New insights on sources contributing dust to the loess record of the western edge of the Pampean Plain during the transition from the late MIS 2 to the early Holocene. (April 2020)

• Record Type: Journal Article
• Authors: Torre, Gabriela; Gaiero, Diego M; Cosentino, Nicolás Juan; Coppo, Renata; Oliveira-Sawakuchi, André
• Other Names: De Vleeschouwer François guest-editor.; Stuut Jan-Berend W guest-editor.; Lambert Fabrice guest-editor.
• Is Part Of: Holocene. Volume 30:Number 4(2020)
• Page Start: 537
• Page End: 545
• Publication Date: 2020-04
• Subjects: early Holocene -- grain-size -- loess -- Pampas -- provenance -- REE; Geology, Stratigraphic -- Holocene -- Periodicals; Paleoclimatology -- Periodicals; 333.7
• DOI: 10.1177/0959683619875187
• Languages: English
• ISSNs: 0959-6836

Abstract

High-resolution studies of palaeorecords located closer to the dust source areas of South America are relevant for increasing the knowledge on past climatic conditions in the Southern Hemisphere. In this sense, the Pampean loess archives can offer explicit records of dust source, transport, and deposition in the region, providing new insights which may be used to better understand the role of dust in future climate change scenarios. In this work, we studied a loess sequence located at the westernmost Pampean Plain. The studied sequence covers a span of time from the late Marine Isotope Stage (MIS 2) period up to the early Holocene. Loess samples from this record have two grain-size populations, indicating more than one dust source area. The dominance of a coarse-silt subpopulation during the transition from the late MIS 2 to the early Holocene suggests that proximal dust sources were dominant at that time. Two of the most proximal dust sources were analyzed as probable contributors to the Lozada site: sediments derived from the Eastern Pampean Ranges and sediments derived from the shorelines of the Mar Chiquita Lake. The geochemical data suggest that neither area was a significant dust source to the eastern Pampean Plain during the studied interval. Instead, our geochemical data suggest a dominant supply from a southern and relatively closer area, linked to the foothills of the Andes, and the increased activation during the early Holocene of a more distant source to the north in the Puna region, which contributed finer loess.