# Alkenone paleotemperature estimates, d18O seawater data, and coarse fraction data from the Gulf of Alaska spanning the past 18,000 years. #----------------------------------------------------------------------- # World Data Service 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/ # Description: NOAA Landing Page # Online_Resource: https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/by_contributor/praetorius2016/praetorius2016-66-d18o.txt # Description: NOAA location of the template # # Archive: Paleoceanography # # Parameter_Keywords: biomarkers, oxygen isotopes, age controls, physical properties, reconstructions #--------------------------------------- # Contribution_Date # Date: 2017-07-18 #--------------------------------------- # File_Last_Modified_Date # Date: 2017-07-18 #--------------------------------------- # Title # Study_Name: Alkenone paleotemperature estimates, d18O seawater data, and coarse fraction data from the Gulf of Alaska spanning the past 18,000 years. #--------------------------------------- # Investigators # Investigators: Praetorius, Summer; Mix, Alan; Jensen, Britta; Froese, Duane; Milne, Glenn; Wolhowe, Matthew; Addison, Jason; Prahl, Fredrick. #--------------------------------------- # Description_Notes_and_Keywords # Description: Source reference for EW0408-66JC and EW0408-26JC age models and planktonic oxygen isotopes: Praetorius, S.K. & Mix, A.C. Synchronization of North Pacific and Greenland climates preceded abrupt deglacial warming. Science 345, 444 (2014). Please cite original reference when using this data. Not all alkenone and isotope samples were taken from precisely the same depth intervals. Some isotope samples were measured on 2cm interval samples, whereas alkenone measurements were conducted on 1cm samples. Therefore, some of the d18O sw calculations are based on alkenone temperature and d18O pairs that have minor offsets in the midpoint depth range. Nearly all of these pairs are within a decade of one another in the age model. # Provided Keywords: volcanism, deglacial, isostatic rebound, abrupt climate change #--------------------------------------- # Publication # Authors: Praetorius, S.K, A.C. Mix, B. Jensen, D. Froese, G. Milne, M.D. Wolhowe, J.A. Addison, and F.G. Prahl # Published_Date_or_Year: 2016 # Published_Title: Interaction between climate, volcanism, and isostatic rebound in Southeast Alaska during the last deglaciation # Journal_Name: Earth and Planetary Science Letters # Volume: 452 # Edition: # Issue: # Pages: 79-89 # Report Number: # DOI: 10.1016/j.epsl.2016.07.033 # Online_Resource: http://www.sciencedirect.com/science/article/pii/S0012821X16303892 # Full_Citation: # Abstract: Observations of enhanced volcanic frequency during the last deglaciation have led to the hypothesis that ice unloading in glaciated volcanic terrains can promote volcanism through decompression