Abstract

The micro-Raman spectroscopy was used to identify manganese oxides, pyrolusite, manganite and cryptomelane in archaeological sites in northern Atacama Desert, Chile. The present micro-Raman data allow us to compare and expand the origins of raw materials used by archaic groups of the Atacama Desert. In the Andean highlands, pyrolusite and manganite were identified while in the coastal lowlands manganite and cryptomelane were found. The present results complement the data obtained from the lithic materials and rock art painting analyses pointing to a better understanding of the daily life of ancient populations and minerals use in this region. Black pigments found in three archaeological sites from northern Chile. Two of them are from the highlands: Tangani (Ta-1 and Ta-14) and one from the coast, Maderas Enco (Ari-26 and Ari-27). Raman spectra of different manganese oxides a) Ta-1, b) Ta-14, c) Ari-26 and d) Ari-27.

Highlights

  • Manganese (Mn) is one of the most abundant elements in nature–tenth within the Earth’s crust [1]

  • According to Ossa [2], the genesis of manganese deposits in northern Chile was traced to the deposition by circumvolcanic hot springs during the Pleistocene, deposits of manganese occurring at modern erosion levels are due to secondary mobilization

  • The molecular analysis allowed the characterization of the black pigments used by archaic communities in the lowlands and the highlands of northern Chile. From this point of view and focusing on the manganese oxides analyses, the results suggested that the sample from Ta-1 contains different manganese minerals, pyrolusite and manganite

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Summary

Introduction

Manganese (Mn) is one of the most abundant elements in nature–tenth within the Earth’s crust [1]. Mn is part of minerals formed in the early stages of magmatic crystallization. Significant quantities of Mn persist, it melts and can be plentiful in late-stage deposits such as pegmatites; near the Earth’s surface, Mn is oxidized, giving rise to several oxide-hydroxide minerals [1]. The most common mineral is pyrolusite (MnO2), which is black in colour [5]. Manganese is found in other minerals [6], such as rhodochrosite (MnCO3), rhodonite (MnSiO3), manganite (MnO(OH)), alabandite (MnS), cryptomelane (Kx(Mn4+,Mn3+)8O16), and hollandite (Ba(Mn46+Mn32+)O16) [7, 8]

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