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Fish and Blue Crab Assemblages in the Shore Zone of Tidal Creeks in the Delaware Coastal Bays
Brian P. Boutin and Timothy E. Targett

Northeastern Naturalist, Volume 20, Issue 1 (2013): 69–90

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2013 NORTHEASTERN NATURALIST 20(1):69–90 Fish and Blue Crab Assemblages in the Shore Zone of Tidal Creeks in the Delaware Coastal Bays Brian P. Boutin1,2,* and Timothy E. Targett1 Abstract - Spatial and temporal dynamics of shore zone fish and Callinectes sapidus (Blue Crab) densities in tidal creeks of the Delaware Coastal Bays were examined during the spring/summer nursery period and in the winter of 2004, 2005, and early 2006 to identify underlying abiotic conditions driving the structure of species assemblages. Distinct spring/summer species assemblages were identified within separate tidal creeks, correlated with dissolved oxygen range. Differences were driven by the dominance of hypoxia-tolerant species in the intensely developed White Creek watershed and hypoxia-sensitive species in the less-developed Miller Creek watershed. In winter, species assemblages were somewhat homogenized and were less influenced by abiotic conditions. Results of this study indicate that the fish and Blue Crab assemblage in the shore zone of tidal creeks in the Delaware Coastal Bays is affected primarily by location-specific influences, such as anthropogenic alteration and associated hypoxia, particularly in the spring and summer. Introduction Coastal embayments and their tributaries provide important habitat for numerous economically and ecologically important fishes and invertebrates (Nixon 1982, Sogard and Able 1991, Szedlmayer and Able 1996, Yanez-Arancibia et al. 1994). Unlike river-dominated estuarine systems, coastal bays are generally well mixed with less dramatic environmental gradients (Kjerfve 1986, Kjerfve and Magill 1989, Mariani 2001). The physical and hydrodynamic features of coastal bays, as well as their interaction with tides and predominant patterns in wind speed and direction can therefore influence the structure of the associated faunal communities (Mariani 2001, Murphy and Secor 2006). Fishes that use coastal bay habitats can be classified into numerous groups that describe their level of residency in the system (Yanez-Arancibia et al. 1994, Whitfield 1999). Resident species remain in the coastal bay for their entire life cycle. Transient species use coastal bays as opportunistic foraging grounds, spawning areas, juvenile nurseries, and migration corridors (Day et al. 1989, Moyle and Cech 1982). Some transient species are facultative in their use of coastal lagoons, while others commonly described as estuary dependent use coastal bays as primary nursery habitats. The high productivity, abundant prey resources, suitable physicochemical conditions, and shallow nature of coastal bays provide fishes with favorable conditions for reproduction, growth, and refuge from predation (Nixon 1982, Yanez-Arancibia et al. 1994). 1University of Delaware, School of Marine Science and Policy, Lewes, DE 19958. 2Current address - The Nature Conservancy, 701 W Ocean Acres Drive, Kill Devil Hills, NC 27948. *Corresponding author - bboutin@tnc.org. 70 Northeastern Naturalist Vol. 20, No. 1 The coastal bays of Delaware, Maryland, and Virginia on the Delmarva Peninsula support numerous species of resident, estuary-dependent, and facultative transient fishes (Derickson and Price 1973; Love et al. 2009; Murphy and Secor 2006; Pacheco and Grant 1965; Richards and Castagna 1970; Schwartz 1961, 1964; Weston 1993). As in most temperate estuaries, the composition and abundance of the fish fauna of the Delmarva coastal bays is seasonally variable. Many estuary-dependent fishes, such as those in the families Sciaenidae and Clupeidae, utilize these bays as seasonal nursery grounds (Able and Fahay 2010, Wang and Kernehan 1979), occurring in greatest abundance during summer and early autumn (Cowan and Birdsong 1985, Derickson and Price 1973, Pacheco and Grant 1965, Weston 1993). The nekton assemblages in the Delmarva coastal bays have been found to differ spatially among individual embayments (Murphy and Secor 2006) with distributions within embayments influenced by variability of environmental factors such as salinity (Love et al. 2009). The Delaware Coastal Bays are the most anthropogenically impacted on the Delmarva Peninsula (Chaillou et al. 1996, DIBEP 1995, Maxted et al. 1997, Price 1998, Valdes-Murtha 1997). Since 1950, the population of Sussex County, DE, the county bordering the bays, has increased 221% (Delaware Population Consortium 2010, US Census Bureau 1995). Shoreline alteration and nutrient enrichment have contributed to the disappearance of Zostera marina L. (Eelgrass) and Ruppia maritima L. (Widgeongrass) and an increase of dense drift macroalgal communities dominated by Agardhiella tenera J. Ag. (Red Weed) and Ulva lactuca L. (Sea Lettuce) (DIBEP 1995, Maxted et al. 1997, Price 1998, Timmons and Price 1996, Tyler 2010, Weston 1993). Such changes to both physical and chemical environments often adversely affect the functional role of specific habitats for the faunal assemblages by altering food webs and species composition (Deegan 2002, Holland et al. 2004). These changes can result in a homogenization of species assemblages to those only tolerant of variable conditions (Maxted et al. 1997) as well as a loss of productive habitat for transient fauna that rely on such habitat as nursery grounds (Holland et al. 2004). A review of previous studies examining the shore-zone fish community in the Delaware Coastal