名古屋大学博物館報告
Bull. Nagoya Univ. Museum
No. 19, 9–19, 2003

First discovery of Bugula stolonifera Ryland, 1960
(Phylum Bryozoa) in Japanese waters, as an alien species
to the Port of Nagoya
Joachim SCHOLZ1), NAKAJIMA Kiyonori2), NISHIKAWA Teruaki3),
KASELOWSKY Jürgen4) and MAWATARI F. Shunsuke5)
1,4) Forschungsinstitut und Naturmuseum Senckenberg, Section Marine Evertebrates III (Bryozoology),
Senckenberganlage 25, D-60325 Frankfurt am Main, Germany
1,2) Port of Nagoya Public Aquarium, 1-3, Minatomachi, Minato-ku, Nagoya 455-0033, Japan1,3) The Nagoya University Museum, Chikusa-ku, Nagoya 464-8601, Japan1,5) Division of Biological Sciences, Graduate School of Science, Hokkaido University, Sapporo 060-0810,
Japan

Abstract
Samples taken in 1997 from the Port of Nagoya, Japan, revealed the first record of the cheilostomebryozoan, Bugula stolonifera Ryland in Japanese waters. The species, which has been reported
within the last years from several localities over the world, has probably been imported by ships
coming to the Port of Nagoya. The species record illustrates the changes to which the Japanesebryozoan communities are subjected due to neozoan immigration.

1. Introduction
Bryozoans represent a phylum of colonial, suspension feeding animals. They are abundantly
found in both cool waters and tropical reefs, silicoclastic shelves, polar regions, and even in the
deep sea realm. The phylum is the only major group of exclusively clonal animals. Colonies areformed by repeated budding of genetically (but not always morphologically) identical, physicallyconnected, intercommunicating member zooids (McKinney and Jackson, 1989; Cook, 1988).
The modular construction of their fixosessile, mostly calcifying colonies makes it possible toreconstruct life histories and interactive relationships on substratum surfaces. Skeletal growthmodifications of both single units (zooids) and colonies (zoaria) preserve the influence of the outside environment at the time of growth.
The large percentage of surface occupied by laminar bryozoans despite the small biomass makes
them important in any biological interactions on hard substrata (Riedl, 1966). Bryozoans are frequently the dominant biota covering the surfaces of dead coral reef colonies. This suggests thatbryozoans serve as a major frame-binding agent for maintaining the integrity of the reefs, in opposition to bioeroding biota (Soule and Soule, 1972).
Fouling bryozoa are an economic problem since for example in boats and ships, a 1 mm thicklayer of slime can cause a 15% loss in ship speed compared to values obtained for a clean hull
(Lewthaite et al., 1985). Bryozoans are frequently overgrowing and suffocating marine oyster beds,
and fresh-water bryozoans may foul water system distribution pipes (Cuffey, 1970).
Today, the arrival of fouling bryozoans settling e.g. on ship hulls is rapidly altering the species
composition of bryozoans on a world wide scale, occasionally with dramatical impacts (see Gordon—9—and Mawatari, 1992). Bryozoans may even be distributed by aeroplanes, such as probably happened during the Second World War, when European Conopeum seurati were introduced to theremote Chatham island lagoon by allied “Sunderland” flying boats (Scholz, 2001). As early as 1971,
J. Ryland cited the number of 54 species of bryozoans known to colonize ship’s hulls, and 139
fouling bryozoans form ships, buoys, wrecks, and harbour installations. For fouling bryozoans it istypical that they do not have a competitive advantage over less-generalist species, but may thrivein the particular conditions of ports and harbours since the mature colonies are more tolerant of
the wider ranges of the prevailing temperature, salinity, turbidity, and pollution (literature reviewed by Gordon and Mawatari, 1992).
For the Japanese islands, little is known on the magnitude of this event, although it is readily
evident that for example harbour sites or floating piers are heavily colonized by dense clusters offouling species of Watersipora subovoidea, Bugula neritina and some other species (Nandakumar
et al., 1993). Aside from this comparatively recent contribution, we have to rely on data that record
the state of the art as it has been several decades ago (A. Grischenko, Sapporo, pers. comm.), suchas the articles of Yanagi and Okada (1918) and S. Mawatari (1953), and a consideration of theneozoan impact must be part of any new taxonomic inventory of the Japanese seas. Every species
counts, and in the following, we report on the arrival of a new fouling bryozoan to Japan. Furthermore, a state of the art of biodiversity research of Japanese bryozoans is given.

