Chinese Journal of Oceanology and Limnology   2017, Vol. 35 issue(5): 1179-1188     PDF       
http://dx.doi.org/10.1007/s00343-017-6093-6
Institute of Oceanology, Chinese Academy of Sciences
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Article Information

LIU Huilian(刘会莲), Kamil ZÁGORŠEK(KamilZÁGORŠEK), WANG Shiwei(王世伟), MA Shide(马士德), Paul D. TAYLOR(PaulD.TAYLOR)
Interactions between Cryptosula and Watersipora (Bryozoa:Cheilostomata) on a ship's hull in Qingdao Harbour (South Yellow Sea) after five and a half years of immersion
Chinese Journal of Oceanology and Limnology, 35(5): 1179-1188
http://dx.doi.org/10.1007/s00343-017-6093-6

Article History

Received Mar. 28, 2016
accepted in principle Jun. 22, 2016
accepted for publication Aug. 12, 2016
Interactions between Cryptosula and Watersipora (Bryozoa:Cheilostomata) on a ship's hull in Qingdao Harbour (South Yellow Sea) after five and a half years of immersion
LIU Huilian(刘会莲)1, Kamil ZÁGORŠEK(KamilZÁGORŠEK)1,2, WANG Shiwei(王世伟)1, MA Shide(马士德)1, Paul D. TAYLOR(PaulD.TAYLOR)3        
1 Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;
2 Department of Geography, Technical University of Liberec, Studentská 2, CZ-461 17 Liberec, Czech Republic;
3 Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom
ABSTRACT: The distributions of two ubiquitous fouling cheilostome bryozoans, Cryptosula pallasiana (Moll, 1803) and Watersipora sp., on a ship moored for almost six years in Qingdao Bay show differences with respect to illumination, Cryptosula being dominant on the side of the ship which was exposed to the sun and Watersipora dominating on the other side which was in shadow for most of the time. Competitive interactions for substrate space were nearly always won by Watersipora, which succeeded in overgrowing the edges of Cryptosula colonies regardless of the side of the ship. Reasons for the superiority of Watersipora in spatial competition with Cryptosula could include faster growth rate and the stronger feeding currents created by the larger lophophores of Watersipora.
1 INTRODUCTION

Cryptosula and Watersipora are two of the most ubiquitous and widely distributed genera of fouling cheilostome bryozoans (Gordon and Mawatari, 1992). They have been recorded from numerous harbours around the world and there are many papers dealing with their biology (e.g., Cohen, 2011; Vieira et al., 2014 and references there). However, there appear to have been no studies about the competition between colonies of these two genera for living space.

Cryptosula pallasiana (Moll, 1803), originally described from Mediterranean Sea, now occurs in almost all harbours and adjacent shallow waters globally. In New Zealand C. pallasiana was recorded as early as 1898 (Gordon and Mawatari, 1992), found on ships in 1960, and on non-transient substrates in 1967 (Cohen, 2011). It was first reported on the Pacific Coast of North America in the mid-1940s at Newport Bay and San Francisco Bay (Cohen, 2011). Subsequently it was found in Hawaii [first reported in 1968], Japan [first reported in 1963, although it was reported even earlier as Hippodiplosia pallasiana by Okada (1929) and Mawatari (1952)], Australia including South Australia [reported in 1977], Victoria [in Port Phillip Bay in the late 1800s], New South Wales and northern Queensland, Argentina [reported in 1965] and Chile (Gordon and Mawatari, 1992; Cohen, 2011). This ascophoran cheilostome was likely introduced either as a hull fouler or with shipments of Atlantic oysters, with which it occurs in Atlantic coastal regions. Since its larvae spend a very short time in the plankton, it is a poor candidate for inter-oceanic transport by ballast water (Cohen, 2011).

