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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

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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
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):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Sample code/labelSample labelNunes, FlaviaDSDP/ODP/IODP sample designation
DEPTH, sediment/rockDepth sedmGeocode
AGEAgeka BPGeocode
Nuttallides truempyi, δ13CN. truempyi δ13C‰ PDBNunes, Flavia
Nuttallides truempyi, δ18ON. truempyi δ18O‰ PDBNunes, Flavia
Reference of dataRef dataNunes, Flavia
Size:
1557 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Sample label

Depth sed [m]

Age [ka BP]

N. truempyi δ13C [‰ PDB]

N. truempyi δ18O [‰ PDB]

Ref data
22-213 22-213-16R-3,13-15145.1354602.20.863-0.005this study
22-21322-213-16R-3,20-22145.2054620.00.812-0.353this study
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48-40148-401-14R-3,42-44201.9255168.4-0.165-0.867this study
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48-40148-401-14R-3,58-60202.0855186.7-0.355-0.934this study
48-40148-401-14R-3,63-65202.1355190.0-0.564-1.094this study
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48-40148-401-14R-3,133-134202.8355236.00.896-0.343this study
48-40148-401-14R-3,138-140202.8855239.20.966-0.252this study
48-40148-401-14R-3,143-145202.9355242.50.904-0.139this study
48-40148-401-14R-3,148-150202.9855245.81.073-0.123this study
80-549 80-549-16R-5,8-10337.2654877.80.410-0.551this study
80-54980-549-16R-5,19-20337.3754910.90.330-0.493this study
80-54980-549-16R-5,28-30337.4654938.00.379-0.489this study
80-54980-549-16R-5,39-41337.5754971.00.254-0.612this study
80-54980-549-16R-5,49-51337.6755001.10.254-0.621this study
80-54980-549-16R-5,61-63337.7855034.2-0.159-0.841this study
80-54980-549-16R-5,71-73337.8855064.2-0.433-0.958this study
80-54980-549-16R-5,80-82337.9755091.3-0.602-0.956this study
80-54980-549-16R-5,90-92338.0755121.4-0.727-0.952this study
80-54980-549-16R-5,100-102338.1755151.4-1.090-1.515this study
80-54980-549-16R-5,110-112338.2755181.5-1.537-1.726this study
80-54980-549-16R-5,110-112338.2755181.5-1.338-1.521this study
80-54980-549-16R-5,120-122338.3755186.1-1.405-1.752this study
80-54980-549-16R-5,120-122338.3755186.1-1.488-1.759this study
80-54980-549-16R-6,71.5-74339.4055233.80.599-0.722this study
80-54980-549-16R-6,80-82339.4855237.71.153-0.521this study
80-54980-549-16R-6,90-92339.5855242.40.809-0.603this study
80-54980-549-16R-6,98-100339.6655246.11.327-0.211this study
80-54980-549-16R-6,108-110339.7655250.71.157-0.351this study
80-54980-549-16R-6,118-120339.8655255.41.061-0.303this study
199-1220B 199-1220B-20X-1,15-17197.5554500.00.674-0.415this study
199-1220B199-1220B-20X-1,20-22197.6054520.00.712-0.459this study
199-1220B199-1220B-20X-1,30-32197.7054560.10.573-0.495this study
199-1220B199-1220B-20X-1,35-37197.7554580.20.624-0.582this study
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199-1220B199-1220B-20X-1,45-47197.8554620.30.568-0.624this study
199-1220B199-1220B-20X-1,50-52197.9054640.30.733-0.481this study
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199-1220B199-1220B-20X-1,60-62198.0054680.40.766-0.490this study
