The genesis of Yedoma Ice Complex permafrost – grain-size endmember modeling analysis from Siberia and Alaska

• Published in: E&G Quaternary Science Journal
• Main Authors: Schirrmeister, Lutz, Dietze, Elisabeth, Matthes, Heidrun, Grosse, Guido, Strauss, Jens, Laboor, Sebastian, Ulrich, Mathias, Kienast, Frank, Wetterich, Sebastian
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Copernicus 2020
• Subjects: Arctic; Remma; Ice; permafrost; wedge*; Alaska; Beringia; Siberia
• Online Access: https://epic.awi.de/id/eprint/52054/; https://epic.awi.de/id/eprint/52054/2/Schirrmeister_et_al_egqsj-69-33-2020.pdf; https://epic.awi.de/id/eprint/52054/3/Schirrmeister_et_al_egqsj-69-33-2020-supplement.pdf; https://hdl.handle.net/10013/epic.d71456e4-8077-4f7b-9cdd-980315052810

The late Pleistocene Yedoma Ice Complex is an ice-rich and organic-bearing type of permafrost deposit widely distributed across Beringia and is assumed to be especially prone to deep degradation with warming temperature, which is a potential tipping point of the climate system. To better understand Yedoma formation, its local characteristics, and its regional sedimentological composition, we compiled the grain-size distributions (GSDs) of 771 samples from 23 Yedoma locations across the Arctic; samples from sites located close together were pooled to form 17 study sites. In addition, we studied 160 samples from three non-Yedoma ice-wedge polygon and floodplain sites for the comparison of Yedoma samples with Holocene depositional environments. The multimodal GSDs indicate that a variety of sediment production, transport, and depositional processes were involved in Yedoma formation. To disentangle these processes, a robust endmember modeling analysis (rEMMA) was performed. Nine robust grain-size endmembers (rEMs) characterize Yedoma deposits across Beringia. The study sites of Yedoma deposits were finally classified using cluster analysis. The resulting four clusters consisted of two to five sites that are distributed randomly across northeastern Siberia and Alaska, suggesting that the differences are associated with rather local conditions. In contrast to prior studies suggesting a largely aeolian contribution to Yedoma sedimentation, the wide range of rEMs indicates that aeolian sedimentation processes cannot explain the entire variability found in GSDs of Yedoma deposits. Instead, Yedoma sedimentation is controlled by local conditions such as source rocks and weathering processes, nearby paleotopography, and diverse sediment transport processes. Our findings support the hypothesis of a polygenetic Yedoma origin involving alluvial, fluvial, and niveo-aeolian transport; accumulation in ponding waters; and in situ frost weathering as well as postdepositional processes of solifluction, cryoturbation, and ...