Nunes, Flavia; Norris, Richard D (2006): (Table S1) Stable carbon and oxygen isotope ratios of Nuttallides truempyi of the Paleocene/Eocene Thermal Maximum [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.769834, Supplement to: Nunes, F; Norris, RD (2006): Abrupt reversal in ocean overturning during the Palaeocene/Eocene warm period. Nature, 439(7072), 60-63, https://doi.org/10.1038/nature04386
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
An exceptional analogue for the study of the causes and consequences of global warming occurs at the Palaeocene/Eocene Thermal Maximum, 55 million years ago. A rapid rise of global temperatures during this event accompanied turnovers in both marine (Kelly et al., 1998, doi:10.1016/S0031-0182(98)00017-0; Bralower, 2002, doi:10.1029/2001PA000662; Crouch et al., 2001, doi:10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2) and terrestrial biota (Bowen et al., 2002, doi:10.1126/science.1068700), as well as significant changes in ocean chemistry (Dickens et al., 1997, doi:10.1130/0091-7613(1997)025<0259:ABOGIT>2.3.CO;2; Zachos et al., 2005, doi:10.1126/science.1109004) and circulation (Kennett and Stott, 1991, doi:10.1038/353225a0; Pak and Miller, 1992, doi:10.1029/92PA01234). Here we present evidence for an abrupt shift in deep-ocean circulation using carbon isotope records from fourteen sites. These records indicate that deep-ocean circulation patterns changed from Southern Hemisphere overturning to Northern Hemisphere overturning at the start of the Palaeocene/Eocene Thermal Maximum. This shift in the location of deep-water formation persisted for at least 40,000 years, but eventually recovered to original circulation patterns. These results corroborate climate model inferences that a shift in deep-ocean circulation would deliver relatively warmer waters to the deep sea, thus producing further warming (Bice and Marotzke, 2002, doi:10.1029/2001PA000678). Greenhouse conditions can thus initiate abrupt deep-ocean circulation changes in less than a few thousand years, but may have lasting effects; in this case taking 100,000 years to revert to background conditions.
Related to:
Bralower, Timothy J; Zachos, James C; Thomas, Ellen; Parrow, Matthew; Paull, Charles K; Kelly, Daniel Clay; Premoli Silva, Isabella; Sliter, William V; Lohmann, Kyger C (1995): Late Paleocene to Eocene paleoceanography of the equatorial Pacific Ocean: Stable isotopes recorded at Ocean Drilling Program Site 865, Allison Guyot. Paleoceanography, 10(4), 841-865, https://doi.org/10.1029/95PA01143
Katz, Miriam E; Katz, David R; Wright, James D; Miller, Kenneth G; Pak, Dorothy K; Shackleton, Nicholas J; Thomas, Ellen (2003): Early Cenozoic benthic foraminiferal isotopes: Species reliability and interspecies correction factors. Paleoceanography, 18(2), 1024, https://doi.org/10.1029/2002PA000798
Kennett, James P; Stott, Lowell D (1990): Proteus and Proto-Oceanus: ancestral Paleogene oceans as revealed from Antarctic stable isotopic results; ODP Leg 113. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 865-878, https://doi.org/10.2973/odp.proc.sr.113.188.1990
Lu, Gangyi; Keller, Gerta (1993): The Paleocene-Eocene transition in the Antarctic Indian Ocean: Inference from planktic foraminifera. Marine Micropaleontology, 21(1-3), 101-142, https://doi.org/10.1016/0377-8398(93)90012-M
Stott, Lowell D; Sinha, Ashish; Thiry, Medard; Aubry, Marie-Pierre; Berggren, William A (1996): Global d13C changes across the Paleocene-Eocene boundary: criteria for terrestrial-marine correlations. In: Knox, RWO'B; Corfield, RM; Dunay, RE (eds.), Correlation of the Early Paleogene in Northwest Europe, Geological Society Special Publication, 101, 381-399
Thomas, Deborah J; Zachos, James C; Bralower, Timothy J; Thomas, Ellen; Bohaty, Steven M (2002): Warming the fuel for the fire: Evidence for the thermal dissociation of methane hydrate during the Paleocene-Eocene thermal maximum. Geology, 30(12), 1067-1070, https://doi.org/10.1130/0091-7613(2002)030%3C1067:WTFFTF%3E2.0.CO;2
Thomas, Ellen; Shackleton, Nicholas J (1996): The Paleocene-Eocene benthic foraminiferal extinction and stable isotope anomalies. In: Knox, RWO'B; Corfield, RM; Dunay, RE (eds.), Correlation of the Early Paleogene in Northwest Europe, Geological Society Special Publication, 101, 401-441, https://doi.org/10.1144/GSL.SP.1996.101.01.20
Project(s):
Deep Sea Drilling Project (DSDP)
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -3.362029 * Median Longitude: -23.346723 * South-bound Latitude: -65.161000 * West-bound Longitude: -143.694180 * North-bound Latitude: 49.088000 * East-bound Longitude: 93.896200
Date/Time Start: 1972-02-04T00:00:00 * Date/Time End: 2003-02-01T07:50:00
Minimum DEPTH, sediment/rock: 101.97 m * Maximum DEPTH, sediment/rock: 513.80 m
Event(s):
22-213 * Latitude: -10.211800 * Longitude: 93.896200 * Date/Time: 1972-02-04T00:00:00 * Elevation: -5601.0 m * Penetration: 163 m * Recovery: 143.6 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 163 m cored; 0 m drilled; 88.1 % recovery
