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Pine stump showing growth ringsDendrochronology or tree-ring dating is the method of scientific dating based on the analysis of tree ring patterns. This technique was invented and developed during the 20th century originally by Andrew E. Douglass, the founder of the Laboratory of Tree-Ring Research at the University of Arizona. This dating technique can give dates for wood in exact calendar years.
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Overview
Many trees in temperate zones grow one growth ring each year. For the entire period of a tree's life, a year-by-year record or ring pattern is formed that in some way reflects the climatic conditions in which the tree grew. Adequate moisture and a long growing season results in a wide ring. A drought year may result in a very narrow one. Trees from the same region will tend to develop the same patterns of width for a given period. These patterns can be compared and matched ring for ring with trees growing in the same geographical zone and under similar climatic conditions. Following these tree-ring patterns from living trees back through time, chronologies can be built up. We can thus compare wood from old or ancient structures to our known chronologies, match the ring patterns (a technique called cross-dating), and determine precisely the age of the wood used by the ancient builder. Cross dating was originally done by just visual inspection. Later statistical methods were added to select samples to be visually inspected. Nowadays, computers are used to do the statistical matching. Manual visual inspection is always done in the end.
In practice, to eliminate individual variations in tree ring growth, dendrochronologists take the smoothed average of the tree ring widths of multiple tree samples to build up a ring history. This process is termed replication. A tree ring history whose beginning and end dates are not known is called a floating chronology. It can be anchored by cross-matching either the beginning or the end section against the end sections of another chronology (tree ring history) whose dates are known. Fully anchored chronologies which extend back more than 10000 years exist for river oak trees from South Germany (from the Main and Rhine rivers). A fully anchored chronology which extends back 8500 years exists for the bristlecone pine in the southwest US (White Mountains of California).
In areas where the climate is reasonably predictable, trees develop annual rings of different properties depending on weather, rain, temperature, etc. in different years. These variations may be used to infer past climate variations — see dendroclimatology.
More detail
Laboratory analysis of timber core samples measures the width of annual rings. By taking samples from different sites and different strata within a particular region, researchers can build a comprehensive historical sequence that becomes a part of the scientific record; for example, ancient timbers found in buildings can be dated to give an indication of when the source tree was alive and growing, setting an upper limit on the age of the wood. Some trees are more suitable than others for this type of analysis. Likewise, in areas where trees grew in marginal conditions such as aridity or semi-aridity, the techniques of dendrochronology are more consistent than in humid areas. These tools have been important in archaeological dating of timbers of the cliff dwellings of Native Americans in the arid Southwest.
Scientific value
A benefit of dendrochronology is that it makes available specimens of once-living material accurately dated to a specific year to be used as a calibration and check of radiocarbon dating. The bristlecone pine, being exceptionally long-lived and slow growing, has been used for this purpose, with still-living and dead specimens providing tree ring patterns going back thousands of years. For dating purposes, in some regions sequences of more than 10,000 years are available.
The dendrochronologist faces many obstacles, however, including some species of ant which inhabit trees and extend their galleries into the wood, thus destroying ring structure.
Similar seasonal patterns also occur in ice cores and in varves (layers of sediment deposition in a frozen-over/ vs ice-free "lake" /fine sediments vs coarse). These are used for dating in a manner similar to dendrochronology, and such techniques are used in combination with dendrochronology, to plug gaps and to extend the range of the seasonal data available to archeologists.
One problem that archaeologists have when using dendrochronology is that while they can use the technique to age the piece of wood, and when it was felled, it may be difficult to use that to definitively determine the age of a building or structure that the wood is in. The wood could have been used for something else first, may have been felled and left for many years before use, or could have been used to replace an older rotten or broken piece of wood.
See also
External links
- The Laboratory of Tree-Ring ReSearch with Google
- Wiener Laboratory for Aegean and Near Eastern Dendrochronology at Cornell University website
- Dendrochronology on musical instruments and art objects
- University of Tennessee Dendrochronology
- Oxford Dendrochronology Laboratory
- Online Glossary of Dendrochronology