# Santa Barbara Basin Stable Isotope, Geochemistry, and Lithology Data from Marine Isotope Stage 16-15 Boundary at 631.5 ka #----------------------------------------------------------------------- # World Data Center for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # 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/ # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/by_contributor/dean2015/dean2015-11jpc-icp.txt # # Archive: Paleoceanography # # Parameter_Keywords: carbon isotopes, geochemistry, oxygen isotopes, lithology #--------------------------------------- # Contribution_Date # Date: 2016-01-20 #--------------------------------------- # Title # Study_Name: Santa Barbara Basin Stable Isotope, Geochemistry, and Lithology Data from Marine Isotope Stage 16-15 Boundary at 631.5 ka #--------------------------------------- # Investigators # Investigators: Dean, W.E.; Kennett, J.P.; Behl, R.J.; Nicholson, C.; Sorlien, C.C. #--------------------------------------- # Description and Notes # Description: Cores # Core MV0508-19JPC (lat. 34.25042 deg. N; long. 119.76428 deg. W; water depth 135 m; hereafter referred to as "19JPC") is one of a suite of 32 jumbo piston cores ranging in length from 3 to 5.5 m collected in Santa Barbara Basin during a 2005 R/V Melville cruise (MV0508). These cores sampled progressively older dipping seismic stratigraphic reflectors that crop out across the submerged flank of an actively growing anticline as described by Nicholson et al. (2006), and Marshall (2012). Many of these cores that date as old as 735 ka exhibit alternating laminated (varved) and massive (bioturbated) sediment. Results of three of these cores (11JPC, ~293 ka), 16JPC (~450 ka), and 20JPC (~735 ka) are reported by Afshar (2011) and White et al. (2013). Upon recovery, each core was cut into 1.5-m-long sections. Each section was then run through a GEOTEK Multi-Sensor core logger at 1-cm intervals for measurements of P-wave velocity, magnetic susceptibility, and gamma-ray attenuated porosity, which was calibrated to yield wet bulk density. Each core section was then cut longitudinally, described, and stored on board under refrigeration. The 2005 Melville cores are stored in the core repository at Oregon State University # Dating and Sedimentation Rate # Approximate ages for 19JPC and other MV0508 cores were first assigned based on their stratigraphic position within a series of well-defined seismic sequence boundaries. The ages of these boundaries were estimated assuming relatively constant sedimentation rates between dated stratigraphic reference horizons that were correlated and mapped across the basin to seafloor outcrops and industry wells using multichannel and high-resolution USGS deep-towed chirp data (Nicholson et al., 2006; Marshall, 2012). These preliminary ages were later refined by correlating glacial-interglacial patterns in the oxygen-isotope records of the surface-dwelling planktic foraminifer Globigerina bulloides of each core with the “LR04” stacked global benthic oxygen isotope record of Lisiecki and Raymo (2005). Additional age control was provided by diatom, coccolith and planktic foraminiferal biostratigraphic datums (Afshar, 2011; White et al., 2013). By this method, the glacial-interglacial oxygen-isotope transition in core 19JPC at 105 cm was correlated with the MIS 16-MIS 15 boundary in the stacked benthic record of Lisiecki and Raymo (2005). This boundary, also known as Termination VII, marks the first time during the Quaternary that global climate transitioned from extremely cold glacial climate and low sea-levels (high d18O; MIS 16) to warm conditions and high sea levels of a following interglacial (low d18O; MIS 15). # A linear sedimentation rate through the core was estimated using varve thickness measurements. Digital images (grayscale) of scraped split faces of each core section were acquired using a line scanner mounted on a multi-sensor track at Oregon State University core repository. The images were analyzed using NIH Image J software to determine an average linear sedimentation rate by counting laminations within minimally disturbed intervals using grayscale contrast of the light-dark couplets (Escobedo, 2009), assuming that these are annual layers, i.e., varves, as