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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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Journal ArticleDOI

Benthic foraminifera from the Southeastern Mediterranean shelf: Dead assemblages and living-dead comparisons recording consequences of Nile River damming

TL;DR: The role of the Nile River damming in shaping the recent benthic ecology in the southeastern Levantine (SL) Basin, the saltiest, hottest and the most oligotrophic basin within the Mediterranean Sea was explored in this paper.
Journal ArticleDOI

Response of benthic foraminiferal communities to changes in productivity and watermass conditions in the epicontinental Paratethys during the middle Miocene

TL;DR: In this article, a study based on a combination of organic geochemistry (δ13Corg, n-alkane based indices; TOC/TIC) with benthic foraminiferal stable isotopic data from the time interval of ~14.4 to 14.36
Journal ArticleDOI

Pleistocene biogeochemical record in the south‐west Pacific Ocean (images site MD97‐2114, Chatham Rise)

TL;DR: In this article, the main paleoceanographic and paleoclimate changes that have influenced the surface and deep-water circulation in the SW Pacific Ocean (Chatham Rise, eastern New Zealand) during the last million years are reconstructed.
Book ChapterDOI

The “Turritella Layer”: A Potential Proxy of a Drastic Holocene Environmental Change on the North–East Atlantic Coast

TL;DR: In this article, a collection of data including sub-bottom VHR seismic (Seistec boomer), bathymetry and cores, was conducted in three sea lochs of the north west coast of Scotland, as part of an investigation of the sedimentological and climatic change records since the Last Glacial Maximum.
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.