# 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-composite-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: EW0408-26TC/JC and 66JC # Location: Gulf of Alaska # Country: # Northernmost_Latitude: 58.87 # Southernmost_Latitude: 56.96 # Easternmost_Longitude: -136.43 # Westernmost_Longitude: -137.1 # Elevation: #--------------------------------------- # Data_Collection # Collection_Name: EW0408-26TC/JC and 66JC d18O Praetorius2016 # First_Year: 18170 # Last_Year: 4246 # Time_Unit: cal yr BP # Core_Length: # 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_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,composite record of 66JC and 26JC/TC,,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_tuned d18O_Nps EW0408-66JC 0.070 4.246 2.06 EW0408-66JC 0.110 4.605 2.09 EW0408-66JC 0.130 4.784 1.72 EW0408-66JC 0.150 4.963 1.94 EW0408-66JC 0.170 5.143 1.80 EW0408-66JC 0.190 5.322 1.60 EW0408-66JC 0.210 5.501 2.02 EW0408-66JC 0.230 5.681 1.89 EW0408-66JC 0.250 5.860 1.84 EW0408-66JC 0.270 6.039 1.65 EW0408-66JC 0.290 6.218 1.85 EW0408-66JC 0.310 6.398 1.83 EW0408-66JC 0.330 6.577 1.83 EW0408-66JC 0.350 6.756 1.83 EW0408-66JC 0.370 6.936 1.76 EW0408-66JC 0.390 7.115 1.69 EW0408-66JC 0.410 7.294 1.55 EW0408-66JC 0.430 7.474 1.66 EW0408-66JC 0.450 7.653 1.92 EW0408-66JC 0.470 7.832 1.72 EW0408-66JC 0.490 8.011 1.98 EW0408-66JC 0.510 8.191 1.96 EW0408-66JC 0.530 8.370 1.87 EW0408-66JC 0.550 8.497 1.78 EW0408-66JC 0.570 8.623 1.88 EW0408-66JC 0.590 8.750 2.06 EW0408-66JC 0.610 8.877 1.79 EW0408-66JC 0.630 9.003 1.86 EW0408-66JC 0.650 9.130 1.95 EW0408-66JC 0.670 9.378 1.74 EW0408-66JC 0.690 9.626 1.75 EW0408-66JC 0.710 9.874 1.84 EW0408-66JC 0.730 10.122 2.09 EW0408-66JC 0.750 10.370 2.07 EW0408-66JC 0.770 10.618 1.93 EW0408-66JC 0.790 10.866 1.91 EW0408-66JC 0.810 11.114 1.99 EW0408-66JC 0.830 11.362 1.89 EW0408-66JC 0.850 11.610 1.92 EW0408-66JC 0.870 11.618 1.92 EW0408-66JC 0.890 11.626 2.09 EW0408-66JC 0.910 11.634 2.22 EW0408-66JC 0.930 11.642 2.16 EW0408-66JC 0.950 11.650 2.38 EW0408-66JC 0.970 11.658 2.37 EW0408-66JC 0.990 11.666 2.44 EW0408-66JC 1.030 11.682 2.61 EW0408-66JC 1.050 11.690 2.44 EW0408-66JC 1.070 11.698 2.63 EW0408-66JC 1.100 11.710 2.54 EW0408-66JC 1.120 11.714 2.80 EW0408-66JC 1.150 11.720 2.70 EW0408-66JC 1.170 11.724 