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HS005
Nutrient and microbial characteristics of mountain stream fine benthic organic matter in the H.J. Andrews Experimental Forest, 1995 to 1996

CREATOR(S): Robert P. Griffiths, Heather L. Bonin
PRINCIPAL INVESTIGATOR(S): Robert P. Griffiths
ORIGINATOR(S): Heather L. Bonin
OTHER RESEARCHER(S): Bruce A. Caldwell
DATA SET CONTACT PERSON: Robert P. Griffiths
ABSTRACTOR: Heather L. Bonin
METADATA CREATION DATE:
8 Apr 1999
MOST RECENT METADATA REVIEW DATE:
26 Sep 2013
KEYWORDS:
Organic matter, communities, stream ecology, timber harvest, organic matter, forest ecosystems, aquatic ecosystems, streams, microbes
PURPOSE:
The purpose of this study was to examine the fundamental relationship between FBOM nutrient availability, or substrate quality, and microdecomposer activity and to investigate the link between organic matter inputs and FBOM substrate quality. To this end, we compared the qualitative characteristics of FBOM from streams flowing through stands with riparian zones dominated by coniferous, deciduous (red alder) or herbaceous vegetation at two elevations for one year.
METHODS:
Experimental Design - HS005 :
Description: Streams were sampled for FBOM on 8 occasions: August 9, October 14, October 28, November 4, November 18 and December 9, 1995, and April 6 and May 12, 1996. As a way of integrating FBOM characteristics from small watersheds over larger spatial scales and longer time periods, sediments were also collected from the settling basins of 5 HJA experimental small watersheds.
Field Methods - HS005 :
Description:

Sample collection, preparation, and storage:

FBOM was collected from stream beds with a hand vacuum pump into a 2 L collecting jar. The intake line was fitted with a 1 mm stainless steel screen, allowing benthic material to be wet-sieved during sampling. Samples were transferred to polystyrene jars (500 ml) and stored during field sampling in an insulated chest with stream water and ice. In the laboratory, a slurry was prepared by decanting excess stream water from the jars and mixing, keeping FBOM suspended while subsampling. Subsamples were dispensed using 1, 3, or 5 ml plastic syringes with enlarged openings. All laboratory analyses involving slurry began immediately upon return from FBOM collection which took 8-12 hours.

Laboratory Methods - HS005:
Description:

Because of significant perturbation (e.g., suction, sieving, mixing, and preparing slurries) of FBOM during sampling and subsampling, we performed laboratory analyses described in the following sections to measure potential activity rates. These rates do not reflect in-stream FBOM activity rates, but rather give us a relative sense of the variability of rates among treatments and over time.

Denitrification potential rates

Denitrification potential was determined as N2O emission by anaerobically incubating FBOM supplemented with glucose and NaNO3 (Martin et al., 1988). Duplicate 5-ml slurry samples in 25-ml Erlenmeyer flasks were capped with rubber stoppers and purged for 3 min with argon at a rate of at least 120 cc /min. In the middle of the purge, the flasks were shaken gently to ensure removal of air bubbles. The flasks were allowed to incubate for 1 h at 24 degrees C, and then 2 ml of sterile solution of 1 mM glucose and 1 mM NaNO3 were injected through the stopper, and 2 ml of headspace gas were withdrawn with the syringe. Flasks were allowed to incubate for another hour at 24 degrees C. At zero and 2 h time, 0.5 ml of headspace gas was removed from the flasks and assayed for N2O in a gas chromatograph equipped with an electron capture detector. All gas chromatographs had stainless steel columns packed with Poropak-Q, either 50/80 or 80/100 mesh (Water Associates, Inc., Medford, MA).

Respiration rates

To determine respiration rates, duplicate 5-ml subsamples were placed in 25-ml Erlenmeyer flasks, and then capped with rubber stoppers. After incubating for 1 h at 24 degrees C, 0.5 ml of headspace gas was analyzed for CO2 in a gas chromatograph fitted with a thermal conductivity conductor. After incubating for an additional 2 h under the same conditions, a second headspace gas sample (0.5 ml) was collected and analyzed.

