Impact of Atrazine on Periphyton in Freshwater Enclosures and Some Ecological Consequences

1986 ◽  
Vol 43 (10) ◽  
pp. 1917-1925 ◽  
Author(s):  
David Herman ◽  
Narinder K. Kaushik ◽  
Keith R. Solomon
Keyword(s):  
Organic Matter ◽  
Algal Biomass ◽  
Carbon Assimilation ◽  
Ecological Consequences ◽  
Periphyton Community ◽  
Surface Application ◽  
Herbicide Atrazine

The herbicide atrazine inhibited production of periphyton within limnocorrals (in situ aquatic enclosures) and altered the composition of the periphyton community. On two occasions, 6 wk apart, three limnocorrals were treated with a surface application of atrazine equivalent to a nominal enclosure concentration of 100 μg∙L−1 During the first atrazine pulse, the Cyanophyta disappeared and organic matter decreased to values significantly less than those within three control enclosures. Within 3 wk of the second atrazine application, a 36–67% reduction in organic matter, chlorophyll, and algal biomass and a significant decrease in the rate of carbon assimilation were evident. These events coincided with a decrease in number of certain Chlorophyta species, although other Chlorophyta species increased in number. The Bacillariophyceae maintained biomass levels greater than those in the controls for 9 wk after the second atrazine application. Total limnocorral periphyton production was greater than that of the phytoplankton after 5–10 wk of periphyton colonization in both the control and atrazine limnocorrals.

Response of Lake Michigan Benthic Algae to in situ Enrichment with Si, N, and P

1988 ◽  
Vol 45 (2) ◽  
pp. 271-279 ◽  
Author(s):  
Hunter J. Carrick ◽  
Rex L. Lowe
Keyword(s):  
Chlorophyll A ◽  
Algal Biomass ◽  
Lake Michigan ◽  
Benthic Algae ◽  
Benthic Diatoms ◽  
Nearshore Area

The possibility that benthic algae in the nearshore area of Lake Michigan might be growth limited by Si was tested using nutrient-releasing substrata. Nutrient treatments were Si, N + P, Si + N + P, and controls (CONT) and were sampled after 7, 14, and 31 d of exposure. Addition of Si alone had little stimulatory effect on algal biomass, while enrichment with Si + N + P led to the greatest increase in chlorophyll a, particulate Si, total biovolume, and diatom biovolume after 14 d of incubation (P < 0.0001). By day 31, communities on CONT and Si substrata exhibited little change in biomass and remained dominated by diatoms (98% of total biovolume), while algal biomass on both N + P and Si + N + P substrata increased more than eightfold (P < 0.0001) and consisted mainly of Stigeoclonium tenue (Chlorophyta) and Schizothrix calcicolas (Cyanophyta). These results indicate that benthic diatoms in Lake Michigan are not currently limited by Si, but may become Si limited following enrichment with N + P.

scholarly journals Lipid biomarkers in Holocene and glacial sediments from ancient Lake Ohrid (Macedonia, Albania)

2010 ◽  
Vol 7 (11) ◽  
pp. 3473-3489 ◽  
Author(s):  
J. Holtvoeth ◽  
H. Vogel ◽  
B. Wagner ◽  
G. A. Wolff
Keyword(s):  
Organic Matter ◽  
Lipid Biomarkers ◽  
Lake Ohrid ◽  
Labile Organic Matter ◽  
Glacial Sediments ◽  
Plant Matter ◽  
Lipid Biomarker ◽  
First Results ◽  
Near Shore

Abstract. Organic matter preserved in Lake Ohrid sediments originates from aquatic and terrestrial sources. Its variable composition reflects climate-controlled changes in the lake basin's hydrology and related organic matter export, i.e. changes in primary productivity, terrestrial plant matter input and soil erosion. Here, we present first results from lipid biomarker investigations of Lake Ohrid sediments from two near-shore settings: site Lz1120 near the southern shore, with low-lying lands nearby and probably influenced by river discharge, and site Co1202 which is close to the steep eastern slopes. Variable proportions of terrestrial n-alkanoic acids and n-alkanols as well as compositional changes of ω-hydroxy acids document differences in soil organic matter supply between the sites and during different climate stages (glacial, Holocene, 8.2 ka cooling event). Changes in the vegetation cover are suggested by changes in the dominant chain length of terrestrial n-alkanols. Effective microbial degradation of labile organic matter and in situ contribution of organic matter derived from the microbes themselves are both evident in the sediments. We found evidence for anoxic conditions within the photic zone by detecting epicholestanol and tetrahymanol from sulphur-oxidising phototrophic bacteria and bacterivorous ciliates and for the influence of a settled human community from the occurrence of coprostanol, a biomarker for human and animal faeces (pigs, sheep, goats), in an early Holocene sample. This study illustrates the potential of lipid biomarkers for future environmental reconstructions using one of Europe's oldest continental climate archives, Lake Ohrid.

