# South Atlantic Late Pleistocene Sea Surface Temperature, Dust and Paleoproductivity Data #----------------------------------------------------------------------- # 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: http://www.hurricane.ncdc.noaa.gov/pls/paleox/f?p=519:1:::::P1_STUDY_ID: 16464 # # Original_Source_URL: ftp://ftp.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/anderson2014/anderson2014-06pc4.txt # # Archive: Paleoceanography #--------------------------------------- # Contribution_Date # Date: 2014-05-19 #--------------------------------------- # Title # Study_Name: South Atlantic Late Pleistocene Sea Surface Temperature, Dust and Paleoproductivity Data #--------------------------------------- # Investigators # Investigators: Anderson, R.F.; Fleisher, M.Q; Sachs, J.P. #--------------------------------------- # Description and Notes # Description: Portions of the data reported here were described previously in the four papers by Sachs and co-workers, cited below, as well as in the paper by Martinez-Garcia et al., cited below. # EXPLANATION OF DERIVED PARAMETERS: # xs230Tho (initial unsupported 230Th concentration): xs230Tho refers to the measured value as corrected for ingrowth of 230Th from authigenic and detrital (lithogenic) uranium. # These values are calculated using measured concentrations of 230Th, 232Th and 238U, and assuming that all 232Th is detrital in nature. # It also assumes a detrital U/Th ratio, which varies by region. # Concentrations are finally corrected for decay since deposition. # # 230Th-normalized mass flux (Flux: g/cm^2/kyr): 230Th-normalized mass accumulation rate (or flux) # For a discussion of this proxy and the relevant corrections and parameters, # please see Francois et al. (2004), cited above. # # Lithogenic content: The lithogenic content of the dry bulk sediment was calculated from # the measured 232Th concentration assuming that the lithogenic material has a # uniform 232Th concentration of 10 ppm. # # The 230Th-normalized flux of any constituent can be derived by multiplying the # 230Th-normalized mass flux by the reported concentration of the constituent. # # Alkenone SSTs were calculated using the definition of Uk'37 = C37:2 / (C37:2 + C37:3) and temperature calibration # Uk'37 = 0.034*SST + 0.039 from Prahl, F.G., Muehlhausen, L.A., Zahnle, D.L., 1988. Further evaluation of long-chain alkenones # as indicators of paleoceanographic conditions. Geochimica et Cosmochimica Acta 52, 2303-2310. # #--------------------------------------- # Publication # Authors: Anderson, R.F., S. Barker, M.Q. Fleisher, R. Gersonde, S.L. Goldstein, G. Kuhn, P.G. Mortyn, K. Pahnke, and J.P. Sachs # Published_Date_or_Year: 2014 # Published_Title: Biological response to millennial variability of dust supply in the subantarctic South Atlantic Ocean. # Journal_Name: Philosophical Transactions of the Royal Society of London Series a-Mathematical Physical and Engineering Sciences. # Volume: in press # Issue: # Pages: # DOI: # Online_Resource: http://rsta.royalsocietypublishing.org/ # Full_Citation: # Abstract: Fluxes of lithogenic material and fluxes of three palaeo-productivity proxies (organic carbon, biogenic opal and alkenones) over the past 100 000 years were determined using the 230Th-normalization method in three sediment cores from the Subantarctic South Atlantic Ocean. Features in the lithogenic flux record of each core correspond to similar features in the record of dust deposition in the EPICA Dome C ice core. Biogenic fluxes correlate with lithogenic fluxes in each sediment core. Our preferred interpretation is that South American dust, most probably from Patagonia, constitutes a major source of lithogenic material in Subantarctic South Atlantic sediments, and that past biological productivity in this region responded to variability in the supply of dust, probably due to biologically available iron carried by the dust. Greater nutrient supply as well as greater nutrient utilization (stimulated by dust) contributed to Subantarctic productivity during cold periods, in contrast to the region south of the Antarctic Polar Front (APF), where reduced nutrient supply during cold periods was the principal factor limiting productivity. The anti-phased patterns of productivity on opposite sides of the APF point to shifts in the physical supply of nutrients and to dust as cofactors regulating productivity in the Southern Ocean. #--------------------------------------- # Publication # Authors: Sachs, J.P.; R.F. Anderson; S.J. Lehman # Published_Date_or_Year: 2001 # Published_Title: Glacial Surface Temperatures of the Southeast Atlantic Ocean # Journal_Name: Science # Volume: 293 # Issue: 5537 # Pages: 2077-2079 # Report Number: # DOI: 10.1126/science.1063584 # Online_Resource: http://www.sciencemag.org/content/293/5537/2077.abstract # Full_Citation: # Abstract: A detailed record of sea surface temperature from sediments of the Cape Basin in the subtropical South Atlantic