One of the most common species of Watersipora is W. subtorquata (d'Orbigny, 1852), originallydescribed from Rio de Janeiro, Brazil, and later collected in the Pacific off southern California at Rincon Beach, Ventura County in 1963 (Cohen, 2011). It is possible that it was present at many more sites in the 1960s and 1970s but confused with other species of Watersipora, especially W. subatra and W. cucullata, (see Vieira et al., 2014), and with W. arcuata which was first collected in southern California at about the same time but was apparently much more common than Watersipora subtorquata until at least the late 1960s (Cohen, 2011). Watersipora subtorquata is now, however, reported predominantly from subtropical and tropical waters of the Atlantic and Mediterranean (Vieira et al., 2014), but occurs also in Korea. The similar species W. subatra differs mainly in the presence of multiporous septula and occurs mainly in the NE Atlantic (British Isles), Indo-West Pacific (Indonesia, Japan) and Pacific (New Zealand, Australia and California). The provenance for dispersal of W. subatra in the East China Sea may have been Japan, where it has been known for many years (Mawatari, 1952), while the source of W. subtorquata may have been Korea (Seo, 1999). As with Cryptosula pallasiana, W. subtorquata larvae spend less than a day in the plankton before settling (Cohen, 2011), so its transportation over long distances as larvae in oceanic currents or in ballast water is unlikely, although ships' ballasts can include locally sourced rocks which may theoretically be encrusted by this and other bryozoans. However, W. subtorquata more probably reached the west coast of North America by fouling ships' hulls. It has often been found on ships' bottoms as it is highly tolerant of copper-based, antifouling compounds (McKenzie et al., 2012). Watersipora subtorquata is also reported to be capable of self-fertilization, which would make it easier for one or a small number of colonies transported to a distant location to establish a viable population (Cohen, 2011). Due to the problems of distinguishing between W. subtorquata and W. subatra in the present paper, we refer to the studied specimens as Watersipora sp. Although one of the reviewers suggested that our species might be Watersipora subatra, the presence of strong calcification on the proximal lateral margin, and the shape of the operculum and sinus do not allow us to identify our specimens unequivocally as this species.

The aim of the present paper is to describe the distributions and competition for living space between these two common, sheet-like cheilostome bryozoan species that are important as invasive foulers, and to suggest factors that may influence the outcome of this competition.

2 MATERIAL AND METHOD

We studied six sections on the hull of the Sea Gull (Hai'ou in Chinese). This is a wharf ship used as a pontoon for mooring other ships, and has a metal hull, length 48.52 m, width 7.09 m and with a gross tonnage of 381 tons. The hull was treated with HJ 406 copper anti-fouling paint just before mooring.

This ship was anchored in Middle Harbour (Zhong Gang) in Qingdao Bay (GPS coordinates 36°05′N, 120°18′E) from September 2009 until its dockage in April 2015. It was oriented with the bow to the south and moored to the wharf by its stern. Therefore, the port side of the ship was exposed to the sun, while the starboard side was in shadow of the wharf throughout most of the five and a half-year period of anchorage. Water depth around the ship was 4–5 m. Water temperature (Fig. 1) was measured using a portable CTD type AAQ1183-1F just under the ship from November to August. Unfortunately, the values for the other months are unavailable due to lack of access to the harbour. However, the values can be predicted from Fig. 1. The measured values varied on average from 3.04℃ during the winter to 24.19℃ in the summer. While we studied the interaction after 5.5 years, temperature data only pertain to one year. Exposure to wave action and current flow did not differ on the port and starboard sides of the hull.

Figure 1 Seawater temperature at 1 m, 2 m and 3 m in Middle Harbour (Qingdao) during the period November 2012 to August 2013, measured using portable CTD type AAQ1183-1F just under the ship

We scraped all fouling organisms off sections of the hull from the formerly submerged part of the ship, each section about 25 cm×25 cm in size. These samples were numbered 1 to 6, with even numbers used for samples from the port side (sunny) and odd numbers for samples from the starboard side (shaded). Each sample has two parts, A and B, part A being taken from the side of the hull near the waterline (vertically oriented), and part B from the bilge (inclined underside) of the hull at the corresponding position just under part A (Fig. 2). Therefore, 12 samples were taken altogether.

Figure 2 Locations of the samples taken The paper marks the position of Sample 1, comprising Sample 1A (grey arrow) from the vertical part of the hull near the former waterline, and Sample 1B (white arrow) from the inclined underside (bilge) of the hull.