Sea of Japan

Nagoya
Osaka

Tokyo

Sampling site
Pacific Ocean

Port of
NagoyaPort of Nagoya
Public Aquarium
100m

Ise Bay

Garden pier2000m

Fig. 1: Map showing the sampling site in the Port of Nagoya, Middle Japan.

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2. Material and Methods
The specimen, registered as NUM-Az 0363 in The Nagoya University Museum, was collectedon15 Nov. 1997 from a vinyl-chloride panel set in a launch harbour in front of the Port of Nagoya
Public Aquarium, northern end of Ise Bay on the Pacific coast of Middle Japan (Fig. 1). The Port ofNagoya is one of the biggest harbours in Japan, with arrivals of 9,231 (in 2001) and 9,132 (in 2002)
foreign vessels (data from www.port-of-nagoya.jp).
The panel had been set subtidally from 5 July 1997, just below the mean low water of springtide. Water temperature and salinity at the sampling site were 21.8°C on an average (ranging from
11.3 to 31.6°C), and 31‰ (from 20 to 37‰), based on the daily data throughout 2000 and 2002,
respectively. The specimen was fixed and preserved in 10% formalin.
The sample was transferred to ethanol in a dehydration series, critical-point-dried and sputtered for SEM observation.
3. On the genus Bugula Oken, 1815
Species of Bugula have intrigued biologists for more than 100 years, due to their abundance andto the presence of spectacular, strange bird head avicularia (Fig. 2). For example, in the first 1969
edition of Ricketts’ famous account on the intertidal fauna of California, he states : “The avicularia(‘bird beaks’) of Bugula, thought to be defensive in function, are classic objects of interest to theinvertebrate zoologist. It is a pity that these … can be seen only with a microscope. If the movable
beaks of avicularia were a foot or so long, instead of a fraction of a millimeter, newspaper photographers and reporters would flock to see them. The snapping process would be observed excitedly,
some enterprising cub would certainly have one of his fingers snipped off, and the crowds would
amuse themselves by feeding stray puppies into the pincers.”
Bird head avicularia are one of most useful features to identify Bugula species. This is important since the genus is diverse, and the ERMS (European Register of Marine Species) report (Hayward, 2001) cites 20 species of Bugula for European waters alone.
The function of bird head avicularia, and avicularia in general is still obscure. The function was
discussed in Darwin’s “Origin of Species”, but Darwin and his successors provided inconclusive
evidence on the evolutionary significance of avicularia. Defense against predators, cleaning, locomotion, nutrient storage, respiration, chemical defense, current flow modifications, or larval inoculation are among the functions possible for the diverse type of bryozoan avicularia (literature reviewed in Winston, 1984).
For bird head avicularia, a very early observation may be the most probable explanation, pointing out a peculiar way of agriculture in invertebrates: “On one occasion I saw one with the mandibles closed, grasping a tuft of confervoid-like substance, just like a bird with a wisp of hay in its
beak. This is retained for some days, while the peculiar waving motion was still kept up. The only
explanation seemed to be that the decaying conferva would attract minute infusoria, which would
thus be brought within easy reach of the tentacles of the Polyzoon” (Goldstein, 1880).
Aside from the presence of bird head avicularia in most but not all species, the following description can be given for bryozoans of the genus Bugula: Colony are erect and branched, growing
from an upright ancestrula (first zooid). The colony may be attached by rhizoids which issue fromthe autozooidal surfaces. Zooids arranged unilaminar in two or more series, alternating, the proximal end being forked. The basal and lateral walls are lightly calcified, and the membrane occupies
most of the frontal surface. Spines are usually present. The ovicells (brood champers) are
hyperstomial and globular (summarised from Ryland and Haward, 1977: p.150).

