# Late Miocene to Present Global Ocean Alkenone and SST Reconstruction Data #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite original publication, online resource and date accessed when using this data. # If there is no publication information, please cite Investigator, title, online resource and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/25390 # Description: NOAA Landing Page # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/herbert2016/herbert2016-odp1010.txt # Description: NOAA location of the template # # Archive: Paleoceanography # # Dataset_DOI: # # Parameter_Keywords: biomarkers #--------------------------------------- # Contribution_Date # Date: 2018-10-10 #--------------------------------------- # File_Last_Modified_Date # Date: 2018-10-10 #--------------------------------------- # Title # Study_Name: Late Miocene to Present Global Ocean Alkenone and SST Reconstruction Data #--------------------------------------- # Investigators # Investigators: Herbert, T.D.; Lawrence, K.T.; Tzanova, A.; Peterson, L.C.; Caballero-Gill, R.; Kelly, C.S. #--------------------------------------- # Description_Notes_and_Keywords # Description: Note: age models for Sites 907 and 982 refined following publication of Herbert et al., 2016 NGS # Provided Keywords: Global ocean cooling, mid-Miocene to Present #--------------------------------------- # Publication # Authors: Herbert, T.D., K.T. Lawrence, A. Tzanova, L.C. Peterson, R. Caballero-Gill, and C.S. Kelly # Published_Date_or_Year: 2016 # Published_Title: Late Miocene Global Cooling and the Rise of Modern Ecosystems # Journal_Name: Nature Geoscience # Volume: 9 # Edition: # Issue: # Pages: 843-847 # Report_Number: # DOI: 10.1038/ngeo2813 # Online_Resource: # Full_Citation: # Abstract: During the late Miocene epoch, about seven million years ago, large areas of the continents experienced drying, enhanced seasonality, and a restructuring of terrestrial plant and animal communities. These changes are seen throughout the subtropics, but have typically been attributed to regional tectonic forcing. Here we present a set of globally distributed sea surface temperature records spanning the past 12 million years based on the alkenone unsaturation method. We find that a sustained late Miocene cooling occurred synchronously in both hemispheres, and culminated with ocean temperatures dipping to near-modern values between about 7 and 5.4 million years ago. The period of maximum cooling coincides with evidence for transient glaciations in the Northern Hemisphere and with a steepening of the pole-to-equator temperature gradient, as well. We thus infer that late Miocene aridity and terrestrial