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MARINE ECOLOGY PROGRESS SERIES Vol. 167: 155-169, 1998 Published June 18 Mar Ecol Prog Ser

Spatial and temporal variability of patterns of colonization by mussels ( trossulus, M. edulis) on a wave-exposed rocky shore

Heather L. Hunt*, Robert E. Scheibling

Department of Biology. Dalhousie University, Halifax, Nova Scotia B3H 451. Canada

ABSTRACT: Colonization rates of mussels (Mytilus trossulus and M. edulis) were measured on natural substrata in tidepools and on emergent rock in recently ice-scoured and non-scoured regions of a rocky shore near Halifax, Nova Scotia, Canada. The relative importance of initial settlement/colonization, compared to subsequent dispersal and mortality, in determining the distribution and abundance of mussels was examined by comparing patterns and rates of mussel colonization at sampling intervals of days to months over a 17 mo period. Lrss than 4 ":, of mussels which colonized the quadrats sampled at short (2 to 7 d) intervals were settling larvae (2 mm, too large to be dispersed by byssal drifting, suggesting they \Yere redistributed by wave dislodgment and deposition. At both short (2 to 7 d) and long (5 to 16 mo) sarnpllng ~ntervdls,colon~sts were most abundant in ice-scoured tide- pools and least abundant on ice-scoured emergent rock, probably reflecting d~fferences In the

macrobenthic assemblaqe. the sllhc;tratl~m fnr co!oniza!ic~. 1:: addi:ion, thr- luny L~IIIIdbunaance oi colonists was linearly related to the cumulativct short term abundance during all but one of the inter- vals. Therefore, our results ~ndicatethat, over time scales up to 16 mo, patterns of initial colonization by settlers and larger post-larval mussels were inore important than post-colonizati.on mortality and dis- persal in determining pattt=rns of distribution and abundance of n~usselson this shore

KEY WORDS: Colonization Post-settlement dispersal . Mussels . lMytilus Ice scour . Intertidal zone Tidepools

INTRODUCTION (Woodin 1991). Post-settlement transport of juvenile molluscs can be actively initiated (Martel & Chia Studies of the role of recruitment variability in the 1991a), and is generally facilitated by the production of population and community dynamics of benthic long byssal or mucous threads which increase hydro- marine invertebrates have focused largely on pro- dynamic drag (Sigurdsson et al. 1976. De Blok & Tan- cesses influencing patterns of settlement by planktonic Maas 1977, Lane et al. 1985, Martel & Chia 1991a). larvae (reviewed by Butman 1987, Pawlik 2992, Young post-larval mussels can use threads to drift in Rodriguez et al. 1993).However, many benthic marine the water column at least until th~yreach a size of invertebrates, particularly molluscs, can disperse in -2 mm shell length (Sigurdsson et al. 1976, De Blok & the water column as juveniles (e.g. Sigurdsson et al. Tan-Maas 1977, Lane et al. 1985). Bayne (1964) 1976, Beukema & de Vlas 1989, Martel & Chia 1991b, demonstrated that Mytilus edulisentered a secondary Arrnonies 1992). When the rate of waterborne disper- pelagic phase at a size of 1 to 2 mm and moved from sal of juveniles is high, it may be an important deter- initial settlement sites on filamentous algae to a more minant of the distribution and abundance of adults permanent attachment on established beds of adult mussels. Although a temporary association between recently settled mussels and filamentous algae has 'Present address: MS 34, Woods Hole Oceanograph~clnstjtu- tion, Woods Hole, Massachusetts 02543, USA. been observed in several other studies (e.g. Seed 1969, E-mall: hlhunt@\uhoi.edu King et al. 1989), mussels also may settle directly onto

0 Inter-Research 1998 Resale of full article not perm~tted 156 Mar Ecol Prog Ser 167: 155-169, 1998

adult mussel beds (McGrath et al. 1988, Caceres- to compare the relative abundance of the 2 species Martinez et al. 1993, 1994). Patterns of post-settlement between habitats. In Ma.rch 1997, we collected 32 mus- dispersal may partially account for sporadic and un- sels in 3 size classes from each of 3 tidepools and 3 predictable pulses of recruitment which characterize adjacent areas of emergent rock. <5 mm (n = 8), many populations of Mytilus (Seed & Suchanek 1992). 5-9.9 mm (n = 8), and 10-24.9 mm shell length (SL) Although byssal drifting in the water column generally (n = 16). The mussels were identified to species using a involves small juveniles, larger mussels may be redis- polymerase chain reaction assay of a marker for inter- tributed by wave action or may move by crawling nal transcribed spacer regions between the 18s and (Paine 1974, Hunt 1997) Dispersal of large mussels 28s nuclear rDNA coding regions (Heath et al. 1995). may increase the rate of recovery of mussel cover after DNA was extracted from the whole for mussels disturbance and influence the dynamics of established

