# 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/19685 # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/by_contributor/dean2015/dean2015-20jpc-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: The Marine Isotope Stage 16-15 boundary (Termination VII) is the first deglacial warming step of the late Quaternary following the end of 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 because of lack of high-resolution paleoclimate archives. Core MV0508-19JPC from Santa Barbara Basin (SBB), California contains a decadal-scale climatic and geochemical sediment record of 4000 years duration. This record reveals that the climatic shift during the deglacial occurred rapidly (<700 yr), in a progression of three abrupt warming steps. The onset of 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 (639.0±2 ka) from Yellowstone Caldera used to date the onset of Termination VII at 639.2 ka. The late MIS 16 and early MIS 15 interval exhibits multiple decadal-scale negative excursions in ?13C of planktic foraminifera, likely the result of repeated discharges from methane hydrates associated with ocean warming or low sea level. A warm interstadial that interrupts late MIS 16 is characterized by elevated concentrations of redox-sensitive elements indicating sulfidic, oxygen-deficient bottom and pore waters, and elevated concentrations of TOC and Cd, reflecting increased surface productivity. Unlike younger sediments on the California margin, these geochemical 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. See original reference for further details on the cores and methods. #--------------------------------------- # Publication # Authors: Dean, W.E., Kennett, J.P., Behl, R.J., Nicholson, C., and Sorlien, C.C. # 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: MV0508-20JPC # Location: Eastern Pacific Ocean # Country: Santa Barbara Basin # Northernmost_Latitude: 34.215583 # Southernmost_Latitude: 34.215583 # Easternmost_Longitude: 119.672667 # Westernmost_Longitude: 119.672667 # Elevation: -120 #--------------------------------------- # Data_Collection # Collection_Name: 20JPC-ICP-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 ## Fe% iron,,,percent,,Paleoceanography,,,N ## Na% sodium,,,percent,,Paleoceanography,,,N ## K% potassium,,,percent,,Paleoceanography,,,N ## Mg% magnesium,,,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 ## Ni-ppm nickel,,,ppm,,Paleoceanography,,,N ## Cr-ppm chromium,,,ppm,,Paleoceanography,,,N ## Cu-ppm copper,,,ppm,,Paleoceanography,,,N ## Li-ppm lithium,,,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 ## Be-ppm beryllium,,,ppm,,Paleoceanography,,,N ## Cd-ppm cadmium,,,ppm,,Paleoceanography,,,N ## Ce-ppm cesium,,,ppm,,Paleoceanography,,,N ## Co-ppm cobalt,,,ppm,,Paleoceanography,,,N ## Ga-ppm gallium,,,ppm,,Paleoceanography,,,N ## La-ppm lanthanum,,,ppm,,Paleoceanography,,,N ## Lu-ppm lutetium,,,ppm,,Paleoceanography,,,N ## Mo-ppm molybdenum,,,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 ## Sn-ppm tin,,,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% Fe% Na% K% Mg% Ti% S% P-ppm Mn-ppm Ba-ppm Sr-ppm Ni-ppm Cr-ppm Cu-ppm Li-ppm V-ppm Zn-ppm Zr-ppm Ag-ppm As-ppm Be-ppm Cd-ppm Ce-ppm Co-ppm Ga-ppm La-ppm Lu-ppm Mo-ppm Nb-ppm Pb-ppm Rb-ppm Sb-ppm Sc-ppm Sn-ppm Th-ppm U-ppm Y-ppm Yb-ppm 2 7.87 2.27 4.36 2.26 2.27 1.42 0.42 2.32 990 354 333 243 39.5 74 34.9 62 133 101 35.3 0.15 13 1.8 1.27 72.7 11.1 20 38 0.27 14.7 15.1 16.8 118 1.76 13.4 2.2 13.9 5.09 22.5 1.9 6 7.74 2.68 4.42 2.19 2.28 1.45 0.41 2.2 960 376 398 267 41.4 76 34.5 61 127 99 33.4 0.14 17 1.8 1.4 72.6 11.7 20 37.6 0.3 14.5 14.3 16.7 120 1.69 13.6 2.1 14.1 5.99 23.3 2 10 7.31 3.62 3.49 2.21 2.18 1.31 0.39 1.29 1070 325 617 314 31.8 72 29.4 55 123 88 33.2 0.14 13 1.7 0.65 65.6 9.4 18.3 34.1 0.27 7.41 13.4 15.3 110 1.63 12.2 1.9 12.5 5.22 22.1 1.8 14 7.38 3.48 3.94 2.26 2.22 1.4 0.38 1.78 1020 344 481 319 46.4 76 32.7 59 125 95 33.7 0.14 11 1.7 1.68 66.1 11.3 18.7 34.4 0.28 12.4 13.2 15.4 114 1.37 13 2 12.3 6.74 22.2 1.9 18 7.81 2.92 4.2 2.2 2.33 1.5 0.41 1.75 990 358 366 291 41.3 81 35.4 66 135 104 34.5 0.14 13 1.9 0.98 71 10.9 20.4 37.3 0.26 14.7 14.5 16.8 125 2.2 13.9 2.1 14 5.24 21.7 1.8 22 7.29 3.23 3.81 2.26 2.25 1.41 0.38 1.45 1090 347 547 306 40.6 78 33.4 58 131 100 34.1 0.15 11 1.7 1.45 66.5 10.4 18.4 34.7 0.28 12.9 13.2 15 115 1.51 13 2 12.6 6.28 22.7 1.9 26 7.66 3.25 3.75 2.33 2.11 1.48 0.41 1.28 1050 347 616 297 40.4 80 34.6 64 134 102 34.2 0.12 9 1.8 1.26 68.1 10.6 19.1 35.9 0.27 10.6 14.1 15.8 108 1.47 13.2 2.1 13.2 5.56 22.2 1.8 30 7.36 3.42 4.41 2.19 1.92 1.41 0.39 2.36 970 361 346 304 41.6 75 34.8 61 129 100 34.3 0.2 16 1.7 1.76 65.7 10.8 18.7 34.7 0.28 37.6 13.3 15.6 97.5 1.68 12.7 1.9 12.5 5.95 21.8 1.8 34 7.62 3.53 3.71 2.26 2.12 1.44 0.4 1.62 940 338 497 306 38.1 75 34.6 65 131 98 33.8 0.13 10 1.8 1.39 66.7 10.7 19 35 0.26 10.6 13.6 15.8 110 1.48 13 2 12.9 5.67 21.8 1.8 38 8.03 1.94 4 2.25 2.43 1.56 0.44 1.23 1070 347 589 235 44.9 81 37 70 145 107 38.4 0.16 9 1.9 1.39 73.8 11.9 21.2 38.8 0.27 7.09 15.1 17.5 132 1.72 14.1 2.2 14.3 