# Borneo 160,000 Year Stalagmite Oxygen Isotope Data #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # 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.ncdc.noaa.gov/paleo/study/19806 # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/pacific/borneo2016fc12-15.txt # # Archive: Speleothems # # Parameter_Keywords: oxygen isotopes #--------------------------------------- # Contribution_Date # Date: 2016-02-24 #--------------------------------------- # Title # Study_Name: Borneo 160,000 Year Stalagmite Oxygen Isotope Data #--------------------------------------- # Investigators # Investigators: Carolin, S.A.; Cobb, K.M.; Lynch-Stieglitz, J.; Moerman, J.W.; Partin, J.W.; Lejau, S.; Malang, J.; Clark, B.; Tuen, A.A.; Adkins, J.F. #--------------------------------------- # Description and Notes # Description: Oxygen stable isotope records (d18O) from stalagmites collected in different caves in Gunung Mulu National Park, Borneo, Malaysia. # Chronologies were established by 238U-234U-230Th dating. A full composite spliced d18O record (0-161ky) and d18O record at 100yr time steps (0-160ky) # is also provided for simple plotting/analysis of data. # Provided Keywords: speleothem; stable isotopes; glacial cycles; Termination 2; penultimate interglacial; tropical west Pacific #--------------------------------------- # Publication # Authors: Stacy A. Carolin, Kim M. Cobb, Jean Lynch-Stieglitz, Jessica W. Moerman, Judson W. Partin, Syria Lejau, Jenny Malang, Brian Clark, Andrew A. Tuen, Jess F. Adkins # Published_Date_or_Year: 2016-04-01 # Published_Title: Northern Borneo stalagmite records reveal West Pacific hydroclimate across MIS 5 and 6 # Journal_Name: Earth and Planetary Science Letters # Volume: 439 # Edition: # Issue: # Pages: 182-193 # Report Number: # DOI: 10.1016/j.epsl.2016.01.028 # Online_Resource: http://www.sciencedirect.com/science/article/pii/S0012821X16000509 # Full_Citation: # Abstract: Over the past decades, tropical stalagmite d18O records have provided valuable insight on glacial and interglacial hydrological variability and its relationship to a variety of natural climate forcings. The transition out of the penultimate glaciation (MIS 6) represents an important target for tropical hydroclimate reconstructions, yet relatively few such reconstructions resolve this transition. Particularly, comparisons between Termination 1 and 2 provide critical insight on the extent and influence of proposed climate mechanisms determined from paleorecords and model experiments spanning the recent deglaciation. Here we present a new compilation of western tropical Pacific hydrology spanning 0-160 kyBP, constructed from eleven different U/Th-dated stalagmite d18O records from Gunung Mulu National Park in northern Borneo. The reconstruction exhibits significant precessional power in phase with boreal fall insolation strength over the 0-160 ky BP period, identifying precessional insolation forcing as the dominant driver of hydroclimate variability in northern Borneo