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Waterfowl and Wetlands of Long Point Bay and Old Norfolk County

6.0 Aquatic Macroinvertebrate Distribution and Abundance in Long Point Bay

6.2 Distribution and abundance of native aquatic macroinvertebrates in Long Point Bay

Table 6.1 Invertebrate Distribution and Composition in Long Point's Inner Bay, Shown as an Average Number per m2 at Each Sampling Station.

Table 6.2 Mean Numbers of Invertebrate Taxa in Samples Collected from Throughout the Nearshore Region of Lake Erie, Grouped by Type of Sediment and Water Depth.

Table 6.3 Density Of Macroinvertebrates (# per m2) Sampled at Selected Ponds on the Long Point National Wildlife Area.

Based on the LPWWRF 1992 survey, native aquatic macroinvertebrates are distributed somewhat unevenly throughout the Inner Bay (Table 5.1, see Figure 5.1 for the boundaries of sampling areas) and the densities are below those considered to be sufficient for successful growth and survival of ducklings in nearby Brant County (>3600 per mē)(Godin and Joyner 1981). The North Shore, and Big Creek areas in particular had low invertebrate densities, while the open water area had slightly higher densities (Table 6.1). Turkey Point, Crown Marsh and Thoroughfare Point had the highest invertebrate densities on the Inner Bay. This may be attributed to the fact that the distribution and abundance of aquatic macroinvertebrates is influenced both spatially and temporally by several abiotic and biotic factors. For instance, invertebrate community structure at any given time or location is influenced by the type of substrate, amount and species composition of aquatic vegetation, kinds and amount of organic matter available, and the quality (high phosphorus loadings increase the availability of phytoplankton to herbivorous invertebrates), depth, temperature and oxygen concentration of water (Krecker and Lancaster 1933; Dermott 1978; Barton 1988). As over 90% of the Inner Bay is covered by submerged aquatic plants, and the water characteristics and depth are fairly uniform, differences in invertebrate species composition and availability among areas is most likely a function of the availability of particular plant species and type of substrate. Due to a lack of thermal stratification and macrophyte photosynthesis, dissolved oxygen is probably not limiting to invertebrates on the Inner Bay in (Leach 1981).

Table 6.1 Invertebrate Distribution and Composition in Long Point's Inner Bay, Shown as an Average Number per m2 at Each Sampling Station, Summer 1992.

  Area
Common name Scientific Name Entire Inner Bay Turkey Point North Shore Big Creek Crown Marsh Through fare Point Open water
Snail Gastropoda 690 366 973 1222 484 660 668
Clam Pelecepod 34 85 14 42 16 67 27
Zebra mussels Dreissens polymorpha 854 839 629 210 48 319 1752
Chironamid larvae Diptera 685 1111 255 234 1164 790 819
Scuds Amphipoda 427 456 195 362 576 612 471
Sow bugs Isopoda 140 157 108 181 136 172 128
Mites Acarina 58 231 33 2 8 38 58
Worms Oligochaeta 53 77 84 49 28 40 39
Blood suckers Hirudinaea 22 22 19 5 60 23 23
Caddisfly larvae Tricoptera 17 11 12 20 12 26 19
Nematode Planaria 7 3 9 20 8 2 5
Mayfly larvae Ephemeroptera 2 6 1 2 0 2 2
Dragonfly larvae Odonata 1 0 1 0 0 0 0
Avg. # per/m2 2990 3364 2333 2349 2540 2751 4010
# sample stations 159 16 33 18 11 23 58
Note: Introduced quagga mussels (Dreissena bugensis) were combined with zebra mussels.

The aquatic plant species composition of each area of the Inner Bay is characteristic (Chapter 5), and aquatic plant species generally have specific assemblages of invertebrates associated with them. For example, species associated with the invasive Eurasian milfoil differ from the invertebrates associated with neighboring native plants (Johnson and Brinkhurst 1971; Gerrish and Bristow 1979; Keast 1984). Also, submerged, leafy types of vegetation are more densely populated than are the emergent, hard surfaced, non-leafy types (Krecker 1939). Krecker (1939) studied the invertebrates associated with several species of submerged macrophytes in the wetlands of western Lake Erie. Water weed hosted the greatest number of genera (26) and wild celery contained the fewest (4) per 3.05 m (10 ft) length of transect. Interestingly, Eurasian milfoil (finely divided leaves) and curly leaved pondweed (curled and crenulated leaves), harbored much higher numbers of individuals per 3.05 m (10 ft) than the other species (1442 and 1139 respectively). Therefore, while both Eurasian milfoil and curly leaved pondweed are of limited importance as waterfowl foods at Long Point (Table 5.4), they may be indirectly important for waterfowl, because they harbor large quantities of invertebrates. Interestingly, declines in Eurasian milfoil in certain aquatic systems have been attributed to consumption by insects (Oliver 1984). Whitewater buttercup, Richardson's pondweed, and musk grass also host large quantities of insects, and this has been attributed to the fact that these plant species harbor large quantities of detritus and diatoms which are consumed by invertebrates (Brooke 1984).

