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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

Another look at confidence limits for species proportions

TL;DR: The binomial distribution was used by Dryden (1931), Dennison and Hay (1967), Wright and Hay as discussed by the authors, and Patterson and Fishbein (1989) for this purpose.
Journal ArticleDOI

The impact of the Mediterranean Outflow Water (MOW) on benthic foraminiferal assemblages and surface sediments at the southern Portuguese continental margin

TL;DR: In this article, foraminifera and surface sediments were analyzed from 23 box-core and core-top samples from 250 to 3600 m depth at the southern Portuguese continental margin between 37 and 38 °N.
Journal ArticleDOI

Microhabitat preferences and stable carbon isotopes of endobenthic Foraminifera: clue to quantitative reconstruction of oceanic new production?

TL;DR: In this paper, the carbon isotopic composition of the benthic foraminifera was compared to that of the dissolved inorganic carbon (DIC) of simultaneously sampled bottom water.
Journal ArticleDOI

The distribution of contemporary intertidal foraminifera at Cowpen Marsh, Tees Estuary, UK: implications for studies of Holocene sea-level changes

TL;DR: Foraminiferal assemblages were collected at 2-weekly intervals over a period of 12-months from the intertidal zone of Cowpen Marsh as discussed by the authors, and cluster analysis was performed to identify the vertical relationship of the local environment in which the assemblage accumulated to a reference tide level.