Food-web manipulations influence grazer control of phytoplankton growth rates in Lake Michigan

1987 ◽  
Vol 9 (5) ◽  
pp. 891-899 ◽  
Author(s):  
Robert M. Dorazio ◽  
James A. Bowers ◽  
John T. Lehman
1991 ◽  
Vol 48 (1) ◽  
pp. 116-122 ◽  
Author(s):  
Paul E. Sager ◽  
Sumner Richman

The functional interaction of phytoplankton and zooplankton, expressed in terms of the numerical difference between phytoplankton growth rates per day (in situ,14C method) and zooplankton grazing rates per day (in situ feeding experiments), was studied along the trophic gradient in Green Bay, Lake Michigan. Growth–grazing differences increased with trophic conditions, averaging 0.08 for the water column in the meso-oligotrophic northern bay and 0.56 in the eutrophic southern bay for the summers of 1986, 1987, and 1988. Eutrophic conditions produced dominance of growth by large-size cyanobacteria and low grazing rates by microcrustaceans Small and occasionally negative growth–grazing differences in the meso-oligotrophic region were associated with dominance of larger cladocerans and calanoid copepods and small algal species Phytoplankton growth rates in the northern bay averaged about 28% those of the eutrophic region. A unimodal phytoplankton growth response to increased grazing was observed in the northern bay, suggesting variation in positive (growth stimulating) and negative (grazing losses) effects of zooplankton on the phytoplankton.


1983 ◽  
Vol 61 (5) ◽  
pp. 1120-1127 ◽  
Author(s):  
L. M. Carl

Coho salmon spawning peaked in the late fall. Spawning densities ranged from fewer than 5 coho salmon per hectare up to 90 fish per hectare. Subyearling coho salmon densities ranged from 10 to 60 fish per 100 m2 in June and dropped to 5–20 fish by early fall. Coho salmon fry increased in length from 40 mm in early May, to over 120 mm by smolt out-migration in the following April. Coho salmon instantaneous daily change in density coefficients ranged from 0.004 to 0.019 and were dependent on initial coho density. Daily coho salmon growth rates ranged from 0.38 to 0.60 mm per day and were not dependent on initial coho salmon density. Downstream movement of rainbow trout fry began in May, and continued into July. In the spring 10–20 yearlings and one to five 2-year-olds per 100 m2 were present. Most fry emerged in June at a size of 25 mm and grew to 85 mm by fall. Daily growth rates varied from 0.23 to 0.45 mm per day for yearling rainbow trout and were not correlated with rainbow trout density.


1987 ◽  
Vol 13 (2) ◽  
pp. 218-223 ◽  
Author(s):  
B.A. Manny ◽  
G.L. Fahnenstiel ◽  
W.S. Gardner

2005 ◽  
pp. 183-204
Author(s):  
M. Munawar ◽  
I.F. Munawar ◽  
M. Fitzpatrick ◽  
D. Lynn

Ecosphere ◽  
2017 ◽  
Vol 8 (7) ◽  
pp. e01862 ◽  
Author(s):  
Monica Granados ◽  
Ianina Altshuler ◽  
Stéphane Plourde ◽  
Gregor F. Fussmann

2014 ◽  
Vol 71 (7) ◽  
pp. 1072-1086 ◽  
Author(s):  
Mark W. Rogers ◽  
David B. Bunnell ◽  
Charles P. Madenjian ◽  
David M. Warner

Ecosystems undergo dynamic changes owing to species invasions, fisheries management decisions, landscape modifications, and nutrient inputs. At Lake Michigan, new invaders (e.g., dreissenid mussels (Dreissena spp.), spiny water flea (Bythotrephes longimanus), round goby (Neogobius melanostomus)) have proliferated and altered energy transfer pathways, while nutrient concentrations and stocking rates to support fisheries have changed. We developed an ecosystem model to describe food web structure in 1987 and ran simulations through 2008 to evaluate changes in biomass of functional groups, predator consumption, and effects of recently invading species. Keystone functional groups from 1987 were identified as Mysis, burbot (Lota lota), phytoplankton, alewife (Alosa pseudoharengus), nonpredatory cladocerans, and Chinook salmon (Oncorhynchus tshawytscha). Simulations predicted biomass reductions across all trophic levels and predicted biomasses fit observed trends for most functional groups. The effects of invasive species (e.g., dreissenid grazing) increased across simulation years, but were difficult to disentangle from other changes (e.g., declining offshore nutrient concentrations). In total, our model effectively represented recent changes to the Lake Michigan ecosystem and provides an ecosystem-based tool for exploring future resource management scenarios.


1990 ◽  
Vol 47 (9) ◽  
pp. 1836-1841 ◽  
Author(s):  
Gwenyth Laird Pernie ◽  
Donald Scavia ◽  
Michael L. Pace ◽  
Hunter J. Carrick

We estimated Lake Michigan epilimnetic heterotrophic bacterial loss rates, predator size, and substrate limitation in 1986 and 1987. The bacterial growth rates were always enhanced by organic substrate additions indicating that bacterial growth is limited, to some degree, by substrate availablility. In this study we obtained loss rates and intrinsic growth rates each between 0.32 and 1.45 d−1. The grazers were predominantly picoplankton-size organisms, presumably heterotrophic flagellates. Using radiolabeled bacteria, only a small percentage (2–3%) of bacterial cells were incorporated into larger size fractions after 24 h. These results indicate that during our experiments heterotrophic bacteria were not a direct, significant, carbon source for the upper trophic levels.


2018 ◽  
Vol 44 (5) ◽  
pp. 910-923 ◽  
Author(s):  
Bart T. De Stasio ◽  
Ashley E. Beranek ◽  
Michael B. Schrimpf

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