4.0.  Benthic Community Patterns in the Lower
Cape Fear River System
 

Martin Posey and Troy Alphin
Benthic Ecology Laboratory
University of North Carolina at Wilmington

 

 

4.1 Summary

 

4.2 Background

        Benthic organisms (benthos) are those organisms living in or on the bottom. In estuarine systems, the benthic community is dominated primarily by species that burrow into the sediments (infauna), often living within tubes or burrow systems. Taxa dominating the infauna in most estuaries include small worms (polychaetes and oligochaetes), amphipod crustaceans, clams, and insect larvae, with actual dominance changing based on region of the estuary and salinities. Benthos may also include larger animals such as rock crabs and blue crabs. Many benthic animals consume detrital or planktonic food, although some species are predatory, and are in turn prey for larger fish, shrimp and crabs.  In many estuarine systems there is a strong link between timing of fish recruitment and their benthic prey, indicating that this group is a crucial link in these food webs.

        Benthic fauna are considered important indicators of general water quality conditions. They are used in a variety of monitoring programs to assess overall estuarine health and to follow long-term trends in estuarine communities, especially related to anthropogenic impacts (Boesch et al. 1976, Aschan and Skullerod 1990, Simboura et al. 1995, Hyland et al. 1996). From a monitoring perspective, benthos offer 3 positive features: 1) they are relatively sedentary and long-lived, 2) they occupy an important intermediate trophic position, and 3) they respond differentially to varying environmental conditions. After settlement, most benthos remain within a relatively constrained area, often less than 5 m2, for their entire adult lives. Therefore, unlike many other biotic or chemical measures, benthos reflect conditions at a specific location. Although a few opportunistic species may live for only a few weeks, most benthic animals have life spans ranging from months to over a year, leading to a community structure that reflects average physical conditions over a time period of months. However, benthos vary greatly in their responses to changes in physical conditions, such as water quality. Some taxa are relatively tolerant of organic enrichment and low dissolved oxygen while others are quickly eliminated under low DO conditions (Boesch et al. 1976, Simboura et al. 1995). Increased nutrient inputs can strongly affect abundances of some species, through indirect and direct influences on food availability and sediment conditions, while not affecting others. Similarly, there is a wide variation in tolerance to pesticides and metal contaminants such as mercury and cadmium. In general, sediment type (clays, silts, sands, etc.), organic content, deposition rates of sediments (from upstream erosion), dissolved oxygen, salinity and temperature are considered most important in determining abundances and types of animals in bottom communities. By examining shifts in the benthic community over time (years), one can gain an understanding of the major environmental processes affecting the local biota (Hyland et al. 1996).

        A variety of indices have been developed to quantify the health of estuarine systems based on the relative proportions of species tolerant or susceptible to specific water quality parameters (e.g.; EPA Benthic Index; Ampelisca toxicity tests; suspension feeder : deposit feeder ratios; deep burrower : shallow burrower ratios; the Chandler Score, and the BMWP Score Index) (Whitehurst and Lindsey 1990). However, application of most indices requires long-term monitoring sufficient in duration to separate seasonal or annual variations from variations due to changes in water quality. Benthic community studies are a major component of the national EPA Environmental Monitoring and Assessment Program for estuaries as well as regional monitoring efforts, such as in Chesapeake Bay, Florida Bay, Long Island Sound, Pamlico Sound, and Tampa Bay.

        In spring 1996, the Benthic Ecology Laboratory of the UNCW Center for Marine Science Research began long-term studies of benthic infauna in the Cape Fear River as part of the basic monitoring plan of the Cape Fear River Program. Preliminary samples were also taken during winter 1996 as part of other research efforts. The benthic monitoring component has four major long-term objectives: 1) characterize the benthic communities in the lower Cape Fear River and compare them with that of other river-dominated estuaries to gain a first-order assessment of estuarine health, 2) determine seasonal, annual and spatial patterns of variability, 3) correlate benthic abundances and physical measures over short and long time periods, and 4) establish a baseline for detecting changes in the estuarine community through examination of changes in abundances of specific indicator taxa and eventual application of standard benthic indices.

