Dendrochronology of Cypress (Taxodium spp.)

A special issue of Forests (ISSN 1999-4907). This special issue belongs to the section "Forest Ecophysiology and Biology".

Deadline for manuscript submissions: closed (21 April 2022) | Viewed by 413

Special Issue Editor


E-Mail Website
Guest Editor
United States Department of Agriculture, Center for Bottomland Hardwoods Research, Stoneville, MS, USA
Interests: dendroecology; dendrochemistry; endangered tree and shrub species

Special Issue Information

Dear Colleagues,

Tree rings can provide a record of the effects of climate on growth and indicate disturbances in the environment caused by fire, insects, or pollution for example. Tree ring chronologies have been employed for climate reconstruction, to date ancient structures, and to document the presence and effects of chemical deposition in annual tree rings, among other uses.

Cypress is a long-lived gymnosperm that occurs in wetlands in parts of the United States and farther south.  Swamp cypress (Taxodium distichum) and pond cypress (T. ascendens) occur in the southeastern United States and Montezuma cypress (T. mucronatum) occurs in Mexico and southeastern Guatemala. Cypress tree ring chronologies have been applied to a broad range of problems in recent years. This Special Issue will include articles on the various ways cypress chronologies have been used to provide information that has not been obtainable by other methods.

Dr. Margaret Devall
Guest Editor

Manuscript Submission Information

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Keywords

  • pond cypress
  • T. Ascendens
  • Montezuma cypress
  • T. Mucronatum
  • dendroecology
  • dendrochemistry
  • bald cypress
  • tree rings
  • tree ring chronologies

Published Papers

There is no accepted submissions to this special issue at this moment.
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