indicates a previously undocumented progression of marine climate change between 41 and 18 thousand years before the present (ky B.P.), during the last glacial period. Whereas marine records typically indicate a long-term cooling into the Last Glacial Maximum (around 21 ky B.P.) consistent with gradually increasing global ice volume, the Cape Basin record documents an interval of substantial temperate ocean warming from 41 to 25 ky B.P. The pattern is similar to that expected in response to changes in insolation owing to variations in Earth's tilt. #--------------------------------------- # Publication # Authors: Julian P. Sachs and Robert F. Anderson # Published_Date_or_Year: 2003-10-15 # Published_Title: Fidelity of alkenone paleotemperatures in southern Cape Basin sediment drifts. # Journal_Name: Paleoceanography # Volume: 18 # Issue: 4 # Pages: PA1082 # Report Number: # DOI: 10.1029/2002PA000862 # Online_Resource: http://onlinelibrary.wiley.com/doi/10.1029/2002PA000862/abstract # Full_Citation: # Abstract: Multiple geochemical analyses were performed in order to test the fidelity of alkenone paleotemperature reconstructions in southern Cape Basin sediment drifts. Sea surface temperatures (SSTs) derived from the alkenone unsaturation ratio, U37k', in two drift cores (TN057-21 and Ocean Drilling Program Site 1089) are nearly identical during the interval of overlapping analyses, MIS 4-5c. SSTs in a nearby nondrift core (TN057-6) covary with those in core TN057-21 throughout MIS 1-5c. While climatological SSTs overlying TN057-21 and TN057-6 are similar and consistent with reconstructed Holocene SSTs in the nondrift core, surface waters overlying TN057-21 are ~6C colder than Holocene alkenone SSTs in the drift core. Temperatures remain ~6C warmer in TN057-21 relative to TN057-6 during the ~100 kyr duration of the records. We hypothesize that alkenone-derived SSTs in TN057-21 are higher than climatological SSTs in the overlying surface water and those in TN057-6 as a result of the winnowing and focusing of sedimentary alkenones produced in warmer waters to the north. Climatological SSTs in the central and northern Cape Basin are 16-20C. A 1.5% offset of fine fraction d18O values relative to planktonic foraminifera in TN057-21 supports this hypothesis. Temporal changes in sediment focusing were evaluated directly using uranium series radioisotopes. While higher sediment focusing factors would be expected to result in higher alkenone-derived SSTs if sediment advection were the primary control on down-core changes in alkenone-derived SSTs, 230Th-derived focusing factors indicate no such correlation exists. We conclude that alkenone paleotemperature reconstructions from southern Cape Basin drifts reliably record regional SST variations in the Cape Basin. #--------------------------------------- # Publication # Authors: Roger Francois, Martin Frank, Michiel M. Rutgers van der Loeff and Michael P. Bacon # Published_Date_or_Year: 2004-03-05 # Published_Title: 230Th normalization: An essential tool for interpreting sedimentary fluxes during the late Quaternary # Journal_Name: Paleoceanography # Volume: 19 # Issue: 1 # Pages: PA1018 # Report Number: # DOI: 10.1029/2003PA000939 # Online_Resource: http://onlinelibrary.wiley.com/doi/10.1029/2003PA000939/abstract # Full_Citation: # Abstract: There is increasing evidence indicating that syndepositional redistribution of sediment on the seafloor by bottom currents is common and can significantly affect sediment mass accumulation rates. Notwithstanding its common incidence, this process (generally referred to as sediment focusing) is often difficult to recognize. If redistribution is near synchronous to deposition, the stratigraphy of the sediment is not disturbed and sediment focusing can easily be overlooked. Ignoring it, however, can lead to serious misinterpretations of sedimentary fluxes, particularly when past changes in export flux from the overlying water are inferred. In many instances, this problem can be resolved, at least for sediments deposited during the late Quaternary, by normalizing to the flux of 230Th scavenged from seawater, which is nearly constant and equivalent to the known rate of production of 230Th from the decay of dissolved 234U. We review the principle, advantages and limitations of this method. Notwithstanding its limitations, it is clear that 230Th normalization does provide a means of achieving more accurate interpretations of sedimentary fluxes and eliminates the risk of serious misinterpretations of sediment mass accumulation rates. #--------------------------------------- # Publication # Authors: Julian P. Sachs and Robert F. Anderson # Published_Date_or_Year: 2005-04-28 # Published_Title: Increased productivity in the subantarctic ocean during Heinrich events. # Journal_Name: Nature # Volume: 434 # Issue: # Pages: 1118-1121 # Report Number: # DOI: 10.1038/nature03544 # Online_Resource: http://www.nature.com/nature/journal/v434/n7037/abs/nature03544.html # Full_Citation: # Abstract: Massive iceberg discharges from the Northern Hemisphere ice sheets, 'Heinrich events', coincided with the coldest periods of the last ice age. There is widespread evidence for Heinrich events and their profound impact on the climate and circulation of the North Atlantic Ocean, but their influence beyond that region remains uncertain. Here we use a combination of molecular fingerprints of algal productivity and radioisotope tracers of sedimentation to document eight periods of increased productivity in the subpolar Southern Ocean during the past 70,000 years that occurred within 1,000-2,000 years of a Northern Hemisphere Heinrich event. We discuss possible causes for such a link, including increased supply of iron from upwelling and increased stratification during the growing season, which imply an alteration of the global ocean circulation during Heinrich events. The mechanisms linking North Atlantic iceberg discharges with subantarctic productivity remain unclear at this point. We suggest that understanding how the Southern Ocean was altered during these extreme climate perturbations is critical to understanding the role of the ocean in climate change. #--------------------------------------- # Publication # Authors: Katharina Pahnke and Julian P. Sachs # Published_Date_or_Year: 2006-04-13 # Published_Title: Sea surface temperatures of southern midlatitudes 0-160 kyr B.P. # Journal_Name: Paleoceanography # Volume: 21 # Issue: 2 # Pages: PA2003 # Report Number: # DOI: 10.1029/2005PA001191 # Online_Resource: http://onlinelibrary.wiley.com/doi/10.1029/2005PA001191/abstract # Full_Citation: # Abstract: Late Quaternary climate fluctuated between extremes of glaciations, lasting ~90 kyr on average, and interglacial episodes, lasting ~10 kyr. Still largely unknown are the spatial and temporal evolution of these global climate states, with vigorous debate still underway on the mechanisms responsible for glacial inceptions and terminations. Though it is widely believed that the Southern Hemisphere oceans play a central role in global climate changes, few paleoclimate records exist from there. Here we present three new alkenone-derived SST records from the midlatitude Southern Hemisphere spanning the last 160 kyr, a full glacial-interglacial cycle. Our subtropical SST records from the last glacial period are characterized by (1) warming 47-23 kyr B.P., when high latitudes in both hemispheres cooled, and (2) milder temperatures during the penultimate glacial period than during the last glacial interval. These SST features are found to be of tropical- to subtropical-wide extent, implying increased thermal gradients at times of high-latitude ice sheet growth. This has implications for the vigor of atmospheric and upper ocean circulation and the transport of heat and moisture to the poles that may have been instrumental in the growth and maintenance of polar ice sheets during glacial periods. #--------------------------------------- # Publication # Authors: Martinez-Garcia, A., D.M. Sigman, H. Ren, R.F. Anderson, M. Straub, D.A. Hodell, S.L. Jaccard, T.I. Eglinton, and G.H. Haug. # Published_Date_or_Year: 2014-03-21 # Published_Title: Iron Fertilization of the Subantarctic Ocean During the Last Ice Age # Journal_Name: Science # Volume: 343 # Issue: 6177 # Pages: 1347-1350 # Report Number: # DOI: 10.1126/science.1246848 # Online_Resource: http://www.sciencemag.org/content/343/6177/1347.abstract # Full_Citation: # Abstract: John H. Martin, who discovered widespread iron limitation of ocean productivity, proposed that dust-borne iron fertilization of Southern Ocean phytoplankton caused the ice age reduction in atmospheric carbon dioxide (CO2). In a sediment core from the Subantarctic Atlantic, we measured foraminifera-bound nitrogen isotopes to reconstruct ice age nitrate consumption, burial fluxes of iron, and proxies for productivity. Peak glacial times and millennial cold events are characterized by increases in dust flux, productivity, and the degree of nitrate consumption; this combination is uniquely consistent with Subantarctic iron fertilization. The associated strengthening of the Southern Ocean's biological pump can explain the lowering of CO2 at the transition from mid-climate states to full ice age conditions as well as the millennial-scale CO2 oscillations. #--------------------------------------- # Publication # Authors: Stephen Barker and Paula Diz # Published_Date_or_Year: 2014 # Published_Title: Timing of the descent into the last ice age determined by the bipolar seesaw # Journal_Name: Paleoceanography # Volume: in press # Edition: # Issue: # Pages: # DOI: 10.1002/2014PA002623 # Online_Resource: http://onlinelibrary.wiley.com/doi/10.1002/2014PA002623/abstract # Full_Citation: # Abstract: We present planktonic foraminiferal fauna and isotope records from the SE Atlantic that highlight the nature of millennial-scale variability over the last 