48-401 * Latitude: 47.427500 * Longitude: -8.810300 * Date/Time: 1976-06-06T00:00:00 * Elevation: -2495.0 m * Penetration: 341 m * Recovery: 103.1 m * Location: North Atlantic/TERRACE * Campaign: Leg48 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 228 m cored; 38 m drilled; 45.2 % recovery
74-525A * Latitude: -29.070700 * Longitude: 2.985300 * Date/Time: 1980-06-10T00:00:00 * Elevation: -2467.0 m * Penetration: 678.1 m * Recovery: 406.6 m * Location: South Atlantic/CREST * Campaign: Leg74 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 62 cores; 549.7 m cored; 6 m drilled; 74 % recovery
Comment:
Sediment depth is given in mbsf. Further relevant datasets see: Pak and Miller (1992) doi:10.1594/PANGAEA.52489. Benthic foraminiferal d13C data for Site 690 published by Thomas and Shackleton (1996) were excluded from this analysis (total = 28 data points, out of 91 published data points). These data were systematically offset towards more positive values (~0.5 per mil to 1 per mil) from the data published by Kennett and Stott 1990, Stott et al., 1990 and Thomas et al, 2002.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Sample code/label | Sample label | Nunes, Flavia | DSDP/ODP/IODP sample designation | ||
3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
4 | AGE | Age | ka BP | Geocode | ||
5 | Nuttallides truempyi, δ13C | N. truempyi δ13C | ‰ PDB | Nunes, Flavia | ||
6 | Nuttallides truempyi, δ18O | N. truempyi δ18O | ‰ PDB | Nunes, Flavia | ||
7 | Reference of data | Ref data | Nunes, Flavia |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1557 data points
Data
1 Event | 2 Sample label | 3 Depth sed [m] | 4 Age [ka BP] | 5 N. truempyi δ13C [‰ PDB] | 6 N. truempyi δ18O [‰ PDB] | 7 Ref data |
---|---|---|---|---|---|---|
22-213 | 22-213-16R-3,13-15 | 145.13 | 54602.2 | 0.863 | -0.005 | this study |
22-213 | 22-213-16R-3,20-22 | 145.20 | 54620.0 | 0.812 | -0.353 | this study |
22-213 | 22-213-16R-3,30-32 | 145.30 | 54645.4 | 0.841 | -0.296 | this study |
22-213 | 22-213-16R-3,40-42 | 145.40 | 54670.8 | 0.843 | -0.269 | this study |
22-213 | 22-213-16R-3,50-52 | 145.50 | 54696.2 | 0.821 | -0.329 | this study |
22-213 | 22-213-16R-3,60-62 | 145.60 | 54721.6 | 0.842 | -0.240 | this study |
22-213 | 22-213-16R-3,70-72 | 145.70 | 54747.0 | 0.694 | -0.372 | this study |
22-213 | 22-213-16R-3,89-91 | 145.89 | 54795.3 | 0.658 | -0.433 | this study |
22-213 | 22-213-16R-3,98-100 | 145.98 | 54818.2 | 0.693 | -0.416 | this study |
22-213 | 22-213-16R-3,119-121 | 146.19 | 54871.5 | 0.605 | -0.356 | this study |
22-213 | 22-213-16R-3,139-141 | 146.39 | 54922.3 | 0.548 | -0.412 | this study |
22-213 | 22-213-16R-4,8-10 | 146.58 | 54970.6 | 0.647 | -0.127 | this study |
22-213 | 22-213-16R-4,18-20 | 146.68 | 54996.0 | 0.601 | -0.390 | this study |
22-213 | 22-213-16R-4,38-40 | 146.88 | 55046.8 | 0.340 | -0.624 | this study |
22-213 | 22-213-16R-4,55-58 | 147.05 | 55090.0 | 0.286 | -0.445 | this study |
22-213 | 22-213-16R-4,59-61 | 147.09 | 55100.2 | 0.445 | -0.411 | this study |
22-213 | 22-213-16R-4,60-63 | 147.10 | 55102.7 | 0.103 | -0.535 | this study |
22-213 | 22-213-16R-4,66-68 | 147.16 | 55118.0 | 0.003 | -0.572 | this study |
22-213 | 22-213-16R-4,69-71 | 147.19 | 55125.6 | 0.216 | -0.463 | this study |
22-213 | 22-213-16R-4,74-77 | 147.24 | 55138.3 | -0.267 | -0.707 | this study |
22-213 | 22-213-16R-4,80-82 | 147.30 | 55153.6 | -0.524 | -0.885 | this study |
22-213 | 22-213-16R-4,81-84 | 147.31 | 55156.1 | -0.551 | -0.891 | this study |
22-213 | 22-213-16R-4,85-88 | 147.35 | 55166.3 | -0.532 | -0.836 | this study |
22-213 | 22-213-16R-4,91-93 | 147.41 | 55181.5 | -0.559 | -1.074 | this study |
22-213 | 22-213-16R-4,91-93 | 147.41 | 55181.5 | -0.443 | -0.867 | this study |
22-213 | 22-213-16R-4,96-98 | 147.46 | 55187.5 | -0.354 | -0.818 | this study |
22-213 | 22-213-16R-4,103-105 | 147.53 | 55195.8 | -0.289 | -0.796 | this study |
22-213 | 22-213-16R-4,107-109 | 147.57 | 55200.6 | -0.343 | -0.761 | this study |
22-213 | 22-213-16R-4,112-114 | 147.62 | 55206.6 | -0.292 | -0.641 | this study |
22-213 | 22-213-16R-4,112-114 | 147.62 | 55206.6 | -0.485 | -0.832 | this study |
22-213 | 22-213-16R-4,114-117 | 147.64 | 55208.9 | -0.383 | -0.818 | this study |
48-401 | 48-401-14R-1,4-6 | 198.54 | 54614.1 | 0.511 | -0.562 | this study |
48-401 | 48-401-14R-1,19-21 | 198.73 | 54645.2 | 0.390 | -0.613 | this study |
48-401 | 48-401-14R-1,30-32 | 198.84 | 54663.3 | 0.483 | -0.609 | this study |
48-401 | 48-401-14R-1,45-47 | 198.99 | 54687.9 | 0.633 | -0.501 | this study |
48-401 | 48-401-14R-1,56-58 | 199.06 | 54699.3 | 0.609 | -0.549 | this study |
48-401 | 48-401-14R-1,81-83 | 199.31 | 54740.3 | 0.708 | -0.480 | this study |
48-401 | 48-401-14R-1,91-93 | 199.41 | 54756.7 | 0.458 | -0.829 | this study |
48-401 | 48-401-14R-1,101-103 | 199.51 | 54773.1 | 0.623 | -0.566 | this study |
48-401 | 48-401-14R-1,110-113 | 199.60 | 54787.9 | 0.599 | -0.417 | this study |
48-401 | 48-401-14R-1,120-122 | 199.70 | 54804.3 | 0.647 | -0.399 | this study |
48-401 | 48-401-14R-1,128-130 | 199.78 | 54817.4 | 0.638 | -0.422 | this study |
48-401 | 48-401-14R-1,138-140 | 199.88 | 54833.8 | 0.703 | -0.307 | this study |