4.9 23 1.9 42 7.96 2.48 3.88 2.26 2.11 1.5 0.42 1.19 930 360 528 263 38.2 75 36.2 69 133 104 33.5 0.15 9 1.8 1.09 71.2 11.4 20.6 37.7 0.27 5.26 14.5 17.1 112 1.99 13.4 2.1 14.1 4.89 22.4 1.9 46 8.06 3.03 3.79 2.41 2.38 1.4 0.42 1.15 1060 357 735 309 38.5 80 33.3 63 129 97 36.9 0.12 10 1.8 0.62 72 11.3 20.1 37.6 0.29 4.59 14.7 17 122 1.72 13.2 2 13.2 4.84 23.5 2 50 7.88 2.55 3.67 2.36 2.34 1.38 0.41 1.15 1000 347 772 280 35.4 78 32.1 61 124 96 36.9 0.12 11 1.8 0.85 69.4 11.2 19.7 36.3 0.27 2.97 14.7 16.3 122 1.4 12.8 2.1 12.8 4.24 22.6 1.9 54 7.82 3.16 3.47 2.4 2.37 1.34 0.4 1.22 1010 330 591 307 33.8 74 31.8 60 117 90 34.2 0.13 13 1.8 0.91 68.6 10.8 19.3 35.5 0.28 2.46 14 16.1 119 1.25 12.6 1.9 12.4 4.67 23 1.9 62 7.82 2.68 3.57 2.4 2.35 1.35 0.4 1.18 1030 331 581 284 35.3 74 32.6 60 118 96 33.7 0.15 11 1.7 1.07 68.4 10.8 19.1 35.4 0.27 3.47 13.8 16.1 117 1.24 11.9 2 12.5 4.24 22 1.8 66 7.61 2.98 3.61 2.31 2.24 1.28 0.39 1.22 1000 322 607 296 31.1 70 29.8 59 113 93 31.9 0.13 9 1.7 0.79 68.4 10.3 18.7 35.2 0.28 3.6 13.5 15.8 112 1.02 11.9 1.9 12.3 4.12 22.2 1.8 70 7.66 2.87 3.56 2.29 2.1 1.31 0.4 1.17 1000 328 582 288 31.3 69 31.7 62 119 91 32.2 0.11 9 1.7 0.7 65.9 10.6 19 34.2 0.27 3.85 13.8 15.9 108 1.19 12.3 1.9 12.2 4.66 22.5 1.9 74 7.61 3.35 3.62 2.38 2.2 1.27 0.39 1.24 1000 326 658 315 31.2 69 29.5 59 114 90 32.2 0.1 14 1.6 0.77 67.5 10.1 18.6 35.1 0.28 6.14 13.5 15.7 109 1.19 12.1 1.9 12.2 4.87 22.3 1.9 78 7.69 2.91 3.75 2.37 2.2 1.34 0.39 1.31 1040 327 553 287 34.1 73 31.5 61 122 91 33.5 0.13 16 1.7 1 67.3 10.7 19.2 35 0.26 6.33 13.7 16 114 1.25 12.3 1.9 12.5 4.88 22.1 1.8 82 7.46 4.16 3.79 2.34 2.19 1.24 0.39 1.39 1020 323 552 336 33.8 73 29.9 59 116 86 33.9 0.11 16 1.6 1.15 68.3 10.9 18.2 35.4 0.28 6.79 13.4 15.5 111 1.3 12 1.9 12.3 5.26 22.5 1.9 86 7.33 4.43 3.45 2.38 2.1 1.17 0.37 1.43 1040 316 578 350 30.4 67 27.3 55 110 82 32.1 0.13 13 1.6 1.06 67.6 9.8 17.6 34.7 0.29 7.98 13.1 15.3 102 1.13 11.3 1.8 11.8 5.11 22.5 1.9 90 7.49 3.19 4.09 2.18 2.22 1.37 0.4 1.79 1070 342 318 302 37.9 78 36.3 64 128 94 32.9 0.15 16 1.7 1.43 67.1 11.3 19.3 34.9 0.27 11.6 13.8 15.3 116 1.6 12.9 2 12.6 5.31 22.5 1.9 94 7.69 3.46 3.95 2.34 2.27 1.44 0.39 1.51 1020 345 565 309 38.7 78 36.4 67 133 95 33.2 0.14 10 1.7 1.46 67.3 11.3 19.4 35.1 0.27 10.8 13.6 15.5 119 1.42 13 1.9 12.6 5.34 22.3 1.8 99 7.85 3.36 4.06 2.23 2.17 1.46 0.41 1.31 1030 356 551 316 38.6 78 35 68 144 100 34.6 0.14 8 1.8 1.46 69.1 11.9 20.6 36.1 0.27 10.5 14.5 16 121 2.13 13.7 2.1 13.1 4.96 22.7 1.8 102 7.47 3.9 3.83 2.27 2.17 1.43 0.39 