demonstrated by Schimmelmann et al. (2006) for younger sediment in SBB. Core 19JPC is only intermittently laminated, so Escobedo (2009) counted the laminations in three distinctly laminated sections of 19JPC and determined sedimentation rates of 76 cm/kyr (at 231 cm), 120 cm/kyr (at 303 cm), and 94 cm/kyr (at 305 cm), with an average of 97 cm/kyr for the 4-kyr interval recorded in 19JPC . Varve counts were also made on two nearby cores (Fig. 1A) with more abundant laminations, 11JPC (~293ka; 80 cm/kyr) and 20JPC (~735 ka; 82 cm/kyr) (Escobedo; 2009), yielding similar sedimentation rates; these are all consistent with bathyal sedimentation rates (about 100 cm/kyr) determined in other SBB investigations based on biostratigraphy, oxygen isotope stratigraphy, tephrochronology, and seismic stratigraphy (Nicholson et al., 2006; Behl et al., 2007; Marshall, 2012; White et al., 2013). # Carbon Analyses # A total of 181 samples were analyzed for weight percentages of total carbon (TC) and total inorganic carbon (IC) using a carbon-dioxide coulometer (Engleman et al., 1985) in the laboratories of California State University, Long Beach, CA (CSULB). For details of the method used at CSULB, see Afshar (2011). Percent total organic carbon (TOC) was calculated as the difference (TC – TIC). Percent CaCO3 was calculated as # CaCO3 = IC/0.12, # where 0.12 is the weight fraction of carbon in CaCO3. The accuracy for both TOC and CaCO3, determined by comparison with standards is ±0.58 wt. %; the precision of TOC and CaCO3 are ±0.05 wt. % and ±0.47 wt. %, respectively (Afshar, 2011). # # Oxygen and Carbon Isotopes # Stable-isotope analyses of oxygen and carbon were made on 406 samples, including duplicates, of the surface-dwelling planktic foraminifer Globigerina bulloides collected from 19JPC at 1-cm intervals. Limited intervals of special interest were also analyzed for the isotopic composition of other species to characterize different depths in the water column. Between 5 and 15 foraminifera were picked for each stable isotopic analysis, which was performed on a Finnegan MAT 251 mass spectrometer in the isotope laboratory at the University of California, Santa Barbara following standard preparation techniques. Instrumental precision was <0.09 ‰ for both isotopes; all data are expressed as standard delta notation in per mil (‰) relative to the Vienna Pee Dee Belemnite (VPDB) standard as related to repeated analysis of NBS-19 and NBS-20 (Coplen, 1997): # delta ‰=[(Rsample/RVPDB)-1]×103 # where R is the ratio (13C: 12C) or (18O: 16O). # # Inorganic Geochemistry # A total of 116 samples from 11JPC, 97 samples fro 20JPC, and 112 samples from 19JPC were analyzed for 40 major, minor, and trace elements by a combination of inductively coupled plasma optical emission spectrometry (ICP-OES) and ICP mass spectrometry (ICP-MS) at SGS Minerals Services in Toronto, Canada. Samples were digested in a sequential acid leach with HNO3, HCl, HF, and HClO4 and heated until dry. The residue was then dissolved in HNO3 and HCl. Accuracy of the ICP-MS method was determined by what SGS calls a Measurement Uncertainty (MU) for each element at various concentration ranges. The estimated MU is assessed using the reference material uncertainty from the certificate of analysis, the uncertainty of the laboratory bias, the uncertainty of the long-term contribution, and the uncertainty from the precision of replicate samples or duplicate samples for a period of greater than three months. The MU is the relative percent of the amount present. For Mo in 19JPC in the range of 1-3 ppm the MU is 10.1% so for a sample containing 2 ppm Mo, the uncertainty is 2±0.20 ppm. For U in the range of 1-10 ppm the MU is 16.6% so for a sample containing 5 ppm U, the uncertainty is 5±0.83 ppm. For all 40 elements in the 19JPC data set, the average MU is 15.4%, ranging from 7.1% (Ca) to 32.1% (Cu). For the precision of this data set, the average percent difference between duplicate analyses for each element was 3.1% (range: 0-3.9%). # # REFERENCES: # Afshar, D.S., 2011, High-resolution windows into abrupt and millennial-scale changes in climate and ocean since the mid-Pleistocene transition, Santa Barbara Basin, California. MS Thesis, California State University, Long Beach, 