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Jonkers, Lukas (2024): XRD and planktonic foraminifera abundance and isotope data for core LO09-18 spanning MIS3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.971425

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Abstract:
Multiproxy data from core LO09-18 from the Reykjanes Ridge. Calcite content and quartz/plagioclase measured using XRD. The quartz/plagioclase ratio of North Atlantic sediments reflects the varying contribution of continental derived quartz versus that of basaltic plagioclase and can be used as a proxy for the contribution of ice-rafted detritus. Details about the measurements and interpretation can be found in https://doi.org/10.1016/S0025-3227(02)00592-3 and https://doi.org/10.1016/S0012-821X(03)00675-7.
Stable carbon and oxygen isotope ratios were measured on at least three aliquots of seven shells of N. pachyderma >150 µm using a Finnigan MAT 253 coupled to a Kiel IV device. Reproducibility of an external standard (NBS19) amounted to 0.05 ‰ and 0.03 ‰ (1 s.d.) for δ18O and δ13C, respectively.
Foraminiferal census counts of core LO09-18 were performed on the >150 µm fraction. The assemblage data were used to derive summer sea surface temperatures using weighted averaging partial least squared regression (WA-PLS) (https://doi.org/10.1007/BF00028046) and the training set of https://doi.org/10.1016/j.quascirev.2004.07.014. The modern temperature values for 10 m water depth during summer (July, August, September) for the calibration dataset were taken from the World Ocean Atlas version 2 (WOA, 1998).
Two age models are presented. The first is based on radiocarbon ages of Neogloborquadrina pachyderma. The second is a refinement of this age model and is also based on tuning the IRD (quartz/plagioclase) time series to the oxygen isotope time series of NGRIP.
Keyword(s):
Ice Rafted Debris; Planktonic foraminifera abundances; Stable carbon and oxygen isotopes
Related to:
Jonkers, Lukas; Moros, Matthias; Prins, Maarten Arnoud; Dokken, Trond; Andersson Dahl, Carin; Dijkstra, Noortje; Perner, Kerstin; Brummer, Geert-Jan A (2010): A reconstruction of sea surface warming in the northern North Atlantic during MIS 3 ice-rafting events. Quaternary Science Reviews, 29(15-16), 1791-1800, https://doi.org/10.1016/j.quascirev.2010.03.014
Moros, Matthias; Kuijpers, Antoon; Snowball, Ian; Lassen, Stephan; Bäckström, Denise L; Gingele, Franz; McManus, Jerry F (2002): Were glacial iceberg surges in the North Atlantic triggered by climatic warming? Marine Geology, 192(4), 393-417, https://doi.org/10.1016/S0025-3227(02)00592-3
Moros, Matthias; McManus, Jerry F; Rasmussen, T; Kuijpers, Antoon; Dokken, Trond; Snowball, Ian; Nielsen, Tove; Jansen, Eystein (2004): Quartz content and the quartz-to-plagioclase ratio determined by X-ray diffraction: a proxy for ice rafting in the northern North Atlantic? Earth and Planetary Science Letters, 218(3-4), 389-401, https://doi.org/10.1016/S0012-821X(03)00675-7
Coverage:
Latitude: 58.967333 * Longitude: -30.681667
Date/Time Start: 1993-09-10T00:00:00 * Date/Time End: 1993-09-10T00:00:00
Minimum DEPTH, sediment/rock: 2.995 m * Maximum DEPTH, sediment/rock: 5.545 m
Event(s):
LO09/18-2 * Latitude: 58.967333 * Longitude: -30.681667 * Date/Time: 1993-09-10T00:00:00 * Elevation: -1771.0 m * Recovery: 5.5 m * Campaign: LO09 * Basis: Professor Logachev * Method/Device: Gravity corer (Kiel type) (SL)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmJonkers, LukasGeocode
2AGEAgeka BPJonkers, LukasAge, calculated calendar yearsGeocode
3CalciteCal%Jonkers, LukasX-ray diffraction (XRD)
4Quartz/Plagioclase ratioQz/PlJonkers, LukasX-ray diffraction (XRD)
5Neogloboquadrina pachyderma, δ13CN. pachyderma δ13C‰ PDBJonkers, LukasMass spectrometer, Finnigan, MAT 253; coupled with Carbonate preparation device, Finnigan, KIEL IV
6Neogloboquadrina pachyderma, δ18ON. pachyderma δ18O‰ PDBJonkers, LukasMass spectrometer, Finnigan, MAT 253; coupled with Carbonate preparation device, Finnigan, KIEL IV
7Neogloboquadrina pachydermaN. pachyderma#Jonkers, LukasCounting >150 µm fraction
8Neogloboquadrina incomptaN. incompta#Jonkers, LukasCounting >150 µm fraction
9Globigerina bulloidesG. bulloides#Jonkers, LukasCounting >150 µm fraction
10Globoconella inflataG. inflata#Jonkers, LukasCounting >150 µm fraction
11Globigerinita uvulaG. uvula#Jonkers, LukasCounting >150 µm fraction
12Globigerinita glutinataG. glutinata#Jonkers, LukasCounting >150 µm fraction
13Turborotalita quinqueloba sinistralT. quinqueloba s#Jonkers, LukasCounting >150 µm fraction
14Turborotalita quinqueloba dextralT. quinqueloba d#Jonkers, LukasCounting >150 µm fraction
15Globorotalia scitulaG. scitula#Jonkers, LukasCounting >150 µm fraction
16Foraminifera, planktic indeterminataForam plankt indet#Jonkers, LukasCounting >150 µm fraction
17AgeAgeka b2kJonkers, LukasAge model, ice core correlationNGRIP age (IRD-tuned)
18Sea surface temperature, summerSST sum°CJonkers, LukasCalculated from planktonic foraminifera assemblages using WA-PLS
19Sea surface temperature, summer, standard deviationSST sum std dev±Jonkers, LukasCalculated from planktonic foraminifera assemblages using WA-PLS
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
1137 data points

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