Pore water chemistry of sediment core GeoB13820-1
| Cobertura |
LATITUDE: -39.301000 * LONGITUDE: -53.967167 * DATE/TIME START: 2009-06-01T03:12:00 * DATE/TIME END: 2009-06-01T03:12:00 * MINIMUM DEPTH, sediment/rock: 0.15 m * MAXIMUM DEPTH, sediment/rock: 9.40 m |
|---|---|
| Data(s) |
07/02/2014
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| Formato |
text/tab-separated-values, 190 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.772980 doi:10.1594/PANGAEA.772980 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.773188 Riedinger, Natascha; Formolo, Michael J; Lyons, Timothy W; Henkel, Susann; Beck, A; Kasten, Sabine (2014): An inorganic geochemical argument for coupled anaerobic oxidation of methane and iron reduction in marine sediments. Geobiology, 12(2), 172-181, doi:10.1111/gbi.12077 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #397; Center for Marine Environmental Sciences; DEPTH, sediment/rock; GC; GeoB13820-1; Gravity corer; High Performance Liquid Chromatography (HPLC); Hydrogen sulfide; ICP-MS, Inductively coupled plasma - mass spectrometry; Iron; M78/3A; Manganese; MARUM; Meteor (1986); Nickel; pH; Photospectrometer, methylene blue; Punch-in electrode; Sulfate |
| Tipo |
Dataset |
