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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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Microbiotic signatures of the Anthropocene in marginal marine and freshwater palaeoenvironments

TL;DR: The term "Anthropocene" has been proposed to indicate a geological interval character- ized by global anthropogenic environmental change as mentioned in this paper, which can be defined micropalaeontologically by considering microfloras and microfaunas from nearshore waters through to paralic and freshwater aquatic milieux.
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Environmental changes during the Paleocene–Eocene Thermal Maximum in Spitsbergen as reflected by benthic foraminifera

TL;DR: In this paper, the effects of hypoxic and hyposaline conditions in a stratified water column, due to extreme warming with its accompanying intensified hydrologic cycle, were investigated in the Gilsonryggen Formation.
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Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes

TL;DR: In this article, temperature and salinity reconstructions for two 1000-year high-resolution sedimentary records, located at the boundary between Atlantic and Arctic surface waters on the North Icelandic shelf, are based on transfer functions and oxygen isotopes for planktonic and benthic foraminifera.
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The chronostratigraphy of a Quaternary sequence at the distal part of the Nile littoral cell, Haifa Bay, Israel

TL;DR: In this paper, the authors presented a detailed chronostratigraphic framework of the last 1 Ma of an eastern Mediterranean sequence (Haifa Bay, Israel) aimed to examine the relative roles of sea-level changes, climate and tectonics.
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Foraminifera as bioindicators of water quality: The FoRAM Index revisited.

TL;DR: The development and application of the FoRAM Index (FI), which provides a bioindicator metric for water quality that supports reef accretion, is reviewed and how it can be applied more effectively across different geographical regions is proposed.
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.