1.23 980 348 559 351 39 74 34.9 66 132 96 34 0.14 9 1.7 1.58 65.1 11.2 19.3 34.1 0.28 7.34 13.5 14.9 117 1.74 13.1 1.9 12.3 5.15 22.4 1.9 106 7.58 3.71 3.65 2.3 2.24 1.47 0.39 1.2 930 341 558 325 37.1 73 34.9 67 134 94 33.1 0.18 10 1.7 1.36 68 10.9 19.7 35.6 0.27 6.4 13.7 15.4 119 1.74 12.7 2 12.8 5.17 22.4 1.9 110 7.44 3.58 4.21 2.18 2.18 1.39 0.39 1.88 900 345 482 313 43.8 75 33.8 65 128 93 32.5 0.16 14 1.7 1.4 68.3 11.8 19 35.5 0.28 14.4 13.4 15.2 117 1.95 12.6 1.9 12.8 4.96 21.9 1.9 114 7.46 4.22 3.95 2.2 2.02 1.42 0.39 1.55 970 343 525 340 46.6 76 34.3 67 132 93 32.3 0.14 12 1.7 1.43 65.8 11.5 19.2 34.5 0.28 7.63 13.1 14.9 105 1.61 12.9 1.9 12.2 5.54 22 1.9 118 7.59 3.32 3.58 2.28 2.19 1.42 0.39 1.19 980 337 727 302 44.4 79 34.7 68 133 96 31.6 0.14 6 1.7 1.4 64.5 10.9 19.6 33.7 0.26 4.98 13.2 15.4 115 1.26 12.2 2 12.1 4.91 21.1 1.7 122 7.27 4.25 3.62 2.24 2.19 1.33 0.37 1.25 950 326 380 346 40.6 70 32.5 63 121 86 31 0.2 8 1.7 1.37 64.4 10.6 18.5 33.6 0.28 6.86 12.9 14.8 114 1.56 12.5 1.9 12 5.51 22.3 1.9 126 7.55 3.56 3.65 2.27 2.27 1.29 0.39 1.42 1000 319 595 313 39.1 71 29.8 62 119 86 33.3 0.14 8 1.7 0.77 66.4 10.5 18.4 34.4 0.27 3.24 13.3 15.2 114 1.72 11.6 1.8 11.8 4.18 21.6 1.8 130 7.63 3.52 3.46 2.27 2.3 1.34 0.39 1.23 1020 324 591 309 40.8 76 31.4 64 122 91 34.3 0.14 11 1.7 0.86 67.3 10.8 19.1 35 0.27 3.75 13.7 15.5 117 1.25 12 1.9 12.1 4.47 21.9 1.8 134 7.47 3.52 3.59 2.22 2.24 1.35 0.4 1.5 970 324 544 298 40.2 75 32.5 64 122 92 33.1 0.14 15 1.7 1.15 66.1 11 19.2 34.4 0.27 5.55 13.7 15.3 116 1.29 12.2 1.9 12 5.03 22 1.8 138 7.74 3.87 3.76 2.29 2.29 1.36 0.4 1.46 1040 331 603 318 38 75 32.8 65 122 90 34.2 0.15 14 1.7 1.08 68.7 10.8 19.4 35.4 0.29 5.95 13.6 15.4 116 1.2 12.6 1.9 12.2 5.21 23.3 1.9 142 7.58 3.13 3.68 2.25 2.31 1.31 0.39 1.24 910 326 586 289 35.9 71 32.6 65 119 90 33.6 0.14 10 1.7 0.98 67.6 10.9 19.5 34.9 0.27 7.16 13.7 16.2 118 1.28 12.3 1.9 12 4.63 22.1 1.9 146 7.59 3.62 3.73 2.25 2.29 1.29 0.38 1.46 930 322 586 308 36.8 72 30.8 64 116 90 31.6 0.13 8 1.7 0.7 66.8 10.9 19.3 34.5 0.27 5.35 13.2 15.6 117 1.13 11.9 1.8 12 4.17 21.8 1.8 150 7.52 4.1 3.58 2.21 2.27 1.29 0.38 1.41 930 326 602 325 33.4 72 30.6 63 113 90 32.1 0.11 10 1.6 0.82 69.4 11.3 19.3 35.6 0.27 4.47 13.6 15.6 118 1.11 12 1.8 12.1 4.3 22.4 1.9 154 7.28 4.06 3.64 2.16 2.21 1.22 0.37 1.57 950 314 574 320 33.1 68 28.7 58 109 81 32.1 0.12 18 1.6 0.83 65.6 10.6 18.3 33.8 0.27 7.46 12.9 15 111 1.13 11.3 1.8 11.5 4.68 22.2 1.9 158 7.35 4.42 3.32 2.26 2.24 1.22 0.37 1.18 970 322 630 341 31.1 69 29.6 58 107 81 