# 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-SSC01-noaa.txt # Data_Download_Description: NOAA Template File; Stalagmite SSC01 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: SSC01 # First_Year: 26430 # Last_Year: 0 # Time_Unit: cal yr BP # Core_Length_m: # Parameter_Keywords: # Notes: #-------------------- # 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 SSC01 UTh Dating and Stable Isotope Data, updated 2009 age model. Hiatuses Indentified, their depths and durations: 48.1 mm: 1860 +/- 669 years (2s); 220 mm: 1500 +/- 544 years (2s); 272.4 mm: 574 +/- 279 years (2s); 303 mm: 754 +/- 558 years (2s); 333.6 mm: 994 +/- 383 years (2s); 402.2 mm: 444 +/- 397 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 #sf21 8.90 102.7 0.0 0.3 0.1 -57.1 0.6 0.01045 0.00101 101 56 578 115 yes MC-ICP-MS U/Th #sf19 22.30 120.1 0.0 1.0 0.1 -69.0 0.5 0.02367 0.00089 270 42 1116 273 yes MC-ICP-MS U/Th #sg01 46.65 160.7 0.0 13.2 0.0 -81.8 0.6 0.13157 0.00055 3307 -9 -2073 -3307 no MC-ICP-MS U/Th #hiatus1 48.1 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #sf20 48.70 212.1 0.0 12.8 0.1 -81.5 0.5 0.13462 0.00054 2310 15 3691 2310 no MC-ICP-MS U/Th #si21 55.20 184.3 0.0 0.4 0.0 -86.3 0.5 0.03867 0.00018 80 19 4219 82 yes MC-ICP-MS U/Th #sf24 86.60 216.9 0.0 5.4 0.1 -83.6 0.5 0.07394 0.00051 873 26 3804 874 no MC-ICP-MS U/Th #sf25 86.60 257.2 0.1 1.3 0.1 -82.6 0.4 0.05349 0.00041 178 42 5443 183 no MC-ICP-MS U/Th #sf26 86.60 356.3 0.1 1.4 0.1 -85.2 1.3 0.05026 0.00033 136 35 5316 140 no MC-ICP-MS U/Th #sf27 86.60 352.8 0.1 1.2 0.1 -85.7 1.1 0.04790 0.00034 117 36 5142 122 yes MC-ICP-MS U/Th #sf18 110.80 269.0 0.1 1.4 0.1 -93.9 0.4 0.06056 0.00042 173 45 6472 178 yes MC-ICP-MS U/Th #sf11 143.90 322.5 0.1 4.1 0.0 -95.8 0.7 0.08440 0.00307 445 289 7935 530 no MC-ICP-MS U/Th #si27 150.60 324.5 0.1 1.0 0.0 -91.1 0.5 0.07335 0.00016 109 18 8514 110 yes MC-ICP-MS U/Th #sf12 159.60 336.0 0.1 2.7 0.0 -93.1 0.8 0.07889 0.00320 273 334 8235 432 no MC-ICP-MS U/Th #si14 175.05 262.6 0.1 0.7 0.0 -96.6 0.5 0.07922 0.00021 90 25 9468 93 yes MC-ICP-MS U/Th #sf13 189.80 258.6 0.1 2.4 0.0 -106.6 0.9 0.09122 0.00381 320 408 9771 519 no MC-ICP-MS U/Th #si07 197.45 234.5 0.1 3.4 0.0 -98.1 0.5 0.10189 0.00025 518 24 9885 518 no MC-ICP-MS U/Th #sg19 201.45 237.0 0.1 2.4 0.0 -103.4 0.5 0.09673 0.00036 351 38 10293 353 yes MC-ICP-MS U/Th #sg18 211.95 214.1 0.1 0.9 0.0 -105.1 0.5 0.09347 0.00041 149 49 11128 157 yes MC-ICP-MS U/Th #sg24 214.55 202.9 0.0 0.8 0.0 -103.7 0.5 0.09371 