Human Decomposition Ecology

Total Page:16

File Type:pdf, Size:1020Kb

Human Decomposition Ecology Organisms and their environment, including other organisms Ecology investigates: Resource colonization Resource decomposition and distribution Competition Succession Reproduction and development Production 6CO2 + 6H20 C6H1206 + 6O2 Decomposition C6H1206 + 6O2 6CO2 + 6H20 Energy = carbon (C) Ultimately measured in kilocalories/calories Nutrients = nitrogen (N) phosphorus (P) potassium (K) magnesium (Mg) Several other elements and compounds Autotroph Heterotroph zymogenous Acquires energy through autochthonous photosynthesis Acquires energy through Plants, algae eating Humans, mammals, birds, bacteria, fungi, insects, etc. Can be viewed from two perspectives: 1. Taxonomy: what is doing the decomposing? 2. Taphonomy: what processes are taking place? Most decomposition is biologically mediated (minimum 80%) Microorganisms (bacteria, fungi) Insects (flies, beetles) Scavengers Catalysis—enzymatic and chemical reactions transforming complex to simple. Comminution—physical breakdown of resource. Leaching—soluble material moved by water Resource Quality Decomposer Physicochemical Community environment Physicochemical Environment Four primary modulators of decomposition: Moisture Temperature Aeration (oxygen, carbon dioxide) pH A high quality carbon:nitrogen resource Wood 145:1 Straw 100:1 An ephemeral Leaf litter 50:1 resource Manure 25:1 patch/disturbance A source of water A habitat for microorganisms Stages of Decomposition In reality: 1. Fresh Stages do not exist 2. Bloated Stage 3. Active Decay characteristics can 4. Advanced Decay blend from one stage into another 5. Skeleton Stages provide a convenient means for taphonomists to assess decomposition • Autolysis starts: abiotic breakdown of cells and tissues • Associated with start of mortis triad • Little release of fluids and disturbance of surroundings • Flies first colonize: looking for place to lay eggs. • If too cold: microbes and scavengers dominate • If outside: vegetation and soil surface covered. The mortis triad Algor mortis—body temperature changes to ambient temperature Rigor mortis—temporary stiffening of the joints Livor mortis—settling and pooling of blood; blood will become “fixed” after a period of time. Gunn (2009) Gunn (2009) Fresh Stage (biological changes) Initial insect colonization (response to chemical disturbance, i.e. presence of corpse) Release of ammonia, sulphuric acid, carbon dioxide, nitrogen Increased microbial activity (response to physical disturbance) Initial shift in bacterial and fungal community structure (response to physical disturbance) Fresh Stage (chemical changes) • Increase in Increase in gravesoil atmospheric + • ammonium (NH4 ) • carbon dioxide - • nitrate (NO3 ) (CO ) 2 • phosphorus (P) • methane (CH ) 4 • soil pH • hydrogen sulfide (H2S) • nitrogen (N2) • ammonia (NH3) Bloat Stage Decomposition • Enteric microbial community produces gases (putrefaction) • Purge fluids released from orifices: mouth, nose, anus, etc. • Buildup of gas can cause rupturing, fluids released from ruptures in skin. • Fly larvae (maggots) are active Gunn (2009) Bloated (biological changes) Maggot activity Elevated microbial activity (CO2 respiration) Shift in bacterial community structure Bloated (chemical changes) Increased in gravesoil: ammonium calcium chloride fatty acids (butyric, propionic, valeric) magnesium organic N, ammonium, nitrate phosphorus potassium sodium sulphate Active Decay • Maggot activity at its peak • Increased release of fluids • Increased marbling, slippage of skin • Exposure of internal organs Active Decay (biological changes) Peak insect activity Death of associated vegetation (not sure why) Elevated microbial activity Shift in bacterial community structure Active Decay (chemical changes) Same elevated concentrations as