48-401 | 48-401-14R-1,148-150 | 199.98 | 54850.2 | 0.656 | -0.289 | this study |
48-401 | 48-401-14R-2,8-10 | 200.08 | 54866.6 | 0.673 | -0.341 | this study |
48-401 | 48-401-14R-2,21-23 | 200.21 | 54887.9 | 0.424 | -0.548 | this study |
48-401 | 48-401-14R-2,31-33 | 200.31 | 54904.3 | 0.637 | -0.403 | this study |
48-401 | 48-401-14R-2,40-42 | 200.40 | 54919.1 | 0.530 | -0.470 | this study |
48-401 | 48-401-14R-2,50-52 | 200.50 | 54935.5 | 0.567 | -0.477 | this study |
48-401 | 48-401-14R-2,63-65 | 200.63 | 54956.8 | 0.643 | -0.496 | this study |
48-401 | 48-401-14R-2,72-74 | 200.72 | 54971.6 | 0.709 | -0.339 | this study |
48-401 | 48-401-14R-2,83-85 | 200.83 | 54989.6 | 0.574 | -0.971 | this study |
48-401 | 48-401-14R-2,91-93 | 200.91 | 55002.7 | 0.666 | -0.358 | this study |
48-401 | 48-401-14R-2,100-102 | 201.00 | 55017.5 | 0.639 | -0.449 | this study |
48-401 | 48-401-14R-2,110-112 | 201.10 | 55033.9 | 0.846 | this study | |
48-401 | 48-401-14R-2,120-122 | 201.20 | 55050.3 | 0.453 | -0.312 | this study |
48-401 | 48-401-14R-2,129-131 | 201.29 | 55065.1 | 0.371 | -0.455 | this study |
48-401 | 48-401-14R-2,140-142 | 201.40 | 55083.1 | 0.213 | -0.491 | this study |
48-401 | 48-401-14R-2,148-150 | 201.48 | 55096.2 | 0.502 | -0.441 | this study |
48-401 | 48-401-14R-3,6-8 | 201.56 | 55109.3 | 0.084 | -0.800 | this study |
48-401 | 48-401-14R-3,11-13 | 201.61 | 55117.5 | 0.155 | -0.337 | this study |
48-401 | 48-401-14R-3,16-18 | 201.66 | 55125.7 | 0.134 | -0.492 | this study |
48-401 | 48-401-14R-3,21-23 | 201.71 | 55133.9 | 0.060 | -0.464 | this study |
48-401 | 48-401-14R-3,26-27 | 201.76 | 55142.1 | -0.218 | -0.730 | this study |
48-401 | 48-401-14R-3,31-33 | 201.81 | 55150.3 | -0.209 | -0.867 | this study |
48-401 | 48-401-14R-3,37-39 | 201.87 | 55160.2 | -0.339 | -1.055 | this study |
48-401 | 48-401-14R-3,42-44 | 201.92 | 55168.4 | -0.165 | -0.867 | this study |
48-401 | 48-401-14R-3,47-49 | 201.97 | 55176.6 | -0.254 | -0.735 | this study |
48-401 | 48-401-14R-3,52-54 | 202.02 | 55182.8 | -0.730 | -1.262 | this study |
48-401 | 48-401-14R-3,58-60 | 202.08 | 55186.7 | -0.355 | -0.934 | this study |
48-401 | 48-401-14R-3,63-65 | 202.13 | 55190.0 | -0.564 | -1.094 | this study |
48-401 | 48-401-14R-3,68-70 | 202.18 | 55193.3 | -0.276 | -0.844 | this study |
48-401 | 48-401-14R-3,84-86 | 202.34 | 55203.8 | -0.292 | -0.894 | this study |
48-401 | 48-401-14R-3,90-92 | 202.40 | 55207.8 | -0.364 | -0.981 | this study |
48-401 | 48-401-14R-3,108-110 | 202.58 | 55219.6 | 0.716 | -0.293 | this study |
48-401 | 48-401-14R-3,112-114 | 202.62 | 55222.2 | 0.881 | -0.110 | this study |
48-401 | 48-401-14R-3,122-123 | 202.72 | 55228.8 | 1.008 | -0.100 | this study |
48-401 | 48-401-14R-3,127-128 | 202.77 | 55232.0 | 1.088 | -0.134 | this study |
48-401 | 48-401-14R-3,133-134 | 202.83 | 55236.0 | 0.896 | -0.343 | this study |
48-401 | 48-401-14R-3,138-140 | 202.88 | 55239.2 | 0.966 | -0.252 | this study |
48-401 | 48-401-14R-3,143-145 | 202.93 | 55242.5 | 0.904 | -0.139 | this study |
48-401 | 48-401-14R-3,148-150 | 202.98 | 55245.8 | 1.073 | -0.123 | this study |
80-549 | 80-549-16R-5,8-10 | 337.26 | 54877.8 | 0.410 | -0.551 | this study |
80-549 | 80-549-16R-5,19-20 | 337.37 | 54910.9 | 0.330 | -0.493 | this study |
80-549 | 80-549-16R-5,28-30 | 337.46 | 54938.0 | 0.379 | -0.489 | this study |
80-549 | 80-549-16R-5,39-41 | 337.57 | 54971.0 | 0.254 | -0.612 | this study |
80-549 | 80-549-16R-5,49-51 | 337.67 | 55001.1 | 0.254 | -0.621 | this study |
80-549 | 80-549-16R-5,61-63 | 337.78 | 55034.2 | -0.159 | -0.841 | this study |
80-549 | 80-549-16R-5,71-73 | 337.88 | 55064.2 | -0.433 | -0.958 | this study |
80-549 | 80-549-16R-5,80-82 | 337.97 | 55091.3 | -0.602 | -0.956 | this study |
80-549 | 80-549-16R-5,90-92 | 338.07 | 55121.4 | -0.727 | -0.952 | this study |
80-549 | 80-549-16R-5,100-102 | 338.17 | 55151.4 | -1.090 | -1.515 | this study |
80-549 | 80-549-16R-5,110-112 | 338.27 | 55181.5 | -1.537 | -1.726 | this study |
80-549 | 80-549-16R-5,110-112 | 338.27 | 55181.5 | -1.338 | -1.521 | this study |
80-549 | 80-549-16R-5,120-122 | 338.37 | 55186.1 | -1.405 | -1.752 | this study |
80-549 | 80-549-16R-5,120-122 | 338.37 | 55186.1 | -1.488 | -1.759 | this study |
80-549 | 80-549-16R-6,71.5-74 | 339.40 | 55233.8 | 0.599 | -0.722 | this study |
80-549 | 80-549-16R-6,80-82 | 339.48 | 55237.7 | 1.153 | -0.521 | this study |
80-549 | 80-549-16R-6,90-92 | 339.58 | 55242.4 | 0.809 | -0.603 | this study |
80-549 | 80-549-16R-6,98-100 | 339.66 | 55246.1 | 1.327 | -0.211 | this study |
80-549 | 80-549-16R-6,108-110 | 339.76 | 55250.7 | 1.157 | -0.351 | this study |
80-549 | 80-549-16R-6,118-120 | 339.86 | 55255.4 | 1.061 | -0.303 | this study |
199-1220B | 199-1220B-20X-1,15-17 | 197.55 | 54500.0 | 0.674 | -0.415 | this study |
199-1220B | 199-1220B-20X-1,20-22 | 197.60 | 54520.0 | 0.712 | -0.459 | this study |
199-1220B | 199-1220B-20X-1,30-32 | 197.70 | 54560.1 | 0.573 | -0.495 | this study |
199-1220B | 199-1220B-20X-1,35-37 | 197.75 | 54580.2 | 0.624 | -0.582 | this study |
199-1220B | 199-1220B-20X-1,40-42 | 197.80 | 54600.2 | 0.641 | -0.493 | this study |
