Non-mammalian synapsids were the dominant terrestrial vertebrates from the Late Carboniferous to the Middle Triassic and play a key role in understanding the origin and evolution of mammals. Despite these facts and the outstanding fossil record of the group, early synapsids remain obscure. This book showcases the full breadth of contemporary research on non-mammalian synapsids, ranging from taxonomy and phylogenetics to functional morphology, biogeography, paleoecology, and patterns of diversity. It also underscores the importance and potential of studying non-mammalian synapsid paleobiology in its own right, not just in the context of mammalian evolution.

Reconstructing the paleobiology of fossil non-human primates, this book is intended as an exposition of non-human primate evolution that includes information about evolutionary theory and processes, paleobiology, paleoenvironment, how fossils are formed, how fossils illustrate evolutionary processes, the reconstruction of life from fossils, the formation of the primate fossil record, functional anatomy, and the genetic bases of anatomy. Throughout, the emphasis of the book is on the biology of fossil primates, not their taxonomic classification or systematics, or formal species descriptions. The author draws detailed pictures of the paleoenvironment of fossil primates, including contemporary animals and plants, and ancient primate communities, emphasizing our ability to reconstruct lifeways from fragmentary bones and teeth, using functional anatomy, stable isotopes from enamel and collagen, and high resolution CT-scans of the cranium. Fossil Primates will be essential reading for advanced undergraduates and graduate students in evolutionary anthropology, primatology and vertebrate paleobiology.

Georges Cuvier (1769-1832), one of the founding figures of vertebrate palaeontology, pursued a successful scientific career despite the political upheavals in France during his lifetime. In the 1790s, Cuvier's work on fossils of large mammals including mammoths enabled him to show that extinction was a scientific fact. In 1812 Cuvier published this collection of his geological and osteological papers, focusing on living and extinct pachyderms, ruminants, horses and pigs. Volume 1 begins with a substantial essay on human origins and the formation of the earth, which was translated into English by Robert Kerr in 1813 (also available). It also includes an essay on the Egyptian ibis mummy brought back from Napoleon's campaign in Egypt, and an updated version of Cuvier's influential 1810 geological description of the Paris basin, co-authored with Alexandre Brogniart (1770-1847), which helped establish the principle of faunal succession in rock strata of different ages.

Georges Cuvier (1769-1832), one of the founding figures of vertebrate palaeontology, pursued a successful scientific career despite the political upheavals in France during his lifetime. In the 1790s, Cuvier's work on fossils of large mammals including mammoths enabled him to show that extinction was a scientific fact. In 1812 Cuvier published this four-volume illustrated collection of his papers on palaeontology, osteology and stratigraphy. It was followed in 1817 by his famous Le regne animal, available in the Cambridge Library Collection both in French and in Edward Griffith's expanded English translation (1827-35). Volume 2 of Recherches sur les ossemens fossiles describes eleven species of pachyderm found in recent alluvial deposits. They include elephants, mastodons, rhinoceros, hippopotamus, tapir and the hyrax (which Cuvier classified as an ungulate rather than a rodent). Cuvier argued from osteological comparisons with living species that all should be considered distinct species in their own right.

Georges Cuvier (1769-1832), one of the founding figures of vertebrate palaeontology, pursued a successful scientific career despite the political upheavals in France during his lifetime. In the 1790s, Cuvier's work on fossils of large mammals including mammoths enabled him to show that extinction was a scientific fact. In 1812 Cuvier published this four-volume illustrated collection of his papers on palaeontology, osteology (notably dentition) and stratigraphy. It was followed in 1817 by his famous Le regne animal, available in the Cambridge Library Collection both in French and in Edward Griffith's expanded English translation (1827-35). Volume 3 of Recherches sur les ossemens fossiles recounts Cuvier's excitement at acquiring fossils from gypsum quarries near Paris, and the challenges of piecing the fragments together correctly. Cuvier describes the methodical reconstruction of the pachyderm fossils and lists other fossils occurring in the same rock formations: carnivores, an opossum, birds, reptiles, and fish.

Georges Cuvier (1769-1832), one of the founding figures of vertebrate palaeontology, pursued a successful scientific career despite the political upheavals in France during his lifetime. In the 1790s, Cuvier's work on fossils of large mammals including mammoths enabled him to show that extinction was a scientific fact. In 1812 Cuvier published this four-volume illustrated collection of his papers on palaeontology, osteology (notably dentition) and stratigraphy. It was followed in 1817 by his famous Le regne animal, available in the Cambridge Library Collection both in French and in Edward Griffith's expanded English translation (1827-35). Volume 4 of Recherches sur les ossemens fossiles focuses first on ruminants, horses and pigs. Cuvier then discusses fossils of carnivores, including bears, hyenas and big cats. The book concludes by describing fossil sloths, and the oviparous reptiles found in older strata, such as crocodiles, turtles, and marine dinosaurs.

