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Ecology is the study of the patterns and processes governing the abundance and distribution of organisms and their relationships to their environment. The environment includes abiotic factors—such as the soils, geology, sunlight, climate, and other physical and chemical factors—as well as biotic factors, such as other organisms within the same or neighboring habitats. The term ecology derives from oekologie, first coined in 1866 by the biologist Ernst Haeckel, joining the Greek oikos, or household, and logos, or study. The field of ecology combines diverse scientific traditions from natural history, experimentation, field study and mathematical modeling to advance our understanding of the processes and patterns maintaining and altering biodiversity. As a positive science, ecology does not make a priori value judgments; nevertheless, it is strongly associated with the normative goals of modern environmentalism that ascribe a fundamental intrinsic and utilitarian value to nature. As such, ecological research and study is a key component of conservation biology, concerned with understanding and protecting biological diversity at multiple scales.

Ecology is a broad field that encompasses several thematic, areal, hierarchical, systematic, and methodological foci and traditions. For instance, distinct thematic/areal traditions are reflected in tropical ecology, desert ecology, freshwater ecology, marine ecology, and so on. Distinct hierarchical scales of biodiversity correspond to behavioral ecology (individual adaptations), autecology (populations of one species), synecology (communities of multiple species), and landscape ecology (structure, composition and function of landscapes). Disciplinary and methodological approaches define chemical ecology, genetic ecology, mathematical/theoretical ecology, statistical ecology, spatial ecology, and evolutionary ecology. These distinct traditions are not mutually exclusive, but often overlap in significant ways and have evolved over time.

History of Ecological Thought

The history of ecological thought, like that of the field of conservation biology, traces back several centuries. The earliest formal practice of ecological research on the relationship between organisms and their environment dates to the botanist Alexander von Humboldt, who in the early 19th century, described the relationship between plant distributions and regional climates. His work was followed by the publication of Charles Darwin's The Origin of Species in the mid 1800s, postulating an evolutionary, mechanistic perspective for ecology that departed from its earlier, descriptive focus. As developments in ecology continued over the next several decades, advances were made in the understanding of global bio-geochemical cycles (e.g., the nitrogen cycle); and the term biosphere came to be coined in 1875 by geologist Eduard Suess, to refer to that global sphere where the biota interacts with the lithosphere, atmosphere and hydrosphere. Such dynamic interactions were the focus of ecologists such as Henry Cowles and Frederic Clements toward the dawn of the 20th century, who established a tradition known as “dynamic ecology.” In the coastal dunes of the Great Lakes and the western prairies of the United States, respectively, Cowles and Clement examined the process of ecological succession, the sequence of ecological changes following a disturbance. Succession is the process by which an ecological community progresses over time from an initial, simple state to a latter, complex state as the system approached a stable equilibrium (sometimes called homeostasis). The change in the overall ecological community over time reflects, among other things, the loss and gain of individual species. A disturbance; such as wind damage, opening up of a forest gap by treefall, plowing of a field, creation of a patch by waves in an inter-tidal zone, or a rainfall event that creates an ephemeral pool, creates new localized habitats for different species to colonize and exploit. According to successional theory, early colonizers or invaders tend to be those that are best adapted to reproduce rapidly and quickly colonize the new habitat, and typically have high reproductive rates and small life spans. Such species are often referred to as r–strategists. During later stages in the successional sequence, r–strategists are gradually replaced by species that are slower to exploit the initial post-disturbance conditions, but are better adapted to continuing a viable population in the long term at or near the system's carrying capacity. Such slow-growing species are often referred to as K–strategists. According to strict Clementsian interpretation, most successional patches (seres) in a given locality will tend eventually toward a particular assemblage of “climax” species (i.e., a “monoclimax”) at the conclusion of the successional sequence, even when those seres reflect different stages in the successional series. The role of humans in ecological processes was viewed in a negative light, as interfering with the processes of natural succession.

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