posted on 2023-05-21, 10:35authored byMoser, DE, Jackson, S, Kjaer, HA, Markle, B, Ngoumtsa, E, Joel PedroJoel Pedro, Segato, D, Spolaor, A, Tetzner, D, Vallelonga, P, Thomas, ER
The climate of the sub-Antarctic is important in understanding the environmental conditions of Antarctica and the Southern Ocean. However, regional climate proxy records from this region are scarce. In this study, we present the stable water isotopes, major ion chemistry, and dust records from the first ice core from the (sub-)Antarctic Young Island. We present and discuss various dating approaches based on commonly used ice core proxies, such as stable water isotopes and seasonally deposited ions, together with site-specific characteristics such as melt layers. The dating approaches are compared with estimated precipitation rates from reanalysis data (ERA5) and volcanic cryptotephra shards likely presenting an absolute tie point from a 2001 CE eruption on neighboring Sturge Island. The resulting ice core age scale spans the period 2016 to 1995, with an uncertainty of ±2 years.
History
Publication title
Geosciences
Volume
11
Issue
9
Article number
368
Number
368
Pagination
1-18
ISSN
2076-3263
Department/School
Institute for Marine and Antarctic Studies
Publisher
MDPIAG
Place of publication
Switzerland
Rights statement
Copyright 2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https:// creativecommons.org/licenses/by/4.0/).
Repository Status
Open
Socio-economic Objectives
Effects of climate change on Antarctic and sub-Antarctic environments (excl. social impacts)