199-1220B199-1220B-20X-1,65-67198.0554700.40.723-0.520this study
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199-1220B199-1220B-20X-1,75-77198.1554740.50.755-0.387this study
199-1220B199-1220B-20X-1,80-82198.2054760.60.662-0.448this study
199-1220B199-1220B-20X-1,85-87198.2554780.60.677-0.452this study
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199-1220B199-1220B-20X-1,100-102198.4054840.70.714-0.422this study
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199-1220B199-1220B-20X-1,110-112198.5054880.80.695-0.467this study
199-1220B199-1220B-20X-1,115-117198.5554900.90.748-0.254this study
199-1220B199-1220B-20X-1,120-122198.6054920.90.653-0.475this study
199-1220B199-1220B-20X-1,125-127198.6554941.00.711-0.303this study
199-1220B199-1220B-20X-1,130-132198.7054961.00.683-0.281this study
199-1220B199-1220B-20X-1,135-137198.7554981.10.563-0.312this study
199-1220B199-1220B-20X-1,140-142198.8055001.10.624-0.331this study
199-1220B199-1220B-20X-1,145-147198.8555021.10.447-0.307this study
199-1220B199-1220B-20X-1,146-148198.8655025.20.501-0.395this study
199-1220B199-1220B-20X-2,5-7198.9555061.20.372-0.354this study
199-1220B199-1220B-20X-2,10-12199.0055081.30.123-0.603this study
199-1220B199-1220B-20X-2,15-17199.0555101.3-0.270-0.662this study
199-1220B199-1220B-20X-2,20-22199.1055121.40.242-0.587this study
199-1220B199-1220B-20X-2,25-27199.1555141.4-0.647-0.991this study
199-1220B199-1220B-20X-2,30-32199.2055161.5-0.575-1.016this study
199-1220B199-1220B-20X-2,35-37199.2555181.5-0.697-1.028this study
199-1220B199-1220B-20X-2,40-42199.3055186.3-0.572-0.977this study
199-1220B199-1220B-20X-2,45-47199.3555191.0-1.421-1.035this study
199-1220B199-1220B-20X-2,80-82199.7055224.50.641-0.377this study
199-1220B199-1220B-20X-2,85-87199.7555229.20.510-0.341this study
199-1220B199-1220B-20X-2,90-92199.8055234.00.791-0.315this study
199-1220B199-1220B-20X-CC,0-2199.8555238.80.623-0.277this study
199-1220B199-1220B-20X-CC,8-10199.9355246.40.808-0.185this study
199-1221C 199-1221C-11X-2,3-5151.9354491.10.813-0.140this study
199-1221C199-1221C-11X-2,23-25152.1354560.50.833-0.047this study
199-1221C199-1221C-11X-2,43-45152.3354629.90.709-0.188this study
199-1221C199-1221C-11X-2,53-55152.4354664.60.525-0.297this study
199-1221C199-1221C-11X-2,62-64152.5254695.80.711-0.290this study
199-1221C199-1221C-11X-2,73-75152.6354734.00.892-0.236this study
199-1221C199-1221C-11X-2,83-85152.7254765.20.788-0.365this study
199-1221C199-1221C-11X-2,93-95152.8354803.40.777-0.378this study
199-1221C199-1221C-11X-2,103-105152.9354838.00.981-0.279this study
199-1221C199-1221C-11X-2,113-115153.0354872.70.874-0.271this study
199-1221C199-1221C-11X-2,124-126153.1454910.90.783-0.389this study
199-1221C199-1221C-11X-2,133-135153.2354942.10.745-0.301this study
199-1221C199-1221C-11X-2,144-146153.3454980.30.776-0.191this study
199-1221C199-1221C-11X-3,4-6153.4455015.00.860-0.083this study
199-1221C199-1221C-11X-3,5-8153.4555018.41.3060.068this study
199-1221C199-1221C-11X-3,9-12153.4955032.31.1800.082this study
199-1221C199-1221C-11X-3,10-13153.5055035.80.7580.257this study
199-1221C199-1221C-11X-3,15-18153.5555053.10.6760.237this study
199-1221C199-1221C-11X-3,15-17153.5555053.10.670-0.235this study
