Preprints
https://doi.org/10.5194/egusphere-2026-4779
https://doi.org/10.5194/egusphere-2026-4779
23 Sep 2026
 | 23 Sep 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Preservation of Glaciochemical Signals in a Warming Tropical Ice Cap: Evidence from the 2022 Quelccaya Ice Core

João Gomes Ilha, Manoela Brum Poitevin Portella, Oscar Vilca Gomez, Filipe Gaudie Lindau, Mariusz Potocki, Elena Barbaro, Susan Kaspari, Carlo Barbante, Jefferson Cardia Simões, and Paul Andrew Mayewski

Abstract. Paleoclimate records stored in ice cores are facing great threat as on-going mass loss is rapidly accelerating. To study Amazon’s paleoclimate, an ice core was drilled in the Quelccaya ice cap, in Peru, in 2022. However, as a first step, post-depositional alterations need to be discussed and described. During drilling, one water table (WT) associated with the firn-ice transition and a major fracture at 45 m depth were identified. Here we present the first chemical results retrieved from the ice core and discuss the preservation state of the record in terms of post-depositional alterations. Concentrations of levoglucosan, Na+, K+, Cl, SO42− and NO3 were analyzed and compared with the relatively insoluble and immobile black carbon signal. Furthermore, signal preservation was evaluated using descriptive statistics, covariance analysis, ionic balance, and multivariate classification. Statistical analyses reveal enhanced ion concentration atop the WT. The section below the WT extending to the fracture is marked by a highly altered chemical signal, as indicated by multivariate analysis. Within this interval, Cl is strongly depleted and Na+ shows increased association with SO42− and NO3, while the ionic balance indicates increased acidity relative to the WT onset. Below the fracture, chemical signals are attenuated but largely preserved. Principal Component Analysis coupled to Fuzzy C-Means clustering independently identifies the WT, altered ice interval, the fracture zone and a deep ice anomaly, suggesting variable preservation along the core. We define depth intervals characterized by preserved, amplified, altered and attenuated signals and show that despite significant meltwater influence, post-depositional alterations are locally concentrated rather than affecting the entire record. These results provide a basis for future paleoclimatic investigations using what could be the last Quelccaya Ice Cap ice core before continued melting irreversibly alters the record.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
Share
João Gomes Ilha, Manoela Brum Poitevin Portella, Oscar Vilca Gomez, Filipe Gaudie Lindau, Mariusz Potocki, Elena Barbaro, Susan Kaspari, Carlo Barbante, Jefferson Cardia Simões, and Paul Andrew Mayewski

Status: open (until 04 Nov 2026)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
João Gomes Ilha, Manoela Brum Poitevin Portella, Oscar Vilca Gomez, Filipe Gaudie Lindau, Mariusz Potocki, Elena Barbaro, Susan Kaspari, Carlo Barbante, Jefferson Cardia Simões, and Paul Andrew Mayewski
João Gomes Ilha, Manoela Brum Poitevin Portella, Oscar Vilca Gomez, Filipe Gaudie Lindau, Mariusz Potocki, Elena Barbaro, Susan Kaspari, Carlo Barbante, Jefferson Cardia Simões, and Paul Andrew Mayewski
Metrics will be available soon.
Latest update: 23 Sep 2026
Download
Short summary
Glaciers preserve records of past climate, but melting is rapidly damaging this information. We examined a new ice core from the Quelccaya Ice Cap in Peru by comparing a variety of chemical markers and using statistical tools. We found that melting has altered the archive mainly where water accumulated and near a fracture, rather than throughout the core. Much of the ice still preserves valuable climate information. Our approach can help assess other threatened glacier records around the world.
Share