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4. Results
Bugula stolonifera Ryland, 1960
(Fig. 2)
Bugula stolonifera Ryland, 1960, p.78; Ryland, 1962, p.50; Gordon and Mawatari, 1992, p.3.
Colonies are greyish-buff. in a compact and non-spiral tuft 3-4 cm high. Branches with zooids in
two series, with long and narrow zooids. Frontal membranes occupying 2/3 to 3/4 of the length of
the zooid. the length of the avicularia not exceeding the length of the zooid, and avicularian beak isshorter than the head. Spines are rather slender (see Ryland, 1960; Ryland and Hayward, 1977;
Zabala and Mauquer, 1988). The slender spines are important to distinguish the species from Bugula

Fig. 2: Bugula stolonifera Ryland from the Port of Nagoya, Japan.
A: Frontal and lateral surfaces of the erect colony. SEM Image, Critical-point-dried sample. B: Biserial
row of zooids, bifurcating; surfaces are nearly free of microbial fouling, thus indicating the presence of
secondary metabolites. C: Lateral view of autozooids and sections of the parent and daughter zooid,
showing tentacles and bird head avicularia. D: Autozooid and part of neighboring zooids, showing
orificial spines, frontal membranes, lateral walls, ovicells (brood chambers), and a bird head aviculariumwith mandible opened. E: Tentacle sheet, showing multiciliate cells and phytoplancton (diatoms), which
is a food source of bryozoans. F: Single bird head avicularium with closed rounded mandible.
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californica Roberston (1905) which was reported from Japan already, but judging from Soule et al.
(1995), has more stout finger-like spines.
Like many species of Bugula, B. stolonifera is a widely distributed neozoan. The type locality is
Swansea, Wales. In the 1960’s and 70’s, it arrived in Australia and New Zealand. The report of
Gordon and Mawatari (1992) does not mention any occurence in Japan. The species is not mentioned in the PhD thesis of S. Mawatari (1958) that focussed e.g. on the genus Bugula in Japan.
SEM-images (Fig. 2) show that the colony surface is very clean. This phenomenon has been
observed for many fouling bryozoans, which may probably be attributable to some anti-foulingchemicals produced by the colony.
5. Discussion
Bugula stolonifera Ryland has been reported from the docks in the Southwest of the British
Isles (Ryland, 1960). It settles between early summer to mid-autumn and is well known as a fouling species. It has been introduced to other countries, for example to New Zealand (Harger 1964,
Gordon & Mawatari 1992), by ships. It has been recorded also from the Mediterranean sea, Ireland, Ghana, Massachusetts to Florida, Brazil and South Australia (Winston, 1982; Cook, 1985;
Ryland and Hayward, 1991).
Studies on bryozoans and bryozoan diversity have implications in very diverse fields of basic
and applied research, four of them being listed below:
1) Bryozoans have been well established as biological indicators of anthropogenic influences incoastal waters (e.g. Soule and Soule, 1981; Scholz, 1991; Hillmer and Scholz, 1991; Winston,1995). Thus, the contribution of bryozoans and other supension feeding benthos to the management equation cannot be ignored.
2) The development of molecular methods has led to the recognition of high marine microbial
diversity, which can be used as a resource for the detection of novel marine natural products.
Since the 1980’s, Bryozoans and their cultivatable bacterial associates have become a focal point
for marine natural product research (e.g. Newman, 1996; Shellenberger and Ross, 1998; Pukall
et al., 2001, 2003).
3) Bryozoans are excellent tools for paleoecological studies (e. g. Voigt, 1930; Hageman et al., 1998)
since they commonly die in such a way that their relations to one another are preserved as they
were in life (McKinney and Jackson, 1989). Presence or absence, zooid size, colonial form andintegration of bryozoans contain conclusions about substrate, sedimentation, environmental
stability and conditions, food supply and temperature (Smith, 1995).
4) Accordingly, bryozoans have become an example for the study of functional morphology (Schäfer,1991), evolution (McKinney and Jackson, 1989, with review of literature) and zoogeographicalaspects of speciation (Hayward, 1983; Soule and Soule, 1985a; Moyano, 1996). Data on bryozoans have significantly contributed the punctuated equilibrium theory (Gould, 2002 with review
of literature), and biological individuality (Beklemishev, 1958-1960; Scholz and Levit, 2003).
Yet, “the use of bryozoan growth forms in the interpretation of palecology without adequate
taxonomic classification is probably meaningless” (Kelly and Horowitz, 1987), and non- or ill-classified organisms cannot be as a subject used in other fields of biology (Mawatari and Kajihara,
2003). Likewise, the utilisation of bryozoan data depends on continuous geographical coverage incollections. However, even in a comparatively well studied region such as the European coastal
waters, monitoring activities have been subject to great variation through the last decades (Hayward, 2001). The aspect of fragmentary documentation is ever the more true for the modern Indo— 13 —