199-1221C199-1221C-11X-3,16-19153.5655056.61.4210.121this study
199-1221C199-1221C-11X-3,24-26153.6455084.40.619-0.359this study
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199-1221C199-1221C-11X-3,30-33153.7055105.20.7420.199this study
199-1221C199-1221C-11X-3,34-36153.7455119.10.609-0.196this study
199-1221C199-1221C-11X-3,35-38153.7555122.50.5990.178this study
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199-1221C199-1221C-11X-3,45-48153.8555157.20.2750.317this study
199-1221C199-1221C-11X-3,52-54153.9255181.50.0740.397this study
199-1221C199-1221C-11X-3,54-56153.9455184.30.1820.524this study
199-1221C199-1221C-11X-3,56-58153.9655187.00.3010.719this study
199-1221C199-1221C-11X-3,58-60153.9855189.80.4660.880this study
199-1221C199-1221C-11X-3,60-62154.0055192.60.1370.504this study
199-1221C199-1221C-11X-3,62-64154.0255195.30.2420.481this study
199-1221C199-1221C-11X-3,70-72154.1055206.40.5840.108this study
199-1221C199-1221C-11X-3,88-90154.2855231.21.0630.064this study
199-1221C199-1221C-11X-3,90-92154.3055234.01.0490.028this study
199-1221C199-1221C-11X-3,92-94154.3255236.81.0000.152this study
199-1221C199-1221C-11X-3,94-96154.3455239.50.9820.127this study
199-1221C199-1221C-11X-3,96-98154.3655242.30.9760.041this study
199-1221C199-1221C-11X-3,98-100154.3855245.10.8870.020this study
199-1221C199-1221C-11X-3,105-108154.4555254.71.0700.088this study
199-1221C199-1221C-11X-3,115-118154.5555268.51.1930.020this study
199-1221C199-1221C-11X-3,120-123154.6055275.41.1960.055this study
199-1221C199-1221C-11X-3,125-128154.6555282.41.2720.032this study
199-1221C199-1221C-11X-3,130-133154.7055289.31.1980.012this study
199-1221C199-1221C-11X-3,135-138154.7555296.21.2840.040this study
199-1221C199-1221C-11X-3,140-142154.8055303.11.1190.005this study
207-1258C 207-1258C-8R-4,0-1191.7054847.8-0.351-3.194this study
207-1258C207-1258C-8R-4,0-1191.7054847.80.056-0.862this study
207-1258C207-1258C-8R-4,10-11191.8054856.8-0.177-0.974this study
207-1258C207-1258C-8R-4,20-21191.9054865.8-0.670-3.185this study
207-1258C207-1258C-8R-4,30-31192.0054874.8-0.267-3.196this study
207-1258C207-1258C-8R-4,40-41192.1054883.8-0.458-3.020this study
207-1258C207-1258C-8R-4,50-51192.2054892.9-0.476-3.216this study
207-1258C207-1258C-8R-4,75-76192.4554915.40.131-0.668this study
207-1258C207-1258C-8R-4,80-81192.5054919.9-0.034-0.894this study
207-1258C207-1258C-8R-4,85-86192.5554924.4-0.205-0.910this study
207-1258C207-1258C-8R-4,140-141193.1054974.0-0.130-0.936this study
207-1258C207-1258C-8R-4,145-146193.1554978.5-0.136-0.984this study
207-1258C207-1258C-8R-4,149-150193.1954982.2-0.248-1.123this study
207-1258C207-1258C-8R-5,0-1193.2054983.1-0.258-1.021this study
207-1258C207-1258C-8R-5,20-21193.4055001.1-0.319-0.934this study
207-1258C207-1258C-8R-5,70-71193.9055046.2-0.701-1.241this study
207-1258C207-1258C-8R-5,90-91194.1055064.2-0.710-1.202this study
207-1258C207-1258C-8R-5,100-101194.2055073.3-0.633-1.178this study
207-1258C207-1258C-8R-5,110-111194.3055082.3-0.498-0.980this study
207-1258C207-1258C-8R-5,149-150194.6955117.5-1.404-1.512this study
207-1258C207-1258C-8R-6,0-1194.7055118.4-1.215-1.320this study
207-1258C207-1258C-8R-6,10-11194.8055127.4-1.452-1.598this study
207-1258C207-1258C-8R-6,20-21194.9055136.4-1.522-1.640this study
