干旱区生态环境知识资源中心

Stable oxygen isotopes from fossils, both vertebrate and invertebrate, or inorganic sedimentary minerals frequently have been used to make interpretations about ancient global climates. Oxygen isotope values measured from terrestrial vertebrates or sedimentary carbonates provide information about paleotemperature and amounts of precipitation at a particular site. In general, these inferences are made on the centennial to millennial scale.

Serial, i.e. ontogenetic, sampling of Equus and Bison tooth enamel provides climatic data on the scale of months to a few years. We present models showing bow annual environmental patterns of delta(18)O would be replicated in the tooth enamel of Equus and Bison. Changes in delta(18)O due to shifts in temperature (in terrestrial environments delta(18)O increases with increased temperature) and amount and timing of precipitation (increased precipitation may result in a decrease in delta(18)O- a phenomenon called the "Amount Effect") are archived in both Equus and Bison teeth. The input signal is better resolved in Bison due to its more rapid enamel growth.

Modeled patterns are compared with actual data from modem sites in the Sonoran and Chihuahuan deserts of the southwesten United States. The isotopic patterns from modem teeth agree with that predicted from known variations in meteoric water. Known floral and faunal assemblages as well as computer models suggest summer rain for the Chihualuan Desert of Late Glacial time (15,000- 10,000 years ago), but little summer rain for the Sonoran Desert at that same time. Serial data from fossil teeth show a clear pattern interpreted to represent the Amount Effect that includes increased summer rains in the Chihuahuan Desert and only minor summer rains in the Sonoran Desert. (C) 2004 Elsevier B.V. All rights reserved.