199-1220B | 199-1220B-20X-1,45-47 | 197.85 | 54620.3 | 0.568 | -0.624 | this study |
199-1220B | 199-1220B-20X-1,50-52 | 197.90 | 54640.3 | 0.733 | -0.481 | this study |
199-1220B | 199-1220B-20X-1,55-57 | 197.95 | 54660.3 | 0.688 | -0.504 | this study |
199-1220B | 199-1220B-20X-1,60-62 | 198.00 | 54680.4 | 0.766 | -0.490 | this study |
199-1220B | 199-1220B-20X-1,65-67 | 198.05 | 54700.4 | 0.723 | -0.520 | this study |
199-1220B | 199-1220B-20X-1,70-72 | 198.10 | 54720.5 | 0.702 | -0.528 | this study |
199-1220B | 199-1220B-20X-1,75-77 | 198.15 | 54740.5 | 0.755 | -0.387 | this study |
199-1220B | 199-1220B-20X-1,80-82 | 198.20 | 54760.6 | 0.662 | -0.448 | this study |
199-1220B | 199-1220B-20X-1,85-87 | 198.25 | 54780.6 | 0.677 | -0.452 | this study |
199-1220B | 199-1220B-20X-1,90-92 | 198.30 | 54800.7 | 0.604 | -0.577 | this study |
199-1220B | 199-1220B-20X-1,95-97 | 198.35 | 54820.7 | 0.638 | -0.482 | this study |
199-1220B | 199-1220B-20X-1,100-102 | 198.40 | 54840.7 | 0.714 | -0.422 | this study |
199-1220B | 199-1220B-20X-1,105-107 | 198.45 | 54860.8 | 0.707 | -0.402 | this study |
199-1220B | 199-1220B-20X-1,110-112 | 198.50 | 54880.8 | 0.695 | -0.467 | this study |
199-1220B | 199-1220B-20X-1,115-117 | 198.55 | 54900.9 | 0.748 | -0.254 | this study |
199-1220B | 199-1220B-20X-1,120-122 | 198.60 | 54920.9 | 0.653 | -0.475 | this study |
199-1220B | 199-1220B-20X-1,125-127 | 198.65 | 54941.0 | 0.711 | -0.303 | this study |
199-1220B | 199-1220B-20X-1,130-132 | 198.70 | 54961.0 | 0.683 | -0.281 | this study |
199-1220B | 199-1220B-20X-1,135-137 | 198.75 | 54981.1 | 0.563 | -0.312 | this study |
199-1220B | 199-1220B-20X-1,140-142 | 198.80 | 55001.1 | 0.624 | -0.331 | this study |
199-1220B | 199-1220B-20X-1,145-147 | 198.85 | 55021.1 | 0.447 | -0.307 | this study |
199-1220B | 199-1220B-20X-1,146-148 | 198.86 | 55025.2 | 0.501 | -0.395 | this study |
199-1220B | 199-1220B-20X-2,5-7 | 198.95 | 55061.2 | 0.372 | -0.354 | this study |
199-1220B | 199-1220B-20X-2,10-12 | 199.00 | 55081.3 | 0.123 | -0.603 | this study |
199-1220B | 199-1220B-20X-2,15-17 | 199.05 | 55101.3 | -0.270 | -0.662 | this study |
199-1220B | 199-1220B-20X-2,20-22 | 199.10 | 55121.4 | 0.242 | -0.587 | this study |
199-1220B | 199-1220B-20X-2,25-27 | 199.15 | 55141.4 | -0.647 | -0.991 | this study |
199-1220B | 199-1220B-20X-2,30-32 | 199.20 | 55161.5 | -0.575 | -1.016 | this study |
199-1220B | 199-1220B-20X-2,35-37 | 199.25 | 55181.5 | -0.697 | -1.028 | this study |
199-1220B | 199-1220B-20X-2,40-42 | 199.30 | 55186.3 | -0.572 | -0.977 | this study |
199-1220B | 199-1220B-20X-2,45-47 | 199.35 | 55191.0 | -1.421 | -1.035 | this study |
199-1220B | 199-1220B-20X-2,80-82 | 199.70 | 55224.5 | 0.641 | -0.377 | this study |
199-1220B | 199-1220B-20X-2,85-87 | 199.75 | 55229.2 | 0.510 | -0.341 | this study |
199-1220B | 199-1220B-20X-2,90-92 | 199.80 | 55234.0 | 0.791 | -0.315 | this study |
199-1220B | 199-1220B-20X-CC,0-2 | 199.85 | 55238.8 | 0.623 | -0.277 | this study |
199-1220B | 199-1220B-20X-CC,8-10 | 199.93 | 55246.4 | 0.808 | -0.185 | this study |
199-1221C | 199-1221C-11X-2,3-5 | 151.93 | 54491.1 | 0.813 | -0.140 | this study |
199-1221C | 199-1221C-11X-2,23-25 | 152.13 | 54560.5 | 0.833 | -0.047 | this study |
199-1221C | 199-1221C-11X-2,43-45 | 152.33 | 54629.9 | 0.709 | -0.188 | this study |
199-1221C | 199-1221C-11X-2,53-55 | 152.43 | 54664.6 | 0.525 | -0.297 | this study |
199-1221C | 199-1221C-11X-2,62-64 | 152.52 | 54695.8 | 0.711 | -0.290 | this study |
199-1221C | 199-1221C-11X-2,73-75 | 152.63 | 54734.0 | 0.892 | -0.236 | this study |
199-1221C | 199-1221C-11X-2,83-85 | 152.72 | 54765.2 | 0.788 | -0.365 | this study |
199-1221C | 199-1221C-11X-2,93-95 | 152.83 | 54803.4 | 0.777 | -0.378 | this study |
199-1221C | 199-1221C-11X-2,103-105 | 152.93 | 54838.0 | 0.981 | -0.279 | this study |
199-1221C | 199-1221C-11X-2,113-115 | 153.03 | 54872.7 | 0.874 | -0.271 | this study |
199-1221C | 199-1221C-11X-2,124-126 | 153.14 | 54910.9 | 0.783 | -0.389 | this study |
199-1221C | 199-1221C-11X-2,133-135 | 153.23 | 54942.1 | 0.745 | -0.301 | this study |
199-1221C | 199-1221C-11X-2,144-146 | 153.34 | 54980.3 | 0.776 | -0.191 | this study |
199-1221C | 199-1221C-11X-3,4-6 | 153.44 | 55015.0 | 0.860 | -0.083 | this study |
199-1221C | 199-1221C-11X-3,5-8 | 153.45 | 55018.4 | 1.306 | 0.068 | this study |
199-1221C | 199-1221C-11X-3,9-12 | 153.49 | 55032.3 | 1.180 | 0.082 | this study |
199-1221C | 199-1221C-11X-3,10-13 | 153.50 | 55035.8 | 0.758 | 0.257 | this study |
199-1221C | 199-1221C-11X-3,15-18 | 153.55 | 55053.1 | 0.676 | 0.237 | this study |
199-1221C | 199-1221C-11X-3,15-17 | 153.55 | 55053.1 | 0.670 | -0.235 | this study |
199-1221C | 199-1221C-11X-3,16-19 | 153.56 | 55056.6 | 1.421 | 0.121 | this study |
199-1221C | 199-1221C-11X-3,24-26 | 153.64 | 55084.4 | 0.619 | -0.359 | this study |
199-1221C | 199-1221C-11X-3,25-28 | 153.65 | 55087.8 | 0.694 | 0.190 | this study |
199-1221C | 199-1221C-11X-3,30-33 | 153.70 | 55105.2 | 0.742 | 0.199 | this study |
199-1221C | 199-1221C-11X-3,34-36 | 153.74 | 55119.1 | 0.609 | -0.196 | this study |
199-1221C | 199-1221C-11X-3,35-38 | 153.75 | 55122.5 | 0.599 | 0.178 | this study |