2.61 EW0408-66JC 1.190 11.728 2.58 EW0408-66JC 1.210 11.732 2.67 EW0408-66JC 1.230 11.736 2.52 EW0408-66JC 1.250 11.740 2.36 EW0408-66JC 1.270 11.744 2.60 EW0408-66JC 1.290 11.748 2.63 EW0408-66JC 1.310 11.752 2.63 EW0408-66JC 1.330 11.756 2.69 EW0408-66JC 1.350 11.760 2.66 EW0408-66JC 1.350 11.760 2.66 EW0408-66JC 1.380 11.766 2.54 EW0408-66JC 1.390 11.768 2.64 EW0408-66JC 1.410 11.772 2.72 EW0408-66JC 1.430 11.776 2.83 EW0408-66JC 1.450 11.780 2.62 EW0408-66JC 1.470 11.784 2.35 EW0408-66JC 1.490 11.788 2.72 EW0408-66JC 1.510 11.792 2.51 EW0408-66JC 1.530 11.796 2.60 EW0408-66JC 1.550 11.800 2.53 EW0408-66JC 1.570 11.804 2.72 EW0408-66JC 1.590 11.808 2.49 EW0408-66JC 1.610 11.812 2.54 EW0408-66JC 1.630 11.816 2.68 EW0408-66JC 1.650 11.820 2.58 EW0408-66JC 1.670 11.824 2.70 EW0408-66JC 1.690 11.828 2.66 EW0408-66JC 1.710 11.832 2.56 EW0408-66JC 1.730 11.836 2.59 EW0408-66JC 1.750 11.840 2.76 EW0408-66JC 1.770 11.844 2.72 EW0408-66JC 1.790 11.848 2.89 EW0408-66JC 1.810 11.852 2.75 EW0408-66JC 1.830 11.856 2.51 EW0408-66JC 1.850 11.860 2.79 EW0408-66JC 1.870 11.864 2.59 EW0408-66JC 1.890 11.868 2.75 EW0408-66JC 1.910 11.872 2.53 EW0408-66JC 1.930 11.876 2.64 EW0408-66JC 1.950 11.880 2.36 EW0408-66JC 1.970 11.884 2.73 EW0408-66JC 1.990 11.888 2.75 EW0408-66JC 2.010 11.892 2.70 EW0408-66JC 2.030 11.896 2.44 EW0408-66JC 2.050 11.900 2.71 EW0408-66JC 2.070 11.904 2.60 EW0408-66JC 2.090 11.908 2.65 EW0408-66JC 2.110 11.912 2.66 EW0408-66JC 2.130 11.916 2.75 EW0408-66JC 2.150 11.920 2.67 EW0408-66JC 2.170 11.924 2.77 EW0408-66JC 2.190 11.928 2.86 EW0408-66JC 2.210 11.932 2.75 EW0408-66JC 2.230 11.936 3.05 EW0408-66JC 2.250 11.940 2.79 EW0408-66JC 2.270 11.944 2.90 EW0408-66JC 2.290 11.948 2.61 EW0408-66JC 2.310 11.952 2.56 EW0408-66JC 2.330 11.956 2.91 EW0408-66JC 2.350 11.960 2.78 EW0408-66JC 2.370 11.964 2.69 EW0408-66JC 2.390 11.968 2.73 EW0408-66JC 2.450 11.980 2.92 EW0408-66JC 2.510 11.992 2.65 EW0408-66JC 2.550 12.000 2.68 EW0408-66JC 2.610 12.012 2.75 EW0408-66JC 2.650 12.020 2.50 EW0408-66JC 2.710 12.032 2.53 EW0408-66JC 2.750 12.040 2.56 EW0408-66JC 2.810 12.052 2.60 EW0408-66JC 2.850 12.060 2.88 EW0408-66JC 2.910 12.072 2.83 EW0408-66JC 2.950 12.080 2.82 EW0408-66JC 3.010 12.092 2.62 EW0408-66JC 3.050 12.100 2.70 EW0408-66JC 3.110 12.112 2.71 EW0408-66JC 