134 p. # Behl, R. J., Escobedo, D. K., Kennett, J. P., Nicholson, C., and Sorlien, C. C., 2007, Decadal to Million-Year Sedimentation Rates and the Ultra-High-Resolution Marine Record From Santa Barbara Basin. . Eos Trans. AGU, 88(52), Jt. Assem.. Suppl., Abstract PP41C-0677. # Coplen, T.B., 1997, Editorial: More uncertainty than necessary, Paleoceanography, 11, 369-370. # Engleman, E.E., Jackson, L.L., Norton, D.R., Fischer, A.G., 1985, Determination of carbonate carbon in geological materials by coulometric titration, Chem. Geol., 53, 125-128. # Escobedo, D.K., 2009, Extreme erosional events recorded by flood deposits in the Late Quaternary Santa Barbara Basin, coastal southern California, MS Thesis, California State University, Long Beach, 101 p. # Lisiecki, L.E., and Raymo, M. E., 2005 A Pliocene-Pleistocene stack of 57 globally distributed benthic ?18O records, Paleoceanography , 20, PA1003, doi:10.1029/2004PA001071. # Marshall, C. J., 2012, Sedimentation in an active fold and thrust belt, from 1 Ma to present, Santa Barbara Channel, California, MS Thesis, California State University, Long Beach, 94 p. # Nicholson, C., Kennett, J., Sorlien,C., Hopkins, S., Behl, R., Normark, SW., Sliter, R., Hill, T., Pak, D., Schimmelmann, A., and Cannariato, K., 2006, Santa Barbara Basin study extends global climate record, EOS (Trans. Am. Geophys. Union), 87, n. 21, 205, 208. # Schimmelmann, A., Lange, C. B., Roark, E. B., and Ingram, B. L., 2006, Resources for paleoceanographic and paleoclimatic analysis: A 6, 700-year stratigraphy and regional radiocarbon reservoir-age (AR) record based on varve counting and C-14-AMS dating for the Santa Barbara Basin, offshore California, USA, J. Sed. Res., 76, 74-80 # White, S.M., Hill, T. M., Kennett, J. P., Behl, R. J., and Nicholson, C., 2013, Millennial-scale variability to 735 ka: High-resolution climate records from Santa Barbara Basin, CA, Paleoceanography, 28, 213-226, doi: 10.1002/palo.20022. #--------------------------------------- # Publication # Authors: Dean, W.E., J.P. Kennett, R.J. Behl, C. Nicholson, and C.C. Sorlien # Published_Date_or_Year: 2015 # Published_Title: Abrupt termination of Marine Isotope Stage 16 (Termination VII) at 631.5ka in Santa Barbara Basin, California # Journal_Name: Paleoceanography # Volume: 30 # Issue: # Pages: 1373-1390 # Report Number: # DOI: 10.1002/2014PA002756 # Full_Citation: # Abstract: The Marine Isotope Stage 16-15 boundary (Termination VII) is the first deglacial warming step of the late Quaternary following the mid-Pleistocene transition (MPT), when 41?kyr climatic cycles shifted to strong 100?kyr cycles. The detailed structure of this important climatic event has remained unknown until now. Core MV0508-19JPC from Santa Barbara Basin, California, contains a decadal-scale climatic and geochemical sediment record of 4000?years duration that includes the early part of this deglacial episode. This record reveals that the climatic shift during the early deglacial occurred rapidly (<700?years), in a progression of three abrupt warming steps. The onset of Marine Isotope Stage (MIS) 15 was remarkably abrupt with 4-5°C sea surface warming in ~50?years. The deglacial sequence contains the well-dated Lava Creek tephra (631.3?±?4?ka) from Yellowstone Caldera used to date the onset of Termination VII at 631.5?ka. The late MIS 16 and early MIS 15 interval exhibits multiple decadal-scale negative excursions in d13C of planktic foraminifera, likely the result of repeated discharges of methane from methane hydrates associated with both ocean warming and low sea level. A warm interstadial that interrupts late MIS 16 is marked by elevated concentrations of redox-sensitive elements indicating sulfidic, oxygen-deficient bottom and pore-waters, and elevated concentrations of total organic carbon and Cd, reflecting increased surface productivity. Unlike younger sediments on the California margin, these indicators of increased productivity and low dissolved oxygen do not consistently correspond with each other or with preserved laminations, possibly reflecting instability of a still evolving ocean-atmosphere system following the MPT. #--------------------------------------- # Publication # Authors: Nicholson, C., J. Kennett, C. Sorlien, S. Hopkins, R. Behl, W. Normark, R. Sliter, T. Hill, D. Pak, A. Schimmelmann, and K. Cannariato # Published_Date_or_Year: 2006 # Published_Title: Santa Barbara Basin study extends global climate record # Journal_Name: EOS # Volume: 87 # Issue: 21 # Pages: 205-207 # Report Number: # DOI: 10.1029/2006EO210001 # Full_Citation: # Abstract: #--------------------------------------- # Publication # Authors: White, S.M., T.M. Hill, J.P. Kennett, R.J. Behl, and C. Nicholson # Published_Date_or_Year: 2013 # Published_Title: Millennial-scale variability to 735 ka: High-resolution climate records from Santa Barbara Basin, CA # Journal_Name: Paleoceanography # Volume: 28 # Issue: # Pages: 213-226 # Report Number: # DOI: 10.1002/palo.20022 # Full_Citation: # Abstract: #--------------------------------------- # Funding_Agency # Funding_Agency_Name: # Grant: #--------------------------------------- # Site Information # Site_Name: MV0508-11JPC # Location: Eastern Pacific Ocean # Country: Santa Barbara Basin # Northernmost_Latitude: 34.250333 # Southernmost_Latitude: 34.250333 # Easternmost_Longitude: -119.764333 # Westernmost_Longitude: -119.764333 # Elevation: -120 #--------------------------------------- # Data_Collection # Collection_Name: 11JPC Dean16 # First_Year: # Last_Year: # Time_Unit: # Core_Length: # Notes: Results of this core were reported in White et al. (2013). #--------------------------------------- # 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) ## depth_cm depth,,,cm,,,,,N ## Al% aluminum,,,percent,,,,,N ## Ca% calcium,,,percent,,Paleoceanography,,,N ## Mg% magnesium,,,percent,,Paleoceanography,,,N ## F% iron,,,percent,,Paleoceanography,,,N ## Na% sodium,,,percent,,Paleoceanography,,,N ## K% potassium,,,percent,,Paleoceanography,,,N ## Ti% titanium,,,percent,,Paleoceanography,,,N ## S% sulfur,,,percent,,Paleoceanography,,,N ## P-ppm phosphorus,,,ppm,,Paleoceanography,,,N ## Mn-ppm manganese,,,ppm,,Paleoceanography,,,N ## Ba-ppm barium,,,ppm,,Paleoceanography,,,N ## Sr-ppm strontium,,,ppm,,Paleoceanography,,,N ## Cr-ppm chromium,,,ppm,,Paleoceanography,,,N ## Cu-ppm copper,,,ppm,,Paleoceanography,,,N ## Co-ppm cobalt,,,ppm,,Paleoceanography,,,N ## Mo-ppm molybdenum,,,ppm,,Paleoceanography,,,N ## Cd-ppm cadmium,,,ppm,,Paleoceanography,,,N ## Ce-ppm cesium,,,ppm,,Paleoceanography,,,N ## Ni-ppm nickel,,,ppm,,Paleoceanography,,,N ## V-ppm vanadium,,,ppm,,Paleoceanography,,,N ## Zn-ppm zinc,,,ppm,,Paleoceanography,,,N ## Zr-ppm zirconium,,,ppm,,Paleoceanography,,,N ## Ag-ppm silver,,,ppm,,Paleoceanography,,,N ## As-ppm arsenic,,,ppm,,Paleoceanography,,,N ## Ga-ppm gallium,,,ppm,,Paleoceanography,,,N ## Nb-ppm niobium,,,ppm,,Paleoceanography,,,N ## Pb-ppm lead,,,ppm,,Paleoceanography,,,N ## Rb-ppm rubidium,,,ppm,,Paleoceanography,,,N ## Sb-ppm antimony,,,ppm,,Paleoceanography,,,N ## Sc-ppm scandium,,,ppm,,Paleoceanography,,,N ## Th-ppm thorium,,,ppm,,Paleoceanography,,,N ## U-ppm uranium,,,ppm,,Paleoceanography,,,N ## Y-ppm yttrium,,,ppm,,Paleoceanography,,,N ## Yb-ppm ytterbium,,,ppm,,Paleoceanography,,,N #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: depth_cm Al% Ca% Mg% F% Na% K% Ti% S% P-ppm Mn-ppm Ba-ppm Sr-ppm Cr-ppm Cu-ppm Co-ppm Mo-ppm Cd-ppm Ce-ppm Ni-ppm V-ppm Zn-ppm Zr-ppm Ag-ppm As-ppm Ga-ppm Nb-ppm Pb-ppm Rb-ppm Sb-ppm Sc-ppm Th-ppm U-ppm Y-ppm Yb-ppm 2 7.21 2.32 3.31 2.73 2.49 1.17 0.36 0.79 1140 305 736 300 68 19.6 9.5 3.12 0.53 58.2 31.6 94 80 27.4 0.23 12 20.4 12.3 13.6 105 0.84 9.1 8.8 3.1 17.7 1.8 7 7.38 2.44 2.91 2.76 2.55 1.08 0.35 0.83 1120 301 842 317 59 17.1 9.2 1.7 0.35 62.2 27.4 87 74 25 0.17 6 21 12.5 14.1 108 0.77 8.8 9.5 2.8 18.2 1.9 12 6.59 2.39 3.04 2.67 2.57 0.84 0.29 0.76 1150 243 864 315 67 11.4 5.8 1.95 0.28 45.1 19.9 66 54 21.8 0.03 7 17.3 9.6 11 94.9 0.77 7 7.8 2.3 20.2 1.6 17 6.75 2.03 2.61 2.74 2.61 0.77 0.28 0.61 1120 237 907 309 52 11 5.5 2.06 0.43 44.6 20.3 64 53 21.8 0.02 8 17.1 9.4 11.2 91.9 0.85 6.5 6.9 2.5 18.2 1.5 22 6.9 2.23 2.79 2.68 2.51 0.89 0.31 0.82 1110 256 1110 310 56 14.4 7.7 5.68 0.44 57.9 24.3 75 61 23 0.14 9 19.7 11.7 13.4 100 0.8 8.3 8.2 3.6 18.6 1.9 27 6.56 2.06 3.76 2.6 2.7 0.92 0.3 0.84 1450 252 1220 312 68 12.5 7.3 8.42 0.45 69.5 20.6 75 59 23 0.1 14 20 11.8 13 103 0.86 8.7 9.5 3.8 22.8 2.2 32 7.72 2.44 3.9 2.56 2.5 1.45 0.42 1.47 1110 334 622 