Fritz, Michael; Wolter, Juliane; Rudaya, Natalya A; Palagushkina, Olga V; Nazarova, Larisa B; Obu, Jaroslav; Rethemeyer, Janet; Lantuit, Hugues; Wetterich, Sebastian (2016): Sedimentology, biogeochemistry stable isotopes, pollen, plant macrofossils, and diatoms from two sediments cores from the northern Yukon permafrost peatlands (Canada). PANGAEA, https://doi.org/10.1594/PANGAEA.856781, Supplement to: Fritz, M et al. (2016): Holocene ice-wedge polygon development in northern Yukon permafrost peatlands (Canada). Quaternary Science Reviews, 147, 279-297, https://doi.org/10.1016/j.quascirev.2016.02.008
Always quote citation above when using data! You can download the citation in several formats below.
Ice-wedge polygon (IWP) mires in the Arctic and Subarctic are extremely vulnerable to climatic and environmental change. We present the results of a multidisciplinary paleoenvironmental study on IWPs in the northern Yukon, Canada. High-resolution laboratory analyses were carried out on a permafrost core and the overlying seasonally thawed (active) layer, from a low-centered IWP located in a drained lake basin on Herschel Island. In relation to 14 Accelerator Mass Spectrometry (AMS) radiocarbon dates spanning the last 5000 years, we report sedimentary data including grain size distribution and biogeochemical parameters (organic carbon, nitrogen, C/N ratio, d13C), stable water isotopes (d18O, dD), as well as fossil pollen, plant macrofossil and diatom assemblages. Three sediment units (SUs) correspond to the main stages of deposition (1) in a thermokarst lake (SU1: 4950 to 3950 cal yrs BP), (2) during transition from lacustrine to palustrine conditions after lake drainage (SU2: 3950 to 3120 cal yrs BP), and (3) in palustrine conditions in the IWP field that developed after drainage (SU3: 3120 cal yrs BP to AD 2012). The lacustrine phase (pre 3950 cal yrs BP) is characterized by planktonic-benthic and pioneer diatoms species indicating circumneutral waters, and very few plant macrofossils. The pollen record has captured a regional signal of relatively stable vegetation composition and climate for the lacustrine stage of the record until 3950 cal yrs BP. Palustrine conditions with benthic and acidophilic species characterize the peaty shallow-water environments of the low-centered IWP. The transition from lacustrine to palustrine conditions was accompanied by acidification and rapid revegetation of the lake bottom within about 100 years. Since the palustrine phase we consider the pollen record as a local vegetation proxy dominated by the plant communities growing in the IWP. Ice-wedge cracking in water-saturated sediments started immediately after lake drainage at about 3950 cal yrs BP and led to the formation of an IWP mire. Permafrost aggradation through downward closed-system freezing of the lake talik is indicated by the stable water isotope record. The originally submerged IWP center underwent gradual drying during the past 2000 years. This study highlights the sensitivity of permafrost landscapes to climate and environmental change throughout the Holocene.
Latitude: 69.579530 * Longitude: -138.957400
Date/Time Start: 2012-07-31T00:00:00 * Date/Time End: 2012-08-03T00:00:00
Datasets listed in this publication series
- Fritz, M; Wolter, J; Rudaya, NA et al. (2016): (Table 1) Age determination of sediment core PG2100. https://doi.org/10.1594/PANGAEA.856771
- Fritz, M; Wolter, J; Rudaya, NA et al. (2016): (Table 1) Age determination of sediment core YC12-HP-Mc. https://doi.org/10.1594/PANGAEA.856772
- Fritz, M; Wolter, J; Rudaya, NA et al. (2016): (Table 2) Sedimentology and biogeochemistry of sediment cores YC12-HP-Mc and PG2100. https://doi.org/10.1594/PANGAEA.856773
- Fritz, M; Wolter, J; Rudaya, NA et al. (2016): (Table 3) Stable water isotopes of sediment cores YC12-HP-Mc and PG2100. https://doi.org/10.1594/PANGAEA.856775
- Fritz, M; Wolter, J; Rudaya, NA et al. (2016): (Table 4) Pollen profile of sediment core PG2100. https://doi.org/10.1594/PANGAEA.856777
- Fritz, M; Wolter, J; Rudaya, NA et al. (2016): (Table 5) Plant macrofossils of sediment cores YC12-HP-Mc and PG2100. https://doi.org/10.1594/PANGAEA.856778
- Fritz, M; Wolter, J; Rudaya, NA et al. (2016): (Table 6) Diatoms of sediment core PG2100. https://doi.org/10.1594/PANGAEA.856780