Sulphur isotope analyses in the southern ocean and the central Dronning Maud Land, East Antarctica

Sulphur isotope analyses are an important tool for the study of the natural sulphur cycle. On the northern hemisphere such studies of the atmospheric part of the cycle are practically impossible due to the high emission rate of anthropogenic sulphur. Merely in remote areas of the world such as the A...

Full description

Bibliographic Details
Main Authors: Wand, Ulrich, Maaß, Ingeborg, Haendel, Dietmar
Format: Dataset
Language:English
Published: PANGAEA 1992
Subjects:
Dronning Maud Land
Antarctica
MULT
Multiple investigations
Novolazarevskaya_Station
Rozovoye
Schirmacher_Oasis
Untersee_Oasis
Antarctic
East Antarctica
Gruber Mountains
Southern Ocean
The Antarctic
Antarc*
Polarforschung
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.763872
https://doi.org/10.1594/PANGAEA.763872
Description
Summary:Sulphur isotope analyses are an important tool for the study of the natural sulphur cycle. On the northern hemisphere such studies of the atmospheric part of the cycle are practically impossible due to the high emission rate of anthropogenic sulphur. Merely in remote areas of the world such as the Antarctic 34S analyses can be used to identify the various sulphur sources (sea spray, biogenic und volcanic sources). We report here results of 34S measurements on sulphates from recent atmospheric precipitations (snow), lake waters, and salt efflorescences sampled in the Schirmacher Oasis and the Gruber Mountains, central Dronning Maud Land, East Antarctica. By plotting the delta 34S of precipitation versus % sea-spray sulphate the isotopic composition of the excess sulphate (which is probably of marine-biogenic origin) is extrapolated to be +4 per mil. Lake water sulphate and atmospheric precipitations have a comparable sulphur isotope composition (about +5 per mil). The analyzed secondary sulphates from the salt efflorescences, mainly gypsum and a few water-soluble sulphatcs (hexahydrite, epsomite, burkeite. and pickeringite), vary in their isotopic composition between about -12 and +8 per mil. This wide scatter is probably due to chemical weathering of primary sulphides having different delta 34S values in the substratum.

Similar Items