EGU21-16152
https://doi.org/10.5194/egusphere-egu21-16152
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

The response of deep soil carbon to climate change: From experiments to meta-analysis

Caitlin Pries1, Katherine Heckman2, Pamela Templer3, Serita Frey4, and Susan Crow5
Caitlin Pries et al.
  • 1Dartmouth College, Biological Sciences, Hanover, United States of America (caitlin.pries@dartmouth.edu)
  • 2Northern Research Station, United States Forest Service, Houghton, MI, USA
  • 3Department of Biology, Boston University, Boston, MA, USA
  • 4Department of Natural Resources and the Environment, University of New Hampshire, Durham, NH, USA
  • 5Department of Natural Resources & Environmental Management, University of Hawaii Manoa, Honolulu, HI, USA

Over half of global soil organic carbon (SOC) is stored in subsurface soils (>20 cm depth), but the vulnerability of this deeper SOC to climate change has only recently been tested. Most soil warming experiments have either only warmed surface soils or only examined the response of the surface carbon dioxide flux, so the sensitivity of SOC at different soil depths to climate change is undetermined. As predictive models of terrestrial carbon storage move toward more mechanistic representations, we need to understand how the carbon cycle differs across soil depths. We present depth-explicit measurements of soil CO2 production from six studies, including four in situ deep soil warming experiments. The experiments’ locations ranged from coniferous to hardwood temperate forests in the United States to volcanic soils in Hawaii. We have found that in temperate forests, deep soil carbon is just as vulnerable to warming-induced losses as surface soils. However, where minerals are strongly associated with organic carbon, as in Hawaii, or in degraded soils where much of the organic matter has been lost, deep soil carbon resists warming-induced losses. Thus, the response of deep soil to climate change is dependent on its availability to microbes. This conclusion is supported by a worldwide meta-analysis of radiocarbon data among soil density fractions, which found that the amount of carbon in the particulate free light fraction decreased with mean annual temperature, but the carbon in the heavy, mineral-associated fraction did not.

How to cite: Pries, C., Heckman, K., Templer, P., Frey, S., and Crow, S.: The response of deep soil carbon to climate change: From experiments to meta-analysis, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-16152, https://doi.org/10.5194/egusphere-egu21-16152, 2021.

Corresponding presentation materials formerly uploaded have been withdrawn.