Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter
Abstract
Increasing global temperatures have the potential to stimulate decomposition and alter the composition of soil organic matter (SOM). However, questions remain about the extent to which SOM quality and quantity along the soil profile may change under future warming. In this study we assessed how +4 °C whole-soil warming affected the quantity and quality of SOM down to 90 cm depth in a mixed-coniferous temperate forest using biomarker analyses. Our findings indicate that 4.5 years of soil warming led to divergent responses in subsoils (>20 cm) as compared to surface soils. Warming enhanced the accumulation of plant-derived n-alkanes over the whole soil profile. In the subsoil, this was at the expense of plant- and microorganism-derived fatty acids, and the relative abundance of SOM molecular components shifted from less microbially transformed to more transformed organic matter. Fine root mass declined by 24.0 ± 7.5% with warming over the whole soil profile, accompanied by reduced plant-derived inputs and accelerated decomposition of aromatic compounds and plant-derived fatty acids in the subsoils. Our study suggests that warming accelerated microbial decomposition of plant-derived inputs, leaving behind more degraded organic matter. The non-uniform, and depth dependent SOM composition and warming response implies that subsoil carbon cyclingmore »
- Authors:
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- OSTI Identifier:
- 1766654
- Alternate Identifier(s):
- OSTI ID: 1813383
- Grant/Contract Number:
- AC02-05CH11231; SC0001234
- Resource Type:
- Published Article
- Journal Name:
- Soil Biology and Biochemistry
- Additional Journal Information:
- Journal Name: Soil Biology and Biochemistry Journal Volume: 156 Journal Issue: C; Journal ID: ISSN 0038-0717
- Publisher:
- Elsevier
- Country of Publication:
- United Kingdom
- Language:
- English
- Subject:
- 59 BASIC BIOLOGICAL SCIENCES; whole soil warming; deep soil organic matter; biomarker; alkanes; fatty acids; decomposition
Citation Formats
Ofiti, Nicholas O. E., Zosso, Cyrill U., Soong, Jennifer L., Solly, Emily F., Torn, Margaret S., Wiesenberg, Guido L. B., and Schmidt, Michael W. I. Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter. United Kingdom: N. p., 2021.
Web. doi:10.1016/j.soilbio.2021.108185.
Ofiti, Nicholas O. E., Zosso, Cyrill U., Soong, Jennifer L., Solly, Emily F., Torn, Margaret S., Wiesenberg, Guido L. B., & Schmidt, Michael W. I. Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter. United Kingdom. https://doi.org/10.1016/j.soilbio.2021.108185
Ofiti, Nicholas O. E., Zosso, Cyrill U., Soong, Jennifer L., Solly, Emily F., Torn, Margaret S., Wiesenberg, Guido L. B., and Schmidt, Michael W. I. Sat .
"Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter". United Kingdom. https://doi.org/10.1016/j.soilbio.2021.108185.
@article{osti_1766654,
title = {Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter},
author = {Ofiti, Nicholas O. E. and Zosso, Cyrill U. and Soong, Jennifer L. and Solly, Emily F. and Torn, Margaret S. and Wiesenberg, Guido L. B. and Schmidt, Michael W. I.},
abstractNote = {Increasing global temperatures have the potential to stimulate decomposition and alter the composition of soil organic matter (SOM). However, questions remain about the extent to which SOM quality and quantity along the soil profile may change under future warming. In this study we assessed how +4 °C whole-soil warming affected the quantity and quality of SOM down to 90 cm depth in a mixed-coniferous temperate forest using biomarker analyses. Our findings indicate that 4.5 years of soil warming led to divergent responses in subsoils (>20 cm) as compared to surface soils. Warming enhanced the accumulation of plant-derived n-alkanes over the whole soil profile. In the subsoil, this was at the expense of plant- and microorganism-derived fatty acids, and the relative abundance of SOM molecular components shifted from less microbially transformed to more transformed organic matter. Fine root mass declined by 24.0 ± 7.5% with warming over the whole soil profile, accompanied by reduced plant-derived inputs and accelerated decomposition of aromatic compounds and plant-derived fatty acids in the subsoils. Our study suggests that warming accelerated microbial decomposition of plant-derived inputs, leaving behind more degraded organic matter. The non-uniform, and depth dependent SOM composition and warming response implies that subsoil carbon cycling is as sensitive and complex as in surface soils.},
doi = {10.1016/j.soilbio.2021.108185},
journal = {Soil Biology and Biochemistry},
number = C,
volume = 156,
place = {United Kingdom},
year = {Sat May 01 00:00:00 EDT 2021},
month = {Sat May 01 00:00:00 EDT 2021}
}
https://doi.org/10.1016/j.soilbio.2021.108185
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