# Sikuiui Lake, Greenland 9,500 Year Sediment Biomarker Data #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. # If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/24570 # Description: NOAA Landing Page # Online_Resource: https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/greenland/sikuiui2018biomarker.txt # Description: NOAA location of the template # # Original_Source_URL: # Description: # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Paleolimnology # # Parameter_Keywords: #--------------------------------------- # Contribution_Date # Date: 2018-11-09 #--------------------------------------- # File_Last_Modified_Date # Date: 2018-11-09 #--------------------------------------- # Title # Study_Name: Sikuiui Lake, Greenland 9,500 Year Sediment Biomarker Data #--------------------------------------- # Investigators # Investigators: Thomas, E.K.; Castaņeda, I.S.; McKay, N.P.; Briner, J.P.; Salacup, J.M.; Nguyen, K.Q.; Schweinsberg, A.D. #--------------------------------------- # Description_Notes_and_Keywords # Description: Fatty acid and GDGT biomarker data from sediments collected in Sikuiui Lake, west Greenland, for the past 9,500 years. #--------------------------------------- # Publication # Authors: E.K. Thomas, I.S. Castaņeda, N.P. McKay, J.P. Briner, J.M. Salacup, K.Q. Nguyen, A.D. Schweinsberg # Published_Date_or_Year: 2018-10-16 # Published_Title: A Wetter Arctic Coincident With Hemispheric Warming 8,000 Years Ago # Journal_Name: Geophysical Research Letters # Volume: 45 # Edition: # Issue: 19 # Pages: 10637-10647 # Report Number: # DOI: 10.1029/2018GL079517 # Online_Resource: https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018GL079517 # Full_Citation: # Abstract: Arctic precipitation is predicted to increase this century, with dramatic consequences for high-latitude systems. Observations remain spatiotemporally limited, hampering determination of the forcings causing wetter Arctic conditions, although two mechanisms have been proposed: enhanced local evaporation and greater poleward atmospheric moisture transport. Here a subcentennial-resolution multiproxy lake sediment record from western Greenland sheds light on these mechanisms. Cool summers throughout the Northern Hemisphere and in western Greenland 9 to 8 ka are associated with aridity in this region, via reductions in local evaporation and in meridional moisture gradients, which suppressed poleward moisture transport. Summers became more humid starting 8.1 ka, mainly due to increased evaporation from warmer Arctic seas but also to increased poleward moisture transport caused by hemispheric warming. This record provides independent support for predictions of both enhanced local evaporation and increased poleward moisture transport causing wetter Arctic summers in step with global ocean and atmosphere warming. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: National Science Foundation # Grant: 1349595, 1204005 #--------------------------------------- # Site Information # Site_Name: Sikuiui Lake # Location: North America>Greenland # Country: # Northernmost_Latitude: 70.218 # Southernmost_Latitude: 70.218 # Easternmost_Longitude: -51.122 # Westernmost_Longitude: -51.122 # Elevation: 604 #--------------------------------------- # Data_Collection # Collection_Name: Sikuiui2018 # First_Year: 9563 # Last_Year: -55 # Time_Unit: cal yr BP # Core_Length: 0.98 # Notes: only the lowermost 28 cm of core 13MCRD3 were analyzed for this study #--------------------------------------- # Chronology_Information # Chronology: # # LabID Lab ID # corrected midpoint depth (cm) depth from top of sediment cm # thickness (cm) thickness cm # 14C age Material measured NaN # 14C age uncertainty 14C age yr BP # 1s range min 14C age uncertainty yr BP # 1s range max Fraction Modern NaN # 1s mid Fraction Modern uncertainty NaN # 2s range min d13C per mil # Sample ID Lab ID depth from top of sediment thickness Material measured 14C age 14C age uncertainty Fraction Modern Fraction Modern uncertainty d13C # 13MCR-D3-14.25 OS-106899 4.75 0.5 aquatic moss 890 20 0.8949 0.0025 -25.67 # 13MCR-D3-25.25 OS-106900 15.75 0.5 aquatic moss 1800 20 0.7993 0.0022 -22.32 # 13MCR-D3-34.5 OS-110852 25 0.5 aquatic moss 2690 20 0.7149 0.0019 -24.04 # 13MCR-D3-50.75 OS-106901 41.25 0.5 aquatic moss 3200 25 0.6712 0.0019 -21.53 # 13MCRD3 59.0-59.5 cm OS-117858 49.75 0.5 aquatic moss 4150 20 0.5963 0.0014 -21.82 # 13MCR-D3-68.25 OS-106872 58.75 0.5 aquatic moss 5080 30 0.5312 0.0021 -21.23 # 13MCRD3 76.0-76.5 cm OS-116885 66.75 0.5 aquatic moss 5970 25 0.4758 0.0015 -22.84 # 13MCR-D3-85.25 OS-110853 75.75 0.5 aquatic moss 6640 30 0.4374 0.0017 -23.1 # 13MCRD3 87.25-87.75 cm OS-116884 78 0.5 aquatic moss 7110 30 0.4128 0.0014 -21.89 # 13MCR-D3-96.25 OS-106873 86.75 0.5 aquatic moss 8020 40 0.3684 0.0018 -25.22 # 13MCRD3 101.5-102.0 cm OS-116949 92.25 0.5 aquatic moss 8090 35 0.3655 0.0016 -26.17 # 13MCR-D3-107.25 OS-106902 97.75 0.5 aquatic moss 8390 40 0.3518 0.0017 -27.4 # #--------------------------------------- # 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) ## depth depth,,,cm,,,,,N,midpoint depth in core ## thick thickness of sample,,,cm,,,,,N, ## age age,,,cal yr BP,,,,,N,modeled age of sediment ## minAge age minimum,,minimum of 95% confidence interval,cal yr BP,,,,,N,modeled age of sediment ## maxAge age_maximum,,maximum of 95% confidence interval,cal yr BP,,,,,N,modeled age of sediment ## C23d2H delta D, C23 n-alkane,,per mil,,paleolimnology,,,N,dDSummerPrecipitation.air.positive ## C23stdev standard deviation of replicate measurements of C23 n-alkane d2H,,,per mil,,paleolimnology,,,N, ## C23n number of replicate measurements of C23 n-alkane d2H,,,,,paleolimnology,,,N, ## C25d2H delta D,C25 n-alkane,,per mil,,paleolimnology,,,N, ## C25stdev standard deviation of replicate measurements of C25 n-alkane d2H,,,per mil,,paleolimnology,,,N, ## C25n number of replicate measurements of C25 n-alkane d2H,,,,,paleolimnology,,,N, ## C27d2H delta D,C27 n-alkane,,per mil,,paleolimnology,,,N, ## C27stdev standard deviation of replicate measurements of C27 n-alkane d2H,,,per mil,,paleolimnology,,,N, ## C27n number of replicate measurements of C27 n-alkane d2H,,,,,paleolimnology,,,N, ## C29d2H delta D,C29 n-alkane,,per mil,,paleolimnology,,,N,dDSummerPrecipitation_Evaporation.air.positive ## C29stdev standard