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Kasten, Sabine (2004): Ammonium in porewater of sediment core GeoB4419-5. PANGAEA, https://doi.org/10.1594/PANGAEA.222557

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Related to:
Haese, Ralf R; Petermann, Harald; Dittert, Lars; Schulz, Horst D (1998): The early diagenesis of iron in pelagic sediments: a multidisciplinary approach. Earth and Planetary Science Letters, 157(3-4), 233-248, https://doi.org/10.1016/S0012-821X(98)00042-9
Hensen, Christian (1996): Frühdiagenetische Prozesse und Quantifizierung benthischer Stoff-Flüsse in Oberflächensedimenten des Südatlantiks. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 88, 132 pp, urn:nbn:de:gbv:46-ep000102178
Kasten, Sabine (1996): Early diagenetic metal enrichments in marine sediments as documents of nonsteady-state depositional conditions. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 82, 118 pp, urn:nbn:de:gbv:46-ep000102114
Kasten, Sabine; Freudenthal, Tim; Gingele, Franz; Schulz, Horst D (1998): Simultaneous formation of iron-rich layers at different redox boundaries in sediments of the Amazon deep-sea fan. Geochimica et Cosmochimica Acta, 62, 2253-2264, https://doi.org/10.1016/S0016-7037(98)00093-3
Coverage:
Latitude: 9.678333 * Longitude: -54.258333
Date/Time Start: 1997-03-30T14:41:00 * Date/Time End: 1997-03-30T14:41:00
Minimum DEPTH, sediment/rock: 0.0000 m * Maximum DEPTH, sediment/rock: 0.1750 m
Event(s):
GeoB4419-5 * Latitude: 9.678333 * Longitude: -54.258333 * Date/Time: 1997-03-30T14:41:00 * Elevation: -4515.0 m * Recovery: 0.34 m * Location: Guayana continental slope * Campaign: M38/2 * Basis: Meteor (1986) * Method/Device: MultiCorer (MUC) * Comment: 8/4; 20 m pinger, 50 m CTD
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Ammonium[NH4]+µmol/lKasten, SabineContinuous Flow Analysis (CFA)
Size:
13 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth sed [m]

[NH4]+ [µmol/l]
0.00000.0
0.00250.0
0.00750.0
0.01250.0
0.01750.0
0.02250.0
0.02750.0
0.03500.0
0.04500.0
0.06250.0
0.08750.0
0.12500.0
0.17500.0