Brenda J. Hann

Littoral microcrustaceans (Cladocera, Copepoda) in a prairie coastal wetland: seasonal abundance and community structure

Seasonal species abundance and community structure of the littoralmicrocrustacean community (Cladocera, Copepoda) in two areas of DeltaMarsh were investigated over the open-water season. Cladoceranabundance in Crescent Pond, with no fish, only invertebrate predatorswas considerably higher than in Blind Channel, with both fish andinvertebrate predators, and where cyclopoid copepods were thedominant microcrustaceans. In both areas, a small number of speciesof planktonic cladocerans characterized the community in spring andearly summer, whereas a diverse array of species of phytophilouscladocerans comprised the community throughout the summer. Daphnia rosea was the most abundant species in the planktoniccommunity in Crescent Pond for the first half of the summer, and Ceriodaphnia dubia was most abundant in the last half. In contrast,no single planktonic cladoceran species was consistently mostabundant in Blind Channel. The sequence of dominant phytophilouscladoceran species observed in Crescent Pond through the season wasChydorus sp. 2, Simocephalus vetulus, Pleuroxusdenticulatus, and Ceriodaphnia dubia, and in Blind Channel,Alona circumfimbriata, Simocephalus vetulus, and Ceriodaphnia dubia. Dominant planktonic and phytophilous copepods inboth areas were Diacyclops thomasi, Acanthocyclops vernalis,Eucyclops agilis, and Macrocyclops albidus. Canonicalcorrespondence analysis revealed differences in community structurebetween areas of the marsh related to turbidity, phytoplanktonbiomass, and soluble reactive phosphorus concentration.

Truncated foodweb effects of omnivorous minnows in a recovering acidified lake

Cyprinids (Margariscus margarita, Phoxinus spp., Pimephales promelas) have resumed reproduction in a boreal headwater lake (Lake 302S, Experimental Lakes Area, northwestern Ontario) that is recovering from experimental acidification. Concomitant changes to the littoral food web suggested that these omnivorous minnows suppressed the development of green algal mats, termed metaphyton. We tested this hypothesis by conducting an experiment using minnow enclosures, minnow exclosures, and open control plots in the shallow littoral zone of Lake 302S. Minnows significantly suppressed zooplankton biomass, and altered community composition by disproportionally reducing large daphnids and chydorids. Epiphytic chironomids were also significantly less abundant in the presence of minnows. Minnows had a significant time-dependent, negative effect on benthic invertebrate biomass and community composition because chironomids and anisopterans were suppressed during the second half of the 6-wk experiment. However, minnows did not reduce the abundance of the dominant primary producer, namely metaphyton. Stable isotope analyses revealed that minnows did not suppress metaphyton because these algae were not the primary C source for the food web. Instead, our findings suggest that the littoral food web depended mainly on sedimentary C, which resulted in the foodweb effect of minnows being truncated at the level of invertebrates. Therefore, metaphyton appears to be regulated primarily by abiotic factors (e.g., availability of dissolved inorganic C) and not herbivory in recovering acidified lakes.

Waterfowl feces as a source of nutrients to a prairie wetland: responses of microinvertebrates to experimental additions

We tested the hypothesis that inorganic nutrients released fromwaterfowl feces would stimulate primary production, therebyaffecting microinvertebrate grazers, by making controlledadditions of waterfowl feces to fishless wetland enclosures andmeasuring the response of planktonic and phytophilouscladocerans, copepods, and rotifers. Feces were added in twopulses, four weeks apart, to duplicate enclosures at a ‘high’level (115 g m−2 wet feces), simulating the total P load(1.6 g m−2) applied in an earlier fertilizationexperiment, and a ‘low’ level (11.5 g m−2). Density ofmicrocrustacean grazers in the water column increased inresponse to both feces additions, although the response wasmore noticeable after the second feces addition. After eachaddition, cladocerans (predominantly Ceriodaphnia dubia)and copepodites in the water column (and associated withperiphyton on acrylic rods in the water column) were mostabundant in enclosures with high loading. In contrast, densityof microcrustacean grazers associated with macrophytes(predominantly Chydorus spp. and copepodites) increasedin response to the second feces addition only.Microinvertebrate density increased only slightly with lowfeces loading. Community composition showed similar changesover the season in all enclosures, and differences in relativeabundance were not attributable to treatment effects. Given thesmall effects produced by nutrient additions that greatlyexceed natural loadings, nutrients leaching from waterfowlfeces do not appear to have a significant impact on the foodwebof this wetland.

Naturally occurring interspecific hybridization in Simocephalus (Cladocera, Daphniidae): its potential significance

Among the Cladocera, the occurrence of interspecific hybrids in nature has been reported frequently but rarely adequately documented. During the course of a survey of the genetic variation and population structure of several species of Simocephalus in ponds in southern Ontario, Canada, readily distinguishable congeners often co-occurred in a pond. Occasionally, clones were recovered that were intermediate in phenotype (as determined from both morphological and electrophoretic analyses) between two species. Two different hybrid clones have been examined in detail to determine the parentals involved in the crosses. Evidence from field and laboratory studies is presented to document the hybrid nature of these clones. Factors favouring formation and long-term survival of hybrids in littoral zone and pelagic species are discussed.