This monograph on the Central European Magdalenian aims to provide a comprehensive overview of the archaeological record of this period. It sheds new light on five regional groups between the Rhône valley to the west and the Vistula-valley to the east, which existed roughly between 20,000 and 14,000 years ago. Readers will discover that these groups are characterized with regard to their environmental setting (including faunal and vegetational aspects), lithic raw material and mollusk shell procurement, typology, technology and artesian craftworks. The work also explores an alternative interpretation of bidirectional recolonization from both Franco-Cantabria and Eastern Central Europe after the Last Glacial Maximum. This book will appeal to researchers and scholars in archaeology and cognate fields.

This book broadens readers' understanding of the stratigraphic framework and structural styles for improved hydrocarbon prospectivity in the intermediate and deeper horizons of the eastern Coastal Swamp Depo-belt of Nigeria's Niger Delta Basin. It equips readers to interpret complex sedimentary units, such as the paralic sequence of the Niger Delta Basin, using sequence stratigraphic tools integrated with well logs, biostratigraphic, paleobathymetric and seismic data. It also offers numerous tips and insights into reservoirs, seals, source rocks and hydrocarbon-type trends/distribution across several production fields, and provides a valuable guide to support exploration and production.

This book provides an overview, research compendium and an introduction to the science of molecular paleontology, including literature overview for non-geochemists. Analytical methods employed are included as a part of each chapter that underpin this branch of paleontology and indeed geochemistry. The primary usefulness of this volume is for organic geochemists, molecular palaeontologists, and molecular archeologists. Researchers, graduate students and academics interested in astrobiology from a paleontological perspective may also find this to be valuable.

For the physician and natural historian John Woodward (c.1655-1728), fossils were the key to unlocking the mystery of the Earth's past, which he attempted to do in this controversial work, first published in 1695 and here reissued in the 1723 third edition. Woodward argues that the 'whole Terrestrial Globe was taken all to Pieces, and dissolved at the Deluge', and that fossilised remains were proof of the flood as described in the Bible. In the first part of the work, Woodward examines other theories of the Earth's history before presenting evidence - much of it based on his own fossil collection - in support of his theory. The work immediately prompted heated debate among his scientific contemporaries. Despite the controversy, Woodward was acknowledged as an expert on fossil classification, cementing this reputation with his influential Fossils of All Kinds (1728), which is also reissued in the Cambridge Library Collection.

Barthelemy Faujas de Saint-Fond (1741 1819) abandoned the legal profession to pursue studies in natural history. Appointed a royal commissioner of mines in 1785, he also served as professor of geology at the natural history museum in Paris from 1793 until his death. His keen interest in rocks, minerals and fossils led to a number of important discoveries, among which was confirmation that basalt was a volcanic product. The present work appeared in three parts between 1803 and 1809. The second volume was divided into two. This second part lists the principal active volcanoes around the world and classifies volcanic products. Of related interest in the history of geology, Mineralogie des volcans (1784) and the revised English edition of A Journey through England and Scotland to the Hebrides in 1784 (1907) are two other works by Faujas which are also reissued in this series."

This book provides a summary of the discoveries made during the course of excavations at the Paleolithic cave site of Fontechevade, France, between 1994 and 1998. The excavation team used modern field and analytic methods to address major problems raised by earlier excavations at the site from 1937 to 1954. These earlier excavations produced two sets of data that have been problematic in light of data from other European Paleolithic sites: first, the Lower Paleolithic stone tool industry, the Tayacian, that differs in fundamental ways from other contemporary industries and, second, the human skull fragment that has been interpreted as modern in nature but that apparently dates from the last interglacial, long before there is any evidence for humans from any other site in Europe. By applying modern stratigraphic, lithic, faunal, geological, geophysical, and radiometric analyses, the interdisciplinary team demonstrates that the Tayacian industry is a product of site formation processes and that the actual age of the Fontechevade I fossil is compatible with other evidence for the arrival of modern humans in Europe."

Recent genetic data showing that Neanderthals interbred with modern humans have made it clear that deeper insight into the behavioral differences between these populations will be critical to understanding the rapid spread of modern humans and the demise of the Neanderthals. This volume, which brings together scholars who have worked with faunal assemblages from Europe, the Near East, and Africa, makes an important contribution to our broader understanding of Neanderthal extinction and modern human origins through its focus on variability in human hunting behavior between 70-25,000 years ago-a critical period in the later evolution of our species.

Originally published in 1921, this book presents a detailed account 'of the two Devonian land floras'. Illustrative figures and textual notes are incorporated throughout. This book will be of value to anyone with an interest in the Devonian period, botany and the history of science.