199-1221C | 199-1221C-11X-3,44-46 | 153.84 | 55153.7 | 0.436 | -0.331 | this study |
199-1221C | 199-1221C-11X-3,45-48 | 153.85 | 55157.2 | 0.275 | 0.317 | this study |
199-1221C | 199-1221C-11X-3,52-54 | 153.92 | 55181.5 | 0.074 | 0.397 | this study |
199-1221C | 199-1221C-11X-3,54-56 | 153.94 | 55184.3 | 0.182 | 0.524 | this study |
199-1221C | 199-1221C-11X-3,56-58 | 153.96 | 55187.0 | 0.301 | 0.719 | this study |
199-1221C | 199-1221C-11X-3,58-60 | 153.98 | 55189.8 | 0.466 | 0.880 | this study |
199-1221C | 199-1221C-11X-3,60-62 | 154.00 | 55192.6 | 0.137 | 0.504 | this study |
199-1221C | 199-1221C-11X-3,62-64 | 154.02 | 55195.3 | 0.242 | 0.481 | this study |
199-1221C | 199-1221C-11X-3,70-72 | 154.10 | 55206.4 | 0.584 | 0.108 | this study |
199-1221C | 199-1221C-11X-3,88-90 | 154.28 | 55231.2 | 1.063 | 0.064 | this study |
199-1221C | 199-1221C-11X-3,90-92 | 154.30 | 55234.0 | 1.049 | 0.028 | this study |
199-1221C | 199-1221C-11X-3,92-94 | 154.32 | 55236.8 | 1.000 | 0.152 | this study |
199-1221C | 199-1221C-11X-3,94-96 | 154.34 | 55239.5 | 0.982 | 0.127 | this study |
199-1221C | 199-1221C-11X-3,96-98 | 154.36 | 55242.3 | 0.976 | 0.041 | this study |
199-1221C | 199-1221C-11X-3,98-100 | 154.38 | 55245.1 | 0.887 | 0.020 | this study |
199-1221C | 199-1221C-11X-3,105-108 | 154.45 | 55254.7 | 1.070 | 0.088 | this study |
199-1221C | 199-1221C-11X-3,115-118 | 154.55 | 55268.5 | 1.193 | 0.020 | this study |
199-1221C | 199-1221C-11X-3,120-123 | 154.60 | 55275.4 | 1.196 | 0.055 | this study |
199-1221C | 199-1221C-11X-3,125-128 | 154.65 | 55282.4 | 1.272 | 0.032 | this study |
199-1221C | 199-1221C-11X-3,130-133 | 154.70 | 55289.3 | 1.198 | 0.012 | this study |
199-1221C | 199-1221C-11X-3,135-138 | 154.75 | 55296.2 | 1.284 | 0.040 | this study |
199-1221C | 199-1221C-11X-3,140-142 | 154.80 | 55303.1 | 1.119 | 0.005 | this study |
207-1258C | 207-1258C-8R-4,0-1 | 191.70 | 54847.8 | -0.351 | -3.194 | this study |
207-1258C | 207-1258C-8R-4,0-1 | 191.70 | 54847.8 | 0.056 | -0.862 | this study |
207-1258C | 207-1258C-8R-4,10-11 | 191.80 | 54856.8 | -0.177 | -0.974 | this study |
207-1258C | 207-1258C-8R-4,20-21 | 191.90 | 54865.8 | -0.670 | -3.185 | this study |
207-1258C | 207-1258C-8R-4,30-31 | 192.00 | 54874.8 | -0.267 | -3.196 | this study |
207-1258C | 207-1258C-8R-4,40-41 | 192.10 | 54883.8 | -0.458 | -3.020 | this study |
207-1258C | 207-1258C-8R-4,50-51 | 192.20 | 54892.9 | -0.476 | -3.216 | this study |
207-1258C | 207-1258C-8R-4,75-76 | 192.45 | 54915.4 | 0.131 | -0.668 | this study |
207-1258C | 207-1258C-8R-4,80-81 | 192.50 | 54919.9 | -0.034 | -0.894 | this study |
207-1258C | 207-1258C-8R-4,85-86 | 192.55 | 54924.4 | -0.205 | -0.910 | this study |
207-1258C | 207-1258C-8R-4,140-141 | 193.10 | 54974.0 | -0.130 | -0.936 | this study |
207-1258C | 207-1258C-8R-4,145-146 | 193.15 | 54978.5 | -0.136 | -0.984 | this study |
207-1258C | 207-1258C-8R-4,149-150 | 193.19 | 54982.2 | -0.248 | -1.123 | this study |
207-1258C | 207-1258C-8R-5,0-1 | 193.20 | 54983.1 | -0.258 | -1.021 | this study |
207-1258C | 207-1258C-8R-5,20-21 | 193.40 | 55001.1 | -0.319 | -0.934 | this study |
207-1258C | 207-1258C-8R-5,70-71 | 193.90 | 55046.2 | -0.701 | -1.241 | this study |
207-1258C | 207-1258C-8R-5,90-91 | 194.10 | 55064.2 | -0.710 | -1.202 | this study |
207-1258C | 207-1258C-8R-5,100-101 | 194.20 | 55073.3 | -0.633 | -1.178 | this study |
207-1258C | 207-1258C-8R-5,110-111 | 194.30 | 55082.3 | -0.498 | -0.980 | this study |
207-1258C | 207-1258C-8R-5,149-150 | 194.69 | 55117.5 | -1.404 | -1.512 | this study |
207-1258C | 207-1258C-8R-6,0-1 | 194.70 | 55118.4 | -1.215 | -1.320 | this study |
207-1258C | 207-1258C-8R-6,10-11 | 194.80 | 55127.4 | -1.452 | -1.598 | this study |
207-1258C | 207-1258C-8R-6,20-21 | 194.90 | 55136.4 | -1.522 | -1.640 | this study |
207-1258C | 207-1258C-8R-6,30-31 | 195.00 | 55145.4 | -1.419 | -1.579 | this study |
207-1258C | 207-1258C-8R-6,40-41 | 195.10 | 55154.4 | -1.451 | -1.739 | this study |
207-1258C | 207-1258C-8R-6,50-51 | 195.20 | 55163.5 | -1.609 | -1.645 | this study |
207-1258C | 207-1258C-8R-6,55-56 | 195.25 | 55168.0 | -1.880 | -2.053 | this study |
207-1258C | 207-1258C-8R-6,60-61 | 195.30 | 55172.5 | -2.006 | -2.216 | this study |
207-1258C | 207-1258C-8R-6,65-66 | 195.35 | 55177.0 | -2.060 | -2.160 | this study |
207-1258C | 207-1258C-8R-6,70-71 | 195.40 | 55181.5 | -2.057 | -2.140 | this study |
207-1258C | 207-1258C-8R-6,106-108 | 195.76 | 55228.7 | 0.354 | -0.764 | this study |
207-1258C | 207-1258C-8R-6,110-111 | 195.80 | 55234.0 | 0.543 | -0.730 | this study |
207-1258C | 207-1258C-8R-6,130-131 | 196.00 | 55260.2 | 0.590 | -0.739 | this study |
207-1258C | 207-1258C-8R-6,148-149 | 196.18 | 55283.9 | 0.517 | -1.048 | this study |
