Kinetic pathways for the anaerobic decomposition of <Emphasis Type="Italic">Ludwigia inclinata</Emphasis>

This study is aimed at using kinetic modeling to investigate the yield of mineralization products from anaerobic decomposition of the aquatic macrophyte Ludwigia inclinata. The initial hypothesis was that the decay of different fractions of detritus and the kinetics of gases productions are both positively correlated to temperature. The plants and water samples were collected from a tropical oxbow lake; the anaerobic decomposition was described using incubations maintained at controlled temperatures. The methane and carbon dioxide productions were determined daily by gas chromatography. The mass loss of detritus owing to leaching and chemical oxidation was also measured, with the results being used to develop a mathematical (kinetic) model considering the heterogeneity of the resource and three mineralization pathways: (i) oxidation of the labile particulate organic carbon; (ii) formation of dissolved organic carbon leached from the detritus, and subsequent oxidation of those compounds; and (iii) oxidation of refractory particulate organic carbon (RPOC). The temperature did not affect the leaching rate constant or the mineralization of labile and dissolved fractions. On the other hand, the mineralization of RPOC was improved with increasing temperatures. The yield of CO₂ formation was higher at 20.1°C and decreased with increasing temperatures. The methanogenesis was significantly affected by the temperature; it abbreviated the beginning of the process and increased the CH₄ yield. Conversely as hypothesized, the results suggest that the increase in temperature improved the decay rates of RPOC, but did not affect the leaching process and the subsequent leachate oxidation. Furthermore, the rising temperatures had positive correlation with methanogenesis and negative with CO₂ production. Handling editor: S. M. Thomaz     

Transformation of detritus by a European native and two invasive alien freshwater decapods

Invasive alien species have the potential to alter biodiversity and ecosystem processes. In freshwaters, detritus decomposition is a major ecosystem service but it remains uncertain whether invasive alien decapods process detritus differently to natives. This study examined leaf litter processing, and cascading effects on biofilms, by the European native white clawed crayfish (Austropotamobius pallipes) compared to two invasive alien decapod species: the American signal crayfish (Pacifastacus leniusculus) and the Chinese mitten crab (Eriocheir sinensis). Invasive alien decapods were responsible for higher leaf litter decomposition than the native. In comparison with native crayfish, invasive alien crab and crayfish showed higher rates of litter consumption, increased production of smaller leaf fragments, fine particulate organic matter (FPOM) and dissolved organic carbon. Nutrients (ammonia and soluble reactive phosphorous) derived from excretion (measured separately in the absence of biofilms) varied among decapod species, being lower for P. leniusculus. However, nutrient concentrations did not vary among species in the detritivory experiments with biofilm, implying nutrients were utilised for biofilm production and respiration as no differences in biomass were evident among decapod treatments. These results show invasive alien decapods have the potential to increase the magnitude of detrital processing to FPOM in rivers, but indirect impacts on primary producers due to nutrient release are uncertain based on this experimental context.     

Dynamics of phytoplankton detritus in a shallow,eutrophic lake (Lake Loosdrecht,The Netherlands)

A study was made of the mortality and aerobic decomposition of light- and phosphorus-limited cultures of Oscillatoria limnetica, a dominant phytoplankton species in shallow, eutrophic Lake Loosdrecht (The Netherlands). When placed in the dark at 20 °C, most cells died and lysed within twelve days. The labile organic matter was completely decomposed within three weeks. Absorbance spectra indicated that blue green algae may contributed significantly to the refractory dissolved substances in the lake. Refractory particulate matter constituted from 7 to 24% of the biomass of O. limnetica, depending on the growth rate before incubation in the dark. The decomposition rate of this fraction was 0.005 d^–1. On a basis of a steady-state model of the dynamics of phytoplankton detritus, the areal organic dry weight concentration of the detritus in the lake is ca. 60 g m^–2. This means the quantities of detritus in the seston and epipelon are about equal.     