Six of the samples (1A, 1B, 3A, 4B, 6A, and 6B) were fouled mainly by bryozoans. As the other samples contained mainly oysters, mussels, tunicates and only a few bryozoan colonies, but with no interactions between colonies of Cryptosula pallasiana and Watersipora sp., they were discarded for this study

We counted the number of colonies of Watersipora sp. and Cryptosula pallasiana from each sample; in the case of merged colonies, we tried to find the ancestrulae on the back-side of the colonies and counted the number. The maximum diameter of the encrusting colonies was small (45 mm), so colonies were collected almost intact when the samples were taken. Subsequently we searched for interactions between these two species along the edges of the colonies (Figs. 3, 4). The overgrowing species for each interaction was recorded but only when there was evidence that the overgrown colony was alive at the time, i.e., it contained organic tissues or showed a clear morphological response (producing smaller or incompletely developed zooids, for example) to being overgrown. Only a few interactions involved reciprocal overgrowth in which the outcome was reversed along the line of contact between the colonies. In these cases, there was no clear winner (Fig. 5). In one unusual example, contact between two colonies of the different species resulted in bifoliate erect growth, with one side being formed by Cryptosula and the other by Watersipora (Fig. 6).

Figure 3 Example of a typical contact between Cryptosula pallasiana (left) and Watersipora sp. (right) resulting in overgrowth by Watersipora The arrow indicates the position of the contact. Note the presence of opercula in both colonies showing that they were alive at the time of the interaction.
Figure 4 Example of overgrowth of Cryptosula pallasiana (right) by Watersipora sp. (left) The picture is taken from the under side, because, the Cryptosula was completely overgrown by Watersipora, so on the frontal side, only Watersipora is observable. Note the reaction of the Cryptosula colony in producing smaller zooids (arrow) showing that it was alive at the time of the interaction.
Figure 5 Example of an unclear winner in an interaction between Cryptosula pallasiana (pale coloured) and Watersipora sp. (red coloured) Note reciprocal overgrowth between Watersipora and Cryptosula from one part of the contact between the colonies to another part close to the arrow. Scale bar 1 cm
Figure 6 Example of an unusual contact between Cryptosula pallasiana (pale coloured) and Watersipora sp. (red coloured) that resulted in bifoliate erect growth of the combined colonies (arrowed) Scale bar 1 cm

The coverage of the Bryozoa on the selected samples was measured from photographic images using CorelDraw8 software. The sizes of Cryptosula and Watersipora zooids were measured using the integrated software with an Opto-digital microscope Olympus DSX500 system. We made 82 to 122 measurements on three to five colonies of each of four types (82 measurements on three colonies of Cryptosula from the sunny side, 122 measurements on five colonies of Watersipora from the sunny side, 112 measurements on four colonies of Cryptosula from the shaded side, and 82 measurements on four colonies of Watersipora from the shaded side). We used an online Chi-square test with one degree of freedom and a two-tailed P value to test the statistical significance of our results.

3 RESULT 3.1 Species composition

Altogether four bryozoan species were found fouling the ship's hull: Watersipora sp., Cryptosula pallasiana, Pacificincola perforata (Okada and Mawatari, 1937) and Tricellaria occidentalis (Trask, 1857). The dominant species were Watersipora sp. and Cryptosula pallasiana, whereas Pacificincola perforata was the least common.

Species composition and coverage by bryozoans differed on the starboard and port sides of the ship. The starboard vertical side, which was in shadow during mooring, was fouled by all four identified bryozoan species. However, on the port vertical side, which was exposed to the sun, only Cryptosula and Watersipora were found. The difference in the hull bilge (underside) was less pronounced: on the starboard side all four species were found, but on the port side Tricellaria occidentalis was found as well as Cryptosula and Watersipora.

The coverage of the Bryozoa on the vertical face of the hull ('A' samples) on the port side (sunny side) of the ship was approximately 22%–35% (measured from photographic images), while on the starboard (shaded) coverage was greater than 55%.

