Linked from

The 24 pages that link to Paleoclimate proxy, each with the reason it gives.

• PaleoclimatologyNarrower topic: Proxy records provide paleoclimatology’s evidence when direct measurements do not exist.

• Last Glacial MaximumNarrower topic: Different proxies capture distinct aspects of LGM climate and can yield differing reconstructions.

• PaleoclimateNarrower topic: Paleoclimate depends on indirect records that translate physical traces into climate estimates.

• PlioceneNarrower topic: Proxy records underpin estimates of Pliocene temperatures, ice volume, and rainfall.

• African Humid PeriodNarrower topic: Proxy records differ in resolution and can yield contrasting regional chronologies.

• K–Pg boundaryNarrower topic: Proxy records help distinguish volcanic climate effects from abrupt impact-related changes.

• Faint young Sun paradoxNarrower topic: Temperature and atmospheric estimates depend on interpreting sparse ancient proxies.

• Antarctic glaciationNarrower topic: Proxy records provide indirect estimates of early Antarctic ice volume and temperature.

• Michael E. MannNarrower topic: Mann combined proxy records to estimate temperatures before thermometer coverage.

• Hirnantian glaciationNarrower topic: Isotopes and sedimentary features help reconstruct this glaciation’s timing and intensity.

• Holocene climatic optimumNarrower topic: Proxy records supply the temperature and precipitation evidence for this interval.

• Late Paleozoic icehouseNarrower topic: Glacial deposits and other proxies allow the icehouse's climate history to be reconstructed.

• Older DryasNarrower topic: The interval is reconstructed from indirect records rather than direct temperature measurements.