ecosystem changes occurred in a global context of increasing meridional temperature gradients. We conclude that a global forcing mechanism, such as the previously hypothesized decline in atmospheric CO2 levels between eight and six million years ago, is required to explain the late Miocene changes in temperature, climate and ecosystems. #--------------------------------------- # Publication # Authors: LaRiviere, J.P., A.C. Ravelo, A. Crimmins, P.S. Dekens, H.L. Ford, M. Lyle, and M.W. Wara # Published_Date_or_Year: 2012 # Published_Title: Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing # Journal_Name: Nature # Volume: 486 # Edition: # Issue: # Pages: 97-100 # Report_Number: # DOI: 10.1038/nature11200 # Online_Resource: # Full_Citation: # Abstract: Deep-time palaeoclimate studies are vitally important for developing a complete understanding of climate responses to changes in the atmospheric carbon dioxide concentration (that is, the atmospheric partial pressure of CO2, pCO2)1. Although past studies have explored these responses during portions of the Cenozoic era (the most recent 65.5 million years (Myr) of Earth history), comparatively little is known about the climate of the late Miocene (~12–5 Myr ago), an interval with pCO2 values of only 200–350?parts per million by volume but nearly ice-free conditions in the Northern Hemisphere2,3 and warmer-than-modern temperatures on the continents4. Here we present quantitative geochemical sea surface temperature estimates from the Miocene mid-latitude North Pacific Ocean, and show that oceanic warmth persisted throughout the interval of low pCO2~12–5 Myr ago. We also present new stable isotope measurements from the western equatorial Pacific that, in conjunction with previously published data5,6,7,8,9,10, reveal a long-term trend of thermocline shoaling in the equatorial Pacific since ~13?Myr ago. We propose that a relatively deep global thermocline, reductions in low-latitude gradients in sea surface temperature, and cloud and water vapour feedbacks may help to explain the warmth of the late Miocene. Additional shoaling of the thermocline after 5?Myr ago probably explains the stronger coupling between pCO2, sea surface temperatures and climate that is characteristic of the more recent Pliocene and Pleistocene epochs. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: National Science Foundation Ocean Sciences # Grant: 1459280, 1545859 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Evolving Earth Foundation # Grant: #--------------------------------------- # Site_Information # Site_Name: ODP 1010 # Location: Eastern Pacific Ocean # Country: # Northernmost_Latitude: 29.798 # Southernmost_Latitude: 29.798 # Easternmost_Longitude: -118.107 # Westernmost_Longitude: -118.107 # Elevation: -3464 #--------------------------------------- # Data_Collection # Collection_Name: ODP1010-2016alkenones Herbert # First_Year: 13526890 # Last_Year: 38750 # Time_Unit: cal yr BP # Core_Length: # Notes: alkenone data reported from LaRiviere et al., interpreted in anomaly framework by Herbert et al., 2016. Chronology taken from LaRiviere et al., 2012 #--------------------------------------- # Chronology_Information # Chronology: #--------------------------------------- # Variables # Data variables follow that are preceded by "##" in columns one and two. # Variables list, one per line, shortname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) ## sitename sample identification,,,,,paleoceanography,,,C,Site ## Hole notes,,,,,paleoceanography,,,C,hole name ## core notes,,,,,paleoceanography,,,C,core ## section notes,,,,,paleoceanography,,,C,section ## cm_top depth at sample end,,,centimeter,,paleoceanography,,,N, ## cm_base depth at sample start,,,centimeter,,paleoceanography,,,N, ## depth_mbsf depth,,,meter,,paleoceanography,,,N,shipboard meters below sea floor ## depth_mcd depth,,,meter,,paleoceanography,,,N,composite depth ## age_kaBP age,,,calendar kiloyear before present,,paleoceanography,,,N, ## age_uncert_ka age,,90% confidence interval margin of error,calendar kiloyear before present,,paleoceanography,,,N, ## Uk'37 alkenone unsaturation index,sediment,,dimensionless,,paleoceanography,,gas chromatography - flame ionization detection,N,GC-FID ## SST_P sea surface temperature,alkenone unsaturation index,,degree Celsius,,climate reconstructions,,,N,SST calibration following F.G. Prahl et al., 1988; estimated ## SST_M sea surface temperature,alkenone unsaturation index,,degree Celsius,,climate reconstructions,,,N,SST calibration following P.J. Muller et al. 1998; estimated ## SST_anom-M sea surface temperature,alkenone unsaturation index,,degree Celsius,,climate reconstructions,anomalized,,N,SST anomaly relative to modern; Muller calibration ## SST_anom_back sea surface temperature,alkenone unsaturation index,,degree Celsius,,climate reconstructions,anomalized,,N,SST anomaly relative to modern; backtraced for paleolatitude/longitude #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: NaN sitename Hole core section cm_top cm_base depth_mbsf depth_mcd age_kaBP age_uncert_ka Uk'37 SST_P SST_M SST_anom-M SST_anom_back 1010 C 1 1 46 48 0.47 0.47 38.75 NaN 0.478 12.91 13.15 -4.2 -4.2 1010 C 1 1 97 99 0.98 0.98 80.80 NaN 0.557 15.24 15.55 -1.7 -1.8 1010 C 1 1 145 147 1.46 1.46 120.38 NaN 0.645 17.83 18.22 0.9 0.9 1010 C 1 2 44 46 1.95 1.95 160.78 