What can the interactions of ancient mammals and their environments tell us about the present-and the future? Classic paleontology has focused on the study of fossils and the reconstruction of lineages of extinct species. But as diverse fossils of animals and plants were unearthed and catalogued, it became possible to reconstruct more elaborate ecosystems, tying together plants, animals, and geology. By the second half of the twentieth century, this effort gave birth to the field of paleoecology: the study of the interactions between organisms and their environments across geologic timescales. In Mammalian Paleoecology, Felisa Smith broadly considers extinct mammals in an ecological context. Arguing that the past has much to teach us and that mammals, which display an impressive array of diverse life history and ecological characteristics, are the ideal organism through which to view the fossil record, Smith * reviews the history, major fossil-hunting figures, and fundamental principles of paleoecology, including stratigraphy, dating, and taphonomy * discusses the importance of mammal body size, how to estimate size, and what size and shape reveal about long-dead organisms * explains the structure, function, and utility of different types of mammal teeth * highlights other important methods and proxies used in modern paleoecology, including stable isotopes, ancient DNA, and paleomidden analyses * assesses nontraditional fossils * presents readers with several case studies that describe how the fossil record can help inform the scientific discussion on anthropogenic climate change Mammalian Paleoecology is an approachable overview of how we obtain information from fossils and what this information can tell us about the environments of the distant past. It will profoundly affect the way paleontologists and climatologists view the lives of ancient mammals.

This book is divided in two parts, the first of which shows how, beyond paleontology and systematics, macroevolutionary theories apply key insights from ecology and biogeography, developmental biology, biophysics, molecular phylogenetics and even the sociocultural sciences to explain evolution in deep time. In the second part, the phenomenon of macroevolution is examined with the help of real life-history case studies on the evolution of eukaryotic sex, the formation of anatomical form and body-plans, extinction and speciation events of marine invertebrates, hominin evolution and species conservation ethics. The book brings together leading experts, who explain pivotal concepts such as Punctuated Equilibria, Stasis, Developmental Constraints, Adaptive Radiations, Habitat Tracking, Turnovers, (Mass) Extinctions, Species Sorting, Major Transitions, Trends and Hierarchies – key premises that allow macroevolutionary epistemic frameworks to transcend microevolutionary theories that focus on genetic variation, selection, migration and fitness. Along the way, the contributing authors review ongoing debates and current scientific challenges; detail new and fascinating scientific tools and techniques that allow us to cross the classic borders between disciplines; demonstrate how their theories make it possible to extend the Modern Synthesis; present guidelines on how the macroevolutionary field could be further developed; and provide a rich view of just how it was that life evolved across time and space. In short, this book is a must-read for active scholars and because the technical aspects are fully explained, it is also accessible for non-specialists. Understanding evolution requires a solid grasp of above-population phenomena. Species are real biological individuals and abiotic factors impact the future course of evolution. Beyond observation, when the explanation of macroevolution is the goal, we need both evidence and theory that enable us to explain and interpret how life evolves at the grand scale.

To the naturalist John Woodward (c.1665 1728), fossils were 'much neglected, and left wholly to the Care and Treatment of Miners and meer Mechanicks'. He had built up a large personal collection of these samples of the Earth's petrified remains and spent much of his life developing a system for their classification, the results of which were published in this important illustrated work of 1728. A distinguished physician and a fellow of the Royal Society, Woodward wrote extensively on scientific topics, and had developed a theory that fossils were creatures destroyed in the flood described in the Bible. These ideas attracted critics and supporters in equal measure, but his contribution to techniques of fossil collection and classification were influential. In the present work, he devotes the early chapters to questions of description and classification, while the later sections contain some of his letters to his scientific contemporaries, including Isaac Newton."

Employed early on in his career by Sir Joseph Banks, the botanist John Lindley (1799 1865) went on to conduct important research on the orchid family and also recommended that Kew Gardens should become a national botanical institution. This pioneering three-volume work of palaeobotany, first published between 1831 and 1837, catalogues almost 300 species of fossil plants from the Pleistocene to the Carboniferous period. The geologist and palaeontologist William Hutton (1797 1860), with whom Lindley collaborated, was responsible for collecting the fossil specimens from which the 230 plates were drawn. The first serious attempt at organising and interpreting the evidence of Britain's primeval plant life, this resource is notable also for its prefatory discussion of topics such as coal seams and prehistoric climate. Volume 1 opens with a context-setting introduction and list of genera, followed by the descriptions of plates 1-79."

