Stein, Ruediger; Frederichs, Thomas; Fahl, Kirsten; Geibert, Walter; Matthiessen, Jens; Niessen, Frank; Vogt, Christoph; Sassenroth, Cynthia; Bazhenova, Evgenia A: X-Ray Diffraction anaylsis of sediment core PS115/2_2 [dataset]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.975865 (dataset in review), In: Stein, R et al.: A 430 kyrs multi-proxy record of Eurasian Ice Sheet history and organic carbon burial in the eastern Eurasian Basin, Arctic Ocean [dataset bundled publication]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.975790 (dataset in review)
Abstract:
Sediment Core PS115/2-2 was recovered from the Amundsen Basin in 3600 m water depth at the eastern flank of the Gakkel Ridge during Polarstern Expedition PS115/2 in 2018 (Stein, 2019). The well-dated core is used to reconstruct in detail the interrelationship between ice-sheet dynamics and organic carbon burial in the central Eurasian Basin during the last 430 kyr, and to correlate marine and terrestrial records of the Eurasian Ice Sheet (EIS) history. Due to the complex geology of the circum-Arctic Ocean hinterland, specific mineral assemblages determined in sediment cores from the eastern Eurasian Basin may give information about the detrital sediment provenance, transport processes and EIS history (cf., Stein et al., 1994; Vogt, 1997; Wahsner et al., 1999; Stein, 2008). In this context, X-Ray diffraction (XRD) analyses were carried-out using ground bulk sediment. The relative contents of the determined minerals are expressed as ratio of the XRD single mineral peak intensity vs. sum of total analyzed intensities (Vogt, 2009). For details and methods, we refer to Stein et al. (this paper).
References:
Stein, Ruediger (2019): The Expedition PS115/2 of the Research Vessel POLARSTERN to the Arctic Ocean in 2018. Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 728, 249 pp, https://doi.org/10.2312/BzPM_0728_2019
Stein, Ruediger; Fahl, Kirsten (2004): The Laptev Sea: Distribution, Sources, Variability and Burial of Organic Carbon. In: Stein, R & Macdonald, RW (eds.), The Organic Carbon Cycle in the Arctic Ocean. Springer-Verlag, Berlin, 213-237
Stein, Ruediger; Grobe, Hannes; Wahsner, Monika (1994): Organic carbon, carbonate, and clay mineral distributions in eastern central Arctic Ocean surface sediments. Marine Geology, 119(3-4), 269-285, https://doi.org/10.1016/0025-3227(94)90185-6
Vogt, Christoph (1997): Zeitliche und räumliche Verteilung von Mineralvergesellschaftungen in spätquartären Sedimenten des Arktische Ozeans und ihre Nützlichkeit als Klimaindikatoren während der Glazial/Interglazial-Wechsel (Regional and temporal variations of mineral assemblages in Arctic Ocean sediments as climate indicator during glacial/interglacial changes). Berichte zur Polarforschung = Reports on Polar Research, 251, 309 pp, https://doi.org/10.2312/BzP_0251_1997
Vogt, Christoph (2009): Data report: semiquantitative determination of detrital input to ACEX sites based on bulk sample X-ray diffraction data. In: Backman, J., Moran, K., McInroy, D.B., Mayer, L.A., and the Expedition 302 Scientists, Proc. IODP: Edinburgh (Integrated Ocean Drilling Program Management International, Inc.), 302, https://doi.org/10.2204/iodp.proc.302.203.2009
Funding:
German Research Foundation (DFG), grant/award no. 447617953: "Arctic Ocean Paleoceanography (ArcOP)": Pilot research and lead of IODP Expedition 377 (ArcOP-Pilot)
Coverage:
Median Latitude: 81.244115 * Median Longitude: 123.481940 * South-bound Latitude: 81.244100 * West-bound Longitude: 123.479940 * North-bound Latitude: 81.244130 * East-bound Longitude: 123.483940
Date/Time Start: 2018-09-14T14:49:00 * Date/Time End: 2018-09-14T17:41:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 7.64 m
Event(s):
PS115/2_2-1 * Latitude: 81.244130 * Longitude: 123.479940 * Date/Time: 2018-09-14T14:49:00 * Elevation: -3665.0 m * Location: Arctic Ocean * Campaign: PS115/2 * Basis: Polarstern * Method/Device: Giant box corer (GKG)
PS115/2_2-2 * Latitude: 81.244100 * Longitude: 123.483940 * Date/Time: 2018-09-14T17:41:00 * Elevation: -3669.0 m * Location: Arctic Ocean * Campaign: PS115/2 * Basis: Polarstern * Method/Device: Box corer (BC)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Stein, Ruediger | |||
2 | DEPTH, sediment/rock | Depth sed | m | Stein, Ruediger | Geocode | |
3 | AGE | Age | ka BP | Stein, Ruediger | Geocode | |
4 | Peak area, total | Peak area tot | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
5 | Smectite (17-14.5 Å), relative abundance | Sme 17-14.5 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
6 | Illite 10Å, relative abundance | Ill10Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
7 | Illite (5Å), relative abundance | Ill 5Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
8 | Kaolinite (3.58 Å), relative abundance | Kln 3.58 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
9 | Chlorite (3.54 Å), relative abundance | Chl 3.54 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
10 | Quartz (4.26 Å), relative abundance | Qz 4.26Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
11 | Plagioclase (3.15-3.22 Å), relative abundance | Pl 3.15-3.22 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
12 | Kalifeldspar (3.24-3.26 Å ), relative abundance | Kfs 3.24-3.26 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
13 | Quartz/Feldspar ratio | Qz/Fsp | Vogt, Christoph | Calculated | ||
14 | Kalifeldspar/Plagioclase ratio | Kfs/Pl | Vogt, Christoph | Calculated | ||
15 | Calcite (3.03 Å), relative abundance | Cal 3.03 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
16 | Aragonite (3.4 Å), relative abundance | Arg 3.4 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
17 | Aragonite (3.4 Å), relative abundance | Arg 3.4 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
18 | Siderite (2.79 Å), relative abundance | Sd 2.79 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
19 | Calcite/Dolomite ratio | Cal/dol | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
20 | Dolomite/Calcite ratio | Dol/Cal | 10-3 | Vogt, Christoph | Calculated | |
21 | Pyrite (2.71 Å), relative abundance | Py 2.71 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
22 | Amphibole (8.1-8.6 Å), relative abundance | Amp 8.1-8.6 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
23 | Pyroxene (2.99-2.92 Å), relative abundance | Pyrox 2.99-2.92 Å | Vogt, Christoph | X-ray diffraction; bulk sample; peak intensity devided by sum of measured mineral intensities | ||
24 | Pyroxene/Amphibole atio | Pyrox/Amph | Vogt, Christoph | Calculated |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0) (License comes into effect after moratorium ends)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
7994 data points
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