on orbital timescales. A comparison with a network of paleoclimate records from the circum-Pacific suggests the insolation sensitivity may arise from changes in the Walker circulation system. Distinct millennial-scale increases in stalagmite d18O, indicative of reduced regional convection, occur within glacial terminations and may reflect a response to shifts in inter-hemispheric temperature gradients. Our results imply that hydroclimate in this region is sensitive to external forcing, with a response dominated by large-scale temperature gradients. #-------------------- # Publication # Authors: Stacy A. Carolin, Kim M. Cobb, Jess F. Adkins, Brian Clark, Jessica L. Conroy, Syria Lejau, Jenny Malang, Andrew A. Tuen # Published_Date_or_Year: 2013-06-28 # Published_Title: Varied Response of Western Pacific Hydrology to Climate Forcings over the Last Glacial Period # Journal_Name: Science # Volume: 340 # Edition: # Issue: 6140 # Pages: 1564-1566 # DOI: 10.1126/science.1233797 # Online_Resource: http://science.sciencemag.org/content/340/6140/1564 # Full_Citation: # Abstract: Atmospheric deep convection in the west Pacific plays a key role in the global heat and moisture budgets, yet its response to orbital and abrupt climate change events is poorly resolved. Here, we present four absolutely dated, overlapping stalagmite oxygen isotopic records from northern Borneo that span most of the last glacial cycle. The records suggest that northern Borneo's hydroclimate shifted in phase with precessional forcing but was only weakly affected by glacial-interglacial changes in global climate boundary conditions. Regional convection likely decreased during Heinrich events, but other Northern Hemisphere abrupt climate change events are notably absent. The new records suggest that the deep tropical Pacific hydroclimate variability may have played an important role in shaping the global response to the largest abrupt climate change events. #------------------ # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: 645291, 1502830, 903099 #--------------------------------------- # Site_Information # Site_Name: Clearwater Cave # Location: Ocean>Indian Ocean>Malaysia # Country: Malaysia # Northernmost_Latitude: 4.1 # Southernmost_Latitude: 4.1 # Easternmost_Longitude: 114.8333 # Westernmost_Longitude: 114.8333 # Elevation: m #------------------ # Data_Collection # Collection_Name: Borneo2016FC12-15 # First_Year: 155970 # Last_Year: 139860 # Time_Unit: cal yr BP # Core_Length: # Notes: Fairy City chamber stal FC12-15 #--------------------------------------- # Chronology_Information # Chronology: # # Original U-Series MC-ICP-MS measured values and calculated ages. ++indicates isochrons. Samples used in final published age model marked by asterisk (*) # Batch ID identifies MC-ICP-MS batch (2 letters) and sample run order within batch (1-24) # Isotope and isotope ratio errors are listed as 1sigma. # Age errors (2sigma) are Monte Carlo derived, with the following initial 230/232 ratios used to