Seasonal variation in stable C and N isotope ratios of the Rhone River inputs to the Mediterranean Sea (2004–2005)

The temporal variation in the stable carbon and nitrogen isotope ratios of particulate organic matter (POM) in the Rhone River was investigated on a monthly basis during a 2-year period (2004–2005). In spite of high month-to-month variation, interannually consistent seasonal trends appeared, with significantly lower δ¹³C (<?28.2‰) in spring than in the other seasons. In contrast, δ¹⁵N did not exhibit significant temporal variation. In spring and summer, high chlorophyll a and b concentrations were associated with low C/N values (<8) and a high percentage of organic carbon (%C) and organic nitrogen (%N), testifying to high development of autochthonous riverine phytoplankton (mainly diatoms and chlorophytes). In fall and winter, higher δ¹³C (>?27.2‰) and C/N (>8) values, and lower %C, %N, and chlorophylls concentrations indicated the predominance of allochthonous terrestrial detritus material in the river POM. The lower δ¹³C values recorded in spring–summer, when the phytoplankton biomass was high, were related to the lower carbon isotopic signatures of freshwater diatoms and chlorophytes compared to those of terrestrial plants. Overall, Rhone River POM was mainly composed of terrestrially derived material (90%), with autochthonous phytoplankton representing only 10% as a mean, in spite of a higher mean contribution of phytoplankton (27%) to river POM in summer.     

The utilization of organic matter in shallow marine sediments by an epibenthic deposit-feeding holothurian

The utilization of organic matter and constituent food items in shallow marine sediments by Parastichopus parvimensis (Clark), an epibenthic deposit-feeding holothurian, has been investigated.Organic matter ingested from sediments of varying organic content was used by P. parvimensis with 22 % efficiency. In experiments with ¹⁴C labelled food all microorganisms associated with both plant detritus and decomposed matter of animal origin were used with over 40 % efficiency. Species of fresh brown, red, green, and blue-green algae were not assimilated. Detritus derived from the brown alga Dictyopteris zonarioides (Farlow) was used with a low efficiency while detritus from red and green algae was not assimilated. These results indicate that P. parvimensis does not utilize the large energy reserve available as plant detritus in near shore bottom habitats off Santa Catalina Island before to its decomposition by bacteria and fungi.     

The diet of the spiny-cheek crayfish Orconectes limosus in the Czech Republic

The composition of the diet of the invasive spiny-cheek crayfish Orconectes limosus was studied using qualitative and quantitative analyses of stomach contents. A total of 368 specimens collected in 2003–2005 and 2008 in Czech localities were examined, predominantly from the Labe (Elbe) and Vltava River basins. Food components were compared for three size classes of crayfish and both sexes. The following conclusions were reached: (1) the spiny-cheek crayfish is an omnivorous species consuming plants, animals and detritus; (2) quantitatively, the main food component of O. limosus is detritus, while the plant component was second; (3) O. limosus may swallow whole food particles up to 4 mm in size, and the bodies of small animals may sometimes be found undamaged in their stomachs.     

Detritus as a potential food source for protozoans: utilization of fine particulate plant detritus by a heterotrophic flagellate, <Emphasis Type="Italic">Chilomonas paramecium</Emphasis>, and a ciliate, <Emphasis Type="Italic">Tetrahymena pyriformis</Emphasis>

We investigated the direct utilization of fine particulate detritus (dried and homogenized plant material in the size range of bacteria) as a food source for protozoans using axenic cultures of the cryptomonad, heterotrophic flagellate, Chilomonas paramecium, and the hymenostome ciliate, Tetrahymena pyriformis. When fed media containing only particulate detritus, these species revealed growth rates similar to those reported for field populations. The growth rates of Chilomonas fed exclusively particulate detritus were similar to those obtained on a bacterial diet. Considering the high percentage of detritus particles in the size range of bacteria in lakes, our results imply that direct utilization of detritus by protozoans may form an additional pathway of carbon in aquatic food webs that has generally been overlooked.     

Aspects of aerobic mineralization during spring in Lake Vechten with special reference to the 14C-labelling technique

Aerobic mineralization, i.e. seston respiration, microbial breakdown of detritus and microbial assimilation-dissimilation of photosynthetically derived D(issolved) O(rganic) C(arbon) was measured in concentrated samples from the pelagic zone of Lake Vechten. The samples were described by cell numbers of dominant algae prior to concentrating by centrifuge with continuous rotor. The concentrated samples were incubated in the laboratory at in situ temperature and a light intensity of 30 W · m^–2 for measuring primary production and photosynthetically derived DOC. After filtration the particulate fraction was incubated in unlabelled lake water far measuring respiratory production of DI¹⁴C. Portions of the same particulate fraction were sterilized and incubated in unlabelled sample concentrate for measuring microbial breakdown of detritus. The seston respiration amounted to 19–30% loss of the particulate fraction over 15–45 h. Microbial breakdown of detritus amounted to 28–40% loss of the particulate fraction over 24–168 h. In both cases P(articulate) O(rganic) ¹⁴C(arbon) was transformed to mainly DI¹⁴C. Microbial assimilation-dissimilatioh of photosynthetically derived DOC could not be measured reliably.     

