The Early Settlement of North America is an examination of the first recognisable culture in the New World: the Clovis complex. Gary Haynes begins his analysis with a discussion of the archaeology of Clovis fluted points in North America and a review of the history of the research on the topic. He presents and evaluates all the evidence that is now available on the artefacts, the human populations of the time, and the environment, and he examines the adaptation of the early human settlers in North America to the simultaneous disappearance of the mammoths and mastodonts. Haynes offers a compelling re-appraisal of our current state of knowledge about the peopling of this continent and provides a significant new contribution to the debate with his own integrated theory of Clovis, which incorporates vital new biological, ecological, behavioural and archaeological data.
The diminishing populations of African and Asian elephants call to mind the extinctions of other elephantlike species, such as mammoths and mastodons, that occurred more than 10000 years ago. The purpose of this book is to examine the ecology and behaviour of modern elephants to create models for reconstructing the lives and deaths of extinct mammoths and mastodons. The sources for these models are long-term continuing studies of elephants in Zimbabwe, Africa. These models are clearly described with respect to the anatomical, behavioural, and ecological similarities between past and present proboscideans. The implications of these similarities for the lives and deaths of mammoths and mastodons are explored in detail. The importance of this book is primarily its unifying perspective on living and extinct proboscideans: The fossil record is as carefully examined as is the natural history of surviving elephants. Dr Haynes's studies of the situations in which African elephants die (sometim
The volume contains summaries of facts, theories, and unsolved problems pertaining to the unexplained extinction of dozens of genera of mostly large terrestrial mammals, which occurred ca. 13,000 cal
