Reynolds, Ben C; Sherlock, Sarah C; Kelley, Simon P; Burton, Kevin W (2004): (Table DR1) Argon isotope data and dating for individual >63 µm amphibole grains from Labrador Sea sediments, ODP Hole 105-647A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.713697, Supplement to: Reynolds, BC et al. (2004): Radiogenic isotope records of Quaternary glaciations: Changes in the erosional source and weathering processes. Geology, 32(10), 861-864, https://doi.org/10.1130/G20734.1
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Abstract:
Variations of global and regional silicate weathering rates and paleo-ocean circulation patterns are estimated by using radiogenic isotope records, but the effects of changes in provenance are generally ignored. Here sediment provenance has been constrained through the use of Ar-Ar ages for individual detrital minerals from the Labrador Sea, which can be compared directly to the radiogenic isotope compositions from the same core material. Dramatic changes in the radiogenic isotope composition of North Atlantic Deep Water through the Quaternary Period are shown to reflect discrete changes in both sources and weathering processes accompanying Northern Hemisphere glaciation. Changes in the different radiogenic isotope systems reflect the influence of source, physical weathering, and chemical weathering, and not simply changes in the underlying weathering rate or ocean circulation patterns that are typically inferred.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 53.331300 * Longitude: -45.262000
Date/Time Start: 1985-10-15T04:10:00 * Date/Time End: 1985-10-23T18:15:00
Minimum Elevation: -3869.0 m * Maximum Elevation: -3869.0 m
Event(s):
105-647A * Latitude: 53.331300 * Longitude: -45.262000 * Date/Time Start: 1985-10-15T04:10:00 * Date/Time End: 1985-10-23T18:15:00 * Elevation: -3869.0 m * Penetration: 736 m * Recovery: 444.6 m * Location: South Atlantic Ocean * Campaign: Leg105 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 75 cores; 716.6 m cored; 0 m drilled; 62 % recovery
Comment:
Parameter "Age" shows sediment age.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | AGE | Age | ka BP | Geocode | ||
2 | Sample code/label | Sample label | Reynolds, Ben C | DSDP/ODP/IODP sample designation | ||
3 | Number | No | Reynolds, Ben C | |||
4 | Method comment | Method comm | Reynolds, Ben C | |||
5 | Argon-40 | 40Ar | arbitrary units | Reynolds, Ben C | ||
6 | Argon-40, standard deviation | 40Ar std dev | ± | Reynolds, Ben C | error, +/- | |
7 | Argon-39 | 39Ar | arbitrary units | Reynolds, Ben C | ||
8 | Standard deviation | Std dev | ± | Reynolds, Ben C | Ar39, error, +/- | |
9 | Argon-36/Argon-39 | 36Ar/39Ar | 10-3 | Reynolds, Ben C | Infrared laser ablation microprobe (IRLAMP) | |
10 | Argon-36/Argon-39, standard deviation | 36Ar/39Ar std dev | ± | Reynolds, Ben C | Calculated | |
11 | Argon-37/Argon-39 | 37Ar/39Ar | Reynolds, Ben C | Infrared laser ablation microprobe (IRLAMP) | ||
12 | Argon-37/Argon-39, standard deviation | 37Ar/39Ar std dev | ± | Reynolds, Ben C | Calculated | |
13 | Argon-38/Argon-39 | 38Ar/39Ar | Reynolds, Ben C | Infrared laser ablation microprobe (IRLAMP) | ||
14 | Argon-38/Argon-39, standard deviation | 38Ar/39Ar std dev | ± | Reynolds, Ben C | Calculated | |
15 | Argon-40/Argon-39 | 40Ar/39Ar | Reynolds, Ben C | Infrared laser ablation microprobe (IRLAMP) | ||
16 | Argon-40/Argon-39 | 40Ar/39Ar | Reynolds, Ben C | Infrared laser ablation microprobe (IRLAMP) | 40Ar*/39Ar | |
17 | Argon-40/Argon-39, standard deviation | 40Ar/39Ar std dev | ± | Reynolds, Ben C | Calculated | |
18 | Argon-40/Argon-39, standard deviation | 40Ar/39Ar std dev | ± | Reynolds, Ben C | Calculated | 40Ar*/39Ar |
19 | Age, dated | Age dated | ka | Reynolds, Ben C | Infrared laser ablation microprobe (IRLAMP) | of amphibole grains |
20 | Age, dated standard deviation | Age dated std dev | ± | Reynolds, Ben C | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4595 data points
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