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References

  • Amundson, R. (2001), The carbon budget in soils, Annu. Rev. Earth Planet Sci., 29, 535562.
  • Arkley, R. J., and H. C. Brown (1954), The origin of mima mound (hogwallow) microrelief in the far western states, Soil Sci. Soc. Am. Proc., 18, 195199.
  • Baisden, W. T., R. Amundson, A. C. Cook, and D. L. Brenner (2002a), Turnover and storage of C and N in five density fractions from California annual grassland surface soils, Global Biogeochem. Cycles, 16(4), 1117, doi:10.1029/2001GB001822.
  • Baisden, W. T., R. Amundson, and D. L. Brenner (2002b), A multiisotope C and N modeling analysis of soil organic matter turnover and transport as a function of soil depth in a California annual grassland soil chronosequence, Global Biogeochem. Cycles, 16(4), 1135, doi:10.1029/2001GB001823.
  • Basile-Doelsch, I., R. Amundson, W. E. E. Stone, C. A. Masiello, J. Y. Bottero, F. Colin, F. Masin, D. Borschneck, and J. D. Meunier (2005), Mineralogical control of organic carbon dynamics in a volcanic ash soil on La Reunion, Eur. J. Soil Sci., 56(6), 689703.
  • Bundt, M., M. Jäggi, P. Blaser, R. Siegwold, and F. Hagedorn (2001a), Carbon and nitrogen dynamics in preferential flow paths and matrix of a forest soil, Soil Sci. Soc. Am. J., 65, 15291538.
  • Bundt, M., F. Widmer, M. Pesaro, J. Zeyer, and P. Blaser (2001b), Preferential flow paths: biological ‘hot spots’ in soils, Soil Biol. Biochem., 33, 729738.
  • Fang, C., P. Smith, J. B. Moncrieff, and J. U. Smith (2005), Similar response of labile and resistant soil organic matter pools to changes in temperature, Nature, 433, 5759.
  • Gaudinski, J. B., S. E. Trumbore, E. A. Davidson, and S. Zheng (2000), Soil carbon cycling in a temperate forest: Radiocarbon-based estimates of residence times, sequestration rates and partitioning of fluxes, Biogeochemistry, 51, 3369.
  • Hagedorn, F., and M. Bundt (2002), The age of preferential flow paths, Geoderma, 108, 119132.
  • Harden, J. W. (1982), A quantitative index of soil development from field descriptions—Examples from a chronosequence in central California, Geoderma, 28, 128.
  • Harden, J. W. (1987), Soils developed on granitic alluvium near Merced, California, U. S. Geol. Surv. Bull., 1590-A, 65 pp.
  • Heimsath, A. M., W. E. Dietrich, K. Nishiizumi, and R. C. Finkel (1997), The soil production function and landscape equilibrium, Nature, 388, 358361.
  • Janada, R. J., and M. G. Croft (1967), The stratigraphic significance of a sequence of noncalcic brown soils formed on the Quaternary alluvium of the northeastern San Joaquin Valley, California, in Quaternary Soils, vol. 9, edited by R. B. Morrison, and H. E. Wright, pp. 158190, Int. Assoc. for Quat. Res., Reno, Nev.
  • Jobbagy, E. G., and R. B. Jackson (2000), The vertical distribution of soil organic carbon and its relation to climate and vegetation, Ecol. Appl., 10(2), 423436.
  • Johnson, D. L. (1990), Biomantle evolution and the redistribution of earth materials and artifacts, Soil Sci., 149, 84102.
  • Kong, A. Y. Y., J. Six, D. C. Bryant, R. F. Denison, and C. van Kessel (2005), The relationship between carbon input, aggregation, and soil organic carbon stabilization in sustainable cropping systems, Soil Sci. Soc. Am. J., 69, 10781085.
  • Masiello, C. A., O. A. Chadwick, J. Southon, M. S. Torn, and J. W. Harden (2004), Weathering controls on mechanisms of carbon storage in grassland soils, Global Biogeochem. Cycles, 18, GB4023, doi:10.1029/2004GB002219.
  • Miller, A. J., R. Amundson, I. C. Burke, and C. Yonker (2004), The effect of climate and cultivation on soil organic C and N, Biogeochemistry, 67, 5772.
  • Minagawa, M., D. A. Winter, and I. R. Kaplan (1984), Comparison of Kjeldahl and combustion methods for measurement of nitrogen isotope ratios in organic matter, Anal. Chem., 56(11), 18591861.
  • Moniz, A. C., and S. W. Buol (1982), Formation of an oxisol-ultisol transition in Sao Paulo, Brazil: I. Double water flow model of soil development, Soil Sci. Soc. Am. J., 46, 12281233.
