Invasion History
First Non-native North American Tidal Record: 1871First Non-native West Coast Tidal Record: 1871
First Non-native East/Gulf Coast Tidal Record:
General Invasion History:
Lyrodus pedicellatus was described from Spain but is probably of Indo-Pacific origin. It is now widespread in tropical-to-warm-temperate waters around the globe and its precise native range cannot be determined yet. It was described from the Bay of Biscay, Spain, in 1849 and has been collected and redescribed under many synonymous names (Turner 1966; Turner 1971). One description, as ‘Teredo chlorotica’ was made in Boston Harbor, Massachusetts, from the hull of a whaling ship which had cruised in the Pacific Ocean (Gould 1870). It was first collected on the Pacific coast of the US in the 1870s and appears to be localized in shallow harbors where water temperatures are warm enough for breeding (Carlton 1979). This species and an unidentified Lyrodus sp. were said to have established temporary populations in thermal effluents in England and Barnegat Bay, New Jersey (Coughlan 1977; Hoagland and Turner 1980). It may be that 'Lyrodus pedicellatus' represents a complex of numerous species, but further work needs to be conducted (Borges et al. 2012; Borges et al. 2014b). This shipworm has a short (up to 36 hours) larval duration in the plankton, so long-distance dispersal is largely by ships or driftwood (Lebour 1946).
North American Invasion History:
Invasion History on the West Coast:
Lyrodus pedicellatus was first reported on the West Coast of the US from Los Angeles-Long Beach Harbor, as Teredo navalis in 1871 (Mendell 1871, cited by Carlton 1979). In San Diego Bay, it was collected in 1907 as Xylotrya stuchburyi (Kelsey 1907, cited by Carlton 1979), and reported by Bartsch (1916, cited by Carlton 1979) as Teredo diegensis. In 1920, it was collected in San Bruno Slough, San Mateo County, off South San Francisco Bay (1920, Kofoid 1921, cited by Carlton 1979). Subsequently, it was collected from many sites along the Bay, including Hunters Point, Yerba Buena, Mare Island, and Benicia (Wallour 1960; Carlton 1979). Lyrodus pedicellatus has been found in many of the smaller bays, including Elkhorn Slough (MacGinitie 1935, cited by Carlton 1979), Santa Barbara Harbor, Port Hueneme, Santa Monica Bay (Miller 1951, cited by Carlton 1979), Mugu Lagoon (Burch 1945, cited by Carlton 1979) and Newport Bay (Reish 1972, cited by Carlton 1979).
Invasion History on the East Coast:
Lyrodus pedicellatus was reported (as T. chlorotica) to occur from Florida to Texas (Dall 1889). We regard it as cryptogenic in the Western Atlantic, from North Carolina to Argentina (Turner 1966; Wallour 1960; Farrapeira et al. 2011; Museum of Comparative Zoology 2012), where it may have been introduced in the 16th–19th centuries. However, these tropical shipworms are occasionally transported north of Cape Hatteras by wooden boats and ships. In 1870, A. A. Gould described a specimen as T. chlorotica from a Pacific whaling ship in Boston harbor (Gould 1870). In 1974, a single juvenile Lyrodus sp. (L. pedicellatus or L. floridanus) was found in wood in the effluent of a nuclear power plant in Oyster Creek, Barnegat Bay, New Jersey (Hoagland and Turner 1980).
Invasion History in Hawaii:
The first collection of L. pedicellatus in the Hawaiian Islands is from a dredged, sunken, palm log, from ~ 400 m depth off Oahu in 1902 (as Teredo hawaiensis) (Dall, Bartsch & Rehder 1938, cited by Carlton and Eldredge 2009). Later collections were in Pearl Harbor (in 1935, Coles et al. 1999), Kauai (Dall, Bartsch & Rehder 1938, as T. kauaiensis, cited by Carlton and Eldredge 2009), Midway (Edmondson 1942, cited by Carlton and Eldredge 2009); and Johnston Island, Pacific Ocean (Srinivasan 1968).