melting in the shallow mantle or a reduction in crustal magma storage time. However, a direct link between regional climate change, isostatic adjustment, and the initiation of volcanism remains to be demonstrated due to the difficulty of obtaining high-resolution well-dated records that capture short-term climate and volcanic variability traced to a particular source region. Here we present an exceptionally resolved record of 19 tephra layers paired with foraminiferal oxygen isotopes and alkenone paleotemperatures from marine sediment cores along the Southeast Alaska margin spanning the last deglacial transition. Major element compositions of the tephras indicate a predominant source from the nearby Mt. Edgecumbe Volcanic Field (MEVF). We constrain the timing of this regional eruptive sequence to 14.6–13.1 ka. The sudden increase in volcanic activity from the MEVF coincides with the onset of Bølling–Allerød interstadial warmth, the disappearance of ice-rafted detritus, and rapid vertical land motion associated with modeled regional isostatic rebound in response to glacier retreat. These data support the hypothesis that regional deglaciation can rapidly trigger volcanic activity. Rapid sea surface temperature fluctuations and an increase in local salinity (i.e., d18Osw) variability are associated with the interval of intense volcanic activity, consistent with a two-way interaction between climate and volcanism in which rapid volcanic response to ice unloading may in turn enhance short-term melting of the glaciers, plausibly via albedo effects on glacier ablation zones. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: National Science Foundation # Grant: AGS-0602395, OCE-1204204 #--------------------------------------- # Site Information # Site_Name: EW0408-66JC # Location: Gulf of Alaska # Country: # Northernmost_Latitude: 58.87 # Southernmost_Latitude: 58.87 # Easternmost_Longitude: -137.1 # Westernmost_Longitude: -137.1 # Elevation: -426 #--------------------------------------- # Data_Collection # Collection_Name: EW0408-66JC d18O Praetorius2016 # First_Year: 13570 # Last_Year: 4200 # Time_Unit: cal yr BP # Core_Length: 13.79 # Notes: #--------------------------------------- # Chronology_Information # Chronology: # All radiocarbon data published in Praetorius & Mix, Science 345, 444 (2014): please cite original reference when using this data # Core core name # Depth midpoint depth in core # 14C Age calibrated radiocarbon age mixed planktonic foraminifera # 14C uncertainty radiocarbon age uncertainty NaN one standard deviation yr # Marine reservoir correction total marine reservoir correction NaN NaN yr # Marine13 age 2 s lower lower range of calibrated radiocarbon age NaN two standard deviation cal yr BP Calibrated using Marine13 (Reimer et al., 2013) # Marine13 age 2 s upper upper range of calibrated radiocarbon age NaN NaN cal yr BP