# Comparison of published versus recalibrated age models for Lake Keilambete, Victoria #----------------------------------------------------------------------- # 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/21731 # Description: NOAA Landing Page # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/pages2k/dixon2017australasia/dixon2017keilambete-ost.txt # Description: NOAA location of the template # # # Archive: Sediment, Ostracods # # Parameter_Keywords: #--------------------------------------- # Contribution_Date # Date: 2017-12-11 #--------------------------------------- # File_Last_Modified_Date # Date: 2017-12-11 #--------------------------------------- # Title # Study_Name: Comparison of published versus recalibrated age models for Lake Keilambete, Victoria #--------------------------------------- # Investigators # Investigators: Dixon, Bronwyn C.; Tyler, Jonathan J.; Lorrey, Andrew M; Goodwin, Ian D; Gergis, Joelle; Drysdale, Russell N #--------------------------------------- # Description_Notes_and_Keywords # Description: # Provided Keywords: age modelling, Bayesian #--------------------------------------- # Publication # Authors: Dixon, Bronwyn C.; Tyler, Jonathan J.; Lorrey, Andrew M; Goodwin, Ian D; Gergis, Joelle; Drysdale, Russell N # Published_Date_or_Year: 2017 # Published_Title: Low-resolution Australasian palaeoclimate records of the last 2000 years # Journal_Name: Climate of the Past # Volume: # Edition: # Issue: # Pages: # Report Number: # DOI: # Online_Resource: # Full_Citation: # Abstract: Non-annually resolved palaeoclimate records in the Australasian region were compiled to facilitate investigations of decadal to centennial climate variability over the past 2000 years. A total of 661 lake/wetland, geomorphic, marine, and speleothem records were identified and then assessed against a set of a priori criteria based on temporal resolution, record length, dating methods, and confidence of the proxy-climate relationship over the Common Era. A high quality subset of 22 records across Australasia met the criteria and they are endorsed for subsequent analyses. New chronologies based on progressive Bayesian techniques were constructed for the high quality records to ensure a consistent approach to age modelling and quantification of age uncertainties. Chronological uncertainty was the primary reason why records did not meet the selection criteria. Despite present limitations, existing proxies and reconstruction techniques that successfully capture climate variability in the region show potential to address spatial gaps and expand the range of climate variables covering the last 2000 years from the Australasian region. #--------------------------------------- # Publication # Authors: Wilkins, D; Gouramais, C; De Deckker, P; Fifield, LK; Olley, J # Published_Date_or_Year: 2013 # Published_Title: Holocene lake-level fluctuations in Lakes Keilambete and Gnotuk, souwestern Victoria, Australia # Journal_Name: Holocene # Volume: 23 # Edition: # Issue: 6 # Pages: 784-795 # Report Number: # DOI: 10.1177/0959683612471983 # Online_Resource: # Full_Citation: Wilkins, D., Gouramanis, C., De Deckker, P., Fifield, L. K. & Olley, J. 2013. Holocene lake-level fluctuations in Lakes Keilambete and Gnotuk, southwestern Victoria, Australia. Holocene, 23, 784-795. # Abstract: Reconstructed Holocene lake-level curves from two saline, hydrologically closed maar crater lakes in southwestern Victoria, Australia, show near synchronous lake-level changes throughout the Holocene. We show that lake