Bays concluded that a shift in dominance had occurred since the 1950s, with a greater abundance of species in the Family Cyprinodontidae, which are more tolerant of low dissolved oxygen (DO), and lower abundances of estuary-dependent species (Chaillou et al. 1996, Price 1998). This shift was primarily attributed to recent nutrient enrichment in these bays. Although several studies have examined the fish and Callinectes sapidus Rathbun (Blue Crab) assemblage structure in the shore zone of the Delaware Coastal Bays (Clark 2002, Derickson and Price 1973, Pacheco and Grant 1965, Weston 1993), most did not link trends in assemblage structure to environmental variability, and all relied on measurements of relative abundance rather than quantitative measurements of density. This approach limits the usefulness of the data to identify habitat areas and/or conditions that promote productive, biodiverse faunal communities. Additionally, the most spatially and temporally comprehensive studies were conducted several decades ago, while more recent 2013 B.P. Boutin and T.E. Targett 71 studies consist mostly of limited temporal sampling at specific locations. The need for more extensive current data is highlighted by the fact that there has been a continued shift in the shore fish assemblage towards hypoxia-tolerant resident species since those early studies were conducted (Price 1998). The objective of the present study was to use quantitative sampling to examine spatial and temporal dynamics of the shore zone fish and the Blue Crab assemblage in tidal creeks of the Delaware Coastal Bays and attribute those dynamics to habitat-specific variations in temperature, salinity, and DO. Specifically, we compared differences in densities of fishes and Blue Crabs among sections of tidal creeks within different embayments across the spring/ summer nursery period and winter of two years. This comparison provided insight into spatial and seasonal differences in the density of individuals and assemblage structure and the underlying physicochemical characteristics that drive those changes. Field-Site Description Located in southeastern Delaware, the Delaware Coastal Bays consist of three interconnected embayments—Rehoboth Bay, Indian River Bay, and Little Assawoman Bay—and their associated tributaries and canals (Fig. 1). These shallow (average depth is 1.2 m), polyhaline to mesohaline systems have a combined water surface area of 83 km2 and are sheltered from substantial direct interaction with the Atlantic Ocean (DIBEP 1995, Martin et al. 1996, NOAA 1990). The northernmost bays are contiguous with the Atlantic Ocean at Indian River Inlet, while Little Assawoman Bay is connected with the ocean through Ocean City Inlet, MD. All bays are fringed by salt or brackish, tidally influenced marshes (Tiner 2001, Weston 1993) and have little freshwater inflow (Martin et al. 1996, Weston 1993). Indian River and Rehoboth bays have more extensive drift macroalgal communities than does Little Assawoman Bay (Price 1998; Timmons and Price 1996; Tyler 2005, 2010; Valdes-Murtha 1997). Sampling was conducted in White Creek (a tributary of Indian River Bay), Miller Creek (a tributary of Little Assawoman Bay), and Assawoman Canal (a man-made waterway connecting the two tributaries) (Fig. 1). Two stations were sampled in both tidal creeks, and four stations were sampled in Assawoman Canal (Fig. 1). Both White Creek stations were adjacent to substantial shoreline development and contained dense drift macroalgae. In contrast, the Miller Creek stations were bordered by conservation lands (Assawoman Wildlife Area) with salt marsh and sediment bank shorelines and generally contained no macroalgae. Habitat characteristics of Assawoman Canal varied between northern and southern stations. Northern Assawoman Canal stations (A1 and A2) were bordered by steeply sloping, high-bank shorelines and contained scattered deposits of large woody debris. In contrast, the southern stations (A3 and A4) were bordered by forested wetlands and fringing salt marsh with wood/leaf-litter detritus. All stations in Assawoman Canal were bordered by moderate upland development, and two of the stations (A2 and A4) were adjacent to bridges that traversed the canal. 72 Northeastern Naturalist Vol. 20, No. 1 Methods Fishes and Blue Crabs were collected in the shore zone with two standardized quarter-circle hauls of a 7.6-m seine net (1.2 m in height; 5-mm mesh), which resulted in a total area swept of 45.6 m2. Prior to the initiation of this study, it was determined that two swiftly replicated seine hauls sampled 95% of the fish and Blue Crab individuals residing in the area seined, with 70% collected in the first haul. Thus, two replicate seine hauls were employed at each station, and the contents were combined as one sample. Fish were identified to species, and numerical densities of each species and all species combined were calculated as the number of individuals per area swept. Sampling was conducted from May through September 2004 and April through September 2005 during the spring/summer nursery period and in December 2004, February Figure 1. Sampling stations in tidal creeks of the Delaware Coastal Bays. Numbers indicate individual stations in White Creek (W), Assawoman Canal (A), and Miller Creek (M). 