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Ecology and Applications of Benthic Foraminifera

TLDR
This book presents the ecological background required to explain how fossil forms are used in dating rocks and reconstructing past environmental features including changes of sea level and demonstrates how living foraminifera can be used to monitor modern-day environmental change.
Abstract
In this volume John Murray investigates the ecological processes that control the distribution, abundance, and species diversity of benthic foraminifera in environments ranging from marsh to the deepest ocean. To interpret the fossil record it is necessary to have an understanding of the ecology of modern foraminifera and the processes operating after death leading to burial and fossilisation. This book presents the ecological background required to explain how fossil forms are used in dating rocks and reconstructing past environmental features including changes of sea level. It demonstrates how living foraminifera can be used to monitor modern-day environmental change. Ecology and Applications of Benthic Foraminifera presents a comprehensive and global coverage of the subject using all the available literature. It is supported by a website hosting a large database of additional ecological information (www.cambridge.org/0521828392) and will form an important reference for academic researchers and graduate students in Earth and Environmental Sciences.

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Microfossils from coastal environments as indicators of paleo-earthquakes, tsunamis and storms

TL;DR: In this article, microfossil habitat preferences and taphonomic character are used to constrain sediment provenance and identify overwash deposits, and how this information can be used to reconstruct the recurrence of tsunamis and storms.
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Late-Holocene climate variability in the Adriatic sea (Central Mediterranean)

TL;DR: Foraminifera assemblages collected from a set of sediment cores, collected on the Adriatic shelf and the Southern basin, provide compelling evidence of submillennial-scale environmental changes during the last 6000 years.
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The roles of elevation and salinity as primary controls on living foraminiferal distributions: Cowpen Marsh, Tees Estuary, UK

TL;DR: In this article, the authors determined the spatial and temporal variability of intertidal benthic foraminifera in the surface (0-1 cm) sediments from a time series survey of 31 sampling stations at Cowpen Marsh, for a period of 12 months.

The Central Paratethys palaeoceanography: A water circulation model based on microfossil proxies, climate, and changes of depositional environment

TL;DR: In this article, a model of the semi-closed Central Paratethys Sea history was proposed for the entire time span of 25 Ma and a set of modified palinspastic palaeogeographic maps were reconstructed taking into account the enormous changes in depositional systems and sedimentary facies, reflecting the tectonic events from the Oligocene to Miocene.
References
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A mathematical theory of communication

TL;DR: This final installment of the paper considers the case where the signals or the messages or both are continuously variable, in contrast with the discrete nature assumed until now.
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The measurement of diversity in different types of biological collections

TL;DR: Information content may be used as a measure of the diversity of a many-species biological collection whereby the sample size is progressively increased by addition of new quadrats and the mean increment in total diversity that results from enlarging the sample still more provides an estimate of the Diversity per individual in the whole population.
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The Relation Between the Number of Species and the Number of Individuals in a Random Sample of an Animal Population

TL;DR: It is shown that in a large collection of Lepidoptera captured in Malaya the frequency of the number of species represented by different numbers of individuals fitted somewhat closely to a hyperbola type of curve, so long as only the rarer species were considered.