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Revised and updated, it reflects the recent developments and changing emphasis in the field of paleoecology. While the basic organization remains the same as the original edition, there are several major changes, including an extensive reorganization and shortening of Chapter 2, focusing now on environmental parameters rather than individual taxonomic groups; greater use of tables with references to pertinent literature; inclusion of a new chapter on taphonomy; elimination of the chapter on skeletons as sedimentary particles; removal of many of the recurring examples from the Neogene of the Kettlemen Hills; and inclusion of new references on all topics. Older references have been kept and will serve to blend the historical and important milestones in the development of paleoecology with the most current research.
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This is a book for beginners. Not geological beginners, because an introductory course in paleontology and some knowledge of the petrographic microscope is assumed, but for beginners in the study of the petrography of fossil constituents in sedimentary rocks. Fossils are studied for various reasons: 1) to provide chron ologic (time) frameworks, 2) to delineate rock units and ancient environments, or 3) to understand the past development (evolu tion) of living plants and animals. All of these uses may be at tained through petrographic studies of thin sections of fossils embedded in sedimentary rocks. Some knowledge of the appear ance of fossils in thin section is also fundamental for general ...
Covers the period from 1790 to 1905 in The Times of London.
Davis A. Young and Ralph Stearley seek to convince readers of the vast antiquity of the Earth. They point out the flaws of young-Earth creationism and counter the impression by many scientists that all Christians are young-Earth creationists.