Access
To read this story in full you will need to login or make a payment (see right).
Letters to Nature
Nature 411, 466-469 (24 May 2001) | doi:10.1038/35078060; Received 3 January 2001; Accepted 2 April 2001
Open Innovation Challenges
-
Methods to Analyze Consumer Emotions
The Seeker is looking for methods to analyze consumer emotions. This Challenge requires only a writ...
-
Optimizing Sub-cellular Localization Tags
The Seeker is looking for methods to optimize sub-cellular localization tags for protein expression....
nature jobs
Full-Professor of Heart and Thoracic Surgery (W3) (f / m)
- Friedrich-Schiller-University Jena
- Jena Germany
Thermo- Chemical Sciences
- Praj Matrix - Praj Industries Ltd
- Pune, Maharashtra Pune-411021 India
Limited carbon storage in soil and litter of experimental forest plots under increased atmospheric CO2
William H. Schlesinger1 & John Lichter2
- Nicholas School of the Environment and Earth Sciences, Duke University, Durham, North Carolina 27708, USA
- Biology Department and Environmental Studies Program, Bowdoin College, Brunswick, Maine 04011, USA
Correspondence to: William H. Schlesinger1 Correspondence and requests for materials should be addressed to W.H.S. (e-mail: Email: schlesin@duke.edu).
Abstract
The current rise in atmospheric CO2 concentration is thought to be mitigated in part by carbon sequestration within forest ecosystems1, 2, where carbon can be stored in vegetation or soils. The storage of carbon in soils is determined by the fraction that is sequestered in persistent organic materials, such as humus. In experimental forest plots of loblolly pine (Pinus taeda) exposed to high CO2 concentrations3, 4, nearly half of the carbon uptake is allocated to short-lived tissues, largely foliage. These tissues fall to the ground and decompose, normally contributing only a small portion of their carbon content to refractory soil humic materials5. Such findings call into question the role of soils as long-term carbon sinks, and show the need for a better understanding of carbon cycling in forest soils. Here we report a significant accumulation of carbon in the litter layer of experimental forest plots after three years of growth at increased CO2 concentrations (565
l l-1). But fast turnover times of organic carbon in the litter layer (of about three years) appear to constrain the potential size of this carbon sink. Given the observation that carbon accumulation in the deeper mineral soil layers was absent, we suggest that significant, long-term net carbon sequestration in forest soils is unlikely.
- Nicholas School of the Environment and Earth Sciences, Duke University, Durham, North Carolina 27708, USA
- Biology Department and Environmental Studies Program, Bowdoin College, Brunswick, Maine 04011, USA
Correspondence to: William H. Schlesinger1 Correspondence and requests for materials should be addressed to W.H.S. (e-mail: Email: schlesin@duke.edu).
To read this story in full you will need to login or make a payment (see right).