3.150 12.120 2.87 EW0408-66JC 3.210 12.132 2.73 EW0408-66JC 3.250 12.140 2.59 EW0408-66JC 3.310 12.152 2.46 EW0408-66JC 3.350 12.160 2.55 EW0408-66JC 3.410 12.172 2.73 EW0408-66JC 3.450 12.180 2.81 EW0408-66JC 3.510 12.192 2.69 EW0408-66JC 3.550 12.200 2.99 EW0408-66JC 3.610 12.206 2.74 EW0408-66JC 3.650 12.211 2.88 EW0408-66JC 3.710 12.217 2.46 EW0408-66JC 3.750 12.221 2.41 EW0408-66JC 3.810 12.227 2.71 EW0408-66JC 3.850 12.232 2.63 EW0408-66JC 3.910 12.238 2.65 EW0408-66JC 3.950 12.242 2.87 EW0408-66JC 4.010 12.249 2.69 EW0408-66JC 4.050 12.253 2.68 EW0408-66JC 4.110 12.259 2.88 EW0408-66JC 4.150 12.263 2.73 EW0408-66JC 4.210 12.270 2.86 EW0408-66JC 4.250 12.274 2.79 EW0408-66JC 4.310 12.280 2.77 EW0408-66JC 4.350 12.285 2.79 EW0408-66JC 4.410 12.291 2.75 EW0408-66JC 4.450 12.295 2.66 EW0408-66JC 4.510 12.301 2.79 EW0408-66JC 4.550 12.306 2.95 EW0408-66JC 4.610 12.312 2.59 EW0408-66JC 4.650 12.316 2.70 EW0408-66JC 4.710 12.323 2.99 EW0408-66JC 4.750 12.327 2.88 EW0408-66JC 4.810 12.333 2.52 EW0408-66JC 4.850 12.337 2.77 EW0408-66JC 4.910 12.344 2.57 EW0408-66JC 4.950 12.348 2.49 EW0408-66JC 5.010 12.354 2.55 EW0408-66JC 5.050 12.359 2.49 EW0408-66JC 5.110 12.365 2.75 EW0408-66JC 5.150 12.369 2.68 EW0408-66JC 5.250 12.380 2.86 EW0408-66JC 5.310 12.386 2.70 EW0408-66JC 5.350 12.390 2.67 EW0408-66JC 5.410 12.397 2.78 EW0408-66JC 5.450 12.401 2.92 EW0408-66JC 5.510 12.407 2.72 EW0408-66JC 5.550 12.411 2.77 EW0408-66JC 5.610 12.418 2.58 EW0408-66JC 5.650 12.422 2.66 EW0408-66JC 5.710 12.428 2.85 EW0408-66JC 5.750 12.433 2.78 EW0408-66JC 5.810 12.439 2.80 EW0408-66JC 5.850 12.443 2.73 EW0408-66JC 5.910 12.449 2.72 EW0408-66JC 5.950 12.454 2.99 EW0408-66JC 6.050 12.464 2.63 EW0408-66JC 6.110 12.471 2.69 EW0408-66JC 6.150 12.475 2.83 EW0408-66JC 6.210 12.481 2.49 EW0408-66JC 6.250 12.485 2.76 EW0408-66JC 6.310 12.492 2.68 EW0408-66JC 6.350 12.496 2.84 EW0408-66JC 6.410 12.502 2.59 EW0408-66JC 6.450 12.507 2.75 EW0408-66JC 6.510 12.513 2.66 EW0408-66JC 6.550 12.517 2.90 EW0408-66JC 6.610 12.523 2.52 EW0408-66JC 6.650 12.528 2.67 EW0408-66JC 6.710 12.534 2.65 EW0408-66JC 6.750 12.538 2.80 EW0408-66JC 6.810 12.545 2.70 EW0408-66JC 6.850 12.549 2.68 EW0408-66JC 6.910 12.555 2.53 EW0408-66JC 6.950 12.559 2.70 EW0408-66JC 7.010 12.566 2.78 EW0408-66JC 7.050 12.570 