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The studies in this second volume by Martin Rudwick (the first being The New Science of Geology: Studies in the Earth Science in the Age of Reform) focus on the figures of Charles Lyell and Charles Darwin. Lyell rose to be of pivotal importance in the second quarter of the 19th century because he challenged other geologists throughout Europe by probing their methods and conclusions to the limit. While adopting their goal of reconstructing the contingent history of the earth, he claimed that the physical processes observable in action in the present could explain far more about the past than was commonly believed, and that it was unnecessary to postulate occasional catastrophic events of still greater intensity. Far more controversial was Lyell's further claim that the earth and its life had always been in a stable steady state, rather than developing in a broadly linear or directional fashion. His younger friend Charles Darwin first made his name as a Lyellian geologist; Darwin's early work in geology, studied here, provided important foundations for his later and more famous research on speciation and other biological problems.
The science of geology was constructed in the decades around 1800 from earlier practices that had been significantly different in their cognitive goals. In the studies collected here Martin Rudwick traces how it came to be recognised as a new kind of natural science, because it was constituted around the idea that the natural world had its own history. The earth had to be understood not only in relation to unchanging natural laws that could be observed in action in the present, but also in terms of a pre-human past that could be reliably known, even if not directly observable and its traces only fragmentarily preserved. In contrast to this radically novel sense of nature's own contingent history, the earth's unimaginably vast timescale was already taken for granted by many naturalists (though not yet by the wider public), and the concurrent development of biblical scholarship precluded any significant sense of conflict with religious tradition. A companion volume, Lyell and Darwin, Geologists: Studies in the Earth Sciences in the Age of Reform, was published in 2005.
In the late eighteenth and early nineteenth centuries, scientists
reconstructed the immensely long history of the earth--and the
relatively recent arrival of human life. The geologists of the
period, many of whom were devout believers, agreed about this vast
timescale. But despite this apparent harmony between geology and
Genesis, these scientists still debated a great many questions: Had
the earth cooled from its origin as a fiery ball in space, or had
it always been the same kind of place as it is now? Was prehuman
life marked by mass extinctions, or had fauna and flora changed
slowly over time?
In the late eighteenth and early nineteenth centuries, scientists
reconstructed the immensely long history of the earth--and the
relatively recent arrival of human life. The geologists of the
period, many of whom were devout believers, agreed about this vast
timescale. But despite this apparent harmony between geology and
Genesis, these scientists still debated a great many questions: Had
the earth cooled from its origin as a fiery ball in space, or had
it always been the same kind of place as it is now? Was prehuman
life marked by mass extinctions, or had fauna and flora changed
slowly over time?
During a revolution of discovery in the late eighteenth and early
nineteenth centuries, geologists reconstructed the immensely long
history of the earth--and the relatively recent arrival of human
life. "Bursting the Limits of Time" is a herculean effort by one of
the world's foremost experts on the history of geology and
paleontology to illuminate this scientific breakthrough that
radically altered existing perceptions of a human's place in the
universe as much as the theories of Copernicus and Darwin did.
It is not often that a work can literally rewrite a person's view of a subject. And this is exactly what Rudwick's book should do for many paleontologists' view of the history of their own field.--Stephen J. Gould, Paleobotany and Palynology Rudwick has not merely written the first book-length history of palaeontology in the English language; he has written a very intelligent one. . . . His accounts of sources are rounded and organic: he treats the structure of arguments as Cuvier handled fossil bones.--Roy S. Porter, History of Science
Arguably the best work to date in the history of geology.--David R. Oldroyd, Science After a superficial first glance, most readers of good will and broad knowledge might dismiss [this book] as being too much about too little. They would be making one of the biggest mistakes in their intellectual lives. . . . [It] could become one of our century's key documents in understanding science and its history.--Stephen Jay Gould, New York Review of Books Surely one of the most important studies in the history of science of recent years, and arguably the best work to date in the history of geology.--David R. Oldroyd, Science
How did the earth look in prehistoric times? Our images of the remote past, museum displays of dinosaurs and book illustrations of exotic plants and animals, are based on fragmentary evidence, yet these depictions are realistic enough to suggest that we can know exactly what the earth looked like millions of years ago. Today depictions of the earliest stages of the earth - deep time - are so common that we take them for granted, but less than 200 years ago no such pictures existed. In Scenes from Deep Time, Martin J. S. Rudwick traces the earliest attempts to reconstruct the past no one has ever seen. With over 100 stunning lithographs and engravings from the eighteenth and nineteenth centuries, many reproduced here for the first time since their original publication and accompanied by portions of the original explanatory texts, Rudwick argues that scientists and artists made earth history visually compelling as evidence from nature supplanted the biblical view of the distant past. Until 1820, the only pictorial reconstructions of earth history were illustrations of the biblical creation story. During the following decades, geologists and biologists gathered and interpreted fossil evidence that suggested the earth was millions of years old. Fossil finds inspired a new collaboration between scientists and artists, and as they became more confident in their visions of the past, they produced increasingly realistic portrayals of deep time. By 1870, the prehistoric past was depicted in the same style as the scenes we see today, and these representations continue to reflect and often shape scientific as well as public views. Because we can never completely know what life was like in deeptime, these images fascinate scientists and laypeople alike.