270 68 29.1 11.6 7.95 0.73 67.8 39.7 124 101 31.1 0.18 10 23.9 14.6 15.2 120 1.48 11.7 11.3 5.4 20.2 2.5 37 7.84 2.17 3.66 2.54 2.54 1.51 0.42 1.13 1100 342 611 260 78 29.4 12.4 6.83 0.88 70.5 41 134 105 31.7 0.18 8 25.6 15.4 16 134 1.62 12.3 11.7 4.8 21.2 2.2 42 7.6 2.33 3.66 2.54 2.49 1.44 0.41 1.24 1050 322 600 254 73 30.4 11.6 6.51 0.89 69.5 39.1 130 100 29.6 0.26 10 25.1 15 15.8 128 1.44 12 11.6 4.5 20.6 2.1 47 7.82 2.65 3.74 2.55 2.54 1.64 0.42 1.13 1020 332 574 260 82 33.3 12.5 5.56 1.28 68.6 46 152 111 32.8 0.25 9 25.5 14.4 16.1 130 1.63 12.6 11.9 6.3 20.4 2.2 52 7.59 2.4 3.73 2.64 2.44 1.54 0.41 1.41 1030 324 587 261 75 32.5 12 9.51 1.1 68.8 46.7 150 106 32.3 0.23 10 25 14.5 15.8 127 1.14 12.2 11.3 5.6 20.4 2.1 57 7.67 3.56 4.17 2.33 2.48 1.63 0.41 2.12 970 335 507 276 80 33 13.4 9.23 1.19 72.5 43.6 158 113 32.7 0.26 12 26.2 15.1 16.3 139 3.35 13.3 12.5 6.4 21.2 2.2 62 7.48 2.66 3.48 2.53 2.46 1.46 0.41 1.54 1050 313 583 257 77 31.3 10.6 8.82 1.17 63.2 42.6 140 104 30.9 0.25 9 22.8 13.8 14.4 120 1.22 11 10.9 4.6 18.5 1.9 67 8.34 1.27 4.17 2.71 2.73 1.59 0.46 1.45 1130 341 652 235 84 35.1 14.1 32.2 2.23 80.3 50.8 162 122 34.1 0.25 13 28.2 17 18.1 146 1.77 13.5 13.3 4.9 22.4 2.2 72 7.17 2.58 3.45 2.49 2.32 1.48 0.39 1.22 1010 306 552 256 81 31.7 11.2 13.5 1.84 63.6 46.1 148 105 29.7 0.21 10 22.9 13.8 14.5 117 1.64 11.3 11 7.2 20.8 2.2 77 7.9 1.83 3.75 2.65 2.57 1.54 0.36 1.53 1030 328 601 242 80 36.4 10.6 18.5 2.2 58.7 49.2 131 117 24.6 0.21 8 24 3.5 13.8 130 0.69 11.7 11.7 5.2 21.4 1.8 82 7.8 1.74 3.93 2.59 2.55 1.53 0.43 1.8 1070 331 594 240 80 34.5 13.6 27.2 3.06 70.7 48.9 152 115 31 0.3 13 26 15.3 15.9 135 2.08 13 12.2 5.3 21.3 2.1 87 7.66 1.18 3.94 2.54 2.51 1.53 0.42 1.64 1030 320 583 215 88 36.5 10.8 21.5 2.88 56.9 52.6 155 117 32.9 0.15 10 23.7 13.4 13 122 2.02 11.5 11.6 4.8 20.1 1.7 92 7.62 2.59 3.8 2.62 2.49 1.56 0.41 1.52 990 333 551 265 82 34.7 12.2 12.9 1.85 69.6 49.4 155 107 31.8 0.24 12 25.1 15 14.9 128 1.96 12.5 11.8 7.8 22.1 2.4 97 7.87 1.93 3.82 2.64 2.56 1.59 0.44 1.71 1040 324 782 247 68 38.1 13.2 17.4 3.01 71.3 50.4 166 121 32.5 0.26 10 25.9 16.4 16.2 136 1.38 12.9 12.2 5.8 19.8 2 102 7.69 3.05 3.72 2.48 2.48 1.64 0.42 1.19 1090 331 583 276 83 37.2 12.3 13.6 2.15 69.1 49.3 175 119 32.3 0.29 10 24.6 14.5 15.4 128 1.79 12.6 12.2 9.5 21.4 2.2 107 8.22 1.55 4.15 2.54 2.67 1.63 0.45 1.47 1010 333 594 228 78 38.8 12.6 28.6 2.12 68.3 49.4 170 123 33.2 0.3 15 25.2 14.9 16.4 135 4.15 12.1 12 6.3 18.3 1.8 112 7.78 1.76 3.65 2.71 2.56 1.52 0.41 1.43 1090 325 606 238 80 36.1 11.7 15.8 2.25 64.5 48.4 152 113 30.8 0.38 11 23.6 12.7 15.6 122 1.25 11.3 11.1 5.9 20.6 2.1 116 7.63 1.84 2.93 2.69 2.59 1.16 0.37 0.98 1100 301 728 273 64 24.6 9.4 6.61 0.99 66.1 32.6 108 84 26.7 0.22 9 21.3 10.7 14.7 113 0.93 9.6 10.7 4.6 19.7 1.9 118 7.4 2.03 2.85 2.76 2.5 1.12 0.38 1.04 1160 299 701 279 69 23.2 9.1 8.87 1 68.7 32 105 79 28.5 0.22 11 21.7 13.5 14.4 111 1.25 9.6 11 5.3 21.3 2.2 122 7.32 1.46 3.64 2.67 2.41 1.54 0.41 1.56 1060 312 528 212 88 35.9 11.6 18.5 2.32 69 52.7 165 114 32.6 0.31 10 22.3 14.6 15 125 1.75 12.3 11.9 6.6 20.8 2.2 126 7.39 1.12 3.39 2.75 2.43 1.49 0.4 1.33 1000 302 549 208 81 34.9 11.9 20.8 2.48 68.4 50.8 162 114 31.4 0.37 9 22 15 15.4 128 2.01 12.1 11.8 6.1 20.4 2.1 130 7.47 1.29 3.37 2.74 2.48 1.54 0.31 1.17 990 310 571 213 78 34.8 11.4 12.4 1.79 68.8 46.3 136 109 25.1 0.26 9 22.3 4.5 16 128 1.96 12.2 11.7 5.4 20.2 2.1 134 7.13 1.38 3.54 2.67 2.37 1.39 0.39 1.45 1050 293 566 221 80 31.4 10.1 20.8 1.79 62.7 46.1 142 103 30.2 0.27 14 19.8 13.1 13.5 111 1.67 10.6 10.4 4.9 18.7 1.9 137 7.68 1.21 3.52 2.63 2.55 1.52 0.42 1.14 1040 304 587 220 78 34.3 10 19.9 1.32 56.4 47.6 158 111 31.4 0.17 7 20.8 11.5 13.2 123 1.23 11.6 12 5.1 20.8 1.8 140 7.25 1.18 4.14 2.49 2.49 1.39 0.38 1.79 1100 298 571 216 90 32.8 10.9 55.5 2.63 66.7 45.3 146 109 30.4 0.27 14 20 13.5 14.6 119 2.21 11.2 11.3 5.8 20.1 2.1 143 6.87 1.12 3.46 2.57 2.27 1.35 0.38 1.8 1080 284 538 208 79 36 9.3 57.1 3.8 52.2 56.9 156 113 31.9 0.23 15 18.2 11.6 11.4 107 2.33 10.1 10.7 6.7 20.3 1.8 146 6.77 2.48 3.21 2.68 2.25 1.35 0.37 1.44 1150 287 516 252 73 36.5 8.5 30.1 2.73 51.1 53.5 152 112 28.9 0.22 8 17.7 11.5 11 104 1.57 9.9 10 9.5 21.4 1.9 149 6.79 2.16 3.08 2.62 2.26 1.36 0.37 1.25 1070 287 538 237 78 33.5 10.6 27.3 2.93 63.7 