Invasion History Elsewhere in the World:
Lyrodus pedicellatus is now widespread in warm-temperate to tropical waters around the world, including the Atlantic Ocean, Mediterranean and Black Seas, Indian Ocean, and West Pacific (Wallour 1960; Turner 1966; Srinivasan 1968; Sen et al. 2010; Museum of Comparative Zoology 2012). We regard it as cryptogenic over most of this range. It is apparently introduced in False Bay, South Africa (in 1931, Mead et al. 2011b), New Zealand (McKoy 1980; Cranfield et al. 1998), and the Galapagos Islands (Cruz 1996; Carlton et al. 2019). In the Tagus estuary, Portugal it replaced and apparently eliminated Teredo navalis from the 1960s–70s to the 1990s–2000s (Borges et al. 2010). In England, specimens are known from ships’ hulls and from thermal discharges (Turner 1966; Coughlan 1977). However, this species is now established and dominant in the English Channel, apparently as a result of increased temperatures (Borges 2007, cited in Borges et al. 2010).
Description
Lyrodus pedicellatus is commonly known as the Blacktip Shipworm. It belongs to the family Teredinidae (shipworms), which are highly modified mollusks, hardly recognizable as bivalves, adapted for boring into wood. The shell is reduced to two small, ridged valves, covering the head, and is used for grinding and tearing wood fibers. The body is naked and elongated, and ends with two siphons, protected by elaborate calcareous structures called pallets (Turner 1966).
In the genus Lyrodus, the shell resembles that of the Naval Shipworm (Teredo navalis), but is smaller and more finely sculptured. The pallets have a calcareous base, which is conical distally and a brown to black cap made of periostracum. The outline resembles that of the stem and cup of a wineglass. The cap has straight sides, while the outer margin varies from a shallow U-shape to being deeply excavated, so that the conical, calcareous base protrudes (Turner 1966; Turner 1971; Coan et al. 2000). In one study, off Mumbai, India, the largest specimens reached 205 mm (Raveendram and Wagh 1991).
Genetic analysis of Lyrodus pedicellatus in the northeast Atlantic and Mediterranean Sea indicates that these two populations may represent two cryptic species (Borges et al. 2012). Further genetic analysis is needed to evaluate the possibility of cryptic species and cryptic invasions throughout the reported range of L. pedicellatus.
Potentially misidentified species - The diversity of shipworms in tropical waters is very great. Many are now widely distributed in the Atlantic, Pacific, and Indian Oceans, largely as a result of shipping. The species listed have been reported in Florida, the Caribbean, the West Coast of North America, or Hawaiian waters.
Taxonomy
Taxonomic Tree
Kingdom: | Animalia | |
Phylum: | Mollusca | |
Class: | Bivalvia | |
Subclass: | Heterodonta | |
Order: | Myoida | |
Superfamily: | Pholadoidea | |
Family: | Teredinidae | |
Genus: | Lyrodus | |
Species: | pedicellatus |
Synonyms
Teredo chlorotica (Gould, 1870)
Teredo pertingens (Iredale, 1932)
Teredo (Lyrodus) hibicola (Koronuma, 1931)
Teredo (Pingoteredo) tristi (Iredale, 1936)
Teredo (Teredo) honoluluensis (Edmondson, 1946)
Teredo (Teredo) india (Nair, 1956)
Teredo (Teredo) madrasensis (Nair, 1956)
Teredo (Teredops) diegensis midwayensis (Edmondson, 1946)
Teredo (Teredops) hawaiensis (Dall, Bartsch, and Rehder, 1938)
Teredo (Teredops) kauiensis (Dall, Bartsch, and Rehder, 1938)
Teredo (Teredops) tateyamensis (Koronuma, 1931)
Teredo calmani (Roch, 1931)
Teredo dagmarae (Roch, 1931)
Teredo dalli (Moll and Roch, 1931)
Teredo franziusi (Roch, 1929)
Teredo helleniusi (Moll, 1936)
Teredo kiiensis (Taki and Habe, 1945)
Teredo lomensis (Roch, 1929)
Teredo malaccana (Roch, 1935)
Teredo nodosa (Roch, 1929)
Teredo pedicellata (de Quatrefages, 1849)
Teredo pedicellata truncata (Jeffreys, 1865)
Teredo pochhammeri (Moll, 1931)
Teredo robsoni (Roch, 1931)
Teredo samoanensis (Bartsch, 1927)
Teredo siamensis (Bartsch, 1927)
Teredo togoensis (Roch, 1929)
Teredo townsendi (Bartsch, 1922)
Teredo yatsui (Moll, 1929)
Teredo hawaiensis (Dall, Bartsch & Rehder, 1938)
Potentially Misidentified Species
Cosmopolitan, tropical, subtropical
Lyrodus floridanus
W Atlantic, subtropical. It was synonymized with L. pedicellatus, but later found to differ in its life history and geneitcs (Borges et al. 2012).