calculated the Corrected Age: # SC03 and SC02 = 111 +/- 41 ppm (2s); WR12-01 and WR12-02 = 60 +/- 20 ppm (2s); FC12-12, FC12-14, and FC15-15 = 78 +/- 42 ppm (2s) # U234 and U230 halflives provided in Cheng et al. 2013 # # Stalagmite Name Batch Depth U238 conc U238 conc 232Th 232Th d234U(T) d234U(T) 230Th/238U 230Th/238U 232Th/238U 232Th/238U Uncorr Monte Carlo Error Error init d234U # ID mm ppb error pmol/g error permil error activity activity activity activity Age Corr Age Minus Plus calc using # (1s) (1s) permil (1s) error (1s) error (1s) (cal yr BP) (cal yr BP) (2s) (2s) corr age # SC03 ck10 381.5 119.3 0.1 0.28 0.01 -87.1 0.6 0.5432 0.0006537 0.0001783 0.000005207 100544 100091 530 521 * -115.5 # SC03 ct02 397.5 130.0 0.1 0.40 0.02 -101.7 0.7 0.5446 0.0004749 0.0002343 0.000008866 104237 103627 498 500 * -136.2 # SC03 cl10 430 147.9 0.1 0.11 0.02 -115.2 0.7 0.5404 0.0005699 0.0000548 0.000010070 106018 105872 522 502 * -155.3 # SC03 ct03 454 143.5 0.1 0.84 0.02 -127.3 0.7 0.5434 0.0005381 0.0004445 0.000008733 110130 108917 683 694 * -173.2 # SC03 cs01 476 102.7 0.1 0.31 0.01 -95.1 1.3 0.5823 0.0009222 0.0002258 0.000006834 115595 115010 1007 1038 * -131.6 # SC03 cs02 505 88.5 0.1 0.14 0.01 -93.5 1.6 0.5917 0.0011065 0.0001175 0.000008411 118619 118316 1196 1265 * -130.6 # SC03 cs03 522 122.3 0.1 0.18 0.01 -91.0 1.2 0.5960 0.0008257 0.0001114 0.000005979 119510 119223 935 921 -127.4 # SC03 ct04 533.5 127.2 0.1 0.09 0.02 -85.1 0.8 0.5956 0.0006196 0.0000559 0.000010679 117672 117530 620 628 -118.6 # SC03 cs04 541 109.4 0.1 0.21 0.01 -76.9 1.3 0.6368 0.0009688 0.0001490 0.000006567 131050 130673 1206 1169 -111.2 # SC03 ct05 556.5 101.3 0.1 0.05 0.01 -80.4 0.8 0.6077 0.0005888 0.0000379 0.000010243 120835 120739 629 632 -113.1 # SC03 cr05 576 107.6 0.1 0.05 0.01 -93.7 1.4 0.5974 0.0013608 0.0000377 0.000007926 120812 120715 1283 1334 -131.7 # SC03 cr01 594 95.2 0.1 0.03 0.01 -71.6 1.4 0.6232 0.0016051 0.0000253 0.000009894 124045 123982 1447 1535 -101.6 # SC03 cl18 642.5 90.3 0.1 0.08 0.02 -51.4 0.9 0.6432 0.0006838 0.0000632 0.000017717 125564 125410 728 724 -73.2 # FC12-14 co13 19 190.7 0.1 1.25 0.08 -124.7 0.7 0.4303 0.0003462 0.0004972 0.000031161 75267 74337 581 562 * -153.9 # FC12-14 cp18 166 70.9 0.1 1.19 0.02 -146.4 0.9 0.4708 0.0007857 0.0012702 0.000021825 90209 87714 1476 1437 * -187.5 # FC12-14 cs21 207 54.3 0.1 1.69 0.01 -73.2 3.1 0.6526 0.0019786 0.0023583 0.000016697 136379 132135 3537 3677 -106.2 # FC12-14 cp19 216.5 64.1 0.1 0.29 0.03 -111.0 1.3 0.6071 0.0012678 0.0003481 0.000033334 130241 129585 1455 1466 * -160.0 # FC12-14 cx01 227.75 51.2 0.1 2.48 0.00 -88.2 3.2 0.6414 0.0010229 0.0036794 0.000006351 136973 130104 4624 4374 * -127.3 # FC12-14 cx02 239.5 51.4 0.1 2.06 0.00 -111.7 2.7 0.6319 0.0013265 0.0030451 0.000007193 141766 135858 4112 4031 * -163.9 # FC12-14 ct08 247 57.5 0.1 1.27 0.01 -142.9 1.2 0.6062 0.0008136 0.0016783 0.000017054 142342 138928 2298 2265 * -211.5 # FC12-14 ct09 261 58.6 0.1 1.79 0.01 -146.3 1.3 0.6133 0.0009450 0.0023153 