74-525A | 74-525A-32R-4,75-77 | 388.86 | 54381.0 | 0.520 | -0.740 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-4,125-127 | 389.36 | 54493.7 | 1.190 | -0.370 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-5,25-27 | 389.86 | 54606.5 | 1.070 | -0.340 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-5,48-50 | 390.08 | 54656.1 | 0.980 | -0.280 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-5,77-79 | 390.38 | 54723.7 | 1.090 | -0.370 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-5,115-117 | 390.76 | 54809.4 | 1.150 | -0.030 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-6,25-27 | 391.36 | 54944.7 | 0.960 | -0.250 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-6,50-52 | 391.61 | 55001.1 | 0.880 | -0.520 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-6,76-78 | 391.87 | 55059.7 | 1.100 | -0.300 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-6,90-92 | 392.01 | 55091.3 | 1.090 | -0.290 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-6,113-115 | 392.24 | 55143.2 | -1.090 | -1.060 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-6,130-132 | 392.41 | 55181.5 | -1.470 | -1.500 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-6,145-147 | 392.56 | 55201.2 | -0.030 | -0.930 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-7,22-24 | 392.81 | 55234.0 | 1.270 | 0.030 | Thomas and Shackleton, 1996 |
74-525A | 74-525A-32R-7,53-55 | 393.11 | 55273.4 | 1.530 | -0.320 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-1,62-64 | 199.63 | 54954.5 | 0.820 | -0.140 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-1,85-89 | 199.86 | 55001.1 | 0.760 | -0.110 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-1,102-104 | 200.03 | 55035.6 | 0.650 | -0.320 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-1,136-138 | 200.37 | 55104.5 | 0.290 | -0.450 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-2,5-7 | 200.56 | 55143.0 | -0.180 | -0.670 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-2,20-22 | 200.71 | 55173.4 | -0.980 | -1.350 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-2,38-40 | 200.89 | 55191.3 | -0.920 | -1.350 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-2,56-58 | 201.07 | 55203.9 | 1.120 | -0.320 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-2,68-70 | 201.19 | 55212.3 | 1.000 | -0.740 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-2,80-82 | 201.31 | 55220.7 | 1.230 | -0.320 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-2,88-90 | 201.39 | 55226.3 | 1.400 | -0.220 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-2,115-117 | 201.66 | 55245.2 | 1.420 | -0.030 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-3,28-30 | 202.29 | 55289.3 | 1.300 | -0.070 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-3,48-50 | 202.49 | 55303.3 | 1.150 | -0.370 | Thomas and Shackleton, 1996 |
74-527 | 74-527-24R-3,75-77 | 202.76 | 55322.2 | 1.250 | -0.160 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-18H-4,110-114 | 162.80 | 54724.1 | 1.050 | -0.050 | Kennett and Stott, 1990 |
113-690B | 113-690B-18H-5,36-40 | 163.56 | 54772.4 | 0.920 | -0.390 | Kennett and Stott, 1990 |
113-690B | 113-690B-18H-5,110-114 | 164.30 | 54819.4 | 0.900 | -0.390 | Kennett and Stott, 1990 |
113-690B | 113-690B-18H-6,36-40 | 165.06 | 54867.6 | 1.040 | -0.220 | Kennett and Stott, 1990 |
113-690B | 113-690B-18H-6,110-114 | 165.80 | 54914.7 | 0.970 | -0.140 | Kennett and Stott, 1990 |
113-690B | 113-690B-19H-1,15-19 | 167.05 | 54994.1 | 0.561 | -0.200 | Stott et al., 1996 |
113-690B | 113-690B-19H-1,27-30 | 167.17 | 55001.7 | 0.626 | -0.112 | Stott et al., 1996 |
113-690B | 113-690B-19H-1,45-49 | 167.35 | 55013.1 | 0.470 | -0.316 | Stott et al., 1996 |
113-690B | 113-690B-19H-1,55-59 | 167.45 | 55019.5 | 0.533 | -0.161 | Stott et al., 1996 |
113-690B | 113-690B-19H-1,64-68 | 167.54 | 55025.2 | 0.551 | -0.235 | Stott et al., 1996 |
113-690B | 113-690B-19H-1,73-77 | 167.63 | 55031.0 | 0.409 | -0.308 | Stott et al., 1996 |
113-690B | 113-690B-19H-1,86-88 | 167.76 | 55039.3 | 0.411 | -0.304 | Stott et al., 1996 |
113-690B | 113-690B-19H-1,109-112 | 167.99 | 55053.7 | 0.330 | -0.360 | Kennett and Stott, 1990 |
113-690B | 113-690B-19H-1,135-139 | 168.25 | 55069.9 | 0.518 | 0.026 | Stott et al., 1996 |
113-690B | 113-690B-19H-1,147-150 | 168.37 | 55077.8 | 0.246 | -0.414 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,6-9 | 168.46 | 55083.8 | 0.318 | -0.315 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,15-19 | 168.55 | 55089.6 | 0.337 | -0.124 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,45-49 | 168.85 | 55108.6 | 0.114 | -0.464 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,58-62 | 168.98 | 55116.9 | 0.100 | -0.370 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,73-77 | 169.13 | 55126.5 | -0.052 | Stott et al., 1996 | |
113-690B | 113-690B-19H-2,86-89 | 169.26 | 55134.7 | -0.198 | 0.582 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,94-99 | 169.34 | 55139.8 | 0.052 | -0.439 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,109-112 | 169.49 | 55149.4 | -0.470 | -0.830 | Kennett and Stott, 1990 |
113-690B | 113-690B-19H-2,125-129 | 169.65 | 55162.6 | -0.853 | -0.989 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,137-141 | 169.77 | 55172.0 | -0.902 | -1.063 | Stott et al., 1996 |
113-690B | 113-690B-19H-2,145-149 | 169.85 | 55176.0 | -0.999 | -1.161 | Stott et al., 1996 |
113-690B | 113-690B-19H-3,4-5 | 169.94 | 55180.5 | -1.163 | -1.316 | Stott et al., 1996 |
