Pore water chemistry of gravity core GeoB15101-7
Cobertura |
LATITUDE: 35.231167 * LONGITUDE: 21.471667 * DATE/TIME START: 2011-02-11T15:46:00 * DATE/TIME END: 2011-02-11T15:46:00 * MINIMUM DEPTH, sediment/rock: 15 m * MAXIMUM DEPTH, sediment/rock: 440 m |
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Data(s) |
08/06/2015
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Formato |
text/tab-separated-values, 374 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.846795 doi:10.1594/PANGAEA.846795 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.846796 Goldhammer, Tobias; Schwärzle, Andreas; Aiello, Ivano W; Zabel, Matthias (2015): Temporal stability and origin of chemoclines in the deep hypersaline anoxic Urania basin. Geophysical Research Letters, 42(12), 4888-4895, doi:10.1002/2015GL063758 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Aluminium; Ammonium; Barium; Boron; Bromide; Calcium; Carbon, inorganic, dissolved; Center for Marine Environmental Sciences; Chloride; Conductivity; Conductivity meter; DARCLIFE; Deep subsurface Archaea: carbon cycle, life strategies, and role in sedimentary ecosystems; DEPTH, sediment/rock; Flow injection conductometry; GC; GeoB15101-7; Gravity corer; Hydrogen sulfide anion; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Ion chromatography; Iron; Lithium; M84/1; M84/1_113-1; Magnesium; Manganese; MARUM; Mediterranean Sea, Urania Basin; Meteor (1986); Phosphate; Phosphorus; Potassium; Silicon; Sodium; Spectrophotometry; Strontium; Sulfate; Sulfur |
Tipo |
Dataset |