Some Bag Experiments on Tibbs Run Lake,W.V., A Eutrophic Acidified Lake

Tibbs Run Lake was sampled from December 1979 to December 1980, monthly during the winter and biweekly during the spring, summer, and autumn. Primary production was measured from March 1980 to February 1981, either monthly or biweekly, as indicated above. The mean annual hydrogen ion concentration was equivalent to pH 4.33. This pH was 46% lower (based on H⁺ concentrations) than the 1977–1978 mean. The low pH of the lake is due to inputs of acid precipitation and the low buffering capacity of the watershed. Predictions of further reductions in the lake pH, based on mean annual hydrogen ion concentrations and hydrogen ion retention coefficients (RH) from Shellito (1979) and this study, indicate that the lake pH should reach an equilibrium with the precipitation pH between 1982 and 1985, assuming the precipitation pH continues to average 4.10. The stratified period mean chlorophyll a and total phosphorus concentrations were 22.1 mg/m³ and 19.3 μg/1, respectively. Total phosphorus loading to the lake was 0.233 gP/m²/yr. To examine the effects of neutralization and fertilization with phosphorus an in situ bag enclosure experiment, lasting 16 days, was performed during the summer of 1980. In the bags, phosphorus (20 μg/1 on days 0,4,8,12 as KH₂PO₄) was added alone and in combination with a base addition (IN KOH). The base additions raised the pH to approximately 7.8. Other treatments included base addition alone and a control. The maximum chlorophyll a concentration was found in the phosphorus treatment (∼30 mg/m³) on day 6. The phosphorus plus base treatment exhibited a 10 day lag before reaching a maximum chlorophyll a concentration (∼27 mg/m³) on day 16. The highest production rate was found in the phosphorus plus base treatment on day 12 (∼27 mgC/m³/hr.). A similar bag experiment, lasting 46 days, was performed during the late summer and early autumn of 1980. The treatments were the same as in the first experiment, however, the nitrate-nitrogen depletion in the lake and treatments necessitated the addition of nitrogen (2 mg/1 as NaNO₃) to one of each replicate treatment on day 5. On day 34, the maximum chlorophyll a concentrations were found in the phosphorus plus base nitrogen treatment (∼120 mg/m³) and the phosphorus plus nitrogen treatment (∼38.8 mg/m³). The control plus nitrogen treatment was submerged and possibly contaminated on day 5. All treatments not receiving nitrogen, except for the phosphorus plus base treatment, decreased in the chlorophyll a concentration throughout the experiment. The phosphorus plus base treatment peaked in the chlorophyll a concentration on day 45 (∼28 mg/m³) despite non-detectable levels of nitrate-nitrogen. The maximum primary production rate was found in the phosphorus plus base plus nitrogen treatment (∼32 mgC/m³/hr.) on day 11.     

Sediment Chemistry of Lake Bhim Tal,U. P., India

Certain chemical constituents (NO₃-N, bio-available P, Ca, Na, K, Mn, Cu, Co and organic matter) together with pH, Eh and clay content of surface sediments at various depths of the overlying water in Lake Bhim Tal were examined during 1977—1978. In addition, NH₃-N and dissolved oxygen at the mud-water interface (water immediately above the sediments) were measured. The values of Eh, pH and NO₃-N in the sediments showed a negative relationship with water depth and positive relationship with dissolved oxygen at the interface. The other variables of the sediment were positively related to water depth and negatively related to dissolved oxygen at the interface. Organic matter, K, Na and Ca showed positive relationship with the amount of clay while the cations (K, Na, Ca) and trace metals (Cu, Mn, Co) showed a positive relationship with the amount of organic matter in the sediments.     

Psychrosphaera saromensis gen. nov., sp. nov., within the family Pseudoalteromonadaceae, isolated from Lake Saroma, Japan

Three Gram-negative, motile, coccoid- and ellipsoidal-shaped, non-pigmented, chemoheterotrophic bacteria, designated strains SA4-31, SA4-46 and SA4-48(T), were isolated from Lake Saroma in Japan and subjected to a polyphasic taxonomical study. 16S rRNA gene sequence analysis revealed that the novel isolates could be affiliated to the family Pseudoalteromonadaceae of the order Alteromonadales. The strains shared approximately 99.7-100% sequence similarity with each other and showed 89.5-93.2% similarity with members of the family Pseudoalteromonadaceae with validly published names. The DNA-DNA relatedness among the strains SA 4-31, SA 4-46 and SA 4-48(T) was higher than 80%, a value that is accepted as a phylogenetic definition of one species. The DNA G+C contents of the three strains were 38.7-39.6 mol%. The major isoprenoid quinone was Q-8 and C16:0, C16:1 ω7c, C18:1 ω7c and C12:1 3OH were the major fatty acids. Based on the evidence from the polyphasic taxonomical study, it was concluded that the three strains should be classified as representing a new genus and species of the family Pseudoalteromonadaceae, for which the name Psychrosphaera saromensis gen. nov., sp. nov. (type strain SA4-48(T) =NBRC 107123(T)= KCTC 23240(T)) is proposed.