Peti, Leonie; Nilsson, Andreas; Muscheler, Raimund; Fitzsimmons, Kathryn E; Fink, David; Fujioka, Toshiyuki; Mifsud, Charles; Hopkins, Jenni L; Christl, Marcus; Augustinus, Paul C (2020): Beryllium-10 in sediment cores OB16A and OB16B from Orakei maar, Auckland, New Zealand [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.920773
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
10Be (atoms/g) and native 9Be (atoms/g) concentrations from sediment of Orakei maar, Auckland, New Zealand, measured at the Centre of Accelerator Science (Australian Nuclear Science and Technology Organisation), Sydney (Australia). 10Be (atoms/g) concentrations from sediment measured at the Laboratory of Ion Beam Physics, ETH Zurich (Switzerland).
Supplement to:
Peti, Leonie; Fitzsimmons, Kathryn E; Hopkins, Jenni L; Nilsson, Andreas; Fujioka, Toshiyuki; Fink, David; Mifsud, Charles; Christl, Marcus; Muscheler, Raimund; Augustinus, Paul C (2020): Development of a multi-method chronology spanning the Last Glacial Interval from Orakei maar lake, Auckland, New Zealand. Geochronology (GChron), 2, 367-410, https://doi.org/10.5194/gchron-2-367-2020
Related to:
Peti, Leonie; Nilsson, Andreas; Muscheler, Raimund; Fitzsimmons, Kathryn E; Fink, David; Fujioka, Toshiyuki; Mifsud, Charles; Hopkins, Jenni L; Christl, Marcus; Augustinus, Paul C (2020): Basaltic tephra composition in sediment cores OB16A and OB16B from Orakei maar, Auckland, New Zealand [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.921122
Peti, Leonie; Nilsson, Andreas; Muscheler, Raimund; Fitzsimmons, Kathryn E; Fink, David; Fujioka, Toshiyuki; Mifsud, Charles; Hopkins, Jenni L; Christl, Marcus; Augustinus, Paul C (2020): Paleomagnetic data from sediment cores OB16A and OB16B from Orakei maar, Auckland, New Zealand [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.921134
Peti, Leonie; Nilsson, Andreas; Muscheler, Raimund; Fitzsimmons, Kathryn E; Fink, David; Fujioka, Toshiyuki; Mifsud, Charles; Hopkins, Jenni L; Christl, Marcus; Augustinus, Paul C (2020): Rhyolitic tephra composition in sediment cores OB16A and OB16B from Orakei maar, Auckland, New Zealand [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.921121
Coverage:
Median Latitude: -36.866500 * Median Longitude: 174.812795 * South-bound Latitude: -36.866530 * West-bound Longitude: 174.812730 * North-bound Latitude: -36.866470 * East-bound Longitude: 174.812860
Minimum DEPTH, sediment/rock: 41.06 m * Maximum DEPTH, sediment/rock: 79.10 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Peti, Leonie | Geocode | |
2 | Beryllium-9 | 9Be | atoms/g | Peti, Leonie | Accelerator mass spectrometry (AMS) | |
3 | Beryllium-9, error | 9Be e | ± | Peti, Leonie | Accelerator mass spectrometry (AMS) | |