2.97 EW0408-66JC 7.110 12.584 2.94 EW0408-66JC 7.150 12.594 3.06 EW0408-66JC 7.210 12.609 2.87 EW0408-66JC 7.250 12.618 2.88 EW0408-66JC 7.310 12.633 2.46 EW0408-66JC 7.350 12.642 2.39 EW0408-66JC 7.430 12.661 2.58 EW0408-66JC 7.450 12.666 2.96 EW0408-66JC 7.470 12.671 3.00 EW0408-66JC 7.490 12.676 2.87 EW0408-66JC 7.530 12.686 2.81 EW0408-66JC 7.550 12.690 2.95 EW0408-66JC 7.570 12.695 2.76 EW0408-66JC 7.590 12.700 2.69 EW0408-66JC 7.630 12.711 2.66 EW0408-66JC 7.650 12.717 2.71 EW0408-66JC 7.670 12.723 2.78 EW0408-66JC 7.690 12.728 2.74 EW0408-66JC 7.730 12.740 2.71 EW0408-66JC 7.750 12.745 2.58 EW0408-66JC 7.770 12.751 2.71 EW0408-66JC 7.790 12.757 2.74 EW0408-66JC 7.830 12.768 2.66 EW0408-66JC 7.850 12.773 2.72 EW0408-66JC 7.870 12.779 2.76 EW0408-66JC 7.890 12.785 2.60 EW0408-66JC 7.910 12.790 2.76 EW0408-66JC 7.930 12.796 2.78 EW0408-66JC 7.950 12.802 2.40 EW0408-66JC 7.970 12.807 2.59 EW0408-66JC 7.990 12.813 2.51 EW0408-66JC 8.010 12.819 2.66 EW0408-66JC 8.050 12.830 2.55 EW0408-66JC 8.110 12.863 2.47 EW0408-66JC 8.150 12.885 2.34 EW0408-66JC 8.210 12.917 2.69 EW0408-66JC 8.250 12.939 2.48 EW0408-66JC 8.310 12.972 2.47 EW0408-66JC 8.350 12.994 2.31 EW0408-66JC 8.410 13.026 2.69 EW0408-66JC 8.450 13.048 2.60 EW0408-66JC 8.510 13.081 2.86 EW0408-66JC 8.550 13.103 2.61 EW0408-66JC 8.610 13.132 2.56 EW0408-66JC 8.650 13.141 2.56 EW0408-66JC 8.710 13.155 2.51 EW0408-66JC 8.750 13.164 2.35 EW0408-66JC 8.810 13.177 2.84 EW0408-66JC 8.850 13.186 2.80 EW0408-66JC 8.960 13.211 2.62 EW0408-66JC 9.010 13.222 2.63 EW0408-66JC 9.050 13.230 2.76 EW0408-66JC 9.070 13.231 2.55 EW0408-66JC 9.110 13.233 2.48 EW0408-66JC 9.150 13.235 2.44 EW0408-66JC 9.190 13.237 2.36 EW0408-66JC 9.240 13.240 2.55 EW0408-66JC 9.310 13.243 2.30 EW0408-66JC 9.350 13.245 2.48 EW0408-66JC 9.450 13.250 2.50 EW0408-66JC 9.550 13.255 2.29 EW0408-66JC 9.650 13.260 2.26 EW0408-66JC 9.710 13.262 1.92 EW0408-66JC 9.750 13.264 1.78 EW0408-66JC 9.850 13.269 2.41 EW0408-66JC 9.890 13.271 2.04 EW0408-66JC 9.950 13.274 2.10 EW0408-66JC 10.050 13.279 2.14 EW0408-66JC 10.110 13.282 2.11 EW0408-66JC 10.150 13.284 1.96 EW0408-66JC 10.250 13.289 2.05 EW0408-66JC 10.310 13.292 2.32 EW0408-66JC 10.350 13.294 1.97 EW0408-66JC 10.450 13.299 2.67 EW0408-66JC 10.510 13.302 2.17 EW0408-66JC 10.550 13.304 