Deception Island (South Shetland Islands) is one of the most active volcanoes in Antarctica, with more than 20 explosive eruptive events registered over the past few centuries. Recent eruptions (1967, 1969, and 1970) and volcanic unrest episodes (1992, 1999, and 2014–2015) demonstrate that volcanic activity will likely occur in the future. Despite this, there has been a considerable increase in the number of scientific bases, tourist activities and air and vessel traffic in the region during the last several decades. The escalation in interest has increased the amount of infrastructure and population numbers exposed to a future eruption. Thus, there is an urgent need to develop an accurate long-term assessment of the volcanic hazard of the island. However, past attempts have always been limited by the incompleteness of the eruptive record. Volcanic ash layers found in marine and lacustrine sediment cores and glaciers outside Deception Island are a fundamental source of information for reconstructing the explosive eruptive record of the volcano. The spatial distribution of the tephra layers, as well as their physicochemical analysis are invaluable for determining the size and explosiveness of past eruptive events, as well as for assessing the extent and impact of their related hazards (e.g., ash fall out). In order to overcome the dispersion of existing data among numerous publications and to facilitate the analysis of available information on tephra layers sourced in Deception Island, we present the DecTephra (Deception Island Tephra Record) database. The current database version contains 362 tephra layers (including cryptotephras) located at sites up to 3115 km distant from the island. For each tephra layer, the database includes: (i) the location and simple description of the sampling site; and (ii) the key petrologic and geochemical features of each tephra layer. A preliminary analysis of the information contained in the DecTephra database (e.g., magma composition, explosiveness, eruptive recurrence, etc.), validates it as a key tool for evaluating past explosive activity of the volcano. In addition, it can function as a valuable resource for paleoenvironmental and paleoclimatic studies requiring tephrostratigraphical and tephrochronological control at local and regional scales. DecTephra also has the potential to help to assess the contribution of volcanic forcing to Holocene climate variability in the Southern Hemisphere.

This research was supported by MINECO projects VOLCLIMA (CGL2015-72629-EXP), VOLGASDEC (PGC2018-095693-B-I00) (AEI/FEDER, EU) and the MCIN/AEI/10.13039/501100011033 grant HYDROCAL (PID2020-114876GB-I00). A.G. is grateful for her Ramón y Cajal contract (RYC-2012-11024), A.M.A-V for the grant under the “JSPS invitation fellowship” program (S18113) and A.P·S is grateful for his PhD grant “Programa Propio III Universidad de Salamanca co-funded by Banco de Santander” and his JAE_Intro scholarship (JAEINT_20_00670). This research is part of POLARCSIC and PTI VOLCAN activities. We are grateful to Grant George Buffett (TERRANOVA SCIENTIFIC; www.terranova.barcelona) for English editing of an early draft of this paper.

Peer reviewed