# Partin et al. 2007 Northern Borneo Stalagmite Oxygen Isotope Data #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # Template Version 4.0 # Encoding: UTF-8 # NOTE: Please cite original publication, NOAA Landing Page URL, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, study title, NOAA Landing Page URL, and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/5538 # Landing_Page_Description: NOAA Landing Page of this file's parent study, which includes all study metadata. # # Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-cave-5538.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Speleothems # # Dataset_DOI: 10.25921/vd61-pw29 # # Science_Keywords: Last Glacial Maximum #-------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/speleothem/pacific/gunung-buda2007-BA04-noaa.txt # Data_Download_Description: NOAA Template File; Stalagmite BA04 Isotope Data # #-------------------- # Contribution_Date # Date: 2011-06-01 #-------------------- # File_Last_Modified_Date # Date: 2025-01-31 #-------------------- # Title # Study_Name: Partin et al. 2007 Northern Borneo Stalagmite Oxygen Isotope Data #-------------------- # Investigators # Investigators: Partin, J.W.; Cobb, K.M.; Adkins, J.F.; Clark, B.; Fernandez, D.P. #-------------------- # Description_Notes_and_Keywords # Description: Three stalagmite d18O records from Gunung Buda National Park, Northern Borneo, Malaysia (4º02'N, 114º48'E, elev. 150m), for the last 27ka. Samples SSC01 and SCH02 originate from Snail Shell Cave and formed ~250m from the cave entrance and ~20m from each other. Sample BA04 formed >500m from the cave entrance in Bukit Assam Cave, which lies ~6km NNE from Snail Shell Cave. # # The age model for each record is comprised of 24-26 U/Th Dates corrected using stalagmite specific 230Th/232Th (Suppl. Info in Partin et al., 2007; Adkins et al., 2007); breaks in the record are dated hiatuses. The average temporal resolution for each d18O record is 72, 56, and 60 yrs/sample for SCH02, SSC01, and BA04, respectively. Rules for establishing the age models from U/Th dates, as well as known hiatuses, are provided below. A "master d18O record" is constructed by splicing together portions of the three individual records. The master record is best used with error bars calculated from overlapping portions of all three stalagmites. For all records, d18O data are reported with respect to PDB, and ages are reported as years before present. Two rules were used for establishing the final age model: 1) For ages older than 11,000 years, individual age errors for a U-series point must be less than 2% (2s), 2) For ages younger than 11,000 years we only keep points with uncertainties of less than 400 years. Two additional rules used to pick dates: 1) Use only one point per isochron – that with the lowest error bar, 2) When there is overlap between two ages within error, take the age with the smallest error bar. # # Rules for establishing length of a hiatus: After visually examining the stalagmites for indications of a hiatus, all potential bands were checked for missing years by extending the young part of the adjacent age constraints downward and the older age constraints upward. If there is a difference in predicted age at the visual band's depth that is