Temperature reconstructions for the distant past utilize various proxies, which are weighted differently based on their reliability and the specific time periods they represent. Some proxies, like tree rings, are limited by environmental factors such as moisture and CO2 levels, and their reliability can vary significantly. The current leading proxy for paleo-temperature is Tex86, but all proxies face challenges due to the complexity of climate variables. If tree ring data from the last 2,000 years were excluded, the overall temperature reconstruction would likely be only marginally affected, as other reliable proxies like ice cores, boreholes, corals, and sediment data are available. Research often focuses on periods that do not depend on tree rings, such as the Pliocene, where climate conditions were understood through different methods.