Quaternary dating methods mike walker
His most recent book is Quaternary Dating Methods, (John Wiley, Chichester & New York, 2005). He has published more than 140 scientific papers and other contributions, and is co-author of two Quaternary textbooks: Reconstructing Quaternary Environments (with John Lowe), (1st edition, Longman, 1984; 2nd edition, Addison-Wesley-Longman, 1997), and Late Quaternary Environmental Change: Physical and Human Perspectives (with Martin Bell), (1st edition, Longman, 1992; 2nd edition, Pearson International, 2005). Formal subdivision of the Holocene Series/ Epoch: a Discussion Paper by a Working Group of INTIMATE (Integration of ice-core marine and terrestrial records) and the Subcommission on Quaternary Stratigraphy (International Commission on Stratigraphy). He has been President of the Quaternary Research Association of Great Britain (1999-2002), and Editor of Journal of Quaternary Science (1995-1999). He continues to serve on the Editorial Board of Journal of Quaternary Science (John Wiley) and is a former member of the Editorial Board of Quaternary Science Reviews (Elsevier: 2000-2005).
This introductory textbook introduces the basics of dating, the range of techniques available and the strengths and limitations of each of the principal methods.
That is, it is these methods are used for dates up to around 2.5 million years ago. There are numerous examples that are in-depth, for each dating method discussed in the book.
For example, actual tree ring data (dendochronology) used to detect and estimate climate changes throughout Europe, Asian, and North America.
The coverage includes: the concept of time in Quaternary Science and related fields; the history of dating from lithostratigraphy and biostratigraphy; the development and application of radiometric methods; and, different methods in dating: radiometric dating, incremental dating, relative dating and age equivalence.
Presented in a clear and straightforward manner with the minimum of technical detail, this text is a great introduction for both students and practitioners in the Earth, Environmental and Archaeological Sciences.This is addressed by defining the standard to be 0.95 times the activity of HOx I.