3.2 Distributions and interactions between Cryptosula pallasiana and Watersipora sp.

Overgrowth interactions between Cryptosula pallasiana and Watersipora sp. and the occurrence of these two species in the studied samples are summarised in Table 1. A significantly greater number of Watersipora sp. colonies were found on the starboard side of the ship, which was in shadow during the period of mooring (249 vs 57, Chi squared X2=120.471, P < 0.000 1). In contrast, Cryptosula pallasiana colonies dominated on the port side of the ship, which was exposed to the sun (187 vs 124; X2=10.646, P=0.001 1). Despite the small number of samples (only six samples were suitable for studying interactions), these results show a strong contrast in the relative dominance of the two major fouling species between the shaded and sunny sides of the hull. The range of colony diameters (15–45 mm) in both species was limited, so the dominance in number of colonies corresponds to dominance in spatial coverage.

Table 1 Results of the interaction between Watersipora sp. and Cryptosula pallasiana in the different samples analysed

Watersipora sp. won almost all of its overgrowth interactions with Cryptosula pallasiana (Fig. 3). Competitive dominance of Watersipora sp. was particularly pronounced on the shaded side (X2=63.000, P < 0.000 1). However, even in samples from the sunny (port) side where Watersipora sp. was less common and occasionally had the older parts of the colonies overgrown by Cryptosula pallasiana, it still won a significantly greater proportion of interactions (X2=19.593, P < 0.000 1).

3.3 Differences in size of zooids of Cryptosula pallasiana and Watersipora sp. from sunny and shaded sides

We measured the lengths and widths of Cryptosula pallasiana and Watersipora sp. zooids in samples from the sunny and shaded sides of the ship. As shown in Fig. 7, there are considerable differences in the size of C. pallasiana zooids from sunny and shaded sides, while the average size of Watersipora sp. zooids is almost the same on both sides. The width of C. pallasiana zooids from the sunny side of the ship is slightly larger (362–609 μm, average 474 μm±57 μm) than zooids from the shaded site (334–504 μm, average 393 μm±52 μm), and length showed a similar pattern: 616–1 046 μm (average 875 μm±101 μm) on the sunny side vs. 522–827 μm (average 655 μm±52 μm) on the shaded side. The width of Watersipora sp. zooids on the sunny side was 341–605 μm (average 474 μm± 54 μm), compared with 421–690 μm (average 540 μm±61 μm) on the shaded side. Zooid length was 910–1 459 μm (average 1 131 μm±116 μm) on the sunny side and 845–1 442 μm (average 1 069 μm± 119 μm) on the shaded side.

Figure 7 Chart showing the differences of size of Cryptosula pallasiana and Watersipora sp. zooecia from sunny and shaded sides of the ship The lines show linear regressions of the values
3.3.1 Statistical analyses of size data (see Table 2)
Table 2 Statistical analysis of length and width (μm) of Cryptosula and Watersipora on the shaded side versus the sunny side

Length of Watersipora zooids: according to two sample F-test for variance for alpha 0.01 the test criterion are 1.06; because critical value for 80 and 120 measurements are 1.60. The value shows that the standard deviations are not different. We used a twosample t-test with equal variance to show that the average length is significantly smaller on the shaded side than on the sunny side. Test criterion is -3.67, one tail critical value for alpha 0.01 is -2.35, therefore the test criterion lies outside critical area (-2.35; infinity), so the null hypothesis is falsified and the average values of length are significantly different.

Width of Watersipora: according to two sample F-test for variance for alpha 0.01 the test criterion is 1.26. Therefore we used two-sample t-test with equal variance to show significant differences in average values in shaded and sunny sides. The null hypothesis is that the average values are same. Test criterion is 7.96, one tail critical value for alpha 0.01 is 2.35. Because the test criterion lies outside critical area (minus infinity; 2.35), the null hypothesis is rejected and the average values of width are significantly different (the average width on the shaded side is smaller than on the sunny side).

Length of Cryptosula: according to two sample F-test for variance for alpha 0.01 the test criterion are 2.00; because critical value for 70 and 110 measurements are 1.64, this value shows that the standard deviations are different. Therefore we used a two-sample t-test with unequal variance to show statistically significant differences in average value between the shaded side, which is smaller and the sunny side. The null hypothesis is that the average values are the same. Test criterion is -15.70; one tail critical value for alpha 0.01 is -2.36, therefore, the test criterion lies outside critical area (-2.36; infinity), so the null hypothesis is rejected and the average values of length are significantly different.