observed in the bloated stage. Increased: Lipid phosphorus Enzyme activity Protease activity Phosphodiesterase activity Total nitrogen Total phosphorus Advanced Decay (biological changes) Maggots have migrated. Corpse comprises skin, organs, hair and bone. Declining microbial biomass and activity, but still greater than non-gravesoil. Fruiting of postputrefaction fungi. Shift in bacterial community structure. Advanced Decay (chemical changes) Same as observed during bloated and active decay. Postputrefaction fungus Skeleton Stage Decomposition • Can persist from weeks to millenia • Materials present: bone, teeth, hair, dried skin Gunn (2009) Gunn (2009) Time Advanced Fresh Bloated Active Decay Skeleton Decay •Declining •Increased •Initial microbial microbial disturbance •Increased •Increased activity and activity, •Increased microbial microbial biomass biomass microbial activity, activity •early phase •Succession of Gravesoil activity biomass •Shift in postputrefactio fungi from early •Shift in •Shift in Biology bacterial n fungi phase to late bacterial and bacterial community •Shift in phase fungal community structure bacterial •Shift in community structure community bacterial structure structure community •Increased ammonium, butyric acid, •See Bloated calcium, •See Bloated •Increased •Increased chloride, •Increased lipid ammonium, •Initial amino acids, magnesium, phosphorus, electrical disturbance nitrate, ninhydrin- protease conductivity, •Increased ninhydrin- Gravesoil reactive N, activity, ninhydrin- ammonium, reactive nitrate, phosphodiester reactive Chemistry carbon dioxide, nitrogen, total potassium, ase activity, nitrogen, lipid nitrate, nitrogen, total phosphate, total nitrogen, phosphorus, phosphate phosphorus propionic acid, total total nitrogen, •Decreased pH sodium, phosphorus total sulphate, phosphorus valeric acid •Increased pH Gunn A (2009) Essential Forensic Biology. Wiley- Blackwell. Hopkins DW (2008) The role of soil organisms in terrestrial decomposition. In: Tibbett M, Carter DO; Soil Analysis in Forensic Taphonomy. CRC Press: 53-66..
Recommended publications
  • Forensic Medicine
    YEREVAN STATE MEDICAL UNIVERSITY AFTER M. HERATSI DEPARTMENT OF Sh. Vardanyan K. Avagyan S. Hakobyan FORENSIC MEDICINE Handout for foreign students YEREVAN 2007 This handbook is adopted by the Methodical Council of Foreign Students of the University DEATH AND ITS CAUSES Thanatology deals with death in all its aspects. Death is of two types: (1) somatic, systemic or clinical, and (2) molecular or cellular. Somatic Death: It is the complete and irreversible stoppage of the circulation, respiration and brain functions, but there is no legal definition of death. THE MOMENT OF DEATH: Historically (medically and legally), the concept of death was that of "heart and respiration death", i.e. stoppage of spontaneous heart and breathing functions. Heart-lung bypass machines, mechanical respirators, and other devices, however have changed this medically in favor of a new concept "brain death", that is, irreversible loss of Cerebral function. Brain death is of three types: (1) Cortical or cerebral death with an intact brain stem. This produces a vegetative state in which respiration continues, but there is total loss of power of perception by the senses. This state of deep coma can be produced by cerebral hypoxia, toxic conditions or widespread brain injury. (2) Brain stem death, where the cerebrum may be intact, though cut off functionally by the stem lesion. The loss of the vital centers that control respiration, and of the ascending reticular activating system that sustains consciousness, cause the victim to be irreversibly comatose and incapable of spontaneous breathing. This can be produced by raised intracranial pressure, cerebral oedema, intracranial haemorrhage, etc.(3) Whole brain death (combination of 1 and 2).