Employed early on in his career by Sir Joseph Banks, the botanist John Lindley (1799 1865) went on to conduct important research on the orchid family and also recommended that Kew Gardens should become a national botanical institution. This pioneering three-volume work of palaeobotany, first published between 1831 and 1837, catalogues almost 300 species of fossil plants from the Pleistocene to the Carboniferous period. The geologist and palaeontologist William Hutton (1797 1860), with whom Lindley collaborated, was responsible for collecting the fossil specimens from which the 230 plates were drawn. The first serious attempt at organising and interpreting the evidence of Britain's primeval plant life, this resource is notable also for its prefatory discussion of topics such as coal seams and prehistoric climate. Volume 2 opens with a preface on coal, followed by descriptions of some of the fossil plants found therein (plates 80-156)."

Employed early on in his career by Sir Joseph Banks, the botanist John Lindley (1799 1865) went on to conduct important research on the orchid family and also recommended that Kew Gardens should become a national botanical institution. This pioneering three-volume work of palaeobotany, first published between 1831 and 1837, catalogues almost 300 species of fossil plants from the Pleistocene to the Carboniferous period. The geologist and palaeontologist William Hutton (1797 1860), with whom Lindley collaborated, was responsible for collecting the fossil specimens from which the 230 plates were drawn. The first serious attempt at organising and interpreting the evidence of Britain's primeval plant life, this resource is notable also for its prefatory discussion of topics such as coal seams and prehistoric climate. Volume 3 includes a note on the action of water on plants. This is followed by the descriptions of plates 157 230."

Carina Klein examines the quality of the existing modern ammonoid zonation based on three methods, being Unitary Associations (UA), Constrained Optimization (CONOP) as well as Ranking and Scaling (RASC). The author sets out which of these three methods is best suitable to refine these zones. The results obtained are compared to each other with regard to ammonoid succession and resolution as well as with empirical data from selected reference sections. The analysis reveals that the UA and RASC methods are the most suitable since the results best mirror the empirical data from the single outcrops.

Bryophytes, which are important constituents of ecosystems globally and often dominate carbon and water dynamics at high latitudes and elevations, were also among the pioneers of terrestrial photosynthesis. Consequently, in addition to their present day ecological value, modern representatives of these groups contain the legacy of adaptations that led to the greening of Earth. This volume brings together experts on bryophyte photosynthesis whose research spans the genome and cell through whole plant and ecosystem function and combines that with historical perspectives on the role of algal, bryophyte and vascular plant ancestors on terrestrialization of the Earth. The eighteen well-illustrated chapters reveal unique physiological approaches to achieving carbon balance and dealing with environmental limitations and stresses that present an alternative, yet successful strategy for land plants.

In a one-stop resource, this book provides a state-of-the-art overview of all aspects of pure and applied forams studies. Building from introductory chapters on the history of foraminiferal research, and research methods, the book then takes the reader through biology, ecology, palaeoecology, biostratigraphy and sequence stratigraphy. This is followed by key chapters detailing practical applications of forams in petroleum geology, mineral geology, engineering geology, environmental science and archaeology. All applications are fully supported by numerous case studies selected from around the world, providing a wealth of real-world data. The book also combines lavish illustrations, including over seventy stunning original picture-diagrams of foraminifera, with comprehensive references for further reading, and online data tables providing additional information on hundreds of foram families and species. Accessible and practical, this is a vital resource for graduate students, academic micropalaeontologists and professionals across all disciplines and industry settings which make use of foram studies.

Dinosaur bones had been found centuries before scientists understood what they were and what creatures they came from; ancient Chinese writings spoke of 'dragon' bones, and large fossils discovered in the UK were thought to belong to human giants. It was only with the exploration and meticulous research of generations of intrepid palaeontologists that the truth about dinosaurs was discovered.

The Dinosaur Hunters tells the story of these discoverers of prehistoric life, and the revelations found through their research. Illustrated with 30 rare documents, photographs and hand-drawn maps, it explores the unearthing of Iguanodon teeth, the discovery of the first flying dinosaur, the infamous Bone Wars and consultant editor Dr Mark Norell's radical study of feathered dinosaurs. This is a tale of daring exploits, luck, science and wanderlust, and of the thrilling lives and work of heroic scientists and adventurers.

Louis Figuier (1819-94) was destined to remain in academia until disagreements with fellow scholars led him to abandon this path and instead pursue 'the idea that scientific knowledge, which until then had been almost exclusively the property of the learned, should be put within the reach of the reading public'. Published in 1863, La Terre avant le deluge became a classic of popular science and introduced palaeontology to a wider readership; that this English translation appeared only two years later is an indication of its impact. Figuier wrote that his aim was 'to trace the progressive steps by which the earth has reached its present state ... and to describe the various convulsions and transformations through which it has successively passed'. The book was also celebrated for its inclusion of more than 200 illustrations by a pupil of Dore, Edouard Riou (1833-1900), who became famous as Jules Verne's illustrator a few years later.