Lyrodus medilobatus
Cosmopolitan, tropical, subtropical
Lyrodus takanoshimensis
Cosmopolitan, tropical, subtropical, temperate, introduced in NE Pacific (British Columbia)
Nototeredo knoxi
Subtropical W Atlantic, oceanic
Psiloteredo megotara
N Atlantic, oceanic
Teredo bartschi
Cosmopolitan, tropical, subtropical, introduced in NE Pacific
Teredo clappi
Cosmopolitan, tropical, subtropical
Teredo fulleri
Cosmopolitan, tropical,
Teredo furcifera
Cosmopolitan, tropical, subtropical
Teredo navalis
Cryptogenic in NE Atlantic, NW Pacific, and Indo-West Pacific, but introduced in NW Atlantic, S Atlantic, NE Pacific, and SW Pacific
Teredora malleolus
Temperate-subtropical Atlantic, oceanic
Ecology
General:
Shipworms dig long burrows in submerged wood in marine environments. They burrow by rocking and abrading the wood fibers. The mantle covers most of the length of the body, and secretes a calcareous lining along the interior of the burrow. They normally have their anterior end, with head and shells inside the burrow, and their siphons protruding. The pallets plug the burrow when the siphons are retracted (Barnes 1983).
Shipworms are protandrous hermaphrodites, beginning life as male and transforming to female, but they have no capacity for self-fertilization. Males release sperm into the water column, which fertilizes eggs for the female. The fertilized eggs are then brooded in the gills. Larvae are retained in the gills to the veliger stage. Lyrodus pedicellatus, releases its larvae in an advanced stage, as pediveligers, which spend only 2 to 24 hours in the plankton (Turner and Johnson 1971). The larvae settle in the pediveliger stage, and then rapidly metamorphose and begin boring into wood within 2–3 days. They quickly develop a calcified shell, pallets, and burrow lining (Turner and Johnson 1971). Shipworms may obtain some (or most, Paalvast and van der Velde 2013) of their nutrition from plankton, but some comes from wood, which consists largely of cellulose. Symbiotic bacteria fix nitrogen, essential for protein synthesis (Turner and Johnson 1971; Barnes 1983).
Lyrodus pedicellatus is known from fixed wood structures and panels, and from driftwood in tropical and subtropical climates. In New Zealand, it was absent in mangrove habitats (Turner 1966; McKoy 1980), but it is reported to be abundant, together with five other shipworm species, in mangrove forests of southeastern India (Nair 1984). In experiments, L. pedicelllatus from California and New Guinea did not tolerate salinities below 20–25 PSU (Eckelbarger and Reish 1972; Rayner 1979). However, this shipworm is present in the Black Sea (~18–20 PSU) (Sen et al. 2010). This shipworm survived winter temperatures as low as 4.7 °C in England (Borges 2007, cited by Borges et al. 2011).
Food:
Phytoplankton, detritus
Trophic Status:
Suspension Feeder
SusFedHabitats
General Habitat | Coarse Woody Debris | None |
General Habitat | Marinas & Docks | None |
General Habitat | Vessel Hull | None |
Salinity Range | Polyhaline | 18-30 PSU |
Salinity Range | Euhaline | 30-40 PSU |
Tidal Range | Mid Intertidal | None |
Tidal Range | Subtidal | None |
Tidal Range | Low Intertidal | None |
Vertical Habitat | Epibenthic | None |
Life History
Tolerances and Life History Parameters
Minimum Temperature (ºC) | 11 | Experimental 50% survival, 7 days (Ecklebarger and Reish 1972). |
Minimum Salinity (‰) | 21.6 | Experimental, 50% survival, 7 days (Ecklebarger and Reish 1972). |
Minimum Reproductive Temperature | 14 | Carlton 1979 |
Maximum Reproductive Temperature | 24 | Experimental, highest tested (Ecklebarger and Reish 1972). |
Minimum Reproductive Salinity | 21.6 | Experimental, 50% survival, 7 days (Ecklebarger and Reish 1972). |
Minimum Duration | 0.2 | Larval duration (Turner and Johnson 1971) |
Maximum Duration | 1 | Larval duration (Turner and Johnson 1971) |
Maximum Length (mm) | 205 | off Mumbai, India (Raveendram and Wagh 1991) |
Broad Temperature Range | None | Warm temperate-Tropical |
Broad Salinity Range | None | Polyhaline-Euhaline |
General Impacts
Specific impacts of Lyrodus pedicellatus are difficult to determine, because this shipworm often co-occurs with Teredo navalis (Naval Shipworm) and a few other species (Psiloteredo megotara, North Atlantic; Bankia gouldi, Northwest Atlantic; Bankia setacea, Northeast Pacific) in temperate waters, and with a more diverse community of shipworms in subtropical and tropical waters. However, L. pedicellatus was the dominant, or one of the most abundant, shipworm species in many tropical, subtropical, and warm-temperate harbors and bays (Wallour 1960; Turner 1966; Ibrahim 1981; Nair 1984; Raveendran and Wagh 1991).
