ABSTRACT
The microbiome is the complex collection of microorganisms, their genes, and their metabolites, colonizing the human and animal mucosal surfaces, digestive tract, and skin. It is now well known that the microbiome interacts with its host, assisting in digestion and detoxification, supporting immunity, protecting against pathogens, and maintaining health. Studies published to date have demonstrated that healthy individuals are often colonized with different microbiomes than those with disease involving various organ systems. This review covers a brief history of the development of the microbiome field, the main objectives of the Human Microbiome Project, and the most common microbiomes inhabiting the human respiratory tract, companion animal digestive tract, and skin in humans and companion animals. The main changes in the microbiomes in patients with pulmonary, gastrointestinal, and cutaneous lesions are described.
Subject(s)
Microbiota , Animals , Gastrointestinal Tract/microbiology , Humans , Lung/microbiology , Pets , Respiratory System/microbiology , Skin/microbiologyABSTRACT
Orimulsion is a bitumen-based heavy fuel that is a less expensive alternative to traditional fuel oils. However, because its density is intermediate between that of freshwater and seawater, in the event of a spill, the fuel could strand in the sediments. Previous work indicated that only 0.6-2.7% of the bitumen would degrade in long incubations of marine sediments. We added various natural carbon substrates to stimulate the degradation of bitumen by native populations of benthic bacteria. The concentration and carbon isotopic signature of the respired carbon dioxide was measured to partition the substrates that supported bacterial respiration. We found that the addition of seagrass and pinfish stimulated the degradation of bitumen by as much as 2-9-fold relative to incubations without these substrates. Biodegradation of bitumen may be enhanced by the addition of natural marine carbon substrates and may be a useful approach for bioremediation. Preadaptation of the bacteria to bitumen did not significantly enhance their ability to degrade it.
Subject(s)
Carbon/metabolism , Fuel Oils/analysis , Geologic Sediments/chemistry , Hydrocarbons/metabolism , Water Pollutants, Chemical/metabolism , Animals , Biodegradation, Environmental , Fishes , Oxidation-Reduction , PlantsABSTRACT
Bacteria are the most abundant and active organisms in marine sediments and are critical for nutrient cycling and as a food source to many benthic and pelagic organisms. Bacteria are found both as free-living cells and as particle-associated cells, which can make investigations of these communities difficult. We found that common procedures for extracting bacteria from sediments leave the bacteria clay particle-associated and the clay particles clump, which reduce the reproducibility of direct counts. We optimized a sonication/surfactant method that produces a homogeneous suspension of bacterial cells against a uniform background of clay particles, which results in reproducible samples for epifluorescence microscopy. We developed a method to estimate CTC-positive cells and cell-specific CTC content in intact cores of surficial sediment communities from riverine, estuarine and coastal sites. Benthic bacterial abundances averaged 4.9x10(8) cells/g dry wt sediments in Apalachicola River, Florida sediments, 4.9-13.8x10(9) cells/g dry wt sediments in a variety of Apalachicola Bay sediments and 3.6x10(8) cells/g dry weight in shallow, anoxic Gulf of Mexico sediments. Percent CTC-positive cells ranged from low values of 9-10% CTC-positive cells in Apalachicola River and Apalachicola Bay sediments to high values of 25% CTC-positive cells in anoxic Gulf of Mexico sediments. After correction for abiotic CTC reduction and chlorophyll interference, estimates of cell-specific CTC reduction ranged from 0.15 to 0.55 fmol CTC(red)/active cell in the Apalachicola Bay sediments to 1.6 to 3.8 fmol CTC(red)/active cell in anoxic Gulf of Mexico sediments.
Subject(s)
Bacteria/isolation & purification , Bacteria/metabolism , Colony Count, Microbial , Geologic Sediments/microbiology , Tetrazolium Salts/metabolism , Water Microbiology , Bacteria/growth & development , Bacteriological Techniques , Microscopy, Fluorescence , Oxygen ConsumptionABSTRACT
Two symbiotic species, Photobacterium leiognathi and Vibrio fischeri, and one non-symbiotic species, Vibrio harveyi, of the Vibrionaceae were tested for their ability to grow by anaerobic respiration on various electron acceptors, including trimethylamine N-oxide (TMAO) and dimethylsulphoxide (DMSO), compounds common in the marine environment. Each species was able to grow anaerobically with TMAO, nitrate or fumarate, but not with DMSO, as an electron acceptor. Cell growth under microaerophilic growth conditions resulted in elevated levels of TMAO reductase, nitrate reductase and fumarate reductase activity in each strain, whereas growth in the presence of the respective substrate for each enzyme further elevated enzyme activity. TMAO reductase specific activity was the highest of all the reductases. Interestingly, the bacteria-colonized light organs from the two squids, Euprymna scolopes and Euprymna morsei, and the light organ of the ponyfish, Leiognathus equus, also had high levels of TMAO reductase enzyme activity, in contrast to non-symbiotic tissues. The ability of these bacterial symbionts to support cell growth by respiration with TMAO may conceivably eliminate the competition for oxygen needed for both bioluminescence and metabolism.
