Preface to the Princeton Landmarks in Biology Edition vii Preface xi Symbols Used xiii 1. The Importance of Islands 3 2. Area and Number of Speicies 8 3. Further Explanations of the Area-Diversity Pattern 19 4. The Strategy of Colonization 68 5. Invasibility and the Variable Niche 94 6. Stepping Stones and Biotic Exchange 123 7. Evolutionary Changes Following Colonization 145 8. Prospect 181 Glossary 185 References 193 Index 201

The Theory of Island Biogeography

Statistics for Spatial Data.

The use of stable isotopes to solve biogeochemical problems in ecosystem analysis is increasing rapidly because stable isotope data can contribute both source-sink (tracer) and process information: The elements C, N, S, H, and all have more than one isotope, and isotopic compositions of natural materials can be measured with great precision with a mass spectrometer. Isotopic compositions change in predictable ways as elements cycle through the biosphere. These changes have been exploited by geochemists to understand the global elemental cycles. Ecologists have not until quite recently employed these techniques. The reasons for this are, first, that most ecologists do not have the background in chemistry and geochemistry to be fully aware of the possibilities for exploiting the natural variations in stable isotopic compositions, and second, that stable isotope ratio measurements require equipment not normally available to ecologists. This is unfortunate because some of the more intractable problems in ecology can be profitably addressed using stable isotope measurements. Stable isotopes are ideally suited to increase our understanding of element cycles in ecosystems. This review is written for ecologists who would like to learn more about how stable isotope analyses have been and can be used in ecosystem studies. We begin with an explanation of isotope terminology and fractionation, then summarize isotopic distributions in the C, N, and S biogeochemical cycles, and conclude with five case studies that show how stable isotope measurements can provide crucial information for ecosystem analysis. We restrict this review to studies of natural variations in C, N, and S isotopic abundances, cxcluding from consideration ~5N enrichment studies and hydrogen and oxygen isotope studies. Our focus on C, N, and S derives in part from our

Stable isotopes in ecosystem studies

Aquatic chemistry is becoming both a rewarding and substantial area of inquiry and is drawing many prominent scientists to its fold. Its literature has changed from a compilation of compositional tables to studies of the chemical reactions occurring within the aquatic environments. But more than this is the recognition that human society in part is determining the nature of aquatic systems. Since rivers deliver to the world ocean most of its dissolved and particulate components, the interactions of these two sets of waters determine the vitality of our coastal waters. This significant vol ume provides not only an introduction to the dynamics of aquatic chem istries but also identifies those materials that jeopardize the resources of both the marine and fluvial domains. Its very title provides its emphasis but clearly not its breadth in considering natural processes. The book will be of great value to those environmental scientists who are dedicated to keeping the resources of the hydrosphere renewable. As the size of the world population becomes larger in the near future and as the uses of materials and energy show parallel increases, the rivers and oceans must be considered as a resource to accept some of the wastes of society. The ability of these waters and the sediments below them to accommodate wastes must be assessed continually. The key questions relate to the capacities of aqueous systems to carry one or more pollutants."

Metal pollution in the aquatic environment

We review the biogeography of microorganisms in light of the biogeography of macroorganisms A large body of research supports the idea that free-living microbial taxa exhibit biogeographic patterns Current evidence confirms that, as proposed by the Baas-Becking hypothesis, 'the environment selects' and is, in part, responsible for spatial variation in microbial diversity However, recent studies also dispute the idea that 'everything is everywhere' We also consider how the processes that generate and maintain biogeographic patterns in macroorganisms could operate in the microbial world

/pdf/microbial-biogeography-putting-microorganisms-on-the-map-1k7e5do5pn.pdf

Microbial biogeography : putting microorganisms on the map

Microbial communities that developed on glass slides suspended in acid-polluted (pH=2.9) and nonpolluted (pH=6.5) but otherwise similar waters showed evidence of stress when suspended at the opposite station. Glucose incorporation was inhibited in both translocated communities, but the inhibition was not as severe and recovery of activity was faster for the acid-developed community as compared to the circumneutral community. The communities contained a substantially different set of members with little overlap. The range of pH values at which the members of the acid-developed community could function suggested that the members of that community were generalists, as opposed to narrowly constrained members of the community from the circumneutral station. Based on the proportion of test characters that received positive responses, the organisms from the acidic site were more general in their abilities (47.6% positive) as compared with the neutral counterparts (18.7% positive). The results support the concept that communities developed in extreme environments tend to be generalists, whereas those from mesic environments, due to the higher levels of competition present, tend to be specialists. Furthermore, the study of microbial communities in dynamic systems such as streams and reservoir inflows is facilitated by the use of solid surfaces which allow an assemblage of nontransient microbes to develop.

https://www.jstor.org/stable/info/4250957

The Community Structure of Sessile Heterotrophic Bacteria Stressed by Acid Mine Drainage

Factors associated with accuracy and precision in the enumeration of aquatic aerobic heterotrophs by the spread plate method were evaluated by using a nested analysis of variance experimental design. Variances associated with individual components of the spread plate procedure were isolated, and optimal replications of each step were allocated. A practical scheme for optimal allocation of resources is proposed, consisting of four subsamples and two plates per subsample and yielding a total variance decrease of 70% from a single-subsample, 10-plate series. Data transformation was, in general, unnecessary for intraexperiment or intrasample statistical analysis, whereas interexperiment or intersample comparisons may require transformation of data. Rapid changes in the numbers of organisms in stored water samples were observed that were not reproducible and did not follow detectable trends, with increases or decreases in counts occurring in samples regardless of whether they were stored at room temperature or refrigerated, or stored in plastic or glass containers. Rapid sample handling is strongly recommended to minimize variations in the microbial populations of samples for aquatic environments.

Evaluation of the accuracy and precision of enumerating aerobic heterotrophs in water samples by the spread plate method.

Distribution of reduced inorganic sulfur compounds in lake sediments receiving acid mine drainage

Dimethylnitrosamine was formed in samples of soil, municipal sewage, and lake water supplemented with 250 ppm of dimethylamine and 100 ppm of nitrite-N. The toxic compound was formed in similar quantities in soil and sewage samples sterilized by gamma radiation and in lake water sterilized by autoclaving. Nitrosation occurred in samples with a pH as high as 7.7, although nitrosamine was not formed in buffered solutions above pH 5.0. The amount of dimethylnitrosamine produced in soil at pH 5.2 was directly related to the amount of the precursors added to the soil. When the organic matter was partially removed from a sample of soil by treatment with peroxide, the amount of dimethylnitrosamine formed upon incubation with dimethylamine and nitrite decreased. No nitrosamine was produced from the precursors when the soil was freed of organic matter by ignition. Incubation of the ignited soil with glucose and an inoculum of microorganisms led to the formation of nonleachable organic matter and the return of the nitrosating capacity. The results show that nitrosamines may be produced in nonacid environments containing organic materials.

Factors Affecting Dimethylnitrosamine Formation in Samples of Soil and Water

Changes in the sorption capacity of Coastal Plain sediments due to redox alteration of mineral surfaces

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