(Figure 3 and S1): Stable isotopes (δ18O and δ34S) in porewater sulfate in sediment cores from station AC in Van Keulenfjorden, Svalbard

• DEPTH
• Fjord
• Sediment corer
• Svalbard
• biogeochemistry
• glacier
• iron reactivity
• sediment
• sediment rock
• sulfate
• sulfide oxidation
• δ18O
• δ34S

Identifier
DOI	https://doi.org/10.1594/PANGAEA.906827
Related Identifier	IsPartOf https://doi.org/10.1594/PANGAEA.906889
Related Identifier	References https://doi.org/10.1016/j.gca.2019.12.033
Metadata Access	https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.906827

Provenance
Creator	Michaud, Alexander B ; Laufer, Katja; Findlay, Alyssa ; Pellerin, Andre; Antler, Gilad ; Turchyn, Alexandra V ; Røy, Hans ; Wehrmann, Laura Mariana ; Jørgensen, Bo Barker
Publisher	PANGAEA
Publication Year	2019
Rights	Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess	true

Representation
Resource Type	Dataset
Format	text/tab-separated-values
Size	48 data points
Discipline	Biogeochemistry; Biospheric Sciences; Geosciences; Natural Sciences
Spatial Coverage	(15.657 LON, 77.538 LAT); Van Keulenfjorden, Svalbard