1964). We examined the effects of post-colonization We grouped the mussels collected at the shortest mortality and dispersal on patterns of initial coloniza- sampling intervals (2 to 7 d) into 4 size classes: 5 mm SL. We refer to mussels mussel colonists) at different frequencies, since the ex- which are 5 mm SL). and crustose forms. 158 Mar Ecol Prog Ser 167. 155-169, 1998

RESULTS cantly between tidepools (76%) and emergent rock (66%) (G, = 1.20, p = 0.27). These results are consistent Species composition with a similar analysis of mussels collected the previ- ous year which indicated that -80 % of mussels in both We compared the frequency of Mytilus trossulus and habitats were M. trossulus (Hunt & Scheibling 1996). M. edulis (Table 1) among size classes (<5, 5-9.9, At another wave-exposed shore in Nova Scotia (ca 110 mm) and between tidepools and emergent rock 30 km away), Pedersen (1991) found that 77 to 91 D/oof using contin.gency tables. Hybrids were not included settlers (

Table 1 Frequency of Mytilus trossulus, M. edulis, and hybrids of the 2 species in 3 size classes (<5,5-9.9, and 10-24.9 mm) of musse1.s collected from tidepools and emergent rock

Size class Habitat M, trossulus M. eduhs Hybrids

Tidepool Emergent rock Tidepool Emergent rock Tidepool Emergent rock

Total Tidepool Emergent rock

Tldepools Non-scoured --- Scoured Emergent Rock -- Non-scoured - Scoured Fig. 1 Mytilus spp. Colonization rate of mussels of each of 4 size classes (5 mm SL) in quadrats in ice- 5 15 3 .-+ scoured and non- .W- scoured tidepools 0C and emergent rock -o monitored at short 10 2 E (2 to 7 d) sampling Cf intervals from July r0 1993 to November c 1994. Data were '" 5 1 averaged across 3 quadrats per plot and across 3 plots within each combi- 0 0 nation of habitat J ASONDJ FMAMJ J ASON JASONDJFMAMJJASON and stratum 1993 1994 1993 1994 Hunt & Scheibling: Vanability of mussel colonization patterns -- 159

Table 2. Mytilus spp. Three-factor ANOVA of the cumulative density (no. 100cm-') of mussels of each of 4 size classes colonizillg quadrats sampled at short intervals from July to November 1993 and from May to November 1994. Factors are Habitat (H. tide- pools and emergent rock), Stratum (S, ice-scoured and non-scoured), and Plot (nested within H X S). Effects of Habitat. Stratum, and the interact~onbetween Habitat and Stratum were tested against the mean square error of Plot, and the effect of Plot was tested against the residual mean square error. 'p < 0.05; "p < 0.01; "'p < 0.001. The results of a posterior1 tests are presented in the 'Comparison' column. When there was a significant H X S interaction, means were compared between habitats within each stratum and between strata within each habitat uslng t-tests (TP = tidepool. ER = emergent rock. N-S = non-scoured, S = ice- scoured). = indicates a non-significant result, while < or > indicates a significant result (a= 0.05)

Size class Source df MS P Comparison -- -- -P P 1993 ER Res~dual 24 0.05

0.5-1.9 mm Habitat 1 11.46 0.003 m TP: N-S=S Stratum 1 0 25 0 55 ER: N-S>S Habitat X Stratum 1 6.57 0.01 ' N-S: TP=ER Plot (H X S) 8 0 65 0.006 ' S: TP>ER Residual 24 0.18 2-4.9 mm Habitat 1 4.58 0.004 " TP: N-S=S Stratum 1 2 39 0.02' ER. N-S>S Habitat X Stratum 1 2.44 0.02' N-S. TP=ER Plot (H X S) 8 0.29 0.07 S: TP>ER Residual 24 0.14 >5 mm Habitat 1 2.45 <0.001"' TP: N-S=S Stratum 1 0.88 0.008" ER- N-S>S Habitat X Stratum 1 1.18 0.004. N-S. TP=EK Plot (H X S) 8 0.07 0.54 S: TP>ER Residual 24 0.08 1994 <0.5 mm Habitat 1 3 82 0.002" TP. N-S