50 150 108 28.3 0.33 9 19.8 13.5 13.5 113 1.59 10.9 11.9 8.1 20 2 152 7.46 1.58 3.64 2.65 2.47 1.5 0.36 1.61 1020 308 551 214 78 34.9 11.8 26.1 3.04 68.2 50.4 150 116 24.8 0.3 11 21.8 4 15.3 127 1.94 11.7 11.8 5 19.3 1.9 156 7.04 2.82 3.32 2.73 2.35 1.46 0.39 1.36 1020 299 525 256 82 33.5 10.9 21.6 2.78 62 48.9 153 108 30.2 0.33 11 20.1 13.4 13.4 114 2.02 11 10.7 7.6 19.1 2 160 6.23 2.58 2.87 2.87 2.11 1.28 0.34 1.39 980 262 482 243 69 32.9 9.1 19.4 3.07 52.3 48.5 136 96 26.7 0.37 11 17.1 9.9 11.7 101 1.47 9.3 8.7 6.2 17.7 1.8 163 6.59 3.97 3.03 2.56 2.24 1.48 0.36 1.29 1030 282 532 295 74 32 9.1 17.8 2.3 55.2 47 146 106 28.3 0.3 8 16.9 11.6 11.9 102 1.48 9.6 9.5 7.7 17.6 1.8 166 6.79 3.6 3.11 2.6 2.27 1.52 0.37 1.26 1010 284 539 275 71 34.5 10.1 16.9 2.5 60.3 48.6 154 105 29.2 0.37 9 19.2 12.8 13.1 111 1.43 10.5 10.3 6.3 18.5 1.9 169 5.81 7.89 2.81 2.17 1.94 2.26 0.31 1.22 1090 254 783 392 59 29.3 8.4 13.6 2.27 48 39.3 134 86 25.9 0.27 9 14.8 10.3 11.4 90 1.42 9 8.5 6.6 16.3 1.8 172 5.29 9.59 2.52 1.99 1.77 2.74 0.28 0.96 1140 223 923 416 60 27.5 6.8 16.1 2.39 37.2 38.4 133 80 24.2 0.16 5 15.6 9 8.6 86.7 1.81 7.7 7.9 4.3 14.6 1.3 177 6.03 8.26 2.92 2.05 2 3.05 0.32 1 1140 265 598 393 67 30.4 10 22.3 2.69 56.1 41.3 149 93 25.6 0.32 9 19.6 12 12.6 103 2.61 10 10 5.4 17.2 1.8 182 7.32 1.78 3.15 2.66 2.44 1.33 0.39 1.12 980 292 607 241 83 32.7 9.4 5.69 1.21 60.5 45.2 137 99 29 0.33 9 20.5 12.8 13.4 106 1.93 9.7 10.2 4.1 17.2 1.8 187 5.37 9.38 2.48 1.93 1.81 4.06 0.29 0.87 1050 244 644 460 53 28.3 8.1 14.7 3.02 44.5 37.2 122 78 23.7 0.27 7 16.1 10 9.9 84.6 1.27 8.2 8 5.2 14.8 1.5 192 7.56 2.42 3.44 2.6 2.5 1.52 0.41 1.16 970 324 577 251 89 38.3 10.1 10.2 2.21 56.7 52.5 167 114 30.3 0.22 6 22.9 13.2 12.8 126 1.72 11.3 12.1 6.9 22.1 1.9 194 7.38 2.87 3.31 2.59 2.43 1.46 0.41 1.12 1010 308 545 267 83 36.6 10.7 7.86 1.8 65.5 48 161 105 32.1 0.37 9 22.5 14 13.7 118 1.61 11.2 11.5 7.1 21.9 2.3 200 7.5 1.78 3.04 2.73 2.5 1.17 0.29 0.88 1080 292 730 275 56 21.9 9.3 4.17 0.45 69.1 34.1 86 82 22.3 0.17 16 21.5 5.8 14.2 112 2.32 9.6 11.9 3.6 20.1 2 202 7.54 2.38 3.27 2.69 2.51 1.26 0.28 1.15 1050 311 665 281 57 24.1 9.1 2.89 0.42 56.8 36.4 88 89 20.4 0.14 11 22 3.3 12.8 118 1.66 10.3 10.5 5 21.9 1.9 207 7.47 2.37 3.18 2.65 2.49 1.22 0.38 1.32 1090 312 658 279 72 23.2 9.5 4.03 0.76 64.2 35.1 110 88 27.9 0.15 11 20.2 12.4 13.8 108 1.79 9.5 10.6 4.3 18.9 2 210 7.68 1.96 3.6 2.54 2.54 1.44 0.41 1.36 1030 322 595 242 82 30.2 12.2 7.39 1.53 72 42.7 142 105 29.6 0.24 12 25.9 15.9 15.9 132 1.71 12.8 12.6 5.4 21.9 2.2 213 7.66 2.28 3.6 2.64 2.53 1.43 0.42 1.4 1010 323 589 257 74 30.7 11.5 8.08 1.77 71.4 40.6 144 103 31.7 0.23 12 24.7 14.9 15.4 128 1.53 12.1 12.6 6.1 22.3 2.3 216 7.57 1.81 3.76 2.66 2.51 1.42 0.41 1.68 1030 314 606 238 80 32.1 11.4 10.4 1.74 69.4 45 145 110 30.1 0.27 11 24.3 15.1 14.5 128 1.06 11.9 12 5.1 20.5 2 220 7.37 2.66 3.69 2.59 2.43 1.42 0.4 1.43 1000 320 570 265 74 32.7 12.2 10.2 2.35 73.7 43.4 146 112 30.4 0.31 8 25.2 15 15.4 129 1.16 12.4 12.7 7.4 22.8 2.4 223 7.42 2.21 3.39 2.58 2.43 1.38 0.36 1.34 970 311 550 243 73 32.1 11.2 7.62 1.94 69 43.4 138 108 24.8 0.28 6 23.2 5.5 14.9 123 0.96 11.3 11.7 6.1 19.9 2.1 226 7.51 2.73 3.74 2.52 2.46 1.41 0.41 1.7 960 329 564 267 76 34.1 11 9.14 1.6 66.3 46.1 144 109 29.7 0.24 12 22.2 14 14.1 115 1.24 10.8 11.4 6.1 20.4 2.2 228 7.5 2.7 3.55 2.67 2.47 1.41 0.41 1.53 930 327 563 265 75 33.6 10.6 9.06 1.94 59.6 43.4 148 107 29.1 0.14 7 23.4 13.9 13.1 126 1.34 11.5 12.8 6 22.6 2 231 7.44 2.08 3.53 2.57 2.45 1.41 0.41 1.46 960 317 571 238 70 33.7 11.2 8.31 2.38 67.8 43.2 156 109 29.6 0.25 8 23.7 14.3 14.8 120 1.2 11.4 11.8 4.7 20 2 233 7.39 2.13 3.36 2.6 2.43 1.36 0.4 1.52 990 321 626 246 74 30.9 9.8 9.52 2.21 57.8 44.6 150 104 29 0.14 5 22.3 13.5 12.4 120 1.15 10.9 12.2 4.9 21.7 1.9 236 7.66 2.42 3.47 2.61 2.51 1.48 0.41 1.32 970 334 578 254 77 33.8 12.3 7.98 2.1 70.2 44.2 157 109 30.9 0.25 5 24.8 15.4 15.8 132 1.27 12.1 12 5.7 21.1 2.2 239 7.55 2.63 3.34 2.61 2.48 1.45 0.34 1.24 1010 322 585 264 76 31.9 10.2 6.2 1.72 58 45.2 131 111 23.9 0.21 5 23.6 5.4 13.4 125 1.09 11.3 12.2 5.6 21.5 1.9 242 7.37 3.52 3.32 2.58 2.41 1.45 0.35 1.31 970 322 562 300 61 33.3 11.5 6.06 2.31 66.3 41.6 144 113 23.9 0.24 7 22.5 7.4 13.9 119 0.9 11.4 11.3 8.9 21.1 2.2 245 7.52 3.01 3.55 2.6 