    [Show full text]
  • Terrestrial Decomposition
    Terrestrial Decomposition • Objectives – Controls over decomposition • Litter breakdown • Soil organic matter formation and dynamics – Carbon balance of ecosystems • Soil carbon storage 1 Overview • In terrestrial ecosystems, soils (organic horizon + mineral soil) > C than in vegetation and atmosphere combined 2 Overview • Decomposition is: 1. Major pathway for C loss from ecosystems 2. Central to ecosystem C loss and storage 3 Overview 4 Incorporation 1 year later Overview • Predominant controls on litter decomposition are fairly well constrained 1. Temperature and moisture 2. Litter quality • N availability • Lignin concentration • Lignin:N • Mechanisms for soil organic matter stabilization: 1. Recalcitrance (refers to chemistry) 2. Physical protection • Within soil aggregates • Organo-mineral associations 3. Substrate supply regulation (energetic limitation) 5 Overview • Disturbance can override millenia in a matter of days or years: 1. Land use change 2. Invasive species 3. Climate change • Understanding the mechanistic drivers of decomposition, soil organic matter formation, and carbon stabilization help us make management decisions, take mitigation steps, and protect resources. 6 Overview Native Ōhiʻa - Koa forest Conversion to Reforestation in grass-dominated pasture (80 yr) Eucalyptus plantation (10 yr) Conventional sugar cane harvest. 20° C 18° C 16° C 14° C 7 Sustainable ratoon harvest. Decomposition • Decomposition is the biological, physical and chemical breakdown of organic material – Provides energy for microbial growth
    [Show full text]
  • Death & Decomposition Part II
    Death & Decomposition Part II Review: Why is TSD/PMI so important? Review: What happens in the Fresh (1st) Stage of Decomposition? STAGE 2: Bloat ⦿ 0-10 days ⦿ Putrefaction: bacterially-induced destruction of soft tissue and gas formation › Skin blisters and marbling › Build-up of fluids from ruptured cells and intestines Putrefaction – the gross stuff ➢ Decomposition that occurs as a result of bacteria and other microorganisms ➢ Results in gradual dissolution of solid tissue into gases and liquids, and salts Putrefaction ➢ Characteristics: ○ Greenish discoloration ○ Darkening of the face ○ Bloating and formation of liquid or gas-filled blisters ○ Skin slippage Putrefaction ➢ Begins about 36 hours after death ➢ Further destruction is caused by maggots and insects ➢ Above 40 F, insects will feed until the body is skeletonized Influences of Putrefaction ➢ Heavy clothing and other coverings speed up the process by holding in body heat ➢ Injuries to the body surface promote putrefaction ○ provide portals of entry for bacteria Marbling Stage 3: Active Decay ➢ 10-20 days after death ➢ Body begins to collapse and black surfaces are exposed ➢ Bloated body collapses and leaves a flattened body ➢ Body fluids drain from body Active Decay Active Decay: Destruction of Tissue • Severe decomp can result in complete destruction of soft tissue Active Decay: Advanced Decomposition Stage 4: Dry Decay ➢ 20-365 days after death ➢ Remaining flesh on body is removed and body dries out ➢ Body is dry and continues to decay very slowly due to lack of moisture ➢
    [Show full text]
  • Plant Species Effects on Nutrient Cycling: Revisiting Litter Feedbacks
    Review Plant species effects on nutrient cycling: revisiting litter feedbacks Sarah E. Hobbie Department of Ecology, Evolution and Behavior, University of Minnesota, St. Paul, MN 55108, USA In a review published over two decades ago I asserted reinforce those gradients and patterns of NPP, focusing that, along soil fertility gradients, plant traits change in on feedbacks operating through plant litter decomposition. ways that reinforce patterns of soil fertility and net Specifically, I evaluate two key assumptions underlying primary productivity (NPP). I reevaluate this assertion the plant litter feedback idea: (i) plant litter traits vary in light of recent research, focusing on feedbacks to NPP predictably along fertility gradients, and (ii) such variation operating through litter decomposition. I conclude that reinforces soil fertility gradients through effects on decom- mechanisms emerging since my previous review might position and litter N release. Given the number of synthetic weaken these positive feedbacks, such as negative cross-site analyses of plant traits and their consequences effects of nitrogen on decomposition, while others for nutrient cycling over the past two decades, the time is might strengthen them, such as slower decomposition ripe for revisiting my original assertions. Indeed, I show of roots compared to leaf litter. I further conclude that that my original assertion is more nuanced and complex predictive understanding of plant species effects on than originally claimed. In particular, I discuss the need to nutrient cycling will require developing new frameworks consider leaf litter decomposition more carefully and move that are broadened beyond litter decomposition to con- beyond consideration of leaf litter feedbacks to a more sider the full litter–soil organic matter (SOM) continuum.
    [Show full text]
  • Three End-Of-Life Cases: Resolving Their Moral Dilemmas
    Vol. 33:2 Summer 2017 Three End-of-Life Cases: Resolving Their Moral Dilemmas RENÉ E MIRKES, OSF, PHD An organization of Roman Catholic physicians presented a set of questions to guide moral assessment of three end-of-life cases. The questions for each scenario highlight a corresponding ethical dilemma: (Case #1) the determination of brain death by neurological criteria; (Case #2) the decision to withhold or withdraw artificial nutrition and hydration from an unresponsive wakefulness syndrome (UWS) (formerly referred to as persistent vegetative state, [PVS]) patient; and (Case #3) the administration of pain medication that hastens death. To adjudicate the moral concern raised in each of these clinical cases, the following moral analyses appeal to the natural law perspective summarized in the Ethical & Religious Directives for Catholic Health Care Services1 and in other philosophical resources, both Catholic and secular. CASE #1 An 18-year-old involved in a motorcycle accident was brought to the emergency room with massive head trauma and life support. A brain angiogram showed no blood flow, and a neurological examination revealed no brainstem reflexes as well as persistent apnea. Blood pressure medication was required for heart rate and blood pressure control. Since the patient was an organ donor, the organ recovery team was called in after he was declared brain dead. Discussion (1) When and how do we declare a person dead? What is the difference between theological and scientific definitions of death? (A) A living human being is a substantial union of a (mammalian) body and a rational soul. We are not spiritual beings who use or have bodies.