Stratum 1 2.06 0.009 m ER:W-S=S Habitat X Stratum 1 1.79 0.01 ' N-S: TP=ER Plot (H X S) 8 0.18 0.002 " S: TP>ER Residual 24 0.04 0.5-1 9 mm Habitat 1 6.26 0.004" TP: N-S=S Stratum 1 0.53 0.28 ER:N-S>S Habitat x Stratum 1 2.71 0.03' N-S: TP=ER Plot (H X S) 8 0.40 0.005" S: TP>ER Residual 24 0.10 2-4 9 mm Habitat 1 3.70 Stratum 1 0.06 Habitat X Stratum 1 1.18 Plot (Hx S] 8 0.24 Residual 24 0.10 >5 mm Habitat 1 4.60 <0.001 "' TP: N-S=S Stratum 1 0.12 0.40 ER N-S>S Habitat X Stratum 1 2.08 0.01 ' N-S: TP=ER Plot (H X S) 8 0.16 0.23 S: TP>ER Residual 24 0.110 were settling larvae (<0.5 mill SL). Settlement oc- August and October/November in 1994. Colonization curred from August to November, while larger mussels by larger size classes was at a peak when sampling colonized the quadrats over a more extended period began in July 1993 and peaked again in JuneIJuly from May to December. The daily colonization rate by 1994. Colonization by 0.5-1.9 mm mussels also peaked all size classes of mussels was negligible in winter/ in September/October in both years. early spring (January to April 1994). Settlement of ANOVA (Table 2) showed a significant interaction in ~0.5mm mussels peaked in September in 1993 and in the effects of Habitat and Stratum on the cumulative 160 Mar Ecol Prog Ser 167. 155-169, 1998

Scoured Non-scoured July-November 1993 0.5-1.9mm 2-4.9mm >5 mm Total 15

lo~c~m~ 202515 300400500 0 Fig. 2. ~Vytilus spp. 0 Mean (+ SE) cumula- 70 ::IA 10 200 tive number of mussels 5 50 0 5 100 (per 100 cm2) collected C from July to November c O 0 0 0 0 1993 and from May to .--U November 1994 from t Mav-November l994 the quadrats sampled >5 mm Total at short intervals in ice-scoured and non- scoured tidepools (TP) and emergent rock (ER). Data were aver- aged across 3 quadrats per plot and across 3 plots wi.thin each com- bination of habitat and stratum

density of colonists for each size class of mussels in emergent rock (Fig. 2). We did not compare coloniza- both years, except for 2-4.9 mm mussels in 1994 when tion between years because sampling in 1993 began in the interaction was marginally non-significant and the July when colonization by large mussels was at a peak. cumulative density of colonists was significantly We examined the size distributions of mussel higher in tidepools than on emergent rock. Post hoc colonists by pooling individuals over the main colo- comparisons of means showed that settlers (<0.5 mm) nization periods in 1993 and 1994 (Fig. 3). Small mus- were 1 to 2 orders of magnitude more abundant in sels were proportionately more abundant in 1993, tidepools than on emergent rock in ice-scoured areas, when sampling began in July, than in 1994, when sam- but did not differ significantly between habitats in non- pling was carried out throughout the entire coloniza- scoured areas (Fig. 2, Table 2). Cumulative abundance tion period. In each year, 53% of colonists in any of settlers was significantly higher in ice-scoured than habitatktratum combination were recent settlers in non-scoured areas in tidepools, but did not differ (<0.5 mm). Mussels that were 0.5-1.9 mm represented significantly between strata on emergent rock. In con- the majority (50 to 81 %) of colonists in 1993, while trast, cumulative abundance of larger colonists was 2-4.9 mm mussels were the most abundant (53 to more similar among ice-scoured tidepools, and non- 71 %) colonists in 1994. Mussels that were >5 mm rep- scoured tidepools and emergent rock, but was consis- resented 3 to 8% of colonists in 1993 and 11 to 16% in tently lowest on ice-scoured emergent rock (Fig. 2). 1994. For each year, we compared the size distribu- Cumulative colonization by these larger mussels was tions of mussels between strata within each habitat significantly higher in tidepools than on emergent rock and between habitats within each strata using Kol- in ice-scoured areas, but did not differ significantly mogorov-Smirnov tests (Seigel & Castellan 1988) between habitats in non-scoured areas (Table 2). (Fig. 3). Mussels were pooled across quadrats and plots Moreover, colonization by larger mussels was signifi- within a habitat/stratum combination. In both years, cantly higher in non-scoured than in ice-scoured areas mussels 5 mm significantly between non-scoured and ice-scoured mussels. In both 1993 and 1994, the cumulative num- areas in each year In non-scoured areas, size distribu- ber of colonists summed across size classes was highest tions of colonists did not differ significantly between in ice-scoured tidepools and lowest on ice-scoured tidepools and emergent rock in 1993. However, this Hunt & Scheibling: Variability of mussel colonization patterns 161

difference was statistically significant in Tidepools Emergent Rock 1994, which reflected larger sample Non-scoured Scoured Non-scoured Scoured sizes in 1994 since the degree of differ- July-NOV93 ence remained small (D,,, = 0.07).

