Wu, Junjie; Mollenhauer, Gesine; Stein, Ruediger; Köhler, Peter (2022): Ice retreat, C fluxes, atmospheric Delta14C, and atmospheric CO2 simulations [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.939846, In: Wu, J et al. (2022): Biomarker and radiocarbon data of core ARA04C/37 and JPC15 from the Beaufort Sea, Arctic Ocean [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.939847
Always quote citation above when using data! You can download the citation in several formats below.
Keyword(s):
Further details:
Amiotte Suchet, Philippe; Probst, Jean-Luc; Ludwig, Wolfgang (2003): Worldwide distribution of continental rock lithology: Implications for the atmospheric/soil CO2 uptake by continental weathering and alkalinity river transport to the oceans. Global Biogeochemical Cycles, 17(2), https://doi.org/10.1029/2002GB001891
Peltier, W R; Argus, Donald F; Drummond, R (2015): Space geodesy constrains ice age terminal deglaciation: The global ICE-6G_C (VM5a) model. Journal of Geophysical Research: Solid Earth, 120(1), 450-487, https://doi.org/10.1002/2014JB011176
Winterfeld, Maria; Mollenhauer, Gesine; Dummann, Wolf; Köhler, Peter; Lembke-Jene, Lester; Meyer, Vera D; Hefter, Jens; McIntyre, Cameron; Wacker, Lukas; Kokfelt, Ulla; Tiedemann, Ralf (2018): Deglacial mobilization of pre-aged terrestrial carbon from degrading permafrost. Nature Communications, 9(1), https://doi.org/10.1038/s41467-018-06080-w
Comment:
Koehler_NH_iceretreat_over_shales_20ka: Ice retreat over shales in North America is calculated in the area 180°W-75°W, 45°N-90°N based on maps available in 1°x1° spatial resolution of: 1) land ice: ICE6G after Peltier, et al. (2015) lithology from Amiotte Suchet et al. (2003).
Koehler_cfluxes_20ka: C fluxes (oxidation of pedrogenic organic carbon) from ice retreat over shales in North America.
Koehler_atmD14C_20ka: Simulated changes in atmospheric Delta14C (permil) using the BICYCLE-SE mode. (process A): caused by release oxidation of pedrogenic organic carbon, (process B): caused by Arctic permafrost mobilization (Winterfeld et al., 2018).
Koehler_atmCO2_20ka: Simulated changes in atmospheric CO2 (ppm) using the BICYCLE-SE model. (process A): caused by release oxidation of pedrogenic organic carbon, (process B): caused by Arctic permafrost mobilization (Winterfeld et al., 2018).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | File content | Content | Wu, Junjie | |||
| 2 | Binary Object | Binary | Wu, Junjie |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Basic curation (CurationLevelB)
Size:
8 data points
Data
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| 1 Content | 2 Binary |
|---|---|
| Ice retreat over shales in North America | Koehler_NH_iceretreat_over_shales_20ka.dat |
| C fluxes (oxidation of pedrogenic organic carbon) from ice retreat over shales in North America | Koehler_cfluxes_20ka.dat |
| Simulated changes in atmospheric Delta14C (permil) using the BICYCLE-SE mode. (process A): caused by release oxidation of pedrogenic organic carbon, (process B): caused by Arctic permafrost mobilization (Winterfeld et al., 2018) | Koehler_atmD14C_20ka.dat |
| Simulated changes in atmospheric CO2 (ppm) using the BICYCLE-SE model. (process A): caused by release oxidation of pedrogenic organic carbon, (process B): caused by Arctic permafrost mobilization (Winterfeld et al., 2018) | Koehler_atmCO2_20ka.dat |