In this book the first three chapters outline the chemistry of nickel and heme largely associated with anaerobic life and believed to represent reactions which took place some 3-4x109years ago. Nickel has disappeared from the chemistry of man. The fascinating detail of the "primitive" catalysts is of interest to industrial society since very simple feed-stock is used, hydrogen, carbon monoxide and sulphate for example. The fourth chapter switches attention to a metal which became valuable later in evolution, copper, and which is involved with the use of dioxygen. It also has extremely interesting catalytic sites in enzymes. The essence of the volume lies in an appreciation of metallo- enzymes and their changing roles as the environment changed.

The spectra of ferric haems and haemoproteins.- The absolute configuration of transition metal complexes.- The application of nuclear quadrupole resonance spectroscopy to the study of transition metal compounds.- Kationenverteilung zweiwertiger 3d n -ionen in oxidischen spinell-, granat- und anderen strukturen.

Valence-shell expansion studied by radio-frequency spectroscopy.- Ligand-field spectroscopy and chemical bonding in Cr3+-containing oxidic solids.- Spectra of 3d five-coordinate complexes.- Valence-shell expansion studied by ultra-violet spectroscopy.- Polynuclear complexes of iron and their biological implications.- Ionic radii and enthalpies of hydration of ions.

This book is written as an addition to Darwin's work and that of molecular biologists on evolution so as to include views of it from the point of view of chemistry rather than just from our knowledge of the biology and genes of organisms. By concentrating on a wide range of chemical elements, not just those in traditional organic compounds, we show that there is a close relationship between the geological or environmental chemical changes from the formation of Earth and those of organisms from the time of their origin. These are considerations which Darwin or other scientists could not have explored until very recent times since sufficient analytical data were not available. They lead us to suggest that there is a combined geo- and bio-chemical evolution, that of an ecosystem, which has had a systematic chemical development. In this development the arrival of new very similar species is shown to be by random Darwinian competitive selection processes such that a huge variety of species coexist with only minor differences in chemistry and advantages. This is in agreement with previous studies. On the large scale of evolution of very different organisms, and over greater timescales, by way of contrast, we observe that groups of species have special, different, chemical features and function. It is more difficult to understand how they evolved and therefore we examine their chemical development in detail. Overall there is a cooperative evolution of a chemical system driven by capture of energy, mainly from the sun, and its degradation in which the chemistry of both the environment and organisms are facilitating intermediates. We shall suggest that the overall drive of the whole joint system is to optimise the rate of this energy degradation. Since the environmental changes are inorganic and relatively fast they move inevitably to equilibrium. The living part of the system, the organisms, under the influence of this inevitable environmental change are forced to follow but as they are increasingly energised and their reactions are slow, they move further away from equilibrium. We are able to explore the ways in which this chemical system evolved, recognising that as complexity of the chemistry of organisms increased, they had to be formed from more and more compartments and to become part of a chemically cooperative overall activity. They could not remain as isolated species. Only in the last chapter do we attempt to make a connection between the changing chemistry of organisms with the coded molecules of each cell which have to exist to explain reproduction.

This fascinating and unique history reveals the major influence of the Oxford Chemistry School on the advancement of chemistry. It shows how the nature of the University, and individuals within it, have shaped the school and made great achievements both in teaching and research. The book will appeal to those interested in the history of science and education, the city of Oxford and chemistry in general. Chemistry has been studied in Oxford for centuries but this book focuses on the last 400 years and, in particular, the seminal work of Robert Boyle, Robert Hooke, and the proto- Royal Society of the 1650's. Arranged in chronological fashion, it includes specialist studies of particular areas of innovation. The book shows that chemistry has advanced, not just as a consequence of research but, because of the idiosynchratic nature of the collegiate system and the characters of the individuals involved. In other words, it demonstrates that science is a human endeavour and its advance in any institution is conditioned by the organization and people within it. For chemists, the main appeal will be the book's examination of the way separate branches of chemistry (organic, physical, inorganic and biological) have evolved in Oxford. It also enables comparison with the development of the subject at other universities such as Cambridge, London and Manchester. For historians and sociologists, the book reveals the motivations of both scientists and non-scientists in the management of the School. It exposes the unusual character of Oxford University and the tensions between science and administration. The desire of the college to retain its academic values in the face of external and financial pressures is emphasized.

