Postfire carbon balance in boreal bogs of Alberta, Canada
Abstract Boreal peatland ecosystems occupy about 3.5 million km 2 of the earth's land surface and store between 250 and 455 Pg of carbon (C) as peat. While northern hemisphere boreal peatlands have functioned as net sinks for atmospheric C since the most recent deglaciation, natural and anthrop...
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crwiley:10.1111/j.1365-2486.2008.01756.x 2024-06-23T07:57:24+00:00 Postfire carbon balance in boreal bogs of Alberta, Canada WIEDER, R. KELMAN SCOTT, KIMBERLI D. KAMMINGA, KATHERINE VILE, MELANIE A. VITT, DALE H. BONE, TIFFANY XU, BIN BENSCOTER, BRIAN W. BHATTI, JAGTAR S. 2009 http://dx.doi.org/10.1111/j.1365-2486.2008.01756.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2486.2008.01756.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2486.2008.01756.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Global Change Biology volume 15, issue 1, page 63-81 ISSN 1354-1013 1365-2486 journal-article 2009 crwiley https://doi.org/10.1111/j.1365-2486.2008.01756.x 2024-06-11T04:41:59Z Abstract Boreal peatland ecosystems occupy about 3.5 million km 2 of the earth's land surface and store between 250 and 455 Pg of carbon (C) as peat. While northern hemisphere boreal peatlands have functioned as net sinks for atmospheric C since the most recent deglaciation, natural and anthropogenic disturbances, and most importantly wildfire, may compromise peatland C sinks. To examine the effects of fire on local and regional C sink strength, we focused on a 12 000 km 2 region near Wabasca, AB, Canada, where ombrotrophic Sphagnum ‐dominated bogs cover 2280 km 2 that burn with a fire return interval of 123±26 years. We characterized annual C accumulation along a chronosequence of 10 bog sites, spanning 1–102 years‐since‐fire (in 2002). Immediately after fire, bogs represent a net C source of 8.9±8.4 mol m −2 yr −1 . At about 13 years after fire, bogs switch from net C sources to net C sinks, mainly because of recovery of the moss and shrub layers. Subsequently, black spruce biomass accumulation contributes to the net C sink, with fine root biomass accumulation peaking at 34 years after fire and aboveground biomass and coarse root accumulation peaking at 74 years after fire. The overall C sink strength peaks at 18.4 mol C m −2 yr −1 at 75 years after fire. As the tree biomass accumulation rate declines, the net C sink decreases to about 10 mol C m −2 yr −1 at 100 years‐since‐fire. We estimate that across the Wabasca study region, bogs currently represent a C sink of 14.7±5.1 Gmol yr −1 . A decrease in the fire return interval to 61 years with no change in air temperature would convert the region's bogs to a net C source. An increase in nonwinter air temperature of 2 °C would decrease the regional C sink to 6.8±2.3 Gmol yr −1 . Under scenarios of predicted climate change, the current C sink status of Alberta bogs is likely to diminish to the point where these peatlands become net sources of atmospheric CO 2 ‐C. Article in Journal/Newspaper Wabasca Wiley Online Library Canada Wabasca ENVELOPE(-113.919,-113.919,55.987,55.987) Global Change Biology 15 1 63 81 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Abstract Boreal peatland ecosystems occupy about 3.5 million km 2 of the earth's land surface and store between 250 and 455 Pg of carbon (C) as peat. While northern hemisphere boreal peatlands have functioned as net sinks for atmospheric C since the most recent deglaciation, natural and anthropogenic disturbances, and most importantly wildfire, may compromise peatland C sinks. To examine the effects of fire on local and regional C sink strength, we focused on a 12 000 km 2 region near Wabasca, AB, Canada, where ombrotrophic Sphagnum ‐dominated bogs cover 2280 km 2 that burn with a fire return interval of 123±26 years. We characterized annual C accumulation along a chronosequence of 10 bog sites, spanning 1–102 years‐since‐fire (in 2002). Immediately after fire, bogs represent a net C source of 8.9±8.4 mol m −2 yr −1 . At about 13 years after fire, bogs switch from net C sources to net C sinks, mainly because of recovery of the moss and shrub layers. Subsequently, black spruce biomass accumulation contributes to the net C sink, with fine root biomass accumulation peaking at 34 years after fire and aboveground biomass and coarse root accumulation peaking at 74 years after fire. The overall C sink strength peaks at 18.4 mol C m −2 yr −1 at 75 years after fire. As the tree biomass accumulation rate declines, the net C sink decreases to about 10 mol C m −2 yr −1 at 100 years‐since‐fire. We estimate that across the Wabasca study region, bogs currently represent a C sink of 14.7±5.1 Gmol yr −1 . A decrease in the fire return interval to 61 years with no change in air temperature would convert the region's bogs to a net C source. An increase in nonwinter air temperature of 2 °C would decrease the regional C sink to 6.8±2.3 Gmol yr −1 . Under scenarios of predicted climate change, the current C sink status of Alberta bogs is likely to diminish to the point where these peatlands become net sources of atmospheric CO 2 ‐C. |
format |
Article in Journal/Newspaper |
author |
WIEDER, R. KELMAN SCOTT, KIMBERLI D. KAMMINGA, KATHERINE VILE, MELANIE A. VITT, DALE H. BONE, TIFFANY XU, BIN BENSCOTER, BRIAN W. BHATTI, JAGTAR S. |
spellingShingle |
WIEDER, R. KELMAN SCOTT, KIMBERLI D. KAMMINGA, KATHERINE VILE, MELANIE A. VITT, DALE H. BONE, TIFFANY XU, BIN BENSCOTER, BRIAN W. BHATTI, JAGTAR S. Postfire carbon balance in boreal bogs of Alberta, Canada |
author_facet |
WIEDER, R. KELMAN SCOTT, KIMBERLI D. KAMMINGA, KATHERINE VILE, MELANIE A. VITT, DALE H. BONE, TIFFANY XU, BIN BENSCOTER, BRIAN W. BHATTI, JAGTAR S. |
author_sort |
WIEDER, R. KELMAN |
title |
Postfire carbon balance in boreal bogs of Alberta, Canada |
title_short |
Postfire carbon balance in boreal bogs of Alberta, Canada |
title_full |
Postfire carbon balance in boreal bogs of Alberta, Canada |
title_fullStr |
Postfire carbon balance in boreal bogs of Alberta, Canada |
title_full_unstemmed |
Postfire carbon balance in boreal bogs of Alberta, Canada |
title_sort |
postfire carbon balance in boreal bogs of alberta, canada |
publisher |
Wiley |
publishDate |
2009 |
url |
http://dx.doi.org/10.1111/j.1365-2486.2008.01756.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2486.2008.01756.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2486.2008.01756.x |
long_lat |
ENVELOPE(-113.919,-113.919,55.987,55.987) |
geographic |
Canada Wabasca |
geographic_facet |
Canada Wabasca |
genre |
Wabasca |
genre_facet |
Wabasca |
op_source |
Global Change Biology volume 15, issue 1, page 63-81 ISSN 1354-1013 1365-2486 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1365-2486.2008.01756.x |
container_title |
Global Change Biology |
container_volume |
15 |
container_issue |
1 |
container_start_page |
63 |
op_container_end_page |
81 |
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1802651017719840768 |