207-1258C207-1258C-8R-6,30-31195.0055145.4-1.419-1.579this study
207-1258C207-1258C-8R-6,40-41195.1055154.4-1.451-1.739this study
207-1258C207-1258C-8R-6,50-51195.2055163.5-1.609-1.645this study
207-1258C207-1258C-8R-6,55-56195.2555168.0-1.880-2.053this study
207-1258C207-1258C-8R-6,60-61195.3055172.5-2.006-2.216this study
207-1258C207-1258C-8R-6,65-66195.3555177.0-2.060-2.160this study
207-1258C207-1258C-8R-6,70-71195.4055181.5-2.057-2.140this study
207-1258C207-1258C-8R-6,106-108195.7655228.70.354-0.764this study
207-1258C207-1258C-8R-6,110-111195.8055234.00.543-0.730this study
207-1258C207-1258C-8R-6,130-131196.0055260.20.590-0.739this study
207-1258C207-1258C-8R-6,148-149196.1855283.90.517-1.048this study
74-525A 74-525A-32R-4,75-77388.8654381.00.520-0.740Thomas and Shackleton, 1996
74-525A74-525A-32R-4,125-127389.3654493.71.190-0.370Thomas and Shackleton, 1996
74-525A74-525A-32R-5,25-27389.8654606.51.070-0.340Thomas and Shackleton, 1996
74-525A74-525A-32R-5,48-50390.0854656.10.980-0.280Thomas and Shackleton, 1996
74-525A74-525A-32R-5,77-79390.3854723.71.090-0.370Thomas and Shackleton, 1996
74-525A74-525A-32R-5,115-117390.7654809.41.150-0.030Thomas and Shackleton, 1996
74-525A74-525A-32R-6,25-27391.3654944.70.960-0.250Thomas and Shackleton, 1996
74-525A74-525A-32R-6,50-52391.6155001.10.880-0.520Thomas and Shackleton, 1996
74-525A74-525A-32R-6,76-78391.8755059.71.100-0.300Thomas and Shackleton, 1996
74-525A74-525A-32R-6,90-92392.0155091.31.090-0.290Thomas and Shackleton, 1996
74-525A74-525A-32R-6,113-115392.2455143.2-1.090-1.060Thomas and Shackleton, 1996
74-525A74-525A-32R-6,130-132392.4155181.5-1.470-1.500Thomas and Shackleton, 1996
74-525A74-525A-32R-6,145-147392.5655201.2-0.030-0.930Thomas and Shackleton, 1996
74-525A74-525A-32R-7,22-24392.8155234.01.2700.030Thomas and Shackleton, 1996
74-525A74-525A-32R-7,53-55393.1155273.41.530-0.320Thomas and Shackleton, 1996
74-527 74-527-24R-1,62-64199.6354954.50.820-0.140Thomas and Shackleton, 1996
74-52774-527-24R-1,85-89199.8655001.10.760-0.110Thomas and Shackleton, 1996
74-52774-527-24R-1,102-104200.0355035.60.650-0.320Thomas and Shackleton, 1996
74-52774-527-24R-1,136-138200.3755104.50.290-0.450Thomas and Shackleton, 1996
74-52774-527-24R-2,5-7200.5655143.0-0.180-0.670Thomas and Shackleton, 1996
74-52774-527-24R-2,20-22200.7155173.4-0.980-1.350Thomas and Shackleton, 1996
74-52774-527-24R-2,38-40200.8955191.3-0.920-1.350Thomas and Shackleton, 1996
74-52774-527-24R-2,56-58201.0755203.91.120-0.320Thomas and Shackleton, 1996
74-52774-527-24R-2,68-70201.1955212.31.000-0.740Thomas and Shackleton, 1996
74-52774-527-24R-2,80-82201.3155220.71.230-0.320Thomas and Shackleton, 1996
74-52774-527-24R-2,88-90201.3955226.31.400-0.220Thomas and Shackleton, 1996
74-52774-527-24R-2,115-117201.6655245.21.420-0.030Thomas and Shackleton, 1996
74-52774-527-24R-3,28-30202.2955289.31.300-0.070Thomas and Shackleton, 1996
74-52774-527-24R-3,48-50202.4955303.31.150-0.370Thomas and Shackleton, 1996
74-52774-527-24R-3,75-77202.7655322.21.250-0.160Thomas and Shackleton, 1996
113-690B 113-690B-18H-4,110-114162.8054724.11.050-0.050Kennett and Stott, 1990
113-690B113-690B-18H-5,36-40163.5654772.40.920-0.390Kennett and Stott, 1990
