The effects of dissolved organic matter from a native and an invasive plant species on juvenile Daphnia survival and growth

2020 ◽  
Vol 42 (4) ◽  
pp. 453-456
Author(s):  
Keiko W Wilkins ◽  
Erin Overholt ◽  
Craig Williamson

Abstract Shifts in the composition of terrestrial plant communities could have significant effects on freshwater zooplankton due to changes in the quality of inputs of terrestrially derived dissolved organic matter (DOM). Leachate from native red maple (RM) and invasive Amur honeysuckle (AH) were used to explore the effects of DOM source on survival and growth of juvenile Daphnia ambigua. Prior research with both terrestrial and aquatic organisms indicates that AH-derived DOM has negative effects. Comparing bioassays in the presence and absence of algae with no additional DOM, RM- or AH-derived DOM, RM had stronger negative effects on both Daphnia survival and growth while AH only decreased growth. The negative effects seen in the presence and absence of algae provided evidence for both indirect and direct effects due to phytotoxicity and plant secondary compounds, respectively. DOM source may play a key role in regulating consumers in aquatic ecosystems.


2021 ◽  
pp. 108191
Author(s):  
Morgan Luce McLeod ◽  
Lorinda Bullington ◽  
Cory C. Cleveland ◽  
Johannes Rousk ◽  
Ylva Lekberg


2004 ◽  
Vol 1 (3) ◽  
pp. 197 ◽  
Author(s):  
Julia A. Howitt ◽  
Darren S. Baldwin ◽  
Gavin N. Rees ◽  
Barry T. Hart

Environmental Context. Iron oxides, as suspended minerals or as a colloidal phase, are common in Australian freshwater systems. Freshwater systems are also loaded with carbon-based substances, ‘dissolved organic matter’, but not all is biologically available as food to freshwater organisms. However, photochemical interactions between these iron oxides and dissolved organic matter provide a mechanism for biologically resistant carbon to re-enter the food web. Suspended iron oxides thus need to be considered in carbon cycles in aquatic ecosystems. Abstract. The photochemical degradation of dissolved organic matter (DOM) derived from the leaves of River Red Gum (Eucalyptus camaldulensis) was examined, with a particular focus on the photochemical generation of CO2, consumption of O2, and the effect of particulate iron minerals on these photochemical reactions. Solutions of leaf leachate were irradiated with ultraviolet and visible light in the presence and absence of amorphous iron oxides. Addition of fresh iron oxide was found to increase the rate of photodegradation of the organic matter by up to an order of magnitude compared to the reactions without added iron oxide. The ratio of CO2 produced to O2 consumed was ~1:1 in both the presence and absence of iron oxyhydroxide. The reactivity of the iron oxides was dependent on the preparation method and decreased with increased storage time. These results suggest that photochemical reactions on particle surfaces should be considered when examining carbon transformation in aquatic ecosystems, especially at sites with potential for the production of iron oxyhydroxides.



2009 ◽  
Vol 43 (23) ◽  
pp. 9044-9044 ◽  
Author(s):  
Thomas L. ter Laak ◽  
Martin A. ter Bekke ◽  
Joop L. M. Hermens


2016 ◽  
Vol 67 (9) ◽  
pp. 1313 ◽  
Author(s):  
Richard L. Miller ◽  
Matthew M. Brown ◽  
Ryan P. Mulligan

Rivers are major conduits for the transport of allochthonous dissolved organic matter (DOM) to the ocean in coupled land–coastal systems. DOM can regulate biogeochemical processes and affect water quality, depending on the concentration and quality of DOM. By using spectral parameters calculated from chromophoric dissolved organic matter (CDOM) ultraviolet-visible absorption spectra, along with dissolved organic carbon (DOC) concentrations, we examined the input and change in the amount and quality of DOM in surface waters of the lower Neuse River and upper–middle regions of the Neuse Estuary following a major rainfall (30cm in 1 day) associated with Hurricane Irene (2011). CDOM and DOC nearly tripled in the 3 days following the storm. Although a strong linear relationship was observed between DOC and CDOM absorption coefficient at 350nm (R2=0.85), a higher fraction of non-chromophoric DOC to CDOM was observed during the rising river discharge. The spectral slope at 275–295nm and the slope ratio (275–295:350–400nm) indicated a shift from higher to lower molecular-weight DOM as it transited through the estuary, probably as a result of photodegradation. The present study demonstrated the utility of using CDOM spectral parameters for examining the flux and transformation of DOM in coastal waters following major rain events.





2009 ◽  
Vol 56 (5) ◽  
pp. 672-685 ◽  
Author(s):  
Stuart J. Goldberg ◽  
Craig A. Carlson ◽  
Dennis A. Hansell ◽  
Norm B. Nelson ◽  
David A. Siegel


2016 ◽  
Vol 97 ◽  
pp. 370-380 ◽  
Author(s):  
Yanping Li ◽  
Li Zhang ◽  
Shengrui Wang ◽  
Haichao Zhao ◽  
Rui Zhang


2013 ◽  
Vol 98 (2) ◽  
pp. 931-943 ◽  
Author(s):  
Benjamin Horemans ◽  
Johanna Vandermaesen ◽  
Philip Breugelmans ◽  
Johan Hofkens ◽  
Erik Smolders ◽  
...  


1993 ◽  
Vol 12 (1) ◽  
pp. 167-176 ◽  
Author(s):  
Valerie A. Hodge ◽  
Gary T. Fan ◽  
Keith R. Solomon ◽  
Narinder K. Kaushik ◽  
Gary G. Leppard ◽  
...  


2016 ◽  
Author(s):  
Harshad Kulkarni ◽  
◽  
Natalie Mladenov ◽  
Debashis Chatterjee ◽  
Saugata Datta


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