Conventionally, evolution has always been described in terms of species. The Chemistry of Evolution takes a novel, not to say revolutionary, approach and examines the evolution of chemicals and the use and degradation of energy, coupled to the environment, as the drive behind it. The authors address the major changes of life from bacteria to man in a systematic and unavoidable sequence, reclassifying organisms as chemotypes. Written by the authors of the bestseller The Biological Chemistry of the Elements - The Inorganic Chemistry of Life, the clarity and precision of The Chemistry of Evolution plainly demonstrate that life is totally interactive with the environment. This exciting theory makes this work an essential addition to the academic and public library.
* Provides a novel analysis of evolution in chemical terms
* Stresses Systems Biology
* Examines the connection between life and the environment, starting with the 'big bang' theory
* Reorientates the chemistry of life by emphasising the need to analyse the functions of 20 chemical elements in all organisms

Conventionally, evolution has always been described in terms of species. The Chemistry of Evolution takes a novel, not to say revolutionary, approach and examines the evolution of chemicals and the use and degradation of energy, coupled to the environment, as the drive behind it. The authors address the major changes of life from bacteria to man in a systematic and unavoidable sequence, reclassifying organisms as chemotypes. Written by the authors of the bestseller The Biological Chemistry of the Elements - The Inorganic Chemistry of Life (Oxford University Press, 1991), the clarity and precision of The Chemistry of Evolution plainly demonstrate that life is totally interactive with the environment. This exciting theory makes this work an essential addition to the academic and public library.
* Provides a novel analysis of evolution in chemical terms
* Stresses Systems Biology
* Examines the connection between life and the environment, starting with the 'big bang' theory
* Reorientates the chemistry of life by emphasising the need to analyse the functions of 20 chemical elements in all organisms

This beautifully written book is a study of the intimate relationship between the inanimate environment and living organisms. It describes how the evolution of both has been interactive and interdependent: the environment and life developed together, The authors show that this can be explained in terms of the properties of the chemical elements and their compounds. It discusses the physical and chemical balances between the animate and inanimate worlds, with kinetic and thermodynamic principles given to support this analysis. These principles are applied to both organic and inorganic chemical systems to provide a basis for understanding the evolution of life in terms of the interaction of both types of chemistry within ever more complex organisations. The book conludes with an examination of an intriguing problem for mankind: the long-term consequences of man's selection and manipulation of chemicals. This may have consequences for the long-term future of life from changes in the environment - not just only due to bulk but also to trace element alterations.

This book places oxygen on the center stage of chemistry in a manner that parallels the focus on carbon by 19th century chemists. One measure of the significance of oxygen chemistry is the greater diversity of oxygen-containing molecules than of carbon-containing molecules. One of the most important compounds is water, containing the properties of being a unique medium for biological chemistry and life, the source of all the dioxygen in the atmosphere, and the moderator of the earth's climate. Sawyer first introduces the biological origins of dioxygen and role of dioxygen in aerobic biology and oxidative metabolism, and in separate chapters discusses the oxidation-reduction thermodynamics of oxygen species, and the nature of the bonding for oxygen in its compounds. Additional chapters focus on the reactivities of specific oxygen compounds. The book will be of interest to chemists and biochemists, as well as graduate students, life scientists, and medical researchers.

This text describes the functional role of the twenty inorganic elements essential to life in living organisms.

This book is written as an addition to Darwin's work and that of molecular biologists on evolution so as to include views of it from the point of view of chemistry rather than just from our knowledge of the biology and genes of organisms. By concentrating on a wide range of chemical elements, not just those in traditional organic compounds, we show that there is a close relationship between the geological or environmental chemical changes from the formation of Earth and those of organisms from the time of their origin. These are considerations which Darwin or other scientists could not have explored until very recent times since sufficient analytical data were not available. They lead us to suggest that there is a combined geo- and bio-chemical evolution, that of an ecosystem, which has had a systematic chemical development. In this development the arrival of new very similar species is shown to be by random Darwinian competitive selection processes such that a huge variety of species coexist with only minor differences in chemistry and advantages. This is in agreement with previous studies. On the large scale of evolution of very different organisms, and over greater timescales, by way of contrast, we observe that groups of species have special, different, chemical features and function. It is more difficult to understand how they evolved and therefore we examine their chemical development in detail. Overall there is a cooperative evolution of a chemical system driven by capture of energy, mainly from the sun, and its degradation in which the chemistry of both the environment and organisms are facilitating intermediates. We shall suggest that the overall drive of the whole joint system is to optimise the rate of this energy degradation. Since the environmental changes are inorganic and relatively fast they move inevitably to equilibrium. The living part of the system, the organisms, under the influence of this inevitable environmental change are forced to follow but as they are increasingly energised and their reactions are slow, they move further away from equilibrium. We are able to explore the ways in which this chemical system evolved, recognising that as complexity of the chemistry of organisms increased, they had to be formed from more and more compartments and to become part of a chemically cooperative overall activity. They could not remain as isolated species. Only in the last chapter do we attempt to make a connection between the changing chemistry of organisms with the coded molecules of each cell which have to exist to explain reproduction.