Seasonal variation of nutrients,organic carbon,ATP, and microbial standing crops in a vertical profile of Pyramid Lake,Nevada

Previous studies of Pyramid Lake, Nevada, led to the hypothesis that detritus could be an important food source for zooplankton because abundance of palatable algal species did not seem to be enough to support the zooplankton community throughout the year. Furthermore, a large portion of the annual primary productivity was attributed to a nonpalatable blue-green alga, Nodularia spumigena. We felt this alga became important to the Pyramid Lake aquatic community upon death, as edible detritus and a source of new nitrogen. Changes in pelagic detritus concentrations and microbial standing crops were monitored to determine the availability of these potential foods. Epilimnetic particulate organic carbon (POC) was primarily living phytoplankton. During holomixis and following spring primary production, hypolimnetic POC was 60–97% detrital, but these profundal POC concentrations were low (ca 650 µg l^-1). Detritus-bacteria aggregates were observed only following the September cyanophyte bloom. Although pelagic detritus availability for zooplankton was low, bacterial populations were sufficient to be at least a supplemental food source. Bacteria numbers ranged from 0.50 10⁶ to 24.7 10⁶ ml^-1 and increased in response to photosynthetic peaks. Microbial diversity, contribution to POC, and particle association were notable after July. The percentage of living carbon (assessed with ATP measurements) attributable to bacteria was highest in late summer and fall hypolimnetic samples. Patterns of change in organic phosphorus and nitrogen, the presence of a nitrogen-fixing cyanophyte, the N:P ratio, and results of other research demonstrated that non-nitrogen-fixing algae of Pyramid Lake are limited by inorganic nitrogen. The importance of N. spumigena to the aquatic community appeared to be as a source of new nitrogen, rather than as a forage; its mineralization is critical for the growth of palatable diatoms and green algae following winter mixing.     

Direct uptake of detrital carbon by the deposit-feeding polychaete Euzonus mucronata (Treadwell)

Bacteria and other microbes colonizing detrital particles are assimilated efficiently by detritivores; in some cases the non-living detrital matter is relatively refractory. This comparison has led to the hypothesis that the bacterial component of detritus, rather than the non-living material, is the principal food resource of detritivores. This hypothesis was tested by feeding radiolabelled detritus to the deposit-feeding polychaete Euzonus mucronata (Treadwell), an abundant inhabitant of Pacific coastal sand beaches. The assimilation of carbon from sterile detritus at a concentration of 0.3 mg ash-free dry weight of detritus per g dry sand (0.03 % organic content) was sufficient to provide about one-half of the carbon requirements of E. mucronata. There was no significant difference in assimilation from chemically-extracted or water-extracted sterile detritus (representing relatively refractory and available material, respectively), or from the same materials after microbial colonization. Thus, the major source of carbon may have been the supposedly refractory component of the detritus. Despite a low estimated assimilation efficiency (0.76–1.72%), the carbon requirements of E. mucronata would be met entirely by direct assimilation of detrital carbon if only 10% of the total organic carbon in the sand is as available as the chemically-extracted detritus in this experiment. Low assimilation efficiency does not preclude the acquisition of nutritionally important quantities of carbon by direct assimilation from detritus.     

Summer drought disturbance on plant detritus decomposition processes in three River Tirso (Sardinia, Italy) sub-basins

