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Titlebook: Linking Species & Ecosystems; Clive G. Jones,John H. Lawton Book 1995 Springer Science+Business Media Dordrecht 1995 Charles Darwin.Darwin

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Bioturbators as Ecosystem Engineers: Control of the Sediment Fabric, Inter-Individual Interactions, in muddy sediment are competitions between the activities of microbes, which usually consume oxygen, and the activities of burrowing sediment consumers, which usually bring oxygen to the sediment by mixing of surface sediment with the overlying water or by irrigating burrows. Alterations of the sed
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Floods, Food Chains, and Ecosystem Processes in Riversesilient following physical disturbance but subsequently vulnerable to predation. After prolonged low flow during drought, or in regulated channels with artificially stabilized hydrographs, lower trophic levels become dominated by armored or sessile taxa that are relatively invulnerable to predators
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Population Variability in Experimental EcosystemsThe most variable zoo-plankton populations were those most susceptible to fish predation. Ecosystem level changes clearly affect population dynamics, and shifts in populations can have strong impacts on ecosystem processes such as primary production. Integration of population and ecosystem studies s
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Linking Tree Population Dynamics and Forest Ecosystem Processestem processes, and that the rates of many ecosystem processes are strongly influenced by physical, environmental factors. However, in the absence of evidence of stronger control of tree population dynamics by ecosystem processes and physical factors, we conclude that the spatial and temporal dynamic
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Soil Organisms as Engineers: Microsite Modulation of Macroscale Processesregates, burrows, or buried organic matter, which continue to function in the absence of the organisms creating them. The effects of these artifacts, most notably those created by earthworms and termites, are cumulative and can therefore be manifested in macroscale measurements. It is shown, however
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Atmospheric Oxygen and the Biosphereimits the biological productivity of the oceans..The early earth almost certainly was clothed in a mildly reducing atmosphere. The earliest organisms probably used photosystem I and hence did not generate O.. The origination of photosystem II has not been dated, but it probably preceded the major ri
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