Pacific province were bryozoan communities constitute a considerable part of the sessile, benthic
biomass, and thus achieve conspicuous presence over a huge ocean area. Especially the Western
Pacific is considered to be the hot spot of bryozoan biodiversity (Gordon, 1984). With such a large
number of regional bryozoan occurrences, and small numbers of systematists it would not be surprising if information about living specimens is rather insufficient (Winston, 1988), and what appears to be a simple request for the name of a bryozoan might be difficult or impossible to provide.
Most of the taxonomical bryozoan monographs are several decades or a century old, and the oldfashioned style of descriptions and illustrations (for example in Ortmann 1890, Waters, 1909, orCanu and Bassler, 1929) precludes their reliable use in species identification. Therefore, the Grantin-aid projects for Monbusho International Scientific Research Programms have already supported
re-descriptions of Japanese Bryozoa and other Japanese taxa (see Mawatari and Suwa, 1998).
What has successfully been started for the Japanese fauna should now be applied on the whole
Indo-Pacific.
How biotas are affected by geographical isolation and environmental change is a question fundamental to ecology, historical biogeography, and phylogeography. A re-evaluation of types fromIndo-Pacific collections (e.g. Waters, 1909, Red Sea; Ortmann, 1890, Japan; Harmer, 1915-1957,
Indonesia; Canu and Bassler, 1929, Philippines), and modern state-of-the-art re-illustration of typematerial has now become necessary to have a new data base about the comparative morphology ofIndopacific bryozoans.
We should carefully consider both re-illustration of morphology, and geographical range. Specimens may not always be assigned unequivocally to a known species based on the holotype only.
There is a need to understand morphological plasticity of species throughout their range of distribution. One of the first important achievements outlining regionalism and a high degree of speciation in tropical bryozoans is represented by the monograph of the Smittinidae of Hawaii (Soule andSoule, 1973), a family of ascophorine bryozoans that accordingly became known as “marine Darwin
Finches”.
During the past years, molecular biology has become a powerful tool in contribution to bryozoan
taxonomy, on the grounds of combination with methods of traditional morphology (Levington et al.,2001). Meanwhile, studies on genetic relatedness have revealed metapopulations (Okamura, 2000),
identified the presence of cryptic species in alleged cosmopolitan bryozoans (Hoare et al., 2001),
and started to contribute to revised classifications of gymnolaemate bryozoans ( Dick et al., 2000,
2003). It has been found out that morphological differences are often, but not always consistent
with taxonomical differences (Mackie et al., 2002). Accordingly, the statement made by McKinney
and Jackson in 1989 that îmost descriptions of living bryozoans with calcified skeletons do notdiffer substantially from descriptions of fossil species in the same classî is only partly true today.
Despite of the increasing demand for research in molecular biology and taxonomy of bryozoans,
traditional morphology still has its values. Important regions of the Indo-Pacific like, for example,
the Arabian (Persian) Gulf is still a terra incognita in terms of bryozoology. Aside from a brief
account of Soule and Soule (1985b) on epiphytic bryozoans, nothing is known on the bryozoan
fauna off the northern coast of Saudi Arabia. Recently, Azis et al. (2001) observed that bryozoans
belong to the most important fouling organisms in the Persian Gulf region, but they did not provide
a list of species that occur. The very diverse bryozoan fauna of Socotra (Yemen) is virtually unknown aside from a very preliminary account by Scholz et al. (2001), and a more extensive report isunder way. The eastern coast of Africa is poorly studied, and aside from the report of Brood (1976)
on certain taxa, and the Mauritius report of Hayward (1988), we still wait for an overview on theregional biodiversity of the phylum. Fortunately, for the Japanese bryozoans, the situation is not— 14 —