larger than 400 years and the age difference is larger than the propagated uncertainty, we declare that band a hiatus. A hiatus' duration is taken to be the difference in age between the upper and lower age model constraints. # # UPDATE: 6/2008 (substitute revised age model) Corregendum, Nature 4 June 2009: A recalibration of the Caltech 236U and 229Th spike has determined that the original spike value used for the stalagmite chronologies yielded U-Th ages that were too old by a margin of ~2-3%. U-Th ages and subsequent age models have been recalculated using the new spike value for all stalagmites. The new age models alter the absolute timing of certain events, but do not alter any major conclusions of the original manuscript. The highest d18O values (inferred driest conditions) now occur at 16.0 +/- 0.3 kyr ago. A late deglacial d18O plateau in the Borneo stalagmite records is now centered at 13.0 +/- 0.2 kyr ago. The lowest d18O values (inferred wettest conditions) now occur at 5.0 +/- 0.1 kyr ago. Examples of original and adjusted dates, respectively, at 5 kyr intervals are as follows: 5280 versus 5141 (SSC01); 10581 versus 10293 (SSC01); 15673 versus 15231 (BA04); 20937 versus 20322 (BA04); and 26387 versus 25602 (SCH02). # # UPDATE: 6/16/2011 (add spliced record) # # LAST UPDATE: 8/4/2022 (updated spliced "master" record added) ** Both original citations Partin et al. 2007 (doi:10.1038/nature06164) and Buckingham et al. 2022 (doi:10.1029/2021GL096937) should be cited when using this updated spliced record! ** Notes for updated spliced "master" record: Spliced master record updated to include Mulu Secret Chamber stalagmite SC02 d18O, published in Buckingham et al., 2022 (doi:10.1029/2021GL096937). SC02 replaces SCH02 at the end of the deglaciation (12-15ka) in this updated spliced record as SC02 has the most reliable age model during that time period (see Buckingham et al., 2022). SC02 d18O values have been adjusted by +0.2 permil for the splice record, following the methods of Carolin et al., 2016 (doi:10.1016/j.epsl.2016.01.028). #-------------------- # Publication # Authors: Partin, J.W., K.M. Cobb, J.F. Adkins, B. Clark, and D.P. Fernandez # Published_Date_or_Year: 2007-03-01 # Published_Title: Millennial-scale trends in west Pacific warm pool hydrology since the Last Glacial Maximum # Journal_Name: Nature # Volume: 449 # Edition: # Issue: 7161 # Pages: 452-455 # Report_Number: # DOI: 10.1038/nature06164 # Online_Resource: # Full_Citation: # Abstract: Models and palaeoclimate data suggest that the tropical Pacific climate system plays a key part in the mechanisms underlying orbital-scale and abrupt climate change. Atmospheric convection over the western tropical Pacific is a major source of heat and moisture to extratropical regions, and may therefore influence the global climate response to a variety of forcing factors. The response of tropical Pacific convection to changes in global climate boundary conditions, abrupt climate changes and radiative forcing remains uncertain, however. Here we present three absolutely-dated oxygen isotope records from stalagmites in northern Borneo that reflect changes in west Pacific warm pool hydrology over the past 27,000 years. Our results suggest that convection over the western