deviation of replicate measurements of C29 n-alkane d2H,,,per mil,,paleolimnology,,,N, ## C29n number of replicate measurements of C29 n-alkane d2H,,,,,paleolimnology,,,N, ## EpsilonC29-C23 Epsilon between C29 n-alkane d2H and C23 n-alkane d2H,,,per mil,,paleolimnology,,,N,Evaporation.air.positive ## EpsilonUncertainty uncertainty propagated through epsilon calculation,,,per mil,,paleolimnology,,,N, ## RH Median Relative Humidity anomaly,,,%,,climate reconstructions,,,N,RelativeHumidity.air.positive; relative to 7.8 to 7.3 ka baseline calculated using methods from Rach et al. 2017; epsilon; and brGDGT-inferred MSAT ## minRH minimum of 95% confidence interval, Relative Humidity anomaly, given all uncertainties in Rach et al. and input parameters,,,climate reconstructions,,,N,RelativeHumidity.air.positive ## maxRH maximum of 95% confidence interval, Relative Humidity anomaly, given all uncertainties in Rach et al. and input parameters,,,climate reconstructions,,,N,RelativeHumidity.air.positive ## MSATRussell2018 Mean Summer Air Temperature,,,degrees C,,climate reconstructions,,,N,SummerTemperature.air.Positive. Calculated using brGDGT fractional abundances in Russell et al 2018 calibration ## f1050_III branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-III (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1050'_III' branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-III' (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1048_IIIb branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-IIIb (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1048'_IIIb' branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-IIIb' (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1046_IIIc branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-IIIc (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1046'_IIIc' branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-IIIc' (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1036_II branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-II (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1036'_II' branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-II' (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1034_IIb branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-IIb (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1034'_IIb' branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-IIb' (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1032_IIc branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-IIc (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1032'_IIc' branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-IIc' (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1022_I branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-I (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1020_Ib branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-Ib (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) ## f1018_Ic branched glycerol dialkyl glycerol tetraether,,,fractional abundance out of 1,,paleolimnology,,,N, fraction of GDGT-Ic (see Russell et al. 2018 for GDGT compound structures; m/z values; and