2.34 EW0408-66JC 10.610 13.306 2.71 EW0408-66JC 10.650 13.308 2.43 EW0408-66JC 10.710 13.311 2.44 EW0408-66JC 10.750 13.313 2.43 EW0408-66JC 10.810 13.316 2.27 EW0408-66JC 10.850 13.318 2.50 EW0408-66JC 10.970 13.324 2.51 EW0408-66JC 11.050 13.328 2.36 EW0408-66JC 11.150 13.333 2.15 EW0408-66JC 11.250 13.338 2.10 EW0408-66JC 11.350 13.343 2.24 EW0408-66JC 11.550 13.352 2.20 EW0408-66JC 11.650 13.357 2.48 EW0408-66JC 11.750 13.362 2.04 EW0408-66JC 11.950 13.372 2.46 EW0408-66JC 12.050 13.377 2.39 EW0408-66JC 12.150 13.382 2.26 EW0408-66JC 12.250 13.387 2.21 EW0408-66JC 12.350 13.391 2.32 EW0408-66JC 12.450 13.396 2.54 EW0408-66JC 12.550 13.401 2.26 EW0408-66JC 12.650 13.406 2.24 EW0408-66JC 12.750 13.413 2.25 EW0408-66JC 12.850 13.428 2.49 EW0408-66JC 13.010 13.453 2.25 EW0408-66JC 13.050 13.459 2.41 EW0408-66JC 13.150 13.475 2.31 EW0408-66JC 13.210 13.484 2.56 EW0408-66JC 13.310 13.499 2.28 EW0408-66JC 13.410 13.515 2.66 EW0408-66JC 13.510 13.530 2.44 EW0408-66JC 13.550 13.536 2.65 EW0408-66JC 13.590 13.542 2.40 EW0408-66JC 13.650 13.550 2.47 EW0408-26JC 0.010 13.550 2.47 EW0408-26JC 0.025 13.560 2.43 EW0408-26JC 0.035 13.567 2.73 EW0408-26JC 0.045 13.574 2.78 EW0408-26JC 0.055 13.581 2.62 EW0408-26JC 0.065 13.588 2.71 EW0408-26JC 0.085 13.602 2.63 EW0408-26JC 0.105 13.616 2.41 EW0408-26JC 0.125 13.630 2.68 EW0408-26JC 0.145 13.644 2.65 EW0408-26JC 0.165 13.658 2.36 EW0408-26JC 0.185 13.672 2.32 EW0408-26JC 0.205 13.686 2.26 EW0408-26JC 0.225 13.700 2.71 EW0408-26JC 0.245 13.726 2.53 EW0408-26JC 0.265 13.752 2.28 EW0408-26JC 0.290 13.785 2.18 EW0408-26JC 0.305 13.804 2.33 EW0408-26JC 0.325 13.830 2.56 EW0408-26JC 0.355 13.870 2.23 EW0408-26JC 0.365 13.883 2.12 EW0408-26JC 0.385 13.909 2.36 EW0408-26JC 0.405 13.935 2.36 EW0408-26JC 0.425 13.961 2.67 EW0408-26JC 0.455 14.000 2.41 EW0408-26JC 0.465 14.006 2.34 EW0408-26JC 0.485 14.017 2.60 EW0408-26JC 0.510 14.032 2.11 EW0408-26JC 0.525 14.040 2.35 EW0408-26JC 0.555 14.058 2.32 EW0408-26JC 0.565 14.064 2.19 EW0408-26JC 0.585 14.075 1.91 EW0408-26JC 0.605 14.087 2.26 EW0408-26JC 0.625 14.098 2.45 EW0408-26JC 0.655 14.116 1.80 EW0408-26JC 0.655 14.116 1.85 EW0408-26JC 0.675 14.127 2.07 EW0408-26JC 0.705 14.145 2.22 EW0408-26JC 0.725 14.156 2.18 EW0408-26JC 0.755 14.173 2.95 EW0408-26JC 0.765 14.179 2.01 