Width of Cryptosula: according to two sample F-test for variance for alpha 0.01 the test criterion are 1.20; because critical value for 70 and 110 measurements are 1.64, this value shows that the standard deviations are not significantly different. Therefore, we used a two-sample t-test with equal variance to show statistically significant differences in average value between the shaded side, which is smaller, and the sunny side. The null hypothesis is that the average values are the same. Test criterion is -9.75; one tail critical value for alpha 0.01 is -2.35, therefore, the test criterion lies outside the critical area (-2.35; infinity), so the null hypothesis is falsified and the average values of length are significantly different.

4 DISCUSSION

Species of Watersipora and Cryptosula pallasiana are invasive foulers (Gordon and Mawatari, 1992; Vieira et al., 2014), adapted for rapid growth and winning in competition for substrate space. Following previously published data (Jackson, 1983; Abdel Salam and Ramadan, 2008 and many others; Cohen, 2011), these species can be categorized as r-strategists, allocating a relatively high proportion of their available energy to the rapid production of gametes capable of fouling surfaces as soon as they become available. Both normally lack polymorphs (although according to Winston (1982) small suboral avicularia are occasionally developed in C. pallasiana), and neither have ovicells for larval brooding (larvae are brooded internally, see Ostrovsky et al., 2009 and references therein).

Putative Watersipora subovoidea was found to be little affected by contact with neighbouring organisms in Tomioka Bay, Japan (Nandakumar and Tanaka, 1994). In this Japanese study, Watersipora showed significantly better growth than the two other studied bryozoans (Celleporaria aperta (Hincks, 1882) and Schizoporella serialis (Heller, 1867)) when growing close to neighbouring organisms such as algae, polychaetes, bryozoans and ascidians. In an earlier study on interspecific competition among sessile organisms from the same area, putative W. subatra was found to be higher in the competitive hierarchy for space than either C. aperta or S. serialis (see Nandakumar et al., 1993). Even though the species identity of the bryozoans used in these studies is not clear (see Vieira et al., 2014), the results may be applicable to species of Watersipora, including the Watersipora sp. in the current study.

Watersipora is apparently more immune than Cryptosula to the effects of various antifouling paints. A study in which a ship's hull was coated with three antifouling paints resulted in 64% of its surface being covered with W. subtorquata within 16 weeks; 22 other species (including Cryptosula pallasiana) occurred exclusively on top of the W. subtorquata colonies; no Cryptosula colonies were found directly encrusting the surface of the hull (Floerl et al., 2004). In our study, however, colonies of Cryptosula were found directly encrusting the surface of the hull on both sides. This might reflect depletion of the antifouling agent after a long period (>5 years) since its application.

An important difference between the Chinese Watersipora sp. and Cryptosula pallasiana may be in their growth rates. Amui-Vedel et al. (2007) gave the minimum specific growth rate (r) for C. pallasiana as 0.017 and the maximum rate as 0.092 (this study calculated specific growth rate as r=ln(N/N0)/t, where N0 is the number of zooids at the beginning of the experiment, and N the number of zooids on day 27 at the end of the experiment). Lonhart (2012) reported the linear growth rate of putative Watersipora subtorquata to be 0.33 mm per day in California (Monterey Harbour). Fine and Loya (2003) gave the growth rate of Watersipora sp. in summer in the vermetid reefs of Sdot-Yam (Israel), at depths of 1–6 m, to be 6 mm±3 mm per month. The specific growth rate of Watersipora calculated from these linear growth rates by the method of Amui-Vedel et al. (2007) is 0.085–0.125, which is appreciably greater than the 0.017–0.092 reported in C. pallasiana. It should, however, be noted that these studies were undertaken in climatically different regions; Kuklinski et al. (2013), for example, found growth rates of sheet-like bryozoans to be greater in lower latitudes.