    [Show full text]
  • Organic Matter Decomposition in Simulated Aquaculture Ponds Group Fish Culture and Fisheries Daily Supervisor(S) Dr
    O rganic matter decomposition in simulated aquaculture ponds Beatriz Torres Beristain Promotor: Prof. Dr. J.A .J. V erreth H oogleraar in de V isteelt en V isserij W ageningen U niversiteit C o-promotor: Dr. M .C .J. V erdegem U niversitair docent bij the Leerstoelgroep V isteelt en V isserij W ageningen U niversiteit Samenstelling promotiecommissie: Prof. Dr. Y . A vnimelech Technion, Israel Institute of Technology Prof. Dr. Ir. H .J. Gijzen U N ESC O -IH E, Delf, N etherlands Prof. Dr. Ir. M . W .A . V erstegen W ageningen U niversiteit Prof. Dr. Ir. A .A . K oelmans W ageningen U niversiteit Dit onderzoek is uitgevoerd binnen de onderzoekschool W IA S O rganic matter decomposition in simulated aquaculture ponds Beatriz Torres Beristain Proefschrift Ter verkrijging van de graad van doctor O p gezag van de rector magnificus van W ageningen U niversiteit, Prof. Dr. Ir. L. Speelman, In het openbaar te verdedigen O p dinsdag 15 A pril 2005 des namiddags te half tw ee in de A ula Torres Beristain, B. O rganic matter decomposition in simulated aquaculture ponds PhD thesis, Fish C ulture and Fisheries Group, W ageningen Institute of A nimal Sciences. W ageningen U niversity, P.O . Box 338, 6700 A H W ageningen, The N etherlands. - W ith R ef. œW ith summary in Spanish, Dutch and English ISBN : 90-8504-170-8 A Domingo, Y olanda y A lejandro Table of contents C hapter 1 General introduction. 1 C hapter 2 R eview microbial ecology and role in aquaculture ponds.
    [Show full text]
  • Fermentation and Anaerobic Decomposition in a Hot Spring
    Fermentation and anaerobic decomposition in a hot spring microbial mat by Karen Leigh Anderson A thesis submitted in partial fulfillment of requirements for the degree of Master of Science in Microbiology Montana State University © Copyright by Karen Leigh Anderson (1984) Abstract: Fermentation was investigated in a low sulfate hot spring microbial mat (Octopus Spring) according to current models on anaerobic decomposition. The mat was studied to determine what fermentation products accumulated, where in the mat they accumulated, and what factors affected their accumulation. Mat samples were incubated under dark anaerobic conditions to measure accumulation of fermentation products. Acetate and propionate (ca. 3:1) were the major products to accumulate in a 55&deg,C mat. Other products accumulated to a much lesser extent. Incubation of mat samples of varying thickness showed that fermentation occurred in the top 4mm of the mat. This has interesting implications for fermentative organisms in the mat due to the diurnal changes in mat oxygen concentrations. Fermentation measured in mat samples collected at various temperatures (50&deg,-70°C) showed acetate and propionate to be the major accumulation products. According to the interspecies hydrogen transfer model, the hydrogen concentration in a system affects the types of fermentation products produced. At a 65° C site, with natural high hydrogen levels, and at a 55°C site, with active methanogenesis, fermentation product accumulation was compared. There was a greater ratio of reduced fermentation products to acetate, with the exception of propionate, at 65°C. Ethanol accumulated at the 65°C site, as did lactate, though to a lesser extent.