0.000019119 147620 142835 3079 3043 * -218.9 # FC12-14 cs22 270.75 36.6 0.1 1.44 0.01 -106.5 4.6 0.6560 0.0028045 0.0029866 0.000024148 151556 145788 5833 6281 * -160.7 # FC12-14 ct10 275.5 44.0 0.1 4.15 0.01 -95.5 1.6 0.7019 0.0010949 0.0071605 0.000024045 171999 157800 8745 8083 -149.1 # FC12-14 cx03 294.5 53.4 0.0 1.65 0.00 -113.5 0.6 0.6642 0.0006588 0.0023492 0.000005624 159597 155001 2730 2652 -175.8 # FC12-14 ct11 311.5 82.9 0.1 1.50 0.01 -141.3 0.8 0.6337 0.0006701 0.0013733 0.000012007 156600 153792 2005 1901 * -218.0 # FC12-14 cx05 324.5 86.5 0.0 0.80 0.00 -131.7 0.5 0.6480 0.0006043 0.0006983 0.000003902 159879 158483 1161 1142 * -206.0 # FC12-14 cn19 332.25 79.3 0.2 1.26 0.02 -165.9 2.4 0.6252 0.0015844 0.0012106 0.000019478 165631 163008 3900 4187 * -262.8 # FC12-12 co07 14.8 368.0 0.2 2.94 0.08 -349.3 0.4 0.2443 0.0001587 0.0006069 0.000017375 53981 52358 879 881 -404.9 # FC12-12 cs14 329.2 0.2 2.34 0.01 -392.4 0.6 0.2687 0.0003203 0.0005396 0.000002686 69261 67625 950 923 -474.9 # FC12-12 cp01 124.9 294.7 0.1 0.79 0.02 -330.1 0.3 0.3430 0.0002614 0.0002033 0.000005073 85157 84603 392 387 -419.2 # FC12-12 cp20 153.8 183.4 0.1 0.96 0.02 -319.1 0.4 0.3948 0.0003770 0.0003977 0.000008573 105350 104247 770 743 -428.2 # FC12-12 cu14 223.8 277.3 0.2 1.60 0.00 -282.5 0.6 0.4304 0.0003330 0.0004380 0.000000904 110016 108888 817 810 * -384.2 # FC12-12 cx10 240.8 196.3 0.1 0.66 0.00 -294.5 0.2 0.4285 0.0002837 0.0002553 0.000001275 113498 112819 504 490 * -405.0 # FC12-12 ++ cx06 258.3 134.6 0.1 0.29 0.00 -271.7 0.3 0.4512 0.0003381 0.0001651 0.000002068 116374 115956 461 475 * -376.8 # FC12-12 ++ cx07 258.3 225.2 0.1 0.42 0.00 -268.7 0.2 0.4532 0.0003017 0.0001423 0.000001460 116274 115915 397 400 -372.7 # FC12-12 ++ cx09 258.3 142.4 0.1 0.55 0.00 -268.2 0.3 0.4555 0.0003988 0.0002957 0.000002223 117235 116488 619 607 -372.6 # FC12-12 cu15 275.8 104.3 0.2 0.55 0.00 -249.6 1.7 0.4762 0.0008381 0.0003974 0.000002667 120482 119514 1658 1695 * -349.7 # FC12-12 cu16 330.8 142.6 0.2 0.10 0.00 -231.6 1.3 0.4895 0.0006317 0.0000544 0.000001741 120236 120108 1155 1181 * -325.1 # FC12-12 cn15 380.8 92.5 0.1 0.24 0.02 -217.0 1.6 0.5111 0.0009677 0.0001946 0.000013048 125272 124827 1603 1615 * -308.7 # FC12-15 co04 71.8 0.1 0.22 0.09 -80.8 1.7 0.6365 0.0009538 0.0002371 0.000091131 132250 131826 1459 1466 -117.2 # FC12-15 cp12 64.0 0.1 0.27 0.03 -50.0 1.3 0.6632 0.0012794 0.0003204 0.000034394 132845 132298 1355 1388 -72.6 # FC12-15 cp09 18 54.7 0.1 0.36 0.03 -118.3 1.6 0.6236 0.0014285 0.0005011 0.000036827 140536 139573 1987 2018 * -175.5 # FC12-15 cx11 40 48.7 0.0 1.03 0.00 -123.8 0.6 0.6325 0.0006059 0.0016079 0.000004901 147303 144140 1908 1847 * -185.9 # FC12-15 ++ cx13 64 41.7 0.0 0.63 0.00 -86.7 0.7 0.6660 0.0007818 0.0011378 0.000006613 147784 145699 1492 1505 * -130.7 # FC12-15 ++ cx14 64 46.6 0.0 1.07 0.01 -76.2 0.8 0.6771 0.0008530 0.0017349 0.000008248 148694 145557 2014 2022 -114.9 # FC12-15 ++ cx15 64 49.3 0.0 4.11 0.01 -95.0 0.6 0.7036 0.0007858 0.0063287 