113-690B113-690B-18H-5,110-114164.3054819.40.900-0.390Kennett and Stott, 1990
113-690B113-690B-18H-6,36-40165.0654867.61.040-0.220Kennett and Stott, 1990
113-690B113-690B-18H-6,110-114165.8054914.70.970-0.140Kennett and Stott, 1990
113-690B113-690B-19H-1,15-19167.0554994.10.561-0.200Stott et al., 1996
113-690B113-690B-19H-1,27-30167.1755001.70.626-0.112Stott et al., 1996
113-690B113-690B-19H-1,45-49167.3555013.10.470-0.316Stott et al., 1996
113-690B113-690B-19H-1,55-59167.4555019.50.533-0.161Stott et al., 1996
113-690B113-690B-19H-1,64-68167.5455025.20.551-0.235Stott et al., 1996
113-690B113-690B-19H-1,73-77167.6355031.00.409-0.308Stott et al., 1996
113-690B113-690B-19H-1,86-88167.7655039.30.411-0.304Stott et al., 1996
113-690B113-690B-19H-1,109-112167.9955053.70.330-0.360Kennett and Stott, 1990
113-690B113-690B-19H-1,135-139168.2555069.90.5180.026Stott et al., 1996
113-690B113-690B-19H-1,147-150168.3755077.80.246-0.414Stott et al., 1996
113-690B113-690B-19H-2,6-9168.4655083.80.318-0.315Stott et al., 1996
113-690B113-690B-19H-2,15-19168.5555089.60.337-0.124Stott et al., 1996
113-690B113-690B-19H-2,45-49168.8555108.60.114-0.464Stott et al., 1996
113-690B113-690B-19H-2,58-62168.9855116.90.100-0.370Stott et al., 1996
113-690B113-690B-19H-2,73-77169.1355126.5-0.052Stott et al., 1996
113-690B113-690B-19H-2,86-89169.2655134.7-0.1980.582Stott et al., 1996
113-690B113-690B-19H-2,94-99169.3455139.80.052-0.439Stott et al., 1996
113-690B113-690B-19H-2,109-112169.4955149.4-0.470-0.830Kennett and Stott, 1990
113-690B113-690B-19H-2,125-129169.6555162.6-0.853-0.989Stott et al., 1996
113-690B113-690B-19H-2,137-141169.7755172.0-0.902-1.063Stott et al., 1996
113-690B113-690B-19H-2,145-149169.8555176.0-0.999-1.161Stott et al., 1996
113-690B113-690B-19H-3,4-5169.9455180.5-1.163-1.316Stott et al., 1996
113-690B113-690B-19H-3,15-18170.0555186.0-1.150-1.399Stott et al., 1996
113-690B113-690B-19H-3,72-76170.6255228.31.5650.151Stott et al., 1996
113-690B113-690B-19H-3,73-74170.6455230.01.8000.290Thomas et al., 2002
113-690B113-690B-19H-3,74-75170.6555230.81.6100.010Thomas et al., 2002
113-690B113-690B-19H-3,75-76170.6555230.81.6500.080Thomas et al., 2002
113-690B113-690B-19H-3,76-77170.6755232.40.800-0.810Thomas et al., 2002
113-690B113-690B-19H-3,76-77170.6755232.40.600-0.830Thomas et al., 2002
113-690B113-690B-19H-3,77-78170.6855233.21.5800.090Thomas et al., 2002
113-690B113-690B-19H-3,78-80170.6955234.01.3000.070Thomas et al., 2002
113-690B113-690B-19H-3,80-81170.7155237.81.4500.040Thomas et al., 2002
113-690B113-690B-19H-3,81-82170.7255239.71.5900.210Thomas et al., 2002
113-690B113-690B-19H-3,82-83170.7355241.61.5400.000Thomas et al., 2002
113-690B113-690B-19H-3,83-84170.7455243.51.6200.100Thomas et al., 2002
113-690B113-690B-19H-3,84-85170.7555245.51.6400.010Thomas et al., 2002
113-690B113-690B-19H-3,86-90170.7655247.41.5580.270Stott et al., 1996
113-690B113-690B-19H-3,94-97170.8455257.21.4530.078Stott et al., 1996
113-690B113-690B-19H-3,109-112170.9955265.50.930-0.130Kennett and Stott, 1990
113-690B113-690B-19H-3,127-130171.1755275.41.2300.262Stott et al., 1996
113-690B113-690B-19H-4,5-9171.4555288.91.134-0.378Stott et al., 1996
113-690B113-690B-19H-4,15-19171.5555293.70.8030.043Stott et al., 1996