Calibrated using Marine13 (Reimer et al., 2013) # Marine13 midpoint age midpoint age of calibrated radiocarbon age NaN NaN cal yr BP NaN # Tuned age controls tuned age controls allowing for variable marine reservoir age NaN NaN cal yr BP Tuned age based on tied d18O stratigraphy # Data NaN NaN NaN NaN NaN # All radiocarbon data published in Praetorius & Mix, Science 345, 444 (2014): please cite original reference when using this data NaN NaN NaN NaN NaN # Core Depth 14C Age 14C uncertainty Marine reservoir correction Marine13 age 2 s lower Marine13 age 2 s upper Marine13 midpoint age Tuned age controls # # EW0408-66JC 10.5 4585 20 595 + 50 4440 4725 4560 4560 # EW0408-66JC 53 8100 20 595 + 50 8245 8501 8370 8370 # EW0408-66JC 65 8695 25 595 + 50 8985 9279 9130 9130 # EW0408-66JC 85 10610 30 595 + 50 11254 11800 11530 11610 # EW0408-66JC 110 10730 40 595 + 50 11390 12023 11710 11710 # EW0408-66JC 151 10755 25 595 + 50 11450 12048 11750 NaN # EW0408-66JC 205 10900* 30 NaN NaN NaN NaN NaN # EW0408-66JC 215 10895 40 595 + 50 11841 12423 12130 NaN # EW0408-66JC 305 10930 30 595 + 50 11934 12452 12190 NaN # EW0408-66JC 355 10940 45 595 + 50 11926 12479 12200 12200 # EW0408-66JC 405 11085 35 595 + 50 12148 12597 12370 NaN # EW0408-66JC 455 11135 30 595 + 50 12251 12630 12440 NaN # EW0408-66JC 505 11115* 25 NaN NaN NaN NaN NaN # EW0408-66JC 565 11245 30 595 + 50 12481 12705 12590 NaN # EW0408-66JC 605 11335 35 595 + 50 12550 12764 12660 NaN # EW0408-66JC 705 11475 45 595 + 50 12623 12907 12770 12570 # EW0408-66JC 759 11615 30 595 + 50 12718 13060 12890 12700 # EW0408-66JC 805 11715 30 595 + 50 12809 13154 12980 12830 # EW0408-66JC 860 MEd 11250 50 595 + 50 13032 13222 13130 13130 # EW0408-66JC 904.5 11935 50 595 + 50 13076 13375 13230 13230 # EW0408-66JC 1162 12165* 30 NaN NaN NaN NaN NaN # EW0408-66JC 1273 12155 35 595 + 50 13273 13548 13410 13410 # EW0408-66JC 1370.5 12295 35 595 + 50 13389 13725 13560 13560 # EW0408-66JC 1374.5 12100* 70 NaN NaN NaN NaN NaN # # EW0408-26TC 0 NaN NaN NaN NaN NaN NaN 0 # EW0408-26TC 14.5 NaN NaN NaN NaN NaN NaN 11600 # EW0408-26TC 17.5 10330 40 735 + 50 10813 11133 10970 NaN # EW0408-26TC 31.5 NaN NaN NaN NaN NaN NaN 12700 # EW0408-26TC 47.5 12205 40 735 + 50 13236 13446 13340 13340 # # EW0408-26JC 1 12295 30 735 + 50 13277 13542 13410 13550 # EW0408-26JC 22.5 NaN NaN NaN NaN NaN NaN 13700 # EW0408-26JC 45.5 12855 40 735 + 50 13829 14162 14000 14000 # EW0408-26JC 88.5 13290* 35 NaN NaN NaN NaN NaN # EW0408-26JC 151 13195 30 735 + 50 14229 14991 14610 14610 # EW0408-26JC 180.5 13230 45 735 + 50 14270 15066 14670 14670 # EW0408-26JC 290.5 13840 40 735 + 50 15416 15969 15690 15690 # EW0408-26JC 480.5 15165 40 735 + 50 17369 17832 17600 17600 # EW0408-26JC 500 15235 35 735 + 50 17476 17887 17680 17680 # EW0408-26JC 891 15705 35 735 + 50 17977 18369 18170 18170 # # *Radiocarbon ages that are not included in the age model