Earth has been witness to mammoths and dinosaurs, global ice ages, continents colliding or splitting apart, and comets and asteroids crashing catastrophically to the surface, as well as the birth of humans who are curious to understand it. But how was all this discovered? How was the evidence for it collected and interpreted? And what kinds of people have sought to reconstruct this past that no human witnessed or recorded? In this sweeping and accessible book, Martin J. S. Rudwick, the premier historian of the Earth sciences, tells the gripping human story of the gradual realization that the Earth's history has not only been unimaginably long but also astonishingly eventful. Rudwick begins in the seventeenth century with Archbishop James Ussher, who famously dated the creation of the cosmos to 4004 BC. His narrative later turns to the crucial period of the late eighteenth and early nineteenth centuries, when inquisitive intellectuals, who came to call themselves "geologists," began to interpret rocks and fossils, mountains and volcanoes, as natural archives of Earth's history. He then shows how this geological evidence was used and is still being used to reconstruct a history of the Earth that is as varied and unpredictable as human history itself. Along the way, Rudwick rejects the popular view of this story as a conflict between science and religion and shows how the modern scientific account of the Earth's deep history retains strong roots in Judaeo-Christian ideas. Extensively illustrated, Earth's Deep History is an engaging and impressive capstone to Rudwick's distinguished career. Though the story of the Earth is inconceivable in length, Rudwick moves with grace from the earliest imaginings of our planet's deep past to today's scientific discoveries, proving that this is a tale at once timeless and timely.
The studies in this second volume by Martin Rudwick (the first being The New Science of Geology: Studies in the Earth Science in the Age of Reform) focus on the figures of Charles Lyell and Charles Darwin. Lyell rose to be of pivotal importance in the second quarter of the 19th century because he challenged other geologists throughout Europe by probing their methods and conclusions to the limit. While adopting their goal of reconstructing the contingent history of the earth, he claimed that the physical processes observable in action in the present could explain far more about the past than was commonly believed, and that it was unnecessary to postulate occasional catastrophic events of still greater intensity. Far more controversial was Lyell's further claim that the earth and its life had always been in a stable steady state, rather than developing in a broadly linear or directional fashion. His younger friend Charles Darwin first made his name as a Lyellian geologist; Darwin's early work in geology, studied here, provided important foundations for his later and more famous research on speciation and other biological problems.
The science of geology was constructed in the decades around 1800 from earlier practices that had been significantly different in their cognitive goals. In the studies collected here Martin Rudwick traces how it came to be recognised as a new kind of natural science, because it was constituted around the idea that the natural world had its own history. The earth had to be understood not only in relation to unchanging natural laws that could be observed in action in the present, but also in terms of a pre-human past that could be reliably known, even if not directly observable and its traces only fragmentarily preserved. In contrast to this radically novel sense of nature's own contingent history, the earth's unimaginably vast timescale was already taken for granted by many naturalists (though not yet by the wider public), and the concurrent development of biblical scholarship precluded any significant sense of conflict with religious tradition. A companion volume, Lyell and Darwin, Geologists: Studies in the Earth Sciences in the Age of Reform, was published in 2005.
Until quite recently, French zoologist Georges Cuvier (1769-1832) opposed the biological theory of evolution, and championed the geological theory of catastrophism; but his research on fossils helped form and bring credibility to geology and palaeontology, and recent research has proved that his ideas on the importance of mass extinctions and catastrophes were well ahead of their time. In this volume, Martin Rudwick provides a modern translation of Cuvier's essential writings on fossils and catastrophes, together with two previously unpublished pieces. Rudwick links these translated texts together with his own narrative and interpretive commentary, placing Cuvier's work in its biographical, scientific, and social context. A major feature of this book is a translation of Cuvier's best-known work, the "Preliminary Discourse" (1812). Frequently reprinted and translated, this essay became a key document in 19th-century debates about evolutionary theory, and can still be used as source material by many English-speaking historians.
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