NaN 0.523 14.23 14.51 -2.8 -2.8 1010 C 1 2 92 94 2.43 2.43 200.36 NaN 0.615 16.95 17.31 0.0 0.0 1010 C 1 2 140 142 2.91 2.91 239.94 NaN 0.612 16.86 17.22 -0.1 -0.1 1010 C 1 3 38 40 3.39 3.39 279.51 NaN 0.559 15.31 15.62 -1.7 -1.7 1010 C 1 3 87 89 3.88 3.88 319.92 NaN 0.655 18.11 18.51 1.2 1.2 1010 C 1 3 136 138 4.37 4.37 360.32 NaN 0.510 13.86 14.13 -3.2 -3.2 1010 C 1 4 34 36 4.85 4.85 399.89 NaN 0.689 19.11 19.54 2.2 2.2 1010 C 1 4 83 85 5.34 5.34 440.30 NaN 0.488 13.21 13.46 -3.8 -3.9 1010 C 2 1 35 37 5.86 6.72 554.08 NaN 0.603 16.57 16.93 -0.4 -0.4 1010 E 1 5 128 130 7.29 7.29 601.08 NaN 0.639 17.64 18.02 0.7 0.7 1010 E 1 6 26 28 7.77 7.77 640.66 NaN 0.548 14.97 15.27 -2.0 -2.1 1010 E 1 6 77 79 8.28 8.28 682.71 NaN 0.617 17.00 17.37 0.1 0.0 1010 E 1 CC 6 8 8.77 8.77 723.11 NaN 0.543 14.82 15.12 -2.2 -2.2 1010 C 2 2 140 142 8.41 9.27 764.33 NaN 0.591 16.24 16.58 -0.7 -0.8 1010 C 2 3 38 40 8.89 9.75 802.56 NaN 0.465 12.52 12.74 -4.6 -4.6 1010 E 2 1 20 22 9.21 10.21 838.33 NaN 0.544 14.84 15.14 -2.2 -2.2 1010 E 2 1 73 75 9.74 10.74 879.56 NaN 0.537 14.64 14.93 -2.4 -2.4 1010 E 2 1 122 124 10.23 11.23 917.67 NaN 0.550 15.04 15.34 -2.0 -2.0 1010 E 2 2 22 24 10.73 11.73 956.56 NaN 0.570 15.61 15.93 -1.4 -1.4 1010 E 2 2 48 50 10.99 11.99 976.78 NaN 0.579 15.89 16.22 -1.1 -1.1 1010 E 2 2 74 76 11.25 12.25 996.55 NaN 0.552 15.09 15.40 -1.9 -2.0 1010 E 2 2 102 104 11.53 12.53 1016.91 NaN 0.585 16.07 16.41 -0.9 -0.9 1010 E 2 2 128 130 11.79 12.79 1035.82 NaN 0.560 15.33 15.64 -1.7 -1.7 1010 E 2 3 5 7 12.06 13.06 1055.45 NaN 0.673 18.63 19.05 1.7 1.7 1010 E 2 3 32 34 12.33 13.33 1075.69 NaN 0.639 17.63 18.02 0.7 0.7 1010 E 2 3 59 61 12.60 13.60 1097.63 NaN 0.649 17.95 18.35 1.0 1.0 1010 E 2 3 86 88 12.87 13.87 1119.56 NaN 0.528 14.39 14.67 -2.6 -2.7 1010 E 2 3 112 114 13.13 14.13 1140.69 NaN 0.621 17.10 17.47 0.2 0.1 1010 E 2 3 139 141 13.40 14.40 1162.63 NaN 0.689 19.11 19.54 2.2 2.2 1010 E 2 4 16 18 13.67 14.67 1184.56 NaN 0.645 17.83 18.22 0.9 0.9 1010 E 2 4 43 45 13.94 14.94 1217.95 NaN 0.593 16.30 16.64 -0.7 -0.7 1010 C 2 6 133 135 14.34 15.20 1276.30 NaN 0.576 15.81 16.13 -1.2 -1.2 1010 C 2 7 4 6 14.55 15.41 1323.43 NaN 0.541 14.77 15.07 -2.2 -2.3 1010 C 2 7 27 29 14.78 15.64 1375.04 NaN 0.662 18.34 18.74 1.4 1.4 1010 C 2 7 45 47 14.96 15.82 1415.43 NaN 0.496 13.43 13.68 -3.6 -3.7 1010 C 2 7 65 67 15.16 16.02 1460.31 NaN 0.603 16.59 16.94 -0.4 -0.4 1010 E 2 5 22 24 15.23 16.23 1507.44 NaN 0.555 15.18 15.49 -1.8 -1.9 1010 E 2 5 42 44 15.43 16.43 1552.32 NaN 0.510 13.87 14.13 -3.2 -3.2 1010 E 2 5 82 84 15.83 16.83 1642.09 NaN 0.619 17.06 17.42 0.1 0.1 1010 E 2 5 102 104 16.03 17.03 1686.97 NaN 0.636 17.56 17.94 0.6 0.6 1010 C 3 1 14 16 15.15 17.45 