Be10 and U-series isotopes in manganese from the Central North Pacific

The exponential decreases with depth of 10Be , 230Th and 231Pa in two manganese nodules from the central North Pacific is interpreted in terms of slow growth of the nodules: at average rates of millimeters per million years. It is observed in one specimen (Mn 139): 10Be-based rate 230Th-based rate < 231Pa-based rate. This suggests that diffusion-mixing may have modified the depth gradients of these nuclides, such that the true rate would be close to or even lower than the observed 10Be rate of 1.3 mm/10-6 yr. Quantitative assessment using a diffusion-decay model indicates that in Mn 139, 230Th and 231Pa could have been subjected to diffusion-like transport with an effective diffusion coefficient of about 1 10power8xcm-2/yr. After correction for this effect, the 230Th and 231Pa data give a concordant rate of 1.9 mm/10-6 yr, about 2-3 times lower than their uncorrected values. The small and variable amounts of integrated dpm/cmSUP-2 of 10Be, 230Th excess and 231Pa excess found in nodules are best explained by their incorporating only a fraction of the nuclides supplied due to frequent coverage of sediments. The alternative explanation of young 'exposure' ages is refutable on several grounds. Among these, it is shown that diffusion of nuclides required by the exposure-age concept yields depth profiles that are not of the commonly observed exponential form.

From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.

Supplement to: Ku, Teh-Lung; Omura, Akiko; Chen, P S (1979): Be10 and U-series isotopes in manganese from the Central North Pacific. In: Bischoff, J.L., Piper, D.Z. (Eds.), Marine Geology and Oceanography of the Pacific Manganese Nodule Province. Marine Science, Plenum Publishing Corporation, New York, U.S.A., 791-814

Identifier
DOI https://doi.org/10.1594/PANGAEA.867563
PID https://hdl.handle.net/10013/epic.48867.d002
Related Identifier IsSupplementTo https://doi.org/10.1007/978-1-4684-3518-4_26
Related Identifier References https://hdl.handle.net/10013/epic.48867.d003
Related Identifier IsDerivedFrom https://doi.org/10.7289/V52Z13FT
Related Identifier IsDocumentedBy https://doi.org/10.7289/V53X84KN
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.867563
Provenance
Creator Ku, Teh-Lung; Omura, Akiko; Chen, P S
Publisher PANGAEA
Publication Year 1972
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 2 datasets
Discipline Earth System Research
Spatial Coverage (-136.600W, 20.017S, 173.667E, 20.750N); Pacific Ocean
Temporal Coverage Begin 1971-05-18T00:00:00Z
Temporal Coverage End 1976-11-15T00:00:00Z