2013 B.P. Boutin and T.E. Targett 73 and March 2005, and January 2006 during winter. All samples were collected during daylight hours between midmorning and midafternoon. Nursery period samples were collected weekly at the Assawoman Canal stations and biweekly at the Miller and White Creek stations in 2004 and weekly at all stations in 2005. Winter samples were collected once monthly at all stations. Infrequently, during both years, extremely high densities of drift macroalgae prevented sampling in White Creek. This build up of drift macroalgae occurred on one occasion in June 2004 at the W1 station and in May and June 2005 when both stations were sampled biweekly due to macroalgal densities. Temperature, salinity, and DO were recorded prior to sampling at each station. Surface salinity was measured using a temperature-compensated refractometer. Bottom temperature and DO were measured using an YSI 55 handheld DO meter. It should be noted that DO values taken at the time of sampling do not describe the dynamic diel (day-night) cycle of DO often seen in shallow estuarine tributaries (Tyler et al. 2009) and were treated as a relative indication of DO at a given site. Statistical analysis Species richness and total density of fish and Blue Crab individuals were compared among months using one-way ANOVA to examine temporal changes over the spring/summer nursery period into winter. Winter months were analyzed with spring/summer nursery period data from the preceding year (e.g., January 2006 analyzed with 2005 spring/summer nursery period months). Data were averaged across stations for each month. If significant differences were found, a Tukey’s HSD test was used for multiple comparisons. Fish and Blue Crab density data were log10 (x + 1) transformed to reduce heterogeneity of variances. All analyses were conducted using SYSTAT (Version 13.00.05). A significance level of α = 0.05 was used throughout. Fish and Blue Crab assemblage structure was analyzed using nonparametric multivariate statistics to relate seasonal and spatial trends to environmental characteristics. This approach allows for the identification of differences in the assemblage structure among groups of samples and the underlying drivers of those differences through construction of similarity matrices, application of group-average hierarchal cluster analysis and non-metric multidimensional scaling (NMDS) to identify groupings of stations, calculation of similarity percentages to identify species contributing most to the overall dissimilarity between defined groups, and correlating the observed pattern of species assemblages to environmental characteristics. All analyses were conducted using PRIMER (Version 5.2.4). All species composing less than 1% of the total catch at any station during each season were eliminated from the analysis. To identify spatial differences in the fish and Blue Crab assemblage structure within each season of each year, Bray-Curtis similarity matrices (Bray and Curtis 1957) were constructed from fourth-root transformed mean densities of each species at each station. Group-average hierarchal cluster analysis and NMDS based on the Bray-Curtis similarity matrices were performed to identify sample groups 74 Northeastern Naturalist Vol. 20, No. 1 with different assemblage structures. Cluster analysis was used to define levels of similarity that appeared to assemble samples into ecologically meaningful groups, while NMDS was used to illustrate these groupings in two dimensions. NMDS plots were considered adequate if stress coefficients, a measure of goodness of fit, were less than 0.2 (Clarke 1993). The species which contributed most to the observed groupings were then identified using a similarity percentages procedure (SIMPER; Clarke 1993). This procedure calculates each species’ contribution to the average Bray-Curtis dissimilarity between sample groups (δi), as well as its standard deviation (SD[δi]). Species with a high ratio of mean δi values to their respective SD(δi) are deemed important discriminating species. The influence of abiotic variables on observed groupings of species assemblages was examined using the BIOENV procedure (Clarke and Ainsworth 1993). Similarity matrices were constructed for station averages of temperature, salinity, DO, their respective ranges, and all combinations thereof using Euclidean distance of normalized values. Then Spearman’s rank correlations (ρ) were calculated between the species assemblage similarity matrices and all possible abiotic similarity matrices to identify the combination of abiotic variables which best explain the observed pattern of assemblages. Permutations tests were used to determine the significance of these correlations. Results Temperature was generally 1–2 °C higher at the White Creek and Miller Creek stations than at the Assawoman Canal stations in the spring/summer nursery period of 2004 and 2005 (Table 1). A slight salinity gradient was evident across stations, with higher mean values at White Creek stations closest to Indian River Inlet (Table 1). Salinities were higher in 2005 than in 2004, with the largest variability occurring at Assawoman Canal stations during both years. DO concentrations ranged from hypoxic to supersaturated conditions during both years (Table 1). Mean DO concentrations were generally higher at White Creek and Miller Creek stations than at those in Assawoman Canal. However, the lowest DO values were often recorded at White Creek and southern Assawoman Canal stations. Overall, White Creek and Miller Creek stations had greater mean temperatures and DO than Assawoman Canal stations, with White Creek stations exhibiting the greatest variability in DO, and Assawoman Canal stations exhibiting the greatest variability in salinity. Trends in abiotic characteristics during winter sampling were similar to those during the spring/summer nursery period. Temperature was generally 1 °C higher at the White Creek stations than at all other stations. Temperature averaged 7.2 °C in winter 2004/2005 and 8.3 °C in winter 2006 at the White Creek stations, while other stations averaged less than 6 °C in winter 2004/2005 and near 7 °C in winter 2006. A salinity gradient remained evident during winter of both years, with higher mean values at the White Creek stations (25.5 PSU in 2004/2005 and 27 PSU in 2006). However, unlike measurements during the spring/summer nursery period, DO values remained above 6 mg/L at all stations during each sampling event. 