Nearest living relative
The most obvious way to make inferences about the paleoenvironment and paleoclimate using vertebrate fossils is to note the modern environments and climate associated with their nearest living relatives. The presence in the fossil record of one or a few specimens of a single genus or species has been used in this way. Based on such evidence, Vucetich and Verzi (2002) asserted that during the Pleistocene there were warm pulses that enabled tropical forms now known only from Brazil to extend their ranges more than 1,200 km south to the area of Buenos Aires.
Instead of considering only one taxon, it is a more common practice to compare the paleoenvironmental and paleoclimatic preferences for the nearest living relatives of all taxa represented in a fossil assemblage. Using this method with modern small mammals, Antoñanzas and Bescós (2002) inferred that during the Early to Middle Pleistocene at Atapuerca, Burgos, Spain there were several cycles of fluctuation...
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Rich, T.H., Vickers-Rich, P. (2009). Animal Proxies, Vertebrates. In: Gornitz, V. (eds) Encyclopedia of Paleoclimatology and Ancient Environments. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-4411-3_6
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