        In the 2001-2002 annual report, we continue to present data from our long-term monitoring of patterns in benthic community composition, abundance of benthic organisms, benthic species diversity, and numbers of species (richness). We also present information on juvenile blue crab abundances within the lower Cape Fear estuary. Sampling of juvenile blue crabs has been conducted at 4-6 sites in the lower estuary since spring 1998, initially funded by North Carolina Sea Grant (grant #R/MRD-40) and funded since 1999 by the National Science Foundation (grant #9978613). While not funded by the Lower Cape Fear River Program, we present our juvenile blue crab data here because of its relevance to an important fishery and key species in southeastern North Carolina.

 

4.3 Methodology

        Four stations are sampled as part of basic monitoring for benthic infauna: NCF6 in the Northeast Cape Fear River, NAV in the mainstem Cape Fear River, and M54 and M31 in the lower estuary. These stations span the oligohaline to mesohaline/polyhaline zones of the estuary and correspond to stations sampled as part of water quality monitoring. Complete descriptions of these stations are given in previous Cape Fear River reports. The basic monitoring of benthos involves quarterly sampling at each station. Samples are collected in winter (January-February), spring (mid March-May), summer (July-early September), and fall (October-November). Following hurricanes Bertha and Fran in late summer 1996 and Hurricane Bonnie in September 1998, additional samples were also taken to observe recovery patterns (September 1996, October 1996, December 1996, February 1997, September 1998 and November 1998). This additional sampling was supported by the Benthic Ecology Laboratory. Post-hurricane samples collected on 1 October 1996 were only taken from stations M54 and M31 because of debris at the other 2 stations. During 1998, samples were collected in January, April/May, August, September (to examine effects of Hurricane Bonnie), and October/November. Confirmation of identifications for the summer and fall 2001 samples is ongoing and the results from the 2001 sampling will not be reported until all identifications have been completed, confirmed, and QA/QC completed (data will be presented in the next annual monitoring report).

        At each sampling station, benthic infaunal samples are taken with a Petite Ponar grab, 15cm x 15cm opening (0.023m2) and 15cm depth. Five grab samples were taken at each sampling location on each sampling date. Grabs were retained only if the grab was full in order to standardize volume sampled. Grab samples are taken from a boat at stations specified by GPS coordinates and all sampling locations are in approximately 6-8 feet of water (studies in other estuaries have indicated greater abundances in shallow areas as compared to deep channels within an estuary). Immediately after collection, the samples were sieved through a 0.5 mm mesh screen, preserved in 10% buffered formalin with rose bengal dye added, and transferred to 70% ethanol after 3 days for later sorting and identification. Separation of animals from remaining sediment is done under a dissecting microscope. All animals were identified to the lowest reliable taxonomic level, with random specimens verified by outside taxonomists. These procedures follow standard formats for benthic sampling outlined by the EPA Environmental Monitoring and Assessment Program and used in other monitoring programs (Hyland et al. 1996, Posey et al. 1997).

        For the purposes of this report, we have defined dominant taxa as any taxa that comprises greater than 3% of the individuals collected at a given site on a specific date. Most species collected in this monitoring effort were represented by relatively few individuals and are thus unlikely to be important to food web dynamics in the Cape Fear system. Diversity is calculated using the standard Shannon Weiner formula (diversity [H’] = S pi(logpi)) and includes all taxa collected. Species richness is calculated as the total number of species collected at a location over a specified time period. We calculated both diversity and species richness on a per sample basis to compare long-term trends among years because of some variability in sampling effort between hurricane and non-hurricane years. In both cases they represent the average number of species or average diversity per grab sample at a site during a season’s sampling. We used principal components analysis to identify distinct groupings of samples based upon site, year or season. This method allows us to reduce a complicated data set (262 taxa X 6 years X 4 seasons X 4 sampling locations) into a more easily interpretable graphic form. 

