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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.read more
Citations
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Journal ArticleDOI
Effects of natural and human-induced hypoxia on coastal benthos
Lisa A. Levin,Werner Ekau,Andrew J. Gooday,Frans Jorissen,Jack J. Middelburg,S. W. A. Naqvi,Carlos Neira,Nancy N. Rabalais,Jing Zhang +8 more
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
Joachim Schönfeld,Elisabeth Alve,Emmanuelle Geslin,Frans Jorissen,Sergei Korsun,Silvia Spezzaferri +5 more
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.
Elisa Piña-Ochoa,Signe Høgslund,Emmanuelle Geslin,Tomas Cedhagen,Niels Peter Revsbech,Lars Peter Nielsen,Magali Schweizer,Frans Jorissen,Søren Rysgaard,Nils Risgaard-Petersen +9 more
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
Virus-like particles and cytopathological effects in Elphidium excavatum clavatum, a benthic foraminiferan
TL;DR: Transmission electron microscopy gives first evidence of virus-like particles (VLP) in the cytoplasm of Elphidiuni excarraturn clavatum from the western Baltic Sea, limiting the occurrence of VLP to very young chambers.
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The Holocene palaeoceanographic history of Muck Deep, Hebridean shelf, Scotland: has there been a change of wave climate in the past 12 000 years?
TL;DR: In this article, a 70 cm core shows an upper buff sandy mud layer (0-4500 BP, radiocarbon years) overlying a dark grey mud layer, suggesting that the upper sandy layer formed under higher energy conditions comparable to those existing now, where storm waves from southwesterly gales are responsible for transporting material from the adjacent shelf into the deeps.
Journal Article
Diversity and Dominance of Living and Total Foraminiferal Assemblages, Pennar Estuary, Andhra Pradesh
K. R. Reddy,R. Jagadiswara Rao +1 more
TL;DR: A quantitative study has been made of the distribution of recent foraminifera in 180 samples of bottom sediments collected from 15 stations in the Pennar estuary.