2.48 1.49 0.41 1.27 1040 319 594 277 82 33.2 11 6.66 1.88 63.8 44.9 158 115 30 0.24 7 22.7 13.7 14.4 122 1.01 11.6 10.9 6.6 19.5 2 248 7.45 2.82 3.55 2.47 2.43 1.49 0.4 1.28 990 316 597 263 83 35.4 11.8 7.03 1.61 63.4 46.7 162 117 29.4 0.3 10 24.1 14.4 14.3 125 1.17 12 11.4 7 19.8 2.1 251 7.36 2.5 3.59 2.6 2.42 1.44 0.4 1.42 970 315 615 255 77 33.5 10.1 8.48 1.67 56.6 46.2 152 106 30.9 0.17 7 23.2 13.6 12.7 123 1.23 11.3 12 6.3 22.4 2 254 7.87 2.44 3.84 2.4 2.54 1.55 0.42 1.41 960 334 553 242 75 36.6 13.1 6.83 1.31 74.9 42.9 151 117 30.6 0.25 11 26.3 15.2 16.7 136 2.02 12.9 13.2 5.8 21.7 2.3 257 7.15 2.65 3.68 2.46 2.31 1.31 0.37 1.28 970 303 853 258 37 28 9 5.51 0.93 57.6 37.8 138 95 40.7 0.28 6 18 11.2 12.9 104 1.52 11.9 10.2 4.2 19 1.8 259 7.05 1.4 3.43 2.41 2.36 1.27 0.36 0.89 890 282 547 226 39 25.8 8.8 3.41 0.86 59.6 31.8 117 100 28.1 0.25 8 18.1 10.4 14.1 105 1.47 11.9 10.2 3.3 18.1 1.6 261 7.06 1.57 3.8 2.44 2.4 1.29 0.37 1.33 1050 298 594 228 40 25.6 9.4 2.79 0.92 64.3 37.2 130 104 30.5 0.22 12 19.2 11.3 14.6 108 1.36 12.6 11.7 3.5 19.5 1.7 263 7.15 1.64 3.96 2.46 2.4 1.35 0.38 1.3 1080 312 576 222 40 27.4 9.9 2.32 1.02 65.1 37.4 137 103 32.2 0.21 11 19.7 12.1 13.7 118 1.39 13.4 11.6 3.9 21.1 1.8 265 7.23 1.4 3.88 2.38 2.41 1.38 0.39 1.44 1090 308 594 218 38 26.8 9.4 2.68 0.85 66.2 39.9 140 105 32.9 0.21 11 19.1 11.5 14.2 114 1.35 13.1 11.4 3.9 20.2 1.8 267 7.15 1.39 3.91 2.39 2.37 1.36 0.39 1.53 1080 311 579 220 39 26.3 9.8 2.65 0.79 67.5 37.6 141 107 34.6 0.22 11 20 12.5 14.3 121 1.33 13.8 11.9 4.1 20.9 1.8 271 8.01 1.47 3.78 2.16 2.33 1.53 0.42 1.73 1010 338 560 210 54 31.1 10.8 4.11 0.82 73.5 42.8 146 114 34.6 0.26 13 21.1 14.2 15.8 125 1.43 14.7 13.3 4.8 21.5 2 275 7.77 1.56 3.53 2.06 2.28 1.47 0.41 1.57 950 319 525 201 57 30.7 10.4 4.15 1.09 69.4 41.5 149 111 33.6 0.27 10 20.6 13.8 14.7 124 1.45 14.5 12.5 4.9 20.8 1.9 277 8.07 1.74 3.54 2.14 2.39 1.53 0.42 1.61 970 334 568 217 58 31.6 10.7 4.88 1.08 69.8 43.9 155 116 33.1 0.25 9 20.8 13.6 14.9 129 1.46 14.5 12.5 5.2 21.2 1.9 279 7.91 2.18 3.83 2.05 2.31 1.63 0.42 1.51 930 333 520 210 61 35.9 11.1 4.76 1.19 66.7 47.3 172 118 34.3 0.23 9 21.4 13.6 14.2 129 1.53 15.5 12.9 6.1 21.3 2 281 7.88 1.79 3.6 2.19 2.35 1.49 0.4 1.66 920 312 562 214 65 33.8 10.9 6.87 1.5 66 50.6 164 114 34.2 0.25 11 20.6 13.4 13.7 125 1.52 14.3 12.3 5.2 20.6 1.9 283 8.27 1.57 3.67 2.09 2.46 1.68 0.43 1.42 950 323 514 191 75 37.3 11.3 6.04 1.56 70.4 46.8 194 131 36.9 0.29 8 22.9 14.7 16.2 140 1.68 16.6 13.3 5.1 20.6 1.8 285 7.9 2.15 3.44 2.06 2.3 1.51 0.41 1.49 980 317 515 222 54 31.7 10.4 5.24 1.3 67.9 43 172 110 33.2 0.24 7 21 13.7 14.8 125 1.42 15 12.7 6 21.7 2 287 7.81 2.04 3.53 2.08 2.32 1.52 0.41 1.79 840 318 518 208 50 34.4 11 7.25 1.86 67.1 46.7 165 113 32.3 0.27 9 21 13.7 14.7 128 1.42 14.9 12.7 6.3 20.5 1.9 289 7.5 2.92 3.44 2.12 2.18 1.39 0.39 1.77 900 306 517 251 52 30.2 10.2 7.93 1.57 65.9 43 161 101 31.9 0.28 7 20 13.3 13.9 117 1.77 14 11.7 7.7 22.1 2.1 291 7.92 2.24 3.57 2.16 2.27 1.53 0.42 1.45 920 316 488 219 60 34.6 10.8 8.25 1.82 68.3 47.1 181 114 32.8 0.27 6 21.3 13.5 14.2 134 1.45 14.9 12.7 5.9 21.1 1.9 293 8.6 1.85 3.37 1.95 2.52 1.63 0.44 0.91 810 325 506 198 51 37.8 12.3 5.78 1.28 73.4 39 187 123 32.6 0.24 6 23.2 14.8 17.8 152 1.9 16.8 14.8 5.1 20.5 1.8 295 7.59 2.95 3.37 2.15 2.26 1.44 0.39 1.49 840 305 505 253 57 44 11.4 8.62 1.87 63.9 49.8 167 106 31.2 0.29 9 19.9 12.9 13.2 125 1.55 13.9 11.7 6.4 22 2 297 7.95 2.65 3.43 2.23 2.33 1.53 0.41 1.28 960 322 521 245 64 34.9 10.4 6.56 1.86 65 44.5 181 113 32.7 0.29 6 20.5 13.4 14.6 132 1.35 14.6 11.8 6.1 21.2 1.9 299 7.48 3.26 3.17 2.07 2.17 1.43 0.4 1.38 850 309 485 253 54 33.4 10.4 5.84 1.76 66.8 41 163 105 31.7 0.27 6 19.9 13.1 14 131 1.62 14.4 12.3 7.4 22.3 2 301 7.83 3.05 3.59 2.12 2.32 1.49 0.41 1.83 880 319 485 252 59 33 10.7 7.12 1.67 67.1 42.8 173 107 32.6 0.29 7 20.4 13.4 13.9 126 1.59 14.6 11.9 6.4 22 1.9 303 8.12 2.32 3.49 1.98 2.37 1.59 0.43 1.32 880 324 499 223 66 37.7 11.3 6.5 1.62 70.5 44.7 198 119 35 0.3 8 22 14.3 15.4 135 1.95 16 13.8 5.8 21.5 2 305 7.83 3.23 3.37 2.07 2.28 1.5 0.4 1.31 860 326 497 260 59 36 10.7 5.74 1.47 65.6 41.4 178 111 33.7 0.29 7 20.6 13.2 14.3 125 1.88 15 12.7 7.8 23 2.2 307 7.65 2.91 3.45 2.13 2.26 1.42 0.4 1.74 860 323 517 258 60 32.3 10.3 5.95 1.52 64.3 42.1 