Late Quaternary sedimentation and permafrost development in a Svalbard fjord-valley, Norwegian high Arctic

• Published in: Sedimentology
• Main Authors: Gilbert, Graham L., O'Neill, Hugh B., Nemec, Wojciech, Thiel, Christine, Christiansen, Hanne H., Buylaert, Jan-Pieter
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2018
• Subjects: Adventdalen; Cryofacies; Cryostratigraphy; Fjord-head delta; Ground ice; Sedimentary facies; Spitsbergen; Arctic; Ice; permafrost; Svalbard
• Online Access: https://orbit.dtu.dk/en/publications/e6e1d6ca-0fcf-4ffc-a9bc-c1979af1738a; https://doi.org/10.1111/sed.12476

The infilling history of the Adventdalen fjord-valley in central Spitsbergen is reconstructed, with a focus on permafrost development, based on sedimentological and cryostratigraphic evidence from drilling cores. The techniques of optically stimulated luminescence and radiocarbon accelerator mass-spectrometry dating were used to establish sediment chronology. The fjord-fill sedimentary succession includes the fjord-bottom late Weichselian subglacial till of the Last Glacial Maximum, the early Holocene muddy glaciomarine deposits with ice-rafted debris formed during the fjord deglaciation, and the younger Holocene deposits of a fjord-head Gilbert-type delta of which the fluvial distributary plain shows raised alluvial terraces hosting aeolian sedimentation. This sedimentary record of the last glaciation/deglaciation cycle is interpreted in terms of sequence stratigraphy. Zones of epigenetic and syngenetic permafrost are recognized from the vertical distribution of cryofacies, with a conclusion that the formation of permafrost commenced and extended down-fjord as the fluvio-deltaic fjord-fill was gradually reaching subaerial exposure. The upwards-grown syngenetic permafrost and the top part of downwards-grown epigenetic permafrost below contain excess ice in a suite of cryofacies indicating ground-ice segregation and segregative intrusion. The deeper epigenetic permafrost is ice-poor and contains cryofacies formed solely by segregation processes. This case study may serve as an analogue for other similar Arctic fjord-valleys where the fjord-head shoreline was established during the post-Weichselian deglaciation.