due to minor age reversals NaN NaN NaN NaN NaN NaN NaN NaN # # MEd: Mt. Edgecumbe dacite NaN NaN NaN NaN NaN NaN NaN NaN # #--------------------------------------- # Variables # Data variables follow that are preceded by "##" in columns one and two. # Variables list, one per line, shortname-tab- 10 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data,additional info ## core Core name,,,,,paleoceanography,,,C, ## depth_m depth,,,m,,,,,N, ## age_marine13 age,planktonic foraminifera,,calendar ka BP,,,constant marine reservoir ages applied to each core,calibrated radiocarbon ages using Marine13,N, ## age_tuned age,,,calendar ka BP,,,tuned age model allowing for variable marine reservoir ages,tie points to NGRIP d18O isotope stratigraphy,N, ## d18O_Nps delta 18O,Neogloboquadrina pachyderma sinistral,,per mil VPDB,Summer,paleoceanography,,analytical technique: isotope ratio mass spectrometry,N, ## d18O_Nps-off delta 18O,Neogloboquadrina pachyderma sinistral,,per mil VPDB,Summer,paleoceanography,0.4 per mil offset applied to core 66JC,,N, #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: NAN core depth_m age_marine13 age_tuned d18O_Nps d18O_Nps-off EW0408-66JC 0.070 4.246 4.246 1.66 2.06 EW0408-66JC 0.110 4.605 4.605 1.69 2.09 EW0408-66JC 0.130 4.784 4.784 1.32 1.72 EW0408-66JC 0.150 4.963 4.963 1.54 1.94 EW0408-66JC 0.170 5.143 5.143 1.40 1.80 EW0408-66JC 0.190 5.322 5.322 1.20 1.60 EW0408-66JC 0.210 5.501 5.501 1.62 2.02 EW0408-66JC 0.230 5.681 5.681 1.49 1.89 EW0408-66JC 0.250 5.860 5.860 1.44 1.84 EW0408-66JC 0.270 6.039 6.039 1.25 1.65 EW0408-66JC 0.290 6.218 6.218 1.45 1.85 EW0408-66JC 0.310 6.398 6.398 1.43 1.83 EW0408-66JC 0.330 6.577 6.577 1.43 1.83 EW0408-66JC 0.350 6.756 6.756 1.43 1.83 EW0408-66JC 0.370 6.936 6.936 1.36 1.76 EW0408-66JC 0.390 7.115 7.115 1.29 1.69 EW0408-66JC 0.410 7.294 7.294 1.15 1.55 EW0408-66JC 0.430 7.474 7.474 1.26 1.66 EW0408-66JC 0.450 7.653 7.653 1.52 1.92 EW0408-66JC 0.470 7.832 7.832 1.32 1.72 EW0408-66JC 0.490 8.011 8.011 1.58 1.98 EW0408-66JC 0.510 8.191 8.191 1.56 1.96 EW0408-66JC 0.530 8.370 8.370 1.47 1.87 EW0408-66JC 0.550 8.497 8.497 1.38 1.78 EW0408-66JC 0.570 8.623 8.623 1.48 1.88 EW0408-66JC 0.590 8.750 8.750 1.66 2.06 EW0408-66JC 0.610 8.877 8.877 1.39 1.79 EW0408-66JC 0.630 9.003 9.003 1.46 1.86 EW0408-66JC 0.650 9.130 9.130 1.55 1.95 EW0408-66JC 0.670 9.370 9.378 1.34 1.74 EW0408-66JC 0.690 9.610 9.626 1.35 1.75 EW0408-66JC 0.710 9.850 9.874 1.44 1.84 EW0408-66JC 0.730 10.090 10.122 1.69 2.09 EW0408-66JC 0.750 10.330 10.370 1.67 2.07 EW0408-66JC 0.770 10.570 10.618 1.53 1.93 EW0408-66JC 0.790 10.810 10.866 1.51 1.91 EW0408-66JC 0.810 11.050 11.114 1.59 1.99 EW0408-66JC 0.830 11.290 11.362 1.49 1.89 EW0408-66JC 0.850 11.530 11.610 1.52 1.92 EW0408-66JC 0.870 11.544 11.618 1.52 1.92 EW0408-66JC 0.890 11.559 11.626 1.69 2.09 EW0408-66JC 0.910 11.573 11.634 1.82 2.22 EW0408-66JC 0.930 