161 105 32.5 0.29 8 19.7 13.1 13.3 120 1.76 14.1 11.5 6.8 22.7 2.1 309 8.26 2.12 3.52 2.06 2.32 1.57 0.42 1.56 870 323 510 218 66 38.5 11.1 7.67 1.18 68.9 41.6 184 118 31.4 0.31 8 21.9 13.9 15.9 132 1.84 15.7 13.5 5.1 20.8 2 311 7.6 1.31 3.77 2 2.21 1.49 0.4 1.9 800 312 479 182 76 35.1 11 6.33 1.13 64.7 45.4 163 110 32.1 0.32 9 20.5 13.2 14.8 129 1.59 14.9 12.1 4 18.7 1.7 313 7.69 1.44 3.04 2.31 2.16 1.17 0.38 1.11 1070 308 604 238 50 23.2 8.9 2.89 0.68 65.3 30.3 112 87 28.6 0.21 6 18.6 12.3 14.2 110 1.21 12.1 11 3.3 20.2 1.8 315 7.71 1.67 3.19 2.33 2.3 1.22 0.38 1.35 1060 309 619 242 49 22.6 9.3 2.45 0.56 66.5 31.5 117 90 30.3 0.2 11 18.9 12.9 14.1 113 1.17 12.7 11.4 3.4 21.3 1.9 317 7.56 1.6 3.06 2.24 2.22 1.19 0.37 1.33 1060 301 573 239 46 23.2 9.4 2.48 0.6 65.6 31.6 116 88 28.7 0.2 12 19 12.8 14 113 1.16 12.6 11.6 3.4 21.2 1.8 319 7.59 1.66 3.17 2.31 2.24 1.19 0.37 1.35 1350 298 587 247 53 23.6 9 2.35 0.53 64.6 32.7 116 88 27.9 0.19 11 18.7 12.2 13.8 112 1.12 12.4 11.3 3.8 22.1 1.9 321 7.75 1.68 3.22 2.41 2.09 1.18 0.37 1.37 1050 297 619 249 50 23.2 8.8 2.26 0.49 63.6 31.1 114 87 28.8 0.2 12 18.8 12.1 14.3 103 1.1 12.2 10.6 3.6 20.1 1.8 323 7.58 1.59 3.01 2.29 2.22 1.13 0.36 1.34 1060 296 624 246 50 21.7 8.8 1.92 0.47 62.8 31.7 108 84 29.1 0.2 15 18.3 11.6 14.1 110 1.13 11.8 10.9 3.5 19.5 1.8 325 7.44 1.57 2.96 2.21 2.05 1.12 0.36 1.3 1050 293 584 241 47 21.5 8.8 1.94 0.44 63.7 32.3 105 83 29.4 0.19 15 18.1 11.9 13.7 122 1.24 12 11 3.5 20.1 1.9 327 7.61 1.7 3.16 2.27 1.83 1.18 0.37 1.27 1020 288 585 245 58 23 8.7 1.8 0.45 59.8 31.4 112 84 31.4 0.16 15 18 11.8 13.2 87.1 1.17 12 10.7 3.4 19 1.7 329 7.58 1.75 3.01 2.13 2.15 1.2 0.37 1.34 1000 287 577 240 58 23.3 8.8 2.19 0.54 60.2 33.3 115 88 30 0.19 16 18.5 12 13.3 105 1.13 12.2 11.1 3.7 19.4 1.8 331 7.22 2.05 3.06 2.15 2.08 1.11 0.35 1.64 1000 274 564 239 52 20.9 8.3 2.34 0.57 57.4 31.5 107 83 28.6 0.17 13 17.5 11.3 12.5 101 1.09 11.5 10.1 3.7 19.1 1.8 333 7.55 2 3.13 2.23 2.07 1.19 0.36 1.58 1020 284 602 245 62 23.1 8.7 2.73 0.72 58.7 33.4 113 88 29.4 0.2 12 18.5 11.7 12.9 103 1.1 12.5 11.1 4.1 19.5 1.8 335 7.18 2.07 3.08 2.18 2.09 1.11 0.34 1.63 1100 273 561 240 48 22.2 8.1 2.42 0.9 58.1 32.1 104 83 27.9 0.22 11 17.5 11.3 11.9 100 1 11.6 10.1 4 19.4 1.8 337 7.14 2.06 3.18 2.21 1.98 1.13 0.34 1.65 1070 272 598 243 50 23.2 8.4 2.56 0.99 59.2 32.7 107 85 28 0.21 13 17.8 11.4 12.4 97.9 1.11 11.9 10.4 4.4 19.9 1.8 339 7.11 2.18 3.13 2.11 2.03 1.14 0.34 1.58 1080 273 568 242 53 23.3 8.5 2.69 1 58.8 32.9 113 85 28 0.22 10 17.9 11.6 12.7 102 1.21 12 10.3 4.6 20.1 1.7 345 7.5 2.38 3.34 2.12 2.08 1.31 0.37 1.68 1240 301 547 245 57 25.4 9.7 4.06 1.15 59.8 35.4 127 95 31.2 0.21 12 18.9 12.1 13.4 106 1.21 12.8 11.1 5 20.7 1.9 347 7.33 2.48 3.17 1.87 2 1.45 0.37 1.34 1090 312 441 222 67 27.6 10.6 1.71 0.63 62 32.8 142 99 31.5 0.16 8 19.1 12.2 13.9 110 1.2 13.6 12.2 5.3 19.5 1.8 349 7.58 2.71 3.43 2.08 1.84 1.39 0.37 1.48 1210 314 560 252 55 25.7 10.1 3.98 0.95 64.9 35.3 133 96 32.5 0.2 11 19.1 12.3 14 94.8 1.28 13.3 11.5 5.1 20.9 1.9 351 7.63 2.69 3.5 1.96 2.16 1.53 0.39 1.46 1240 330 497 235 58 33.1 11.9 1.89 0.66 65.2 37.8 144 106 34 0.2 11 20.3 12.8 14.6 118 1.46 14.4 12.4 5.1 20.8 1.9 353 7.69 3.15 3.54 2.04 2.07 1.54 0.39 1.38 1330 330 477 245 58 31.7 11.3 2.09 0.55 67.3 36.3 147 103 35.3 0.2 12 20.1 13.1 15.1 111 1.38 14.4 12.5 5.5 21.1 1.9 355 7.58 2.93 3.46 1.95 2.05 1.51 0.39 1.45 1250 328 490 240 54 27.5 11.4 1.78 0.52 66.1 35.8 145 102 34.1 0.19 14 19.8 13 14.7 110 1.46 14.1 12.2 4.8 20.8 1.8 357 7.7 2.79 3.67 1.99 2.11 1.54 0.39 1.8 1220 337 493 237 59 28.2 12.2 2.72 0.6 65.4 36.6 146 103 34 0.18 13 20.8 13.4 15 117 1.64 14.8 12.7 4.7 20.9 1.9 359 7.5 2.99 3.35 1.96 2.12 1.5 0.38 1.45 1260 326 503 241 58 26.5 11.4 1.94 0.58 70 36 142 98 33.4 0.2 12 20.5 13.3 15.9 116 1.49 14.4 13 4.8 21.4 2 369 7.4 3.35 3.44 2.01 2.06 1.4 0.37 1.32 1240 314 519 256 57 24.3 10.7 1.65 0.54 65.2 33.3 133 93 32.1 0.18 16 19.1 12.2 14.2 107 1.19 13.3 12 4.7 20.2 1.8 371 7.58 2.93 3.75 2.05 2.04 1.44 0.38 2.01 1140 329 530 248 52 24.6 11.4 4 0.6 65.1 33.9 135 94 33.4 0.18 24 19.6 12.9 14.2 110 1.34 13.5 12.1 4.3 20.3 1.8 373 7.03 3.4 3.26 1.98 1.89 1.36 0.35 1.64 1170 306 484 247 52 24 10.4 1.84 0.46 60.7 32.7 128 88 31.8 0.18 13 18.2 12.1 13.6 100 1.27 12.9 11.4 4.4 19.5 1.8