        As part of a larger study on blue crab biology, juvenile blue crab abundances have been variously monitored at 8 locations within the Cape Fear estuary since spring 1998. Here we report on abundances at 6 sites with the most continual collection history. These include 3 sites at Southport, one along the waterway near the Southport Marina (SPWW), one near an old canning plant along the main river shoreline between downtown Southport and the Bald Head Island Freight Ferry terminal (SPFC), and the third along the shore within the Southport Marina (SPMA). Two sites are located in the mid river area, one near Carolina Beach State Park (CBSP), along the river shoreline to the south of the marina entrance, and the other along the shore of a dredge spoil island immediately west of Carolina Beach State Park (CFCM). Our 2 upper stations were located near M51, one along the eastern shore where the powerlines cross the river (POWL) and the other along the shore of a dredge spoil island west of that location (CFPM). Abundances of juvenile blue crabs were monitored using standard net sampling approaches (seines and sweep nets) and more recently suction sampling. Ten replicate samples were collected at each site on a bimonthly basis from spring 1998 to summer 1999 and monthly from summer 1999 to the present. This effort is part of a larger study that has examined larval blue crab recruitment, blue crab growth, blue crab prey availability, predators on blue crabs and aspects of blue crab physiology in both the Cape Fear and New Rivers.

 

4.4 Results and Discussion

        A total of 262 taxa have been collected since winter 1996. In general, less than half of the species were collected at any single site and most species are relatively rare. Below we summarize major physical characteristics as they may affect benthos, general patterns of species dominance, diversity and species richness, and patterns of juvenile blue crab distribution and abundance.

 

4.4a. Site descriptions

        Physical conditions at all 4 sites were described in Mallin et al. (1999, 2000) and additional water quality data is provided in the current report. General site characteristics that are important for interpreting benthic community dynamics are summarized here.

        NCF6 is located in the Northeast Cape Fear River. This site is characterized by low salinity and fine sediments. Salinity for the months in which benthos were sampled averaged 1.8 o/oo, with lower salinity during winter months (0.7 o/oo) and higher salinity during summer (5.5 o/oo) and towards the end of 2000 (related to the start of drought conditions). Water temperature ranged from 5.9 oC to 28.3 oC. Dissolved oxygen varied seasonally, with a winter average of 8.8 and a summer average of 3.7. DO exhibited severe declines immediately after the passage of Hurricanes Fran (September 1996) and Bonnie (September 1998) though less so after Hurricane Floyd (September 1999) (Mallin et al. 1998, 1999, 2000). Sediments are fine sands to sandy silts, with macrodetritus present on some sampling dates.

        NAV is located in the mainstem Cape Fear River. Like NCF6, this site is characterized by low salinity and fine sediments. Salinity for the months in which benthos was sampled averaged 1.2 o/oo, with lower salinity during winter months (0.3 o/oo) and higher during summer (4.0 o/oo), though salinities increased towards the end of 2000. Water temperature ranged from 4.2 oC to 28.3 oC. Dissolved oxygen varied seasonally, with a winter average of 9.2 and a summer average of 3.9. DO exhibited declines immediately after the passage of Hurricanes Fran and Bonnie (Malin et al. 1999).

        M54 is located in the mainstem Cape Fear River below the confluence of the Cape Fear and Northeast Cape Fear rivers. It is characterized by higher but more variable salinities than NCF6 and NAV sites. Salinity for the months in which benthos was sampled averaged 5.2 o/oo but ranged from 0 to >20 o/oo. Salinity was lower during winter months (3.4 o/oo) and higher during summer (11.9 o/oo). Water temperature ranged from 8.4 oC to 28.2 oC. Dissolved oxygen varied seasonally, with a winter average of 8.9 and a summer average of 4.8 for the months sampled. DO exhibited severe declines immediately after the passage of Hurricanes Fran and Bonnie. Sediments are fine sands with a layer of flocculent detritus sometimes present over the surface.