EW0408-26JC 0.785 14.191 2.33 EW0408-26JC 0.805 14.202 2.36 EW0408-26JC 0.815 14.208 2.73 EW0408-26JC 0.825 14.214 3.04 EW0408-26JC 0.895 14.254 2.04 EW0408-26JC 0.905 14.260 1.88 EW0408-26JC 0.925 14.272 2.39 EW0408-26JC 0.955 14.289 1.79 EW0408-26JC 0.965 14.295 1.87 EW0408-26JC 0.985 14.306 2.30 EW0408-26JC 1.010 14.321 2.22 EW0408-26JC 1.025 14.330 2.06 EW0408-26JC 1.055 14.347 2.41 EW0408-26JC 1.065 14.353 1.77 EW0408-26JC 1.085 14.364 2.01 EW0408-26JC 1.105 14.376 2.10 EW0408-26JC 1.125 14.387 1.87 EW0408-26JC 1.155 14.405 1.45 EW0408-26JC 1.165 14.411 1.76 EW0408-26JC 1.185 14.422 1.65 EW0408-26JC 1.205 14.434 2.19 EW0408-26JC 1.225 14.445 1.65 EW0408-26JC 1.255 14.463 1.74 EW0408-26JC 1.265 14.468 2.00 EW0408-26JC 1.285 14.480 1.95 EW0408-26JC 1.305 14.491 2.35 EW0408-26JC 1.325 14.503 1.91 EW0408-26JC 1.355 14.520 1.85 EW0408-26JC 1.375 14.532 1.85 EW0408-26JC 1.405 14.549 1.92 EW0408-26JC 1.425 14.561 1.90 EW0408-26JC 1.455 14.578 1.94 EW0408-26JC 1.475 14.590 1.89 EW0408-26JC 1.510 14.610 2.00 EW0408-26JC 1.535 14.615 1.69 EW0408-26JC 1.555 14.619 1.56 EW0408-26JC 1.575 14.623 1.94 EW0408-26JC 1.595 14.627 2.03 EW0408-26JC 1.605 14.629 1.84 EW0408-26JC 1.615 14.631 1.67 EW0408-26JC 1.625 14.633 1.86 EW0408-26JC 1.655 14.639 1.89 EW0408-26JC 1.675 14.644 2.01 EW0408-26JC 1.695 14.648 2.49 EW0408-26JC 1.705 14.650 2.32 EW0408-26JC 1.725 14.654 2.26 EW0408-26JC 1.745 14.658 2.76 EW0408-26JC 1.775 14.664 2.43 EW0408-26JC 1.805 14.670 3.01 EW0408-26JC 1.825 14.689 2.83 EW0408-26JC 1.855 14.716 2.76 EW0408-26JC 1.905 14.763 3.04 EW0408-26JC 1.955 14.809 2.78 EW0408-26JC 2.010 14.860 2.77 EW0408-26JC 2.055 14.902 3.14 EW0408-26JC 2.105 14.948 3.02 EW0408-26JC 2.155 14.995 3.01 EW0408-26JC 2.205 15.041 3.21 EW0408-26JC 2.255 15.087 3.02 EW0408-26JC 2.305 15.134 2.77 EW0408-26JC 2.355 15.180 3.15 EW0408-26JC 2.405 15.226 3.09 EW0408-26JC 2.455 15.273 2.97 EW0408-26JC 2.510 15.324 2.95 EW0408-26JC 2.555 15.365 2.77 EW0408-26JC 2.605 15.412 3.07 EW0408-26JC 2.655 15.458 3.08 EW0408-26JC 2.705 15.505 2.91 EW0408-26JC 2.755 15.551 3.40 EW0408-26JC 2.805 15.597 3.19 EW0408-26JC 2.855 15.644 3.21 EW0408-26JC 2.905 15.690 3.18 EW0408-26JC 2.955 15.740 2.78 EW0408-26JC 3.010 15.796 3.11 EW0408-26JC 3.055 15.841 3.15 EW0408-26JC 3.105 15.891 3.28 EW0408-26JC 3.155 