Abstract

Abstract Throughout much of earth history globally warm intervals prevailed over ice age conditions. Without the constraints imposed by cold climates, forest vegetation populated high-latitude land masses. There are no modern analogs for these biomes, thus fossil remains provide information vital to understanding the structure and function of these forests. This paper reviews methods (some common in neoecology) by which forest structure, biomass and productivity can be quantified from analysis of fossil remains. Common metrics of forest structure, such as stand density, stem diameter, basal area and tree height, can be determined for most fossil forest localities using the methods described herein. When fossils are preserved as in situ forest layers (so-called fossil forests), additional analyses involving detailed stem measurement or the application of allometric regression models may yield estimates of aboveground biomass. Annual growth rates, when paired with estimates of stem wood volume production, p...

Full Text
Paper version not known

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 call

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.