        M31 is located in the Cape Fear estuary and is the furthest downstream site sampled as part of the basic monitoring program. It is characterized by higher salinities than any of the other sites. Salinity for the months in which benthos was sampled averaged 10.8 o/oo, ranging from 0.1 (immediately after Hurricane Bonnie) to >24 o/oo. As with other stations, salinity was lower during winter months (8.9 o/oo) and higher during summer (18.5 o/oo). Water temperature ranged from 6.8 oC to 28.6 oC. Dissolved oxygen varied seasonally, with a winter average of 9.3 and a summer average of 5.0. DO exhibited a decline immediately after the passage of Hurricane Bonnie, but less so after Hurricane Fran (Mallin et al. 1988, 1999). Sediments are predominantly fine sands, with a flocculent layer overlying the substrate surface containing larger detritus.

 

4.4b Community Patterns

        A total of 262 taxa have been collected from the 4 permanent benthic infaunal sampling stations (Tables 4.1-4.5), however only 12 new taxa (all rare) have been collected since winter 2000. As noted in previous reports, while both NAV and NCF6 have similar salinities (at least through 2000), they differ in community patterns. NAV is strongly dominated by oligochaetes (including the oligochaete species Tubificoides heterochaetus) and/or the polychaete Marenzellaria viridis during all sampling periods (Table 4.5). In contrast, oligochaetes often constitute a much smaller proportion of the total fauna at NCF6.  This site is usually dominated by a mix of midge larvae (Procladius, Polypedilum, Chironomids), amphipods (Gammarus, Monoculodes) and polychaetes (Marenzellaria, Spio, Polydora).  Estuarine polychaetes begin to dominate more at the more saline M54 site, including the worms Mediomastus, Streblospsio, Marenzellaria, and Malacoceros. Amphipods (Gammarus and Monoculodes) remain present at this site but oligochaetes are much less abundant than at NAV and insect larvae are generally uncommon (Table 4.5). Polychaete worms dominate the lowest site, M31, with Mediomastus, Parandalia, Streblospio and Marenzellaria being most common. Principal components analysis indicated relatively similar patterns among sites, with the only notable exceptions being the distinct nature of the NAV site, especially during 1996-1998, and the strong dominance of polychaetes at M31 making that site different from the other sites (Figure 4.1). NAV site is distinguished through its dominance by only a few taxa.

        The dominant taxa at all 4 sites are relatively opportunistic species capable of quick recovery after disturbances, often short-lived with good recruitment ability. Among the polychaetes, Streblospio, Mediomastus and Marenzellaria are widespread in occurrence, found in moderately disturbed estuarine environments throughout the mid Atlantic and southeast United States. Midge larvae (Chironomids, Procladius, Polypedilum) can colonize quickly because of aerial dispersal and the amphipods Gammarus and Monoculodes are also known to colonize quickly after disturbances when predation is low. Notably uncommon were bivalves, though juveniles were found and the small clam Mulinea was abundant on some dates. Also uncommon were larger burrowing or tube-dwelling fauna that are often considered characteristic of more stable and less impacted estuarine environments.    

        Total faunal density at the sites showed variable patterns. NCF6 was generally characterized by low abundances except for summer 1999, when it had the highest total faunal abundance among all sites (Figure 4.2). Fall 1998 samples were taken after the passage of Hurricane Bonnie and had low total faunal density at all sites. However, fall 1996 (after Hurricane Fran) and fall 1999 (after Hurricane Floyd) did not have consistently low abundances at all 4 sites and fall 2000 exhibited declines in total faunal abundance at all 4 sites (with no hurricane in 2000). There were no consistent declines at any site over the 5 years of sampling, though abundances at NAV were greatest in the first 2 years of sampling compared to subsequent years.

        Diversity remained consistent over time, with no significant change in diversity aside from periodic spikes and lows from 1996 to 2000 (Figure 4.3). Species richness showed a general decline at most sites from 1996 through 1998 (significant only for M31), but 1999 was a period of higher species richness at NAV, NCF6 and M54 compared to previous years. As with total abundance, species richness declined in summer-fall 2000 (Figure 4.4).

