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Ice Ages
Scientists charged with producing a map of the earth during the last ice age ultimately confirmed the theory that the earth's irregular orbital motions account for the bizarre climatic changes which bring on ice ages. This book tells the story of those periods--what they were like, why they occurred, and when the next ice age is due.
Rereading the Fossil Record
Rereading the Fossil Record presents the first-ever historical account of the origin, rise, and importance of paleobiology, from the mid-nineteenth century to the late 1980s. Drawing on a wealth of archival material, David Sepkoski shows how the movement was conceived and promoted by a small but influential group of paleontologists and examines the intellectual, disciplinary, and political dynamics involved in the ascendency of paleobiology. By tracing the role of computer technology, large databases, and quantitative analytical methods in the emergence of paleobiology, this book also offers insight into the growing prominence and centrality of data-driven approaches in recent science.
Ice Ages
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Too Hot to Touch
A fascinating and authoritative account of the controversies and possibilities surrounding nuclear waste disposal, providing expert discussion in down-to-earth language.
The Paleobiological Revolution
The Paleobiological Revolution chronicles the incredible ascendance of the once-maligned science of paleontology to the vanguard of a field. With the establishment of the modern synthesis in the 1940s and the pioneering work of George Gaylord Simpson, Ernst Mayr, and Theodosius Dobzhansky, as well as the subsequent efforts of Stephen Jay Gould, David Raup, and James Valentine, paleontology became embedded in biology and emerged as paleobiology, a first-rate discipline central to evolutionary studies. Pairing contributions from some of the leading actors of the transformation with overviews from historians and philosophers of science, the essays here capture the excitement of the seismic changes in the discipline. In so doing, David Sepkoski and Michael Ruse harness the energy of the past to call for further study of the conceptual development of modern paleobiology.
A to Z of Earth Scientists, Updated Edition
A to Z of Earth Scientists, Updated Edition is a comprehensive A to Z reference of Earth scientists in areas including plate tectonics, climate change, and planetary science. Designed for high school through early college students, this is an ideal reference of notable Earth scientists from the 19th century to the present. Featuring nearly 200 entries and 100 black-and-white photographs, this title uses the device of biography in order to put a human face on science—a method that adds immediacy to the prose for the high school student who may have an interest in pursuing a career in the earth sciences. People covered include: James Hutton (1726–1797) William Smith (1769–1839) Charles Lyell (1797–1875) Mary Anning (1799–1847) Inge Lehmann (1888–1993) Walter Alvarez (1911–1988) Doris Malkin Curtis (1914–1991) Marie Tharp (1920–2006) David Keeling (1928–2005) Dawn Wright (1961–present)
The Changing Nature of the Maine Woods
The ecology of the ever-changing Maine forest
Dictionary of Mathematical Geosciences
This dictionary includes a number of mathematical, statistical and computing terms and their definitions to assist geoscientists and provide guidance on the methods and terminology encountered in the literature. Each technical term used in the explanations can be found in the dictionary which also includes explanations of basics, such as trigonometric functions and logarithms. There are also citations from the relevant literature to show the term’s first use in mathematics, statistics, etc. and its subsequent usage in geosciences.
Ice Ages and Astronomical Causes
It is not possible to understand the present or future climate unless scientists can account for the enormous and rapid cycles of glaciation that have taken place over the last million years, and which are expected to continue into the future. A great deal has happened in the theory of the ice ages over the last decade, and it is now widley accepted that ice ages are driven by changes in the Earth's orbit. The study of ice ages is very inter-disciplinary, covering geology, physics, glaciology, oceanography, atmospheric science, planetary orbit calculations astrophysics and statistics.
