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Riedel 14 Cenozoic radiolaria Annika Sanfilippo, M. Though several very useful reference works have appeared in the last decade, we feel that there is still a need for such a book for the use of stratigraphers in industry and academia and for advanced students.
It is also widely spread and not always easy to find, hence our endeavour to get as much as possible together in a single volume. Such a project could only be undertaken by a team of specialists and so 18 paleontologists have worked together to produce this book.
We have restricted ourselves to those groups that are used in the dating of deeper water sediments. However, in the case of many taxa particularly the calcareous ones their presence in neritic environments allows correlation of these facies also.
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In fact, because many biostratigraphic studies were completed before the availability of such a wealth of deep sea cores, zonations were largely erected on surface and subsurface sections where the sediments were mostly deposited under bathyal conditions. To keep the length of the book within acceptable limits, authors had to be selective in the number of taxa that could be included and also in the degree of illustration possible.
In as many cases as possible we have included not only the marker species but have also drawn attention to morphologically similar forms with which they might be confused.
Of necessity, the interpretation of taxa and choice of zonal schemes largely reflects the views of the authors, with which some other authorities may disagree to a certain extent. For reasons of space we have been forced to concentrate on certain key regions where the planktic succession has been worked out best.
The editors would like to acknowledge the very good cooperation that they have received from all the contributors. It has been a pleasure to work with Cambridge University Press and we have been exceedingly fortunate in our Press subeditor, Karin Fancett, whose dedication and expertise have been vital to the project.
Beckmann was good enough to read large portions of the text for us. The illustrative material for the majority of the chapters was prepared in these two institutions- the drawings by Mr A. Uhr and photographs by Mr U.
Gerber in Zurich and the wording for figures and charts by Mr R. We are most grateful to all these people for their skill and good cooperation. Note added in reprinting We have taken the opportunity to divide this book into two volumes to facilitate its use.
Doyle, 1 Introduction The last 15 years have been of vital importance in the history of the use of planktic microfossils for the dating of Cretaceous and Cenozoic deep sea sediments. During this time, the Glomar Chall eng er of the Deep Sea Drilling Project DSDP has drilled at a total of sites in almost every ocean basin in the world and brought up Cenozoic and Mesozoic sediment cores from the great majority of them.
A review of some of the important findings of the first ten years of the project is given in Warme et a!. Zonal schemes based on planktic foraminifera and calcareous nannofossils were well established and already proven in many land sections, both surface and subsurface, by the time the DSDP began in They provided the tool for the dating not only of the sedimentary sequences but also of the underlying oceanic crust that was reached at many of the sites.
The latter dating has relied heavily on a knowledge of the age of the sediments immediately above the crust because direct dating of oceanic basalts has hardly ever proved possible.
The stratigraphic significance ofthe siliceous microfossils - radiolaria, silicoflagellates and diatoms - was less well known at the beginning of the Deep Sea Drilling Project. For these groups the zonal schemes that have since been established are based to a large degree on DSDP cores.
For the calcareous groups the wealth of new sections has enabled a considerable refinement in resolution.
The overall result is that there is now a much closer correlation between the fossil groups, both calcareous and siliceous, and this subject is covered in Chapter 2.
A recent book edited by B. BoersmaIntroduction to Marin e Micropal eontology, is useful for its discussion of the biology of the various fossil groups. Introduction However, species are not treated from a stratigraphic viewpoint in any depth. Mention should also be made of Oceanic M icropalaeontology edited by A.
Neogene foraminifera are not covered.costs etc. 7. What are the differences between a job and a task?
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