Preprints
https://doi.org/10.5194/essd-2025-422
https://doi.org/10.5194/essd-2025-422
22 Dec 2025
 | 22 Dec 2025
Status: this preprint is currently under review for the journal ESSD.

TephAta – An online data collection of tephra data from the Atacama Desert

Niklas Leicher, Vincent Feldmar, Andrés Quezada Jara, Paulina Vásquez Illanes, Fernando Sepúlveda Vásquez, Frank Wombacher, Markus Lagos, Tanja Kramm, Gabriel González, Klaudia Kuiper, Christoph Breitkreuz, Alberto Sáez, Domingo Gimeno, Lluís Cabrera, Inés Rodríguez Araneda, Bernd Wagner, Georg Bareth, and Volker Wennrich

Abstract. Tephrostratigraphy and -chronology are powerful tools using volcanic ash (tephra) layers for establishing stratigraphic correlations and/or to obtain chronological information for different kinds of sedimentary archives. To develop tephrostratigraphic frameworks, which ideally document a most complete spatial and temporal record of regional volcanic activity, precise geochemical and chronological characterization of tephra layers is needed. Based on these frameworks, newly discovered tephra layers can be linked to retrieve stratigraphic and chronological information. Tephrostratigraphic frameworks exist or are under construction for various regions. However, for some regions of the world the potential of these methods is not exploited yet, although being influenced by long-term and frequent volcanism and tephra deposition. One of these regions is the Atacama Desert of northern Chile. There geochemical compositions of Pleistocene tephra layers (volcanic glass) were recently systematically investigated for their stratigraphy and chronology within the scope of the Collaborative Research Centre ‘Earth – Evolution at the Dry Limit’ (CRC 1211). These analyses were accompanied by the development of a tephra database called TephAta, which aims at providing a long-term basis for tephrostratigraphic and -chronological data of the Atacama Desert. TephAta allows digital documentation of the full variety of tephra-related datasets within one database and provides search functions to foster and simplify the continuous expansion of the regional framework following the FAIR (findability, accessibility, interoperability, and reusability) data principles. A first data compilation of 106 tephra samples origin from 91 tephra deposits is now available and will be continuously extended spatially and temporally. TephAta does not only provide a stratigraphic and dating tool for paleoenvironmental or mapping studies, but it also helps to explore the integrity of the explosive volcanic history of the region along with the associated volcanic hazard and risk assessment.

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Niklas Leicher, Vincent Feldmar, Andrés Quezada Jara, Paulina Vásquez Illanes, Fernando Sepúlveda Vásquez, Frank Wombacher, Markus Lagos, Tanja Kramm, Gabriel González, Klaudia Kuiper, Christoph Breitkreuz, Alberto Sáez, Domingo Gimeno, Lluís Cabrera, Inés Rodríguez Araneda, Bernd Wagner, Georg Bareth, and Volker Wennrich

Status: open (until 28 Jan 2026)

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Niklas Leicher, Vincent Feldmar, Andrés Quezada Jara, Paulina Vásquez Illanes, Fernando Sepúlveda Vásquez, Frank Wombacher, Markus Lagos, Tanja Kramm, Gabriel González, Klaudia Kuiper, Christoph Breitkreuz, Alberto Sáez, Domingo Gimeno, Lluís Cabrera, Inés Rodríguez Araneda, Bernd Wagner, Georg Bareth, and Volker Wennrich

Data sets

TephATA Niklas Leicher and Vincent Feldmar https://www.crc1211db.uni-koeln.de/tephata

Niklas Leicher, Vincent Feldmar, Andrés Quezada Jara, Paulina Vásquez Illanes, Fernando Sepúlveda Vásquez, Frank Wombacher, Markus Lagos, Tanja Kramm, Gabriel González, Klaudia Kuiper, Christoph Breitkreuz, Alberto Sáez, Domingo Gimeno, Lluís Cabrera, Inés Rodríguez Araneda, Bernd Wagner, Georg Bareth, and Volker Wennrich
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Latest update: 22 Dec 2025
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Short summary
The TephATA database comprises morphological, geochemical, and chronological data of volcanic ash layers from the Atacama Desert. The dataset provides a basis for identifying the same volcanic ash layers in different sediment deposits and to determine their stratigraphic and chronological relationships. Known ages of volcanic eruptions can be transferred among equivalent ash layers, which allows dating of sediments. Also ash dispersal and the volcanic history of a region can be studied.
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