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Bibliographic Details
Main Authors: Wagner, Bernd, Aufgebauer, Anne, Vogel, Hendrik, Zanchetta, Giovanni, Sulpizio, Roberto, Damaschke, Magret
Format: Dataset Open Access
Language:en
Published: PANGAEA 2013
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.804607
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author Wagner, Bernd
Aufgebauer, Anne
Vogel, Hendrik
Zanchetta, Giovanni
Sulpizio, Roberto
Damaschke, Magret
author_facet Wagner, Bernd
Aufgebauer, Anne
Vogel, Hendrik
Zanchetta, Giovanni
Sulpizio, Roberto
Damaschke, Magret
collection Datos científicos de ciencias marinas y ambientales
contents Hydro-acoustic surveys and coring campaigns at Lake Prespa were carried out between 2007 and 2009. This paper presents hydro-acoustic profiles and provide lithological and chronostratigraphical information from three up to 15.75 m long sediment sequences from the Macedonian side of the lake. The sediment sequences comprise glacial and interglacial sediments likely deposited from the end of Marine Isotope Stage (MIS) 5 to present day. The information implies a distinct change of sedimentation patterns at the Pleistocene/Holocene transition and the establishment of a relatively strong Holocene current system and deposition of channel-related contourite drift in Lake Prespa. Potential causes for the establishment of this current during the Holocene include significant lake level change, reduced winter ice cover, and/or higher aeolian activity.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_804607
institution PANGAEA
language en
publishDate 2013
publisher PANGAEA
record_format pangaea
spellingShingle Sedimentology on profiles from Lake Prespa, Greece
Wagner, Bernd
Aufgebauer, Anne
Vogel, Hendrik
Zanchetta, Giovanni
Sulpizio, Roberto
Damaschke, Magret
Co1216; Lake Prespa, Albania; PCUWI; Piston corer, UWITEC
Hydro-acoustic surveys and coring campaigns at Lake Prespa were carried out between 2007 and 2009. This paper presents hydro-acoustic profiles and provide lithological and chronostratigraphical information from three up to 15.75 m long sediment sequences from the Macedonian side of the lake. The sediment sequences comprise glacial and interglacial sediments likely deposited from the end of Marine Isotope Stage (MIS) 5 to present day. The information implies a distinct change of sedimentation patterns at the Pleistocene/Holocene transition and the establishment of a relatively strong Holocene current system and deposition of channel-related contourite drift in Lake Prespa. Potential causes for the establishment of this current during the Holocene include significant lake level change, reduced winter ice cover, and/or higher aeolian activity.
title Sedimentology on profiles from Lake Prespa, Greece
topic Co1216; Lake Prespa, Albania; PCUWI; Piston corer, UWITEC
url https://doi.org/10.1594/PANGAEA.804607