0.00040 131 48 11256 139 yes MC-ICP-MS U/Th #sg22 217.70 257.6 0.1 7.4 0.0 -105.5 0.5 0.13730 0.00035 1062 30 11735 1062 no MC-ICP-MS U/Th #hiatus2 220 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #sf16 220.60 202.3 0.0 0.5 0.1 -113.1 0.5 0.10337 0.00060 91 76 12988 119 no MC-ICP-MS U/Th #sf17 220.60 263.9 0.1 0.7 0.1 -112.0 0.4 0.10401 0.00049 96 61 13032 113 yes MC-ICP-MS U/Th #sf22 220.60 222.6 0.1 0.9 0.1 -112.5 0.5 0.10516 0.00066 149 81 12870 169 no MC-ICP-MS U/Th #sf23 220.60 293.6 0.1 2.8 0.1 -111.9 0.4 0.11278 0.00052 336 59 12761 341 no MC-ICP-MS U/Th #si20 220.60 319.0 0.1 10.8 0.0 -107.4 0.5 0.16351 0.00018 1261 16 14488 1261 no MC-ICP-MS U/Th #sf14 244.00 209.5 0.0 1.0 0.1 -94.5 0.5 0.11186 0.00053 171 63 13349 183 yes MC-ICP-MS U/Th #si25 254.40 257.9 0.1 0.7 0.0 -120.5 0.5 0.11029 0.00024 100 30 14042 105 yes MC-ICP-MS U/Th #sf15 267.00 259.0 0.1 0.3 0.1 -112.7 0.4 0.11312 0.00044 47 57 14637 74 yes MC-ICP-MS U/Th #hiatus3 272.4 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #si23 283.60 215.4 0.1 0.4 0.0 -115.2 0.5 0.12009 0.00023 69 30 15537 76 no MC-ICP-MS U/Th #si13 283.60 215.6 0.1 0.3 0.0 -116.1 0.5 0.11971 0.00030 49 40 15633 63 yes MC-ICP-MS U/Th #si09 283.60 266.7 0.1 0.8 0.0 -111.8 0.5 0.12158 0.00020 104 25 15468 107 no MC-ICP-MS U/Th #si17 283.60 219.2 0.1 0.5 0.0 -111.5 0.5 0.12030 0.00026 76 33 15454 83 no MC-ICP-MS U/Th #si28 300.60 233.7 0.1 0.8 0.0 -109.8 0.5 0.12554 0.00022 121 28 15884 125 yes MC-ICP-MS U/Th #hiatus4 303 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #sf10 306.90 261.0 2.5 0.8 0.0 -130.6 13.8 0.12209 0.00538 106 702 15916 709 no MC-ICP-MS U/Th #sg02 310.50 259.0 0.1 12.5 0.0 -147.7 0.8 0.12862 0.00047 1951 23 6269 1951 no MC-ICP-MS U/Th #si08 315.00 266.2 0.1 1.0 0.0 -146.8 0.5 0.12694 0.00025 134 34 16824 138 yes MC-ICP-MS U/Th #sf06 326.60 234.9 0.1 0.3 0.0 -133.5 1.3 0.13051 0.00632 48 852 17599 853 no MC-ICP-MS U/Th #sg03 329.20 216.4 0.1 1.6 0.0 -139.9 0.9 0.13539 0.00054 267 69 17112 275 yes MC-ICP-MS U/Th #hiatus5 333.6 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #si11 338.10 241.0 0.1 0.8 0.0 -143.7 0.5 0.13778 0.00023 116 31 18517 120 yes MC-ICP-MS U/Th #sf05 339.50 267.5 0.1 0.6 0.0 -152.1 1.4 0.13436 0.00648 82 888 18417 892 no MC-ICP-MS U/Th #sg04 347.20 223.2 0.1 0.4 0.0 -116.0 0.5 0.14470 0.00050 68 66 19167 95 yes MC-ICP-MS U/Th #sf01 356.40 170.6 0.1 0.5 0.0 -117.7 1.8 0.15131 0.01013 106 1336 19959 1340 no MC-ICP-MS U/Th #sf02 356.40 188.1 0.1 0.3 0.0 -118.4 1.5 0.15260 