Colonization over long sampling intervals

The pattern of long term colonization was similar to the pattern of cumulative short term colonization (summed over all size classes of mussels): abundance was May-Nov 94 highest in ice-scoured tidepools and -0.15 lowest on ice-scoured emergent rock "'v (Fig. 4). For the 5, 11, and 16 mo inter- vals beginning in July 1993, ANOVA showed a significant interaction in the effects of Habitat and Stratum on the density of mussel colonists (Table 3). Post hoc comparison of means showed that the patterns of differences between habitats within strata, and between strata within habitats, were the same as Shell Length (mm) those of cumulative short term coloniza- tion of mussels >0.5 mm, i.e. coloniza- Fig. 3. Mytilus spp. Size frequency distributions of mussels collected from tion was greater in tidepools than on July to November 1993 and from May to November 1994 from the quadrats sampled at short intervals. Mussels were pooled across quadrats and plots emergent rock in ire-scoured areas, and ..-;.L;-v.,tL.A,L 2 ,,,,,,;,.a?:sr.rnm~,n of habit=.! cc! stratum. !n the first har. the hlack shad- greater on non-scoured than on ice- ing indicates settlers (~0.5mm SL), while the gray shad~ngindicates individ- scoured emergent rock. Colonization uals which were 0.5-0.9 mm. Brackets show results of Kolmogorov-Smirnov increased significantly over time, but not tests comparing the size distributions of mussels between strata within each habitat and between habitats within each stratum (D,,,, p; "'p > 0.5. 'p < 0.05, in proportion to the time elapsed: abun- "p < 0.01, "'p < 0.001) dance after 5 and 11 mo was 70 and

I1 mo (Jul 93-May 94)

.-V - -m Tidepool Emergent ~ock 6 mo 5 mo 500 (NO" 93-May 94) (May-Oct 94) Fig. 4. Mytilus spp. Mean (+ SE) den- Scoured 400 sity of mussel colonists in ice-scoured Non-scoured and non-scoured tidepools and emer- 300 gent rock after the 5, 11, and 16 mo intervals beginning in July 1993, and after the second and third 5 to 6 mo intervals. Data were averaged across 3 quadrats per plot and across 3 plots within each combination of habitat Tidepool Emergent Tidepool Emergent and stratum Rock Rock 162 Mar Ecol Prog Ser 167: 155-169, 1998

95%,, respectively, of the abundance after 16 mo (159 a significant interaction in the effects of habitat and mussels per 100 cm2, averaged across all habitathtra- stratum on the density of mussel colonists (Table 4). tum combinations). There were no significant interac- Differences between habitats within strata, and tions between time interval and either habitat or stra- between strata within habitats, were the same as for tum, nor was there a significant 3-way interaction. The the 5, 11, and 16 mo intervals beginning in 1993, density of colonists also varied significantly among except for the third 5 to 6 mo interval when the differ- plots within combinations of Habitat and Stratum. For ence between non-scoured and ice-scoured areas each of the three 5 to 6 mo intervals, ANOVA showed on emergent rock was marginally non-significant

Table 3. ~Mytilusspp. ANOVA of the number of mussel colonists in 100 cm2 quadrats after the 5, 11, and 16 mo intervals begin- nlng in July 1993. Factors are Habitat (H, tidepools and emergent rock), Stratum (S, i.ce-scoured and non-scoured), Plot (nested w~thinH X S), and Time (5, 11, and 16 mo). Effects of Habitat, Stratum, and the interaction between Hab~tatand Stratum were tested agalnst the mean square error of Plot, and effects of Time and the interactions between Time, Habitat, and Stratum were tested against the mean square error of the interaction between Time and Plot. The effect of Plot and the interaction between Time and Plot were tested against the residual mean square error. 'p < 0.05; "p < 0.01; "'p c 0.001. The results of a posteriori tests are presented .in the 'Comparison' column. Since there was a significant H X S interaction, means were compared between habitats with~neach stratum and between strata withln each habitat using t-tests (TP = tidepool, ER = emergent rock, N-S =non- scoured, S = ~ce-scoured).Slnce there was a signiflcant effect of Time, means were compared among time intervals (5 = 5 mo, 11 = 11 mo. 16 = 16 mo) using SNK. = indicates a non-significant result, while < or > indicates a significant result (a= 0.05)

Source P Comparison Habltat 0.001 " TP: N-S=S Stratum 0.22 ER: N-S>S Habitat X Stratum 0.001 N-S: TP=ER Plot (H X S) <0.001 "' S: TP>ER Tlme 0.004 5 < 11=16 Hab~tatX T~me 0.13 Stratum X Time 0.16 Habitat x Stratum X Time 0.57 Tlrne X Plot (H X S) 0.23 Residual

