger of inundation. Three treatises were published concerning the animal, by P. Mas-suet, J. Rousset, and Godfrey Sellius. The work of the last-named, which was the best, described the anatomy of the creature and showed that its affinities were with bivalve molluscs. The truth of Sellius's view was not grasped by Linnœus, who placed Teredo together with Serpula in the genus Dentalium ; but its proper position was re-established by Cuvier and Lamarck. Adanson, unaware of the work of Sellius, in 1757 believed himself to be the first to discover the molluscan affinities of Teredo. It will not be necessary to give here a definition of the genus taken from any systematist ; it will be sufficient to point out that the long cy-lindrical body with its two small anterior polygonal valves, the absence of a ligament and accessory valves, the muscular ring into which are inserted the calcareous pallets, and the continuous calcareous tube lining the hole bored by the animal are the diagnostic features.
Jeffreys, in his British Conchology, gives the following species as British:—Teredo norvegica, Spengler; T. navalis, Linn.; T. pedi-eellata, Quatrefages; T. megotara, Hanley. T. norvegica occurs chiefly on the west coast of Great Britain. It was taken by Thompson at Portpatrick in Wigtownshire, and occurred in Jef-reys's time in abundance at Milford Haven. This species has been described by Gmelin and a number of British authors as T. navalis, Linn. It is distinguished by having the base of the pallets simple, not forked, and the tube semi-concamerated at its narrower pos-terior end. The length does not usually exceed a foot. It is the T. navium of Sellius. T. navalis has been identified from the figures of Sellius, to which Linnœus referred ; Sellius called it T. ma.rina. It occurs on all the western and southern coasts of Europe, from Christiania to the Black Sea, and is the species which causes so much damage to the Dutch embankments. The pallets of this species are small and forked, and the stalk is cylindrical. The tube is simple and not chambered at its narrow end. T. pedieellata was originally discovered by Quatrefages in the Bay of Los Pasages on the north coast of Spain ; it has also been found in the Channel Islands, at Toulon, in Provence, and in Algeria. In T. megotara the tube is simple and the pallets like those of T. norvegica ; it occurs at Shetland and Wick, and also on the western shore of the Atlantic, where its range extends from Massachusetts to South Carolina. T. malleolus, Turton, and T. bipinnata, Turton, belong to the West Indies, but are often drifted in floating timber to the coasts of Europe. Other occasional visitants to the British shores are T. excavata, bipartita, S2>atha, fustiailas, eucullata, and fimbriata. These were described by Gwyn Jeffreys in Ann. and Mag. Nat. Hist., 1860. T. fimbriata is stated to be a native of Vancouver's Island. A kind of ship-worm, the Nausitora dunlopei of Perceval Wright, has been discovered in India, 70 miles from the sea, in a stream of perfectly fresh water, namely, the river Kumar, one of the branches of the Ganges. T. corniformis, Lam., is found burrowing in the husks of cocoa-nuts and other woody fruits floating in the tropical seas ; its tubes are extremely crooked and contorted for want of space. Fossil wood and palm-fruits of Sheppey and Brabant are pierced in the same way.
Twenty-four fossil species have been recognized in the Lias and succeeding beds of Europe and the United States. The sub-genus Teredina, Lam., is a fossil of the Eocene of Great Britain and France.
Literature.—See, besides the works already mentioned, Godfrey Sellius, Historia Naturalis Teredinis seu Xylopliagi Marini, 1733; Adanson, Histoire Naturelle dit Senegal, Paris, 1757 ; Quatrefages, Annales des Sel. Nat., 1848-50 ; Forbes and Hanley, Brit. Mollusca, 1S53; B. Hatseliek, Entwicklungv. Teredo:
Arbeiten aus deni Zool. Inst. Wien, 1SS0 ; Deshayes, Mollusques d'Algerie ; Sir E.
Home, "Anatomy of Teredo," in Phil. Trans., vol. xcvi. ; Frey and Leuckart,
Beilrage zur Kenntniss wlrbelloser Thiere, 1S47 ; Woodward, Manual of Mollusca,
London, 1851. (J. T. C.)







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