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Sediments from Lake Cheko (Siberia), a possible impact crater for the 1908 Tunguska Event
Authors:Luca Gasperini  Enrico Bonatti  Sonia Albertazzi  Luisa Forlani  Carla A Accorsi  Giuseppe Longo  Mariangela Ravaioli  Francesca Alvisi  Alina Polonia  Fabio Sacchetti
Institution:1. Istituto di Scienze Marine (ISMAR) CNR, Bologna, Italy;2. Dipartimento di Biologia evoluzionistica sperimentale, Università di Bologna, Italy;3. Dipartimento del Museo di Paleobiologia e dell’Orto Botanico, Università di Modena e Reggio Emilia, Italy;4. Dipartimento di Fisica, Università di Bologna, Italy
Abstract:Cheko, a small lake located in Siberia close to the epicentre of the 1908 Tunguska explosion, might fill a crater left by the impact of a fragment of a Cosmic Body. Sediment cores from the lake’s bottom were studied to support or reject this hypothesis. A 175‐cm long core, collected near the center of the lake, consists of an upper ~1 m thick sequence of lacustrine deposits overlaying coarser chaotic material. 210Pb and 137Cs indicate that the transition from lower to upper sequence occurred close to the time of the Tunguska Event. Pollen analysis reveals that remains of aquatic plants are abundant in the top post‐1908 sequence, but are absent in the lower pre‐1908 portion of the core. These results, including organic C, N and δ13C data, suggest that Lake Cheko formed at the time of the Tunguska Event.
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