1779.00 NaN 0.608 16.74 17.09 -0.2 -0.3 1010 C 3 1 59 61 15.60 17.90 1860.00 NaN 0.638 17.60 17.99 0.7 0.6 1010 C 3 1 74 76 15.75 18.05 1887.00 NaN 0.697 19.36 19.79 2.5 2.4 1010 E 2 6 77 79 17.28 18.28 1928.40 NaN 0.639 17.65 18.03 0.7 0.6 1010 E 2 6 118 120 17.69 18.69 2073.91 NaN 0.630 17.40 17.77 0.5 0.4 1010 E 2 6 139 141 17.90 18.90 2163.64 NaN 0.634 17.51 17.89 0.6 0.5 1010 E 2 7 10 12 18.11 19.11 2253.36 NaN 0.605 16.64 16.99 -0.3 -0.4 1010 E 2 7 32 34 18.33 19.33 2347.36 NaN 0.668 18.51 18.92 1.6 1.5 1010 E 2 cc 5 7 18.53 19.53 2422.00 NaN 0.640 17.68 18.07 0.8 0.7 1010 C 3 2 92 94 17.43 19.73 2435.33 NaN 0.656 18.15 18.55 1.2 1.1 1010 C 3 2 114 116 17.65 19.95 2449.55 NaN 0.651 18.01 18.41 1.1 1.0 1010 E 3 1 14 16 18.65 20.15 2462.27 NaN 0.606 16.66 17.02 -0.3 -0.4 1010 E 3 1 35 37 18.86 20.36 2475.64 NaN 0.627 17.30 17.67 0.4 0.3 1010 E 3 1 73 75 19.24 20.74 2499.82 NaN 0.629 17.35 17.73 0.4 0.3 1010 E 3 1 111 113 19.62 21.12 2524.00 NaN 0.635 17.54 17.92 0.6 0.5 1010 E 3 1 147 149 19.98 21.48 2546.91 NaN 0.606 16.68 17.04 -0.3 -0.4 1010 E 3 2 37 39 20.38 21.88 2572.36 NaN 0.632 17.43 17.81 0.5 0.4 1010 E 3 2 75 77 20.76 22.26 2611.32 NaN 0.589 16.17 16.51 -0.8 -0.9 1010 E 3 2 113 115 21.14 22.64 2657.09 NaN 0.654 18.08 18.48 1.2 1.1 1010 E 3 3 1 3 21.52 23.02 2702.86 NaN 0.671 18.60 19.01 1.7 1.6 1010 E 3 3 39 41 21.90 23.40 2748.64 NaN 0.661 18.28 18.68 1.4 1.3 1010 E 3 3 77 79 22.28 23.78 2794.41 NaN 0.576 15.79 16.11 -1.2 -1.3 1010 E 3 3 115 117 22.66 24.16 2840.18 NaN 0.629 17.34 17.71 0.4 0.3 1010 E 3 4 3 5 23.04 24.54 2885.95 NaN 0.609 16.76 17.12 -0.2 -0.3 1010 C 3 6 11 13 22.62 24.92 2931.73 NaN 0.558 15.27 15.59 -1.7 -1.8 1010 E 3 4 42 44 23.43 24.93 2932.93 NaN 0.565 15.48 15.80 -1.5 -1.6 1010 C 3 6 101 103 23.52 25.82 3040.14 NaN 0.608 16.75 17.10 -0.2 -0.3 1010 C 3 7 40 42 24.41 26.71 3118.30 NaN 0.624 17.20 17.57 0.3 0.1 1010 C 4 1 65 67 25.16 28.52 3166.74 NaN 0.673 18.66 19.07 1.8 1.6 1010 E 3 7 41 43 27.92 29.42 3190.83 NaN 0.580 15.92 16.25 -1.0 -1.2 1010 C 4 2 94 96 26.95 30.31 3214.65 NaN 0.657 18.17 18.57 1.3 1.1 1010 C 4 3 32 34 27.83 31.19 3242.33 NaN 0.667 18.46 18.87 1.6 1.4 1010 C 4 3 128 130 28.79 32.15 3273.85 NaN 0.700 19.45 19.89 2.6 2.4 1010 C 4 4 65 67 29.66 33.02 3302.42 NaN 0.554 15.15 15.45 -1.8 -2.0 1010 E 4 2 16 18 29.67 33.91 3332.94 NaN 0.700 19.45 19.89 2.6 2.4 1010 E 4 2 107 109 30.58 34.82 3386.47 NaN 0.660 18.25 18.65 1.4 1.2 1010 E 4 3 47 49 31.48 35.72 3439.41 NaN 0.719 19.99 20.45 3.1 3.0 1010 E 4 3 137 139 32.38 36.62 3492.35 NaN 0.703 19.52 19.96 2.7 2.5 1010 C 4 7 65 67 34.16 37.52 3545.29 NaN 0.742 20.66 21.14 3.8 3.7 1010 E 4 4 124 126 33.75 37.99 3572.94 NaN 0.693 19.22 19.66 2.4 2.2 