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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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Late Pleistocene-Holocene events on the continental slope of the Laptev Sea: Evidence from benthic and planktonic foraminiferal assemblages

TL;DR: In this paper, a core of the Laptev Sea was used for the study of benthic and planktonic foraminifers and a contribution to the multidisciplinary investigations of core PS51/154-11 from the laptev sea was made.
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Assessing the ecological preferences of agglutinated benthic foraminiferal morphogroups from the western Bay of Bengal

TL;DR: The study suggests a clear ecological preference of a majority of the agglutinated morphotypes and morphogroups and thus their potential application in paleoecological interpretations.
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Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay

TL;DR: The planktic foraminiferal composition indicates that surface water masses were under the influence of the polar front in the early record, which retreated at about 11.5 cal ka BP, and the early Holocene is characterized by relatively warm and stratified water masses at 8.4-4.8 cal Ka BP.
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Late-glacial to Holocene depositional architecture of the Ombrone palaeovalley system (Southern Tuscany, Italy): Sea-level, climate and local control in valley-fill variability

TL;DR: In this article, a detailed sedimentological and stratigraphic study of two cores along the Ombrone palaeovalley axis led to reconstruction of the post-Last Glacial Maximum valley-fill history.
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.