2013 B.P. Boutin and T.E. Targett 75 A total of 21,487 individuals of 32 species were collected during spring/ summer nursery period sampling in 2004 and 2005 (Table 2). The catch was dominated by Fundulus heteroclitus (Mummichog) (47.5% of total catch) and Menidia menidia (Atlantic Silverside) (29.7% of total catch). Other species such as Blue Crab (7%), Leiostomus xanthurus (Spot) (3.9%), and Cyprinodon variegatus (Sheepshead Minnow) (3.7%) were also abundant. During winter, only 135 individuals of six species were collected in the shore zone, with Sheepshead Minnow (64.4%) and Mummichog (25.2%) dominating the catch (Table 3). Species richness varied seasonally between the spring/summer nursery period and winter of each year (Fig. 2). Species richness was significantly higher in May than in September 2004 (F7,122 = 22.52, P < 0.01), indicating a slight decline during the spring/summer nursery period, and was significantly higher in all spring/summer nursery period months than in the following winter months (December 2004, February and March 2005). During the spring/ summer nursery period of 2005, species richness was significantly higher in June and July than all other months with the exception of August, indicating a mid-summer peak (F6,181 = 36.55, P < 0.001). This peak was primarily driven by later recruitment of transient species as compared to that in the spring/ Table 1. Station means (minimum-maximum range) for abiotic variables in tidal creeks of the Delaware Coastal Bays from the spring/summer nursery period in 2004 and 2005. Temperature (°C) Salinity (PSU) DO (mg/L) Creek/station 2004 2005 2004 2005 2004 2005 White Creek W1 26.1 25.8 22.0 27.8 7.2 7.5 (22.8–28.9) (15.7–34.6) (15.0–30.0) (20.0–32.0) (2.7–11.0) (2.4–20.0) W2 26.6 26.0 21.9 27.3 6.8 6.9 (24.2–29.3) (15.8–33.7) (14.0–30.0) (21.0–32.0) (3.3–10.1) (2.2–11.6) Assawoman Canal A1 25.3 24.6 20.5 25.4 5.3 5.9 (21.5–29.0 (13.7–32.2) (9.0–2.09) (18.0–32.0) (3.2–7.3) (3.0–9.5) A2 25.3 24.4 19.7 24.3 4.9 5.1 (21.8–28.8) (13.3–32.1) (11.0–28.0) (17.0–32.0) (3.1–7.3) (2.6–7.0) A3 24.6 22.8 13.3 15.5 3.9 3.7 (21.2–27.5) (13.1–29.8) (5.0–27.0) (0.0–31.0) (2.4–6.1) (1.1–9.2) A3 24.6 22.8 13.3 15.5 3.9 3.7 (21.2–27.5) (13.1–29.8) (5.0–27.0) (0.0–31.0) (2.4–6.1) (1.1–9.2) A4 25.3 24.2 13.6 19.0 5.1 4.1 (21.3–28.6) (12.9–33.5) (4.0–25.0) (5.0–30.0) (2.7–11.1) (2.2–6.3) Miller Creek M1 27.3 24.4 17.8 19.7 7.4 5.7 (23.5–31.6) (12.7–32.3) (10.0–25.0) (11.0–31.0) (6.6–8.5) (3.7–7.8) M2 27.7 24.9 13.9 17.6 7.6 5.5 (24.4–31.7) (13.3–32.9) (5.0–19.0) (9.0–28.0) (5.5–9.1) (3.8–7.5) 76 Northeastern Naturalist Vol. 20, No. 1 Table 2. Mean density (per m2), numerical abundance, and percentage of total catch for fish and Blue Crabs collected from the shore zone in tidal creeks of the Delaware Coastal Bays during the spring/summer nursery period in 2004 and 2005. Species are listed in descending order of percent contribution to the total shore zone catch. White Creek Assawoman Canal Miller Creek Total Species W1 W2 A1 A2 A3 A4 M1 M2 Number Percent Fundulus heteroclitus (L.) (Mummichog) 1.44 0.89 0.43 0.75 0.96 1.13 0.30 0.27 10,205 47.5 Menidia menidia (L.) (Atlantic Sivlerside) 0.25 0.29 0.64 0.36 0.27 0.91 0.52 0.45 6381 29.7 Callinectes sapidus Rathbun (Blue Crab) 0.13 0.29 0.07 0.14 0.08 0.08 0.11 0.08 1505 7.0 Leiostomus xanthurus Lacepède (Spot) 0.09 0.05 0.04 0.07 0.04 0.01 0.10 0.14 834 3.9 Cyprinodon variegatus Lacepède (Sheepshead Minnnow) 0.24 0.02 0.01 0.03 0.05 0.10 <0.01 0.01 797 3.7 Lucania parva (Baird and Girard) (Rainwater Killifish) 0.10 0.06 0.02 0.01 0.12 0.04 <0.01 <0.01 567 2.6 Fundulus majalis (Walbaum) (Striped Killifish) 0.19 0.05 0.01 0.05 0.01 0.01 0.03 0.03 519 2.4 Gobiosoma bosc (Lacepède) (Naked Goby) 0.01 0.05 0.01 0.03 0.02 <0.01 <0.01 <0.01 190 0.9 Pseudopleuronectes americanus (Walbaum) (Winter Flounder) 0.01 0.06 <0.01 0.01 157 0.7 Anchoa mitchilli (Cuvier and Valenciennes) (Bay Anchovy) <0.01 <0.01 0.01 0.01 <0.01 0.01 0.01 68 0.3 Fundulus diaphanus (Lesueur) (Banded Killifish) <0.01 0.01 0.03 <0.01 <0.01 66 0.3 Bairdiella chrysoura (Lacepède) (American Silver Perch) <0.01 0.02 <0.01 <0.01 <0.01 29 0.1 Brevoortia tyrannus (Latrobe) (Atlantic Menhaden) 0.02 <0.01 25 0.1 Alosa aestivalis (Mitchill) (Blueback Herring) 0.01 19 <0.1 Lepomis gibbosus (L.) (Pumpkinseed) <0.01 <0.01 <0.01 <0.01 <0.01 19 <0.1 Trinectes maculatus (Bloch and Schneider) (Hogchoker) <0.01 <0.01 <0.01 0.01 17 <0.1 Apeltes quadracus (Mitchill) (Fourspine Stickleback) <0.01 <0.01 <0.01 <0.01 13 <0.1 Pogonias cromis (L.) (Black Drum) 0.01 <0.01 <0.01 <0.01 13 <0.1 Alosa pseudoharengus (Wilson) (Alewife) <0.01 0.01 12 <0.1 Paralichthys dentatus (L.) (Summer Flounder) <0.01 <0.01 <0.01 <0.01 <0.01 <0.01 11 <0.1 Mugil cephalus L. (Flathead Mullet) <0.01 <0.01 <0.01 <0.01 10 <0.1 Opsanus tau (L.) (Oyster Toadfish) <0.01 <0.01 6 <0.1 Pomatomus saltatrix (L.) (Bluefish) <0.01 <0.01 <0.01 5 <0.1 Micropogonias undulatus (L.) (Atlantic Croaker) <0.01 <0.01 <0.01 <0.01 4 <0.1 Morone americana (Gmelin) (White Perch) <0.01 <0.01 4 <0.1 Syngnathus fuscus Storer (Northern Pipefish) <0.01 <0.01 4 <0.1 Hypsoblennius hentz (Lesueur) (Feather Blenny) <0.01 2 <0.1 Anguilla rostrata (Lesueur) (American Eel) <0.01 1 <0.1 