1010 E 4 5 41 43 34.42 38.66 3612.35 NaN 0.704 19.56 20.00 2.7 2.5 1010 E 4 5 109 111 35.10 39.34 3652.35 NaN 0.724 20.15 20.61 3.3 3.1 1010 E 4 6 27 29 35.78 40.02 3692.35 NaN 0.752 20.96 21.45 4.1 4.0 1010 E 4 6 95 97 36.46 40.70 3732.35 NaN 0.720 20.04 20.50 3.2 3.0 1010 E 4 7 13 15 37.14 41.38 3772.35 NaN 0.666 18.43 18.84 1.5 1.4 1010 E 5 1 55 57 38.06 42.74 3852.35 NaN 0.750 20.91 21.39 4.1 3.9 1010 E 5 1 123 125 38.74 43.42 3892.35 NaN 0.761 21.24 21.73 4.4 4.3 1010 E 5 2 43 45 39.44 44.12 3933.53 NaN 0.749 20.88 21.36 4.1 3.9 1010 E 5 2 110 112 40.11 44.79 3972.94 NaN 0.739 20.58 21.06 3.8 3.6 1010 E 5 3 15 17 40.66 45.34 4005.29 NaN 0.710 19.75 20.20 2.9 2.7 1010 E 5 3 72 74 41.23 45.91 4038.82 NaN 0.758 21.15 21.64 4.3 4.2 1010 C 5 6 10 12 41.61 46.47 4071.76 NaN 0.806 22.56 23.09 5.8 5.6 1010 C 5 6 66 68 42.17 47.03 4104.71 NaN 0.780 21.79 22.30 5.0 4.8 1010 C 5 6 122 124 42.73 47.59 4137.65 NaN 0.785 21.94 22.45 5.2 5.0 1010 C 5 7 29 31 43.30 48.16 4171.18 NaN 0.819 22.94 23.49 6.2 6.0 1010 C 5 cc 8 10 43.86 48.72 4193.26 NaN 0.769 21.48 21.98 4.7 4.5 1010 C 6 1 1 3 43.52 49.30 4212.03 NaN 0.691 19.17 19.60 2.3 2.1 1010 C 6 1 57 59 44.08 49.86 4230.15 NaN 0.709 19.70 20.14 2.8 2.7 1010 C 6 1 113 115 44.64 50.42 4248.26 NaN 0.796 22.28 22.80 5.5 5.3 1010 C 6 2 16 18 45.17 50.98 4266.38 NaN 0.822 23.04 23.59 6.3 6.1 1010 C 6 2 68 70 45.69 51.50 4283.21 NaN 0.810 22.69 23.22 5.9 5.7 1010 E 5 cc 20 22 47.43 52.11 4480.00 NaN 0.749 20.88 21.36 4.1 3.9 1010 E 6 1 57 59 47.58 52.53 4522.00 NaN 0.726 20.22 20.68 3.4 3.2 1010 E 6 1 100 102 48.01 52.96 4565.00 NaN 0.739 20.59 21.07 3.8 3.6 1010 E 6 1 142 144 48.43 53.38 4607.00 NaN 0.724 20.16 20.62 3.3 3.1 1010 C 6 4 2 4 51.53 53.84 4658.32 NaN 0.751 20.93 21.42 4.1 3.9 1010 C 6 4 41 43 51.92 54.23 4703.61 NaN 0.760 21.19 21.68 4.4 4.2 1010 C 6 4 82 84 52.33 54.64 4751.23 NaN 0.735 20.48 20.95 3.7 3.4 1010 C 6 4 127 129 52.78 55.09 4802.35 NaN 0.753 20.99 21.48 4.2 4.0 1010 C 6 5 17 19 53.18 55.49 4833.65 NaN 0.746 20.79 21.27 4.0 3.8 1010 C 6 5 64 66 53.65 55.96 4870.43 NaN 0.683 18.95 19.37 2.1 1.9 1010 C 6 5 102 104 54.03 56.34 4900.17 NaN 0.739 20.60 21.08 3.8 3.6 1010 C 6 5 145 147 54.46 56.77 4933.83 NaN 0.719 20.01 20.47 3.2 3.0 1010 C 6 6 40 42 54.91 57.22 4969.04 NaN 0.758 21.15 21.64 4.3 4.1 1010 C 6 6 88 90 55.39 57.70 4997.45 NaN 0.797 22.30 22.82 5.5 5.3 1010 C 6 6 139 141 55.90 58.21 5023.63 NaN 0.764 21.32 21.81 4.5 4.3 1010 C 6 7 39 41 56.40 58.71 5049.30 NaN 0.770 21.50 22.00 4.7 4.5 1010 C 6 cc 16 18 56.84 59.15 5071.89 NaN 0.798 22.33 22.86 5.6 5.3 1010 E 6 6 76 78 55.27 60.22 5126.82 NaN 0.765 21.35 21.84 4.5 4.3 1010 C 7 1 93 95 53.94 60.37 5134.52 NaN 0.684 18.98 19.41 