nomenclature) #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: NaN depth thick age minAge maxAge C23d2H C23stdev C23n C25d2H C25stdev C25n C27d2H C27stdev C27n C29d2H C29stdev C29n EpsilonC29-C23 EpsilonUncertainty RH minRH maxRH MSATRussell2018 f1050_III f1050'_III' f1048_IIIb f1048'_IIIb' f1046_IIIc f1046'_IIIc' f1036_II f1036'_II' f1034_IIb f1034'_IIb' f1032_IIc f1032'_IIc' f1022_I f1020_Ib f1018_Ic 70.75 0.5 7204 7009 7397 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 6.3 0.3720 0.0270 0.0020 0.0000 0.0007 0.0000 0.3156 0.0619 0.0218 0.0000 0.0020 0.0000 0.1886 0.0080 0.0005 71.25 0.5 7245 7044 7439 -244.4 2.7 3 -246.9 2.9 3 -243.2 0.8 3 -237.5 2.3 3 9.2 0.13 -8.8 -9.3 -8.4 6.5 0.3568 0.0284 0.0019 0.0004 0.0000 0.0000 0.3130 0.0804 0.0189 0.0006 0.0018 0.0000 0.1908 0.0071 0.0000 71.75 0.5 7287 7080 7481 -243.0 0.3 2 -253.6 0.6 2 -248.1 0.7 2 -247.9 0.6 2 -6.5 0.02 4.4 4.1 4.7 6.6 0.3630 0.0345 0.0020 0.0004 0.0007 0.0000 0.2866 0.0932 0.0192 0.0006 0.0019 0.0000 0.1907 0.0072 0.0000 72.25 0.5 7328 7121 7518 -238.8 NaN 1 -251.5 NaN 1 -242.1 NaN 1 -244.4 NaN 1 -7.4 0.00 5.2 4.9 5.5 6.6 0.3403 0.0364 0.0016 0.0000 0.0005 0.0000 0.3282 0.0777 0.0147 0.0000 0.0012 0.0000 0.1939 0.0052 0.0003 72.75 0.5 7370 7163 7556 -238.3 2.0 3 -238.1 1.8 3 -237.8 1.6 3 -240.2 2.5 3 -2.5 0.03 1.0 0.9 1.2 6.7 0.3527 0.0370 0.0014 0.0000 0.0004 0.0000 0.2921 0.1018 0.0158 0.0006 0.0010 0.0000 0.1909 0.0063 0.0000 73.25 0.5 7411 7204 7585 -253.5 NaN 1 -256.1 NaN 1 -252.1 0.3 2 -252.6 0.1 2 1.2 0.00 -2.1 -2.1 -2.0 6.6 0.3742 0.0399 0.0016 0.0000 0.0005 0.0000 0.2619 0.1113 0.0168 0.0005 0.0012 0.0000 0.1859 0.0063 0.0000 73.75 0.5 7452 7246 7614 -248.2 0.4 2 -249.9 1.1 2 -240.8 0.9 2 -237.6 2.4 2 14.1 0.14 -13.0 -13.6 -12.3 6.4 0.3718 0.0392 0.0018 0.0000 0.0006 0.0000 0.2789 0.1005 0.0168 0.0006 0.0012 0.0000 0.1818 0.0065 0.0003 74.25 0.5 7493 7297 7641 -246.4 3.9 2 -244.9 3.7 3 -240.8 1.5 3 -246.8 3.7 3 -0.4 0.01 -0.7 -0.8 -0.7 6.6 0.3653 0.0436 0.0017 0.0000 0.0004 0.0000 0.2441 0.1426 0.0161 0.0000 0.0010 0.0000 0.1789 0.0062 0.0000 74.75 0.5 7534 7348 7667 -251.4 0.7 2 -249.9 2.6 3 -250.7 0.5 3 -253.7 2.2 3 -3.1 0.03 1.5 1.4 1.7 6.9 0.3406 0.0452 0.0019 0.0003 0.0004 0.0000 0.2532 0.1465 0.0198 0.0004 0.0010 0.0000 0.1840 0.0064 0.0000 75.25 0.5 7574 7415 7691 -254.2 1.5 2 -254.0 1.1 3 -260.2 1.8 3 -258.4 2.5 3 -5.6 0.06 3.7 3.4 3.9 6.7 0.3483 0.0410 0.0018 0.0000 0.0006 0.0000 0.2898 0.1024 0.0182 0.0000 0.0015 0.0000 0.1898 0.0062 0.0004 75.75 0.5 7615 7481 7715 -273.8 0.3 2 -271.0 4.8 3 -275.6 1.0 3 -270.8 3.2 3 4.1 0.05 -4.6 -4.7 -4.4 7.0 0.3521 0.0435 0.0021 0.0003 0.0007 0.0000 0.2527 0.1333 0.0177 0.0007 0.0017 0.0000 0.1892 0.0059 0.0000 76.25 0.5 7668 7562 7759 -264.6 2.6 2 -264.6 2.6 2 -271.7 NaN 1 -271.2 0.4 2 -9.0 0.09 6.7 6.2 7.1 7.9 0.3141 0.0460 0.0018 0.0003 0.0004 0.0000 0.2418 0.1761 0.0124 0.0004 0.0009 0.0000 0.2023 0.0035 0.0000 76.75 0.5 7722 7642 7803 -231.9 1.6 3 -240.8 1.0 3 -241.6 1.4 3 -238.9 5.7 3 -9.2 0.23 6.7 6.2 7.2 6.6 0.3190 0.0431 0.0017 0.0000 0.0004 0.0000 0.3156 0.1159 0.0130 0.0000 0.0009 0.0000 0.1864 0.0036 0.0003 77.25 0.5 7809 7705 7923 -250.5 4.9 2 -249.2 1.6 2 -242.1 0.0 2 -242.2 2.1 2 11.1 