Table 4. Myt~lusspp. ANOVA of the number of mussel colonists in 100 cm2 quadrats after th.e three 5 to 6 mo intervals. Factors are Habitat (H, ttdepools and emergent rock), Stratum (S, ~ce-scouredand non-scoured), and Plot (nested cv~thlnH X S). Effects of Habitat, Stratum, and the interaction between Habitat and Stratum were tested against the mean square error of Plot, and the effect of Plot was tested against the residual mean square error 'p < 0.05, "p < 0.01; "'p < 0.001 The results of aposterion tests are presented in the 'Comparison' column. When there was a significant H X S interaction, means wcrc? compared between habi- tats within each stratum and between strata within each habitat using t-tests (TP = tidepool, EK = emergent rock, N-S = non-scoured, S = ice-scoured). = ind~catesa non-slgnlficant result, while < or > indicates a significant result (a = 0.05)

Interval Source Comparison .p 1st 5 to 6 mo Ha b~tat TP: N-S=S Stratum ER: N-S>S Habitat X Stratum N-S: TP=ER Plot (H x S) S: TP>ER Residual 2nd 5 to 6 mo Hab~tat TP: N-S=S Stratum ER: N-S>S Habltat X Stratum N-S: TP=ER Plot (H X S) S: TP>ER Residual 3rd 5 to 6 mo Habitat 1 TP: N-S=S Stratum 1 ER: N-S=S Habltat X Strdtum 1 N-S: TP=ER Plot (H X S) 8 S: TP>ER Hunt 8. Scheibling: Var~ab~l~tyof mussel colonization patlerns 163

Tidepools Emergent Rock After each of the longer term (5 to 16 mo) Non-scoured Scoured Non-scoured Scoured intervals, mussels 15 mm represented 72 to 5 mo (Jul-Nov 93) 100'2: of colonists and mussels > 10 mm repre- 10.13 n- I 0.18 ns~sented <10% (Fig. 5). We compared the size distributions of colonists between habitats within strata and between strata within habi- 40 tats for each interval. Differences in the size 20 distributions between combinations of habi- tat and stratum were not consistent over time and did not reflect the pattern observed in the 11 rno (Jul93-May 94)

019' I size distributions of cumulative short term 10.07' 80 10 15 "1 10.19 1 colonization (Figs. 3 & 5). However, after each of the 5 to 6 mo intervals, and the 11 and I 1 I I 16 mo intervals, mussels l mm SL were pro- portionately less abundant on ice-scoured emergent rock than in the other combinations of habitat and stratum. The absence of signif- 16 rno (Jul 93-0ct 94) 10.23 icant differences in size distributions in some 1 0 15 of the comparisons with ice-scoured emer- - 80 10.10"7 70.15 "1 "1 gent rock resulted from the smaller sample I l sizes from This habitat/stratum combination and not from smaller differences between cumulative size frequency distributions. We did not statistically compare the size distribu- 6 mo (Nov 93-May 94) tions among time intervals because the differ- -0.22 ns 0.28" I ences were clear and larger than the differ- 70.45"1 ences between habitats and strata within an 60,801 -0"01' ! i~terva!, and thc ar,a!yses ;vould have neces- - sitated a large number of comparisons. Mus- sels

Comparison of sampling frequencies

Shell Length (mm) To explore the importance of post-coloniza- tion mortality and dispersal in determining Fig. 5. Mytilus spp. Size frequency distributions of mussels after the 5, the abundance of colonists at the end of the 5 11, and 16 mo intervals beginning in July 1993, and the second and third to 16 mo intervals, we used regression analy- 5 to 6 mo ~ntervals.Mussels were pooled across quadrats and plots sis to examine the relationship between long within a combination of habitat and stratum. In the first bar, the black shading indicates settlers ( 0.5, 'p < 0.05, "p < 0.01, "'p < 0.001) short term colonization during the 5, 11 and 16 mo intervals beginning in July 1993. The slope of the relationship approached the (Table 4). Colonization varied significantly among maximum value of 1 during the first 5 to 6 mo interval plots within combinations of habitat and stratum after and the 11 mo interval, but was lower during the 16 mo the third, but not the first or second, 5 to 6 mo interval. interval. During the second 5 to 6 mo interval, long 164 Mar Ecol Prog Ser 167: 155-169, 1998