2.1 1.9 1010 C 7 2 130 132 55.81 62.24 5231.18 NaN 0.748 20.87 21.35 4.0 3.8 1010 C 7 4 0 2 57.51 63.94 5431.54 NaN 0.759 21.17 21.66 4.4 4.1 1010 E 7 2 100 102 59.01 65.16 5575.32 NaN 0.809 22.65 23.18 5.9 5.6 1010 E 7 3 100 102 60.51 66.66 5752.11 NaN 0.679 18.82 19.23 1.9 1.7 1010 E 7 4 100 102 62.01 68.16 5901.07 NaN 0.754 21.03 21.51 4.2 4.0 1010 E 7 5 100 102 63.51 69.66 5951.41 NaN 0.787 22.01 22.53 5.2 5.0 1010 C 8 1 116 118 67.17 71.16 6001.74 NaN 0.778 21.73 22.24 4.9 4.7 1010 C 8 3 116 118 70.17 74.16 6102.42 NaN 0.793 22.18 22.70 5.4 5.1 1010 C 8 4 116 118 71.67 75.66 6198.12 NaN 0.778 21.74 22.25 5.0 4.7 1010 C 8 5 116 118 73.17 77.16 6372.24 NaN 0.803 22.47 23.00 5.7 5.4 1010 E 8 5 34 36 72.35 78.66 6521.13 NaN 0.859 24.11 24.69 7.4 7.1 1010 E 8 6 34 36 73.85 80.16 6670.01 NaN 0.807 22.59 23.12 5.8 5.5 1010 C 9 3 42 44 75.43 83.16 6966.40 NaN 0.822 23.03 23.57 6.3 6.0 1010 C 9 4 42 44 76.93 84.66 7107.80 NaN 0.844 23.66 24.23 6.9 6.6 1010 E 9 3 0 2 78.51 85.90 7224.70 NaN 0.932 26.28 26.92 9.6 9.3 1010 C 9 5 42 44 78.43 86.16 7249.21 NaN 0.874 24.57 25.16 7.9 7.5 1010 C 9 6 42 44 79.93 87.66 7390.61 NaN 0.860 24.16 24.74 7.4 7.1 1010 E 9 5 26 28 81.77 89.16 7532.01 NaN 0.787 21.99 22.51 5.2 4.9 1010 C 10 3 62 64 75.63 93.66 7956.23 NaN 0.871 24.48 25.07 7.8 7.4 1010 E 10 2 56 58 87.07 95.16 8097.63 NaN 0.830 23.27 23.82 6.5 6.2 1010 E 10 3 56 58 88.57 96.66 8239.04 NaN 0.828 23.22 23.77 6.5 6.1 1010 E 10 4 56 58 90.07 98.16 8380.44 NaN 0.878 24.66 25.26 8.0 7.6 1010 E 10 5 56 58 91.57 99.66 8521.85 NaN 0.913 25.71 26.33 9.0 8.7 1010 E 10 6 56 58 93.07 101.16 8663.25 NaN 0.896 25.20 25.82 8.5 8.1 1010 C 11 2 72 74 93.23 102.66 8804.66 NaN 0.913 25.71 26.34 9.0 8.7 1010 E 11 2 84 86 96.85 105.66 9087.47 NaN 0.884 24.86 25.47 8.2 7.8 1010 E 11 3 84 86 98.35 107.16 9228.87 NaN 0.865 24.30 24.89 7.6 7.2 1010 E 11 4 84 86 99.85 108.66 9370.28 NaN 0.888 24.96 25.57 8.3 7.9 1010 E 11 5 84 86 101.35 110.16 9498.49 NaN 0.903 25.41 26.03 8.7 8.3 1010 E 11 6 84 86 102.85 111.66 9553.84 NaN 0.926 26.10 26.74 9.4 9.0 1010 C 12 2 64 66 102.65 113.16 9609.19 NaN 0.917 25.82 26.46 9.2 8.7 1010 C 12 3 64 66 104.15 114.66 9664.55 NaN 0.896 25.22 25.83 8.5 8.1 1010 E 12 3 112 114 104.63 117.66 9775.25 NaN 0.911 25.64 26.27 9.0 8.6 1010 E 12 4 112 114 106.13 119.16 9830.60 NaN 0.872 24.49 25.08 7.8 7.4 1010 E 12 5 112 114 107.63 120.66 9885.96 NaN 0.909 25.60 26.23 8.9 8.5 1010 E 12 6 98 100 108.99 122.02 9936.14 NaN 0.932 26.26 26.91 9.6 9.2 1010 C 13 1 140 142 111.41 123.48 9990.02 NaN 0.847 23.76 24.33 7.0 6.6 1010 C 13 2 140 142 112.91 124.98 10045.37 NaN 0.906 25.50 26.12 8.8 8.4 1010 E 13 4 136 138 119.37 130.98 10266.78 NaN 0.883 24.84 25.44 8.1 