11.588 11.642 1.76 2.16 EW0408-66JC 0.950 11.602 11.650 1.98 2.38 EW0408-66JC 0.970 11.616 11.658 1.97 2.37 EW0408-66JC 0.990 11.631 11.666 2.04 2.44 EW0408-66JC 1.030 11.660 11.682 2.21 2.61 EW0408-66JC 1.050 11.674 11.690 2.04 2.44 EW0408-66JC 1.070 11.688 11.698 2.23 2.63 EW0408-66JC 1.100 11.710 11.710 2.14 2.54 EW0408-66JC 1.120 11.712 11.714 2.40 2.80 EW0408-66JC 1.150 11.715 11.720 2.30 2.70 EW0408-66JC 1.170 11.717 11.724 2.21 2.61 EW0408-66JC 1.190 11.719 11.728 2.18 2.58 EW0408-66JC 1.210 11.721 11.732 2.27 2.67 EW0408-66JC 1.230 11.723 11.736 2.12 2.52 EW0408-66JC 1.250 11.725 11.740 1.96 2.36 EW0408-66JC 1.270 11.727 11.744 2.20 2.60 EW0408-66JC 1.290 11.729 11.748 2.23 2.63 EW0408-66JC 1.310 11.730 11.752 2.23 2.63 EW0408-66JC 1.330 11.732 11.756 2.29 2.69 EW0408-66JC 1.350 11.734 11.760 2.26 2.66 EW0408-66JC 1.350 11.734 11.760 2.26 2.66 EW0408-66JC 1.380 11.737 11.766 2.14 2.54 EW0408-66JC 1.390 11.738 11.768 2.24 2.64 EW0408-66JC 1.410 11.740 11.772 2.32 2.72 EW0408-66JC 1.430 11.742 11.776 2.43 2.83 EW0408-66JC 1.450 11.744 11.780 2.22 2.62 EW0408-66JC 1.470 11.746 11.784 1.95 2.35 EW0408-66JC 1.490 11.748 11.788 2.32 2.72 EW0408-66JC 1.510 11.750 11.792 2.11 2.51 EW0408-66JC 1.530 11.762 11.796 2.20 2.60 EW0408-66JC 1.550 11.774 11.800 2.13 2.53 EW0408-66JC 1.570 11.786 11.804 2.32 2.72 EW0408-66JC 1.590 11.798 11.808 2.09 2.49 EW0408-66JC 1.610 11.809 11.812 2.14 2.54 EW0408-66JC 1.630 11.821 11.816 2.28 2.68 EW0408-66JC 1.650 11.833 11.820 2.18 2.58 EW0408-66JC 1.670 11.845 11.824 2.30 2.70 EW0408-66JC 1.690 11.857 11.828 2.26 2.66 EW0408-66JC 1.710 11.869 11.832 2.16 2.56 EW0408-66JC 1.730 11.881 11.836 2.19 2.59 EW0408-66JC 1.750 11.893 11.840 2.36 2.76 EW0408-66JC 1.770 11.904 11.844 2.32 2.72 EW0408-66JC 1.790 11.916 11.848 2.49 2.89 EW0408-66JC 1.810 11.928 11.852 2.35 2.75 EW0408-66JC 1.830 11.940 11.856 2.11 2.51 EW0408-66JC 1.850 11.952 11.860 2.39 2.79 EW0408-66JC 1.870 11.964 11.864 2.19 2.59 EW0408-66JC 1.890 11.976 11.868 2.35 2.75 EW0408-66JC 1.910 11.988 11.872 2.13 2.53 EW0408-66JC 1.930 11.999 11.876 2.24 2.64 EW0408-66JC 1.950 12.011 11.880 1.96 2.36 EW0408-66JC 1.970 12.023 11.884 2.33 2.73 EW0408-66JC 1.990 12.035 11.888 2.35 2.75 EW0408-66JC 2.010 12.047 11.892 2.30 2.70 EW0408-66JC 2.030 12.059 11.896 2.04 2.44 EW0408-66JC 2.050 12.071 11.900 2.31 2.71 EW0408-66JC 2.070 12.083 11.904 2.20 2.60 EW0408-66JC 2.090 12.094 11.908 2.25 2.65 EW0408-66JC 2.110 12.106 11.912 2.26 2.66 EW0408-66JC 2.130 12.118 11.916 2.35 2.75 EW0408-66JC 2.150 12.130 11.920 2.27 2.67 EW0408-66JC 2.170 12.131 11.924 2.37 2.77 EW0408-66JC 2.190 12.133 11.928 2.46 2.86 EW0408-66JC 2.210 12.134 11.932 2.35 2.75 EW0408-66JC 2.230 12.135 11.936 2.65 3.05 EW0408-66JC 2.250 12.137 11.940 2.39 2.79 EW0408-66JC 2.270 12.138 11.944 2.50 2.90 EW0408-66JC 2.290 12.139 11.948 2.21 2.61 EW0408-66JC 2.310 12.141 11.952 2.16 2.56 EW0408-66JC 2.330 