/* DATA DESCRIPTION: Citation: Haese, Ralf R; Schulz, Horst D (2003): Iron in porewater of sediment core GeoB1413-3. PANGAEA, https://doi.org/10.1594/PANGAEA.104642 Related to: Haese, Ralf R (1997): Beschreibung und Quantifizierung frühdiagenetischer Reaktionen des Eisens in Sedimenten des Südatlantiks. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 99, 118 pp, urn:nbn:de:gbv:46-ep000102231 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 Project(s): Geosciences, University of Bremen (GeoB) (URI: https://www.geo.uni-bremen.de/page.php?langid=EN) South Atlantic in Late Quaternary: Reconstruction of Budget and Currents (SFB261) Coverage: LATITUDE: -15.678333 * LONGITUDE: -9.455000 DATE/TIME START: 1991-04-17T00:00:00 * DATE/TIME END: 1991-04-17T00:00:00 MINIMUM DEPTH, sediment/rock: 0.300 m * MAXIMUM DEPTH, sediment/rock: 6.500 m Event(s): GeoB1413-3 * LATITUDE: -15.678333 * LONGITUDE: -9.455000 * DATE/TIME: 1991-04-17T00:00:00 * ELEVATION: -3787.0 m * Recovery: 6.67 m * LOCATION: West Angola Basin * CAMPAIGN: M16/1 (URI: https://doi.org/10.2312/cr_m16) * BASIS: Meteor (1986) (URI: https://en.wikipedia.org/wiki/RV_Meteor_(1986)) * METHOD/DEVICE: Gravity corer (Kiel type) (SL) * COMMENT: Geochemie; Rohr abgeknickt, Parameter(s): DEPTH, sediment/rock [m] (Depth sed) * GEOCODE Iron [µmol/l] (Fe) * PI: Schulz, Horst D (hdschulz@geochemie.uni-bremen.de) * METHOD/DEVICE: ICP-AES, Inductively coupled plasma - atomic emission spectroscopy License: Creative Commons Attribution 3.0 Unported (CC-BY-3.0) (URI: https://creativecommons.org/licenses/by/3.0/) Size: 19 data points */ Depth sed [m] Fe [µmol/l] 0.300 0.00 0.500 2.51 0.800 0.00 1.200 0.00 1.500 0.00 1.800 0.90 2.200 1.79 2.600 0.18 2.900 0.54 3.200 1.25 3.600 5.37 3.900 0.00 4.200 0.00 4.600 0.00 5.200 0.00 5.500 0.18 5.800 1.79 6.200 0.00 6.500 0.00