Gobiesox strumosus Cope (Skilletfish) <0.01 1 <0.1 Micropterus salmoides (Lacepède) (Largemouth Bass) <0.01 1 <0.1 Morone saxatilis (Walbaum) (Striped Bass) <0.01 1 <0.1 Synodus foetens (L.) (Inshore Lizardfish) <0.01 1 <0.1 Total 21,487 100.0 2013 B.P. Boutin and T.E. Targett 77 Table 3. Mean density (per m2), numerical abundance, and percentage of total catch for fish and blue crabs collected from the shore zone in tidal creeks of the Delaware Coastal Bays during winter 2004/2005 and 2006. Species are listed in descending order of percent contribution to the total shore zone catch. White Creek Assawoman Canal Miller Creek Total Species W1 W2 A1 A2 A3 A4 M1 M2 # % Cyprinodon variegatus 0.10 0.10 0.08 0.01 0.19 87 64.4 Fundulus heteroclitus 0.15 0.01 0.07 0.01 34 25.2 Lucania parva 0.03 0.01 6 4.4 Fundulus majalis 0.02 0.02 0.01 5 3.7 Apeltes quadracus 0.02 2 1.5 Callinectes sapidus 0.01 1 0.8 Total 135 100.0 Figure 2. Monthly mean (a) species richness (± standard error) and (b) density of fishes and Blue Crab (per m2 ± standard error) collected in the shore zone of all stations in tidal creeks of the Delaware Coastal Bays during 2004, 2005, and 2006. 78 Northeastern Naturalist Vol. 20, No. 1 summer nursery period of 2004. In addition, species richness was significantly lower in winter (January 2006) than in all spring/summer nursery period months of 2005 with the exception of April. Total density followed similar seasonal patterns to that of species richness in each year (Fig. 2). Total density was significantly higher in May 2004 than all other spring/summer nursery period and winter months (F7,122 = 23.74, P < 0.001). Overall, total density showed a seasonal decline, with the lowest density in September 2004 and winter 2004/2005. During the spring/summer nursery period of 2005, total density of fish and Blue Crabs peaked slightly in June and was significantly higher than in May (F6,181 = 5.50, P < 0.05), with no significant differences found among other nursery period months. Total density in winter 2006 was significantly lower than all spring/summer nursery period months in 2005 with the exception of April and May. Cluster analysis and NMDS ordination of station-specific fish and Blue Crab density data indicated discrete spatial groupings of stations for each seasonal period in each year (Fig. 3). For the spring/summer nursery periods in 2004 and 2005, a similarity level of 80% partitioned the stations into biologically meaningful groups. In general, Miller Creek and White Creek assemblages differed from one another. In the spring/summer nursery period of 2004, Miller Creek stations were clearly differentiated from White Creek and Figure 3. Non-metric multidimensional scaling (NMDS) ordination of stations based on fourth-root transformed mean densities (per m2) of fishes and Blue Crab collected from the shore zone in tidal creeks of the Delaware Coastal Bays during (a) spring/summer 2004, (b) winter 2004/2005, (c) spring/summer 2005, and (d) winter 2006. Lines indicate groups of stations identified in group-average cluster analysis. 2013 B.P. Boutin and T.E. Targett 79 Assawoman Canal stations (Stress = 0.03; Fig. 3). Although close geographically, the southern Assawoman Canal station A4 and the Miller Creek stations (M1 and M2) were the most dissimilar. These two groups had a dissimilarity level of 24.4%, discriminated mostly by differing densities of Lucania parva (Rainwater Killifish) (18.1%), Sheepshead Minnow (17.2%), and Spot (13.2%) (Table 4). Spot were absent from the southern Assawoman Canal station A4, while Sheepshead Minnow densities were 20 times higher than that in Miller Creek. A combination of mean temperature, mean salinity, and DO range were found to best correlate with the observed pattern of species assemblages (ρ = 0.59), and this correlation was significant (P < 0.05). In the spring/summer nursery period of 2005, Miller Creek and White Creek stations again differed from one another (Stress = 0.09; Fig. 3). However, unlike 2004, Miller Creek stations grouped with the northern Assawoman Canal stations (A1 and A2). The species assemblages of the White Creek stations (W1 and W2) and the grouped Miller Creek/northern Assawoman Canal stations were the most dissimilar with a dissimilarity level of 25.8%. Species most responsible for the dissimilarity between these two groups of stations were Rainwater Killifish (12.7 %) and Bairdiella chrysoura (Silver Perch) (10.9 %), which had densities 10 times higher at the White Creek stations, and Pseudopleuronectes americanus (Winter Flounder) (10.8%), which were only collected at the Miller Creek/northern Assawoman Canal stations (Table 4). A combination of DO and DO range were significant correlates of the observed pattern of species assemblages during this period (ρ = 0.56, P < 0.05). During the winters following nursery-period collections, a consistent pattern of spatial partitioning of species assemblages was less clear (Fig. 3). A similarity level of 40% clustered stations into biologically meaningful groups for both years. In winter 2004/2005, the Miller Creek station M1 and White Creek station W2 contained different assemblages from all other stations where individuals were collected (no individuals were collected at A1 or W1) (Stress = 0.01; Fig. 3). These two stations were also the most dissimilar due to the absence of Mummichog, Rainwater Killifish, and Apeltes quadracus (Fourspine Stickleback) at the Miller Creek station M1 (Table 4). A combination of DO and DO range were significant correlates of the observed pattern of species assemblages during this period (ρ = 0.56, P < 0.05). In winter 2006, the typical segregation