0.000007878 172748 160298 7279 7090 -149.4 # FC12-15 cx17 99.5 59.8 0.0 0.44 0.00 -127.9 0.6 0.6287 0.0006236 0.0005611 0.000004995 147205 146103 1042 1060 * -193.2 # FC12-15 cx18 176.5 50.1 0.0 0.41 0.00 -129.4 0.5 0.6391 0.0008132 0.0006227 0.000004664 153531 152298 1196 1231 * -198.9 # FC12-15 cx19 217 52.3 0.0 0.66 0.00 -166.2 0.5 0.6104 0.0006499 0.0009598 0.000005533 156270 154212 1475 1509 * -256.9 # FC12-15 cp07 289.8 68.1 0.1 0.17 0.03 -175.8 1.1 0.6117 0.0011345 0.0001884 0.000029831 162728 162315 2000 2078 * -277.9 # FC12-15 cp06 66.1 0.1 1.23 0.03 -184.3 1.1 0.6229 0.0011857 0.0014148 0.000031161 176872 173627 3080 3214 -300.9 # FC12-15 cn18 81.5 0.2 0.45 0.02 -131.9 2.3 0.6708 0.0015767 0.0004169 0.000018234 174659 173817 3701 3964 -215.5 # WR12-01 co11 6.4 491.1 0.2 0.98 0.08 -33.7 0.5 0.6320 0.0002743 0.0001514 0.000012301 116762 116570 466 463 * -46.8 # WR12-01 cp08 26 230.6 0.1 1.32 0.03 -29.2 0.5 0.6492 0.0005800 0.0004355 0.000008759 121459 120907 640 622 * -41.1 # WR12-01 cy01 38.3 523.5 0.2 4.12 0.00 -17.1 0.4 0.6634 0.0003251 0.0005980 0.000000283 123116 122370 551 555 * -24.2 # WR12-01 cs18 42 483.1 0.2 7.87 0.01 -26.5 0.4 0.6685 0.0004471 0.0012361 0.000001701 127589 126019 772 763 * -37.9 # WR12-01 cs19 47.3 379.0 0.2 1.63 0.01 -31.2 0.6 0.6678 0.0005560 0.0003266 0.000002246 128684 128269 670 671 * -44.8 # WR12-01 ++ cp04 54 336.6 0.1 0.15 0.03 -29.0 0.4 0.6694 0.0004805 0.0000330 0.000005963 128645 128604 566 573 * -41.7 # WR12-01 ++ cy03 54 372.1 0.2 0.45 0.00 -29.3 0.4 0.6696 0.0004067 0.0000920 0.000000398 128799 128682 550 554 -42.1 # WR12-01 ++ cy05 54 421.0 0.3 0.29 0.00 -30.2 0.5 0.6656 0.0003703 0.0000517 0.000000315 127597 127532 558 567 -43.3 # WR12-01 ct13 68.5 343.0 0.1 0.48 0.02 -29.4 0.4 0.6712 0.0004395 0.0001057 0.000003407 129445 129311 540 561 * -42.4 # WR12-01 cs17 90 363.7 0.2 0.15 0.01 -34.3 0.6 0.6781 0.0005435 0.0000317 0.000002215 133595 133554 688 704 -34.3 # WR12-01 ct14 92 362.6 0.1 1.20 0.02 -27.9 0.4 0.6763 0.0004260 0.0002513 0.000003230 130884 130566 566 574 * -40.3 # WR12-01 ct15 129 386.3 0.1 0.30 0.02 -20.7 0.3 0.6851 0.0004190 0.0000596 0.000003156 131958 131883 538 545 * -30.0 # WR12-01 cp03 131 389.5 0.2 0.38 0.03 -20.4 0.3 0.6865 0.0004627 0.0000740 0.000005299 132430 132338 576 562 * -29.6 # WR12-01 cs16 134 265.3 0.2 3.19 0.01 -13.2 0.8 0.7125 0.0006723 0.0009116 0.000003029 140222 139088 944 971 * -19.5 # WR12-01 cy02 146 250.1 0.1 0.17 0.00 -13.3 0.4 0.7138 0.0004784 0.0000510 0.000000443 140798 140735 627 634 * -19.8 # WR12-01 cy06 180 333.6 0.2 0.30 0.00 -5.2 0.4 0.7299 0.0004219 0.0000682 0.000000426 144531 144447 631 633 * -7.8 # WR12-01 cp15 197 258.7 0.1 2.27 0.02 -10.3 0.4 0.7376 0.0004254 0.0006670 0.000006612 149714 148889 701 706 * -15.7 # WR12-01 cy07 219 287.1 0.1 0.39 0.00 -3.8 0.4 0.7406 0.0003769 0.0001019 0.000000321 148516 148392 628 625 * -5.8 # WR12-01 cn10 281.5 319.6 0.2 0.23 0.01 -6.9 0.6 0.7479 0.0004968 0.0000539 0.000003493 152906 152840 828 826 * -10.6 # WR12-12 cs06 4.5 383.9 0.2 