100 kyr. We derive an hypothesis-driven age model for our records based on the empirical link between variations in Greenland temperature, ocean circulation and carbonate preservation in the deep SE Atlantic. Our results extend earlier findings of an anti-phase (seesaw) relationship between north and south for the largest abrupt events of Marine Isotope Stage (MIS) 3-2 and the last deglaciation. In particular we find that Heinrich Stadials were paralleled by inferred southward shifts of the thermal Subtropical Front. These were followed by pronounced rebounds of the front with the return to interstadial conditions in the north. Our results also shed light on the mechanism of glaciation. In contrast to the last deglaciation, which was a globally symmetric change superposed by interhemispheric asynchronicity, we find that the descent into full glacial conditions at the onset of MIS 4 (~70 ka) displayed interhemispheric synchrony. We suggest that this globally synchronous descent into glacial MIS 4 was preconditioned by orbital changes but that the timing was ultimately determined by abrupt changes in ocean / atmosphere circulation patterns i.e. the bipolar seesaw. #------------------ # Funding_Agency # Funding_Agency_Name: National Science Foundation # Grant: OCE 0823507 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Jeptha H. and Emily V. Wade Foundation # Grant: #--------------------------------------- # Funding_Agency # Funding_Agency_Name: National Oceanic and Atmospheric Administration # Grant: NA77RJ0453 #--------------------------------------- # Site Information # Site_Name: TN057-06PC4 # Location: Ocean>Atlantic Ocean>South Atlantic Ocean # Northernmost_Latitude: -42.91 # Southernmost_Latitude: -42.91 # Easternmost_Longitude: 8.9 # Westernmost_Longitude: 8.9 # Elevation: -3571 #--------------------------------------- # Data_Collection # Collection_Name: Anderson2014-06PC4 # First_Year: 101960 # Last_Year: 8000 # Time_Unit: cal yr BP # Core_Length: # Notes: #--------------------------------------- # Chronology: # The age model reported here for TN057-06-PC4 was modified from previously published age models (based on oxygen isotope stratigraphy) # by tuning the lithogenic accumulation rate to the dust flux record of the EPICA Dome C ice core. See the primary reference (Anderson et al.2014) for details. # The age model reported here for TN057-21-PC2 is taken from Barker and Diz (2014). #--------------------------------------- # Variables # # Data variables follow that are preceded by "##" in columns one and two. # Data line variables format: Variables list, one per line, shortname-tab-longname-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 ## age_calkaBP age, , , calendar kyears before present, , , , ,N ## 232Th.dpm 232Th concentration, bulk sediment, , dpm/g, , Paleoceanography, analytical technique: ICP mass spectrometry, , N ## 232Th.dpm.err 232Th concentration 1 sigma error, , , 1 sigma, , , , ,N ## 230Th.dpm 230Th concentration, bulk sediment, , dpm/g, , Paleoceanography, analytical technique: ICP mass spectrometry, , N ## 230Th.dpm.err 230Th concentration 1 sigma error, , , 1 sigma, , , , ,N ## 238U.dpm 238U concentration, bulk sediment, , dpm/g, , Paleoceanography, analytical technique: ICP mass spectrometry, , N ## 238U.dpm.err 238U concentration 1 sigma error, , , 1 sigma, , , , ,N ## xsTho.dpm 230Th concentration not supported by radioactive decay of uranium in the sediments - decay corrected to the time of sediment deposition, bulk sediment, , dpm/g, , Paleoceanography, analytical technique: ICP mass spectrometry, , N ## xsTho.dpm.err xsTho.dpm 1 sigma error, , , 1 sigma, , , , ,N ## Lithogenic% Fraction of bulk sediment consisting of lithogenic phases - calculated assuming 10 ppm 232Th in the lithogenic phase, bulk sediment, ,dpm/g, , Paleoceanography,analytical technique: ICP mass spectrometry, , N ## carb% Calcium Carbonate, bulk sediment, ~3%, %, , Paleoceanography, analytical technique: Coulometry, , N ## opal% Opal, bulk sediment, ~3%, %, , Paleoceanography, Alkaline leach followed by spectrophotometry - method of Mortlock and Froelich 1989, , N ## corg% Organic Carbon, bulk sediment, ~5%, %, , Paleoceanography, analytical technique: Elemental analyzer after removing CaCO3 by addition of sulfurous acid, , N ## uk37 Alkenone saturation index, bulk sediment, , , , Paleoceanography, analytical technique: Solvent extraction followed by gas chromatography, , N ## sst-uk37 Sea Surface Temperature from Uk'37, , , deg C, , Paleoceanography, , , N ## Alkng/g Alkenones, bulk sediment, , ng/g, , Paleoceanography, analytical technique: Solvent extraction followed by gas chromatography, , N ## sedflux Sediment flux, bulk sediment, , g/cm2/kr, , Paleoceanography, analytical technique: Derived from water depth and xsTho_dpm_g, , N ## sedflux.err Sediment flux 1 sigma error, , , 1 sigma, , , , , N #--------------------------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Values: depth_cm age_calkaBP 232Th.dpm 232Th.dpm.err 230Th.dpm 230Th.dpm.err 238U.dpm 238U.dpm.err xsTho.dpm xsTho.dpm.err Lithogenic% carb% opal% corg% uk37 sst-uk37 Alkng/g sedflux sedflux.err 0.5 8.00 0.2214 0.0036 7.301 0.155 0.22814 0.00347 7.73 0.17 8.53 86.24 1.14 0.14 0.4333 11.60 48.37 1.28 0.03 2.5 8.34 0.1836 0.0012 7.643 0.051 0.19418 0.00013 8.15 0.06 7.08 0.4183 11.16 29.69 1.21 0.01 4.5 8.68 0.1643 0.0009 7.190 0.045 0.16696 0.00011 7.69 0.05 6.33 0.4252 11.36 21.17 1.28 0.01 6.5 9.02 0.1592 0.0010 7.047 0.044 0.15855 0.00013 7.56 0.05 6.14 0.4383 11.74 16.68 1.30 0.01 8.5 9.37 0.1650 0.0009 7.100 0.033 0.16279 0.00017 7.64 0.04 6.36 0.4940 13.38 18.03 1.29 0.01 10.5 9.71 0.1816 0.0024 7.666 0.113 0.16123 0.00177 8.28 0.13 7.00 85.87 3.57 0.15 0.3992 10.59 13.99 1.19 0.02 12.5 10.05 0.1747 0.0010 7.259 0.034 0.15059 0.00013 7.86 0.04 6.73 0.3294 8.54 1.25 0.01 14.5 10.39 0.1630 0.0007 6.698 0.037 0.14704 0.00011 7.27 0.04 6.28 0.4116 10.96 8.94 1.36 0.01 16.5 10.73 0.1596 0.0008 6.462 0.039 0.14105 0.00012 7.04 0.05 6.15 0.3966 10.52 11.12 1.40 0.01 18.5 11.07 0.1491 0.0007 5.836 0.031 0.12654 0.00007 6.37 0.04 5.74 0.4571 12.30 9.00 1.55 0.01 21.5 11.58 0.1684 0.0020 6.082 0.116 0.13762 0.00152 6.67 0.13 6.49 87.11 2.91 0.14 1.48 0.03 22.5 11.76 0.1400 0.0007 5.653 0.032 0.12133 0.00009 6.22 0.04 5.39 0.4103 10.92 15.61 1.59 0.01 24.5 12.10 0.1347 0.0008 5.458 0.034 0.11451 0.00009 6.02 0.04 5.19 0.4234 11.31 8.33 1.64 0.01 25.5 12.27 0.1321 0.0024 5.769 0.077 0.12315 0.00175 6.38 0.09 5.09 1.55 0.02 26.5 12.44 0.1486 0.0009 5.489 0.032 0.11965 0.00011 6.07 0.04 5.72 0.4264 11.40 9.58 1.63 0.01 28.5 12.78 0.1713 0.0009 5.817 0.032 0.12566 0.00009 6.44 0.04 6.60 0.4025 10.69 10.74 1.53 0.01 30.5 13.04 0.4001 10.62 9.75 31.5 13.29 0.1860 0.0045 6.331 0.101 0.13479 0.00326 7.04 0.12 7.17 85.29 3.28 0.16 1.40 0.02 32.5 13.46 0.1769 0.0009 5.660 0.034 0.12169 0.00009 6.30 0.04 6.82 0.4141 11.03 15.24 1.57 0.01 34.5 13.80 0.2011 0.0010 5.569 0.029 0.12780 0.00009 6.21 0.04 7.75 0.4494 12.07 11.99 1.59 0.01 36.5 14.14 0.1826 0.0010 5.591 0.040 0.11842 0.00010 6.26 0.05 7.04 0.4255 11.37 16.58 1.58 0.01 38.5 14.49 0.1811 0.0010 5.443 0.039 0.11885 0.00009 6.11 0.05 6.98 0.4248 11.35 12.09 1.61 0.01 40.5 14.83 0.2315 0.0026 6.066 0.178 0.14131 0.00209 6.82 0.21 8.92 83.49 3.27 0.15 0.4042 10.74 18.05 1.45 0.04 42.5 15.17 0.2568 0.0010 5.896 0.037 0.13937 0.00011 6.63 0.05 9.89 0.3678 9.67 15.85 1.49 0.01 44.5 15.51 0.2852 0.0013 6.018 0.030 0.14499 0.00009 6.78 0.05 10.99 0.3896 10.31 17.43 1.46 0.01 46.5 15.85 0.2534 0.0010 5.865 0.039 0.14824 0.00012 6.64 0.05 9.76 0.4157 11.08 12.09 1.49 0.01 48.5 16.19 0.3726 0.0017 6.551 0.034 0.18492 0.00010 7.39 0.06 14.36 0.3481 9.09 14.17 1.33 0.01 49.5 16.36 0.3773 0.0043 6.587 0.197 0.17044 0.00550 7.44 0.23 14.54 83.60 3.41 0.15 1.33 0.04 50.5 16.53 0.3282 8.51 19.16 51.5 16.71 0.4224 0.0059 7.152 0.175 0.21051 0.00293 8.10 0.21 16.28 1.22 0.03 52.5 16.88 0.4605 0.0025 6.982 0.049 0.21544 0.00017 7.89 0.08 17.75 0.3473 9.07 24.46 1.25 0.01 54.5 17.22 0.5846 0.0036 7.794 0.061 0.27392 0.00019 8.79 0.10 22.53 0.3805 9.50 29.32 1.12 0.01 56.5 17.56 0.6875 0.0211 8.423 0.214 0.34377 0.00149 9.50 0.26 26.49 0.3841 9.91 82.14 1.04 0.03 58.5 17.90 0.7829 0.0051 7.427 0.040 0.41432 0.00030 8.29 0.10 30.17 0.3598 9.38 131.35 1.19 0.02 60.5 18.37 0.8414 0.0129 8.219 0.083 0.53393 0.00596 9.21 0.14 32.42 69.72 5.97 0.29 0.2142 5.39 210.80 1.07 0.02 62.5 18.85 0.8612 0.0051 7.694 0.058 0.64244 0.00041 8.60 0.13 33.19 0.3299 8.56 383.40 1.15 0.02 64.5 19.32 0.8499 0.0043 7.778 0.046 0.79042 0.00044 8.70 0.12 32.75 0.3724 9.80 526.20 1.13 0.02 66.5 19.79 0.8639 0.0057 7.664 0.047 1.05283 0.00059 8.54 0.12 33.29 0.3656 9.60 606.54 1.16 0.02 68.5 20.27 0.8218 0.0054 7.480 0.046 1.26323 0.00097 8.32 0.11 31.67 0.3901 10.33 573.65 1.19 0.02 70.5 20.74 0.8778 0.0197 8.050 0.214 1.67304 0.01777 8.92 0.28 33.83 59.42 6.81 0.57 0.4021 10.68 519.80 1.11 0.03 72.5 21.21 0.9679 0.0060 8.759 0.073 2.71540 0.00138 9.51 0.15 37.30 0.4015 10.66 603.91 1.04 0.02 74.5 21.69 1.0806 0.0098 9.546 0.078 3.24456 0.00252 10.32 0.17 41.64 0.3881 10.27 523.05 0.96 0.02 76.5 22.16 1.0304 0.0060 9.728 0.061 4.29992 0.00424 10.33 0.15 39.70 0.4514 11.92 525.72 0.96 0.01 78.5 22.63 1.0933 0.0092 10.257 0.093 5.18605 0.00356 10.74 0.18 42.13 0.3919 10.38 604.58 0.92 0.02 80.5 23.10 1.3057 0.0159 11.172 0.191 5.00311 0.05569 11.84 0.29 50.32 47.05 11.51 0.63 0.3832 10.12 596.03 0.83 0.02 82.5 23.58 1.2198 0.0081 11.134 0.075 5.85371 0.00477 11.63 0.18 47.00 0.4052 10.77 640.55 0.85 0.01 84.5 24.05 1.3436 0.0139 11.847 0.097 5.69793 0.00554 12.53 0.21 51.77 0.4003 10.63 623.94 0.79 0.01 86.5 24.52 1.3274 0.0061 11.936 0.064 5.97103 0.00266 12.60 0.19 51.15 0.3937 10.43 650.53 0.78 0.01 88.5 25.00 1.3446 0.0079 11.630 0.079 5.79215 0.00456 12.29 0.20 51.82 0.4062 10.80 646.36 0.80 0.01 90.5 25.47 46.71 8.77 0.68 0.4239 11.32 548.59 91.5 25.71 1.2486 0.0438 10.839 0.292 5.54181 0.06589 11.45 0.41 