levels, reconstructed from sediment particle size and ostracod valve chemistry (delta O-18 and Sr/Ca) have undergone rapid (<100 yr), large (>10 m) fluctuations throughout the Holocene. Finer sampling resolution shows a more sensitive response to Holocene climate than was previously presented for Lake Keilambete. Both maar crater lakes show a short-lived maximum in Holocene lake levels around 7.2 ka. The period of lake filling leading to peak lake levels matches the phase of most effective precipitation (7.4-7.0 ka) reconstructed from a high-resolution speleothem record from northern Tasmania. Water levels declined in both lakes during the mid Holocene, with a more substantive decline after similar to 5 ka which coincides with the end of the Southern Hemisphere hypsithermal. Water levels continued to oscillate with a periodicity of around 300-700 years, before reaching a late-Holocene nadir around 1.8 ka (Keilambete) and 1.3 ka (Gnotuk). The trend and periodicity of oscillations in the maar water levels show commonalities to delta D in the Dome C ice core, and suggest that temperature may be a significant component in influencing the Precipitation/Evaporation (P/E) ratio in southeastern Australia during the Holocene. #--------------------------------------- # Publication # Authors: Quaternary Geochronology # Published_Date_or_Year: # Published_Title: 2012 # Journal_Name: 9 # Volume: # Edition: 3-15 # Issue: # Pages: 10.1016/j.quageo.2012.01.008 # Report Number: # DOI: Sediment core chronologies of optical dates on single-grains/very small aliquots of sand-sized quartz are compared with Accelerator Mass Spectrometry (AMS) radiocarbon (C-14) chronologies from ostracod carbonate, mixed carbonates, sedimentary organic matter and charcoal in order to establish the age of laminated Holocene sediments in maar crater lakes Keilambete and Gnotuk, Victoria, Australia. Samples for optical and AMS C-14 dating were taken from the same Mackereth cores, allowing a direct comparison of the two techniques from two laminated sedimentary sequences. Additional AMS C-14 samples were taken from water in lake Keilambete and from groundwater discharging into Lake Keilambete from the crater wall, with equivalent reservoir ages of 150 +/- 30 and 1940 +/- 30 years respectively. AMS C-14 dating of modern ostracod carbonate in Lake Keilambete demonstrates a reservoir age of 670 +/- 175 years. Optical dating of 'single-grain/very small aliquots' of sand-sized-quartz indicate the presence of a radiocarbon reservoir in Lake Keilambete that is consistent with that measured on modern ostracods, and also demonstrate that there is no C-14 reservoir in Lake Gnotuk during the Holocene. The chronology presented here supports the premise that previously published bulk conventional C-14 dates from Lake Keilambete were affected by old carbon, meaning that past chronologies require revision. Limitations on the use of optical dating of single-grain/very small aliquots include the relative paucity of sand-sized quartz, which decreases the precision of the sample equivalent dose (D-e), and is further confounded by low environmental dose rates and resultant large uncertainties on the final age assessment. Nevertheless, evidence for partial bleaching confirms that single-grain quartz dating is the most appropriate luminescence technique, and may prove a useful alternative in situations where C-14 dating is unsuitable or an alternative chronometer is required. # Online_Resource: Wilkins, D., De Deckker, P., Fifield, L. K., Gouramanis, C. & Olley, J. 