113-690B113-690B-19H-4,26-28171.6655298.61.5800.206Stott et al., 1996
113-690B113-690B-19H-4,45-49171.8555306.51.6210.073Stott et al., 1996
113-690B113-690B-19H-4,65-68172.0555314.71.5730.066Stott et al., 1996
113-690B113-690B-19H-4,109-112172.4955331.71.200-0.100Kennett and Stott, 1990
113-690B113-690B-19H-5,5-9172.9555370.51.439-0.026Stott et al., 1996
113-690B113-690B-19H-5,15-19173.0555382.21.7240.188Stott et al., 1996
113-690B113-690B-19H-5,44-47173.3455416.01.7170.338Stott et al., 1996
113-690B113-690B-19H-5,56-59173.4655430.01.5990.226Stott et al., 1996
113-690B113-690B-19H-5,64-68173.5455439.31.260-0.034Stott et al., 1996
113-690B113-690B-19H-5,73-77173.6355449.81.4240.105Stott et al., 1996
113-690B113-690B-19H-5,86-89173.7655465.01.6110.086Stott et al., 1996
113-690B113-690B-19H-5,94-96173.8455474.31.5290.018Stott et al., 1996
113-690B113-690B-19H-5,109-112173.9955491.81.370-0.220Kennett and Stott, 1990
113-690B113-690B-20H-1,36-38174.5655558.31.330-0.350Kennett and Stott, 1990
113-690B113-690B-20H-1,110-112175.3055644.71.680-0.070Kennett and Stott, 1990
113-690B113-690B-20H-2,36-38176.0655733.31.530-0.280Kennett and Stott, 1990
113-690B113-690B-20H-2,110-112179.8056169.71.920-0.010Kennett and Stott, 1990
113-690B113-690B-18H-3,40-42160.6154584.91.070-0.350Thomas and Shackleton, 1996
113-690B113-690B-18H-4,40-42162.1254680.91.820-0.040Thomas and Shackleton, 1996
113-690B113-690B-18H-5,40-42163.6154775.51.260-0.380Thomas and Shackleton, 1996
113-690B113-690B-18H-6,40-42165.1154870.81.3600.080Thomas and Shackleton, 1996
113-690B113-690B-18H-CC,CC166.6554968.71.4500.150Thomas and Shackleton, 1996
113-690B113-690B-19H-1,40-42167.3155010.61.170-0.340Thomas and Shackleton, 1996
113-690B113-690B-19H-1,74-76167.6555032.21.580-0.780Thomas and Shackleton, 1996
113-690B113-690B-19H-1, 114-120168.0755058.61.670-0.250Thomas and Shackleton, 1996
113-690B113-690B-19H-2,40-42168.8155106.10.770-0.710Thomas and Shackleton, 1996
113-690B113-690B-19H-2,74-76169.1655128.40.540-0.530Thomas and Shackleton, 1996
113-690B113-690B-19H-2,118-124169.5855156.7-0.030-0.770Thomas and Shackleton, 1996
113-690B113-690B-19H-3,40-42170.3155203.3-0.700-1.390Thomas and Shackleton, 1996
113-690B113-690B-19H-3,74-76170.6555230.81.8500.060Thomas and Shackleton, 1996
113-690B113-690B-19H-3,115-121171.0555268.81.2500.020Thomas and Shackleton, 1996
113-690B113-690B-19H-4,42-44171.8555306.51.4700.080Thomas and Shackleton, 1996
113-690B113-690B-19H-4,74-76172.1655319.11.5100.040Thomas and Shackleton, 1996
113-690B113-690B-19H-5,40-42173.3155412.51.610-0.080Thomas and Shackleton, 1996
113-690B113-690B-19H-5,74-76173.6955456.81.5100.060Thomas and Shackleton, 1996
113-690B113-690B-19H-CC,19H,CC174.3055528.02.950-0.240Thomas and Shackleton, 1996
113-690B113-690B-20H-1,40-42174.7155575.81.890-0.160Thomas and Shackleton, 1996
113-690B113-690B-20H-2,40-42176.2155750.82.840-0.140Thomas and Shackleton, 1996
113-690B113-690B-20H-3,40-42177.7155925.82.1800.110Thomas and Shackleton, 1996
113-690B113-690B-20H-4,41-43179.2256102.02.4300.460Thomas and Shackleton, 1996
113-690B113-690B-20H-CC,CC180.2856225.71.8900.070Thomas and Shackleton, 1996
113-690B113-690B-21H-1,40-42180.7156275.82.3300.090Thomas and Shackleton, 1996
113-690B113-690B-21H-2,40-42182.2156450.81.8700.070Thomas and Shackleton, 1996
