Within the geological science of paleoclimatology, the earth's
pre-Quaternary period--more than two million years ago--has been studied
systematically only since the 1960's, when geologists started to take
seriously the concept that the continents have changed position on the
earth's surface. In the decades since, the study of pre-Quaternary
paleoclimatology has expanded greatly. A wide variety of methods have
been developed to study pre-Quaternary climates, but until now, no
single text has sought to synthesize those methods.
Judith Totman Parrish's text offers a much-needed entry point into the
literature. While a number of previous books have dealt with climate
models and paleoclimate, this is the first to offer a sustained
exploration of the methods that are the foundation of any interpretation
of earth processes. Focusing primarily on the description and analysis
of paleoclimatic indicators-signals of a particular climate--this
valuable reference work offers detailed explanations of biotic and
lithologic indicators in the marine and terrestrial realms and includes
case histories of paleoclimatic studies.
The most up-to-date and comprehensive volume on the subject,
Interpreting Pre-Quaternary Climatefrom the Geologic Record will be an
important resource for students and scientists alike. Parrish's focus on
the established, underexploited, and controversial methods bring to
light a spectrum of potential new avenues of research in this field.