    [Show full text]
  • Decomposition Responses to Climate Depend on Microbial Community Composition
    Decomposition responses to climate depend on microbial community composition Sydney I. Glassmana,b,1, Claudia Weihea, Junhui Lic, Michaeline B. N. Albrighta,d, Caitlin I. Loobya,e, Adam C. Martinya,c, Kathleen K. Tresedera, Steven D. Allisona, and Jennifer B. H. Martinya aDepartment of Ecology and Evolutionary Biology, University of California, Irvine, CA 92697; bDepartment of Microbiology and Plant Pathology, University of California, Riverside, CA 92521; cDepartment of Earth System Science, University of California, Irvine, CA 92697; dBioscience Division, Los Alamos National Laboratory, Los Alamos, NM 87545; and eDepartment of Biological Sciences, University of Denver, CO 80210 Edited by Mary K. Firestone, University of California, Berkeley, CA, and approved October 10, 2018 (received for review June 29, 2018) Bacteria and fungi drive decomposition, a fundamental process in soil moisture and extracellular enzyme production across a natural the carbon cycle, yet the importance of microbial community climate gradient (16). composition for decomposition remains elusive. Here, we used an Given that the factors regulating decomposition are often 18-month reciprocal transplant experiment along a climate gradient context dependent and can vary in their influence across a range in Southern California to disentangle the effects of the microbial of spatial and temporal scales (17, 18), we hypothesized that community versus the environment on decomposition. Specifically, decomposition responses to changing climatic conditions would we tested whether the decomposition response to climate change depend on microbial community composition. To test this hy- depends on the microbial community. We inoculated microbial pothesis, we conducted the largest microbial community trans- decomposers from each site onto a common, irradiated leaf litter plant experiment to date.
    [Show full text]
  • Organic Matter Decomposition and Ecosystem Metabolism As Tools to Assess the Functional Integrity of Streams and Rivers–A Systematic Review
    water Review Organic Matter Decomposition and Ecosystem Metabolism as Tools to Assess the Functional Integrity of Streams and Rivers–A Systematic Review Verónica Ferreira 1,* , Arturo Elosegi 2 , Scott D. Tiegs 3 , Daniel von Schiller 4 and Roger Young 5 1 Marine and Environmental Sciences Centre–MARE, Department of Life Sciences, University of Coimbra, 3000–456 Coimbra, Portugal 2 Faculty of Science and Technology, University of the Basque Country (UPV/EHU), P.O. Box 644, 48080 Bilbao, Spain; [email protected] 3 Department of Biological Sciences, Oakland University, Rochester, MI 48309, USA; [email protected] 4 Department of Evolutionary Biology, Ecology and Environmental Sciences, Institut de Recerca de l’Aigua (IdRA), University of Barcelona, Diagonal 643, 08028 Barcelona, Spain; [email protected] 5 Cawthron Institute, Private Bag 2, Nelson 7042, New Zealand; [email protected] * Correspondence: [email protected] Received: 4 November 2020; Accepted: 8 December 2020; Published: 15 December 2020 Abstract: Streams and rivers provide important services to humans, and therefore, their ecological integrity should be a societal goal. Although ecological integrity encompasses structural and functional integrity, stream bioassessment rarely considers ecosystem functioning. Organic matter decomposition and ecosystem metabolism are prime candidate indicators of stream functional integrity, and here we review each of these functions, the methods used for their determination, and their strengths and limitations for bioassessment. We also provide a systematic review of studies that have addressed organic matter decomposition (88 studies) and ecosystem metabolism (50 studies) for stream bioassessment since the year 2000. Most studies were conducted in temperate regions. Bioassessment based on organic matter decomposition mostly used leaf litter in coarse-mesh bags, but fine-mesh bags were also common, and cotton strips and wood were frequent in New Zealand.
    [Show full text]
  • Inherent Factors Affecting Soil Organic Matter
    Soil organic matter (SOM) is the organic component of soil, consisting of three primary parts including small (fresh) plant residues and small living soil organisms, decomposing (active) organic matter, and stable organic matter (humus). Soil organic matter serves as a reservoir of nutrients for crops, provides soil aggregation, increases nutrient exchange, retains moisture, reduces compaction, reduces surface crusting, and increases water infiltration into soil. Components vary in proportion and have many intermediate stages (Figure 1). Plant residues on the soil surface such as leaves, manure, or crop residue are not considered SOM and are usually removed from soil samples by sieving through a 2 mm wire mesh before analysis. Soil organic matter content can be estimated in the field and tested in a lab to provide estimates for Nitrogen, Phosphorus and Sulfur mineralized available for crop production and adjust fertilizer recommendations. Soil organic matter impacts the rate of surface applied herbicides along with soil pH necessary to effectively control weeds. Soil organic matter impacts the potential for herbicide carryover for future crops, and amount of lime necessary to raise pH. Figure 1. Major soil organic matter components (Source: The Soil Food Web, USDA-NRCS). Inherent Factors Affecting Soil Organic Matter Inherent factors affecting soil organic matter such warm and humid and slower in cool, dry climates. as climate and soil texture cannot be changed. Organic matter also decomposes faster when soil is Climatic conditions, such as rainfall, temperature, well aerated (higher oxygen levels) and much moisture, and soil aeration (oxygen levels) affect slower on saturated wet soils (refer to soil the rate of organic matter decomposition.