of Miller Creek and White Creek stations seen during the other seasons broke down, with station M1 clustering with station W1 (Stress = 0.01; Fig. 3). This grouping was the most dissimilar from the northern Assawoman Canal station A1, as Fundulus majalis (Striped Killifish) and Sheepshead Minnow were absent from collections at that station (Table 4). No environmental data were significant correlates to the observed pattern of species assemblages. Discussion The fish and Blue Crab assemblage structure in the shore zone of the tidal creeks sampled in the present study was generally similar to that reported 80 Northeastern Naturalist Vol. 20, No. 1 Table 4. Mean density (per m2), ratio of mean dissimilarity to standard deviation [δi/SD(δi)] and percent contribution of discriminating species to the mean dissimilarity between groups of stations identified by cluster analysis and NMDS ordination during the spring/summer nursery period in 2004 and 2005, and the following winters using SIMPER analysis. Mean density Year Season Mean dissimilarity Group 1 Group 2 δi/SD(δi) Percent 2004 Spring/summer A1, A2, A3, W1, W2 vs. A4 = 20.4 A1, A2, A3, W1, W2 A4 Leiostomus xanthurus 0.033 12.73 22.0 Fundulus majalis 0.120 0.001 1.90 17.2 Anchoa mitchilli <0.001 0.005 2.82 12.1 A1, A2, A3, W1, W2 vs. M1, M2 = 23.2 A1, A2, A3, W1, W2 M1, M2 Anchoa mitchilli <0.001 0.029 4.66 18.8 Lucania parva 0.046 0.001 1.71 15.6 Gobiosoma bosc 0.010 1.64 12.2 A4 vs. M1, M2 = 24.4 A4 M1, M2 Lucania parva 0.048 0.001 2.25 18.1 Cyprinodon variegatus 0.165 0.008 14.58 17.2 Leiostomus xanthurus 0.005 29.17 13.2 2005 Winter A1, A3, A4, M2 vs. M1 = 91.7 A1, A3, A4, M2 M1 Cyprinodon variegatus 0.110 3.95 52.8 Fundulus majalis 0.004 0.011 1.55 25.2 Fundulus heteroclitus 0.004 0.81 11.0 A1, A3, A4, M2 vs. W2 = 83.0 A1, A3, A4, M2 W2 Cyprinodon variegatus 0.110 8.21 28.9 Fundulus heteroclitus 0.004 0.219 2.38 27.2 Apeltes quadracus 0.022 6.33 19.0 M1 vs. W2 = 100.0 M1 W2 Fundulus heteroclitus 0.219 N/A 37.0 Lucania parva 0.044 N/A 24.7 Apeltes quadracus 0.022 N/A 20.8 2013 B.P. Boutin and T.E. Targett 81 Table 4, continued. Mean density Year Season Mean dissimilarity Group 1 Group 2 δi/SD(δi) Percent 2005 Spring/summer A1, A2, M1, M2 vs. A3, A4 = 23.1 A1, A2, M1, M2 A3, A4 Lucania parva 0.008 0.079 1.40 13.5 Pseudopleuronectes americanus 0.008 4.22 13.2 Fundulus heteroclitus 0.287 0.804 2.03 11.3 A1, A2, M1, M2 vs. W1, W2 = 25.8 A1, A2, M1, M2 W1, W2 Lucania parva 0.008 0.096 1.80 12.7 Bairdiella chrysoura <0.001 0.012 2.67 10.9 Pseudopleuronectes americanus 0.008 4.12 10.8 A3, A4 vs. W1, W2 = 22.8 A3, A4 W1, W2 Fundulus diaphanus 0.024 2.70 15.5 Bairdiella chrysoura < 0.001 0.012 1.89 10.3 Cyprinodon variegatus 0.030 0.127 2.34 9.7 2006 Winter A1 vs. A3, A4, M2 = 85.0 A1 A3, A4, M2 Cyprinodon variegatus 0.102 3.77 52.9 Fundulus heteroclitus 0.022 0.080 2.61 35.3 Lucania parva 0.011 0.58 11.8 A1 vs. M1, W1 = 100.0 A1 M1, W1 Fundulus heteroclitus 0.022 3.54 41.7 Fundulus majalis 0.022 3.54 41.7 Cyprinodon variegatus 0.011 0.71 16.7 A3, A4, M2 vs. M1, W1 = 76.4 A3, A4, M2 M1, W1 Cyprinodon variegatus 0.102 0.011 1.35 36.2 Fundulus majalis 0.022 3.37 36.0 Fundulus heteroclitus 0.080 0.64 16.2 82 Northeastern Naturalist Vol. 20, No. 1 from other estuarine creeks along the east coast of the United States (Able et al. 2007, Derickson and Price 1973, Rountree and Able 1992, Wagner 1999, Weinstein 1979). Mummichogs and Atlantic Silversides, which were dominant components of the spring/summer nursery period shore-zone assemblage, are also principal species in the shore zone of Delaware Bay (de Sylva et al. 1962) and the Rehoboth and Indian River bays (Derickson and Price 1973, Price 1998). Rountree and Able (1992) found that these two species were the two most abundant fish species captured during spring, summer, and autumn in the shore zone and adjacent subtidal regions of polyhaline tidal creeks in Great Bay - Little Egg Harbor, NJ. Both species use this habitat for foraging, refuge, and spawning (Able et al. 2003, Conover and Ross 1982, Raichel et al. 2003, Richards and Castagna 1970, Shenker and Dean 1979, Wang and Kernehan 1979). However, during winter collections in the present study, Atlantic Silverside were absent while Sheepshead Minnow and Mummichog constituted the dominate species collected. This discrepancy between seasonal dominants can be attributed to both the emigration of Atlantic Silverside out of the shore zone (Conover and Murawski 1982, Nixon and Oviatt 1973) and the tolerance of resident fishes like those in the family Cyprinodontidae to fluctuating winter temperatures (Able et al. 1996). In addition to the dominant fishes, Blue Crab was also abundant in the present study, particularly in the spring/summer nursery period. Blue Crabs use the shores zone of estuarine creeks as juvenile nursery areas and adult habitat (Orth and van Montfrans 1987, Rountree and Able 1992, Sogard and Able 1991, Weinstein 1979, Wilson et al. 1990). Blue Crabs, most of which were juveniles, were more abundant in White Creek (W1 and W2) than at other locations, similar to findings from associated sampling in subtidal areas with a 1-m beam trawl (Boutin 2008). These stations were characterized by dense drift macroalgae along the shoreline. Several studies have noted the importance of macroalgae as nursery habitat for juvenile Blue Crabs (Epifanio et al. 2003, Sogard and Able 1991). In contrast to the similarities noted with other shore-zone studies, the fish and Blue Crab assemblage structure in the shore zone of the tidal creeks sampled in the present study was quite different than that reported for deeper, subtidal areas in other Delmarva