5 rno 16 rno (Jul 93-Oct 94) 1

Fig. 6. Myfilus spp. Relationship between abundance of colonists (no 100cm-~)after a 5 to 16 mo interval and 5 mo the cumulative short (May-Oct 94) term colonization (no. Tidepools o Non-scoured 100cm-9 during that Scoured interval for the 5, 11, Emergent Rock and 16 mo intervals Non-scoured Scoured beginning in July 1993, I and the second and third 5 to 6 mo inter- vals. Data are averages for 3 quadrats per plot. The dashed line is the l-to-l line, and the solid line is the regres- Cumulative Short Term Colonization sion line

term colonization also was significantly related to frequencies (D,,, = 0.25, p > 0.10). In each habitatktra- cumulative short term colonization, and the slope of tum combination during the third 5 to 6 mo interval, the relationship approached 1. However, during the mussels 69% of the variation, which is enhanced during the first 5 to 6 mo interval on non- unlikely to be due to chance. scoured emergent rock and during the third 5 to 6 mo Differences in the size distributions of colonists sam- interval in all combinations of habitat and stratum. pled at short and long sampling intervals can result from growth of individuals or size specific mortality or dispersal after initial colonization. We compared the Spatial and temporal variation in the macrobenthic size distributions of long term colonists to those of assemblage cumulative short term colonists for the first and third 5 to 6 mo intervals (Figs. 3 & 5) using Kolmogorov- The macrobenthic assemblage in the short and long Smirnov tests. In the first 5 to 6 mo interval, mussels term colonization quadrats varied markedly between

Scoured Tide~ools pools. Because many of the colonists were associated with macroalgae, our low esti- mates of mussel cover may partly reflect an artifact of our sampling method which recorded only the species/group in the top plane if there were several organisms at the same point on the substratum. How- ever, the relatively small size and low abundance (c3 cm-2) of mussel colonists at the end of each of the 5 to 6 mo inter- vals, the 11 mo interval, and the 16 mo Scoured Emergent Rock Non-scoured Emergent Rock interval indicates that the cover of mussels was probably not greatly underestimated.

DISCUSSION

Size of colonists and temporal pattern of colonization

- Sampling at short intervals (2 to 7 d) Sept Apr Jul Oct Sept Apr Jul Oct indicated that more than 96% of mussels 93 94 94 94 93 94 94 94 colonizing the natural substratum were too large (20.5 mm) to be settling larvae. B Sheets Jointed calcareous Most of these mussels (67 to 82 % in 1994) t3 Filarnentous Crustose 6l Coarsely branched Barnacles were > 2 mm and some were as large as 20 0 Thick leathery Bare substratum to 25 mm. Because mussels of this size are prcbably too heavy to drift in the watei- Fig 7 Percentage cover of 6 functional form groups of macroalgae and of column using threads (Sigurdsson et al. barnacles and unoccupied substratum in ice-scoured and non-scoured tide- 1976, De Blok & Tan-Maas 1977, Lane et pools and emergent rock in September 1993 and April, August and October 1994. Data were averaged across short and long term colonization quadrats al. 1985), their redistribution occurs either within a plot (12 per plot in September 1993 and April 1994, 9 per plot in by dislodgment and deposition by waves, August and October 1994) and across 3 plots within each combination of or by crawling (Paine 1974, Hunt 1997). In habitat and stratum. Cover of Mytilus spp. in the long term colonization a tagging study, Hunt (1997) found that quadrats was not included and percentage cover of macroalgae and barna- mussels larger than 5 mm SL usually cles in these quadrats was adjusted to total 100% moved <5 cm over 4 wk. Because we cleared a 10 cm border around our sam- tose macroalgae than non-scoured emergent rock and pling quadrats, it is unlikely that postlarval colonists tidepools. In ice-scoured habitats, the macrobenthic entered the quadrats by crawling. The size range of assemblage differed between years: there wa.s a colonizing mussels encompassed most of the size greater cover of thick leathery algae and barnacles on range of the mussel population at Cranberry Cove: ice-scoured emergent rock, and of coarsely branched -90 % of mussels are smaller than 5 mm and <5% are algae in ice-scoured tidepools, and consequently less larger than 20 mm (Hunt & Scheibling 1995, in press). unoccupied space in October 1994 than in September Since growth rates are low (20.4 mm mo-' for mussels 1993. >5 mm; Hunt 1997), the large size of many of the For the quadrats sampled for long term colonization, colonists indicates that they were several years old. we also estimated the cover of mussels. Percentage The distance of wave dispersal of large mussels is cover of mussels was less than 1 % after each of the unknown. However, even relatively small-scale dis- three 5 to 6 mo intervals, with the exception of ice- persal should increase the rate of recovery of mussel scoured tidepools after the third 5 to 6 mo interval (F = cover from small-scale disturbances and affect the 6 %). On average, percentage cover was less than 3 % dynamics of established mussel aggregations. At the after 11 mo in each combination of habitat and stratum. same field site, Hunt (1997) found that changes in mus- After 16 mo, percentage cover of mussels was < 1 % on sel patch size were affected more by dislodgment and non-scoured and ice-scoured emergent rock, 8% in redistribution of mussels by waves than by mussel non-scoured tidepools, and 17 "/;, in ice-scoured tide- mortality. 166 Mar Ecol Prog Ser 167: 155-169, 1998