48.11 0.86 0.03 92.5 25.94 1.1944 0.0050 11.080 0.054 5.81833 0.00298 11.71 0.17 46.03 0.4237 11.31 622.75 0.84 0.01 94.5 26.42 1.1759 0.0049 10.878 0.048 5.44119 0.00330 11.61 0.17 45.31 0.4218 11.26 579.91 0.85 0.01 96.5 26.89 1.1854 0.0047 11.034 0.056 5.34929 0.00282 11.86 0.17 45.68 0.4168 11.11 616.35 0.83 0.01 98.5 27.36 1.1739 0.0043 10.133 0.042 4.66528 0.00209 10.96 0.17 45.24 0.4442 11.92 462.25 0.90 0.01 99.5 27.60 1.2786 0.0424 11.100 0.405 5.11014 0.09719 12.02 0.55 49.27 45.67 10.87 0.64 0.82 0.04 100.5 27.92 0.4432 11.89 509.32 102.5 28.56 1.1400 0.0042 11.190 0.058 3.45493 0.00172 12.83 0.17 43.93 0.4191 11.18 485.90 0.77 0.01 104.5 29.20 1.1322 0.0043 11.028 0.058 3.45361 0.00145 12.68 0.17 43.63 0.3591 9.42 441.03 0.78 0.01 106.5 29.84 1.1217 0.0048 10.590 0.056 3.44489 0.00144 12.17 0.17 43.22 0.3899 10.32 531.81 0.81 0.01 108.5 30.48 1.0921 0.0045 10.020 0.064 3.19928 0.00143 11.57 0.17 42.09 0.3781 9.97 556.87 0.85 0.01 110.5 31.12 1.0294 0.0161 9.077 0.112 2.86551 0.03552 10.52 0.21 39.67 53.67 7.89 0.60 0.3721 9.80 517.81 0.94 0.02 112.5 31.76 0.8417 0.0042 8.200 0.065 2.96455 0.00157 9.44 0.15 32.44 0.3580 9.38 383.03 1.04 0.02 114.5 32.40 0.7559 0.0037 7.667 0.035 2.72853 0.00143 8.90 0.12 29.13 0.4063 10.80 344.92 1.11 0.01 116.5 33.04 0.7513 0.0041 7.552 0.057 2.53920 0.00156 8.86 0.13 28.95 0.3726 9.81 302.88 1.11 0.02 118.5 33.68 0.7380 0.0032 7.570 0.041 2.55738 0.00136 8.92 0.12 28.44 0.3583 9.39 314.12 1.11 0.01 120.5 34.32 0.3502 9.15 374.93 121.5 34.64 0.7270 0.0123 7.154 0.205 2.33325 0.02753 8.51 0.30 28.01 69.36 5.67 0.46 1.16 0.04 122.5 34.96 0.7086 0.0032 7.039 0.039 2.14200 0.00105 8.46 0.12 27.31 0.3434 9.04 314.13 1.17 0.02 124.5 35.60 0.6284 0.0033 6.747 0.038 1.95319 0.00111 8.21 0.11 24.22 0.2808 7.11 415.95 1.20 0.02 126.5 36.24 0.5666 0.0029 5.959 0.041 1.69725 0.00100 7.29 0.10 21.83 0.3035 7.78 354.71 1.35 0.02 128.5 36.88 0.5436 0.0026 5.547 0.039 1.39838 0.00092 6.89 0.10 20.95 0.3120 8.53 244.72 1.43 0.02 130.5 37.19 0.5896 0.0132 5.823 0.169 1.27047 0.01941 7.36 0.26 22.72 75.08 4.60 0.25 0.3144 8.10 250.44 1.34 0.05 132.5 37.49 0.6513 0.0027 6.251 0.037 1.25782 0.00069 7.98 0.11 25.10 0.2930 7.47 240.00 1.24 0.02 134.5 37.80 0.6390 0.0032 6.417 0.040 1.09474 0.00058 8.34 0.11 24.62 0.3040 7.80 242.33 1.18 0.02 136.5 38.29 0.6701 0.0025 6.296 0.028 1.06553 0.00047 8.20 0.11 25.82 0.3060 7.85 319.41 1.20 0.02 138.5 38.78 0.6570 0.0025 5.634 0.028 1.02752 0.00047 7.30 0.11 25.32 0.2637 6.61 378.52 1.35 0.02 140.5 39.27 0.7391 0.0088 5.532 0.162 1.15351 0.01666 7.08 0.26 28.48 69.23 5.34 0.32 0.2938 7.50 406.21 1.39 0.05 142.5 39.76 0.7308 0.0025 5.489 0.032 1.26737 0.00064 6.99 0.12 28.16 0.2810 7.12 418.07 1.41 0.02 144.5 40.25 0.7455 0.0029 5.424 0.027 1.27712 0.00053 6.91 0.12 28.73 0.2785 7.04 437.87 1.43 0.03 146.5 40.74 0.8264 0.0031 5.727 0.034 1.42241 0.00063 7.26 0.14 31.85 0.2852 7.24 513.50 1.36 0.03 148.5 41.23 0.8738 0.0038 5.542 0.024 1.47199 0.00069 6.97 0.14 33.67 0.2772 7.01 499.45 1.42 0.03 150.5 41.72 1.0524 0.0155 5.357 0.187 1.57409 0.02048 6.58 0.32 40.55 61.99 4.91 0.46 0.2630 6.59 505.29 1.50 0.07 152.5 42.21 1.0082 0.0039 5.204 0.027 1.57853 0.00073 6.40 0.16 38.85 1.54 0.04 154.5 42.70 1.0087 0.0043 5.364 0.026 1.71305 0.00077 6.58 0.17 38.87 0.2706 6.81 545.55 1.50 0.04 156.5 43.19 1.0788 0.0039 5.949 0.032 1.82633 0.00093 7.39 0.18 41.57 0.2620 6.56 441.04 1.33 0.03 158.5 43.68 1.1042 0.0044 6.582 0.029 2.08799 0.00093 8.21 0.18 42.55 0.2385 5.87 578.56 1.20 0.03 160.5 44.17 0.2414 5.95 531.84 161.5 44.42 1.1489 0.0242 6.684 0.233 2.17177 0.03403 8.34 0.40 44.27 61.44 4.23 0.36 1.18 0.06 162.5 44.66 1.0234 0.0040 6.408 0.030 2.19587 0.00081 7.98 0.17 39.44 0.2764 6.98 260.57 1.24 0.03 164.5 45.15 0.9340 0.0035 6.362 0.028 2.01922 0.00079 8.09 0.16 35.99 0.2784 7.04 263.18 1.22 0.02 166.5 45.65 0.9087 0.0035 6.160 0.032 1.87557 0.00081 7.91 0.16 35.02 0.2701 6.80 318.62 1.25 0.02 168.5 46.14 0.7296 0.0027 6.055 0.026 1.59818 0.00070 8.03 0.13 28.12 0.2717 6.85 267.04 1.23 0.02 170.5 46.63 0.7963 0.0112 6.523 0.138 1.45981 0.03622 8.84 0.25 30.68 74.93 4.48 0.25 0.2974 7.60 318.09 1.12 0.03 172.5 47.12 0.8895 0.0035 6.574 0.035 1.30996 0.00064 9.01 0.16 34.28 0.3074 7.89 467.67 1.10 0.02 174.5 47.61 0.9703 0.0039 6.241 0.038 1.11773 0.00053 8.61 0.17 37.39 0.2942 7.51 502.36 1.15 0.02 176.5 48.10 1.0738 0.0041 5.813 0.036 1.02491 0.00041 7.99 0.19 41.38 0.2633 6.60 733.06 1.23 0.03 178.5 48.59 1.1716 0.0048 5.824 0.037 1.02982 0.00043 7.99 0.21 45.15 0.2374 5.83 525.39 1.23 0.03 180.5 49.08 0.2386 5.87 463.80 181.5 49.32 1.1847 0.0128 5.567 0.099 0.95880 0.01010 7.68 0.26 45.65 58.98 5.04 0.41 1.28 0.04 182.5 49.57 1.1257 0.0043 5.585 0.031 0.96587 0.00044 7.75 0.20 43.38 0.2645 6.63 405.37 1.27 0.03 184.5 50.06 1.0559 0.0035 5.448 0.023 0.90183 0.00048 7.64 0.19 40.69 0.2625 6.57 367.23 1.29 0.03 186.5 50.55 1.1665 0.0041 5.323 0.029 1.01990 0.00047 7.34 0.21 44.95 0.2641 6.62 367.54 1.34 0.04 188.5 51.04 1.2876 0.0046 5.161 