Kohfeld, Karen E; Chastain, Stephen; Pellatt, Marlow G; Olid, Carolina (2022): Carbon stocks and carbon accumulation rates of sediment cores in Clayoquot Sound, British Columbia, Canada [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.947803, In: Kohfeld, KE et al. (2022): Salt marsh soil carbon content, loss on ignition, dry bulk density, carbon stocks, lead-210 and carbon accumulation rates, for Clayoquot Sound, British Columbia, Canada [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.947825
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Abstract:
The goal of this project was to provide the first estimates of blue carbon stocks and carbon accumulation rates in the high and low marsh zones of salt marshes from the Pacific Coast of Canada, within the Clayoquot Sound UNESCO Biosphere Reserve and Pacific Rim National Park Reserve on the Pacific Coast of Canada. Sediment cores were collected using a simple percussion coring technique in which a 57-mm diameter, PVC vacuum tubing fitted with a plastic core catcher (AMS Inc.) was hammered into the ground until the depth of refusal. At the GBK location, a steel sledge corer (AMS Inc.) was used to extract four cores before mechanical problems required switching to the simpler percussion method.
This datafile provides a summary of the estimated C stocks and carbon accumulation rates for the thirty-four sediment cores that were collected from seven salt marshes during summer (June-September) 2016. The sediment type at the base of each core was recorded. We also recorded the deepest sediment depth at which peat was found, referred to as the depth of the “Peat Base.” This depth was used to estimate the C stock for the marsh. Compaction was measured as length of core penetration divided by the length of core recovered. Using the compaction factor, we provide estimates of “uncorrected” (using original core depths) and “corrected” (applying compaction factor) values for the dry bulk density (g/cm3) and soil carbon density (g C/cm3). We provide estimates of C stocks (a) to the peat base, (b) for the whole core, and (c) to the depth of the 30-year horizon in the eight cores for which we have measured 210Pb systematics. We calculated the mass of all carbon down to the base of the peat layer to estimate the C-stock to peat base for each core, and this calculation did not require use of the compaction factor. The “corrected” values were provided to facilitate comparison with other studies (and for calculating the 20-cm C stock). ArcMap 10.3 tools were used with 50 x 50 cm resolution aerial orthophotos (taken in July 2014, Government of British Columbia) to estimate the total marsh area for each marsh.
Keyword(s):
Related to:
Chastain, Stephen; Kohfeld, Karen E; Pellatt, Marlow G; Olid, Carolina; Gailis, Maija (2022): Quantification of blue carbon in salt marshes of the Pacific coast of Canada. Biogeosciences, 19(24), 5751-5777, https://doi.org/10.5194/bg-19-5751-2022
Funding:
Coverage:
Median Latitude: 49.158301 * Median Longitude: -125.745918 * South-bound Latitude: 49.087560 * West-bound Longitude: -125.911000 * North-bound Latitude: 49.279350 * East-bound Longitude: -125.666020
Date/Time Start: 2016-01-01T00:00:00 * Date/Time End: 2016-09-16T00:00:00
Event(s):
Comment:
CBE=Cannery Bay East
CBW = Cannery Bay West
CRF = Cypress River Flats
GBK = Grice Bay- Kootowis Creek
KCS = Kennedy Cove South
SWC = Shipwreck Cove
TMF = Tofino Mud Flats
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Location | Location | Kohfeld, Karen E | see comment | Name of marsch | |
2 | Event label | Event | Kohfeld, Karen E | Core ID | ||
3 | Latitude of event | Latitude | Kohfeld, Karen E | Core ID | ||
4 | Longitude of event | Longitude | Kohfeld, Karen E | Core ID | ||
5 | Zone | Zone | Kohfeld, Karen E | marsh zone: high or low marsh | ||
6 | Sediment type | Sediment | Kohfeld, Karen E | soil type at the base of sediment core | ||
7 | Core length | Core length | cm | Kohfeld, Karen E | Uncorrected | |
8 | Compaction factor | Comp fact | Kohfeld, Karen E | unitless factor based on the full core length (corrected_depth) divided by compacted core depth (uncorrected_depth) | ||
9 | Core length | Core length | cm | Kohfeld, Karen E | Corrected | |