Genetic variation in Simocephalus (Anomopoda: Daphniidae) in North America: patterns and consequences

The presumption of intercontinental distributions of many species of Anomopoda has been reinforced by their considerable morphological uniformity and ease of passive dispersal via ephippial eggs. To test the validity of this dogma, genetic variation among taxa in the cladoceran genus Simocephalus was examined on a continental scale. Genetic variability (percentage polymorphic loci = 8.8%, individual heterozygosity = 3.4%) was comparable to that determined on a local scale in Simocephalus and somewhat less than for other zooplankton groups. Four species complexes were distinguished allozymically with unique allelic substitutions found for at least two loci between these taxa. Eight species in North America were differentiated within these complexes (Nei s genetic distance, D>0.30), all of which were clearly separated from two European species. Both S. cf. vetulus and S. cf. serrulatus are broadly distributed in North America, and intraspecific divergence is relatively low. In contrast, S. cf. congener and S. cf. exspinosus represent species complexes, both consisting of several species, differentiated allozymically and morphologically. The concept of generalist species with moderate genetic variation throughout a broad range and specialist species, genetically depauperate, with restricted distributions, is explored.

Naturally occurring interspecific hybridization inSimocephalus (Cladocera, Daphniidae): its potential significance

Among the Cladocera, the occurrence of interspecific hybrids in nature has been reported frequently but rarely adequately documented. During the course of a survey of the genetic variation and population structure of several species ofSimocephalus in ponds in southern Ontario, Canada, readily distinguishable congeners often co-occurred in a pond. Occasionally, clones were recovered that were intermediate in phenotype (as determined from both morphological and electrophoretic analyses) between two species. Two different hybrid clones have been examined in detail to determine the parentals involved in the crosses. Evidence from field and laboratory studies is presented to document the hybrid nature of these clones. Factors favouring formation and long-term survival of hybrids in littoral zone and pelagic species are discussed.

Investigating the invasion of the nonindigenous zooplankter, Eubosmina coregoni, in Lake Winnipeg, Manitoba, Canada

ABSTRACT The spread of nonindigenous species (NIS) over land and via interconnecting water bodies is threatening aquatic ecosystems worldwide. This study examines the invasion of the first known NIS zooplankter, Eubosmina coregoni, into Lake Winnipeg, Manitoba, Canada. Analyses of cladoceran microfossils from a sediment core collected in the North Basin of the lake indicate this species first appeared in sediments dated to the late 1980s. An increase in total cladoceran accumulation rates coupled with increasing N, C, P, and chlorophyll a over the last 40 years provides evidence of eutrophication. Extant samples from fall 2002–2005 indicate that E. coregoni is mainly restricted to the North Basin while Bosmina longirostris is present throughout the lake. Results from this study provide baseline data regarding the invasion and establishment of E. coregoni, a precursor to future NIS that may have substantial ecological and economic impacts on the Lake Winnipeg ecosystem.

Comparative analysis of cladoceran microfossils in the Don and Scarborough Formations, Toronto, Canada

Pleistocene deposits at Toronto, consisting of Don Formation (considered to be of Sangamonian interglacial age) and Scarborough Formation (interpreted to be Early Wisconsinan, >50 000 years B.P.) were examined at three sites: Don Valley Brickyard, Leaside, and at the south end of Brimley Road at the foot of the Scarborough Bluffs. Comparison of the cladoceran microfossil assemblages described from these sites has enabled reconstruction of the lacustrine environment of the region.Cladoceran microfossil evidence from each site confirmed the disparity in community composition and structure, and in environmental conditions that existed during deposition of the Don and Scarborough Formations. Cladocera community composition averaged 40–45% remains of littoral species in the warmer Don interval at all three sites. The Scarborough Formation contained a more homogeneous cladoceran assemblage, with higher community similarity across sites than observed in the Don Formation. However, there was greater variation in the littoral: planktonic ratio among sites, ranging from >0.90 at Leaside to <0.10 at Brimley Road.Stratigraphically constrained cluster analysis of cladoceran microfossil assemblages clearly separated the communities in the Don Formation from those in the Scarborough Formation at each site. During the interglacial, the Don Brickyard site appears to have been a shallow, protected embayment on the lake shore, whereas the other sites are more distinctly lacustrine. The Scarborough assemblage at each site is representative of deeper, oligotrophic, subarctic lakes.

Influence of temperature on hatching of eggs of Lepidurus couesii (Crustacea, Notostraca)

Tadpole shrimps (Notostraca) occur sporadically in temporary ponds and their survival there depends largely upon the drought-resistant eggs they produce. Environmental conditions conducive to hatching of eggs of Lepidurus couesii were investigated in the laboratory. Almost all eggs hatched best at 20 °C, whether desiccated for a short or long period, with a prior freezing shock or without such a shock, with intact shells. Eggs that endured a longer period of desiccation and eggs with abraded shells displayed a more equivocal response to different temperatures for hatching. Long-term hatchability of eggs was demonstrated. Time required for successful hatching was shortest at 20 °C, with no discernible difference between 17 °C and 25 °C. Both short- and long-term survival of populations of the species appears to be fostered by the adaptive response to temperature shown by the eggs.

Exploitation by microcrustacea of a new littoral habitat in an acidified lake

Extensive growths of filamentous green algae (metaphyton) developed at pH 4.5 in the littoral zone of Lake 302S and dense populations of microcrustacean grazers occupied this new habitat. Microcrustacean community composition in this metaphyton consisted predominantly of cladocerans (e.g. Chydorus piger, Acantholeberis curvirostris, Alona intermedia, A. rustica, Acroperus cf. harpae and Simocephalus serrulatus) as well as substantially fewer copepods, including Macrocyclops albidusand Eucyclops agilis. Despite the development of this new littoral habitat, the metaphyton-associated microcrustacea were relatively homogeneous throughout the littoral zone in terms of composition, species richness and diversity, which varied little among any of the benthic habitats (macrophytes, sediments, boulders, metaphyton). Cladoceran and copepod density varied seasonally and synchronously in all habitats with highest densities occurring in June-July and September. Densities were much higher in metaphyton than in other littoral habitats.