7.7 1010 C 14 2 0 2 121.01 134.06 10380.44 NaN 0.920 25.92 26.55 9.3 8.8 1010 C 14 4 0 2 124.01 137.06 10491.14 NaN 0.897 25.25 25.86 8.6 8.1 1010 C 14 5 0 2 125.51 138.56 11014.96 NaN 0.907 25.54 26.16 8.9 8.4 1010 E 14 4 70 72 128.21 140.06 11452.88 NaN 0.944 26.62 27.27 10.0 9.5 1010 E 14 5 70 72 129.71 141.56 11494.89 NaN 0.939 26.46 27.11 9.8 9.4 1010 C 15 1 74 76 129.75 142.96 11534.10 NaN 0.931 26.23 26.88 9.6 9.1 1010 C 15 3 74 76 132.75 145.96 11618.13 NaN 0.928 26.16 26.80 9.5 9.1 1010 C 15 4 74 76 134.25 147.46 11660.14 NaN 0.940 26.50 27.15 9.9 9.4 1010 C 15 5 74 76 135.75 148.96 11702.15 NaN 0.937 26.42 27.07 9.8 9.3 1010 C 15 6 74 76 137.25 150.46 11744.16 NaN 0.932 26.26 26.91 9.6 9.2 1010 C 15 7 69 71 138.70 151.91 11784.77 NaN 0.932 26.26 26.91 9.6 9.2 1010 E 15 5 110 112 139.61 151.96 11786.17 NaN 0.933 26.29 26.93 9.6 9.2 1010 C 16 1 131 133 139.82 153.46 11828.18 NaN 0.949 26.77 27.43 10.1 9.7 1010 C 16 4 131 133 144.32 157.96 11954.21 NaN 0.951 26.81 27.48 10.2 9.7 1010 C 16 5 131 133 145.82 159.46 11996.22 NaN 0.942 26.56 27.22 9.9 9.5 1010 C 17 1 0 2 148.01 160.77 12032.91 NaN 0.935 26.35 26.99 9.7 9.2 1010 C 17 2 0 2 149.51 162.27 12074.92 NaN 0.943 26.60 27.25 10.0 9.5 1010 C 17 3 0 2 151.01 163.77 12116.93 NaN 0.943 26.58 27.24 9.9 9.5 1010 C 17 4 0 2 152.51 165.27 12158.94 NaN 0.947 26.72 27.37 10.1 9.6 1010 C 17 5 0 2 154.01 166.77 12200.96 NaN 0.948 26.74 27.40 10.1 9.7 1010 E 17 4 70 72 156.71 168.27 12259.32 NaN 0.935 26.35 27.00 9.7 9.3 1010 E 17 5 70 72 158.21 169.77 12331.26 NaN 0.945 26.64 27.29 10.0 9.6 1010 E 17 6 70 72 159.71 171.27 12403.19 NaN 0.940 26.51 27.16 9.9 9.4 1010 C 18 2 0 2 159.01 172.77 12475.13 NaN 0.934 26.33 26.97 9.7 9.2 1010 C 18 3 0 2 160.51 174.27 12547.06 NaN 0.941 26.52 27.17 9.9 9.4 1010 C 18 4 0 2 162.01 175.77 12619.00 NaN 0.938 26.44 27.09 9.8 9.4 1010 E 18 5 6 8 163.57 178.77 12762.87 NaN 0.949 26.75 27.41 10.1 9.7 1010 E 18 6 6 8 165.07 180.27 12834.80 NaN 0.945 26.64 27.30 10.0 9.6 1010 C 19 1 0 2 165.21 180.96 12867.89 NaN 0.948 26.74 27.40 10.1 9.7 1010 C 19 2 81 83 167.52 183.27 12978.67 NaN 0.931 26.23 26.88 9.6 9.2 1010 C 21 1 10 12 184.71 184.71 13047.73 NaN 0.938 26.44 27.09 9.8 9.4 1010 C 19 3 81 83 169.02 184.77 13050.60 NaN 0.947 26.69 27.35 10.1 9.6 1010 C 19 4 81 83 170.52 186.27 13113.17 NaN 0.938 26.44 27.09 9.8 9.4 1010 E 19 4 0 2 175.11 189.26 13196.92 NaN 0.932 26.28 26.92 9.6 9.2 1010 C 20 2 52 54 176.93 193.26 13308.96 NaN 0.950 26.78 27.45 10.1 9.7 1010 C 20 3 52 54 178.43 194.76 13350.98 NaN 0.945 26.65 27.31 10.0 9.6 1010 C 20 4 52 54 179.93 196.26 13393.00 NaN 0.936 26.40 27.04 9.7 9.3 1010 C 21 1 10 12 184.71 201.04 13526.89 NaN 0.938 26.44 27.09 9.8 9.4