Here, we study the variation patterns of detritus decomposition along a river continuum in a Mediterranean type river basin, and the influence of summer drought disturbance on this pattern. The study was carried out in three 4th order sub-basins (hereafter referred to as Assolo, Laconi and Olzai) of the river Tirso basin (Sardinia, ITALY), with one study site per stream order in each sub-basin (4 stream orders × 3 sub-basins = 12 study sites). The three sub-basins were selected according to their exposure to summer drought, Assolo being the most exposed and Laconi the least exposed. Reed (Phragmites australis (Cav.) Steudel) detritus decomposition was studied during the fall and spring periods, utilising the leaf packs technique with 3 sampling dates and 8 replicate packs per sample in each period. At all sites, the stream width was recorded fortnightly for one year. Overall, the reed leaf packs underwent rapid decomposition in the river Tirso basin (k=0.0193 d^?1), but very high variation was observed among leaf pack decomposition rates (C.V. = 112.7%). Seasons, sub-basins, and stream orders accounted for 88% of the total variance observed (Three Way ANOVA). The decomposition rate was significantly higher in spring than in fall, in the Laconi sub-basin than in the Olzai and Assolo sub-basins, and in 4th order streams than in 2nd and 3rd. Decomposition rates were also higher at relatively undisturbed sites than at the study sites exposed to complete summer desiccation (e.g., 2nd, 3rd, 4th in the Olzai sub-basin; 1st, 2nd, 3rd in the Assolo sub-basin). The strongest effects of summer drought disturbance occurred at the lowest order stream branches (i.e., 1st and 2nd order) suggesting that the resilience of detritus decomposition processes to the disturbance arising from Mediterranean type climates increases with stream order.     

Detrital traits affect substitutability of a range‐expanding foundation species across latitude

Climate‐driven range shifts of foundation species could alter ecosystem processes and community composition by providing different resources than resident foundation species. Along the US Atlantic coast, the northward expanding foundation species, black mangrove Avicennia germinans, is replacing the dominant salt marsh foundation species, marsh cordgrass Spartina alterniflora. These species have distinct detrital attributes that ostensibly provide different resources to epifauna. We experimentally examined how detritus of these species affects decomposition and community composition in different habitat contexts at regional and local scales. First, we manipulated detritus identity (Avicennia, Spartina) at 13 sites across a 5° latitudinal gradient spanning mangrove, mixed marsh‐mangrove and salt marsh habitats. Across latitude, we found that Avicennia detritus decomposed 2–4 times faster than Spartina detritus, suggesting that detrital turnover will increase with mangrove expansion. Epifaunal abundance and richness increased 2–7 times from south to north (mangrove to salt marsh) and were equivalent between Avicennia and Spartina detritus except for crabs, a dominant taxonomic group that preferred Spartina detritus. Second, to examine the whether changing habitat context affected regional patterns, we manipulated detritus identity and surrounding habitat type (mangrove, salt marsh) at a single mixed site, also including inert mimics to separate structural and nutritional roles of detritus. Epifaunal richness was similar between the two detrital types, but crabs were 2–7 times more abundant in Spartina detritus due to its structural attributes. Surrounding habitat type did not influence decomposition rate or community patterns, which suggests that latitudinal influences, not surrounding habitat, drove the regional community patterns in the first experiment. Overall, mangrove expansion could alter epifaunal communities due to the lower structural value and faster turnover of mangrove detritus. As species shift with changing climate, understanding foundation species substitutability is critical to predict community change, but we must account for concomitant environmental changes that also modify communities.     

An ant–plant mutualism induces shifts in the protist community structure of a tank-bromeliad

Although ants may induce community-wide effects via changes in physical habitats in terrestrial environments, their influence on aquatic communities living in plant-held waters remains largely underexplored. The neotropical tank-bromeliad Aechmea mertensii (Bromeliaceae) occurs along forest edges in ant-gardens initiated by Camponotus femoratus or by Pachycondyla goeldii. Its leaves form wells that hold rainwater and provide suitable habitats for many aquatic organisms. We postulated that these ant–plant mutualisms indirectly affect the microbial community structure via changes in the environmental conditions experienced by the plants. To test this hypothesis, we analyzed the protist communities from 63 tank-bromeliads associated with either C. femoratus or P. goeldii (hereafter Cf-Aechmea and Pg-Aechmea) along a forest edge in French Guiana. For each plant, a large number of environmental variables (including habitat structure, food resources, incident radiation and the presence of aquatic invertebrates) were quantified to determine their relative importance in driving any observed differences across ant-associated plants. Pg-Aechmea are located in sun-exposed areas and hold low volumes of water and low amounts of detritus, whereas Cf-Aechmea are located in partially shaded areas and accumulate higher amounts of water and detritus. Protists (i.e., protozoa and algae) inhabiting Cf-Aechmea exhibit greater richness and abundances than those in Pg-Aechmea. Variations in detritus content, number of leaves, incident radiation, and the epiphyte richness of the ant-garden were the main factors explaining the variation in protist richness. A shift in the functional group composition of protists between bromeliads tended by different ant species suggested that mutualistic ants indirectly mediate changes in the microbial food web.     

