Chironomus
publication ID |
https://doi.org/ 10.5281/zenodo.280836 |
DOI |
https://doi.org/10.5281/zenodo.6169931 |
persistent identifier |
https://treatment.plazi.org/id/038B2C37-FF8E-FFDF-FF72-9C79FBDA1B45 |
treatment provided by |
Plazi |
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Chironomus |
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The Chironomus View in CoL group in Lake Winnipeg
At least 16 species of the Chironomus group occur in Lake Winnipeg. Chironomus (C.) bifurcatus and C. (C.) entis both are very common and distributed all over the lake ( Fig. 1 View FIGURE 1 ). The larvae of C. bifurcatus are most common in the South Basin, while C. entis is more common in the Narrows and in the North Basin. The remaining species of Chironomus are represented by only a few specimens in the bottom samples ( Fig. 1 View FIGURE 1 ).
The fluviatilis type probably is one of two species described by Wülker (2007) from the near-shore sediments of Lake Michigan, C. mozleyi Wûlker View in CoL and C. winnelli Wülker. The View in CoL significance of the different Chironomus View in CoL species as indicators of trophic levels is nicely demonstrated by their distribution in Lake Winnipeg. The oligotrophic fluviatilis type is limited to the extreme northern part of the lake which is isolated from the rest of the lake by a strong current from the outlet of the Saskatchewan River to the outlet. The mesotrophic to moderately eutrophic C. entis View in CoL is most common in the narrows and in the north basin, while the more eutrophic C. bifurcatus View in CoL is among the dominant chironomids of the south basin ( Figs. 1 View FIGURE 1 , 5 View FIGURE 5 , 7 View FIGURE 7 ) present in the same locality and especially the early instars difficult to separate. The inverse of Dyar's Rule or 0.71 is more useful in order to identify earlier instars. This rule is applicable for all examined chironomid larvae from Lake Winnipeg and is further discussed in Saether (2009; 2010a, b; 2011). The head capsule lengths of the instars of are given in Fig. 9 View FIGURE 9 . For both species the variations in head capsule lengths were the median ±11–25%, and the median of one instar was 50–56% higher than the preceding instar. The variation thus is somewhat larger than in the other species examined from Lake Winnipeg and the difference between instars is slightly smaller. (57%–63% in other examined species). The larger than normal range probably is caused by the spring generation being slightly larger than the fall generation.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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