  • National Soil Survey Center (2002), Field Book for Describing and Sampling Soils,Version 2.0, Nat. Resour. Conserv. Serv., U. S. Dep. of Agric., Lincoln, Nebr.
  • O'Brien, B. J., and J. D. Stout (1978), Movement and turnover of soil organic matter as indicated by C isotope measurements, Soil Biol. Biochem., 10, 309317.
  • Preston, C. M., R. H. Newman, and P. Rother (1994), Using 13C CPMAS NMR to assess effects of cultivation on the organic matter of particle size fractions in a grassland soil, Soil Sci., 157, 2735.
  • Randerson, J. T., I. G. Enting, E. A. G. Schuur, K. Caldeira, and I. Y. Fung (2002), Seasonal and latitudinal variability of troposphere Δ14CO2: Post bomb contributions from fossil fuels, oceans, the stratosphere, and the terrestrial biosphere, Global Biogeochem. Cycles, 16(4), 1112, doi:10.1029/2002GB001876.
  • Rasmussen, C., M. S. Torn, and R. J. Southard (2005), Mineral assemblage and aggregates control carbon dynamics in a California conifer forest, Soil Sci. Soc. Am. J., 69, 17111721.
  • Riebe, C. S., J. W. Kirchner, D. E. Granger, and R. C. Finkel (2001), Strong tectonic and weak climatic control of long-term chemical weathering rates, Geology, 29, 511514.
  • Six, J., R. T. Conant, E. A. Paul, and K. Paustian (2002), Stabilization mechanisms of soil organic matter: implications for C-saturation of soils, Plant Soil, 241(2), 155176.
  • Soil Survey Staff (1999), Keys to Soil Taxonomy, 8th ed., Pocahontas, Blacksburg, Va.
  • Southard, R. J., and S. W. Buol (1988), Subsoil blocky structure formation in some North-Carolina Paleudults and Paleaquults, Soil Sci. Soc. Am. J., 52, 10691076.
  • Torn, M. S., S. E. Trumbore, O. A. Chadwick, P. M. Vitousek, and D. M. Hendricks (1997), Mineral control of soil organic carbon storage and turnover, Nature, 389, 170173.
  • Trumbore, S. E. (1993), Comparison of carbon dynamics in tropical and temperate soils using radiocarbon measurements, Global Biogeochem. Cycles, 7(2), 275290.
  • Trumbore, S. (2000), Age of soil organic matter and soil respiration: Radiocarbon constraints on belowground C dynamics, Ecol. Appl., 10(2), 399411.
  • Trumbore, S. (2006), Carbon respired by terrestrial ecosystems—Recent progress and challenges, Global Change Biol., 12, 141153.
  • van der Graaf, R. H. M. (1978), Size of subsoil blocky peds in relation to textural parameters, depth and drainage, in Modification of Soil Structure, edited by W. W. Emerson, pp. 8796, John Wiley, Hoboken, N. J.
  • Vervoort, R. W., D. E. Radcliffe, and L. T. West (1999), Soil structure development and preferential solute flow, Water Resour. Res., 35(4), 913928.
  • Vogel, J. S., J. R. Southon, D. E. Nelson, and T. A. Brown (1984), Performance of catalytically condensed carbon for use in accelerator mass-spectrometry, Nucl. Instrum. Methods Phys. Res. Sect. B, 233(2), 289293.
  • Wang, Y., R. Amundson, and S. Trumbore (1996), Radiocarbon dating of soil organic matter, Quat. Res., 45, 282288.
  • Wang, Y., R. Amundson, and S. Trumbore (1999), The impact of land use change on C turnover in soils, Global Biogeochem. Cycles, 13(1), 4757.
  • Wang, Y., R. Amundson, and X.-F. Niu (2000), Seasonal and altitudinal variation in decomposition of soil organic matter inferred from radiocarbon measurements of soil CO2 flux, Global Biogeochem. Cycles, 14(1), 199211.
  • White, E. M. (1966), Subsoil structure genesis: theoretical consideration, Soil Sci., 101, 135141.
  • Yoo, K., R. Amundson, A. M. Heimsath, and W. E. Dietrich (2005a), Erosion of upland hillslope soil organic carbon: Coupling field measurements with a sediment transport model, Global Biogeochem. Cycles, 19, GB3003, doi:10.1029/2004GB002271.
  • Yoo, K., R. Amundson, A. M. Heimsath, and W. E. Dietrich (2005b), Process-based model linking pocket gopher activity to sediment transport and soil thickness, Geology, 33, 917920.