This book offers a distinct framework for understanding the global past through the study of origins, interactions, and adaptations. The authors examine the full range of human ingenuity over time and space in a comprehensive, even-handed, and critical fashion.

From the author and designer of "ROY G. BIV," a delightful, fully illustrated new volume on patterns, from polka dots to plaid: their histories, cultural resonances, and hidden meanings.

Why does the West rule? In this magnum opus, eminent Stanford polymath Ian Morris answers this provocative question, drawing on 50,000 years of history, archeology, and the methods of social science, to make sense of when, how, and why the paths of development differed in the East and West — and what this portends for the 21st century. There are two broad schools of thought on why the West rules. Proponents of "Long-Term Lock-In" theories such as Jared Diamond suggest that from time immemorial, some critical factor — geography, climate, or culture perhaps — made East and West unalterably different, and determined that the industrial revolution would happen in the West and push it further ahead of the East. But the East led the West between 500 and 1600, so this development can't have been inevitable; and so proponents of "Short-Term Accident" theories argue that Western rule was a temporary aberration that is now coming to an end, with Japan, China, and India resuming their rightful places on the world stage. However, as the West led for 9,000 of the previous 10,000 years, it wasn't just a temporary aberration. So, if we want to know why the West rules, we need a whole new theory. Ian Morris, boldly entering the turf of Jared Diamond and Niall Ferguson, provides the broader approach that is necessary, combining the textual historian's focus on context, the anthropological archaeologist's awareness of the deep past, and the social scientist's comparative methods to make sense of the past, present, and future — in a way no one has ever done before.

Encouraging a broad understanding of continuity, change, and innovation in human history, Patterns in World History presents the global past in a comprehensive, even-handed, and open-ended fashion. Instead of focusing on the memorization of people, places, and events, this text strives topresent important facts in context and draw meaningful connections by examining patterns that have emerged throughout global history.

This work summarizes an ongoing longitudinal study concerned with the nature of human differences as manifest in peoples' life histories. The traditional models for the description of human differences are reviewed, then contrasted with the presentation of alternative models. This volume is also one of the few to investigate different approaches to measurement procedures. Practical applications of these models and the results obtained in a 23 research effort are discussed.

Hypothesis testing is not a straightforward matter in the fossil record and here, too interactions with biology can be extremely profitable. Quite simply, predictions regarding long-term consequences of processes observed in liv ing organisms can be tested directly using paleontological data if those liv ing organisms have an adequate fossil record, thus avoiding the pitfalls of extrapolative approaches. We hope to see a burgeoning of this interactive effort in the coming years. Framing and testing of hypotheses in paleon tological subjects inevitably raises the problem of inferring process from pattern, and the consideration and elimination of a broad range of rival hy is an essential procedure here. In a historical science such as potheses paleontology, the problem often arises that the events that are of most in terest are unique in the history of life. For example, replication of the metazoan radiation at the beginning of the Cambrian is not feasible. How ever, decomposition of such problems into component hypotheses may at least in part alleviate this difficulty. For example, hypotheses built upon the role of species packing might be tested by comparing evolutionary dy namics (both morphological and taxonomic) during another global diversi fication, such as the biotic rebound from the end-Permian extinction, which removed perhaps 95% of the marine species (see Valentine, this volume). The subject of extinction, and mass extinction in particular, has become important in both paleobiology and biology.