@article {659,
	title = {Carbon isotope variation in modern soils of the tallgrass prairie: Analogues for the interpretation of isotopic records derived from paleosols},
	journal = {Quaternary International},
	volume = {162},
	year = {2007},
	note = {158nkTimes Cited:9Cited References Count:144},
	month = {Mar},
	pages = {3-20},
	abstract = {Use of stable carbon isotope data from paleosols to reconstruct past plant community structure (C-3 vs. C-4) has become commonplace. In an effort to improve our ability to make isotope-based reconstructions and to better appreciate the pitfalls, investigations were conducted on both modern soils and paleosols in the Kansas grasslands.Stable carbon isotope data were derived from soils and vegetation on the near-pristine, C-4-dominated grassland of the Konza Tallgrass Prairie Long-Term Ecological Research (LTER) site in northeastern Kansas. In order to evaluate variation of delta C-13 within the landscape, two levels of sampling were employed: 2 m-deep upland cores extracted to assess variation with depth in the soil profile, and, to assess variability across the landscape, surface samples along two transects and from within a 660 x 690 m grid. For transect and grid points, both the upper 2cm of sediment and the aboveground biomass were collected. Core samples taken at Konza reveal that soil organic carbon was depleted in C-13 within the upper 10-20cm relative to the remainder of the soil solum below, a phenomenon previously reported. In transects and the sample grid, soil organic carbon from soil surfaces was consistently more depleted in C-13 than aboveground tissue of associated vegetation samples. Slope, azimuth, and insolation were computed from field data and a highresolution DEM of the sample grid, but these variables offered no significant explanation of the spatial variability in delta C-13 data from soil organic carbon. The observation that modern landscape position has little effect on delta C-13 over short distances, at least in a C4-dominated community, lends support to the application of delta C-13 analysis to buried soils for paleoenvironmental reconstruction where paleolandscape position is often unknown.Stable carbon isotope data were derived from paleosols at from the Beisel-Steinle site located to the west of Konza in central Kansas. Three soils were examined: the interstadial paleosol within the Gilman Canyon Formation (c. 38-27k cal yr BP), the Late Pleistocene-Holocene Brady Soil, and the modern surface soil. With the exception of isotopic depletion at the top of the surface soil, all three soils exhibited similar delta C-13 values of about14 parts per thousand, the same value realized in the soil cores from Konza, suggesting close similarity among the plant communities of the interstade, the Late Pleistocene-Early Holocene transition, and pristine prairie of today.This investigation emphasizes the need for additional research into the variation in stable carbon isotope signals vertically within the profile and across the landscape. Issues include the source of the near-surface depletion zone, the relationship between isotopic values in the soil versus those of the vegetation, and variation in Soil delta 13C values delta 13C throughout the landscape. (c) 2006 Elsevier Ltd and INQUA. All rights reserved.},
	issn = {1040-6182},
	doi = {10.1016/j.quaint.2006.10.036},
	author = {Johnson, W. C. and Willey, K. L. and Macpherson, G. L.}
}
@article {650,
	title = {Stratigraphy and environmental reconstruction at the middle Wisconsinan Gilman Canyon Formation type locality, Buzzard{\textquoteright}s Roost, southwestern Nebraska, USA},
	journal = {Quaternary Research},
	volume = {67},
	year = {2007},
	note = {160ruTimes Cited:17Cited References Count:115},
	month = {May},
	pages = {474-486},
	abstract = {The middle Wisconsinan Gilman Canyon Formation at the Buzzard{\textquoteright}s Roost type locality in southwestern Nebraska was investigated to document the stratigraphy and to reconstruct the environmental and climate record. The Gilman Canyon Formation was subdivided into three loess units and three soils, with radiocarbon ages constraining it between about 40 ka and 25 ka. Stable carbon isotope ratios, magnetic susceptibility, and carbon content were used to define and characterize soils within both the Gilman Canyon Formation and underlying Illinoian Loveland Loess. At the height of soil development within the Gilman Canyon Formation, climate was supporting C-4-dominated grassland, with July temperatures equal to or exceeding those of today. Soil-forming intervals within the Loveland Loess, including the Sangamon Soil, also exhibited relative increases in C-4 biomass. Climate, as recorded in the Gilman Canyon Formation, is corroborated by regional proxy data. The formation accumulated during MIS 3, and concurrent soil formation coincided with a summer insolation maximum. (c) 2007 University of Washington. All rights reserved.},
	issn = {0033-5894},
	doi = {10.1016/j.yqres.2007.01.011},
	author = {Johnson, W. C. and Willey, K. L. and Mason, J. A. and May, D. W.}
}