On the sunny side of the hull of the studied ship moored in Qingdao Harbour, temperatures were almost certainly higher. Our results show the production of larger zooids in Cryptosula pallasiana colonies on the sunny side compared to the shaded side. This is consistent with the findings of AmuiVedel et al. (2007) that Cryptosula produces larger zooids in warmer waters, which is in contrast to previous studies on a number of other cheilostome species that bud smaller zooids in warm summer temperatures than in cold winter temperatures (Okamura, 1987; Okamura and Bishop, 1988; O'Dea and Okamura, 1999). Different genetically defined groups of Watersipora appear to show invasion patterns that can be predicted by ambient temperatures (Mackie et al., 2012). Therefore, within this genus there are probably important variations in temperaturerelated adaptation. However, both survival and growth have been found to be temperature independent (Sorte et al., 2010). A zooid size-temperature relationship has been pointed out in Watersipora across multiple species and environments (Ryland et al., 2009).

It seems possible that the larger zooids budded by C. pallasiana may allow it to compete more successfully with Watersipora sp. on the sunny side of the ship during the summer. Moreover, the specific growth rates of C. pallasiana changed with temperature, ranging from 0.041 to 0.092, with an average rate of 0.066±0.015 8 (standard deviation) at 18℃, whereas the specific growth rate at 14℃, just 4℃ less, was reduced by nearly half to 0.034± 0.009 7 (Amui-Vedel et al., 2007). In our samples the differences of size between C. pallasiana zooids growing on sunny and shaded sides were smaller than the seasonal differences described by Amui-Vedel et al. (2007) (Fig. 7). The average difference in length was 138 μm (the length of zooids on the sunny side averaged 875 μm, while on samples from shaded side the average was 738 μm), and the average difference in width was 69 μm (the width of zooids on the sunny side averaged 474 μm, while samples from the shaded side averaged 405 μm) (see above Table 2 for the statistical significance of these differences). Even this small size increase may perhaps help Cryptosula to win at least some of its interactions with Watersipora on the sunny side. Although we do not know the exact differences in temperature between the sunny and shaded sides of the ship moored in Qingdao Harbour, we expect higher temperature on the side exposed to the sun.

The superiority of Watersipora sp. in competition for space with Cryptosula pallasiana could be linked with feeding intensity. Bryozoans with a greater number of tentacles are capable of creating more powerful feeding currents that may potentially deplete the shared food resources available to their spatial competitors (cf. McKinney, 1992): Watersipora sp. usually has 20–24 tentacles (Vieira et al., 2014), while Cryptosula has only 16–17 tentacles (Calvet, 1900) or 15–16 tentacles (Amui-Vedel et al., 2007).

5 CONCLUSION

The spatial distributions and competition for substrate space between two common fouling species of bryozoans (Watersipora sp. and Cryptosula pallasiana) were studied from different sites on the hull of a ship that had been moored in the water for five and a half years in Qingdao Harbour (China). The position of ship in the harbour meant that one side was exposed to the sun and the other was in the shade. On the shaded side of the ship, a maximum of 115 colonies of Watersipora sp. were recorded in the sample taken (altogether 249 colonies were recorded from all studied samples), compared with 52 colonies of C. pallasiana from the same sample (altogether 124 colonies were recorded from all studied samples). On the sunny side, only 26 colonies of Watersipora sp. were recorded from the sample taken (altogether 57 colonies were recorded from all studied samples), compared to 76 colonies of C. pallasiana in the same sample (altogether 187 colonies were recorded from all studied samples).

In a previous study (Amui-Vedel et al., 2007) of Cryptosula pallasiana, average specific growth rate doubled with an increase of 4℃, while another study (Sorte et al., 2010) has shown Watersipora to have a growth rate that is temperature independent. Unusually for a bryozoan, Cryptosula produces larger zooids in warmer water, which may help it to compete with Watersipora on the sunny (and presumably warmer) side of the hull

Therefore, we can conclude that:

1) colonies of C. pallasiana on the sunny side of the ship were found to have considerably longer zooids than those from the shaded side. The result is consistent with a previous study (Amui-Vedel et al., 2007) and might be related with differences in ambient temperatures;

2) zooids of Watersipora do not show significant differences in size on the sunny vs. shaded sides, which agrees with previously published data (Sorte et al., 2010);

3) regardless of location on the sunny or shaded side of the ship's hull, Watersipora sp. invariably won spatial competitive interactions with Cryptosula pallasiana, although the latter performed slightly better on the sunny side of the hull, which may correlate with the larger size of the zooids in colonies of C. pallasiana on this side.