0.029 1.12342 0.00061 6.98 0.23 49.62 0.2559 6.38 318.33 1.41 0.05 190.5 51.53 1.2947 0.0147 5.258 0.090 1.17339 0.01227 7.13 0.27 49.89 71.23 4.87 0.32 0.3201 8.27 1.38 0.05 192.5 52.02 0.7393 0.0028 5.739 0.027 1.11256 0.00060 8.25 0.14 28.49 0.3419 8.91 151.50 1.20 0.02 194.5 52.51 0.6540 0.0027 5.967 0.047 1.24429 0.00062 8.60 0.14 25.20 0.3478 9.08 162.08 1.15 0.02 196.5 53.00 0.5626 0.0021 6.375 0.033 1.47908 0.00073 9.18 0.12 21.68 0.3617 9.49 149.15 1.07 0.01 198.5 53.67 0.5825 0.0020 6.491 0.029 1.61483 0.00102 9.30 0.12 22.45 0.3470 9.06 233.84 1.06 0.01 200.5 54.34 0.6281 0.0127 6.140 0.236 1.39519 0.01448 8.90 0.41 24.20 72.83 5.33 0.21 0.3705 9.75 203.66 1.11 0.05 202.5 55.02 0.5701 0.0023 5.784 0.032 1.25632 0.00068 8.47 0.12 21.97 0.3743 9.86 201.68 1.16 0.02 204.5 55.69 0.6186 0.0021 5.456 0.037 1.26061 0.00057 7.93 0.13 23.84 0.3671 9.65 172.19 1.24 0.02 206.5 56.36 0.5261 0.0018 5.103 0.025 0.92305 0.00042 7.67 0.11 20.27 0.3511 9.18 199.02 1.29 0.02 208.5 57.03 0.5258 0.0020 5.375 0.028 0.83736 0.00040 8.23 0.11 20.26 0.3551 9.30 171.93 1.20 0.02 210.5 57.71 0.3584 9.39 166.70 211.5 58.04 0.5724 0.0120 5.270 0.143 0.63695 0.00683 8.25 0.27 22.06 75.65 5.01 0.24 1.20 0.04 212.5 58.38 0.4996 0.0020 4.979 0.021 0.58775 0.00032 7.84 0.10 19.25 0.3588 9.40 150.01 1.26 0.02 214.5 59.05 0.5083 0.0020 5.207 0.035 0.53325 0.00029 8.31 0.11 19.59 0.3567 9.34 213.08 1.19 0.02 216.5 59.57 0.5535 0.0019 5.241 0.028 0.49695 0.00025 8.41 0.12 21.33 0.3692 9.71 204.95 1.17 0.02 218.5 60.09 0.6989 0.0027 5.466 0.029 0.49742 0.00024 8.78 0.14 26.93 0.3924 10.39 235.53 1.12 0.02 220.5 60.61 0.3974 10.54 259.46 221.5 60.87 0.7948 0.0088 5.613 0.072 0.44106 0.00502 9.10 0.20 30.63 68.87 6.04 0.20 1.08 0.02 222.5 61.13 0.7320 0.0027 5.344 0.025 0.47735 0.00027 8.65 0.15 28.21 0.4211 11.24 281.02 1.14 0.02 224.5 61.64 0.7996 0.0030 5.567 0.023 0.49172 0.00025 9.04 0.16 30.81 0.4361 11.68 291.50 1.09 0.02 226.5 62.16 0.8326 0.0031 5.646 0.023 0.49305 0.00018 9.21 0.17 32.08 0.4457 11.96 327.84 1.07 0.02 228.5 62.68 0.8408 0.0032 5.475 0.024 0.49862 0.00020 8.94 0.17 32.40 0.4405 11.81 354.99 1.10 0.02 230.5 63.20 0.9053 0.0222 5.461 0.089 0.49620 0.00714 8.93 0.24 34.88 61.72 6.71 0.34 0.4384 11.75 336.82 1.10 0.03 232.5 63.70 0.8276 0.0029 5.427 0.023 0.48702 0.00018 8.95 0.17 31.89 0.4316 11.55 375.99 1.10 0.02 234.5 64.19 0.8395 0.0030 5.501 0.023 0.51445 0.00020 9.09 0.17 32.35 0.4269 11.41 425.80 1.08 0.02 236.5 64.69 0.8330 0.0030 5.389 0.020 0.51546 0.00019 8.93 0.17 32.10 0.4189 11.17 557.60 1.10 0.02 238.5 65.18 0.7944 0.0030 5.240 0.022 0.51199 0.00021 8.72 0.17 30.61 0.4212 11.24 453.65 1.13 0.02 240.5 65.68 68.47 6.21 0.31 0.4032 10.71 482.23 241.5 65.92 0.8016 0.0153 5.005 0.165 0.48748 0.00723 8.37 0.35 30.89 1.18 0.05 242.5 66.17 0.7424 0.0028 4.946 0.023 0.52575 0.00021 8.27 0.16 28.61 0.4132 11.01 490.79 1.19 0.02 244.5 66.67 0.7168 0.0027 4.883 0.020 0.51816 0.00021 8.21 0.15 27.62 0.4013 10.66 571.20 1.20 0.02 246.5 67.16 0.6574 0.0023 4.408 0.020 0.50570 0.00021 7.40 0.14 25.33 0.3715 9.78 553.28 1.33 0.03 248.5 67.66 0.6667 0.0028 4.608 0.023 0.55237 0.00024 7.76 0.15 25.69 0.3765 9.93 572.53 1.27 0.02 249.5 67.90 0.7657 0.0099 4.759 0.160 0.54940 0.00919 8.02 0.34 29.51 68.11 5.99 0.31 1.23 0.05 250.5 68.15 0.3897 10.31 250.56 252.5 68.65 0.6586 0.0024 4.628 0.021 0.68714 0.00027 7.74 0.15 25.38 0.3792 10.01 442.24 1.28 0.02 254.5 69.14 0.6037 0.0022 4.586 0.020 0.73072 0.00027 7.67 0.13 23.26 0.3655 9.60 489.53 1.29 0.02 256.5 69.64 0.5094 0.0031 4.312 0.030 0.78216 0.00034 7.17 0.12 19.63 0.3677 9.67 358.08 1.38 0.02 258.5 70.13 0.4552 0.0016 4.071 0.021 0.92351 0.00038 6.62 0.11 17.54 0.3635 9.54 181.54 1.49 0.02 260.5 70.63 0.3721 9.80 157.35 261.5 70.88 0.4563 0.0048 3.770 0.052 1.07924 0.01124 5.92 0.14 17.58 78.78 3.38 0.21 1.67 0.04 262.5 71.12 0.3778 0.0015 3.826 0.018 1.28344 0.00047 5.86 0.09 14.56 0.3722 9.80 172.29 1.68 0.03 264.5 71.62 0.4738 0.0020 6.013 0.031 1.61533 0.00074 9.73 0.12 18.26 0.3835 10.13 197.81 1.01 0.01 266.5 72.11 0.4939 0.0018 6.298 0.025 1.81457 0.00069 10.10 0.12 19.03 0.3870 10.23 131.61 0.98 0.01 268.5 72.61 0.4946 0.0020 6.031 0.027 1.74587 0.00077 9.69 0.12 19.06 0.3819 10.08 222.18 1.02 0.01 270.5 73.10 0.5375 0.0142 6.255 0.283 1.67512 0.01746 10.22 0.57 20.71 79.92 3.58 0.18 0.3886 10.28 232.65 0.97 0.05 272.5 73.60 0.4383 0.0015 5.712 0.024 1.65889 0.00062 9.25 0.11 16.89 0.3869 10.23 238.20 1.07 0.01 274.5 74.19 0.4830 0.0017 5.842 0.026 1.52182 0.00068 9.68 0.12 18.61 0.3851 10.18 220.35 1.02 0.01 276.5 74.78 0.4100 0.0013 5.413 0.024 1.45102 0.00059 8.98 0.11 15.80 0.4119 10.97 106.67 1.10 0.01 278.5 75.38 0.3873 0.0014 5.187 0.027 1.30368 0.00058 8.75 0.10 14.92 0.4143 11.04 104.51 1.13 0.01 280.5 75.97 0.4138 11.02 119.13 281.5 76.27 0.4151 0.0045 4.903 0.076 0.89685 0.01075 8.69 0.18 15.99 83.03 1.59 0.14 1.13 0.02 282.5 76.56 0.4049 0.0014 4.980 0.025 0.81251 0.00032 8.97 0.11 15.60 0.4220 11.27 95.10 1.10 0.01 284.5 77.15 0.4066 