coastal bays. Bay Anchovy constitutes one of the most abundant species in the subtidal zone of the Maryland and Delaware coastal bays (Clark 2004, 2005; Murphy and Secor 2006; Tyler 2005), and was generally absent from shore-zone collections. During a similar sampling period as the present study, Clark (2004, 2005) found that Spot and Cynoscion regalis (Bloch and Schneider) (Weakfish) were the dominant species in the deep subtidal zone of tidal tributaries in Indian River and Rehoboth bays, including White Creek. These species were rare or absent from our shorezone collections. Furthermore, with the exception of Blue Crab, dominant shore-zone nekton, including Mummichog and Atlantic Silverside, were generally absent from accompanying subtidal sampling done during the present study (Boutin 2008) and from other areas of the Maryland and Delaware 2013 B.P. Boutin and T.E. Targett 83 coastal bays (Clark 2004, 2005; Murphy and Secor 2006; Tyler 2005). These differences may be attributed to the selectivity of the gear type used in the present study (i.e., seine), biasing the sample towards less mobile resident species very close to the shoreline. Seine length and design have been shown to impact estimates of density and community structure (Steele et al. 2006). Murphy (2005) found that, while most species were encountered during both seine and trawl collections in the Maryland Coastal Bays, species dominance was different depending on the gear type used, with generally more littoral fauna collected in seines. Species richness and total fish and Blue Crab exhibited distinct annual trends during the spring/summer nursery period in 2004 and 2005. In 2004, both metrics declined throughout the nursery period. Although studies in shorezone and subtidal areas of New England (Nixon and Oviatt 1973), New Jersey (Rountree and Able 1992), and Virginia (Weinstein and Brooks 1983) have reported spring peaks in catch-per-unit-effort, all have indicated a secondary, sometimes larger peak in catch in late summer or early autumn. The absence of such a secondary peak in 2004 was due to the lack of an influx of species, such as Atlantic Silverside, Bay Anchovy, and Blue Crab, reported in the previous studies. It should be noted, however, several of these studies included both shore-zone and subtidal areas in their assessments of seasonal peaks. In 2005, there was a peak in species richness and a small peak in total fish and Blue Crab density in summer. Murphy and Secor (2006) found a similar pattern in the subtidal zone of the Maryland Coastal Bays; species richness peaked in early summer during most years sampled. However, studies in New Jersey (Able et al. 2001, Szedlmayer and Able 1996) and Virginia (Weinstein and Brooks 1983) reported peaks of species richness in late summer and early autumn. The summer peak in density in the present study, due to high abundances of Mummichog and Atlantic Silverside, is similar to what was found in the shore zone of the Rehoboth and Indian River bays by Derickson and Price (1973), although the peak in the present study was much smaller. Such within-season fluctuations in species richness and total density can be attributed to annual spawning cycles and emigration/immigration patterns, as well as seasonal changes in abiotic habitat conditions (Able et al. 2001, Cowan and Birdsong 1985, Nixon and Oviatt 1973, Rountree and Able 1992, Szedlmayer and Able 1996). Additionally, year-to-year fluctuations in these metrics are directly influenced by year-class strength of dominant species, such as Bay Anchovy, which regularly exhibit poor year classes in the Delaware Coastal Bays (R. Kernehan, Center for the Inland Bays, Rehoboth Beach, DE, pers. comm.). Winter collections indicated a distinct reduction in species richness and density compared to those during the spring/summer nursery period. Few individuals were captured, with Sheepshead Minnows and Mummichogs, estuarine residents, dominating the catch. Numerous authors have documented a seasonal decline in species richness and density in estuaries along the east coast of the United States (Derickson and Price 1973, Nixon and Oviatt 1973, Rountree and Able 1992, Szedlmayer and Able 1996). Derickson and Price (1973) found similar patterns 84 Northeastern Naturalist Vol. 20, No. 1 of decline during sampling in the Rehoboth and Indian River bays. These declines have been attributed to emigration of transient fauna related to declining temperatures and food sources (Able et al. 1996, Nixon and Oviatt 1973, Szedlmayer and Able 1996). Additionally, resident fauna that utilize the shore zone, including Mummichog, move to refugia during winter (Smith and Able 1994), further declining densities and/or richness in the shore zone. However, it must be noted that sampling effort was less in the winter, which may have resulted in missed species or individuals. During the spring/summer nursery period in both 2004 and 2005, assemblage structure differed between tidal creek stations bordering different embayments (i.e., Miller Creek bordering Little Assawoman Bay versus White Creek bordering Indian River Bay). These differences appeared to be driven, at least in part, by the DO range at each tidal creek. While other abiotic factors such as mean temperature, mean salinity, and mean DO were also identified as significant correlates to the observed assemblages, only DO range was consistent from year-to-year. Large fluctuations in DO in shallow estuarine environments are often the result of photosynthesis and respiration cycles of phytoplankton and macroalgae (D’Avanzo and Kremer 1994, Tyler et al. 2009) and can be an indication of anthropogenic