tropical Pacific weakened 18,000-20,000 years ago, as tropical Pacific and Antarctic temperatures began to rise during the early stages of deglaciation. Convective activity, as inferred from oxygen isotopes, reached a minimum during Heinrich event 1, when the Atlantic meridional overturning circulation was weak, pointing to feedbacks between the strength of the overturning circulation and tropical Pacific hydrology. There is no evidence of the Younger Dryas event in the stalagmite records, however, suggesting that different mechanisms operated during these two abrupt deglacial climate events. During the Holocene epoch, convective activity appears to track changes in spring and autumn insolation, highlighting the sensitivity of tropical Pacific convection to external radiative forcing. Together, these findings demonstrate that the tropical Pacific hydrological cycle is sensitive to high-latitude climate processes in both hemispheres, as well as to external radiative forcing, and that it may have a central role in abrupt climate change events. #-------------------- # Publication # Authors: Buckingham, F.; Carolin, S.A.; Partin, J.W.; Adkins, J.F.; Cobb, K.M.; Day, C.C.; Ding, Q.; He, C.; Liu, Z.; Otto-Bliesner, B.; Roberts, W.H.G.; Lejau, S.; Malang, J. # Published_Date_or_Year: 2022-03-16 # Published_Title: Termination 1 Millennial-scale Rainfall Events over the Sunda Shelf # Journal_Name: Geophysical Research Letters # Volume: 49 # Edition: # Issue: 5 # Pages: # Report_Number: e2021GL096937 # DOI: 10.1029/2021GL096937 # Online_Resource: # Full_Citation: # Abstract: Recent paleoclimate reconstructions have suggested millennial-scale variability in the Indo-Pacific Warm Pool region coincident with events of the last deglaciation. Here we present a new stalagmite oxygen isotope record from northern Borneo, which today is located near the center of the region’s mean annual inter-tropical convergence zone. The record spans the full deglaciation, and reveals for the first time distinct oxygen isotope variations at this location connected with the Bølling-Allerød onset and the Younger Dryas event. The full deglaciation in the Borneo stalagmite proxy reconstruction appears remarkably similar to a 20-11 ka transient simulation of rainfall over the area produced using the isotope-enabled Community Earth System Model. In this model, periods of weakened Atlantic Ocean meridional overturning circulation are associated with an anomalous Western North Pacific anticyclone, which is produced in boreal autumn and shifts south over Borneo during boreal winter, causing dry conditions. #-------------------- # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: #-------------------- # Funding_Agency # Funding_Agency_Name: Comer Abrupt Climate Change Fellowship # Grant: #-------------------- # Site_Information # Site_Name: Gunung Buda National Park # Location: Malaysia # Northernmost_Latitude: 4.03 # Southernmost_Latitude: 4.03 # Easternmost_Longitude: 114.8 # Westernmost_Longitude: 114.8 # Elevation_m: 150 #-------------------- # Data_Collection # Collection_Name: BA04 # First_Year: 26162 # Last_Year: 0 # Time_Unit: cal yr BP # Core_Length_m: # Parameter_Keywords: # Notes: Note that these raw BA04 d18O data are ~0.4per mil heavier than SSC01 