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Research about Oneida Lake

Source-linked reports with geographic coverage including Oneida Lake.

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Cormorant predation and the population dynamics of walleye and yellow perch in Oneida Lake

Double-crested Cormorants ( Phalacrocorax auritus ) increased dramatically in North America during the 1990s, providing the opportunity to study the effects of an increase of a top predator on an existing predator-prey system. In Oneida Lake, New York, USA, Double-crested Cormorants were first observed nesting in 1984 and had increased to over 360 nesting pairs by 2000. Concomitant with this increase in piscivorous birds was a decrease in the adult walleye ( Stizostedion vitreum ) and yellow perch ( Perca flavescens ) populations. Analysis of a 40-yr data series shows higher mortality of subadults (age 1-2 yr perch and age 1-3 yr walleye) for both species in the 1990s compared to the previous three decades. Cormorant diet was investigated from 1995 to 2000 using a combination of cast pellets, regurgitants, and stomach analysis. Walleye and yellow perch were a major portion of the cormorant diet during these years (40-82% by number). The number of subadult walleye and yellow perch consumed by cormorants suggests that the increase in subadult mortality can be explained by predation from cormorants. Mean mortality rates of adult percids attributed to cormorant predation were 1.1% per year for walleye and 7.7% per year for yellow perch. Our analysis suggests that predation by cormorants on subadult percids is a major factor contributing to the decline in both the walleye and the yellow perch populations in Oneida Lake. Other ecosystem changes (zebra mussels, lower nutrient loading, decrease in alternate prey) are not likely explanations because the potential mechanisms involved are not consistent with auxiliary data from the lake and would not affect subadult mortality. The likely impact of bird predation on percid populations in Oneida Lake occurs because cormorants feed on larger fish that are beyond the size range where compensatory mechanisms are important.

New York

Growth rates of manganese nodules in Oneida Lake, New York

226 Ra is used to document the growth histories of six manganese nodules from Oneida Lake, New York. Detailed sectioning and analysis reveal that there are discontinuous gradients in 226 Ra content in these samples. These gradients result from periods of rapid growth (>1 mm/100 years) separated by periods of no growth of erosion. Although the 226 Ra “age” of the nodules approximates the age of Oneida Lake, the nodules are not sediment-covered because they occur only in areas of the lake where fine-grained sediments are not accumulating.

New York

Factors contributing to the formation of ferromanganese nodules in Oneida Lake, New York

Oneida Lake is a large, shallow, eutrophic lake situated in the Ontario lowlands of central New York State. It contains the most concentrated deposit of freshwater ferromanganese nodules (in terms of amount per unit area) yet reported in the literature. The mineralogy and bulk chemistry of these saucer-shaped nodules are similar to the mineralogy and bulk chemistry of deep-sea ferromanganese nodules, but the nodules in Oneida Lake contain considerably lower concentrations of trace metals, especially cobalt, nickel, and copper. Budgets for iron and manganese in waters from Oneida Lake and its tributaries indicate that approximately 122 t (metric tons) of iron and 23 t of manganese are lost each year from the lake waters, presumably by incorporation into sediments and ferromanganese nodules. Estimates based on nodule abundance and age of the lake suggest that iron and manganese are being incorporated into ferromanganese nodules at rates of 13 and 22 t/yr, respectively. Most iron lost from the lake waters is apparently incorporated into sediments, which contain an average of 10 times more iron than manganese. Most manganese lost from the lake waters is apparently incorporated into ferromanganese nodules, which contain an average of 1.7 times more manganese than iron. In Oneida Lake, very high rates of phytoplankton productivity, combined with almost continuous wind mixing to the bottom, provide high-pH and high-Eh conditions in most of the lake. Algae also provide an effective means of concentrating and transporting iron and manganese and thereby aid in the extensive development of ferromanganese nodule deposits.

New York