Abstract
Paleomagnetism presents the paleo-bioclimatologist for the first time with an independent determination of latitude. In combination with paleogeography a reconstruction of climatic zones for the geologic periods can be attempted by taking into account the principles underlying the present distribution of climate. This was attempted for the Permian of Europe and the Triassic, Permian and Pennsylvanian (U. Carboniferous) of North America. An extension of this method can be of great importance in future paleo-ecological and bioclimatological studies if the underlying principles of Paleomagnetism prove to be correct.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: International Journal of Bioclimatology Biometeorology
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