4 | Beryllium-10 | 10Be | atoms/g | Peti, Leonie | Accelerator mass spectrometry (AMS) | |
5 | Beryllium-10, error | 10Be e | ± | Peti, Leonie | Accelerator mass spectrometry (AMS) | |
6 | Beryllium-10/Beryllium-9 ratio | 10Be/9Be | Peti, Leonie | Accelerator mass spectrometry (AMS) | ||
7 | Beryllium-10/Beryllium-9, error | 10Be/9Be e | ± | Peti, Leonie | Accelerator mass spectrometry (AMS) | |
8 | Laboratory | Lab | Peti, Leonie |
License:
Creative Commons Attribution-NonCommercial 4.0 International (CC-BY-NC-4.0)
Size:
450 data points
Data
1 Depth sed [m] | 2 9Be [atoms/g] | 3 9Be e [±] | 4 10Be [atoms/g] | 5 10Be e [±] | 6 10Be/9Be | 7 10Be/9Be e [±] | 8 Lab |
---|---|---|---|---|---|---|---|
41.06 | 7.55E8 | 1.58E7 | Lund | ||||
41.09 | 6.50E16 | 6.50E15 | 6.30E8 | 1.60E7 | 9.80E-9 | 1.00E-9 | ANSTO |
41.36 | 8.10E16 | 8.10E15 | 7.80E8 | 1.50E7 | 9.70E-9 | 9.90E-10 | ANSTO |
41.73 | 7.80E16 | 7.90E15 | 7.60E8 | 1.80E7 | 9.60E-9 | 1.00E-9 | ANSTO |
41.83 | 8.27E8 | 2.55E7 | Lund | ||||
42.32 | 6.90E16 | 7.00E15 | 8.20E8 | 1.60E7 | 1.20E-8 | 1.20E-9 | ANSTO |
42.52 | 9.34E8 | 1.91E7 | Lund | ||||
42.91 | 6.94E8 | 1.73E7 | Lund | ||||
42.92 | 6.00E16 | 6.10E15 | 6.50E8 | 1.20E7 | 1.10E-8 | 1.10E-9 | ANSTO |
43.28 | 7.49E8 | 2.87E7 | Lund | ||||
43.32 | 5.60E16 | 5.60E15 | 6.30E8 | 1.50E7 | 1.10E-8 | 1.20E-9 | ANSTO |
43.71 | 7.20E16 | 7.20E15 | 7.00E8 | 1.60E7 | 9.70E-9 | 1.00E-9 | ANSTO |
44.11 | 6.60E16 | 6.60E15 | 6.20E8 | 1.20E7 | 9.50E-9 | 9.70E-10 | ANSTO |
44.31 | 7.70E16 | 7.80E15 | 8.60E8 | 1.70E7 | 1.10E-8 | 1.10E-9 | ANSTO |
44.36 | 4.40E8 | 1.57E7 | Lund | ||||
44.86 | 6.40E16 | 6.50E15 | 6.30E8 | 1.20E7 | 9.80E-9 | 1.00E-9 | ANSTO |
45.03 | 6.48E8 | 1.65E7 | Lund | ||||
45.36 | 5.10E17 | 5.30E16 | 6.70E8 | 1.30E7 | 1.30E-9 | 1.40E-10 | ANSTO |
45.36 | 6.78E8 | 4.16E7 | Lund | ||||
46.45 | 2.00E17 | 2.20E16 | 6.50E8 | 1.30E7 | 3.30E-9 | 3.60E-10 | ANSTO |
46.46 | 9.46E8 | 2.14E7 | Lund | ||||
47.53 | 1.50E17 | 1.50E16 | 5.40E8 | 1.10E7 | 3.70E-9 | 4.00E-10 | ANSTO |
47.54 | 1.35E9 | 3.18E7 | Lund | ||||
48.44 | 6.30E16 | 6.30E15 | 6.30E8 | 1.40E7 | 1.00E-8 | 1.00E-9 | ANSTO |
49.26 | 1.20E17 | 1.30E16 | 5.90E8 | 1.20E7 | 4.90E-9 | 5.30E-10 | ANSTO |
50.26 | 3.10E16 | 3.10E15 | 2.30E8 | 5.90E6 | 7.60E-9 | 7.80E-10 | ANSTO |
51.18 | 6.70E16 | 2.00E16 | 2.10E8 | 4.30E6 | 3.20E-9 | 9.70E-10 | ANSTO |
51.75 | 3.00E16 | 3.10E15 | 2.40E8 | 4.50E6 | 7.80E-9 | 8.20E-10 | ANSTO |
51.91 | 3.40E16 | 3.40E15 | 2.50E8 | 4.80E6 | 7.30E-9 | 7.50E-10 | ANSTO |
52.39 | 8.40E16 | 2.50E16 | 2.50E8 | 4.90E6 | 2.90E-9 | 8.90E-10 | ANSTO |
52.96 | 3.10E16 | 3.10E15 | 2.30E8 | 5.40E6 | 7.50E-9 | 7.70E-10 | ANSTO |
53.60 | 6.00E16 | 1.80E16 | 2.80E8 | 5.50E6 | 4.60E-9 | 1.40E-9 | ANSTO |
53.65 | 3.20E16 | 3.30E15 | 3.00E8 | 7.10E6 | 9.20E-9 | 9.50E-10 | ANSTO |