Lyrodus pedicellatus is a common shipworm in the warmer waters of the world. Its economic impacts include the devouring of historic and modern wooden boats, ships, wharves, pilings, and other structures (Atwood 1922; Turner 1971; Turner and Johnson 1971; Wallour 1960). They can affect structures used in fisheries and aquaculture (Nair 1984), and affect the timber industry in regions where logs are stored in seawater before processing (Tsunoda 1979).
Ecological effects of the L. pedicellatus invasion include competition with other shipworm species (Borges et al. 2011); wood breakdown and the incorporation of wood into marine food webs (Barnes 1983); and providing habitat by riddling wood with tunnels and galleries used by many small mobile animals (polychaetes, amphipods, isopods, etc.) (Carlton 1979). Measures to control the impacts of shipworms on vessels and marine infrastructure include the use of metal, plastic, or toxic substances (creosote, copper salts, etc.) to avoid shipworm attacks (Atwood 1922; Sen et al. 2010), with adverse effects on other marine organisms and possible toxicity to animal and human consumers.
Regional Distribution Map
Bioregion | Region Name | Year | Invasion Status | Population Status |
---|---|---|---|---|
P040 | Newport Bay | 1972 | Non-native | Established |
P058 | _CDA_P058 (San Pedro Channel Islands) | 1964 | Non-native | Established |
P060 | Santa Monica Bay | 1951 | Non-native | Established |
P062 | _CDA_P062 (Calleguas) | 1951 | Non-native | Established |
P065 | _CDA_P065 (Santa Barbara Channel) | 1951 | Non-native | Established |
P061 | _CDA_P061 (Los Angeles) | 1945 | Non-native | Established |
P080 | Monterey Bay | 1935 | Non-native | Established |
NEP-V | Northern California to Mid Channel Islands | 1920 | Non-native | Established |
P090 | San Francisco Bay | 1920 | Non-native | Established |
P020 | San Diego Bay | 1876 | Non-native | Established |
NEP-VI | Pt. Conception to Southern Baja California | 1871 | Non-native | Established |
P050 | San Pedro Bay | 1871 | Non-native | Established |
Occurrence Map
OCC_ID | Author | Year | Date | Locality | Status | Latitude | Longitude |
---|---|---|---|---|---|---|---|
697524 | Reish 1968b, 1972 | 1968 | Alamitos Bay | Non-native | 33.7502 | -118.1185 | |
698634 | Kofoid 1921, cited in Carlton 1979; Bartsch 1922; Miller 1926; Kofoid and Miller 1927 | 1920 | Oyster Point Channel | Non-native | 37.6688 | -122.3863 | |
700195 | Burch 1945 | 1945 | Mugu Lagoon | Non-native | 34.1016 | -119.0999 | |
700641 | Mendell 1871, 1873, 1878, and Sears 1875, 1876, all cited in Carlton 1979; Miller 1926 | 1871 | Los Angeles/Long Beach Harbor Complex | Non-native | 33.7632 | -118.2526 | |
700725 | Reish 1972 | 1972 | Newport Bay | Non-native | 33.6092 | -117.9067 | |
700977 | MacGinitie 1935 | 1935 | Elkhorn Slough at Highway 1 Bridge (Station 7) | Non-native | 36.8093 | -121.7848 | |
702496 | Miller 1926; Carlton 1979 | 1876 | San Diego Bay | Non-native | 32.6717 | -117.1439 | |
759740 | Kofoid and Miller 1923, cited in Carlton 1979; Kofoid and Miller 1927 | 1922 | Los Angeles/Long Beach Harbor Complex | Non-native | 33.7632 | -118.2526 | |
759741 | Miller 1926 | 1924 | Oyster Point Channel | Non-native | 37.6688 | -122.3863 | |
759742 | MacGinitie 1935 | 1935 | Old Salinas River between Sandholdt Road Bridge and mouth of Elkhorn Slough (Station 8) | Non-native | 36.8029 | -121.7859 | |
759743 | Burch 1942 | 1942 | Off Redondo Beach | Non-native | 33.8393 | -118.3946 | |
759744 | Burch 1945 | 1945 | San Pedro Bay | Non-native | 33.7356 | -118.2758 | |
759745 | Museum of Comparative Zoology, Harvard University Collections Database | 1945 | U.S. Navy Drydock at Hunter's Point | Non-native | 37.7256 | -122.3651 | |
