Variation in greenhouse gas production within a thermokarst lagoon system, outer Mackenzie Delta, Canada
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2025
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| _version_ | 1867170129014423552 |
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| author | Jenrich, Maren |
| author_facet | Jenrich, Maren |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | When highly degraded, lowland thermokarst landscapes are flooded by the sea, and thermokarst lagoons, lakes, and the sea become connected with each other, complex lagoon systems are formed. Consequently, a natural gradient of marine submergence age and connectivity emerges within the system with older, well-connected lagoons closer to the sea, and younger, less connected lagoons further inland. The dataset presents the cumulative greenhouse gas production and daily production rates from 7 lagoons of variing sea connectivity and permafrost and active layer as endmembers. In detail sediment of active layer (AL) and permafrost (PF) from a soil pit located on the lowland of Reindeer Island (RI21-P2-AL, RI21-P2-PF), a thermokarst lake (RI21-05 (TKL05)), a limited open lagoon (LAG13), two semi-open lagoons (LAG04; LAG14), two mostly open lagoons (LAG03; LAG16) and two open lagoons (LAG07; LAG12). We incubated the samples anaerobically at 4 °C under fresh (c=0 g/L), brackish (c=13g/L) and marine (36g/L) conditions for one year and measured carbon dioxide (CO2) and methane (CH4) concentrations regularly in a 250 µL subsample using gas chromatography with an Agilent GC 7890A equipped with an Agilent HP-PLOT Q column. Cumulative CO2 and CH4 concentrations and production rates per day are given over time for all samples with three replicates each per gram of dry weight and normalised to gram of soil organic carbon (SOC). |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_974430 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Variation in greenhouse gas production within a thermokarst lagoon system, outer Mackenzie Delta, Canada Jenrich, Maren AWI_Perma; AWI Arctic Land Expedition; CA-Land_2021_ReindeerIsland; CA-Land_2021_Tuktoyaktuk; Carbon dioxide, production, anaerobic, cumulative, per soil dry mass; Carbon dioxide, production, anaerobic, cumulative, per unit mass soil organic carbon; Carbon dioxide, production rate, per mass soil organic carbon; Carbon dioxide, production rate, per soil dry mass; CH4; CO2; DATE/TIME; DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Event label; Gas chromatography on an Agilent Technologies 7890A GC; GCUWI; Gravity corer, UWITEC; HAND; Identification; Incubation duration; incubation experiment; LAG03; LAG04; LAG07; LAG12; LAG13; LAG14; LAG16; Methane, production, anaerobic, cumulative, per soil dry mass; Methane, production, anaerobic, cumulative, per unit mass soil organic carbon; Methane, production rate, per mass soil organic carbon; Methane, production rate, per soil dry mass; Northwest Territories, Canada; Permafrost Research; RI21-12-1; RI21-13-2; RI21-14-1; RI21-16-2; RI21-3-3; RI21-4-3; RI21-5-3; RI21-7-2; RI21-P2-AL-1; RI21-P2-PF-1; Sample code/label; Sampling by hand; seawater impact; Sediment type; talik; TKL05; Treatment; Treatment: salinity When highly degraded, lowland thermokarst landscapes are flooded by the sea, and thermokarst lagoons, lakes, and the sea become connected with each other, complex lagoon systems are formed. Consequently, a natural gradient of marine submergence age and connectivity emerges within the system with older, well-connected lagoons closer to the sea, and younger, less connected lagoons further inland. The dataset presents the cumulative greenhouse gas production and daily production rates from 7 lagoons of variing sea connectivity and permafrost and active layer as endmembers. In detail sediment of active layer (AL) and permafrost (PF) from a soil pit located on the lowland of Reindeer Island (RI21-P2-AL, RI21-P2-PF), a thermokarst lake (RI21-05 (TKL05)), a limited open lagoon (LAG13), two semi-open lagoons (LAG04; LAG14), two mostly open lagoons (LAG03; LAG16) and two open lagoons (LAG07; LAG12). We incubated the samples anaerobically at 4 °C under fresh (c=0 g/L), brackish (c=13g/L) and marine (36g/L) conditions for one year and measured carbon dioxide (CO2) and methane (CH4) concentrations regularly in a 250 µL subsample using gas chromatography with an Agilent GC 7890A equipped with an Agilent HP-PLOT Q column. Cumulative CO2 and CH4 concentrations and production rates per day are given over time for all samples with three replicates each per gram of dry weight and normalised to gram of soil organic carbon (SOC). |
| title | Variation in greenhouse gas production within a thermokarst lagoon system, outer Mackenzie Delta, Canada |
| topic | AWI_Perma; AWI Arctic Land Expedition; CA-Land_2021_ReindeerIsland; CA-Land_2021_Tuktoyaktuk; Carbon dioxide, production, anaerobic, cumulative, per soil dry mass; Carbon dioxide, production, anaerobic, cumulative, per unit mass soil organic carbon; Carbon dioxide, production rate, per mass soil organic carbon; Carbon dioxide, production rate, per soil dry mass; CH4; CO2; DATE/TIME; DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Event label; Gas chromatography on an Agilent Technologies 7890A GC; GCUWI; Gravity corer, UWITEC; HAND; Identification; Incubation duration; incubation experiment; LAG03; LAG04; LAG07; LAG12; LAG13; LAG14; LAG16; Methane, production, anaerobic, cumulative, per soil dry mass; Methane, production, anaerobic, cumulative, per unit mass soil organic carbon; Methane, production rate, per mass soil organic carbon; Methane, production rate, per soil dry mass; Northwest Territories, Canada; Permafrost Research; RI21-12-1; RI21-13-2; RI21-14-1; RI21-16-2; RI21-3-3; RI21-4-3; RI21-5-3; RI21-7-2; RI21-P2-AL-1; RI21-P2-PF-1; Sample code/label; Sampling by hand; seawater impact; Sediment type; talik; TKL05; Treatment; Treatment: salinity |
| url | https://doi.org/10.1594/PANGAEA.974430 |