so bad and there are numerous reports prepared by one of the authors (S. F. M.) and by his father
Shizuo Mawatari. Some bryozoan studies have been conducted within the scope of the comparative
survey “Natural History Researches of northern Hokkaido” of the National Science Museum, Tokyo, that outlined zoogeographical connections of the Hokkaido fauna to Russia (Mawatari et al.,1991), and triggered new research on comparative views of bryozoans from Northern Japan, Okhotsk,
and the Kuril Arc (Grischenko et al., 2002). Previously, an inventorization of Recent marine Bryozoa
living along Hokkaido Island was carried out by the efforts of Mawatari, S. (1957, 1973a, b, 1974),
Mawatari, S.F. (1971, 1972), and by their collaborative researches (Mawatari and Mawatari, 1973,
1974; 1979, 1980, 1981a, b) with 22 cyclostome, 4 ctenostome and more than 130 cheilostome species reported, giving about 170 species in total. However, this is very preliminary number and morework needs to be done to receive a reliable data on bryozoan diversity of this region. Henceforth, abryozoology PhD study (A. Grischenko, Hokkaido University, Sapporo) has been launched, and oneof the goals of this study is to list all species of the bryozoans, that occur off the Oshoro Marine
Biology Station, and other coastal areas of Hokkaido. Aside from the links to Russia that are evident in the bryozoans or the northern Japanese latitudes, there are surprising links of Recent
Japanese bryozoans to the Southern Ocean (Gordon et al., 2002) that are also indicated by thefossil record (Brown, 1952: p.128). Compared with the bryozoans in Northern Japan, the warm
water bryozoans of Japan that are influenced by the Kuroshio current are not so well known. The
Bryozoa fauna of the cool temperate northern latitudes of Japan is strikingly different in bothtaxonomy, and growth morphologies. Therefore, for the bryozoans dwelling in the coastal seas off
Honshu and Kyushu, we still have to rely on the historical accounts such as prepared by Ortmann(1890), Okada (1923), Saito (1931), and Sakakura (1935).
Acknowledgements
It is a pleasure to acknowledge valuable suggestions made by Mr. Andrei Grischenko, Hokkaido
University, Sapporo, and the support of the staff of Port of Nagoya Public Aquarium for providing
us data on the collection site. Furthermore, we would like to thank the Nagoya Port Authority for
helpful support in field work.
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名古屋港で発見されたコケムシ類の外来種 Bugula stolonifera
Ryland, 1960（日本初記録）
Joachim SCHOLZ（ゼンケンベルク自然史博物館）・
中嶋清徳（名古屋港水族館）・西川輝昭（名古屋大学博物館）・
KASELOWSKY Jürgen（ゼンケンベルク自然史博物館）・
馬渡峻輔（北海道大学理学研究科）
名古屋港水族館前の船だまりに垂下していた塩ビ試験板から1997年に採集されたコケムシ類は、日本初記録の Bugula stolonifera Ryland, 1960 であることが判った。本種は最近、世界各地でその新たな出現が記録されている。おそらく名古屋港にも外国船によって到来したものと思われる。あわせて、コケムシ類の生物多様性研究が持つ意義と将来展望、そこでの形態情報の重要性について論じた。

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