759746 | Menzies et al. 1963 | 1951 | 1951-03-30 | Los Angeles Harbor, Slip 1 (Station A) | Non-native | 33.7623 | -118.2661 |
759747 | Menzies et al. 1963 | 1951 | Los Angeles Harbor, Slip No. 5 (Station B) | Non-native | 33.7648 | -118.2634 | |
759748 | Menzies et al. 1963 | 1951 | Los Angeles Harbor, Cerritos Channel, eastern side of Henry Ford Bridge (Station D) | Non-native | 33.7663 | -118.2393 | |
759749 | Menzies et al. 1963 | 1951 | Pontoon Bridge between Terminal Island and Long Beach (Station E) | Non-native | 33.7646 | -118.2211 | |
759750 | Menzies et al. 1963 | 1951 | Los Angeles Harbor, U.S. Navy Operations Base (Station F) | Non-native | 33.7522 | -118.2387 | |
759751 | Menzies et al. 1963 | 1951 | Long Beach Harbor Pilot Jetty (Station G) | Non-native | 33.7473 | -118.2157 | |
759752 | Menzies et al. 1963 | 1951 | Reeves Field Seaplane Hangar Bay (Station H) | Non-native | 33.7460 | -118.2537 | |
759753 | Menzies et al. 1963 | 1951 | Lighthouse Wharf, Los Angeles Harbor Entrance (Station K) | Non-native | 33.7085 | -118.2522 | |
759754 | Menzies et al. 1963 | 1951 | 500 feet south of Boy Scouts of America Explorer Base (Station L) | Non-native | 33.7147 | -118.2845 | |
759755 | Menzies et al. 1963 | 1951 | Los Angeles Harbor, Channel Marker No. 5 (Station M) | Non-native | 33.7165 | -118.2679 | |
759756 | Menzies et al. 1963 | 1951 | Los Angeles Harbor, Berth 70 Municipal Wharf (Station N) | Non-native | 33.7243 | -118.2724 | |
759757 | Menzies et al. 1963 | 1951 | Berth 236, under Small Boat Fueling Wharf (Station P) | Non-native | 33.7370 | -118.2746 | |
759758 | Menzies et al. 1963 | 1951 | Los Angeles Harbor, Berth 147 (Station Q) | Non-native | 33.7577 | -118.2740 | |
759759 | Museum of Comparative Zoology, Harvard University Collections Database | 1959 | 1959-11-06 | Redondo/Palos Verdes Artificial Reef | Non-native | 33.8135 | -118.4060 |
759760 | Turner et al. 1969 | 1961 | Hermosa Beach Artificial Reef | Non-native | 33.8546 | -118.4105 | |
759761 | Turner et al. 1969 | 1961 | Paradise Cove Artifical Reef | Non-native | 34.0172 | -118.7645 | |
759762 | Coan 1964 | 1961 | Coal Oil Point | Non-native | 34.4072 | -119.8801 | |
759763 | Turner et al. 1969 | 1962 | Santa Monica Artificial Reef | Non-native | 34.0094 | -118.5297 | |
759764 | Eckelbarger and Reish 1972a, 1972b | 1972 | Cerritos Channel | Non-native | 33.7665 | -118.2375 | |
759765 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Slip 1, Berth 160 (Station A) | Non-native | 33.7629 | -118.2662 | |
759766 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Basin 5 (Station B) | Non-native | 33.7657 | -118.2602 | |
759767 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Consolidated Slip (Station C) | Non-native | 33.7722 | -118.2491 | |
759768 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Cerritos Channel (Station D) | Non-native | 33.7643 | -118.2471 | |
759769 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Fish Harbor (Station J) | Non-native | 33.7356 | -118.2692 | |
759770 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Shoaling Marker A (Station K) | Non-native | 33.7126 | -118.2550 | |
759771 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Entrance to West Channel (Station L) | Non-native | 33.7151 | -118.2763 | |
759772 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Port Pilot Station (Station N) | Non-native | 33.7207 | -118.2709 | |
759773 | Reish et al. 2015 | 2014 | Los Angeles Harbor, Entrance to West Basin (Station Q) | Non-native | 33.7566 | -118.2773 |
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