Peatland pools are tightly coupled to the contemporary carbon cycle

Dean, Joshua F.; Billett, Michael F.; Turner, T. Edward; Garnett, Mark H.; Andersen, Roxane; McKenzie, Rebecca M. ORCID: https://orcid.org/0009-0009-9928-8780; Dinsmore, Kerry J.; Baird, Andy J.; Chapman, Pippa J.; Holden, Joseph. 2024 Peatland pools are tightly coupled to the contemporary carbon cycle. Global Change Biology, 30 (1), e16999. 16, pp. https://doi.org/10.1111/gcb.16999

Before downloading, please read NORA policies.

Preview

Text
N536305JA.pdf - Published Version
Available under License Creative Commons Attribution 4.0.
Download (4MB) | Preview

Official URL: http://dx.doi.org/10.1111/gcb.16999

Abstract/Summary

Peatlands are globally important stores of soil carbon (C) formed over millennial timescales but are at risk of destabilization by human and climate disturbance. Pools are ubiquitous features of many peatlands and can contain very high concentrations of C mobilized in dissolved and particulate organic form and as the greenhouses gases carbon dioxide (CO2) and methane (CH4). The radiocarbon content (14C) of these aquatic C forms tells us whether pool C is generated by contemporary primary production or from destabilized C released from deep peat layers where it was previously stored for millennia. We present novel 14C and stable C (δ13C) isotope data from 97 aquatic samples across six peatland pool locations in the United Kingdom with a focus on dissolved and particulate organic C and dissolved CO2. Our observations cover two distinct pool types: natural peatland pools and those formed by ditch blocking efforts to rewet peatlands (restoration pools). The pools were dominated by contemporary C, with the majority of C (~50%–75%) in all forms being younger than 300 years old. Both pool types readily transform and decompose organic C in the water column and emit CO2 to the atmosphere, though mixing with the atmosphere and subsequent CO2 emissions was more evident in natural pools. Our results show little evidence of destabilization of deep, old C in natural or restoration pools, despite the presence of substantial millennial-aged C in the surrounding peat. One possible exception is CH4 ebullition (bubbling), with our observations showing that millennial-aged C can be emitted from peatland pools via this pathway. Our results suggest that restoration pools formed by ditch blocking are effective at preventing the release of deep, old C from rewetted peatlands via aquatic export.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1111/gcb.16999
UKCEH and CEH Sections/Science Areas:	Water Resources (Science Area 2017-) Unaffiliated
ISSN:	1354-1013
Additional Information. Not used in RCUK Gateway to Research.:	Open Access paper - full text available via Official URL link.
Additional Keywords:	carbon dioxide (CO2), dissolved organic carbon (DOC), methane (CH4), particulate organiccarbon (POC), peatlands, pools/ponds, radiocarbon (14C), stable carbon isotope (δ13C)
NORA Subject Terms:	Ecology and Environment Agriculture and Soil Science
Related URLs:	Dataset Dataset Other
Date made live:	23 Nov 2023 14:24 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/536305

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1111/gcb.16999

UKCEH and CEH Sections/Science Areas:

Water Resources (Science Area 2017-)
Unaffiliated

ISSN:

1354-1013

Additional Information. Not used in RCUK Gateway to Research.:

Open Access paper - full text available via Official URL link.

Additional Keywords:

carbon dioxide (CO2), dissolved organic carbon (DOC), methane (CH4), particulate organiccarbon (POC), peatlands, pools/ponds, radiocarbon (14C), stable carbon isotope (δ13C)

NORA Subject Terms:

Ecology and Environment
Agriculture and Soil Science

Related URLs:

Date made live:

23 Nov 2023 14:24 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/536305