0.00788 65 1056 20435 1058 no MC-ICP-MS U/Th #sf03 356.40 267.2 0.1 0.5 0.0 -118.7 1.2 0.14823 0.00629 65 839 19781 842 no MC-ICP-MS U/Th #sf04 356.40 270.8 0.1 0.8 0.0 -118.5 1.3 0.15245 0.00670 105 886 20162 892 no MC-ICP-MS U/Th #sg05 376.45 241.2 0.1 0.7 0.0 -125.1 0.5 0.16010 0.00046 107 62 21499 124 yes MC-ICP-MS U/Th #sg06 394.30 227.2 0.1 0.8 0.0 -130.6 0.6 0.16864 0.00053 132 72 22845 150 yes MC-ICP-MS U/Th #hiatus6 402.2 NA NA NA NA NA NA NA NA NA NA NA NA yes hiatus #si04 403.20 214.2 0.1 1.0 0.0 -106.6 0.5 0.18194 0.00033 162 43 23957 168 yes MC-ICP-MS U/Th #sf07 408.10 249.3 0.1 0.5 0.0 -116.4 1.4 0.17411 0.00699 74 948 23611 951 no MC-ICP-MS U/Th #sg07 416.85 240.0 0.1 1.7 0.0 -123.1 0.4 0.17851 0.00049 258 64 23367 266 no MC-ICP-MS U/Th #sf08 431.25 196.9 0.1 0.9 0.0 -124.6 1.7 0.18927 0.00839 156 1142 25779 1153 no MC-ICP-MS U/Th #si10 434.80 184.5 0.0 1.1 0.0 -119.6 0.6 0.19545 0.00031 213 42 26229 217 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 -9.160 * 1 65 -9.286 * 2 130 -9.375 * 3 195 -9.537 * 4 260 -9.459 * 5 325 -9.483 * 6 390 -9.497 * 7 455 -9.283 * 8 520 -9.382 * 9 582 -9.516 * 10 622 -9.613 * 11 662 -9.512 * 12 703 -9.471 * 13 743 -9.509 * 14 783 -9.544 * 15 823 -9.642 * 16 863 -9.528 * 17 903 -9.326 * 18 943 -9.595 * 19 983 -9.441 * 20 1023 -9.366 * 21 1064 -9.594 * 22 1104 -9.791 * 23 1144 -9.774 * 24 1184 -9.492 * 25 1224 -9.415 * 26 1264 -9.596 * 27 1304 -9.505 * 28 1344 -9.504 * 29 1384 -9.645 * 30 1424 -9.550 * 31 1465 -9.450 * 32 1505 -9.577 * 33 1545 -9.535 * 34 1585 -9.537 * 35 1625 -9.510 * 36 1665 -9.396 * 37 1705 -9.673 * 38 1745 -9.249 * 39 1785 -9.480 * 40 1826 -9.933 * 41 1866 -9.678 * 42 1906 -9.505 * 43 1946 -9.883 * 44 1986 -9.534 * 45 2026 -9.396 * 46 2066 -9.480 * 47 2106 -9.439 * 48 2146 -9.871 * 48.1 49 4037 -10.170 * 50 4067 -10.126 * 51 4096 -10.146 * 52 4125 -10.049 * 53 4155 -9.969 * 54 4184 -9.860 * 55 4213 -9.900 * 56 4243 -9.791 * 57 4272 -9.934 * 58 4302 -9.984 * 59 4331 -10.190 * 60 4360 -9.765 * 61 4390 -9.967 * 62 4419 -10.035 * 63 4448 -10.094 * 64 4478 -9.820 * 65 4507 -9.906 * 66 4537 -9.845 * 67 4566 -10.000 * 68 4595 -10.061 * 69 4625 -10.086 * 70 4654 -10.069 * 71 4683 -9.992 * 72 4713 -10.009 * 73 4742 -9.960 * 74 4772 -9.941 * 75 4801 -10.066 * 76 4830 -9.946 * 77 4860 -10.038 * 78 4889 -9.876 * 79 4918 -9.921 * 80 4948 -10.060 * 81 4977 -10.117 * 82 5006 -10.210 * 83 5036 -10.058 * 84 5065 -9.963 * 85 5095 -9.786 * 86 5124 -9.988 * 87 5164 -9.693 * 88 5219 -9.770 * 89 5274 -9.719 * 90 