Reasons for the superiority of Watersipora sp. in spatial competition with Cryptosula pallasiana might include:

a) faster growth rate: previous studies have determined a specific growth rate of 0.085–0.125 in Watersipora sp. (Lonhart, 2012) compared with 0.017–0.092 in Cryptosula pallasiana (Amui-Vedel et al., 2007);

b) stronger feeding currents: lophophores of Watersipora sp. have 20–24 tentacles, while those of Cryptosula pallasiana have 15–17 tentacles.

6 ACKNOWLEDGMENT

We thank PENG Bo and the staffs of Qingdao Tony Machinery and Equipment Co. Ltd. who were helpful with the sample collection and the sites photos. Our thanks also go to the anonymous referees whose valuable comments improved the paper. Thanks go also to Tomáš Zágoršek for help with the statistical analyses.

References
Abdel-Salam K M, Ramadan S E, 2008. Fouling Bryozoa from some Alexandria harbours, Egypt. (Ⅱ) encrusting species. Mediterranean Marine Science, 9(2): 5–20. Doi: 10.12681/mms.129
Amui-Vedel A M, Hayward P J, Porter J S, 2007. Zooid size and growth rate of the bryozoan Cryptosula pallasiana Moll in relation to temperature, in culture and in its natural environment. Journal of Experimental Marine Biology and Ecology, 353(1): 1–12. Doi: 10.1016/j.jembe.2007.02.020
Calvet L, 1900. Contribution à l'histoire naturelle des bryozoaires ectoproctes marins. Travaux de l'institut de zoologie de l'Université de Montpellier et de la station zoologique de Cette Memoire, 8: 1–488.
Cohen A N. 2011. The exotics guide: non-native marine species of the North American Pacific coast. Center for Research on Aquatic Bioinvasions, Richmond, CA, and San Francisco Estuary Institute, Oakland, CA. September 2011. http://www.exoticsguide.org/. Accessed 2015-09-11.
d'Orbigny A. 1852. Paléontologie française, Terrains Crétacés, V, Bryozoaires. Victor Masson, Paris. p. 185-472.
Fine M, Loya Y, 2003. Alternate coral-bryozoan competitive superiority during coral bleaching. Marine Biology, 142(5): 989–996. Doi: 10.1007/s00227-002-0982-7
Floerl O, Pool T K, Inglis G J, 2004. Positive interactions between nonindigenous species facilitate transport by human vectors. Ecological Applications, 14(6): 1724–1736. Doi: 10.1890/03-5399
Gordon D P, Mawatari S F, 1992. Atlas of marine-fouling Bryozoa of New Zealand ports and harbours. Miscellaneous Publication New Zealand Oceanographic Institute, 107: 1–52.
Heller C, 1867. Die Bryozoen des adriatischen Meeres. Verhandlungen der Zoologisch-Botanischen Gesellschaft in Wien, 17: 77–136.
Hincks T, 1882. Contributions towards a general history of the marine Polyzoa. Part X. Foreign Cheilostomata(Miscellaneous). Annals and Magazine of Natural History, 5(10): 160–170.
Jackson J B C. 1983. Biological determinants of present and past sessile animal distributions. In: Tevez M J S, McCall P L eds. Biotic Interactions in Recent and Fossil Benthic Communities. Springer, New York. p. 39-107.
Kuklinski P, Sokolowski A, Ziolkowska M, Balazy P, Novosel M, Barnes D K A. 2013. Growth rate of selected sheetencrusting bryozoan colonies along a latitudinal transect: preliminary results. In: Ernst A, Schäfer P, Scholz J eds. Bryozoan Studies 2010. Springer, Berlin Heidelberg. p. 155-167.
Lonhart S I. 2012. Growth and distribution of the invasive bryozoan Watersipora in Monterey Harbor, California. In: Steller D, Lobel L eds. Proceedings of the American Academy of Underwater Sciences 31st Symposium. AAUS, Dauphin Island, AL. p. 89-98.