Acetylene reduction rates

Putative acetylene reduction rates were determined by the acetylene reduction method (Weaver and Danso, 1994). Samples were prepared in the same way as for denitrification potential, except that the headspace gas contained 1.5% O2, 12.5% acetylene, and 86% argon. After 24 h of incubation, 0.5 ml of headspace gas was removed and analyzed for ethylene in a gas chromatograph fitted with a flame ionization detector. A control was analyzed for ethylene production in the absence of acetylene.

Mineralizable nitrogen and extractable ammonium concentrations

For mineralizable nitrogen measurements, the microbial conversion of organic N to inorganic N in the form of NH4-N was measured by the "anaerobic" incubation method (Koeney, 1982). Duplicate 10-ml sediment subsamples were added to 50-ml screw-topped test tubes, which then were completely filled with deionized water (53 ml), capped, and incubated at 40 degrees C for 7 d. After incubation, subsamples were transferred to 25-ml Erlenmeyer flasks, and 53 ml of 4 M KCl and 0.4 ml of 10 M NaOH were added to each. The flasks were shaken for 1 h, and then analyzed with a selective ion electrode (Corning ammonium electrode, Medford, MA). Extractable ammonium concentrations were measured by adding 50 ml of 2 M KCl to duplicate 10-ml subsamples in 250-ml Erlenmeyer flasks. The flasks were capped, shaken while incubating for 1 h in the presence of 0.4 ml 10 M NaOH, and analyzed with a selective ion electrode to determine KCl-extractable ammonium concentration. Net mineralization was calculated as mineralizable N ( extractable ammonium to account for ammonium present prior to incubation.

Enzyme activities

Phosphatase activity was determined according to the spectrophotometric assay of Tabatabai and Bremner (1969) as modified by Zou et al. (1992) One ml of 50 mM p-nitrophenyl phosphate substrate was added to duplicate 1-ml subsamples containing suspended FBOM. The tubes were shaken and then placed, along with duplicate controls with no phosphatase substrate addition, in a 30 degrees C water bath for 1 h. After incubation, 1 ml of 50 mM Sigma 104 phosphatase substrate was added to the controls; reactions were stopped immediately with the addition of 2 ml 0.5 M NaOH and 0.5 ml 0.5 M CaCl2. The assay mixtures were centrifuged for 5 min at 500 x g. A 0.2-ml subsample of the supernatant was diluted with 1.8 ml deionized water, and the optical density was measured at 410 nm. A standard curve was prepared from 0.02 to 1.00 ?mol ml-1 p-nitrophenol. Enzyme activity was expressed as ?mol p-nitrophenol released gdw-1 h-1. The B-glucosidase activity assay required the same general procedure as was used for phosphatase activity, except that the substrate was 1 ml 10 mM p-nitrophenyl ?-D glucopyranoside, the incubation period was 2 h, and 2 ml 0.1 M tris[hydroxymethyl]aminomethane at pH 12.0, instead of 0.5 M NaOH, were added to terminate the reaction.

Total carbon and nitrogen

Total C and N were determined by dry combustion with a Carlo-Erba NA 1500 Series II high-temperature combustion furnace on oven-dried subsamples ground to pass through a 250-mm sieve.

SUPPLEMENTAL INFORMATION:

Hargrave, B.T. (1972) Aerobic decomposition of sediment and detritus as a function of particle surface area and organic content. Limnol. Oceanogr. 17, 583-596.

Keeney, D.R. (1982) Nitrogen-Availability indices. In: Methods of Soil Analysis, Part 2. Chemical and Microbiological Properties. 2nd Edition. Agronomy no. 9 (Ed. A.L. Page). American Society of Agronomy, Soil Science Society of America, Madison, pp. 711-733.

Martin, K., Parsons, L.L., Murray, R.E. and Smith, M.S. (1988) Dynamics of soil denitrifier populations: Relationships between enzyme activity, most-probable-number counts, and actual N gas loss. Appl. Environ. Microbiol. 54, 2711-2716.

Petersen, R.C., and K.W. Cummins. 1974. Leaf processing in a woodland stream. Freshwater Biology 4: 343-368.