and SCH02. In Figure 3 of Partin et al., 2007, BA04 data were shifted by -0.4 per mil, in order to overlap SSC01 and SCH02. #-------------------- # Chronology_Information # Chronology: Uranium-Thorium # Chronology_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/templates/noaa-wds-paleo-uth-terms.csv # Chronology_Download_Description: Uranium-Thorium terms and definitions. # Chronology_Notes: Stalagmite BA04 UTh Dating and Stable Isotope Data, updated 2009 age model. Hiatuses Indentified, their depths and durations: 28 mm: 1818 +/- 918 years (2s); 133.1 mm: 597 +/- 436 years (2s); 216.8 mm: 850 +/- 273 years (2s); 300.5 mm: 576 +/- 438 years (2s); 391.7 mm: 614 +/- 257 years (2s); 492.9 mm: 4746 +/- 2254 years (2s) # Rejection_Rationale: # 238U_Decay_Constant: # 234U_Decay_Constant: # 230Th_Decay_Constant: # Initial_230Th/232Th: # Initial_230Th/232Th_Method: # Age_Model_Method: # Missing_Values: na # Chronology_Table: #samp_id depth_top_mm 238U_ppb 238U_2s_ppb 232Th_pmol/g 232Th_2s_pmol/g d234U_meas_permil d234U_meas_2s_permil 230Th_238U_act 230Th_238U_act_2s age_uncorr_BM age_uncorr_2s_yr age_corr_BP1950 age_corr_2s_yr date_used date_type #sc01 11.00 1241.96 0.20 93.8 0.14 -605.6 0.4 0.06482 0.00031 1750 10 2119 1750 no MC-ICP-MS U/Th #sg21 14.35 1089.23 0.26 32.8 0.02 -620.2 0.2 0.03037 0.00009 656 6 2206 656 yes MC-ICP-MS U/Th #hiatus1 28 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #sc02 31.20 1055.49 0.24 72.3 0.08 -611.3 0.5 0.06466 0.00040 1603 24 3916 1603 no MC-ICP-MS U/Th #sc03 31.20 1139.40 0.19 86.5 0.12 -612.1 0.4 0.06242 0.00032 1787 6 1254 1787 no MC-ICP-MS U/Th #sc04 31.20 1557.80 0.22 239.9 0.30 -600.6 0.4 0.12418 0.00032 4294 5 2042 4294 no MC-ICP-MS U/Th #sc05 31.20 1562.54 0.20 270.3 0.38 -599.7 0.3 0.12934 0.00048 4958 -7 -1761 -4958 no MC-ICP-MS U/Th #sg09 35.40 1279.56 0.34 6.1 0.00 -619.2 0.2 0.02487 0.00009 99 23 6417 102 yes MC-ICP-MS U/Th #sd01 83.10 1260.72 0.03 2.6 0.00 -613.2 1.3 0.02931 0.00013 43 37 8312 57 yes MC-ICP-MS U/Th #sg20 103.10 1314.99 0.27 12.0 0.01 -611.2 0.1 0.03680 0.00007 191 17 9056 192 no MC-ICP-MS U/Th #sg23 103.10 1361.28 0.29 4.5 0.01 -612.0 0.2 0.03267 0.00007 69 19 9077 71 yes MC-ICP-MS U/Th #sg36 103.10 1414.79 0.30 6.7 0.01 -612.5 0.2 0.03388 0.00006 99 17 9153 100 no MC-ICP-MS U/Th #sg15 103.10 1399.47 0.42 16.4 0.02 -611.1 0.2 0.03794 0.00009 246 21 8826 247 no MC-ICP-MS U/Th #si18 130.70 961.03 0.21 17.8 0.02 -607.8 0.2 0.04628 0.00006 395 13 9872 395 yes MC-ICP-MS U/Th #hiatus2 133.1 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #si05 139.90 1196.00 0.30 6.5 0.02 -609.1 0.2 0.03929 0.00006 114 16 10645 115 yes MC-ICP-MS U/Th #sc06 150.50 1538.14 0.16 203.2 0.20 -591.6 0.3 0.08536 0.00020 3229 -13 -5710 -3229 no MC-ICP-MS U/Th #si26 156.00 1536.29 0.33 3.1 0.02 -605.3 0.1 0.03802 0.00004 42 13 10895 44 yes MC-ICP-MS U/Th #si19 169.15 1548.14 0.32 5.2 0.02 -603.2 0.2 0.03924 0.00005 68 13 10928 70 yes MC-ICP-MS U/Th #sg26 178.85 1995.90 0.41 6.0 0.01 -604.8 0.1 0.03906 0.00005 62 15 10990 64 yes MC-ICP-MS U/Th #sd02 198.15 1714.95 0.04 1.4 0.00 -606.0 1.3 0.03797 0.00013 17 37 11174 41 yes MC-ICP-MS U/Th #si02 203.00 1430.45 0.35 16.3 0.02 -604.9 0.2 0.04620 0.00006 239 16 11413 240 no MC-ICP-MS U/Th #si30 204.60 1578.98 0.38 2.0 0.02 -606.3 0.2 