Mineralogy of cold seep sediment inhabited by vesicomyid clams in the Japan Deep Sea Trench

DOI

Sediment sampling was performed at the center of the clam colony. Immediately after sample recovery onboard, the sediment core was sub-sampled and preserved for later analyses. Pyrite and carbonate content of the sediment was measured by X-ray refraction analysis as previously described (Ertefai et al., 2010).

Identifier
DOI https://doi.org/10.1594/PANGAEA.826490
Related Identifier https://doi.org/10.1594/PANGAEA.826602
Related Identifier https://doi.org/10.1111/gbi.12078
Related Identifier https://doi.org/10.1016/j.gca.2010.08.006
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.826490
Provenance
Creator Ertefai, Tobias F; Hinrichs, Kai-Uwe ORCID logo
Publisher PANGAEA
Publication Year 2014
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 54 data points
Discipline Earth System Research
Spatial Coverage (143.893 LON, 39.106 LAT); Sanriku Escarpment in the Japan Trench