eutrophication. Anthropogenic influence across the study location generally decreased latitudinally from higher in White Creek (intensive shoreline development and stabilization) to lower in Miller Creek (bordered by Assawoman Wildlife Area). Development-induced nutrient loading can significantly affect the types of fish present in a water body (Caddy 2000, Murphy and Secor 2006, Price1998). A review of previous studies by Price (1998) indicated increased nutrient loading, particularly in the northern Delaware Coastal Bays, has shifted the dominant shoreline species from transient species including Spot and Atlantic Silverside to more hypoxia-tolerant resident species, such as Mummichog. This trend was apparent when comparing the shore-zone assemblage structure at stations in White Creek with those in Miller Creek. The White Creek shore-zone assemblage was dominated by Mummichog, whereas the assemblage in Miller Creek contained a higher proportion of hypoxiasensitive species, including Atlantic Silverside (Smith and Able 2003), which dominated there. White Creek stations were characterized by dense drift macroalgae, which can cause frequent hypoxic (<2.0 mg/L O2) to anoxic (<0.2 mg/L O2) conditions (D’Avanzo and Kremer 1994). The dominance of hypoxia- tolerant resident species and general absence of facultative transient and estuary-dependent species in White Creek indicates that macroalgae-induced fluctuations in DO may be creating suboptimal conditions in this creek for nursery use. While abiotic factors such as DO range appeared to be influencing the structuring of distinct assemblages in the spring/summer nursery period, trends were somewhat less clear for winter collections. Only in winter 2004/2005 were abiotic factors found to be significant correlates to the fish 2013 B.P. Boutin and T.E. Targett 85 and Blue Crab assemblage structure, where DO range was again found to be a driver. The absence of a consistent annual wintertime abiotic driver is not surprising as hypoxia, which would cause a large DO range, occurs primarily in spring and summer (Welsh and Eller 1991). This lack of winter hypoxia was apparent during both years, as DO was regularly above 6 mg/L. Additionally, sampling effort in the winter was much less than that in the spring/summer nursery period. More intensive sampling during winter months may lead to more firm conclusions as to the relationship between the fish and Blue Crab assemblage structure and abiotic conditions. Presence and type of structured habitats can also influence species composition and assemblage structure. Szedlmayer and Able (1996) found that the structural heterogeneity of subtidal bottom habitats in a New Jersey estuary affected habitat-use patterns and species composition of fish and macroinvertebrates. In the present study, each tidal creek differed in terms of the dominant bottom type and the presence/absence of structured habitats. Several species appeared to be associated primarily with locations containing structure. For example, Rainwater Killifish densities were highest at stations containing macroalgae (W1 and W2) or woody debris/leaf litter (A3 and A4). Other species, such as the Sheepshead Minnow, followed a similar trend. Thus, such small-scale changes in bottom type have the potential to affect assemblage structure of shore-zone fishes and blue crabs. Numerous authors have suggested the importance of abiotic conditions in structuring faunal assemblages in coastal embayments (Able et al. 2001, Love et al. 2009, Murphy and Secor 2006, Szedlmayer and Able 1996). While salinity is often identified as a major driver in the structuring of assemblages (Able et al. 2001, Love et al. 2009), it did not appear to play a major role in the present study, although a slight salinity gradient was evident across sampling stations. The range of DO at a particular grouping of stations and, more specifically, the incidence of hypoxia was found to consistently correlate with assemblage structures. Tidal creek stations characterized by highly fluctuating DO, such as those in White Creek, were dominated by resident species (e.g., Mummichog), which are particularly tolerant of anthropogenic impacts such as eutrophication and low DO (Price 1998, Stierhof f et al. 2003). These stations generally lacked high densities of facultative transient and estuary-dependent fauna, while those stations more stable in DO (e.g., Miller Creek) contained these species. Tidal creeks are intimately connected to adjacent marsh and upland systems, and thus, alterations to the natural watershed can have significant impacts to the nursery function of these habitats. It appears that the localized shore-zone fish and Blue Crab assemblage in tidal creek systems in the Delaware Coastal Bays, and perhaps other coastal systems (Bilkovic 2011, Partyka and Peterson 2008), is affected primarily by creek watershed influences, such as anthropogenic impacts, and degradation of these habitats may significantly alter the functionality of these areas as nurseries. 86 Northeastern Naturalist Vol. 20, No. 1 Acknowledgments We thank the individuals who provided field assistance for this project. We especially thank M. Rhode, S. Baker, K.L. Miller, D. Tuzzollino, and B. Ciotti. R. Kernehan and J. Clark provided helpful comments on the manuscript. This research was supported by grants to T.E. Targett from the Delaware Department of Natural Resources and Environmental Control (DNREC), Division of Fish and Wildlife, and the US Fish and Wildlife Service, Federal Aid in Sport Fish Restoration, Wallop-Breaux fund (Project F-56-R-10), through Delaware DNREC. 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