Sampling at short intervals indicated that the colo- Although spatial distribution is known to vary among nization rate of mussels >2 mm SL peaked in June to some of the closely related species in the M. edulis spe- July in both 1993 and 1994. In contrast, settlement cies complex (e.g. M. edulis and M. galloprovincialis; occurred in August to October, similar to the pattern Skibinski et al. 1983, Gosllng & McGrath 1990), varia- observed by Pedersen (1991) at another wave-exposed tion in the distribution of M. trossulus and M. edulis shore -30 km from our site. The peak of colonization of probably did not contribute to the pattern we ob- large mussels in late spring and summer may be asso- served, since genetic analysis indicated that the fre- ciated with the low wave action at this time of year. In quency of occurrence of the 2 species did not differ June and July of both years, 2 m (unpubl. data, Department of variation in the macrobenthic assemblage. We ob- Fisheries and , Ottawa, Canada). In contrast, served mussel colonists on a variety of substrata, from September 1993 to May 1994, 11 to 45% of including filamentous algae (Cladophora sp., Spongo- records in each month were >2 m. Decreased wave morpha sp.), jointed calcareous alga (Corallina offici- action is associated with decreased attachment nalis), holdfasts of thick leathery macroalgae (Fucus strength of mussels to the substratum (Price 1980, vesiculosis, Chondrus crispus), pits and crevices in 1982, Witman & Suchanek 1984, Hunt 1997). Conse- rock covered by crustose algae (Phymatolithon sp., quently, during periods of low wave heights, the prob- Hildenbrandia rubra), and barnacle tests. In contrast, ability of a mussel's dislodgment by occasional large we rarely observed mussel colonists on smooth, other- waves may have been increased. wise unoccupied substrata. During the 17 mo period of The influence of colonization by mussels >2 mm is this study, the macrobenthic assemblage differed not usually considered in studies of the dynamics of among the habitatktratum combinations, and the per- mussel assemblages on hard substrata, although dis- centage cover of different macroalgal groups and bar- persal by smaller post-larval mussels is well known. nacles varied over time. Ice-scoured emergent rock, Detection of the movement of large mussels may the habitathtratum combination with the lowest abun- depend on the substratum used to monitor coloniza- dance of colonists, generally lacked filamentous and tion. Most studies of patterns of settlement or recruit- coarsely branched algae, substrata with which recently ment of musse1.s have monitored artificial substrata settled mussels are often associated (authors' pers. (usually filamentous) and have found no evidence of obs., see also Seed & Suchanek 1992, Hunt & Scheib- colonization by mussels >5 mm (e.g.De Rlok & Geelen ling 1996). Filamentous algae was abundant on ice- 1958, King et al. 1990, Caceres-Martinez et al. 1994). scoured emergent rock only in April 1.994 when the In contrast, Paine (1974) observed that large Mytilus short term colonization rate of mussels was negligible. californianus (>3 cm) colonized plots of the natural Ice-scoured emergent rock also had less crustose substratum which had been cleared of mussels. We macroalgae than the other habitathtratum combina- found that mussels that colonized natural substrata tions. In a previous paper, we investigated the factors were larger than those which colonized an artificial fil- influencing the pattern of mussel colonization among amentous substratum, suggesting that filamentous the habitathtratum combinations by comparing colo- substrata are more suitable for smaller than for larger nization rates on natural and artificial substrata (Hunt mussels (Hunt & Scheibling 1996). The high rates of & Scheibling 1996). In contrast to the natural substra- colonization by large mussels in our study compared to tum, colonization of artificial substrata was greatest on others also may result from differences between mus- ice-scoured emergent rock in direct relation to water sel species. Genetic analysis indicated that -70% of flux (Hunt & Scheibling 1996). The difference in colo- mussels at our study site were M. trossulns, while most nization pattern between artificial and natural sub- of the studies employing artificial substrata examined strata indicated that colonization of natural substrata is M. edulis or M. galloprovincialis. influenced by factors other than water flux, including varlation in the macrobenthic assemblage between habitats and strata (Hunt & Scheibling 1996). Patterns of colonization among habitats and strata Within combinations of habitat and stratum, the cumulative short term and long term abundance of Colonization by Mytilus, measured both at short (2 to colonists often varied among plots. Spatial variation in 7 d) and long (5 to 16 mo) sampling intervals, differed colonization at the scale of plots may result from varia- consistently among combinations of habitat and stra- tion in the supply of colonists due to differences in tidal tum. Mussel colonization was greatest in ice-scoured height and wave exposure, or from variation in the tidepools and lowest on ~ce-scouredemergent rock. macrobenthic assemblage. We also observed consider- Hunt & Scheibling: Variabilit.y of mussel colon~zationpatterns