12.142 11.956 2.51 2.91 EW0408-66JC 2.350 12.143 11.960 2.38 2.78 EW0408-66JC 2.370 12.145 11.964 2.29 2.69 EW0408-66JC 2.390 12.146 11.968 2.33 2.73 EW0408-66JC 2.450 12.150 11.980 2.52 2.92 EW0408-66JC 2.510 12.154 11.992 2.25 2.65 EW0408-66JC 2.550 12.157 12.000 2.28 2.68 EW0408-66JC 2.610 12.161 12.012 2.35 2.75 EW0408-66JC 2.650 12.163 12.020 2.10 2.50 EW0408-66JC 2.710 12.167 12.032 2.13 2.53 EW0408-66JC 2.750 12.170 12.040 2.16 2.56 EW0408-66JC 2.810 12.174 12.052 2.20 2.60 EW0408-66JC 2.850 12.177 12.060 2.48 2.88 EW0408-66JC 2.910 12.181 12.072 2.43 2.83 EW0408-66JC 2.950 12.183 12.080 2.42 2.82 EW0408-66JC 3.010 12.187 12.092 2.22 2.62 EW0408-66JC 3.050 12.190 12.100 2.30 2.70 EW0408-66JC 3.110 12.191 12.112 2.31 2.71 EW0408-66JC 3.150 12.192 12.120 2.47 2.87 EW0408-66JC 3.210 12.193 12.132 2.33 2.73 EW0408-66JC 3.250 12.194 12.140 2.19 2.59 EW0408-66JC 3.310 12.195 12.152 2.06 2.46 EW0408-66JC 3.350 12.196 12.160 2.15 2.55 EW0408-66JC 3.410 12.197 12.172 2.33 2.73 EW0408-66JC 3.450 12.198 12.180 2.41 2.81 EW0408-66JC 3.510 12.199 12.192 2.29 2.69 EW0408-66JC 3.550 12.200 12.200 2.59 2.99 EW0408-66JC 3.610 12.220 12.206 2.34 2.74 EW0408-66JC 3.650 12.234 12.211 2.48 2.88 EW0408-66JC 3.710 12.254 12.217 2.06 2.46 EW0408-66JC 3.750 12.268 12.221 2.01 2.41 EW0408-66JC 3.810 12.288 12.227 2.31 2.71 EW0408-66JC 3.850 12.302 12.232 2.23 2.63 EW0408-66JC 3.910 12.322 12.238 2.25 2.65 EW0408-66JC 3.950 12.336 12.242 2.47 2.87 EW0408-66JC 4.010 12.356 12.249 2.29 2.69 EW0408-66JC 4.050 12.370 12.253 2.28 2.68 EW0408-66JC 4.110 12.378 12.259 2.48 2.88 EW0408-66JC 4.150 12.384 12.263 2.33 2.73 EW0408-66JC 4.210 12.392 12.270 2.46 2.86 EW0408-66JC 4.250 12.398 12.274 2.39 2.79 EW0408-66JC 4.310 12.406 12.280 2.37 2.77 EW0408-66JC 4.350 12.412 12.285 2.39 2.79 EW0408-66JC 4.410 12.420 12.291 2.35 2.75 EW0408-66JC 4.450 12.426 12.295 2.26 2.66 EW0408-66JC 4.510 12.434 12.301 2.39 2.79 EW0408-66JC 4.550 12.440 12.306 2.55 2.95 EW0408-66JC 4.610 12.448 12.312 2.19 2.59 EW0408-66JC 4.650 12.454 12.316 2.30 2.70 EW0408-66JC 4.710 12.462 12.323 2.59 2.99 EW0408-66JC 4.750 12.467 12.327 2.48 2.88 EW0408-66JC 4.810 12.475 12.333 2.12 2.52 EW0408-66JC 4.850 12.481 12.337 2.37 2.77 EW0408-66JC 4.910 12.489 12.344 2.17 2.57 EW0408-66JC 4.950 12.495 12.348 2.09 2.49 EW0408-66JC 5.010 12.503 12.354 2.15 2.55 EW0408-66JC 5.050 12.508 12.359 2.09 2.49 EW0408-66JC 5.110 12.516 12.365 2.35 2.75 EW0408-66JC 5.150 12.522 12.369 2.28 2.68 EW0408-66JC 5.250 12.535 12.380 2.46 2.86 EW0408-66JC 5.310 12.544 12.386 2.30 2.70 EW0408-66JC 5.350 12.549 12.390 2.27 2.67 EW0408-66JC 5.410 12.557 12.397 2.38 2.78 EW0408-66JC 5.450 12.563 12.401 2.52 2.92 EW0408-66JC 5.510 12.571 12.407 2.32 2.72 EW0408-66JC 5.550 12.576 12.411 2.37 2.77 EW0408-66JC 5.610 12.585 12.418 2.18 2.58 EW0408-66JC 5.650 12.590 12.422 2.26 2.66 EW0408-66JC 5.710 12.601 12.428 2.45 2.85 EW0408-66JC 