31.8 0.13 13 1.6 0.82 64.3 10 18 32.8 0.27 5.64 12.5 14.6 110 0.96 11.2 1.7 11.3 4.69 21.8 1.8 162 7.28 4.27 3.57 2.2 2.23 1.21 0.37 1.45 950 317 604 330 31.1 72 29.1 59 112 80 32.8 0.12 15 1.6 0.81 64.5 10.1 18.2 33.4 0.26 7.44 12.8 14.6 111 1.08 11.2 1.7 11.2 5.02 21.7 1.8 166 7.36 3.97 3.49 2.22 2.19 1.23 0.37 1.33 950 317 599 330 31.1 70 31.1 60 114 82 33.1 0.13 11 1.6 0.84 62.9 10 18.2 32.6 0.26 6.81 12.7 14.6 107 1.04 11.2 1.8 11.1 5.25 21.4 1.8 170 7.24 3.91 3.65 2.15 2.11 1.25 0.37 1.52 960 313 520 317 34 76 37.2 61 118 85 33.1 0.14 14 1.6 1.11 61.5 10.1 18.4 32 0.26 11.2 12.8 14.4 107 1.08 11.3 1.8 11.1 5.48 21.5 1.8 174 6.87 4.63 3.79 2.19 2 1.19 0.35 1.94 990 297 363 326 35 70 29.4 57 112 79 31.4 0.16 24 1.5 1.55 61.7 9.7 17 31.5 0.27 20.3 12 13.8 100 1.49 11.6 1.7 10.7 6.57 22.5 1.9 178 7.36 2.87 3.9 2.23 2.28 1.38 0.39 1.59 910 330 531 273 41.1 80 34.7 66 127 94 32.3 0.18 18 1.7 1.63 63.8 11.2 19.3 33.2 0.26 21 13.5 14.6 119 1.34 12.3 1.9 11.5 6.58 21.8 1.8 182 7.29 3.14 3.62 2.25 2.15 1.35 0.38 1.53 910 329 554 279 39.1 81 35.3 66 130 92 32 0.17 11 1.6 1.47 61.9 10.4 18.9 32.5 0.25 15 13 14.7 113 1.26 12.1 1.8 11.3 6.16 21 1.8 186 7.36 3.39 3.79 2.2 2.18 1.34 0.38 1.53 880 332 597 295 38.5 77 38.6 64 124 91 31.3 0.16 15 1.6 1.36 63.3 10.6 18.6 33.2 0.26 20.3 12.9 14.9 114 1.42 12.2 1.9 11.4 6.08 21.7 1.8 190 7.25 3.97 3.7 2.2 2.23 1.25 0.37 1.54 960 324 607 316 37.3 76 34.2 62 119 88 33.6 0.14 16 1.6 1.04 63.4 10.8 18.2 32.8 0.26 13.1 12.8 15.7 112 1.54 11.8 1.8 11.4 5.37 21.6 1.8 194 7.17 4.5 3.41 2.25 2.18 1.2 0.36 1.24 940 322 643 353 34.1 70 30.1 59 113 79 32.5 0.11 10 1.6 1 62.7 9.7 17.6 32.4 0.26 11.1 12.2 15 107 1.47 11.5 1.7 11.1 5.36 21.9 1.8 198 6.92 4.43 3.25 2.22 2.14 1.14 0.35 1.32 920 303 623 356 32.5 70 28.2 56 109 78 33.2 0.15 17 1.5 1.24 59.1 9.4 17.1 30.7 0.26 11.7 12 14.4 104 1.41 10.8 1.6 10.2 5.42 20.6 1.7 202 7.24 4.24 3.47 2.21 2.17 1.35 0.37 1.29 900 325 629 358 41.3 75 35.5 64 127 91 32.6 0.17 9 1.6 2.05 61.7 10.5 18.8 32.2 0.27 11.3 12.8 15.3 114 1.67 12.3 1.8 11.1 6.12 22.3 1.9 206 7.09 4.15 3.45 2.21 2.17 1.37 0.37 1.23 920 322 631 355 41.1 78 35.6 63 130 93 35.1 0.2 8 1.6 1.97 60.5 10.3 18.4 31.8 0.26 11.8 12.6 14.6 114 1.62 12 1.8 10.8 5.79 21.7 1.8 210 6.74 4.01 2.11 2.05 1.27 0.35 870 399 275 329 45.1 75 35.2 60 126 89 31.2 0.18 34 1.5 2.35 58 12.2 17.3 30.3 0.26 108 11.9 13.8 108 2.54 11.4 1.7 10.5 6.4 20.4 1.7 214 7.01 4.84 3.39 2.18 1.94 1.35 0.36 1.32 890 315 641 391 39.1 73 34.1 63 127 87 31.2 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