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Fossil foraminifers

 

Books about foraminifera

Biostratigraphic and Geological Significance of Planktonic Foraminifera
Biostratigraphic and Geological Significance of Planktonic Foraminifera
Foraminifera are free-living protozoa that grow an elaborate, solid calcite skeleton. Their well-marked evolutionary record makes them of outstanding value in zonal stratigraphy. The role of fossil planktonic foraminifera as markers for biostratigraphical zonation and correlation underpins most drilling of marine sedimentary sequences and is key to hydrocarbon exploration. Biostratigraphic and Geological Significance of Planktonic Foraminifera presents a comprehensive analysis of existing data on fossil planktonic foraminifera genera and their phylogenetic evolution in time and space. In addition, the book contains new, unpublished data on carbonate thin sections with identified fossil planktonic foraminifera from the Far East to offshore Brazil and South Africa. 
Foraminifera and their Applications
Foraminifera and their Applications
In a one-stop resource, this book provides a state-of-the-art overview of all aspects of pure and applied forams studies. Building from introductory chapters on the history of foraminiferal research, and research methods, the book then takes the reader through biology, ecology, palaeoecology, biostratigraphy and sequence stratigraphy. This is followed by key chapters detailing practical applications of forams in petroleum geology, mineral geology, engineering geology, environmental science and archaeology. All applications are fully supported by numerous case studies selected from around the world, providing a wealth of real-world data. The book also combines lavish illustrations, including over 70 stunning original picture-diagrams of foraminifera, with comprehensive references for further reading. Accessible and practical, this is a vital resource for graduate students, academic micropalaeontologists, and professionals across all disciplines and industry settings which make use of foram studies.
Benthic Foraminifers as Tools to Reconstruct High-Latitude Holocene Climate Variability and Processes During Cold-Water Coral Mound Growth and Develop
Benthic Foraminifers as Tools to Reconstruct High-Latitude Holocene Climate Variability and Processes During Cold-Water Coral Mound Growth and Develop
Cold-water corals occur worldwide from high latitudes to tropical areas, in various settings from the deep-sea to shallow marine environments near the coast. The topic of this thesis is the establishment and extension of knowledge about environmental conditions controlling cold-water coral (CWC) mound development. From literature it is known that glacial-interglacial cycles drive development and geographic distribution of CWC mounds on a large scale. On the other hand, knowledge about the influence of small scale climatic and oceanographic changes during the Holocene is scarce. Thus, this thesis focuses on the investigation of the limited Holocene climatic and oceanographic changes and their effect on the process of mound genesis. For this purpose, a Holocene CWC mound setting in a sound in the Altafjord in northern Norway (70°N) -- the Stjernsund -- was chosen and the local benthic ecosystem was extensively analysed.