Decomposition of Blue-Green Algal (Cyanobacterial) Blooms in Lake Mendota, Wisconsin

Decomposition of natural populations of Lake Mendota phytoplankton dominated by blue-green algae (cyanobacteria) was monitored by using oxygen uptake and disappearance of chlorophyll, algal volume (fluorescence microscopy), particulate protein, particulate organic carbon, and photosynthetic ability (¹⁴CO₂ up-take). In some experiments, decomposition of ¹⁴C-labeled axenic cultures of Anabaena sp. was also measured. In addition to decomposition, mineralization of inorganic nitrogen and phosphorus were followed in some experiments. Decomposition could be described as a first-order process, and the rate of decomposition was similar to that found by others using pure cultures of eucaryotic algae. Nitrogen and phosphorus never limited the decomposition process, even when the lake water was severely limited in soluble forms of these nutrients. This suggests that the bacteria responsible for decomposition can obtain all of their key nutrients for growth from the blue-green algal cells. Filtration of lake water through plankton netting that removed up to 90% of the algal biomass usually did not cause a similar decrease in oxygen demand, suggesting that most of the particulate organic matter used for respiration of the decomposing bacteria was in a small-particle fraction. Short-term oxygen demand correlated well with the particulate chlorophyll concentration of the sample, and a relationship was derived that could be used to predict community respiration of the lake from chlorophyll concentration. Kinetic analysis showed that not all analyzed components disappeared at the same rate during the decomposition process. The relative rates of decrease of the measured parameters were as follows: photosynthetic ability > algal volume > particulate chlorophyll > particulate protein. Decomposition of ¹⁴C-labeled Anabaena occurred at similar rates with aerobic epilimnetic water and with anaerobic sediment, but was considerably slower with anaerobic hypolimnetic water. Of the various genera present in the lake, Aphanizomenon and Anabaena were more sensitive to decomposition than was Microcystis. In addition to providing a general picture of the decomposition process, the present work relates to other work on sedimentation to provide a detailed picture of the fate of blue-green algal biomass in a eutrophic lake ecosystem.     

A mesocosm study of aerobic mineralization of seven aquatic macrophytes

Decomposition experiments were performed using the closed bottles method and seven aquatic macrophytes: Cabombafurcata, Cyperusgiganteus, Egerianajas, Eichhorniaazurea, Salviniaauriculata, Oxycaryumcubense and Utriculariabreviscapa. Cultures with lagoon water and macrophytes detritus were incubated at 20 °C under aerobic conditions. Total particulate and dissolved organic carbon and dissolved oxygen concentrations were analyzed. The major findings were: (i) the maximum amount of consumed oxygen (OC_MAX) and deoxigenation rates (k_d) differ among macrophyte decays (OC_MAX: 165–700 mg g⁻¹ DW; k_d: 0.014–0.045 d⁻¹); these differences depends mainly on molecular and elemental composition of detritus; in short period, the cytoplasm fraction of detritus enhanced the catabolic activity; (ii) the kinetic model adopted to describe the oxygen consumption was shown appropriate; the parameter more affected by the chemical differences of detritus was OC_MAX; the constant rates of oxygen consumption (k_d) were relatively smaller in relation to obtained to oxidative decarboxylation processes (ca. 6 times) and presented minimum changes if compared with the detritus variations.     

Small-scale burial of macroalgal detritus in marine sediments: Effects of Ulva spp. on the spatial distribution of macrofauna assemblages

Patches of dead seaweeds can deposit, bury, and age into the sediment. Decomposition and release of algal-derived nutrients can influence patterns of distribution of benthic organisms. Here, I investigated how small-scale burial of Ulva spp. affected spatial variation of macrofauna in intertidal sediment. I deliberately buried Ulva detritus under the surface of 50 × 50 cm² patches of sediment in three intertidal flats of the Oosterschelde estuary (The Netherlands). Results showed that there was no accumulation of particulate organic carbon and nitrogen in the sediment at the scales examined. The biomass of microphytobenthos did not show any change and there was evidence that grazing was important all over the study area. Burial did not alter composition and diversity of macrofauna, but some animals (Corophium volutator, Eteone spp. and Scoloplos armiger) had less numbers in the plots where detritus was buried than in the controls. These findings showed that burial of macroalgal detritus does not represent a major source of variation at the scales examined. It is suggested that in these sediments, recycling of detritus is fast and it buffers the effects of excess organic matter in the system.     