Mackie J A, Darling J A, Geller J B, 2012. Ecology of cryptic invasions:latitudinal segregation among Watersipora(Bryozoa) species. Scientific Reports, 2: 871. Doi: 10.1038/srep00871
Mawatari S, 1952. On Watersipora cucullata (Busk) Ⅰ.Systematic study. Miscellaneous Reports of the Tokyo Research Institute of Natural Resources, 25: 14–17.
McKenzie L A, Johnston E L, Brooks R, 2012. Using clones and copper to resolve the genetic architecture of metal tolerance in a marine invader. Ecology and Evolution, 2(6): 1319–1329. Doi: 10.1002/ece3.241
McKinney F K, 1992. Competitive interactions between related clades:evolutionary implications of overgrowth interactions between encrusting cyclostome and cheilostome bryozoans. Marine Biology, 114(4): 645–652. Doi: 10.1007/BF00357261
Moll J P C. 1803. Eschara, ex zoophytorum, seu, phytozoorum ordine pulcherrimum ac notatu dignissimum genus, novis speciebus auctum, methodice descriptum et iconibus ad naturam delineatis illustratum. Camesiniana, Vindobonae. p. 1-70.
Nandakumar K, Tanaka M, Kikuchi T, 1993. Interspecific competition among fouling organisms in Tomioka Bay, Japan. Marine Ecology Progress Series, 94(1): 43–50.
Nandakumar K, Tanaka M, 1994. Effects of neighboring organisms on the growth of three intertidal encrusting cheilostome bryozoans. Marine Ecology Progress Series, 114: 157–163. Doi: 10.3354/meps114157
O'Dea A, Okamura B, 1999. Influence of seasonal variation in temperature, salinity and food availability on module size and colony growth of the estuarine bryozoan Conopeum seurati. Marine Biology, 135(4): 581–588. Doi: 10.1007/s002270050659
Okada Y, Mawatari S, 1937. On the collection of Bryozoa along the coast of Onagawa Bay and its vicinity, the northern part of Honshu, Japan. Science Reports Tôhoku University, 11: 433–445.
Okada Y, 1929. Report of the biological survey of Mutsu Bay, 12, Cheilostomatous Bryozoa of Muts Bay. Sciences Report of the Tohoku Imperial University, 4: 11–35.
Okamura B, Bishop J D D, 1988. Zooid size in cheilostome Bryozoans as an indicator of relative palaeotemperature. Palaeogeography, Palaeoclimatology, Palaeoecology, 66(3-4): 145–152. Doi: 10.1016/0031-0182(88)90197-6
Okamura B. 1987. Seasonal changes in zooid size and feeding activity in epifaunal colonies of Electra pilosa. In: Ross J R P ed. Bryozoa: Present and Past. Western Washington University, Bellingham. p. 197-203.
Ostrovsky A N, O'Dea A, Rodríguez F, 2009. Comparative anatomy of internal incubational sacs in cupuladriid bryozoans and the evolution of brooding in free-living cheilostomes. Journal of Morphology, 270(12): 1413–1430. Doi: 10.1002/jmor.10767
Ryland J S, De Blauwe H, Lord R, Mackie J A, 2009. Recent discoveries of alien Watersipora (Bryozoa) in Western Europe, with redescriptions of species. Zootaxa, 2093: 43–59.
Seo J E, 1999. Taxonomic review of Korean Watersipora(Bryozoa, Gymnolaemata, Cheilostomata). Korean Journal of Systematic Zoology, 15(2): 221–229.
Sorte C J B, Williams S L, Zerebecki R A, 2010. Ocean warming increases threat of invasive species in a marine fouling community. Ecology, 91(8): 2198–2204. Doi: 10.1890/10-0238.1
Trask J B, 1857. On some new microscopic organisms. Proceedings of the California Academy of Natural Sciences, 1: 99–102.
Vieira L M, Jones M S, Taylor P D, 2014. The identity of the invasive fouling bryozoan Watersipora subtorquata(d'Orbigny) and some other congeneric species. Zootaxa, 3857(2): 151–182. Doi: 10.11646/zootaxa.3857.2
Winston J E, 1982. Marine bryozoans (Ectoprocta) of the Indian River area, Florida. Bulletin of the American Museum of Natural History, 173: 99–176.