5.750 12.608 12.433 2.38 2.78 EW0408-66JC 5.810 12.618 12.439 2.40 2.80 EW0408-66JC 5.850 12.625 12.443 2.33 2.73 EW0408-66JC 5.910 12.636 12.449 2.32 2.72 EW0408-66JC 5.950 12.643 12.454 2.59 2.99 EW0408-66JC 6.050 12.660 12.464 2.23 2.63 EW0408-66JC 6.110 12.667 12.471 2.29 2.69 EW0408-66JC 6.150 12.671 12.475 2.43 2.83 EW0408-66JC 6.210 12.678 12.481 2.09 2.49 EW0408-66JC 6.250 12.682 12.485 2.36 2.76 EW0408-66JC 6.310 12.689 12.492 2.28 2.68 EW0408-66JC 6.350 12.693 12.496 2.44 2.84 EW0408-66JC 6.410 12.700 12.502 2.19 2.59 EW0408-66JC 6.450 12.704 12.507 2.35 2.75 EW0408-66JC 6.510 12.711 12.513 2.26 2.66 EW0408-66JC 6.550 12.715 12.517 2.50 2.90 EW0408-66JC 6.610 12.722 12.523 2.12 2.52 EW0408-66JC 6.650 12.726 12.528 2.27 2.67 EW0408-66JC 6.710 12.733 12.534 2.25 2.65 EW0408-66JC 6.750 12.737 12.538 2.40 2.80 EW0408-66JC 6.810 12.744 12.545 2.30 2.70 EW0408-66JC 6.850 12.748 12.549 2.28 2.68 EW0408-66JC 6.910 12.755 12.555 2.13 2.53 EW0408-66JC 6.950 12.759 12.559 2.30 2.70 EW0408-66JC 7.010 12.766 12.566 2.38 2.78 EW0408-66JC 7.050 12.770 12.570 2.57 2.97 EW0408-66JC 7.110 12.783 12.584 2.54 2.94 EW0408-66JC 7.150 12.792 12.594 2.66 3.06 EW0408-66JC 7.210 12.806 12.609 2.47 2.87 EW0408-66JC 7.250 12.814 12.618 2.48 2.88 EW0408-66JC 7.310 12.828 12.633 2.06 2.46 EW0408-66JC 7.350 12.837 12.642 1.99 2.39 EW0408-66JC 7.430 12.854 12.661 2.18 2.58 EW0408-66JC 7.450 12.859 12.666 2.56 2.96 EW0408-66JC 7.470 12.863 12.671 2.60 3.00 EW0408-66JC 7.490 12.868 12.676 2.47 2.87 EW0408-66JC 7.530 12.877 12.686 2.41 2.81 EW0408-66JC 7.550 12.881 12.690 2.55 2.95 EW0408-66JC 7.570 12.886 12.695 2.36 2.76 EW0408-66JC 7.590 12.890 12.700 2.29 2.69 EW0408-66JC 7.630 12.898 12.711 2.26 2.66 EW0408-66JC 7.650 12.902 12.717 2.31 2.71 EW0408-66JC 7.670 12.906 12.723 2.38 2.78 EW0408-66JC 7.690 12.910 12.728 2.34 2.74 EW0408-66JC 7.730 12.917 12.740 2.31 2.71 EW0408-66JC 7.750 12.921 12.745 2.18 2.58 EW0408-66JC 7.770 12.925 12.751 2.31 2.71 EW0408-66JC 7.790 12.929 12.757 2.34 2.74 EW0408-66JC 7.830 12.937 12.768 2.26 2.66 EW0408-66JC 7.850 12.941 12.773 2.32 2.72 EW0408-66JC 7.870 12.945 12.779 2.36 2.76 EW0408-66JC 7.890 12.949 12.785 2.20 2.60 EW0408-66JC 7.910 12.953 12.790 2.36 2.76 EW0408-66JC 7.930 12.957 12.796 2.38 2.78 EW0408-66JC 7.950 12.960 12.802 2.00 2.40 EW0408-66JC 7.970 12.964 12.807 2.19 2.59 EW0408-66JC 7.990 12.968 12.813 2.11 2.51 EW0408-66JC 8.010 12.972 12.819 2.26 2.66 EW0408-66JC 8.050 12.980 12.830 2.15 2.55 EW0408-66JC 8.110 12.996 12.863 2.07 2.47 EW0408-66JC 8.150 13.007 12.885 1.94 2.34 EW0408-66JC 8.210 13.024 12.917 2.29 2.69 EW0408-66JC 8.250 13.035 12.939 2.08 2.48 EW0408-66JC 8.310 13.051 12.972 2.07 2.47 EW0408-66JC 8.350 13.062 12.994 1.91 2.31 EW0408-66JC 8.410 13.078 13.026 2.29 2.69 EW0408-66JC 8.450 13.089 13.048 2.20 2.60 EW0408-66JC 8.510 13.105 13.081 2.46 2.86 EW0408-66JC 8.550 13.116 13.103 2.21 2.61 