A multi-proxy study of Argentina loess: Marine oxygen isotope stage 4 and 5 environmental record from pedogenic hematite

• Published in: Palaeogeography, Palaeoclimatology, Palaeoecology
• Main Authors: Carter-Stiglitz, Brian, Banerjee, Subir K., K., Gourlan, Alexandra Gourlan, Oches, Eric
• Other Authors: Institute for Rock Magnetism, Newton Horace Winchell School of Earth Sciences Minneapolis, University of Minnesota Twin Cities (UMN), University of Minnesota System (UMN)-University of Minnesota System (UMN), Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Department of Geology, University of South Florida, Tampa 33620, USA (DEPARTMENT OF GEOLOGY, UNIVERSITY OF SOUTH FLORIDA, TAMPA 33620, USA), University of Florida Gainesville (UF)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2006
• Subjects: [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry; Antarc*; Antarctica
• Online Access: https://hal.science/hal-00148774; https://doi.org/10.1016/j.palaeo.2006.01.008

International audience A 12 m loess–paleosol section (La Angostura) from Tafi del Valle, Tucumán, Argentina was studied using rock magnetic measurements, geochemistry, Mössbauer effect, particle size and Nd isotopes in order to elucidate changes in paleoenvironment at the site. Combining the results of these experiments allowed us to separate the effects of the two major controls (parent material and pedogenesis) on the measured parameters. Two behavior regimes were identified in the sediment: 1) in the lower half of the section pedogenic processes, though weak, dominate the variation of the sediment's physical properties, and 2) for the upper half of the section subtle changes in parent material control the majority of the measured parameters, even those typically controlled by pedogenesis, e.g., clay fraction. Applying rock magnetic, Mössbauer, and bulk geochemistry measurements in concert we calculated an iron budget for the loess. not, vert, similar80% of the iron in the sediment is in paramagnetic minerals; not, vert, similar20% of the iron is in hematite (not, vert, similar1.6% of the sediment's mass), and much less-than 1% of the total iron is present as magnetite/maghemite (not, vert, similar0.1% of the sediment's total mass). Neither the pedogenic formation nor the depletion of ferrimagnetic material with increasing pedogenesis was consistently observed in this sediment. Throughout the entire section the concentration of hematite is argued to be sensitive to in situ alteration, and it is further surmised to be sensitive to the available moisture at the site. Finally we present a curiosity: within the error of our chronology, the concentration of hematite seems to correlate with the coeval climate record from Antarctica (Vostok). It is possible that the sedimentary–magnetic record from La Angostura is a proxy for the strength of the South American summer monsoon.