Megaturbidite Deposits in the Holocene Basin Fill of Lake Como (Southern Alps, Italy) ⁎ Daniela Fanetti A, , Flavio S
This article was published in an Elsevier journal. The attached copy is furnished to the author for non-commercial research and education use, including for instruction at the author’s institution, sharing with colleagues and providing to institution administration. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Available online at www.sciencedirect.com Palaeogeography, Palaeoclimatology, Palaeoecology 259 (2008) 323–340 www.elsevier.com/locate/palaeo Megaturbidite deposits in the Holocene basin fill of Lake Como (Southern Alps, Italy) ⁎ Daniela Fanetti a, , Flavio S. Anselmetti b, Emmanuel Chapron b, Michael Sturm c, Luigina Vezzoli a a Dipartimento di Scienze Chimiche e Ambientali, Università degli Studi dell'Insubria, via Valleggio 11, I-22100 Como, Italy b Geological Institute, Swiss Federal Institute of Technology, ETH Zentrum, CH-8092 Zürich, Switzerland c EAWAG, Überlandstrasse 133, CH-8600 Dübendorf, Switzerland Received 8 October 2005; accepted 28 February 2007 Abstract For the first time, limnogeological investigations have been carried out in Lake Como, the deepest lake of the Alps, combining a bathymetric survey (multibeam Simrad 3000) with a high-resolution seismic reflection study (single-channel 3.5 kHz sub-bottom profiler) and a coring campaign (gravity corer). This data set enables detailed characterization of the sedimentary subsurface in the western branch of the lake, the Como branch, which has a typical fjord morphology.
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