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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

Effects of natural and human-induced hypoxia on coastal benthos

TL;DR: Large areas of low oxygen persist seasonally or continuously beneath upwelling regions, associated with the upper parts of oxygen minimum zones (SE Pacific, W Africa, N Indian Ocean), and support a resident fauna that is adapted to survive and reproduce at oxygen concentrations.
Journal ArticleDOI

The FOBIMO (FOraminiferal BIo-MOnitoring) initiative—Towards a standardised protocol for soft-bottom benthic foraminiferal monitoring studies

TL;DR: The aim is to standardise methodologies used in bio-monitoring only and not to limit the use of different methods in pure scientific studies, and to propose two types of recommendations about living (stained) benthic foraminiferal assemblages.
Journal ArticleDOI

Widespread occurrence of nitrate storage and denitrification among Foraminifera and Gromiida.

TL;DR: Benthic foraminifers inhabit a wide range of aquatic environments including open marine, brackish, and freshwater environments and Gromia, another taxon also belonging to Rhizaria, accumulate and respire nitrates through denitrification.
Book ChapterDOI

The Carboniferous Period

TL;DR: Only the GSSPs for the Bashkirian, Visean and Tournaisian (base of the Mississippian) have been formalized, although the latter now has complications as mentioned in this paper.
Book ChapterDOI

Monitoring in Coastal Environments Using Foraminifera and Thecamoebian Indicators: Conclusions and Final Remarks

TL;DR: A glossary and some basic taxonomy on all of the species used in this book have been provided, as an appendix, for those readers who want to go a step further as discussed by the authors.
References
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Journal ArticleDOI

Propagule transport as a key method of dispersal in benthic foraminifera (Protista)

TL;DR: This work experimentally demonstrate the dispersal of propagules, which include both sexually and asexually produced young (perhaps only the proloculus), though the sexually produced young appear to have a greater potential for dispersal.
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Ecological transitions indicated by foraminiferal assemblages in paralic environments

TL;DR: In this article, foraminiferal assemblages of about 1,500 samples collected worldwide in various types of paralic environments, supplemented by selected published data, led to the determination of several species assemblage typical of Paralic subenvironments.
Journal ArticleDOI

The response of benthic foraminifers to carbon flux and primary production in the Arctic Ocean

TL;DR: A quantitative correlation between the foraminiferal fauna and the local carbon flux is allowed, which may be used as a tool to estimate changes in primary productivity.
Journal ArticleDOI

Benthic foraminiferal distribution and biomass related to pore-water oxygen content: central California continental slope and rise

TL;DR: Foraminiferal numerical densities were determined at selected depths within the uppermost 9 cm of box cores, using either an adenosine triphosphate (ATP) assay or a Rose Bengal vital staining technique as mentioned in this paper.