OGS Core Logging Lab - logging sediment cores in Lago Argentino (Brazo Sur), Argentina
Cite as:
Caburlotto, Andrea; Caffau, Mauro; Lodolo, Emanuele (2025): OGS Core Logging Lab - logging sediment cores in Lago Argentino (Brazo Sur), Argentina. GFZ Data Services. https://doi.org/10.5880/fidgeo.2025.020
Status
I N R E V I E W : Caburlotto, Andrea; Caffau, Mauro; Lodolo, Emanuele (2025): OGS Core Logging Lab - logging sediment cores in Lago Argentino (Brazo Sur), Argentina. GFZ Data Services. https://doi.org/10.5880/fidgeo.2025.020
Abstract
The spectacular water outburst occurring semi-periodically when the ice-dam formed by the external front of the Perito Moreno glacier collapses, is one of the most attracting events in the UNESCO ‘Parque Nacional Los Glaciares’ of southern Patagonia. These occurrences have been documented since 1936. Instead, evidence of previous events has been only indirectly provided by dendrochronology analysis. Four sediments cores have been collected on coastal soil in 2017, analysed by X rays, HR photography and Magnetic Susceptibility. The radiographies of these cores allowed to identify lake floodings deposits due to glacier readvance over the coastal soil related to the collapse of the Perito Moreno ice-dam. In November 2018, 10 undisturbed sediment gravity cores were collected within a small inlet of Brazo Sur, that is, the southern arm of Lago Argentino, at water depths ranging from 10 to 6 m using a 4.5 cm diameter gravity corer ‘KC Kajak Sediment Sampler’ Model 13.030.
The length of these cores varies from 45 to 65 cm. X rays, HR photography and magnetic susceptibility provide the first evidence of an abrupt change in the stratigraphic record found at variable depths of 14–18 cm from the top of the cores, marked by a hiatus spanning ca. 3200 years, separating planar-laminated sediments below from an alternation of erosional and depositional events above it, indicating recurring high-energy conditions generated by the emptying of the lake basin, as well as ash layers observed in the longest cores. Radio carbon data collected on three of these cores record ice-daming in the Little Ice age, at 324-266 cal yrs BP. These well-preserved stratigraphic records highlight the key role of glaciolacustine deposits in reconstructing the glacial dynamics and palaeoclimate evolution of a glaciated region.
Technical Information
Magnetic Susceptibility data has been acquired by a Barrington point sensor MS2E, mounted on Geotek® Multisensoriale Core Logger. Resolution to 2×10-6 SI Range 26 SI Measurement period down to 0.1s
High Resolution Photography have been acquired by the Geoscan V linescan camera installed onto the Geotek® Multi Sensor Core Logger, together with RGB data every centimetre. Specification: Camera Geotek GEOSCAN V 5000 pixel CCD linescan camera, with standard Canon lens mount. Light source Broad-spectrum LED illumination or ultraviolet LEDs for UV fluorescence imaging. Images Output 50 micron per pixel 48-bit RGB TIFF images, converted to 24-bit colour JPG on request.
X Rays have been acquired by Geotek® CT System (XCT).
Acquisition parameters:
XR source: voltage 80 kV current 200 uA
Detector Resolution: 1920 x 1536 pixel
Image resolution: 245 pixel/cm
Authors
Caburlotto, Andrea;OGS-National Institute of Oceanography and Applied Geophysics and University of Trieste, Italy
Caffau, Mauro;OGS-National Institute of Oceanography and Applied Geophysics and University of Trieste, Italy
Lodolo, Emanuele;OGS-National Institute of Oceanography and Applied Geophysics and University of Trieste, Italy
Contact
Caburlotto
(Andrea); OGS-National Institute of Oceanography and Applied Geophysics and University of Trieste, Italy; ➦
Contributors
Core Logging LAB (OGS-National Institute of Oceanography and Applied Geophysics and University of Trieste, Italy); Caburlotto
Keywords
Ice-damming, lithostratigraphic hiatus, Little Ice Age, Perito Moreno glacier, EPOS, multi-scale laboratories, rock and melt physical properties
CharacterString: The spectacular water outburst occurring semi-periodically when the ice-dam formed by the external front of the Perito Moreno glacier collapses, is one of the most attracting events in the UNESCO ‘Parque Nacional Los Glaciares’ of southern Patagonia. These occurrences have been documented since 1936. Instead, evidence of previous events has been only indirectly provided by dendrochronology analysis. Four sediments cores have been collected on coastal soil in 2017, analysed by X rays, HR photography and Magnetic Susceptibility. The radiographies of these cores allowed to identify lake floodings deposits due to glacier readvance over the coastal soil related to the collapse of the Perito Moreno ice-dam. In November 2018, 10 undisturbed sediment gravity cores were collected within a small inlet of Brazo Sur, that is, the southern arm of Lago Argentino, at water depths ranging from 10 to 6 m using a 4.5 cm diameter gravity corer ‘KC Kajak Sediment Sampler’ Model 13.030.
The length of these cores varies from 45 to 65 cm. X rays, HR photography and magnetic susceptibility provide the first evidence of an abrupt change in the stratigraphic record found at variable depths of 14–18 cm from the top of the cores, marked by a hiatus spanning ca. 3200 years, separating planar-laminated sediments below from an alternation of erosional and depositional events above it, indicating recurring high-energy conditions generated by the emptying of the lake basin, as well as ash layers observed in the longest cores. Radio carbon data collected on three of these cores record ice-daming in the Little Ice age, at 324-266 cal yrs BP. These well-preserved stratigraphic records highlight the key role of glaciolacustine deposits in reconstructing the glacial dynamics and palaeoclimate evolution of a glaciated region.
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CharacterString: Caburlotto
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CharacterString: OGS-National Institute of Oceanography and Applied Geophysics and University of Trieste, Italy
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;OGS-National Institute of Oceanography and Applied Geophysics and University of Trieste, Italy
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