The DOI matches its Crossref record; 5 of the 5 references it cites were found in a registry or an index.
Turnover and storage of C and N in five density fractions from California annual grassland surface soils
Abstract
We measured 14 C/12 C in density fractions from soils collected before and after atmospheric thermonuclear weapons testing to examine soil organic matter (SOM) dynamics along a 3 million year California soil chronosequence. The mineral‐free particulate organic matter (FPOM; <1.6 g cm−3) mainly contains recognizable plant material, fungal hyphae, and charcoal. Mineral‐associated light fractions (1.6–2.2 g cm−3) display partially or completely humified fine POM, while the dense fraction (>2.2 g cm−3) consists of relatively OM‐free sand and OM‐rich clays. Three indicators of decomposition (C:N, δ 13 C, and δ 15 N) all suggest increasing SOM decomposition with increasing fraction density. The Δ 14 C‐derived SOM turnover rates suggest that ≥90% of FPOM turns over in <10 years. The four mineral‐associated fractions contain 69–86% “stabilized” (decadal) SOM with the remainder assumed to be “passive” (millenial) SOM. Within each soil, the four mineral‐associated fractions display approximately the same residence time (34–42 years in 200 kyr soil, 29–37 years in 600 kyr soil, and 18–26 years in 1–3 Myr soils), indicating that a single stabilized SOM “pool” exists in these soils and may turn over primarily as a result of soil disruption.
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Cites
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The role of biology in the formation, stabilization and degradation of soil structure
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Soil structure and carbon cycling
Golchin, A., Oades, J., Skjemstad, J., & Clarke, P. (1994) · Australian Journal of Soil Research · doi:10.1071/sr9941043 · Cited by 669
Cited by
SOM fractionation methods: Relevance to functional pools and to stabilization mechanisms
von Lützow, M., Kögel-Knabner, I., Ekschmitt, K., Flessa, H., Guggenberger, G., Matzner, E., & Marschner, B. (2007) · Soil Biology and Biochemistry · doi:10.1016/j.soilbio.2007.03.007 · Cited by 1,590
How relevant is recalcitrance for the stabilization of organic matter in soils?
Marschner, B., Brodowski, S., Dreves, A., Gleixner, G., Gude, A., Grootes, P. M., Hamer, U., Heim, A., Jandl, G., Ji, R., et al. (2008) · Journal of Plant Nutrition and Soil Science · doi:10.1002/jpln.200700049 · Cited by 743
Organic C and N stabilization in a forest soil: Evidence from sequential density fractionation
Sollins, P., Swanston, C., Kleber, M., Filley, T., Kramer, M., Crow, S., Caldwell, B. A., Lajtha, K., & Bowden, R. (2006) · Soil Biology and Biochemistry · doi:10.1016/j.soilbio.2006.04.014 · Cited by 448
Sollins, P., Kramer, M. G., Swanston, C., Lajtha, K., Filley, T., Aufdenkampe, A. K., Wagai, R., & Bowden, R. D. (2009) · Biogeochemistry · doi:10.1007/s10533-009-9359-z · Cited by 365
The turnover of organic carbon in subsoils. Part 2. Modelling carbon turnover
Jenkinson, D. S., & Coleman, K. (2008) · European Journal of Soil Science · doi:10.1111/j.1365-2389.2008.01026.x · Cited by 241
Metadata
- Authors
- Baisden, W. T., Amundson, R., Cook, A. C., & Brenner, D. L.
- Venue
- Global Biogeochemical Cycles
- Publisher
- American Geophysical Union (AGU)
- Published
- 2002-12
- Volume
- 16
- Issue
- 4
- ISSN
- 0886-6236 (ISSN-L)
- 1944-9224
- OpenAlex
- W2151543090
- Cited by
- 316
- References
- 5
- FWCI
- 11.24
- Type
- journal article
- Language
- en
- Open access
- closed
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- Baisden, W. T., Amundson, R., Cook, A. C., & Brenner, D. L. (2002). Turnover and storage of C and N in five density fractions from California annual grassland surface soils. Global Biogeochemical Cycles. https://doi.org/10.1029/2001gb001822
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