0.24 -10.4 -11.1 -9.9 6.6 0.3412 0.0445 0.0024 0.0003 0.0005 0.0000 0.2799 0.1271 0.0161 0.0005 0.0010 0.0000 0.1822 0.0044 0.0000 77.75 0.5 7895 7769 8043 -240.2 1.0 2 -243.1 1.6 2 -241.1 0.2 2 -239.0 0.9 2 1.6 0.01 -2.4 -2.5 -2.4 6.6 0.3661 0.0530 0.0027 0.0000 0.0004 0.0000 0.2431 0.1345 0.0151 0.0005 0.0012 0.0000 0.1794 0.0041 0.0000 78.25 0.5 7975 7850 8095 -246.3 1.4 2 -235.9 4.0 2 -237.0 0.1 2 -235.3 0.5 2 14.6 0.09 -13.2 -13.9 -12.6 5.3 0.3433 0.0525 0.0017 0.0000 0.0002 0.0000 0.3162 0.1109 0.0157 0.0000 0.0010 0.0000 0.1550 0.0031 0.0003 78.75 0.5 8056 7931 8147 -241.0 1.3 3 -236.9 3.3 3 -233.3 1.7 3 -228.6 1.9 3 16.4 0.16 -14.6 -15.4 -13.9 4.7 0.3164 0.0442 0.0022 0.0000 0.0002 0.0000 0.3721 0.0853 0.0308 0.0000 0.0007 0.0000 0.1440 0.0036 0.0005 79.25 0.5 8111 7973 8240 -242.5 0.5 2 -244.2 4.6 2 -236.9 1.5 3 -229.5 2.4 2 17.1 0.18 -15.2 -16.0 -14.4 4.7 0.3279 0.0376 0.0024 0.0000 0.0003 0.0000 0.3686 0.0744 0.0351 0.0000 0.0009 0.0000 0.1480 0.0044 0.0005 79.75 0.5 8167 8015 8333 -248.8 1.8 2 -244.3 1.3 2 -237.8 0.3 2 -230.4 0.5 2 24.5 0.19 -21.3 -22.3 -20.2 4.4 0.3799 0.0350 0.0026 0.0000 0.0004 0.0000 0.3460 0.0626 0.0245 0.0000 0.0014 0.0000 0.1421 0.0049 0.0006 80.25 0.5 8214 8048 8395 -251.9 1.5 2 -253.8 0.4 2 -250.3 0.7 2 -241.0 1.6 2 14.6 0.13 -13.2 -13.8 -12.5 4.9 0.3877 0.0397 0.0024 0.0000 0.0005 0.0000 0.3055 0.0902 0.0166 0.0008 0.0017 0.0000 0.1502 0.0047 0.0000 80.75 0.5 8260 8080 8456 -262.6 NaN 1 -261.1 NaN 1 -249.6 NaN 1 -237.2 NaN 1 34.5 0.00 -29.5 -31.0 -28.1 4.6 0.3866 0.0452 0.0028 0.0004 0.0005 0.0000 0.3038 0.0958 0.0180 0.0007 0.0016 0.0000 0.1401 0.0045 0.0000 81.25 0.5 8307 8114 8511 -252.6 0.8 2 -221.8 1.5 2 -234.7 2.8 2 -224.6 0.5 2 37.5 0.14 -31.8 -33.4 -30.5 4.2 0.4511 0.0434 0.0027 0.0000 0.0006 0.0000 0.2784 0.0760 0.0085 0.0006 0.0018 0.0000 0.1330 0.0035 0.0005 81.75 0.5 8354 8149 8567 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 4.0 0.4832 0.0408 0.0027 0.0005 0.0006 0.0000 0.2428 0.0890 0.0070 0.0007 0.0021 0.0000 0.1275 0.0029 0.0000 82.25 0.5 8402 8186 8624 -261.2 NaN 1 -228.9 NaN 1 -239.8 NaN 1 -231.8 NaN 1 39.7 0.00 -33.4 -35.1 -31.8 3.5 0.5520 0.0000 0.0036 0.0000 0.0007 0.0000 0.2548 0.0502 0.0079 0.0000 0.0022 0.0000 0.1243 0.0038 0.0004 82.75 0.5 8450 8224 8681 -254.9 3.5 2 -248.9 1.5 2 -241.2 2.0 2 -234.3 1.6 2 27.6 0.42 -23.9 -25.2 -22.6 4.9 0.4309 0.0373 0.0031 0.0004 0.0007 0.0000 0.2854 0.0721 0.0090 0.0007 0.0019 0.0000 0.1542 0.0039 0.0004 83.25 0.5 8498 8268 8726 -265.1 7.5 2 -252.4 9.7 2 -250.9 4.6 2 -244.3 0.9 2 28.4 0.81 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 83.75 0.5 8545 8312 8772 -254.9 2.5 3 -239.4 2.6 3 -242.2 2.9 3 -242.3 3.7 3 17.0 0.31 -15.1 -16.0 -14.3 4.8 0.4391 0.0372 0.0026 0.0005 0.0006 0.0000 0.2743 0.0844 0.0068 0.0006 0.0017 0.0000 0.1496 0.0027 0.0000 84.25 0.5 8593 8359 8812 -262.8 0.8 2 -256.1 0.9 2 -258.2 1.2 2 -247.1 0.8 2 21.2 0.10 -18.4 -19.4 -17.6 3.9 0.5222 0.0286 0.0021 0.0000 0.0005 0.0000 0.2586 0.0430 0.0055 0.0000 0.0014 0.0000 0.1346 0.0030 0.0004 84.75 0.5 8641 8405 8852 -262.3 1.7 2 -252.2 1.5 2 -253.0 2.1 2 -243.4 1.0 2 25.7 0.19 -22.3 -23.4 -21.3 4.7 0.3177 0.0437 0.0040 0.0024 0.0000 0.0000 0.3475 0.1078 