0.72 0.01 -40.0 0.6 0.6189 0.0006018 0.0001431 0.000002400 113997 113813 589 588 * -55.2 # WR12-12 cu11 26.75 421.4 0.2 0.36 0.00 -30.3 0.5 0.6382 0.0003586 0.0000640 0.000000581 118012 117931 517 506 * -42.3 # WR12-12 ct21 44.5 370.7 0.1 0.18 0.02 -30.0 0.4 0.6478 0.0004087 0.0000360 0.000003550 121173 121128 499 493 * -42.2 # WR12-12 cu10 50 365.1 0.2 0.11 0.00 -30.7 0.6 0.6488 0.0004310 0.0000234 0.000000745 121711 121681 588 574 * -43.3 # WR12-12 cu09 58.5 435.4 0.2 3.51 0.00 -32.6 0.5 0.6558 0.0003913 0.0006113 0.000000658 124732 123952 609 616 * -46.3 # WR12-12 cy09 60.75 391.8 0.2 7.32 0.00 -34.3 0.4 0.6653 0.0003139 0.0014180 0.000000553 128703 126879 807 791 * -49.0 # WR12-12 cu07 64.75 254.0 0.2 3.70 0.00 -14.9 0.8 0.6899 0.0005125 0.0011070 0.000001127 131999 130618 850 874 * -21.6 # WR12-12 ct22 71.75 272.0 0.1 0.48 0.02 -7.3 0.4 0.6997 0.0004043 0.0001343 0.000004563 133332 133167 566 561 * -10.7 # WR12-12 ++ cu13 85.75 238.0 0.2 0.80 0.00 -4.6 0.8 0.7062 0.0005364 0.0002551 0.000000982 134906 134594 757 799 * -6.7 # WR12-12 ++ cy10 85.75 301.4 0.2 0.33 0.00 -3.6 0.4 0.7067 0.0004484 0.0000837 0.000000531 134821 134719 578 592 -5.2 # WR12-12 ++ cy11 85.75 271.4 0.2 0.80 0.00 -7.0 0.4 0.7012 0.0004365 0.0002246 0.000000542 133789 133514 600 585 -10.2 # WR12-12 cs07 103.25 252.5 0.2 0.54 0.01 -2.6 0.7 0.7182 0.0006948 0.0001622 0.000003260 138890 138693 838 856 * -3.9 # WR12-12 cy13 120.75 238.8 0.2 0.61 0.00 -1.7 0.5 0.7318 0.0004659 0.0001925 0.000000646 144079 143845 687 666 * -2.6 # #--------------------------------------- # 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_mm depth, , , mm, , , , ,N ## age_calBP age, , , calendar years before present, , , , ,N ## d18OcarbVPDB delta18O, calcium carbonate, , per mil VPDB, ,speleothem, , analytical technique: isotope ratio mass spectrometry,N ## d18Ocarbadj delta18O, calcium carbonate, , per mil VPDB, ,speleothem, shifted d18O to align with SCH02's mean d18O, ,N ## d18Ocarbivc delta18O, calcium carbonate, , per mil VPDB, ,speleothem, shifted d18Oadj to remove mean ocean d18O variability due to ice volume growth/decay, ,N # #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: # Fairy City chamber stal FC12-15. # depth_mm age_calBP d18OcarbVPDB d18Ocarbadj d18Ocarbivc 18 139860 -7.37 -6.77 -7.77 19 139931 -7.19 -6.59 -7.59 20 140002 -7.53 -6.93 -7.93 21 140072 -7.45 -6.85 -7.85 22 140143 -7.67 -7.07 -8.06 23 140214 -7.93 -7.33 -8.32 24 140287 -8.10 -7.50 -8.48 25 140360 -7.93 -7.33 -8.31 26 140434 -8.38 -7.78 -8.76 27 140506 -8.05 -7.45 -8.43 28 140579 -8.24 -7.64 -8.62 29 140651 -7.91 -7.31 -8.28 30 140723 -8.01 -7.41 -8.38 31 140796 -7.93 -7.33 -8.30 32 140870 -8.48 -7.88 -8.85 33 140942 -8.34 -7.74 -8.70 34 141015 -8.13 -7.53 -8.50 35 141089 -8.03 -7.43 -8.39 36 141163 -8.12 -7.52 -8.48 37 141238 -8.03 -7.43 -8.39 38 141314 -8.13 -7.53 -8.48 39 141391 -8.51 -7.91 -8.86 40 141470 -7.89 -7.29 -8.23 41 141551 -8.23 -7.63 -8.57 42 141633 -8.14 -7.54 -8.48 43 141717 -8.15 -7.55 -8.49 44 141804 -8.20 -7.60 -8.53 45 141896 -8.28 -7.68 -8.61 46 141993 -8.51 -7.91 -8.84 47 142093 -8.80 -8.20 -9.12 48 142191 -8.39 -7.79 -8.72 49 142283 -8.25 -7.65 -8.57 50 142371 -8.18 -7.58 -8.50 51 142457 -8.52 -7.92 -8.83 52 142541 -8.36 -7.76 -8.68 53 142620 -8.23 -7.63 -8.54 54 142697 -8.32 -7.72 -8.63 55 142775 -8.12 -7.52 -8.42 56 142856 -8.27 -7.67 -8.57 58 143021 -8.15 -7.55 -8.45 60 143173 -8.30 -7.70 -8.60 62 143332 -8.44 -7.84 -8.73 64 143485 -8.40 -7.80 -8.69 66 143624 -8.54 -7.94 -8.83 68 143755 -8.50 -7.90 -8.78 70 143899 -8.41 -7.81 -8.69 72 144034 -8.72 -8.12 -9.00 74 144159 -8.56 -7.96 -8.84 76 144284 -8.31 -7.71 -8.59 78 144420 -9.05 -8.45 -9.32 80 144544 -8.78 -8.18 -9.05 82 144669 -8.43 -7.83 -8.70 84 144788 -8.73 -8.13 -9.00 86 144913 -8.52 -7.92 -8.79 88 145034 -8.66 -8.06 -8.93 90 145148 -8.72 -8.12 -9.00 92 145260 -8.71 -8.11 -8.99 94 145367 -8.62 -8.02 -8.90 96 145480 -9.30 -8.70 -9.59 98 145592 -9.31 -8.71 -9.59 100 145702 -9.58 -8.98 -9.87 102 145811 -9.51 -8.91 -9.80 104 145929 -9.20 -8.60 -9.49 106 146049 -9.28 -8.68 -9.57 108 146172 -9.30 -8.70 -9.60 110 146297 -9.27 -8.67 -9.58 112 146425 -8.99 -8.39 -9.30 114 146559 -8.81 -8.21 -9.12 116 146694 -8.87 -8.27 -9.19 118 146827 -9.01 -8.41 -9.34 120 146959 -9.06 -8.46 -9.39 122 147093 -9.05 -8.45 -9.39 124 147226 -9.19 -8.59 -9.54 126 147361 -9.20 -8.60 -9.55 128 147497 -8.81 -8.21 -9.17 130 147636 -8.89 -8.29 -9.26 132 147772 -9.18 -8.58 -9.55 134 147913 -9.33 -8.73 -9.71 136 148058 -9.50 -8.90 -9.88 138 148201 -8.85 -8.25 -9.23 140 148341 -9.17 -8.57 -9.56 142 148479 -9.06 -8.46 -9.45 144 148618 -9.00 -8.40 -9.40 146 148753 -9.02 -8.42 -9.43 150 149019 -8.97 -8.37 -9.38 152 149149 -9.12 -8.52 -9.53 154 149284 -8.69 -8.09 -9.10 156 149417 -9.08 -8.48 -9.50 158 149550 -9.32 -8.72 -9.74 160 149684 -9.01 -8.41 -9.43 162 149817 -8.87 -8.27 -9.29 164 149954 -8.69 -8.09 -9.11 166 150092 -8.32 -7.72 -8.74 168 150228 -8.57 -7.97 -8.99 169 150300 -8.66 -8.06 -9.08 171 150442 -8.46 -7.86 -8.88 173 150579 -8.26 -7.66 -8.68 175 150719 -8.13 -7.53 -8.55 177 150858 -8.32 -7.72 -8.73 179 151001 -8.31 -7.71 -8.73 181 151143 -8.54 -7.94 -8.96 183 151282 -8.49 -7.89 -8.90 185 151426 -8.68 -8.08 -9.09 187 151571 -8.68 -8.08 -9.09 191 151861 -8.59 -7.99 -8.99 193 152005 -8.57 -7.97 -8.97 195 152146 -8.77 -8.17 -9.18 197 152293 -8.68 -8.08 -9.08 199 152443 -8.93 -8.33 -9.33 201 152589 -8.93 -8.33 -9.32 203 152737 -8.45 -7.85 -8.83 205 152889 -8.25 -7.65 -8.64 207 153039 -8.28 -7.68 -8.66 209 153185 -8.38 -7.78 -8.75 211 153333 -8.77 -8.17 -9.13 213 153479 -8.68 -8.08 -9.04 215 153626 -8.91 -8.31 -9.25 217 153776 -8.43 -7.83 -8.76 219 153925 -8.43 -7.83 -8.75 221 154076 -8.45 -7.85 -8.75 223 154229 -8.46 -7.86 -8.74 225 154380 -8.68 -8.08 -8.95 227 154528 -8.66 -8.06 -8.91 229 154680 -8.51 -7.91 -8.74 231 154834 -8.38 -7.78 -8.59 233 154984 -8.45 -7.85 -8.64 235 155166 -8.56 -7.96 -8.73 237 155341 -8.37 -7.77 -8.52 239 155491 -8.59 -7.99 -8.72 241 155651 -8.53 -7.93 -8.64 243 155807 -8.30 -7.70 -8.40 245 155970 -8.26 -7.66 -8.34