Organic matter chemistry and dynamics in clear-cut and unmanaged hardwood forest ecosystems

Forest harvesting alters the organic matter cycle by changing litter inputs and the decomposition regime. We hypothesized that these changes would result in differences in organic matter chemistry between clear-cut and uncut watershed ecosystems. We studied the chemistry of soil organic matter (SOM), and dissolved organic carbon (DOC) in soil solutions and stream samples in clear-cut and uncut sites at the Hubbard Brook Experimental Forest in New Hampshire using DOC fractionation techniques and solid-state ¹³C nuclear magnetic resonance (NMR) spectroscopy.Alkyl-C (aliphatic compounds) and O-alkyl-C (carbohydrates) were the largest C fractions in soil and dissolved organic matter at Hubbard Brook. Alkyl-C ranged from 29–48% of soil C, 25–42% of soil solution C, and 22–42% of streamwater DOC. Carbohydrates comprised 32–49%, 36–43%, and 29–60% of C in soils, solutions, and streamwater, respectively. In both soils and soil solutions, the carbohydrate fraction decreased with increasing soil depth, while the aromaticity of organic matter increased with depth. There were no significant differences in the structural chemistry of SOM between clear-cut and uncut watersheds.The aromatic-C fractions in soil solutions at the clear-cut site ranged from 12–16%, approximately 40% greater than at the uncut site (8.5–11%). Thus, clear-cutting has resulted in the leaching of more highly decomposed organic matter, and depletion of more aliphatic compounds in the soluble organic pool. Because DOC fluxes are small compared to the SOM pool, large differences in soil solution chemistry do not substantially alter the overall composition of SOM. While the organic chemistry of stream DOC varied greatly among 3 sampling dates, there were no obvious clear-cutting effects. Thus, temporal variations in flowpaths and/or in-stream processes appear to be more important than disturbance in regulating the organic carbon chemistry of these streams.     

Effects of soil freezing disturbance on soil solution nitrogen, phosphorus, and carbon chemistry in a northern hardwood ecosystem

Reductions in snow cover undera warmer climate may cause soil freezing eventsto become more common in northern temperateecosystems. In this experiment, snow cover wasmanipulated to simulate the late development ofsnowpack and to induce soil freezing. Thismanipulation was used to examine the effects ofsoil freezing disturbance on soil solutionnitrogen (N), phosphorus (P), and carbon (C)chemistry in four experimental stands (twosugar maple and two yellow birch) at theHubbard Brook Experimental Forest (HBEF) in theWhite Mountains of New Hampshire. Soilfreezing enhanced soil solution Nconcentrations and transport from the forestfloor. Nitrate (NO₃ ^–) was thedominant N species mobilized in the forestfloor of sugar maple stands after soilfreezing, while ammonium (NH₄ ⁺) anddissolved organic nitrogen (DON) were thedominant forms of N leaching from the forestfloor of treated yellow birch stands. Rates ofN leaching at stands subjected to soil freezingranged from 490 to 4,600 mol ha^–1yr^–1, significant in comparison to wet Ndeposition (530 mol ha^–1 yr^–1) andstream NO₃ ^– export (25 mol ha^–1yr^–1) in this northern forest ecosystem. Soil solution fluxes of P_i from the forestfloor of sugar maple stands after soil freezingranged from 15 to 32 mol ha^–1 yr^–1;this elevated mobilization of P_i coincidedwith heightened NO₃ ^– leaching. Elevated leaching of P_i from the forestfloor was coupled with enhanced retention ofP_i in the mineral soil Bs horizon. Thequantities of P_i mobilized from the forestfloor were significant relative to theavailable P pool (22 mol ha^–1) as well asnet P mineralization rates in the forest floor(180 mol ha^–1 yr^–1). Increased fineroot mortality was likely an important sourceof mobile N and P_i from the forest floor,but other factors (decreased N and P uptake byroots and increased physical disruption of soilaggregates) may also have contributed to theenhanced leaching of nutrients. Microbialmortality did not contribute to the acceleratedN and P leaching after soil freezing. Resultssuggest that soil freezing events may increaserates of N and P loss, with potential effectson soil N and P availability, ecosystemproductivity, as well as surface wateracidification and eutrophication.     