113-690B113-690B-21H-3,40-42183.7156625.82.0800.010Thomas and Shackleton, 1996
113-690B113-690B-21H-4,5-7184.8656760.01.950-0.090Thomas and Shackleton, 1996
119-738C 119-738C-11R-1,108-110284.4955001.11.170-0.270Lu and Keller, 1993
119-738C119-738C-11R-1,115-118284.5255009.80.400-0.120Lu and Keller, 1993
119-738C119-738C-11R-2,2-4284.9355129.1-1.270-1.170Lu and Keller, 1993
119-738C119-738C-11R-2,9-11285.0055149.5-1.250-1.340Lu and Keller, 1993
119-738C119-738C-11R-2,20-22285.1155181.5-1.810-1.760Lu and Keller, 1993
119-738C119-738C-11R-2,44-46285.3555213.80.320-0.460Lu and Keller, 1993
119-738C119-738C-11R-2,52-54285.4355224.6-0.210-0.580Lu and Keller, 1993
119-738C119-738C-11R-2,59-61285.5055234.00.9800.000Lu and Keller, 1993
119-738C119-738C-11R-2,61-63285.5255236.70.840-0.170Lu and Keller, 1993
119-738C119-738C-11R-2,74-76285.6555254.20.870-0.220Lu and Keller, 1993
119-738C119-738C-11R-2,143-145286.3455347.11.160-0.220Lu and Keller, 1993
119-738C119-738C-11R-3,15-17286.5655376.71.020-0.220Lu and Keller, 1993
119-738C119-738C-12H-3,67101.9755001.11.090-0.180Bralower et al., 1995
119-738C119-738C-12H-3,123102.5355181.50.390-0.130Bralower et al., 1995
119-738C119-738C-12H-5,40104.7055423.90.930-0.360Bralower et al., 1995
119-738C107.7055759.01.3400.260Bralower et al., 1995
171-1051B 171-1051B-59X-3,87510.1754927.80.830-0.050Katz et al., 2003
171-1051B171-1051B-59X-3,120510.5054966.20.900-0.270Katz et al., 2003
171-1051B171-1051B-59X-3,150510.8055001.10.820-0.210Katz et al., 2003
171-1051B171-1051B-59X-CC,43511.0055024.40.400-0.590Katz et al., 2003
171-1051B171-1051B-60X-1,65511.5555088.41.3200.220Katz et al., 2003
171-1051B171-1051B-60X-1,78511.6855103.50.220-0.570Katz et al., 2003
171-1051B171-1051B-60X-1,105511.9555134.9-0.010-0.460Katz et al., 2003
171-1051B171-1051B-60X-1,125512.1555158.2-0.300-0.570Katz et al., 2003
171-1051B171-1051B-60X-1,145512.3555181.5-0.670-1.230Katz et al., 2003
171-1051B171-1051B-60X-2,0512.4055192.00.0600.240Katz et al., 2003
171-1051B171-1051B-60X-2,20512.6055234.01.2800.050Katz et al., 2003
171-1051B171-1051B-60X-2,28512.6855250.81.040-0.170Katz et al., 2003
171-1051B171-1051B-60X-2,42512.8255280.21.160-0.040Katz et al., 2003
171-1051B171-1051B-60X-2,50512.9055297.01.2900.140Katz et al., 2003
171-1051B171-1051B-60X-2,56512.9655309.61.1800.060Katz et al., 2003
171-1051B171-1051B-60X-2,56512.9655309.61.100-0.110Katz et al., 2003
171-1051B171-1051B-60X-2,56512.9655309.61.1800.060Katz et al., 2003
171-1051B171-1051B-60X-2,56512.9655309.61.100-0.110Katz et al., 2003
171-1051B171-1051B-60X-2,63513.0355324.31.1200.030Katz et al., 2003
171-1051B171-1051B-60X-2,73513.1355345.31.3400.160Katz et al., 2003
171-1051B171-1051B-60X-2,80513.2055360.01.1500.170Katz et al., 2003
171-1051B171-1051B-60X-2,83513.2355366.31.1000.140Katz et al., 2003
171-1051B171-1051B-60X-2,93513.3355387.31.2700.130Katz et al., 2003
171-1051B171-1051B-60X-2,103513.4355408.31.160-0.040Katz et al., 2003
171-1051B171-1051B-60X-2,110513.5055423.01.3200.220Katz et al., 2003
171-1051B171-1051B-60X-2,113513.5355429.31.3200.140Katz et al., 2003
171-1051B171-1051B-60X-2,120513.6055444.01.5900.080Katz et al., 2003
171-1051B171-1051B-60X-2,140513.8055486.01.4400.360Katz et al., 2003