    [Show full text]
  • Fermentation of Non-Digestible Oligosaccharides by Human Colonic Bacteria
    Proceedings of the Nutrition Society ( 1996), 55,899-9 12 899 Symposium 2 Fermentation of non-digestible oligosaccharides by human colonic bacteria BY GLENN R. GIBSON, ANNE WILLEMS, SALLY READING AND M. DAVID COLLINS Department of Microbiology, Institute of Food Research, Earley Gate, Reading RG6 6BZ The principal substrates for colonic bacterial growth are dietary carbohydrates which have escaped digestion in the upper gastrointestinal tract. These may be starches, dietary fibres, other non-absorbable sugars, sugar alcohols and oligosaccharides. In the large intestine, saccharolytic bacteria are able to metabolize carbohydrates for increased energy and growth with short-chain fatty acids (SCFA) and a variety of other metabolites, such as the electron-sink products lactate, pyruvate, ethanol, H, and succinate, being produced. The majority of human large intestinal micro-organisms, have a strictly anaerobic metabolism, whilst numbers of facultative anaerobes are many orders of magnitude lower than those of the obligate anaerobes. Of the culturable flora, numerically predominant anaerobes are Gram-negative rods belonging to the genus Bacteroides. Other groups which have hitherto been identified as quantitatively significant include bifidobacteria, clostridia, eubacteria, lactobacilli, Gram-positive cocci, coliforms, methanogens and dissimilatory sulphate- reducing bacteria. Generally, the various components of the large intestinal microbiota may be considered as exerting either pathogenic effects or they may have potential health- promoting values. Bifidobacteria and lactobacilli are considered to belong to the latter group. Bacteria in the colon respond largely to the available fermentable substrate, and there is currently some interest in the use of diet to specifically increase groups perceived as health promoting. Non-digestible oligosaccharides seem to have this (prebiotic) potential.
    [Show full text]
  • Soil Food Web: Implications to Soil Health
    Soil Food Web: Implications to Soil Health Dr. Sajeemas “Mint” Pasakdee, Soil Scientist/Agronomist Advisor, Student Operated Organic Farm CIT-Jordan College of Agri. Sci. & Tech., Fresno State 1 Outline • Soil organisms and their interactions • What do soil organisms do? • Where do soil organisms live? • Food web structure • When are soil organisms active? • How is the food web measured? • Living soils—Bacteria; Fungi; Earthworms • Soil Environment 2 Organisms & Their Interaction 3 4 What do soil organisms do? Soil organisms support plant health as • decompose organic matter, • cycle nutrients, • enhance soil structure, • control the populations of soil organisms including crop pests. 5 Organic Matter • Food sources for soil organisms • Agricultural top soil ~1-6% (In CA, ~1-3% SOM) 6 Where do soil organisms live? • Around roots(rhizosphere) • Plant litter (C sources) • Humus (stabilized organic matter) • Surface of soil aggregates 7 Typical Food Web Structure • bacterial-dominated food webs o Grassland & Agri Soils o Ratio of fungi to bacteria, ~1:1 for productive agri. soils • fungal-dominated food webs o Ratio of fungal to bacterial, ~5:1 to 10:1 in a deciduous forest and 100:1 to 1000:1 in a coniferous forest 8 9 When are soil organisms active? 10 How is the food web measured? • Counting. Organism groups (bacteria, protozoa, arthropods, etc.); or subgroups (bacterial-feeding, fungal-feeding, and predatory nematodes), are counted and through calculations, can be converted to biomass. • Measuring activity levels. The amount of by-products, i.e., respiration (CO2); nitrification and decomposition rates • Measuring cellular constituents. Biomass carbon, nitrogen, or phosphorus; Enzymes; Phospholipids and other lipids; DNA and RNA 11 12 Soil Bacteria • One-celled organisms – generally 4/100,000 of an inch wide (1 µm) • A teaspoon of productive soil generally contains between 100 million and 1 billion bacteria (~two cows per acre).
    [Show full text]