 

4.4c. Juvenile Blue Crab Abundance Patterns

        Juvenile blue crabs in the Cape Fear River showed a seasonal pattern consistent with most mid-Atlantic estuaries: peak abundance from late summer into early fall (October) with low numbers from January-March (Figures 4.5-4.6). This pattern has generally been attributed to peak larval recruitment during August-September followed by movement of juveniles into deeper areas or burial into bottom sediments during winter. Spatially, highest abundances were observed at the Southport Marina site (Figure 4.7), but we suggest this may be affected by bait and fish material left in the marina area. Among other sites, highest numbers of crabs in the sweep net catches occurred in the mid estuarine sites, CBSP and CFCM, near Carolina Beach State Park. These sweeps targeted smaller juvenile crabs, mainly <35 mm carapace width.  Catches at the SPWW site were initially high in 1998-1999, but declined in late 2000-2002. Abundances at the uppermost sites, POWL and CFPM, were intermediate. These catch patterns suggest that the most important shallow water nursery habitat may not be occurring near the mouth of the estuary, as has been suggested for some larger systems such as the Chesapeake Bay and Pamlico Sound, but rather may be located in the mid estuary.  Although long-term declines have been suggested for blue crab populations in Pamlico Sound and Core Sound over the past 5 years, 2001 catches of juveniles did not appreciably differ from 1999 catches at most sites. Highest abundances were noted in fall 2000 and lowest abundances were noted in 2002. We have monitored larval recruitment over the past several years and the high larval catches in 2000 were associated with high densities of larval crabs (zoea and megalops) in June of that year (R. Barbour, Posey and Alphin, unpublished data), emphasizing the potential importance of recruitment in determining crab abundances.

        Unlike sweep nets, seines target larger crabs, generally > 40 mm CW. These crabs were least abundant at the mid estuary sites (Figure 4.6) and most abundant at either the upper site (POWL; September of all 3 years) or the lowest site (SPWW; May-June). Movement towards the lower estuary in winter, and then movement back into the estuary and eventually into oligohaline waters by larger blue crabs has been well-documented in Chesapeake Bay and Pamlico Sound. Larger crab abundances were greatest in 2001, following the high juvenile and larval abundances observed in 2000.

 

4.5 Summary and Recommendations

        The Cape Fear River estuary is dominated by opportunistic taxa characteristic of mesohaline to oligohaline reaches of Mid Atlantic to southeastern U.S. estuaries. These taxa are quick to recolonize after disturbances and their dominance suggests the benthic community may be resilient to certain types of disturbance if that disturbance is short-lived and environmental conditions return to pre-disturbance levels. There are few long-term trends in diversity, abundance or species richness that have been consistent over the past 5 years. Similarly, there has been quick recolonization after disturbance and dominance by a relatively consistent group of species at each site over this time period. We interpret these results to indicate that the infauna in the Cape Fear River have been previously strongly affected by both natural and anthropogenic disturbances, leading to dominance by a restricted set of opportunistic species and the paucity of groups such as larger bivalves or larger burrowing worms. However, the current community includes resilient, opportunistic taxa and does not appear to be exhibiting continued decline.  The species present are likely to be able to tolerate or at least recover from water quality changes if these changes are not persistently severe.

        There continues to be a fundamental difference between the upper mainstem Cape Fear site (NAV) and the Northeast Cape Fear River site (NCF6). NCF6 has lower faunal abundances relative to NAV, with the only exception in summer 1999 (due to recruitment and later disappearance of a single polychaete species). NCF6 has higher diversity than NAV because of relatively similar densities among a suite of species at this low density site. In contrast, NAV has similar numbers of species as NCF6, but the community is dominated by only 2 taxa.

