High-resolution dysprosium data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula ...

• Main Authors: Hoffmann-Abdi, Kirstin, Meyer, Hanno, Fernandoy, Francisco, Freitag, Johannes, Shaw, Fyntan M, Werner, Martin, Thomas, Elizabeth R, McConnell, Joseph R, Schneider, Christoph
• Format: Dataset
• Language: English
• Published: PANGAEA 2023
• Subjects: Antarctic Peninsula; Firn chemistry; firn core; glacio-chemistry; proxies; Rare earth elements; Sample ID; DEPTH, ice/snow; AGE; Age; Dysprosium; Ice drill; High resolution inductively coupled plasma mass spectrometer HR-ICP-MS, ThermoFischer Scientific, Element 2; coupled with Continuous Flow Analysis system CFA; ANT-Land_2016_AntarcticPeninsula; AWI Antarctic Land Expedition; Antarc*; Antarctic; Ice cap; ice core
• Online Access: https://dx.doi.org/10.1594/pangaea.961113; https://doi.pangaea.de/10.1594/PANGAEA.961113

Firn core OH-12 was retrieved from Plateau Laclavere, a small ice cap on the northernmost end of the Antarctic Peninsula. It was drilled in January 2016 to a depth of 19.93 m at about 1090 m a.s.l. using a portable solar-powered and electrically operated ice-core drill (Backpack Drill; icedrill.ch AG). Glacio-chemical parameters in OH-12 (calcium, chlorine, strontium, dysprosium, cerium, lanthanum) were determined at the Trace Chemistry Laboratory of the Desert Research Institute (DRI) in Reno, Nevada, USA, in summer 2017 using two Thermo Finnigan Element2 High Resolution-Inductively Coupled Plasma-Mass Spectrometry (HR-ICP-MS) instruments connected to a Continuous Flow Analysis (CFA) system as described by Röthlisberger et al. (2000) and McConnell et al. (2002). The core was dated using annual layer counting of hydrogen peroxide measurements. We additionally accounted for precipitation intermittency at the drill site by using precipitation data from the European Centre for Medium-Range Weather Forecasts ...