scholarly journals Sediment community responses to marine vs. terrigenous organic matter in a submarine canyon

2013 ◽  
Vol 10 (1) ◽  
pp. 67-80 ◽  
Author(s):  
W. R. Hunter ◽  
A. Jamieson ◽  
V. A. I. Huvenne ◽  
U. Witte
Keyword(s):  
Organic Matter ◽  
Feeding Activity ◽  
N Uptake ◽  
Bacterial Biomass ◽  
Submarine Canyon ◽  
Stable Isotope Labelling ◽  
C And N ◽  
13C Label ◽  
Experimental Treatments

Abstract. The Whittard Canyon is a branching submarine canyon on the Celtic continental margin, which may act as a conduit for sediment and organic matter (OM) transport from the European continental slope to the abyssal sea floor. In situ stable-isotope labelling experiments were conducted in the eastern and western branches of the Whittard Canyon, testing short-term (3–7 days) responses of sediment communities to deposition of nitrogen-rich marine (Thalassiosira weissflogii) and nitrogen-poor terrigenous (Triticum aestivum) phytodetritus. 13C and 15N labels were traced into faunal biomass and bulk sediments, and the 13C label traced into bacterial polar lipid fatty acids (PLFAs). Isotopic labels penetrated to 5 cm sediment depth, with no differences between stations or experimental treatments (substrate or time). Macrofaunal assemblage structure differed between the eastern and western canyon branches. Following deposition of marine phytodetritus, no changes in macrofaunal feeding activity were observed between the eastern and western branches, with little change between 3 and 7 days. Macrofaunal C and N uptake was substantially lower following deposition of terrigenous phytodetritus with feeding activity governed by a strong N demand. Bacterial C uptake was greatest in the western branch of the Whittard Canyon, but feeding activity decreased between 3 and 7 days. Bacterial processing of marine and terrigenous OM were similar to the macrofauna in surficial (0–1 cm) sediments. However, in deeper sediments bacteria utilised greater proportions of terrigenous OM. Bacterial biomass decreased following phytodetritus deposition and was negatively correlated to macrofaunal feeding activity. Consequently, this study suggests that macrofaunal–bacterial interactions influence benthic C cycling in the Whittard Canyon, resulting in differential fates for marine and terrigenous OM.

Microbial-accessibility-dependent electron shuttling of in situ solid-phase organic matter in soils

Geoderma ◽  
2019 ◽  
Vol 338 ◽  
pp. 1-4 ◽  
Author(s):  
Wenbing Tan ◽  
Beidou Xi ◽  
Guoan Wang ◽  
Xiaosong He ◽  
Rutai Gao ◽  
...  
Keyword(s):  
Organic Matter ◽  
Solid Phase ◽  
Electron Shuttling

scholarly journals The in situ bacterial production of fluorescent organic matter; an investigation at a species level

2017 ◽  
Vol 125 ◽  
pp. 350-359 ◽  
Author(s):  
B.G. Fox ◽  
R.M.S. Thorn ◽  
A.M. Anesio ◽  
D.M. Reynolds
Keyword(s):  
Organic Matter ◽  
Bacterial Production ◽  
Species Level

scholarly journals In vitro estimation of rumen fermentable organic matter using enzymes

1996 ◽  
Vol 44 (2) ◽  
pp. 103-110 ◽  
Author(s):  
J.W. Cone ◽  
A.H. Van Gelder ◽  
A.M. Van Vuuren
Keyword(s):  
Organic Matter ◽  
Crude Fibre ◽  
Fermentation Products ◽  
In Situ Method ◽  
Degradation Rates ◽  
Digestible Organic Matter ◽  
Similar Accuracy ◽  
The Relationship

The amount of rumen fermentable organic matter (FOM) can be calculated using tables, taking into account the amount of digestible organic matter, the content of fat and fermentation products, and the amount of starch and protein escaping rumen fermentation, or FOM can be calculated using in situ incubations. An in vitro method is described to predict FOM using amylase and other carbohydrate degrading enzymes. FOM estimated by the enzymic method showed a moderate correlation (Rsuperscript 2 = 0.71) with FOM estimated by the in situ method. The relationship could be improved by separating the high crude fibre samples (Rsuperscript 2 = 0.88) from the other samples (Rsuperscript 2 = 0.77). Because degradation rates with the enzymic method were high compared with the assumed rumen passage rates, it proved that FOM could be predicted with a similar accuracy (Rsuperscript 2 = 0.76 - 0.80) by the undegraded fraction after 24 h.

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