0.0305 0.0000 0.0006 0.0000 0.1423 0.0034 0.0000 85.25 0.5 8688 8458 8893 -261.5 NaN 1 -243.5 NaN 1 -250.1 NaN 1 -257.4 NaN 1 5.6 0.00 -5.7 -5.9 -5.4 3.9 0.5048 0.0367 0.0024 0.0000 0.0005 0.0000 0.2504 0.0656 0.0060 0.0005 0.0015 0.0000 0.1280 0.0036 0.0000 85.75 0.5 8734 8511 8933 -265.8 2.5 2 -229.7 4.0 2 -234.9 2.1 2 -235.4 0.7 2 41.4 0.42 -34.9 -36.6 -33.1 3.7 0.5070 0.0397 0.0028 0.0000 0.0005 0.0000 0.2630 0.0508 0.0059 0.0004 0.0010 0.0000 0.1243 0.0038 0.0007 86.25 0.5 8781 8572 8966 -242.7 21.7 2 -257.9 0.1 2 -243.0 3.9 3 -239.9 2.8 2 3.7 0.34 -4.1 -4.6 -3.6 3.8 0.4948 0.0390 0.0032 0.0000 0.0005 0.0000 0.2632 0.0622 0.0067 0.0003 0.0010 0.0000 0.1247 0.0044 0.0000 86.75 0.5 8829 8632 8999 -273.3 0.3 2 -270.8 4.3 3 -277.5 2.3 3 -266.4 2.7 3 9.4 0.10 -8.8 -9.1 -8.3 3.6 0.4706 0.0303 0.0028 0.0003 0.0005 0.0000 0.3524 0.0000 0.0063 0.0002 0.0005 0.0000 0.1321 0.0041 0.0000 87.25 0.5 8874 8706 9035 -284.4 1.2 2 -283.3 2.0 3 -289.9 0.3 3 -276.6 1.7 3 10.8 0.08 -9.9 -10.4 -9.4 3.7 0.4457 0.0000 0.0019 0.0000 0.0005 0.0000 0.4037 0.0000 0.0054 0.0000 0.0004 0.0000 0.1384 0.0039 0.0003 87.75 0.5 8919 8779 9071 -285.8 0.2 2 -284.2 2.7 3 -289.3 0.8 3 -280.0 0.8 3 8.1 0.02 -7.7 -8.1 -7.4 4.3 0.4151 0.0345 0.0023 0.0000 0.0007 0.0000 0.3868 0.0000 0.0070 0.0000 0.0005 0.0000 0.1483 0.0047 0.0000 88.25 0.5 8947 8802 9102 -279.3 1.2 2 -281.6 4.0 3 -286.4 3.0 3 -274.1 3.4 3 7.3 0.10 -7.1 -7.5 -6.8 4.9 0.3801 0.0414 0.0028 0.0000 0.0007 0.0000 0.3980 0.0000 0.0084 0.0000 0.0005 0.0000 0.1617 0.0066 0.0000 88.75 0.5 8975 8825 9133 -284.1 0.5 2 -282.6 2.6 3 -287.1 0.4 3 -275.6 1.7 3 11.8 0.07 -10.9 -11.4 -10.4 5.0 0.3710 0.0350 0.0026 0.0000 0.0008 0.0000 0.4082 0.0000 0.0090 0.0000 0.0007 0.0000 0.1645 0.0079 0.0004 89.25 0.5 9003 8851 9161 -280.9 3.2 2 -280.0 2.7 3 -289.2 0.5 3 -277.6 0.4 3 4.6 0.05 -4.9 -5.1 -4.7 5.1 0.3603 0.0315 0.0026 0.0000 0.0007 0.0000 0.4192 0.0000 0.0084 0.0000 0.0005 0.0000 0.1691 0.0077 0.0000 89.75 0.5 9031 8877 9188 -287.6 0.4 2 -287.6 0.4 2 -292.8 0.1 2 -284.6 0.3 2 4.3 0.01 -4.6 -4.8 -4.5 4.9 0.3736 0.0320 0.0033 0.0000 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9.9 5.0 0.4387 0.0309 0.0054 0.0000 0.0012 0.0000 0.3374 0.0000 0.0125 0.0000 0.0013 0.0000 0.1608 0.0118 0.0000 92.75 0.5 9198 9086 9360 -277.6 0.1 2 -278.6 1.7 3 -285.3 1.4 3 -279.4 3.1 3 -2.4 0.03 0.9 0.8 1.0 5.0 0.4560 0.0310 0.0047 0.0000 0.0010 0.0000 0.3199 0.0000 0.0134 0.0000 0.0009 0.0000 0.1603 0.0129 0.0000 93.25 0.5 9230 9120 9388 -284.0 1.1 2 -284.4 1.0 3 -290.8 3.8 3 -282.6 1.4 3 2.0 0.01 -2.8 -2.8 -2.7 6.1 0.4151 0.0000 0.0037 0.0000 0.0011 0.0000 0.3568 0.0000 0.0120 0.0000 0.0010 0.0000 0.1973 0.0119 0.0011 93.75 0.5 9261 9155 9417 -237.8 1.8 2 -280.1 1.0 2 -286.3 1.4 2 -279.0 2.1 2 -54.0 0.58 NaN NaN NaN 5.5 0.4286 0.0245 0.0043 0.0000 0.0010 0.0000 0.3402 0.0000 0.0115 0.0000 0.0009 0.0000 0.1778 0.0112 0.0000 94.25 0.5 9296 9178 9448 -251.7 NaN 1 -286.0 NaN 1 -301.9 NaN 1 -284.3 NaN 1 -43.6 0.00 NaN NaN NaN 6.0 0.4111 0.0200 0.0048 0.0000 0.0010 0.0000 0.3455 0.0000 0.0123 0.0000 0.0010 0.0000 0.1926 0.0118 0.0000 94.75 0.5 9330 9202 9480 -247.5 2.0 2 -291.2 2.3 2 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