the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Carbon Stocks and Accumulation Rates in Salt Marshes of the Pacific Coast of Canada
Stephen G. Chastain
Karen Kohfeld
Marlow G. Pellatt
Abstract. Tidal salt marshes are known to accumulate blue carbon
at high rates relative to their surface area and have been put forth as a potential means for enhanced CO2 sequestration. However, estimates of salt marsh carbon accumulation rates are based on a limited number of marshes globally and the estimation of carbon accumulation rates require detailed dating to provide accurate estimates. We address one data gap along the Pacific Coast of Canada by estimating carbon stocks in 34 sediment cores and estimating carbon accumulation rates using 210Pb dating on four cores from seven salt marshes within the Clayoquot Sound UNESCO Biosphere Reserve and Pacific Rim National Park Reserve of Canada (49.2° N, 125.80° W). Carbon stocks averaged 80.6 ± 43.8 megagrams of carbon per hectare (Mg C ha−1) between the seven salt marshes, and carbon accumulation rates averaged 146 ± 102 grams carbon per square meter per year (g C m−2 yr−1). These rates are comparable to those found in salt marshes further south along the Pacific coast of North America (32.5–38.2° N) and at similar latitudes in Eastern Canada and Northern Europe (43.6–55.5° N). The seven Clayoquot Sound salt marshes currently accumulate carbon at a rate of 54.28 Mg C yr−1 over an area of 46.94 ha, 87 % of which occurs in the high marsh zone. On a per-hectare basis, Clayoquot Sound salt marsh soils accumulate carbon at least one order of magnitude more quickly than the average of global boreal forest soils, and approximately two times larger than rates for forests in British Columbia. However, because of their relatively small area, we suggest that their carbon accumulation rate capacity could best be considered as a climate mitigation co-benefit when conserving for other salt marsh ecosystem services.
Stephen G. Chastain et al.


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RC1: 'Problem with dating', Anonymous Referee #1, 01 May 2018
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AC1: 'Reply to Anonymous Reviewer #1', Stephen Chastain, 30 May 2018
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AC1: 'Reply to Anonymous Reviewer #1', Stephen Chastain, 30 May 2018
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RC2: 'Review report Manuscript bg-2018-166', Anonymous Referee #2, 22 May 2018
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AC2: 'Reply to Anonymous Reviewer #2', Stephen Chastain, 04 Jun 2018
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AC2: 'Reply to Anonymous Reviewer #2', Stephen Chastain, 04 Jun 2018
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AC3: 'Authors' Final Statement', Stephen Chastain, 20 Jun 2018


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RC1: 'Problem with dating', Anonymous Referee #1, 01 May 2018
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AC1: 'Reply to Anonymous Reviewer #1', Stephen Chastain, 30 May 2018
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AC1: 'Reply to Anonymous Reviewer #1', Stephen Chastain, 30 May 2018
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RC2: 'Review report Manuscript bg-2018-166', Anonymous Referee #2, 22 May 2018
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AC2: 'Reply to Anonymous Reviewer #2', Stephen Chastain, 04 Jun 2018
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AC2: 'Reply to Anonymous Reviewer #2', Stephen Chastain, 04 Jun 2018
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AC3: 'Authors' Final Statement', Stephen Chastain, 20 Jun 2018
Stephen G. Chastain et al.
Stephen G. Chastain et al.
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hotspots, comparable with those from elsewhere on the NE Pacific coast or similar latitude ranges.