Carbon and oxygen isotopic variability in Neogene paleosol carbonates: constraints on the evolution of the C 4-grasslands of the Great Plains, USA

Abstract

Understanding the development of grassland ecosystems is critical for understanding the evolution of their associated vertebrate faunas. We focus on the central and southern portions of the Great Plains, which is the largest continuous grassland in North America and has a well-documented mammalian fossil record. Modern biomass in this region is dominated by C 4 grasses, but paleontological evidence indicates the region was forested prior to the middle Miocene, implying the region was formerly dominated by C 3 plants. We examine long- and short-term variations in the abundance of C 4 grasses and climatic conditions in the central and southern Great Plains using the stable carbon and oxygen isotope composition of paleosol carbonates from 28 sections of 11 lithostratigraphic units in the region. The carbon isotope composition ( δ 13C) of paleosol carbonate reflects the proportion of C 3 and C 4 plants that grew in an ancient soil. The long-term pattern of δ 13C values indicates that the percentage of C 4 grasses in the Great Plains was moderate (ca. 20%) throughout most of the Miocene, increased from 6.4 to 4.0 Ma, and reached modern levels by 2.5 Ma. Based on the range in δ 13C values within sections and the mean δ 13C values for different carbonate morphologies that reflect different intervals of carbonate accumulation, the abundance of C 4 biomass did not vary substantially on short time scales. The variability in C 4 biomass on short time scales does not correlate with age of section, latitude, longitude, or the mean percentage of C 4 biomass. The oxygen isotope composition ( δ 18O) of soil carbonate is controlled by soil temperature and the δ 18O value of soil water. Great Plains paleosol δ 18O values vary considerably in relation to time and latitude. Removing the variation due to latitude with least squares linear regression reveals a temporal pattern that is consistent with the global pattern of Neogene climate change. Quantitative interpretation of the δ 18O record is difficult without independent control on temperature or the oxygen isotope composition of soil water, both of which have probably varied with long-term climate change. Comparisons of measured δ 18O values for each section with predicted values based on modern temperature data and estimated modern meteoric water δ 18O values suggest that (1) most Miocene sections have δ 18O values consistent with warmer temperatures and more positively shifted soil water δ 18O values than today, (2) three Miocene sections in western Nebraska probably had soil water compositions that were more negative than similar-aged localities in the region, and (3) the Plio-Pleistocene sections have δ 18O values consistent with cooler temperatures and more negative soil water δ 18O values than today. The paleosol δ 13C values do not correlate strongly with the pattern of climate change recorded by the δ 18O values, suggesting that long-term change in mean temperature is not the main control on the abundance of δ 13C biomass in the Great Plains. We propose two testable hypotheses to account for our data and other published data that bear on the evolution of the Great Plains ecosystem.