EW0408-66JC 8.610 13.132 13.132 2.16 2.56 EW0408-66JC 8.650 13.141 13.141 2.16 2.56 EW0408-66JC 8.710 13.155 13.155 2.11 2.51 EW0408-66JC 8.750 13.164 13.164 1.95 2.35 EW0408-66JC 8.810 13.177 13.177 2.44 2.84 EW0408-66JC 8.850 13.186 13.186 2.40 2.80 EW0408-66JC 8.960 13.211 13.211 2.22 2.62 EW0408-66JC 9.010 13.222 13.222 2.23 2.63 EW0408-66JC 9.050 13.230 13.230 2.36 2.76 EW0408-66JC 9.070 13.231 13.231 2.15 2.55 EW0408-66JC 9.110 13.233 13.233 2.08 2.48 EW0408-66JC 9.150 13.235 13.235 2.04 2.44 EW0408-66JC 9.190 13.237 13.237 1.96 2.36 EW0408-66JC 9.240 13.240 13.240 2.15 2.55 EW0408-66JC 9.310 13.243 13.243 1.90 2.30 EW0408-66JC 9.350 13.245 13.245 2.08 2.48 EW0408-66JC 9.450 13.250 13.250 2.10 2.50 EW0408-66JC 9.550 13.255 13.255 1.89 2.29 EW0408-66JC 9.650 13.260 13.260 1.86 2.26 EW0408-66JC 9.710 13.262 13.262 1.52 1.92 EW0408-66JC 9.750 13.264 13.264 1.38 1.78 EW0408-66JC 9.850 13.269 13.269 2.01 2.41 EW0408-66JC 9.890 13.271 13.271 1.64 2.04 EW0408-66JC 9.950 13.274 13.274 1.70 2.10 EW0408-66JC 10.050 13.279 13.279 1.74 2.14 EW0408-66JC 10.110 13.282 13.282 1.71 2.11 EW0408-66JC 10.150 13.284 13.284 1.56 1.96 EW0408-66JC 10.250 13.289 13.289 1.65 2.05 EW0408-66JC 10.310 13.292 13.292 1.92 2.32 EW0408-66JC 10.350 13.294 13.294 1.57 1.97 EW0408-66JC 10.450 13.299 13.299 2.27 2.67 EW0408-66JC 10.510 13.302 13.302 1.77 2.17 EW0408-66JC 10.550 13.304 13.304 1.94 2.34 EW0408-66JC 10.610 13.306 13.306 2.31 2.71 EW0408-66JC 10.650 13.308 13.308 2.03 2.43 EW0408-66JC 10.710 13.311 13.311 2.04 2.44 EW0408-66JC 10.750 13.313 13.313 2.03 2.43 EW0408-66JC 10.810 13.316 13.316 1.87 2.27 EW0408-66JC 10.850 13.318 13.318 2.10 2.50 EW0408-66JC 10.970 13.324 13.324 2.11 2.51 EW0408-66JC 11.050 13.328 13.328 1.96 2.36 EW0408-66JC 11.150 13.333 13.333 1.75 2.15 EW0408-66JC 11.250 13.338 13.338 1.70 2.10 EW0408-66JC 11.350 13.343 13.343 1.84 2.24 EW0408-66JC 11.550 13.352 13.352 1.80 2.20 EW0408-66JC 11.650 13.357 13.357 2.08 2.48 EW0408-66JC 11.750 13.362 13.362 1.64 2.04 EW0408-66JC 11.950 13.372 13.372 2.06 2.46 EW0408-66JC 12.050 13.377 13.377 1.99 2.39 EW0408-66JC 12.150 13.382 13.382 1.86 2.26 EW0408-66JC 12.250 13.387 13.387 1.81 2.21 EW0408-66JC 12.350 13.391 13.391 1.92 2.32 EW0408-66JC 12.450 13.396 13.396 2.14 2.54 EW0408-66JC 12.550 13.401 13.401 1.86 2.26 EW0408-66JC 12.650 13.406 13.406 1.84 2.24 EW0408-66JC 12.750 13.413 13.413 1.85 2.25 EW0408-66JC 12.850 13.428 13.428 2.09 2.49 EW0408-66JC 13.010 13.453 13.453 1.85 2.25 EW0408-66JC 13.050 13.459 13.459 2.01 2.41 EW0408-66JC 13.150 13.475 13.475 1.91 2.31 EW0408-66JC 13.210 13.484 13.484 2.16 2.56 EW0408-66JC 13.310 13.499 13.499 1.88 2.28 EW0408-66JC 13.410 13.515 13.515 2.26 2.66 EW0408-66JC 13.510 13.530 13.530 2.04 2.44 EW0408-66JC 13.550 13.536 13.536 2.25 2.65 EW0408-66JC 13.590 13.542 13.542 2.00 2.40 EW0408-66JC 13.650 13.552 13.550 2.07 2.47 EW0408-66JC 13.770 13.570 13.570 1.94 2.34