54.03 | 5.90E16 | 1.80E16 | 2.40E8 | 6.10E6 | 4.00E-9 | 1.20E-9 | ANSTO |
54.29 | 6.00E16 | 6.00E15 | 3.00E8 | 5.70E6 | 5.00E-9 | 5.10E-10 | ANSTO |
55.57 | 6.70E16 | 2.00E16 | 5.80E8 | 1.20E7 | 8.60E-9 | 2.60E-9 | ANSTO |
55.57 | 5.50E16 | 5.60E15 | 6.60E8 | 1.30E7 | 1.20E-8 | 1.20E-9 | ANSTO |
56.47 | 9.30E16 | 9.90E15 | 5.70E8 | 1.50E7 | 6.20E-9 | 6.70E-10 | ANSTO |
57.11 | 4.20E16 | 4.20E15 | 4.90E8 | 2.00E7 | 1.20E-8 | 1.30E-9 | ANSTO |
57.64 | 8.70E16 | 9.40E15 | 5.30E8 | 1.00E7 | 6.00E-9 | 6.60E-10 | ANSTO |
58.59 | 6.60E16 | 2.00E16 | 3.70E8 | 7.40E6 | 5.70E-9 | 1.70E-9 | ANSTO |
59.86 | 6.20E16 | 1.90E16 | 4.30E8 | 8.60E6 | 7.00E-9 | 2.10E-9 | ANSTO |
60.66 | 6.30E16 | 1.90E16 | 4.60E8 | 9.20E6 | 7.30E-9 | 2.20E-9 | ANSTO |
62.46 | 5.20E16 | 1.60E16 | 2.90E8 | 7.20E6 | 5.60E-9 | 1.70E-9 | ANSTO |
63.26 | 4.20E16 | 1.30E16 | 2.90E8 | 7.50E6 | 6.90E-9 | 2.10E-9 | ANSTO |
64.47 | 3.20E16 | 3.20E15 | 1.60E8 | 3.00E6 | 4.90E-9 | 5.00E-10 | ANSTO |
65.45 | 3.10E16 | 3.10E15 | 1.30E8 | 2.50E6 | 4.20E-9 | 4.30E-10 | ANSTO |
65.45 | 3.80E16 | 1.20E16 | 1.40E8 | 2.70E6 | 3.60E-9 | 1.10E-9 | ANSTO |
66.20 | 5.70E16 | 1.70E16 | 2.30E8 | 5.60E6 | 4.00E-9 | 1.20E-9 | ANSTO |
67.00 | 3.90E16 | 1.20E16 | 1.60E8 | 3.10E6 | 4.00E-9 | 1.20E-9 | ANSTO |
68.55 | 3.60E16 | 1.10E16 | 1.60E8 | 5.00E6 | 4.30E-9 | 1.30E-9 | ANSTO |
69.78 | 3.40E16 | 1.00E16 | 1.80E8 | 3.60E6 | 5.20E-9 | 1.60E-9 | ANSTO |
70.56 | 4.90E16 | 1.50E16 | 2.30E8 | 4.90E6 | 4.60E-9 | 1.40E-9 | ANSTO |
71.42 | 2.90E16 | 8.80E15 | 1.20E8 | 2.50E6 | 4.20E-9 | 1.30E-9 | ANSTO |
71.84 | 2.70E16 | 2.80E15 | 1.30E8 | 2.40E6 | 4.60E-9 | 4.70E-10 | ANSTO |
72.63 | 2.50E16 | 7.60E15 | 1.60E8 | 4.40E6 | 6.30E-9 | 1.90E-9 | ANSTO |
73.25 | 3.00E16 | 9.30E15 | 1.90E8 | 3.80E6 | 6.10E-9 | 1.90E-9 | ANSTO |
73.62 | 4.70E16 | 4.70E15 | 2.60E8 | 4.90E6 | 5.40E-9 | 5.50E-10 | ANSTO |
74.11 | 2.80E16 | 8.80E15 | 1.60E8 | 3.80E6 | 5.80E-9 | 1.80E-9 | ANSTO |
74.62 | 6.00E16 | 6.00E15 | 2.90E8 | 5.50E6 | 4.80E-9 | 4.90E-10 | ANSTO |
74.88 | 3.20E16 | 9.70E15 | 2.10E8 | 4.20E6 | 6.60E-9 | 2.00E-9 | ANSTO |
75.33 | 2.50E16 | 2.50E15 | 1.40E8 | 2.80E6 | 5.70E-9 | 5.80E-10 | ANSTO |
75.85 | 2.60E16 | 7.90E15 | 1.70E8 | 3.80E6 | 6.30E-9 | 1.90E-9 | ANSTO |
76.21 | 1.90E16 | 1.90E15 | 7.10E7 | 1.40E6 | 3.70E-9 | 3.80E-10 | ANSTO |
76.47 | 2.00E16 | 5.90E15 | 8.20E7 | 1.90E6 | 4.20E-9 | 1.30E-9 | ANSTO |
76.98 | 1.20E16 | 3.70E15 | 2.40E7 | 5.90E5 | 1.90E-9 | 5.70E-10 | ANSTO |
77.41 | 1.70E16 | 5.10E15 | 1.20E8 | 2.40E6 | 6.70E-9 | 2.00E-9 | ANSTO |
78.06 | 2.00E16 | 2.00E15 | 2.20E7 | 5.60E5 | 1.10E-9 | 1.20E-10 | ANSTO |
78.16 | 2.50E16 | 2.50E15 | 2.80E7 | 6.70E5 | 1.10E-9 | 1.20E-10 | ANSTO |
79.10 | 2.10E16 | 2.10E15 | 1.10E7 | 2.90E5 | 5.50E-10 | 5.70E-11 | ANSTO |