 

            Based on these results we have 4 recommendations for future efforts:

1)     Uninterrupted seasonal monitoring must be continued at all 4 sites. We now have sufficient data to detect deviations from normal patterns and it is critical to continue this database if we are to detect gradual changes in benthic community patterns.

2)      Inclusion of additional sites in the Northeast Cape Fear River and upper mainstem Cape Fear River above the city of Wilmington, as well as an additional site in the lower estuary. One of the strongest patterns to emerge from this monitoring is the difference between the NE and mainstem Cape Fear branches. However, this evidence comes from only one site in each tributary and additional sites are needed to confirm that patterns are not simply reflecting local conditions around these singular sampling locations. Another sampling site in the lower estuary will allow us to observe whether more marine and less opportunistic species begin to appear in the lower estuary where salinity extremes are not as pronounced. In response to recent funding, we plan to begin sampling of an additional upper site in each tributary at locations matching those of ongoing water quality sampling and/or ongoing monitoring for wetland biota.

3)      Addition of biomass data. Several sites experienced spikes in recruitment of selected species that disappeared by subsequent sampling periods. Biomass (size/weight) data would allow us to better understand and quantify these recruitment fluctuations and mortality patterns and allow us to factor these fluctuations out of later trend assessments.

4)      Continuation of blue crab juvenile monitoring. We currently have funding from the National Science Foundation to continue sampling into 2003 and plan to seek additional funds or community assistance to continue that sampling after this project ends.

4.6 Literature Cited

Aschan, M.M. and A.M. Skullerud. 1990. Effects of changes in sewage pollution on soft-bottom macrofauna communities in the inner Oslofjord, Norway. Sarsia 75:169-190.

Boesch, D.F., R.J. Diaz and R.W. Virnstein. 1976. Effects of tropical storm Agnes on soft- bottom macrobenthic communities of the James and York River estuaries and the lower Chesapeake Bay. Ches. Sci. 17:246-259.

Hyland, J.L., T.J. Herlinger, T.R. Snouts, A.H. Ringwood, R.F. Van Dolah, C.T. Hackney,

G.A. Nelson, J.S. Rosen and S.A. Kokkinakis. 1996. Environmental quality of estuaries of the Carolinian Province: 1994. Annual 
    statistical summary for the 1994 EMAP - Estuaries Demonstration Project in the Carolinian Province. NOAA Technical         
    Memorandum NOS ORCA 97.  NOAA/NOS, Office of Ocean Resources Conservation and Assessment, Silver Spring, MD. 
    102p.

Mallin, M.A., M. Posey, M. McIver, S. Ensign, T. Alphin, M. Williams, M. Moser and J. Merritt. 2000. Environmental assessment of the lower Cape Fear River system, 1999-2000. CMS Report No. 00-01.

Mallin, M.A., M. Posey, M. Moser, L. Leonard, T. Alphin, S. Ensign, M. McIver, G. Shank and J. Merritt. 1999. Environmental 
    assessment of the lower Cape Fear River system, 1998-1999. CMSR Report No. 99-01.

Mallin, M.A., M. Posey, M. Moser, G. Shank, M. McIver, T. Alphin, S. Ensign and J. Merritt.1998. Environmental assessment of   
     the lower Cape Fear River system, 1997-1998. CMSR Report No. 98-02.

Posey, M.H., T.D. Alphin and C.M. Powell. 1997. Plant and infaunal communities associated with a created marsh. Estuaries 20:42-47.

Simboura, N., A. Zenetus, P. Panayotides and A. Makra. 1995. Changes in benthic community structure along an environmental pollution gradient. Mar. Poll. Bull. 30:470-474.

van Dolah, R.F., D.R. Calder and D.M. Knott. 1984. Effects of dredging and open water disposal on benthic macroinvertebrates in a South Carolina estuary. Estuaries 7:28-37.

Whitehurst, I. T. and B.I. Lindsey. 1990. The impact of organic enrichment on the benthic macroinvertebrate communities of a lowland river. Wat. Res. 24:625-630.

 

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