5329 -9.814 * 91 5384 -9.705 * 92 5439 -9.724 * 93 5493 -9.759 * 94 5548 -9.888 * 95 5603 -9.649 * 96 5658 -9.737 * 97 5713 -9.775 * 98 5768 -9.820 * 99 5823 -9.787 * 100 5878 -9.654 * 101 5933 -9.716 * 102 5988 -9.641 * 103 6043 -9.656 * 104 6098 -9.601 * 105 6153 -9.409 * 106 6208 -9.356 * 107 6263 -9.731 * 108 6318 -9.951 * 109 6373 -9.644 * 110 6428 -9.403 * 111 6482 -9.626 * 112 6534 -9.843 * 113 6585 -9.837 * 114 6636 -9.383 * 115 6688 -9.498 * 116 6739 -9.390 * 117 6790 -9.342 * 118 6842 -9.246 * 119 6893 -9.183 * 120 6944 -9.270 * 121 6995 -9.390 * 122 7047 -9.485 * 123 7098 -9.167 * 124 7149 -9.081 * 125 7201 -9.123 * 126 7252 -9.072 * 127 7303 -9.192 * 128 7355 -9.529 * 129 7406 -9.557 * 130 7457 -9.524 * 131 7509 -9.233 * 132 7560 133 7611 134 7662 135.6 7745 -9.759 * 136.6 7796 -9.120 * 137.6 7847 -9.245 * 138.6 7898 -9.010 * 139.6 7950 -9.109 * 140.6 8001 -8.744 * 141.6 8052 -8.918 * 142.6 8104 -9.152 * 143.6 8155 -8.946 * 144.6 8206 -8.789 * 145.6 8258 -9.004 * 146.6 8309 -9.115 * 147.6 8360 -9.059 * 148.6 8412 -8.827 * 149.6 8463 -8.906 * 150.6 8514 -8.906 * 151.6 8553 -8.861 * 152.6 8592 -9.048 * 153.6 8631 -8.734 * 154.6 8670 -8.699 * 155.6 8709 -8.732 * 156.6 8748 -8.737 * 157.6 8787 -8.691 * 158.6 8826 -8.794 * 159.6 8865 -8.793 * 160.6 8904 -8.926 * 161.6 8943 -8.903 * 162.6 8982 -9.172 * 163.6 9022 -8.912 * 164.6 9061 -9.131 * 165.6 9100 -8.845 * 166.6 9139 -8.750 * 167.6 9178 -8.687 * 168.6 9217 -8.832 * 169.6 9256 -8.947 * 170.6 9295 -8.823 * 171.6 9334 -8.491 * 172.6 9373 -8.449 * 173.6 9412 -9.011 * 174.6 9451 -8.718 * 175.6 9486 -8.652 * 176.6 9517 -8.592 * 177.6 9548 -8.694 * 178.6 9579 -8.661 * 179.6 9611 -8.592 * 180.6 9642 -8.607 * 181.6 9673 -8.671 * 182.6 9704 -8.722 * 183.6 9735 -8.684 * 184.6 9767 -8.803 * 185.6 9798 -8.621 * 186.6 9829 -8.565 * 187.6 9860 -8.568 * 188.6 9892 -8.459 * 189.6 9923 -8.560 * 190.6 9954 -8.366 * 191.6 9985 -8.248 * 192.6 10017 -8.099 * 193.6 10048 -8.446 * 194.6 10079 -8.547 * 195.6 10110 -8.433 * 196.6 10141 -8.484 * 197.6 10173 -8.432 * 198.6 10204 -8.390 * 199.6 10235 -8.705 * 200.6 10266 -8.621 * 201.6 10305 -8.412 * 202.6 10384 -8.514 * 203.6 10464 -8.375 * 204.6 10544 -8.598 * 205.6 10623 -8.340 * 206.6 10703 -8.443 * 207.6 10782 -8.137 * 208.6 10862 -8.008 * 209.6 10941 -8.000 * 210.6 11021 -8.338 * 211.6 11100 -8.459 * 212.6 11180 -8.338 * 213.6 11260 -8.185 * 214.6 11339 -8.325 * 215.6 11419 -8.220 * 216.6 11498 -8.323 * 217.6 11578 -8.327 * 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