0.0014 4.882 0.025 0.69066 0.00026 8.96 0.11 15.67 0.4058 10.79 123.02 1.10 0.01 286.5 77.75 0.3578 0.0013 4.383 0.017 0.52043 0.00022 8.20 0.09 13.79 0.4071 10.83 118.05 1.20 0.01 288.5 78.34 0.3512 0.0011 4.345 0.022 0.41287 0.00015 8.30 0.09 13.53 0.4153 11.07 79.62 1.19 0.01 290.5 78.93 0.4105 10.93 75.12 291.5 79.23 0.3285 0.0065 3.878 0.046 0.32756 0.00389 7.51 0.12 12.66 84.37 1.46 0.16 1.31 0.02 292.5 79.52 0.2754 0.0010 3.664 0.019 0.31861 0.00014 7.12 0.08 10.61 0.4186 11.17 78.08 1.39 0.02 294.5 80.12 0.2586 0.0009 3.532 0.017 0.27717 0.00013 6.94 0.07 9.96 0.3938 10.44 69.83 1.42 0.01 296.5 80.71 0.2424 0.0009 3.346 0.017 0.25714 0.00011 6.62 0.07 9.34 0.4140 11.03 50.98 1.49 0.02 298.5 81.30 0.2370 0.0008 3.267 0.018 0.24629 0.00010 6.50 0.07 9.13 0.4204 11.22 42.14 1.52 0.02 300.5 81.89 0.2743 0.0077 3.557 0.217 0.22405 0.00436 7.16 0.47 10.57 87.26 0.82 0.11 0.4093 10.89 47.57 1.38 0.09 302.5 82.48 0.2716 0.0009 3.483 0.018 0.26498 0.00011 6.99 0.08 10.46 0.3908 10.35 85.23 1.41 0.02 304.5 83.08 0.2360 0.0008 3.213 0.016 0.20592 0.00010 6.54 0.07 9.09 0.4294 11.48 40.37 1.51 0.02 306.5 83.67 0.2598 0.0009 3.352 0.017 0.18558 0.00009 6.89 0.08 10.01 0.3830 10.12 57.43 1.43 0.02 308.5 84.26 0.2519 0.0009 3.189 0.017 0.16584 0.00008 6.61 0.07 9.71 0.4029 10.70 47.34 1.49 0.02 310.5 84.85 0.3739 9.85 57.44 311.5 85.15 0.2877 0.0039 3.356 0.041 0.13666 0.00190 7.05 0.12 11.09 86.90 2.39 0.12 1.40 0.02 312.5 85.45 0.2985 0.0012 3.419 0.015 0.15193 0.00008 7.18 0.08 11.50 0.3948 10.46 51.84 1.37 0.02 314.5 86.04 0.3031 0.0010 3.367 0.017 0.14277 0.00006 7.12 0.09 11.68 0.4681 12.62 89.03 1.39 0.02 316.5 86.63 0.3197 0.0010 3.595 0.015 0.14601 0.00009 7.65 0.09 12.32 0.4060 10.80 61.95 1.29 0.02 318.5 87.22 0.4307 0.0015 3.944 0.016 0.17779 0.00009 8.38 0.12 16.60 0.4188 11.17 91.26 1.18 0.02 320.5 87.82 0.4283 11.45 92.82 321.5 88.11 0.4660 0.0074 3.927 0.079 0.16554 0.00193 8.41 0.22 17.96 81.99 2.73 1.17 0.03 322.5 88.41 0.4917 0.0016 4.135 0.020 0.20316 0.00010 8.84 0.14 18.95 0.4259 11.38 85.29 1.12 0.02 324.5 89.00 0.5404 0.0018 4.066 0.020 0.22664 0.00012 8.68 0.15 20.83 0.4344 11.63 99.81 1.14 0.02 326.5 89.39 0.4998 0.0017 3.973 0.019 0.22535 0.00011 8.52 0.14 19.26 0.4496 12.08 82.79 1.16 0.02 328.5 89.79 0.4233 0.0015 3.724 0.016 0.17881 0.00009 8.08 0.12 16.31 0.4281 11.45 64.74 1.22 0.02 330.5 90.18 0.4441 11.91 88.31 331.5 90.38 0.4442 0.0051 3.804 0.056 0.16684 0.00240 8.32 0.18 17.12 83.68 2.90 1.19 0.03 332.5 90.57 0.3875 0.0014 3.675 0.020 0.17479 0.00010 8.05 0.12 14.93 0.4145 11.04 71.17 1.23 0.02 334.5 90.96 0.3405 0.0012 3.398 0.017 0.15526 0.00007 7.49 0.10 13.12 0.3979 10.56 69.21 1.32 0.02 336.5 91.36 0.3426 0.0012 3.690 0.015 0.14759 0.00008 8.20 0.10 13.20 0.3741 9.86 76.77 1.20 0.01 338.5 91.75 0.3232 0.0011 3.587 0.015 0.13612 0.00007 8.02 0.10 12.46 0.3894 10.31 86.81 1.23 0.01 340.5 92.14 0.3721 9.80 99.97 341.5 92.34 0.3498 0.0042 3.541 0.111 0.12423 0.00196 7.96 0.28 13.48 83.74 2.87 1.24 0.04 342.5 92.54 0.3166 0.0011 3.373 0.015 0.13973 0.00007 7.57 0.10 12.20 0.3749 9.88 73.45 1.30 0.02 344.5 92.93 0.3337 0.0012 3.370 0.018 0.15026 0.00006 7.57 0.10 12.86 1.30 0.02 346.5 93.32 0.3905 10.34 45.68 348.5 93.71 0.3438 0.0012 3.538 0.017 0.15583 0.00007 7.98 0.10 13.25 0.3905 10.34 45.68 1.24 0.02 350.5 94.11 0.3101 0.0010 3.325 0.016 0.14366 0.00007 7.53 0.10 11.95 84.65 1.08 1.31 0.02 352.5 94.50 0.2972 0.0011 3.605 0.017 0.13002 0.00007 8.29 0.09 11.45 1.19 0.01 354.5 94.89 0.2877 0.0011 3.550 0.018 0.12782 0.00007 8.19 0.09 11.09 1.20 0.01 356.5 95.29 0.2954 0.0011 3.468 0.015 0.13124 0.00006 8.02 0.09 11.38 1.23 0.01 358.5 95.68 0.3120 0.0011 3.662 0.019 0.13916 0.00007 8.49 0.10 12.02 1.16 0.01 360.5 96.07 0.2460 0.0051 3.543 0.047 0.13835 0.00008 8.27 0.13 9.48 1.19 0.02 362.5 96.46 0.3274 0.0015 3.689 0.024 0.15192 0.00008 8.59 0.11 12.62 1.15 0.01 364.5 96.86 0.3051 0.0046 3.612 0.045 0.15038 0.00008 8.45 0.14 11.76 1.17 0.02 366.5 97.25 0.3616 0.0018 3.984 0.023 0.16685 0.00011 9.34 0.12 13.93 1.06 0.01 368.5 97.64 0.3719 0.0019 3.935 0.022 0.16743 0.00010 9.25 0.12 14.33 1.07 0.01 370.5 98.04 0.3584 0.0021 3.830 0.025 0.15561 0.00009 9.05 0.12 13.81 1.09 0.01 372.5 98.43 0.4645 0.0021 4.144 0.022 0.20612 0.00011 9.73 0.15 17.90 1.01 0.02 374.5 98.82 0.4387 0.0026 3.777 0.028 0.19249 0.00013 8.89 0.15 16.90 1.11 0.02 376.5 99.21 0.4360 0.0027 3.737 0.022 0.19160 0.00013 8.82 0.14 16.80 1.12 0.02 378.5 99.61 0.4275 0.0021 3.543 0.019 0.18499 0.00010 8.38 0.14 16.47 1.18 0.02 380.5 100.00 0.4401 0.0026 3.629 0.027 0.19569 0.00012 8.61 0.15 16.96 1.15 0.02 382.5 100.39 0.4145 0.0025 3.717 0.025 0.17729 0.00009 8.90 0.14 15.97 1.11 0.02 384.5 100.79 0.3658 0.0022 3.399 0.023 0.15392 0.00008 8.19 0.13 14.10 1.20 0.02 386.5 101.18 0.4984 0.0022 3.859 0.028 0.18491 0.00010 9.28 0.17 19.21 1.06 0.02 388.5 101.57 0.4615 0.0027 3.807 0.025 0.18770 0.00011 9.19 0.16 17.78 1.07 0.02 390.5 101.96 0.4347 0.0023 3.692 0.020 0.17779 0.00011 8.96 0.14 16.75 1.10 0.02