113-690B | 113-690B-19H-3,15-18 | 170.05 | 55186.0 | -1.150 | -1.399 | Stott et al., 1996 |
113-690B | 113-690B-19H-3,72-76 | 170.62 | 55228.3 | 1.565 | 0.151 | Stott et al., 1996 |
113-690B | 113-690B-19H-3,73-74 | 170.64 | 55230.0 | 1.800 | 0.290 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,74-75 | 170.65 | 55230.8 | 1.610 | 0.010 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,75-76 | 170.65 | 55230.8 | 1.650 | 0.080 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,76-77 | 170.67 | 55232.4 | 0.800 | -0.810 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,76-77 | 170.67 | 55232.4 | 0.600 | -0.830 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,77-78 | 170.68 | 55233.2 | 1.580 | 0.090 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,78-80 | 170.69 | 55234.0 | 1.300 | 0.070 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,80-81 | 170.71 | 55237.8 | 1.450 | 0.040 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,81-82 | 170.72 | 55239.7 | 1.590 | 0.210 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,82-83 | 170.73 | 55241.6 | 1.540 | 0.000 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,83-84 | 170.74 | 55243.5 | 1.620 | 0.100 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,84-85 | 170.75 | 55245.5 | 1.640 | 0.010 | Thomas et al., 2002 |
113-690B | 113-690B-19H-3,86-90 | 170.76 | 55247.4 | 1.558 | 0.270 | Stott et al., 1996 |
113-690B | 113-690B-19H-3,94-97 | 170.84 | 55257.2 | 1.453 | 0.078 | Stott et al., 1996 |
113-690B | 113-690B-19H-3,109-112 | 170.99 | 55265.5 | 0.930 | -0.130 | Kennett and Stott, 1990 |
113-690B | 113-690B-19H-3,127-130 | 171.17 | 55275.4 | 1.230 | 0.262 | Stott et al., 1996 |
113-690B | 113-690B-19H-4,5-9 | 171.45 | 55288.9 | 1.134 | -0.378 | Stott et al., 1996 |
113-690B | 113-690B-19H-4,15-19 | 171.55 | 55293.7 | 0.803 | 0.043 | Stott et al., 1996 |
113-690B | 113-690B-19H-4,26-28 | 171.66 | 55298.6 | 1.580 | 0.206 | Stott et al., 1996 |
113-690B | 113-690B-19H-4,45-49 | 171.85 | 55306.5 | 1.621 | 0.073 | Stott et al., 1996 |
113-690B | 113-690B-19H-4,65-68 | 172.05 | 55314.7 | 1.573 | 0.066 | Stott et al., 1996 |
113-690B | 113-690B-19H-4,109-112 | 172.49 | 55331.7 | 1.200 | -0.100 | Kennett and Stott, 1990 |
113-690B | 113-690B-19H-5,5-9 | 172.95 | 55370.5 | 1.439 | -0.026 | Stott et al., 1996 |
113-690B | 113-690B-19H-5,15-19 | 173.05 | 55382.2 | 1.724 | 0.188 | Stott et al., 1996 |
113-690B | 113-690B-19H-5,44-47 | 173.34 | 55416.0 | 1.717 | 0.338 | Stott et al., 1996 |
113-690B | 113-690B-19H-5,56-59 | 173.46 | 55430.0 | 1.599 | 0.226 | Stott et al., 1996 |
113-690B | 113-690B-19H-5,64-68 | 173.54 | 55439.3 | 1.260 | -0.034 | Stott et al., 1996 |
113-690B | 113-690B-19H-5,73-77 | 173.63 | 55449.8 | 1.424 | 0.105 | Stott et al., 1996 |
113-690B | 113-690B-19H-5,86-89 | 173.76 | 55465.0 | 1.611 | 0.086 | Stott et al., 1996 |
113-690B | 113-690B-19H-5,94-96 | 173.84 | 55474.3 | 1.529 | 0.018 | Stott et al., 1996 |
113-690B | 113-690B-19H-5,109-112 | 173.99 | 55491.8 | 1.370 | -0.220 | Kennett and Stott, 1990 |
113-690B | 113-690B-20H-1,36-38 | 174.56 | 55558.3 | 1.330 | -0.350 | Kennett and Stott, 1990 |
113-690B | 113-690B-20H-1,110-112 | 175.30 | 55644.7 | 1.680 | -0.070 | Kennett and Stott, 1990 |
113-690B | 113-690B-20H-2,36-38 | 176.06 | 55733.3 | 1.530 | -0.280 | Kennett and Stott, 1990 |
113-690B | 113-690B-20H-2,110-112 | 179.80 | 56169.7 | 1.920 | -0.010 | Kennett and Stott, 1990 |
113-690B | 113-690B-18H-3,40-42 | 160.61 | 54584.9 | 1.070 | -0.350 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-18H-4,40-42 | 162.12 | 54680.9 | 1.820 | -0.040 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-18H-5,40-42 | 163.61 | 54775.5 | 1.260 | -0.380 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-18H-6,40-42 | 165.11 | 54870.8 | 1.360 | 0.080 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-18H-CC,CC | 166.65 | 54968.7 | 1.450 | 0.150 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-1,40-42 | 167.31 | 55010.6 | 1.170 | -0.340 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-1,74-76 | 167.65 | 55032.2 | 1.580 | -0.780 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-1, 114-120 | 168.07 | 55058.6 | 1.670 | -0.250 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-2,40-42 | 168.81 | 55106.1 | 0.770 | -0.710 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-2,74-76 | 169.16 | 55128.4 | 0.540 | -0.530 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-2,118-124 | 169.58 | 55156.7 | -0.030 | -0.770 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-3,40-42 | 170.31 | 55203.3 | -0.700 | -1.390 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-3,74-76 | 170.65 | 55230.8 | 1.850 | 0.060 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-3,115-121 | 171.05 | 55268.8 | 1.250 | 0.020 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-4,42-44 | 171.85 | 55306.5 | 1.470 | 0.080 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-4,74-76 | 172.16 | 55319.1 | 1.510 | 0.040 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-5,40-42 | 173.31 | 55412.5 | 1.610 | -0.080 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-5,74-76 | 173.69 | 55456.8 | 1.510 | 0.060 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-19H-CC,19H,CC | 174.30 | 55528.0 | 2.950 | -0.240 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-20H-1,40-42 | 174.71 | 55575.8 | 1.890 | -0.160 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-20H-2,40-42 | 176.21 | 55750.8 | 2.840 | -0.140 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-20H-3,40-42 | 177.71 | 55925.8 | 2.180 | 0.110 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-20H-4,41-43 | 179.22 | 56102.0 | 2.430 | 0.460 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-20H-CC,CC | 180.28 | 56225.7 | 1.890 | 0.070 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-21H-1,40-42 | 180.71 | 56275.8 | 2.330 | 0.090 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-21H-2,40-42 | 182.21 | 56450.8 | 1.870 | 0.070 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-21H-3,40-42 | 183.71 | 56625.8 | 2.080 | 0.010 | Thomas and Shackleton, 1996 |
113-690B | 113-690B-21H-4,5-7 | 184.86 | 56760.0 | 1.950 | -0.090 | Thomas and Shackleton, 1996 |
119-738C | 119-738C-11R-1,108-110 | 284.49 | 55001.1 | 1.170 | -0.270 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-1,115-118 | 284.52 | 55009.8 | 0.400 | -0.120 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,2-4 | 284.93 | 55129.1 | -1.270 | -1.170 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,9-11 | 285.00 | 55149.5 | -1.250 | -1.340 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,20-22 | 285.11 | 55181.5 | -1.810 | -1.760 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,44-46 | 285.35 | 55213.8 | 0.320 | -0.460 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,52-54 | 285.43 | 55224.6 | -0.210 | -0.580 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,59-61 | 285.50 | 55234.0 | 0.980 | 0.000 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,61-63 | 285.52 | 55236.7 | 0.840 | -0.170 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,74-76 | 285.65 | 55254.2 | 0.870 | -0.220 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-2,143-145 | 286.34 | 55347.1 | 1.160 | -0.220 | Lu and Keller, 1993 |
119-738C | 119-738C-11R-3,15-17 | 286.56 | 55376.7 | 1.020 | -0.220 | Lu and Keller, 1993 |
119-738C | 119-738C-12H-3,67 | 101.97 | 55001.1 | 1.090 | -0.180 | Bralower et al., 1995 |
119-738C | 119-738C-12H-3,123 | 102.53 | 55181.5 | 0.390 | -0.130 | Bralower et al., 1995 |
119-738C | 119-738C-12H-5,40 | 104.70 | 55423.9 | 0.930 | -0.360 | Bralower et al., 1995 |
119-738C | 107.70 | 55759.0 | 1.340 | 0.260 | Bralower et al., 1995 | |
171-1051B | 171-1051B-59X-3,87 | 510.17 | 54927.8 | 0.830 | -0.050 | Katz et al., 2003 |
171-1051B | 171-1051B-59X-3,120 | 510.50 | 54966.2 | 0.900 | -0.270 | Katz et al., 2003 |
171-1051B | 171-1051B-59X-3,150 | 510.80 | 55001.1 | 0.820 | -0.210 | Katz et al., 2003 |
171-1051B | 171-1051B-59X-CC,43 | 511.00 | 55024.4 | 0.400 | -0.590 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-1,65 | 511.55 | 55088.4 | 1.320 | 0.220 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-1,78 | 511.68 | 55103.5 | 0.220 | -0.570 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-1,105 | 511.95 | 55134.9 | -0.010 | -0.460 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-1,125 | 512.15 | 55158.2 | -0.300 | -0.570 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-1,145 | 512.35 | 55181.5 | -0.670 | -1.230 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,0 | 512.40 | 55192.0 | 0.060 | 0.240 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,20 | 512.60 | 55234.0 | 1.280 | 0.050 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,28 | 512.68 | 55250.8 | 1.040 | -0.170 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,42 | 512.82 | 55280.2 | 1.160 | -0.040 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,50 | 512.90 | 55297.0 | 1.290 | 0.140 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,56 | 512.96 | 55309.6 | 1.180 | 0.060 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,56 | 512.96 | 55309.6 | 1.100 | -0.110 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,56 | 512.96 | 55309.6 | 1.180 | 0.060 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,56 | 512.96 | 55309.6 | 1.100 | -0.110 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,63 | 513.03 | 55324.3 | 1.120 | 0.030 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,73 | 513.13 | 55345.3 | 1.340 | 0.160 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,80 | 513.20 | 55360.0 | 1.150 | 0.170 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,83 | 513.23 | 55366.3 | 1.100 | 0.140 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,93 | 513.33 | 55387.3 | 1.270 | 0.130 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,103 | 513.43 | 55408.3 | 1.160 | -0.040 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,110 | 513.50 | 55423.0 | 1.320 | 0.220 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,113 | 513.53 | 55429.3 | 1.320 | 0.140 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,120 | 513.60 | 55444.0 | 1.590 | 0.080 | Katz et al., 2003 |
171-1051B | 171-1051B-60X-2,140 | 513.80 | 55486.0 | 1.440 | 0.360 | Katz et al., 2003 |