Density of red alder (Alnus rubra) in headwaters influences invertebrate and detritus subsidies to downstream fish habitats in Alaska

We investigated the influence of red alder (Alnus rubra) stand density in upland, riparian forests on invertebrate and detritus transport from fishless headwater streams to downstream, salmonid habitats in southeastern Alaska. Red alder commonly regenerates after soil disturbance (such as from natural landsliding or timber harvesting), and is common along streams in varying densities, but its effect on food delivery from headwater channels to downstream salmonid habitats is not clear. Fluvial transport of invertebrates and detritus was measured at 13 sites in spring, summer and fall during two years (2000–2001). The 13 streams encompassed a riparian red alder density gradient (1–82% canopy cover or 0–53% basal area) growing amongst young-growth conifer (45-yr-old stands that regenerated after forest clearcutting). Sites with more riparian red alder exported significantly more invertebrates than did sites with little alder (mean range across 1–82% alder gradient was about 1–4 invertebrates m^?3 water, and 0.1–1 mg invertebrates m^?3 water, respectively). Three-quarters of the invertebrates were of aquatic origin; the remainder was of terrestrial origin. Aquatic taxa were positively related to the alder density gradient, while terrestrially-derived taxa were not. Streams with more riparian alder also exported significantly more detritus than streams with less alder (mean range across 1–82% alder gradient was 0.01–0.06 g detritus m^?3 water). Based on these data, we predict that headwater streams with more riparian alder will provide more invertebrates and support more downstream fish biomass than those basins with little or no riparian alder, provided these downstream food webs fully utilize this resource subsidy.     

Nutritional value of detritus and algae in blenny territories on the Great Barrier Reef

The salariin blenny, Salarias patzneri, primarily ingests detrital aggregates and inorganic sediment, with small quantities of filamentous algae. Samples of particulate matter <125 μm and filamentous algae were collected from the territories of S. patzneri and the nutritional value of these resources assessed using organic content and protein/energy ratios calculated from protein, carbohydrate and lipid content. Samples were collected throughout the day, during both summer and winter, to enable temporal comparisons of nutritional value. The particulates <125 μm, which were predominantly amorphic detritus, accounted for 41±2% and 44±3% of the organic matter in the epilithic algal matrix (EAM) during the summer and winter, respectively, whilst filamentous algae accounted for 37±3% and 41±3% of the organic matter in the summer and winter, respectively. Carbohydrate and lipid concentration in the algal samples was significantly greater than in particulate matter <125 μm, although no significant difference was detected in protein levels of algal samples and particulates <125 μm. Consequently, the protein/energy ratio of particulates <125 μm in the summer (11±1 mg kJ⁻¹) and winter (10±1 mg kJ⁻¹) was similar to that of filamentous algae in the summer (9±1 mg kJ⁻¹) and winter (8±1 mg kJ⁻¹). These results suggest detrital aggregates are at least comparable to filamentous algae as a nutritional resource. The large contribution of high quality detritus to organic matter in the epilithic algal matrix collected from S. patzneri territories throughout the day and between seasons provides strong evidence that detritus is a valuable component of small territorial fish diets and is an integral part of coral reef food webs.     

Assessment of particulate organic matter in river water

Particulate organic matter in a downriver riffle of the Grand River, the largest Canadian Great Lakes tributary, was studied between June 1970 and April 1972. In winter and spring, concentrations of particulate organic matter (1.0–26.2 mg/l) varied with river flow. High summer levels (3.4–12.7 mg/l) were attributable to high autochthonous primary production. Mean chlorophyll a concentration in summer (29.8 mg/m³) was nearly 15 times higher than in winter, and 8 times the spring mean level. High algal cell counts (15,000–19,000 cells/l) also occurred in summer. Autochthonous and allochthonous contributions to the total particulate organic carbon input to the river in summer were estimated by daily organic input and river flow relationships, carbon to chlorophyll a and to pheopigments ratios. The allochthonous source accounted for 21.5% of the total organic carbon while the autochthonous contributed the remaining 78.5%. The latter included living algae (23.0%), senescent plant material (30.3%) and detritus (25.2% — including microbes). The study establishes a new approach whereby the various components of particulate organic matter in river water can be indirectly partitioned and their biomass estimated by using quantitative relationships among readily obtainable parameters of river flow, standing biomass, chlorophyll a and pheopigments.