Surface vitrification caused by natural fires in Late Pleistocene wetlandsof the Atacama Desert

Autor: Roperch, Pierrick, GATTACCECA, Jerome, Valenzuela, Millarca, Devouard, Bertrand, Lorand, Jean-Pierre, Al., Et
Přispěvatelé: Géosciences Rennes (GR), Université de Rennes 1 (UR1), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)-Centre National de la Recherche Scientifique (CNRS), Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Collège de France (CdF)-Institut national des sciences de l'Univers (INSU - CNRS)-Aix Marseille Université (AMU)-Institut National de la Recherche Agronomique (INRA), Pontifical Catholic University of Chile, Laboratoire de Planétologie et Géodynamique UMR6112 (LPG), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Nantes - Faculté des Sciences et des Techniques, Université de Nantes (UN)-Université de Nantes (UN)-Université d'Angers (UA), European Geosciences Union, Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS), Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géodynamique [UMR 6112] (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA), Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 1 (UR1), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)
Jazyk: angličtina
Rok vydání: 2017
Předmět:
Zdroj: European Geosciences Union General Assembly 2017
European Geosciences Union General Assembly 2017, Apr 2017, Vienne, Austria. Geophysical Research Abstracts, 19, pp.EGU2017-8946, 2017
Popis: International audience; Melted rocks are a common feature in many of the 175 recognized terrestrial impact structures [1]. However, someglasses, like the Dakhleh Glass [2] or the Edeowie Glass [3] are also attributed to impacts despite the lack of otherdirect evidence. These cases have been attributed to low-altitude airbursts of cosmic bodies (asteroids, comets)during their entry in the Earth’s atmosphere but the identification and mechanism of formation of these glasses arehowever debated.Massive glass blocks were recently discovered [4] in the Tamarugal-Llamara basin of the Atacama desert in Chile.We show that these glasses, found near the town of Pica at four localities separated by up to 70 km, are neitherfulgurites, nor volcanic glasses, nor metallurgical slags related to anthropic activity, but show close similaritieswith other glasses, which have been attributed to large airbursts. However, most glasses contain numerous plantimprints and some glasses are mainly made of partially melted silicified plant twigs and field observations indicatethat the glasses are restricted to specific Late Pleistocene wetlands. Large oases did indeed form in the hyperaridAtacama desert due to elevated groundwater discharge and increased recharge during the Central Andean PluvialEvent (roughly coeval with the Mystery interval and Younger Dryas). 14C dating and paleomagnetic dataindicate that the glasses were formed during at least two distinct periods. The strong environmental control onthe distribution of the glasses and large differences in ages rule out the hypothesis of a single large airburst asthe cause of surface melting. The available data suggest that the Atacama desert surface glasses were formedin situ by natural fires in soils rich in dry organic matter and siliceous biological remains, at a time of strongclimate oscillations between wet (organic matter accumulation in soils) and dry periods (triggering fires) in desertwetlands.Our interpretation likely applies to other cases of silicate glasses attributed to airbursts, challenging the highairburst rate as well as the interpretation of fossils and organic matter in “impact glasses” [5]. Our study alsodemonstrates that exotic mineralogy with glass containing spherules of iron sulphides, metallic iron or ironphosphides may not necessarily imply an impact origin. This in turn cast doubts on some studies relating impactand climate change triggering the Younger Dryas cold event at the end of the Pleistocene [6].1. French, B. M. & Koeberl, C. Earth-Sci. Rev. 98, 123–170 (2010).2. Osinski, G. R. et al. Meteorit. Planet. Sci. 43, 2089–2107 (2008).3. Haines, P. W., Jenkins, R. J. F. & Kelley, S. P. Geology 29, 899 (2001).4. Blanco, N. & Tomlinsson, A. J. Carta Guatacondo, Región de Tarapacá. (2013).5. Schultz, P. H., Harris, R. S., Clemett, S. J., Thomas-Keprta, K. L. & Zarate, M. Geology 42, 515–518 (2014).6. Firestone, R. B. et al. Proc. Natl. Acad. Sci. 104, 16016–16021 (2007
Databáze: OpenAIRE
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