Wild celery (limited leaf dissection) supported the fewest (<50) number of individual invertebrates per 3.05 m transect which explains the low invertebrate availability in the north shore and Big Creek areas, as they are dominated by this plant species. Low North Shore and Big Creek invertebrate availability may also be a function of substrate type and depth, as a study of nearshore Lake Erie invertebrates suggests that muddy substrates with water depths less < 5 m have the lowest invertebrate densities (Barton 1988)(Table 6.2). It has been suggested that even a thin layer of sand or mud over more consolidated sediments can significantly affect invertebrate community structure (Barton 1988). In contrast, muddy sand substrates, such as are found throughout much of the rest of the Inner Bay, support over four times as many invertebrates as do mud substrates alone (Barton 1988)(Table 6.2). Interestingly, large rocks have usually been found to support the most diverse invertebrate communities when appropriate sampling techniques are employed (Barton 1988).

Table 6.2 Mean Numbers of Invertebrate Taxa in Samples Collected from Throughout the Nearshore Region of Lake Erie, Grouped by Type of Sediment and Water Depth. "Coarse" Includes Bedrock, Pebbles, and Gravel.

  Depth (m)
Sediment 0-5 6-10 11-15 16-20
Coarse 4.8 6.6 7.4 6.0
Muddy gravel ns* 11.6 7.2 7.2
Gravelly sand 9.7 7.6 8.8 7.5
Sand 4.4 10.3 7.2 7.2
Muddy Sand 8.2 12.0 11.2 10.2
Sandy mud 7.0 14.7 11.2 10.2
Mud 2.0 11.3 11.2 10.7
*ns means no sample taken                                                                                                            From Barton 1988

Wilcox and Knapton (1994) did not survey the invertebrates in the Outer Bay of Long Point. However, Barton (1988) did do a cursory survey at a few locations. He found that Gammarus fasciatus, Pseudochironomus sp, and Heterotrissocladius changi were largely restricted to Outer Long Point Bay, but he made no mention of biomass or species diversity. Gammarus fasciatus in particular was ubiquitous and randomly distributed within the Outer Bay, but was collected only rarely in the central basin of Lake Erie. While the relative availability of invertebrates in the Inner and Outer Bay have not been studied, invertebrates are much more abundant in vegetated areas than non-vegetated areas (Krull 1970). For example, Voigts (1976) found that maximum numbers of invertebrates occurred where beds of submerged aquatic plants were interspersed with stands of emergent vegetation, and Krieger (1992) determined that wetlands with ample submergent and floating-leaved vegetation possess a higher diversity and biomass of invertebrates than wetlands with limited aquatic plant availability. This can be attributed to the fact that aquatic plants are important as indirect and direct food sources; they also provide shelter from turbulence and predators, sites for oviposition, and sources of oxygen (Brooke 1984). Therefore, the reduced availability of aquatic vegetation and lower productivity of the Outer Bay probably predisposes it to having a lower native aquatic macroinvertebrate availability than does the Inner Bay (Leach 1981).

LPWWRF (unpublished data) sampled invertebrates on 6 ponds and creeks (Helmer's, Cedar Creek, Bouck's, Anderson, Duncan's and Long) on the Long Point spit during late summer, 1992. Surprisingly, no zebra mussels were recorded and the density and diversity of native invertebrates was low, relative even to the Inner Bay (Table 6.3). Amphipods (Gammaridae) and Diptera (Chironomidae) comprised about 80% of all organisms. While only a cursory investigation of Big Creek Marsh has been undertaken, benthic macroinvertebrates appear to be dominated by chironomid larvae and amphipods, while quantities of Physidae, Odonata, and Isopoda were also present from mid July to mid October (Wade 1979).

Table 6.3 Density Of Macroinvertebrates (# per m2) Sampled at Selected Ponds on the Long Point National Wildlife Area. (sites sampled on either 26 August or 4 September, 1992)

Invertebrate group Duncan's Long Anderson Helmer's Cedar Creek Bouck's
Acarina 0 0 0 0 0 172
Annelida 14 43 22 0 43 129
Amphipoda 559 215 409 1763 667 0
Isopoda 0 0 0 0 538 0
Diptera 43 258 129 151 194 129
Tricoptera 86 0 43 0 0 0
Gastropoda 43 0 65 387 150 430
Pelecypoda 29 0 43 43 0 989
Combined density 774 516 710 2343 1591 1849
LPWWRF unpublished data.

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