Lavelle, Mark (2001): (Table 1) Strontium isotope data for marine carbonates of sediment core CRP-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.184981, Supplement to: Lavelle, M (2001): Strontium isotope stratigraphy for CRP-3, Victoria Land Basin, Antarctica. Terra Antartica, 8(4), 593-598, hdl:10013/epic.28217.d001
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Abstract:
Strontium isotope stratigraphy was used to date 5 discrete horizons within the CRP-3 drillhole. A single in situ modiolid bivalve fragment at 10.88 mbsf gives an age of 30.9 (±0.8) Ma for the associated sediment. The four remaining well preserved fragments recovered from 29.94-190.31 mbsf are within error of this age, indicating a high sedimentation rate and suggesting little time is missing in disconformities. The diagenetic alteration of carbonate macrofossils by continental fluids (and possibly seawater) is a common feature to 320 mbsf.
Project(s):
Cape Roberts Project (CRP)
Coverage:
Latitude: -77.006000 * Longitude: 163.719000
Date/Time Start: 1999-10-09T00:00:00 * Date/Time End: 1999-11-19T00:00:00
Minimum Elevation: -295.0 m * Maximum Elevation: -295.0 m
Event(s):
CRP-3 * Latitude: -77.006000 * Longitude: 163.719000 * Date/Time Start: 1999-10-09T00:00:00 * Date/Time End: 1999-11-19T00:00:00 * Elevation: -295.0 m * Penetration: 939 m * Recovery: 936 m * Location: Ross Sea * Campaign: CRP-3 * Basis: Sampling/drilling from ice * Method/Device: Core wireline system (CWS) * Comment: 11.76 km at 76° true from Cape Roberts, 2.04 km at 225° true from CRP-2. Fast ice thickness: 2.0 to 2.2 m. Sea rise embedded to 9.55 mbsf. Lateral ice movement from spudding 5.0 m to 82° true. HQ core to 345.85 mbsf. NQ core to 939.42 mbsf. Core recovery 97%. Phase 1 logging to 345 mbsf, Phase 2 logging to 773 mbsf, Phase 3 logging to 918 mbsf. Deepest Cenozoic lithology and depth: sandstone breccia from 822.87 to 823.11 mbsf. Age of oldest Cenozoic strata: earliest Oligocene or latest Eocene. Deepest core lithology and depth: light red-brown quartz-cemented quartz sandstone to 939.42 mbsf. Age of bedrock: (mid?) Devonian.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Depth, top/min | Depth top | m | Lavelle, Mark | ||
2 | Depth, bottom/max | Depth bot | m | Lavelle, Mark | ||
3 | Lithologic unit/sequence | Unit | Lavelle, Mark | |||
4 | Sample type | Samp type | Lavelle, Mark | |||
5 | Shell debris | Shells | Lavelle, Mark | Shell type | ||
6 | Preservation | Preserv | Lavelle, Mark | |||
7 | Comment | Comment | Lavelle, Mark | Taphonomy | ||
8 | Strontium-87/Strontium-86 ratio | 87Sr/86Sr | Lavelle, Mark | Isotope ratio mass spectrometry | Normalised to long-term laboratory standard NIST-987 = 0.7210248 | |
9 | Strontium-87/Strontium-86 ratio, error | 87Sr/86Sr e | ± | Lavelle, Mark | 2SE | |
10 | Age, dated | Age dated | ka | Lavelle, Mark | Age, strontium isotope, LOWESS fit Howarth & McArthur (1997) | |
11 | Age, dated, range, minimum | Age dated min | ka | Lavelle, Mark | Age, strontium isotope, LOWESS fit Howarth & McArthur (1997) | |
12 | Age, dated, range, maximum | Age dated max | ka | Lavelle, Mark | Age, strontium isotope, LOWESS fit Howarth & McArthur (1997) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
150 data points
Data
1 Depth top [m] | 2 Depth bot [m] | 3 Unit | 4 Samp type | 5 Shells | 6 Preserv | 7 Comment | 8 87Sr/86Sr | 9 87Sr/86Sr e [±] | 10 Age dated [ka] | 11 Age dated min [ka] | 12 Age dated max [ka] |
---|---|---|---|---|---|---|---|---|---|---|---|
10.88 | 10.89 | 1.1 | Modiolid bivalve | Articulated | Well preserved | In situ | 0.707949 | 0.000020 | 30900 | 30100 | 31700 |
29.94 | 29.96 | 1.2 | Pectinid bivalve | Fragments | Well preserved | Uncertain | 0.707946 | 0.000012 | 31000 | 30200 | 31700 |
47.55 | 47.57 | 1.2 | Pectinid bivalve | Fragments | Well preserved | Uncertain | 0.707949 | 0.000017 | 30900 | 30100 | 31700 |
81.29 | 81.39 | 1.4 | Sandy mudstone | Water | not applicable | not applicable | 0.711362 | 0.000016 | |||
89.02 | 89.03 | 2.1 | Unidentified bivalve | Fragments | Partially recrystallised | Uncertain | 0.707988 | 0.000017 | |||
124.96 | 125.01 | 3.1 | Echinoid plates | Fragments | Partially recrystallised | Uncertain | 0.708048 | 0.000020 | |||
127.48 | 127.50 | 3.1 | Unidentified bivalve | Fragments | Partially recrystallised | Uncertain | 0.708328 | 0.000020 | |||
190.29 | 190.31 | 6.1 | Pectinid bivalve | Fragments | Well preserved | Uncertain | 0.707946 | 0.000018 | 31000 | 30200 | 31700 |
190.29 | 190.31 | 6.1 | Pectinid bivalve | Fragments | Well preserved | Uncertain | 0.707934 | 0.000024 | 31300 | 30500 | 32100 |
190.50 | 190.52 | 6.1 | Unidentified bivalve | Articulated | Partially recrystallised | In situ | 0.708357 | 0.000030 | |||
197.61 | 197.64 | 6.1 | Unidentified bivalve | Fragments | Partially recrystallised | Uncertain | 0.708249 | 0.000021 | |||
198.79 | 198.81 | 6.1 | Unidentified shell | Fragments | Partially recrystallised | Uncertain | 0.708224 | 0.000020 | |||
225.47 | 225.57 | 7.2 | Sandy mudstone | Water | not applicable | not applicable | 0.711073 | 0.000020 | |||
247.27 | 247.31 | 7.2 | Unidentified shell | Fragments | Partially recrystallised | Uncertain | 0.710497 | 0.000021 | |||
320.36 | 320.38 | 8.1 | Unidentified bivalve | Fragments | Partially recrystallised | Uncertain | 0.708072 | 0.000024 |