10 | Depth, peat base | Depth peat base | cm | Kohfeld, Karen E | Corrected | depth of deepest layer containing peat and overlying sand, gravel, or clay |
11 | Density, dry bulk | DBD | g/cm3 | Kohfeld, Karen E | Calculated average/mean values | uncorrected, measured to peat base |
12 | Density, dry bulk | DBD | g/cm3 | Kohfeld, Karen E | Calculated standard error (SE) | uncorrected, standard error (stdev/sqrt(n)) of averaged DBD to peat base |
13 | Density, dry bulk | DBD | g/cm3 | Kohfeld, Karen E | Calculated average/mean values | corrected for compaction, measured to peat base |
14 | Density, dry bulk | DBD | g/cm3 | Kohfeld, Karen E | Calculated standard error (SE) | corrected for compaction, standard error (stdev/sqrt(n)) of averaged DBD to peat base |
15 | Carbon | C | % | Kohfeld, Karen E | Calculated average/mean values | to depth of refusal, estimated from LOI using %C = 0.44(%LOI) -1.8 |
16 | Carbon | C | % | Kohfeld, Karen E | Calculated average/mean values | to the base peat layer, percent carbon estimated from LOI using %C = 0.44(%LOI)-1.8 |
17 | Carbon | C | % | Kohfeld, Karen E | Calculated standard error (SE) | standard error (stdev/sqrt(n)) of percent C to peat base |
18 | Carbon density, soil | SCD | g/cm3 | Kohfeld, Karen E | Calculated average/mean values | to depth of refusal, corrected for compaction |
19 | Carbon density, soil | SCD | g/cm3 | Kohfeld, Karen E | Calculated average/mean values | to base of peat layer, corrected for compaction |
20 | Carbon density, soil | SCD | g/cm3 | Kohfeld, Karen E | Calculated standard error (SE) | standard error (stdev/sqrt(n)) of SCD to peat base |
21 | Area in hectare | Area | ha | Kohfeld, Karen E | area of marsh zone in which core was collected | |
22 | Soil carbon stock | C stock | t/ha | Kohfeld, Karen E | to depth of refusal, Sum of partial carbon masses from each 1cm subsection from surface to DoR, MgC/ha | |
23 | Soil carbon stock | C stock | t/ha | Kohfeld, Karen E | to base of peat, Sum of partial carbon masses from each 1cm subsection from surface to base of peat, MgC/ha | |
24 | Soil carbon stock | C stock | t/ha | Kohfeld, Karen E | to 30 cm (corrected) depth | |
25 | Soil carbon stock | C stock | t/ha | Kohfeld, Karen E | to 20 cm (corrected) depth | |
26 | Soil carbon stock | C stock | t/ha | Kohfeld, Karen E | to shared 30 year horizon depth estimated by summing all partial carbon masses from each subsection to depth of 30 years | |
27 | Accumulation rate per year | Acc rate | g/cm2/a | Kohfeld, Karen E | core's mass accumulation rate | |
28 | Accumulation rate per year, standard deviation | Acc rate std dev | ± | Kohfeld, Karen E | ||
29 | Sedimentation rate per year | SR | cm/a | Kohfeld, Karen E | Calculated average/mean values | mean linear sedimentation rate |
30 | Sedimentation rate per year, standard deviation | SR std dev | ± | Kohfeld, Karen E | ||
31 | Accumulation rate, carbon, per year | Acc rate C | g/m2/a | Kohfeld, Karen E | 30 yr CAR: carbon accumulation rate of 30 years prior to 2016; this calculation only uses %C values for the 30 year depth mark and above | |
32 | Accumulation rate, carbon, per year, standard deviation | Acc rate C std dev | ± | Kohfeld, Karen E | 30 yr CAR SD: standard deviation of carbon accumulation rate for 30 years prior to 2016 | |
33 | Carbon | C | % | Kohfeld, Karen E | 30 yr %C: mass percentage of carbon for 30 years prior to 2016, Calculated from the cumulative mass of carbon (relative to total mass) for the past 30 years | |
34 | Accumulation rate, carbon, per year | Acc rate C | g/m2/a | Kohfeld, Karen E | basal peat CAR: carbon accumulation rate to basal age found at the depth of the deepest peat layer overlying sand/gravel | |
35 | Accumulation rate, carbon, per year, standard deviation | Acc rate C std dev | ± | Kohfeld, Karen E | basal peat CAR SD: standard deviation of carbon accumulation rate to depth of the deepest peat layer overlying sand/gravel | |
36 | Carbon | C | % | Kohfeld, Karen E | basal peat %C: mass percentage of carbon to depth of the deepest peat layer overlying sand/gravel | |
37 | Accumulation rate, carbon, per year | Acc rate C | t/a | Kohfeld, Karen E | basal (Mg C/y) | |
38 | Accumulation rate, carbon, per year | Acc rate C | t/a | Kohfeld, Karen E | 30 yr (Mg C/y) |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
834 data points