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Fossil Corals and Sponges
Contents: Sorauf, J. E.: The function of dissepiments and marginaria in the Rugosa (Cnidaria, Zoantharia); Lee, D.-J., Jun, Y.-H., Bae, B.-Y. & Elias, R. J.: Axial increase in some early tabulate corals; Porter, D. R., Elias, R. J. & Young, G. A.: Biometric analysis of corallite size in the colonial rugosan Crenulites; Hladil, J.
The Permian Timescale
This volume brings together state-of-the-art reviews of the non-biostratigraphic and biostratigraphic data that are used to define and correlate Permian time intervals. It includes analyses of Permian radio-isotopic ages, magnetostratigraphy, isotope-based stratigraphy and timescale-relevant biostratigraphy. It is the first book devoted to this subject and represents the cutting edge of Permian time-scale research.
The Geology of Central Europe
Volume 1 focuses on the evolution of Central Europe from the Precambrian to the Permian, a dynamic period which traces the formation of Central Europe from a series of microcontinents that separated from Gondwana through to the creation of Pangaea. Separate summary chapters on the Cadomian, Caledonian and Variscan orogenic events as well as on Palaeozoic magmatism provide an overview of the tectonic and magmatic evolution of the region. These descriptions sometimes extend beyond the borders of Central Europe to take in the Scottish and Irish Caledonides as well as the Palaeozoic successions in the Baltic region.
GAC Special Paper
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Yearbook of International Organizations 2013-2014 (Volumes 1a-1b)
Volume 1 (A and B) covers international organizations throughout the world, comprising their aims, activities and events.
The Indian Paleogene
This unique book provides a concise account of Indian Paleogene and presents a unified view of the Paleogene sequences of India. The Paleogene, comprising the early part of the Cenozoic Era, was the most dynamic period in the Earth’s history with profound changes in the biosphere and geosphere. The period spans ~42 million years, beginning from post- K/T mass extinction event at ~65 Ma and ending at ~23 Ma, when the first Antarctic ice sheet appeared in the Southern Hemisphere. The early Paleogene (Paleocene–Eocene) has been considered a globally warm period, superimposed on which were several transient hyperthermal events of extreme warmth. Of these, the Palaeocene Eocene Thermal Maxima...
Géochronique
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Almanach
Vols. for 1854-19 include section: Die feierliche Jahressitzung (called Die feierliche Sitzung, 1854-1914; Die statutenmässige Jahressitzung, 1915-21; published also separately, 1848-99)