Subject(s)
Fumarates/metabolism , Methylamines/metabolism , Nitrates/metabolism , Oxidoreductases Acting on CH-CH Group Donors , Photobacterium/growth & development , Vibrio/growth & development , Anaerobiosis , Animals , Cell Respiration , Decapodiformes/microbiology , Dimethyl Sulfoxide/metabolism , Ecosystem , Fishes/microbiology , Nitrate Reductases/metabolism , Oxidoreductases/metabolism , Oxidoreductases, N-Demethylating/metabolism , Photobacterium/enzymology , Substrate Specificity , Symbiosis , Vibrio/enzymologyABSTRACT
Methanogenic Archaea are found in a wide range of environments and use several strategies to adjust to changes in extracellular solute concentrations. One methanogenic archaeon, Methanosarcina thermophila TM-1, can adapt to various osmotic conditions by synthesis of alpha-glutamate and a newly discovered compatible solute, Ne-acetyl-beta-lysine, or by accumulation of glycine betaine (betaine) and potassium ions from the environment. Since betaine transport has not been characterized for any of the methanogenic Archaea, we examined the uptake of this solute by M. thermophila TM-1. When cells were grown in mineral salts media containing from 0.1 to 0.8 M NaC1, M. thermophila accumulated betaine in concentrations up to 140 times those of a concentration gradient within 10 min of exposure to the solute. The betaine uptake system consisted of a single, high-affinity transporter with an apparent K3 of 10 microM and an apparent maximum transport velocity of 1.15 nmol/min/mg of protein. The transporter appeared to be specific for betaine, since potential substrates, including glycine, sarcosine, dimethyl glycine, choline, and proline, did not significantly inhibit betaine uptake. M. thermophila TM-1 cells can also regulate the capacity for betaine accumulation, since the rate of betaine transport was reduced in cells pregrown in a high-osmolarity medium when 500 microM betaine was present. Betaine transport appears to be H+ and/or Na+ driven, since betaine transport was inhibited by several types of protonophores and sodium ionophores.
Subject(s)
Betaine/metabolism , Carrier Proteins/genetics , Methanosarcina/metabolism , Adaptation, Physiological , Biological Transport, Active/drug effects , GABA Plasma Membrane Transport Proteins , Kinetics , Methanosarcina/drug effects , Methanosarcina/growth & development , Osmotic Pressure , Sodium Chloride/pharmacology , Uncoupling Agents/pharmacologyABSTRACT
Free viruses are abundant in the world's oceans. With this realization has come renewed interest in marine viruses and the role viruses play in structuring marine planktonic communities, primarily members of the microbial assemblage. The principal means of studying marine viruses has been by electron microscopy. This review discusses the use of microscopy to study free viruses and compares the ultrastructure of free viruses with bacteriophages and viruses which have been cultured from marine hosts. Many of the free viruses are smaller than typical cultured bacteriophages, which suggests that either many native phages are smaller than cultured phages or that many of the free viruses may be members of those phage families with smaller size classes or, in some cases, that many free viruses may be eukaryotic viruses. Some of the forms currently considered free viruses may be "defective phage" or "phage ghosts," noninfectious particles produced by bacteria, or virus-sized inorganic/organic colloids and warrant further study. Gross virus ultrastructure cannot be used as the sole criterion for determining marine virus diversity, since, as with many microbes, many unrelated viruses have similar morphological characters. Determination of DNA or RNA content as well as studies of protein and DNA relatedness of marine viruses will be needed if we are to understand the complexity of marine virus assemblages. Another important direction for future work is the need for marine bacteriophage/host and virus/host systems in order to study the biology of virus infection.
Subject(s)
Bacteriophages/ultrastructure , Viruses/ultrastructure , Water Microbiology , Microscopy, Electron , Virus Assembly , Viruses/classificationABSTRACT
The timing of lytic phage development and the relationship between host generation times and latent periods were investigated by electron microscopy of one-step growth experiments in two strains of marine Vibrio species. Results were used in a correction factor developed to interpret field studies of phage-infected marine bacteria. Both the number of mature phage per average cell section and the percentage of cells with mature phage increased exponentially by 73-86% into the latent periods. Assuming that bacterial infection and lysis take place continually in the ocean, conversion factors for relating the percentage of visibly infected bacteria to the total percentage of the bacterial community that are phage-infected were calculated as 3.70-7.14. When this range of factors was applied to previously-collected field data [Proctor LM, Fuhrman JA (1990) Nature (Lond) 343:60-62; Proctor LM, Fuhrman JA (1991) Mar Ecol Prog Ser 69:133-142] from 3 to 31% of the free-living bacteria and 3 to 26% of particulate-associated bacteria appeared to be phage-infected at any given time. Based upon a steady-state model in which half the daughter cells survive to divide again, the percent of total mortality would be twice the total percentage of phage-infected cells. From 6 to 62% and from 6 to 52% of mortality for the free-living and particulate-associated bacterial community, respectively, may be due to viruses.