15.941 3.07 EW0408-26JC 3.205 15.992 3.35 EW0408-26JC 3.255 16.042 3.19 EW0408-26JC 3.305 16.092 3.59 EW0408-26JC 3.355 16.142 3.70 EW0408-26JC 3.405 16.193 3.47 EW0408-26JC 3.460 16.248 3.54 EW0408-26JC 3.510 16.298 3.47 EW0408-26JC 3.560 16.348 3.24 EW0408-26JC 3.605 16.394 3.51 EW0408-26JC 3.660 16.449 3.56 EW0408-26JC 3.705 16.494 3.56 EW0408-26JC 3.755 16.544 3.52 EW0408-26JC 3.805 16.595 3.68 EW0408-26JC 3.855 16.645 3.74 EW0408-26JC 3.925 16.715 3.59 EW0408-26JC 3.990 16.781 3.57 EW0408-26JC 4.055 16.846 3.69 EW0408-26JC 4.110 16.901 3.26 EW0408-26JC 4.155 16.947 3.45 EW0408-26JC 4.210 17.002 3.41 EW0408-26JC 4.255 17.047 3.35 EW0408-26JC 4.310 17.102 3.58 EW0408-26JC 4.355 17.148 3.77 EW0408-26JC 4.405 17.198 3.56 EW0408-26JC 4.455 17.248 3.51 EW0408-26JC 4.510 17.303 3.43 EW0408-26JC 4.555 17.349 3.42 EW0408-26JC 4.610 17.404 3.55 EW0408-26JC 4.655 17.449 3.50 EW0408-26JC 4.755 17.550 3.45 EW0408-26JC 4.805 17.600 3.80 EW0408-26JC 4.855 17.621 3.62 EW0408-26JC 4.905 17.641 3.59 EW0408-26JC 4.955 17.662 3.55 EW0408-26JC 5.010 17.681 3.51 EW0408-26JC 5.055 17.687 3.42 EW0408-26JC 5.205 17.706 3.51 EW0408-26JC 5.255 17.712 3.55 EW0408-26JC 5.310 17.719 3.43 EW0408-26JC 5.355 17.724 3.61 EW0408-26JC 5.405 17.731 3.64 EW0408-26JC 5.450 17.736 3.29 EW0408-26JC 5.510 17.744 3.36 EW0408-26JC 5.550 17.749 3.48 EW0408-26JC 5.605 17.756 3.63 EW0408-26JC 5.650 17.761 3.54 EW0408-26JC 5.710 17.769 3.41 EW0408-26JC 5.755 17.775 3.45 EW0408-26JC 5.805 17.781 3.63 EW0408-26JC 5.850 17.787 3.63 EW0408-26JC 5.990 17.804 3.60 EW0408-26JC 6.050 17.812 3.48 EW0408-26JC 6.110 17.819 3.26 EW0408-26JC 6.150 17.824 3.37 EW0408-26JC 6.205 17.831 3.66 EW0408-26JC 6.255 17.837 3.66 EW0408-26JC 6.310 17.844 3.58 EW0408-26JC 7.350 17.975 3.45 EW0408-26JC 7.405 17.981 3.41 EW0408-26JC 7.465 17.989 3.55 EW0408-26JC 7.550 18.000 3.58 EW0408-26JC 7.605 18.006 3.55 EW0408-26JC 7.650 18.012 3.57 EW0408-26JC 7.705 18.019 3.43 EW0408-26JC 7.780 18.028 3.62 EW0408-26JC 7.965 18.052 3.65 EW0408-26JC 8.005 18.057 3.32 EW0408-26JC 8.110 18.070 3.72 EW0408-26JC 8.210 18.082 3.50 EW0408-26JC 8.310 18.095 3.59 EW0408-26JC 8.405 18.107 3.55 EW0408-26JC 8.510 18.120 3.61 EW0408-26JC 8.610 18.132 3.65 EW0408-26JC 8.710 18.145 3.41 EW0408-26JC 8.810 18.157 3.56 EW0408-26JC 8.910 18.170 3.45