Carbon and oxygen isotopic variability in Neogene paleosol carbonates: constraints on the evolution of the C4-grasslands of the Great Plains, USA
By David L. Fox, P. Koch. 2004
134 citations recorded by the source corpus.
Subfields: Atmospheric Science, Ecology, Paleontology
View Paper: https://www.semanticscholar.org/paper/361aae74519333baac39912a1ef12aa9588c3733
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Citations in the corpus
- New insight from old bones: stable isotope analysis of fossil mammals (2012, background): “…provided 1 of the most widely used and broadly applied dietary tracers in paleobiological study (Bocherens et al. 1996; Cerling et al. 1997, 1998; Fox and Koch 2004; Franz-Odendaal et al. 2002; Koch et al. 1998, 2004; Latorre et al. 1997; MacFadden and Cerling 1996; MacFadden et al. 1996; Wang…”
- Photorespiration and the evolution of C4 photosynthesis. (2012, background): “Well-preserved silica bodies (phytoliths) indicate that C4 grasses were present on the North American landscape by 19 Mya (130), whereas carbon isotope ratios of fossilized pollen suggest the presence of C4 grasses in southwest Europe by 33 Mya (137).”