“…Sly and Christie (1992) found a strong correlation between Diporeia abundance and sediment organic carbon, bacteria, and sediment redox potential in samples from Lake Ontario collected from 27 to 56 m. In contrast, Dermott (1978) found Diporeia to have a strong inverse relationship with depth, but only weak associations with sediment grain size and organic content in Lake Superior (no data were given on the complete depth strata sampled). This result is supported by the findings of Verhamme and Auer (2009) who reported that slope and profundal habitats exhibiting major differences in Diporeia abundance did not show consistent differences in sediment richness (e.g., bacteria numbers and sediment oxygen demand, an integrator of sediment Table 3 Diporeia length-weight and production characteristics in the shelf, slope, and profundal regions of the HN transect, Lake Superior, 2003, compared to those of Guiguer and Barton (2002) for Lake Huron and Winnell and White (1984) microbial activity). Noting that the high rates of primary production occur in the nearshore waters of Lake Superior in spring, Auer et al (2009) suggested that it was the rate of delivery to and transport through the slope that helped maintain amphipod peaks there.…”