0.03900 0.00005 26 14 11418 29 yes MC-ICP-MS U/Th #sg16 213.10 993.97 0.26 15.0 0.02 -607.4 0.2 0.04696 0.00011 320 25 10895 321 no MC-ICP-MS U/Th #hiatus3 216.8 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #sd03 229.80 1179.69 0.04 8.9 0.00 -604.8 1.2 0.04822 0.00012 157 31 12985 160 yes MC-ICP-MS U/Th #sc07 248.10 1316.25 0.16 58.7 0.08 -604.5 0.3 0.06677 0.00024 1000 38 10508 1001 no MC-ICP-MS U/Th #sd04 256.80 1146.24 0.03 15.3 0.01 -606.8 1.3 0.05477 0.00018 286 46 13932 290 no MC-ICP-MS U/Th #sg11 265.30 1155.21 0.34 33.7 0.01 -605.3 0.2 0.06333 0.00012 641 24 13094 642 no MC-ICP-MS U/Th #sd05 289.40 1377.93 0.04 6.6 0.00 -599.7 1.3 0.05045 0.00011 98 31 14151 103 yes MC-ICP-MS U/Th #hiatus4 300.5 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #sg10 310.00 1213.03 0.30 5.1 0.00 -599.7 0.2 0.05329 0.00009 88 27 15231 92 yes MC-ICP-MS U/Th #sc08 315.60 1324.78 0.15 21.9 0.07 -596.0 0.3 0.06166 0.00022 348 55 15090 352 no MC-ICP-MS U/Th #sg14 316.55 1288.80 0.31 45.5 0.02 -597.0 0.2 0.07284 0.00010 775 20 14614 775 no MC-ICP-MS U/Th #sg27 322.60 1337.98 0.30 18.4 0.02 -597.4 0.2 0.05991 0.00008 289 19 15199 289 no MC-ICP-MS U/Th #si16 328.30 1346.19 0.29 23.9 0.02 -594.1 0.2 0.06350 0.00007 373 16 15358 373 no MC-ICP-MS U/Th #si22 333.50 1389.88 0.31 15.5 0.02 -596.3 0.2 0.06049 0.00007 234 19 15937 234 yes MC-ICP-MS U/Th #sd06 350.70 1199.44 0.04 5.3 0.00 -595.7 1.2 0.06057 0.00013 92 38 17477 100 yes MC-ICP-MS U/Th #sd07 350.70 1139.38 0.03 11.5 0.00 -595.1 1.3 0.06532 0.00017 211 45 17810 216 no MC-ICP-MS U/Th #sd08 350.70 1114.60 0.03 14.8 0.00 -593.7 1.3 0.07202 0.00016 281 42 19370 284 no MC-ICP-MS U/Th #sg13 371.35 1237.86 0.30 6.8 0.00 -596.4 0.2 0.06406 0.00010 115 28 18491 119 yes MC-ICP-MS U/Th #hiatus5 391.7 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #sg12 398.25 1429.53 0.36 4.9 0.00 -598.2 0.2 0.06754 0.00009 72 27 20322 77 yes MC-ICP-MS U/Th #sc09 416.20 1590.87 0.17 231.0 0.18 -574.0 0.2 0.18379 0.00025 4287 42 31075 4288 no MC-ICP-MS U/Th #sc10 416.20 1465.75 0.17 11.9 0.01 -594.2 0.3 0.07225 0.00022 172 62 20675 182 no MC-ICP-MS U/Th #sc11 416.20 1433.32 0.18 2.6 0.01 -595.2 0.3 0.06871 0.00022 38 68 20917 78 yes MC-ICP-MS U/Th #sc12 416.20 1313.43 0.16 3.3 0.01 -594.2 0.3 0.06936 0.00027 53 81 20932 96 no MC-ICP-MS U/Th #sg17 443.85 1351.30 0.40 3.4 0.02 -589.7 0.2 0.07371 0.00010 51 30 22207 60 yes MC-ICP-MS U/Th #si29 453.15 1259.42 0.31 2.5 0.02 -584.6 0.2 0.07572 0.00009 41 26 22692 48 yes MC-ICP-MS U/Th #sd09 478.90 1261.27 0.04 3.3 0.00 -582.6 1.2 0.08259 0.00011 53 34 24901 63 yes MC-ICP-MS U/Th #si24 484.70 1302.56 0.32 7.1 0.02 -580.8 0.2 0.08458 0.00009 112 26 24854 115 no MC-ICP-MS U/Th #sc13 489.00 1214.24 0.19 13.7 0.01 -580.8 0.4 0.09091 0.00030 236 87 25873 252 yes MC-ICP-MS U/Th #hiatus6 492.9 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #sd10 547.80 1501.67 0.05 13.7 0.00 -572.6 1.2 0.10735 0.00014 192 42 31991 196 yes MC-ICP-MS U/Th #sc14 556.00 1108.11 0.17 10.1 0.01 -570.9 0.4 0.10818 0.00032 190 95 32140 213 yes MC-ICP-MS U/Th #-------------------- # Variables # # PaST_Thesaurus_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/PaST-thesaurus/SKOS/past-thesaurus-v1.0.rdf # PaST_Thesaurus_Download_Description: Paleoenvironmental Standard Terms (PaST) Thesaurus terms, definitions, and relationships in SKOS format. # # Data variables follow that are preceded by "##" in columns one and two. # Variables list, one per line, shortname-tab-var components: what, material, error, units, seasonality, data type, detail, method, C or N for Character or Numeric data) # ## depth_mm depth,,,millimeter,,speleothems,,,N, ## age_calBP age,,,calendar year before present,,speleothems,,,N,updated age model ## d18O delta 18O,calcium carbonate,,per mil VPDB,,speleothems,raw,isotope ratio mass spectrometry,N, ## notes notes,,,,,speleothems,,,C,* denotes value was used in Figure 3 for climate interpretation (growth rate > 10 mm/year) # #-------------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: depth_mm age_calBP d18O notes 0 0 -9.356 1 154 -9.254 2 308 -9.261 3 461 -9.315 4 615 -9.334 5 769 -9.212 6 923 -9.236 7 1076 -9.239 8 1230 -9.297 9 1384 -9.217 10 1538 -9.284 11 1691 -9.250 12 1845 -9.247 13 1999 -9.330 14 2153 -9.465 15 2306 -9.374 16 2460 -9.384 17 2614 -9.341 18 2768 -9.359 19 2921 -9.384 20 3075 -9.294 21 3229 -9.284 22 3383 -9.292 23 3537 -9.278 24 3690 -9.304 25 3844 -9.282 26 3998 -9.321 27 4152 -9.277 28 4305 -9.072 28.5 29 6163 -9.138 * 30 6202 -9.096 * 31 6242 -9.035 * 32 6282 -8.902 * 33 6322 -9.197 * 34 6361 -9.223 * 35 6401 -9.243 * 36 6441 -9.047 * 37 6480 -9.025 * 38 6520 -8.882 * 39 6560 -8.880 * 40 6600 -8.885 * 41 6639 -9.061 * 42 6679 -8.971 * 43 6719 -8.941 * 44 6759 -8.902 * 45 6798 -9.027 * 46 6838 -9.017 * 47 6878 -9.129 * 48 6918 -8.924 * 49 6957 -9.104 * 50 6997 -8.932 * 51 7037 -9.117 * 52 7077 -9.084 * 53 7116 -9.323 * 54 7156 -9.126 * 55 7196 -8.909 * 56 7235 -8.867 * 57 7275 -8.821 * 58 7315 -8.742 * 59 7355 -8.949 * 60 7394 -8.932 * 61 7434 -8.981 * 62 7474 -8.826 * 63 7514 -8.842 * 64 7553 -8.858 * 65 7593 -8.732 * 66 7633 -8.899 * 67 7673 -8.763 * 68 7712 -8.833 * 69 7752 -8.809 * 70 7792 -8.802 * 71 7832 -8.726 * 72 7871 -8.748 * 73 7911 -8.904 * 74 7951 -8.684 * 75 7990 -8.496 * 76 8030 -8.679 * 77 8070 -8.678 * 78 8110 -8.677 * 79 8149 -8.540 * 80 8189 -8.501 * 81 8229 -8.489 * 82 8269 -8.722 * 83 8308 -8.787 * 84 8347 -8.756 * 85 8385 -8.747 * 86 8423 -8.584 * 87 8461 -8.549 * 88 8500 -8.693 * 89 8538 -8.808 * 90 8576 -8.656 * 91 8614 -8.834 * 92 8653 -8.771 * 93 8691 -8.828 * 94 8729 -8.569 * 95 8767 -8.526 * 96 8806 -8.446 * 97 8844 -8.407 * 98 8882 -8.376 * 99 8920 -8.344 * 100 8958 -8.280 * 101 8997 -8.474 * 102 9035 -8.683 * 103 9073 -8.737 * 104 9103 -8.463 * 105 9132 -8.586 * 106 9161 -8.601 * 107 9189 -8.571 * 108 9218 -8.469 * 109 9247 -8.203 * 110 9276 -8.131 * 111 9305 -8.231 * 112 9333 -8.235 * 113 9362 -8.251 * 114 9391 -8.327 * 115 9420 -8.474 * 116 9449 -8.315 * 117 9478 -8.201 * 118 9506 -8.159 * 119 9535 -8.405 * 120 9564 -8.445 * 121 9593 -8.287 * 122 9622 -8.200 * 123 9650 -8.367 * 124 9679 -8.396 * 125 9708 -8.379 * 126 9737 -8.374 * 127 9766 -8.457 * 128 9795 -8.380 * 129 9823 -8.141 * 130 9852 -8.252 * 131 9881 -8.377 * 132 9910 -8.324 * 133 9939 -8.264 * 133.1 134 10553 -8.276 * 135 10568 -8.381 * 136 10584 -8.543 * 137 10600 -8.020 * 138 10615 -8.215 * 139 10631 -8.311 * 140 10646 -8.093 * 141 10662 -8.003 * 142 10677 -8.054 * 143 10693 -8.165 * 144 10708 -8.345 * 145 10724 -8.228 * 146 10739 -8.154 * 147 10755 -8.014 * 148 10770 -7.985 * 149 10786 -8.202 * 150 10801 -8.097 * 151 10817 -8.181 * 152 10832 -8.289 * 153 10848 -8.192 * 154 10864 -8.170 * 155 10879 -8.133 * 156 10895 -8.130 * 157 10897 -7.875 * 158 10900 -8.042 * 159 10902 -8.035 * 160 10905 -8.079 * 161 10907 -8.236 * 162 10910 -8.236 * 163 10912 -8.158 * 164 10915 -7.842 * 165 10917 -7.979 * 166 10920 -7.983 * 167 10922 -7.787 * 168 10925 -7.707 * 169 10927 -7.685 * 170 10933 -7.668 * 171 10940 -7.718 * 172 10946 -7.427 * 173 10952 -7.639 * 174 10959 -7.576 * 175 10965 -7.426 * 176 10972 -7.350 * 177 10978 -7.508 * 178 10985 -7.302 * 179 10992 -7.264 * 180 11001 -7.461 * 181 11011 -7.254 * 182 11020 -7.225 * 183 11030 -7.465 * 184 11039 -7.450 * 185 11049 -7.457 * 186 11058 -7.425 * 187 11068 -7.421 * 188 11077 -7.503 * 189 11087 -7.424 * 190 11096 -7.242 * 191 11106 -7.240 * 192 11115 -7.356 * 193 11125 -7.547 * 194 11134 -7.465 * 195 11144 -7.714 * 196 11153 -7.737 * 197 11163 -7.746 * 198 11172 -7.885 * 199 11206 -7.894 * 200 11244 -7.734 * 201 11282 -7.671 * 202 11320 -7.816 * 203 11358 -7.870 * 204 11396 -7.770 * 205 11434 -7.773 * 206 11471 -7.763 * 207 11509 -7.749 * 208 11547 -7.859 * 209 11585 -8.030 * 210 11623 -7.880 * 211 11661 -7.605 * 212 11699 -7.450 * 213 11737 -7.497 * 214 11775 -7.532 * 215 11813 -7.603 * 216 11851 -7.519 * 216.8 217 12735 -7.502 * 218 12754 -7.540 * 219 12774 -7.517 * 220 12793 -7.580 * 221 12813 -7.471 * 222 12833 -7.343 * 223 12852 -7.356 * 224 12872 -7.477 * 225 12891 -7.620 * 226 12911 -7.631 * 227 12930 -7.297 * 228 12950 -7.543 * 229 12970 -7.473 * 230 12989 -7.321 * 231 13009 -7.679 * 232 13028 -7.755 * 233 13048 -7.565 * 234 13067 -7.501 * 235 13087 -7.376 * 236 13107 -7.393 * 237 13126 -7.396 * 238 13146 -7.480 * 239 13165 -7.504 * 240 13185 -7.519 * 241 13204 -7.519 * 242 13224 -7.444 * 243 13243 -7.346 * 244 13263 -7.444 * 245 13283 -7.577 * 246 13302 -7.537 * 247 13322 -7.475 * 248 13341 -7.473 * 249 13361 -7.681 * 250 13380 -7.809 * 251 13400 -7.875 * 252 13420 -7.846 * 253 13439 -7.677 * 254 13459 -8.050 * 255 13478 -7.749 * 256 13498 -7.416 * 257 13517 -7.312 * 258 13537 -7.909 * 259 13557 -8.123 * 260 13576 -8.127 * 261 13596 -8.069 * 262 13615 -7.572 * 263 13635 -7.053 * 264 13654 -7.664 * 265 13674 -7.150 * 266 13694 -7.069 * 267 13713 -6.858 * 268 13733 -7.074 * 269 13752 -7.143 * 270 13772 -7.221 * 271 13791 -7.004 * 272 13811 -7.158 * 273 13830 -7.190 * 274 13850 -7.109 * 275 13870 -7.317 * 276 13889 -7.336 * 277 13909 278 13928 -7.266 * 279 13948 -7.221 * 280 13967 -7.173 * 281 13987 -7.418 * 282 14007 -7.470 * 283 14026 -7.610 * 284 14046 -6.974 * 285 14065 -6.968 * 286 14085 -7.081 * 287 14104 -7.097 * 288 14124 -7.128 * 289 14144 -7.560 * 290 14163 -6.987 * 291 14183 -6.939 * 292 14202 -6.971 * 293 14222 -6.973 * 294 14241 -6.886 * 295 14261 -6.899 * 296 14280 -6.954 * 297 14300 -6.944 * 298 14320 -7.006 * 299 14339 -6.999 * 300 14359 -6.922 * 300.5 301 14960 -6.726 * 302 14990 -6.748 * 303 15020 -6.651 * 304 15050 -6.685 * 305 15080 -6.700 * 306 15110 -6.521 * 307 15140 -6.471 * 308 15170 -6.474 * 309 15201 -6.380 * 310 15231 -6.362 * 311 15261 -6.372 * 312 15291 -6.236 * 313 15321 -6.373 * 314 15351 -6.489 * 315 15381 -6.526 * 316 15411 -6.254 * 317 15441 -6.389 * 318 15471 -6.448 * 319 15501 -6.469 * 320 15531 -6.398 * 321 15561 -6.312 * 322 15592 -6.510 * 323 15622 -6.385 * 324 15652 -6.186 * 325 15682 -6.320 * 326 15712 -6.212 * 327 15742 -6.195 * 328 15772 -6.083 * 329 15802 -6.346 * 330 15832 -6.428 * 331 15862 -6.505 * 332 15892 -6.540 * 333 15922 -6.574 * 334 15982 -6.457 * 335 16072 -6.423 * 336 16161 -6.432 * 337 16251 -6.704 * 338 16340 -6.758 * 339 16430 -6.742 * 340 16519 -6.681 * 341 16609 -6.654 * 342 16698 -6.726 * 343 16788 -6.745 * 344 16877 -6.698 * 345 16967 -6.644 * 346 17056 -6.760 * 347 17146 -6.811 * 348 17235 -6.810 * 349 17325 -6.958 * 350 17414 -6.786 * 351 17492 -6.865 * 352 17541 -6.960 * 353 17590 -6.864 * 354 17639 -6.881 * 355 17688 -6.942 * 356 17737 -6.994 * 357 17786 -7.148 * 358 17836 -7.170 * 359 17885 -7.194 * 360 17934 -7.254 * 361 17983 -7.471 * 362 18032 -7.245 * 363 18081 -7.102 * 364 18130 -7.036 * 365 18179 -7.021 * 366 18228 -7.048 * 367 18277 -7.067 * 368 18327 -7.112 * 369 18376 -7.102 * 370 18425 -7.181 * 371 18474 -7.202 * 372 18523 -7.194 * 373 18572 -7.067 * 374 18621 -7.223 * 375 18670 -7.260 * 376 18719 -7.075 * 377 18768 -7.151 * 378 18818 -7.122 * 379 18867 -7.061 * 380 18916 -7.070 * 381 18965 -7.154 * 382 19014 -7.209 * 383 19063 -7.283 * 384 19112 -7.285 * 385 19161 -7.245 * 386 19210 -7.211 * 387 19259 -7.198 * 388 19309 -7.231 * 389 19358 -7.233 * 390 19407 -7.585 * 391 19456 -7.364 * 391.7 392 20114 -7.188 * 393 20147 -7.220 * 394 20181 -7.126 * 395 20214 -7.299 * 396 20247 -7.251 * 397 20280 -7.318 * 398 20313 -7.305 * 399 20347 -7.121 * 400 20380 -7.176 * 401 20413 -7.244 * 402 20446 -7.276 * 403 20479 -7.316 * 404 20513 -7.366 * 405 20546 -7.245 * 406 20579 -7.223 * 407 20612 -7.192 * 408 20645 -7.205 * 409 20678 -7.416 * 410 20712 -7.246 * 411 20745 -7.201 * 412 20778 -7.181 * 413 20811 -7.537 * 414 20844 -7.182 * 415 20878 -7.120 * 416 20911 -7.244 * 417 20955 -7.554 * 418 21001 -7.278 * 419 21048 -7.241 * 420 21095 -7.278 * 421 21141 -7.137 * 422 21188 -6.986 * 423 21234 -7.011 * 424 21281 -7.089 * 425 21328 -7.181 * 426 21374 -7.182 * 427 21421 -7.149 * 428 21468 -7.201 * 429 21514 -7.040 * 430 21561 -7.199 * 431 21608 -7.208 * 432 21654 -7.101 * 433 21701 -7.082 * 434 21747 -7.100 * 435 21794 -7.171 * 436 21841 -7.180 * 437 21887 -7.195 * 438 21934 -7.235 * 439 21981 -7.170 * 440 22027 -7.087 * 441 22074 -7.147 * 442 22120 -7.151 * 443 22167 -7.191 * 444 22214 -7.273 * 445 22267 -7.233 * 446 22319 -7.112 * 447 22371 -7.154 * 448 22423 -7.167 * 449 22475 -7.166 * 450 22527 -7.221 * 451 22579 -7.204 * 452 22632 -7.212 * 453 22684 -7.482 * 454 22764 -7.120 * 455 22850 -7.219 * 456 22936 -7.180 * 457 23022 -7.221 * 458 23108 -7.433 * 459 23194 -7.326 * 460 23279 -7.201 * 461 23365 -7.140 * 462 23451 -7.210 * 463 23537 -7.254 * 464 23623 -7.176 * 465 23708 -7.161 * 466 23794 -7.100 * 467 23880 -6.983 * 468 23966 -7.010 * 469 24052 -7.069 * 470 24137 -7.019 * 471 24223 -6.947 * 472 24309 -6.930 * 473 24395 -7.108 * 474 24481 -7.147 * 475 24567 -6.977 * 476 24652 -6.827 * 477 24738 -6.912 * 478 24824 -7.529 * 479 24911 -6.992 * 480 25007 -6.763 * 481 25103 -6.694 * 482 25200 -6.681 * 483 25296 -6.856 * 484 25392 -7.045 * 485 25488 -7.039 * 486 25584 -7.040 * 487 25681 -7.051 * 488 25777 -7.150 * 489 25873 -7.356 * 490 25969 -7.362 * 491 26066 -7.446 * 492 26162 -7.506 *