able variability in the abundance of colonists among increase in the estimate of settlement in quadrats from quadrats within plots, most likely resulting from varla- which individuals have not been cleared is contrary to tion in the macrobenthic assemblage. the observations for barnacles (Connell 1985, Bertness The patterns of colonization on natural substrata cor- et al. 1992, Minchinton & Scheibling 1993a, b). How- respond to patterns of distribution and abundance of ever, barnacles require free space on the substratum mussels on ice-scoured but not on non-scoured regions for settlement, wheareas mussels generally settle on of the shore. Colonization rate of ice-scoured emergent filamentous or rough substrata, which can include the rock was low during all sampling intervals and mussels byssal threads of conspecifics. For example, Hunt are rare in these areas. In non-scoured areas, the spa- (1997) found a positive relationship between recruit- tial distribution and abundance of mussels differ be- ment rate of mussels to mussel patches and patch area. tween tidepools and emergent rock, but we did not The lack of a significant relationship between long detect a difference in colonization rate between the term and cumulative short term colonization for the 2 habitats. However, the small size and low percentage third 5 to 6 mo interval suggests that density-depen- cover of mussels after 16 mo (517%) suggests that dent post-colonization processes were more important differences in the mussel assemblage between the tide- during this interval, when cumulative short term colo- pools and emergent rock develop slowly. This is consis- nization was highest, than during the other 5 to 16 mo tent with studies of community recovery on wave- intervals. Post-colonization processes also influenced exposed shores on the Atlantic coast of Nova Scotia the size distributions of colonists. On ice-scoured after a large scale ice scour in 1987 (McCook & Chap- emergent rock (except in fall 1994), the size range of man 1997, Minchinton et al. 1997). On emergent rockin long term colonists was more limited than that of the mid intertidal zone, mussel cover was c20 % 14 mo colonists sampled at short intervals. This suggests that after the ice scour (McCook & Chapman 1997, Mlnchin- ice-scoured emergent rock is not a suitable substratum ton et al. 1997).The pattern of distribution and cover of for some sizes of mussels, particularly those 5mm) were slightly higher in tidepools than important than post-colonization processes in deter- on emergent rock over 5 mo intervals. The size distrib- mining the pattern of spatial distribution of mussels. In utions of long term coloilists also may be influenced by addition, the long term abundance of colonists was lin- an increased attractiveness of the substratum to set- early related to the cumulative short term abundance tling larvae due to the presence of conspecifics, as dis- during each interval except the third 5 to 6 mo interval. cussed above. With the exception of the 16 mo interval, there was Our study demonstrates the potential importance of approximately a l-to-l relationship between long term post-settlement dispersal in determining the distribu- and cumulative short term colonization, implying that tion and population dynamics of benthic marine inver- little post-colonization mortality or dispersal occurred tebrates which remain mobile for a period of time after during these intervals. The low percentage cover of settlement. We found that dispersing post-larval mus- mussels after each of the intervals indicates that there sels were considerably more abundant than settlers was probably little or no competition for space. How- and that mussels >2 mm represented a large propor- ever, some post-colonization mortality or dispersal may tion of colonists. Colonization by mussels >2 mm may have been offset by enhanced settlement in the pres- be overlooked in many studies of mussel colonization ence of conspecifics in the long term colonization because most researchers use a filamentous artificial quadrats. As evidence of this, the abundance of < 1 mm substratum, which may be more suitable for smaller mussels after the third 5 to 6 mo interval, immediately than for larger post-larval mussels. Our results indicate after a settlement peak in 1994, was greater than the that, over time scales up to 16 mo, patterns of Initial cumulative abundance based on short term sampling colonization by settlers and larger post-larval mussels over the same interval This disparity was not observed were more important than post-colonization mortality after the first 5 to 6 mo interval in 1993 when quadrats and dispersal in determining patterns of distribution were sampled a month after the settlement peak. This and abundance of mussels on thls shore. 168 Mar Ecol Prog Se

Acknowledgements. We thank Norman Countway, Allan lapillus (L.)) predation on mussel (~Vytilus trossulus Hennigar, Anna Metaxas, Kristina Sander, and Alyson Shaw (Gould), M edulis (L.))assemblages in tidepools and on for assistance in the field. We are also grateful to Sharlenc emergent rock on a wave-exposed rocky shore in Nova Anthony for counting samples and to Dr S. Walde for Scotia, Canada. J Exp Mar Biol Ecol comments on an earlier draft of this manuscript. H.L.H. was K~ngPA, McGrath D, Britton W (1990) The use of artificial supported by a Natural Science and Engineer~ngResearch substrates in monitoring mussel (iLlytilus eduljs L.) settle- Council (NSERC) Postgraduate Award and an lzaak Walton ment on an exposed rocky shore in the west of Ireland. 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Editorial responsrbility: Roger Hughes (Contributing Editor), Submitted: December 2, 1997; Accepted: March 18, 1998 Gwynedd, UK Proofs received from author[s): May 19, 1998