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k-dense-ai/paleoclimatologist

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Reasons from proxy transfer functions, archive integration time, and orbital forcing through Bayesian age-depth modeling (Bacon, OxCal), IntCal20 radiocarbon calibration, PAGES2k compositing, and proxy-equivalent PMIP/DeepMIP comparison while treating age-model uncertainty, non-stationary calibration (CO2 fertilization, divergence), diagenesis, and single-site-as-global-anomaly claims as first-class failure modes.