Sinsabaugh, R.L., and A.E. Linkins. 1990. Enzymic and chemical analysis of particulate organic matter from a boreal river. Freshwater Biology 23: 301-309.

Sinsabaugh, R.L., and A.E. Linkins. 1993. Statistical modelling of litter decomposition from integrated cellulase activity. Ecology 74: 1594-1597 check p. #

Sinsabaugh, R.L, T.Weiland, and A.E. Linkins. 1992. Enzymic and molecular analysis of microbial communities associated with lotic particulate organic matter. Freshwater Biology 28:393-404.

Suberkropp, K. and M.J. Klug. 1976. Fungi and bacteria associated with leaves during processing in a woodland stream. Ecology 57:707-719.

Suberkropp, K., G.L. Godshalk, and M.K. Klug. 1976. Changes in the chemical composition of leaves during processing in a woodland stream. Ecology 57: 720-727.

Superkropp, K. and M.J. Klug. 1980. Maceration of deciduous leaf litter by aquatic hyphomycetes. Canadian Journal of Botany 58: 1025-1031.

Tabatabai, M.A. and Bremner, J.A. (1969) Use of p-nitrophenyl phosphate for assay of soil phosphatase activity. Soil Biol. Biochem. 1, 301-307.

Taylor, B.R., D. Parkinson, and W.F.J. Parsons. 1989. Nitrogen and lignin content as predictors of litter decay rates: a microcosm test. Ecology 70: 97-104.

Ward, G.M. 1984. Size distribution and lignin content of fine particulate organic matter (FPOM) from microbially processed leaves in an artificial stream. Verhandlungen der Internationalen Vereinigung für Theoretische und Angewandte Limnologie 22: 1893-1898.

Ward, G. M. 1986. Lignin and cellulose content of benthic fine particulate organic matter (FBOM) in Oregon Cascade Mountain Streams. Journal of the North American Benthological Society 5:127-139.

Ward, G. M., A.K. Ward, C.N. Dahm and N.G. Aumen. 1994. The origins, and interactions, of particulate and dissolved matter. Pages 45-74 in Roger S. Wotton, editor. The Biology of Particles in Aquatic Systems. CRC Press, Boca Raton, Florida, USA.

Weaver, R.W. and Danso, S.K.A. (1994) Dinitrogen fixation. In: Methods of Soil Analysis, Part 2. Microbiological and Biochemical Properties. 3rd Edition. Soil Science Society of America Book Series no. 5. Soil Science Society of America, Madison, pp. 1019-1045.

Zou, X., Binkley, D. and Doxtader, K.G. (1992) A new method for estimating gross phosphorus mineralization and immobilization rates in soils. Plant Soil 147, 243-250.

SITE DESCRIPTION:
FBOM samples were collected from 14 first-order streams flowing through forest in three successional age classes: three Douglas-fir (Pseudotsuga menziesii) stands approximately 10 years old (10YS), five 30 year old Douglas-fir stands (30YS) and six old-growth forest (OG) dominated by Douglas-fir and western hemlock (Tsuga heterophylla) in the H.J. Andrews Experimental Forest, in the Western Cascade Mountains of Oregon. Riparian vegetation of the 8 young stands was dominated by herbaceous plants (10YS) or deciduous trees (30YS), primarily alder (Alnus rubra) and maple (Acer macrophyllum, A. circinatum). No riparian vegetation buffers were left on harvested stands and all stands had been replanted with Douglas-fir seedlings. Streams at high (1220-1280 m) and low elevations (580-800 m) were selected. An effort was made to keep similar stand age x elevation plots on the same slope and aspect. FBOM was also collected at the settling basins at the bottom of HJA Water Sheds 1, 2, 3, 9 and 10.
TAXONOMIC SYSTEM:
None
GEOGRAPHIC EXTENT:
H.J. Andrews Experimental Forest
MEASUREMENT FREQUENCY:
seasonal
PROGRESS DESCRIPTION:
Complete
UPDATE FREQUENCY DESCRIPTION:
notPlanned
CURRENTNESS REFERENCE:
Ground condition