How does photorespiration modulate leaf amino acid contents? A dual approach through modelling and metabolite analysis

The aim of this work was to establish the quantitative impact of photorespiration on leaf amino acid contents. Attached leaves of wheat and potato were incubated for 30–40 min under defined conditions in which net CO₂ uptake (A) was manipulated by irradiance, ambient CO₂ or ambient O₂. The incubated portion of the leaf was sampled by a rapid‐quench method and photorespiratory flux (v_o) was modelled from the measured rate of net CO₂ uptake. In both wheat and potato, the ratio between glycine and serine showed a strong positive correlation with v_o. Aspartate and alanine correlated negatively with v_o but glutamate and glutamine showed less clear relationships. In potato, glutamate and glutamine did not correlate clearly with either A or v_o. In wheat, glutamine showed a general increase with A but no relationship with v_o, whereas 2‐oxoglutarate contents correlated positively with v_o and negatively with A. As a result, glutamine : glutamate and glutamine : 2‐oxoglutarate increased with net CO₂ uptake in wheat, observations that are attributed primarily to imperfect and variable coupling between the supply of NH₃ in primary nitrogen assimilation and the associated delivery of 2‐oxoglutarate to the chloroplast. A simple theoretical analysis is used to illustrate the potentially marked impact of primary nitrogen assimilation on leaf glutamine, even against a background of high rates of photorespiratory ammonia recycling.     

An Evaluation of Sources of Uncertainty in a Dredged Material Assessment

The U.S. Army Corps of Engineers and the U.S. Environmental Protection Agency use a four tiered evaluation process to assess the potential for significant impacts from open water disposal of dredged material to the aquatic environment. This tiered approach requires only the appropriate level of analysis to estimate potential chemical and biological effects. Uncertainty is inherent in each tier and can lead to delayed, costly, and potentially inappropriate decisions. This paper discusses sources of uncertainty in the tiered approach with the goal of improving dredged material management decisions. These potential uncertainty sources are common to many dredging projects but might not be applicable to all projects. Although not all uncertainty sources can be quantified, even using the simple scoring procedure described here, they can still contribute significantly to uncertainty in predictions of adverse effects. Of the sources that could be scored and ranked, those identified as most uncertain include trophic transfer, chronic bioassay interpretation, fate and transport model parameter uncertainty, toxicity endpoints based on body burdens, human dose-response models, toxicity of complex mixtures, and estimation of population-level effects. Research directed at these sources of uncertainty will result in improved decision making.     

Extent of invasion of Tasmanian native vegetation by the exotic bumblebee Bombus terrestris (Apoidea: Apidae)

Abstract Observations of the large earth bumblebee, Bombus terrestris (L.), in native vegetation were collated to determine the extent to which this exotic species has invaded Tasmanian native vegetation during the first 9 years after its introduction. The range of B. terrestris now encompasses all of Tasmania's major vegetation types, altitudes from sea level to 1260m a.s.L, and the entire breadth of annual precipitation in the state from more than 3200 mm to less than 600 mm. Observations of workers carrying pollen, together with the presence of large numbers of bumblebees at many localities across this range indicate that colonies are frequently established in native vegetation. Evidence that colonies are often successful was obtained from repeated observations of the species during more than 1 year at particular sites. Unequivocal evidence of colonies was obtained from six National Parks, including four of the five in the Tasmanian Wilderness World Heritage Area (WHA). Indeed, the species has been present in the WHA for at least as long as it has in the city of Hobart, where it was first recorded. In southwestern Tasmania, evidence of colonies was obtained up to 40km from gardens, 61 km from small towns and 93 km from large towns. Hence, contrary to previous suggestions, the species is established in the most remote parts of Tasmania and is not dependent on introduced garden plants. Given their strong record of invasion, it is likely that B. terrestris will form feral populations on the mainland of Australia and in many other parts of the world if introduced. Because of their likely negative impacts on native animals and plants, and potential to enhance seed production in weeds, the spread of bumblebees should be avoided.     

Molecular cloning and immunological characterization of porcine kidney ferredoxin.

Porcine renodoxon is a kidney mitochondrial iron-sulfur protein (ISP) that functions to transfer electron to cytochromes P450 of the vitamin D pathway. A full-length cDNA clone to porcine renodoxin was isolated in the current investigation and used to study the protein's primary structure and immunological properties. The cysteine ligands for the iron-sulfur center, and the surface protein-binding and phosphorylation sites occupied identical positions in both porcine renodoxin and bovine adrenodoxin. Furthermore, porcine renodoxin was functionally indistinguishable from bovine adrenodoxin and the mature forms of both proteins had the same encoded length and shared approximately 91% sequence similarity. A synthetic peptide to the surface protein-binding region was used to demonstrate the antigenicity of the domain in both the porcine and the bovine ISPs. However, porcine renodoxin displayed only limited immunological identity to other regions of bovine adrenodoxin as measured by competitive enzyme-linked immunosorbent assay. Part of this immunological distinction was attributed to the COOH-terminal processing of porcine renodoxin, an action which negated expression of a COOH-terminal antigenic site that is present in bovine adrenodoxin. Other antigenic differences were linked to charged-residue substitutions that were located in predicted surface domains. The highest frequency of surface-residue substitutions in ferredoxin proteins was predicted for porcine renodoxin, which could provide a basis for understanding why the pig protein appears more antigenically divergent than other ferredoxins.     

Genbank accession #: AF111812

Plant Molecular Biology -     

Contents Volume 11 1990

Contents Volume 11 1990