2012. Comparative optical and radiocarbon dating of laminated Holocene sediments in two maar lakes: Lake Keilambete and Lake Gnotuk, south-western Victoria, Australia. Quaternary Geochronology, 9, 3-15. # Full_Citation: # Abstract: #--------------------------------------- # Funding_Agency # Funding_Agency_Name: # Grant: #--------------------------------------- # Site Information # Site_Name: Lake Keilambete # Location: # Country: # Northernmost_Latitude: -38.207 # Southernmost_Latitude: -38.207 # Easternmost_Longitude: 142.878 # Westernmost_Longitude: 142.878 # Elevation: 120 #--------------------------------------- # Data_Collection # Collection_Name: Keil01 # First_Year: 8660 # Last_Year: 50 # Time_Unit: cal yr BP # Core_Length: 334 # Notes: #--------------------------------------- # Chronology_Information # Chronology: # Calibrated ages were determined using SHCal04 # Lab ID ANUA-36023 ANUA-34203 ANUA-34204 ANUA-36024 ANUA-34205 ANUA-35105 ANUA-34206 ANUA-35106 ANUA-35107 ANUA-36013 ANUA-35108 ANUA-34208 ANUA-35109 ANUA-34207 # Dated material ostracod foraminifera ostracod ostracod ostracod ostracod ostracod gyttja gyttja gyttja charcoal ostracod foraminifera ostracod # depth_bot (mm) NaN 170 523 780 1010 1290 1450 1640 2080 2580 2950 3370 3630 3880 # depth_top (mm) modern 160 518 770 990 1280 1430 1630 2070 2570 2940 3360 3620 3860 # age (bp) NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN # age14C (bp) NaN 750 1755 1815 2940 3730 4000 4200 5470 5300 6460 7310 8720 9370 # age_error (years) NaN 170 170 175 190 175 170 180 180 270 210 185 185 175 # calibrated age (cal BP) NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN # 2-sigma error of cal age (years) NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN # cal_age_range_old (bp) NaN 160 1100 1185 2380 3380 3725 3975 5705 5490 7510 7625 9100 9920 # cal_age_range_young (2_s) NaN -4 765 895 1945 2960 3325 3550 5280 4890 7150 7300 8600 9470 # depth (mm) NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN # thickness (mm) NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN # notes modern sample 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir 1s age range includes 670±175 yr reservoir # #--------------------------------------- # 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_top_cm ,Top Depth of Sample,NA,,cm,,NA,,NA,N ## Depth_bottom_cm ,Bottom Depth of Sample,NA,,cm,,NA,,NA,N ## Depth_midpoint_cm ,Midpoint Depth of Sample,NA,,cm,,NA,,NA,N ## Depth_cm ,Depth of Sample,NA,,cm,,NA,,NA,N ## Equivalent Depth ,Equivalent depths between cores extracted from the same lake,NA,,cm,,NA,,laminae sequences used to correlate depths between cores,N ## PublishedAge_YBP ,Ages from original record publication,NA,,years before present (present=1950CE),,NA,Best rounded to whole year, based on accuracy of age model,NA,N ## BACON0.05CI ,5% confidence interval age as calculated in BACON age modelling software,NA,,years before present (present=1950CE),,NA,,,N ## BACON0.95CI ,95% confidence interval age as calculated in BACON age modelling software,NA,,years before present (present=1950CE),,NA,,,N ## BACONmedian ,median sample age as calculated in BACON age modelling software,NA,,years before present (present=1950CE),,NA,,,N ## BACONwmean ,weighted mean age as calculated in BACON age modelling software,NA,,years before present (present=1950CE),,NA,,,N ## Gap adjusted midpoint_cm ,Midpoint Depth ajusted for distruption in core,NA,,cm,,NA,accounts for 14cm expansion gap in core Gn01 from 81.5 to 95.5cm,NA,N ## Depth Below Surface_cm ,Depth of sample below surface-water interface,NA,,cm,,NA,,NA,N ## Density (g/cm3) ,Density,Sediment,,g/cm3,,Sediment,,gamma-ray attenuation; multi-sensor core logger,N ## Magnetic Susceptibility (cgs) ,Magnetic Susceptibility,Sediment,,electromagnetic cgs units,,Sediment,,multi-sensor core logger,N ## Modeled lake depth_m ,modeled lake depth,NA,,metres,,NA,,determined through changes in sediment size,N ## Lake depth relative to modern (smoothed) ,lake depth relative to modern lake levels,NA,2 metre curve fitting error,meters,,NA,three point running mean,,N ## Sediment dry weight_g ,weight of dry sediment,Sediment,,grams,,Sediment,,,N ## Sediment >63 um (%) ,percentage of sediment with grain size greater than 63µm,Subset of Sediment,,%,,Sediment,,,N ## % Carbonate (whole sample) ,percentage of whole sample that is composed of carbonate,Sediment,,%,,Sediment,,,N ## % Carbonate (>63 um fraction) ,percentage of >63µm size fraction that is comprised of carbonate,Subset of Sediment,,%,,Sediment,,,N ## % Carbonate ( <63 um fraction) ,percentage of <63µm size fraction that is comprised of carbonate,Subset of Sediment,,%,,Sediment,,,N ## Laminae ,number of laminae within a one centimeter interval,Sediment,,NA,,Sediment,,,N ## Water content (% dry weight) ,water content of sample,Sediment,,%,,Sediment,,,N ## LOI (% dry weight) ,Loss on Ignition of sample,Sediment,,%,,Sediment,,,N #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: NA Keilambete Depth_top_cm Depth_bottom_cm Depth_midpoint_cm PublishedAge_YBP BACON0.05CI BACON0.95CI BACONmedian BACONwmean Australocypris robusta Diacypris compacta Diacypris dietzi Reticypris clava Reticypris herbstii Platycypris baueri Mytilocypris praenuncia log10(TDS) SE Australocypris robusta (valve Sr/Ca) Diacypris compacta (valve Sr/Ca) Mytilocypris praenuncia (valve Sr/Ca) Reticypris sp. (valve Sr/Ca) Australocypris robusta (water Sr/Ca) Diacypris compacta (water Sr/Ca) Mytilocypris praenuncia (water Sr/Ca) Reticypris sp. (water Sr/Ca) Depth Age (ka) BACON0.05CI BACON0.95CI BACONmedian BACONwmean d18O A. robusta (valve d18O) D. compacta (valve d18O) M. praenuncia (valve d18O) A. beccarii (valve d18O) Live collected at time of coring -51 1 0 0 0 0 0 0 NA NA 0.010180738 0.061182323 0 0 -54 -35.1 -50.1 -48.4 1 0 0.5 -54 -51.6 1.1 -36.2 -33 1 1 0 0 0 1 0 4.87419 0.0812213 0.018822029 0.0856715 0.5 0.134338 -51.6 1.1 -36.2 -33 2.44 2.44 2 1 1.5 -29 -42.7 65.6 -7.1 -1.7 0 1 0 0 0 0 0 4.84834 0.0925747 1.5 0.158612 -42.7 65.6 -7.1 -1.7 4 2 3 8 -22.3 134.9 39.5 44.7 0 0 0 1 0 0 0 4.6231 0.16675 3 0.195023 -22.3 134.9 39.5 44.7 3.68 3.68 5 4 4.5 45 6.9 187.9 83.6 88.2 0 0 0 0 0 0 1 4.3397 0.11358 4.5 0.231434 6.9 187.9 83.6 88.2 6 5 5.5 70 24.9 217.3 107.9 112.2 0 0 0 1 0 1 1 4.10094 0.14377 5.5 0.255708 24.9 217.3 107.9 112.2 3.22 3.22 8 7 7.5 119 59.9 273.3 155.1 159.2 0 1 0 0 0 1 1 4.57923 0.205761 7.5 0.304256 59.9 273.3 155.1 159.2 4.06 4.06 10 9 9.5 169 96.6 328.1 201.3 205.5 0 0 0 0 0 1 1 3.98036 0.178404 9.5 0.352804 96.6 328.1 201.3 205.5 4.28 4.28 12 11 11.5 218 133 377.1 246.7 250.6 0 0 0 0 0 1 1 3.98042 0.178427 11.5 0.401352 133 377.1 246.7 250.6 4.39 4.39 14 13 13.5 267 170.1 426.9 293.9 295.7 0 0 0 0 0 0 0 NA NA 13.5 0.4499 170.1 426.9 293.9 295.7 16 15 15.5 317 210.1 476.4 340.7 341.3 0 0 0 0 0 0 0 NA NA 15.5 0.498448 210.1 476.4 340.7 341.3 18 17 17.5 366 249.2 524.1 386.9 386.7 0 0 0 0 0 0 1 4.3397 0.113579 17.5 0.546996 249.2 524.1 386.9 386.7 19 18 18.5 391 268.3 550.4 410.4 410.7 0 0 0 0 0 0 0 NA NA 18.5 0.57127 268.3 550.4 410.4 410.7 20 19 19.5 416 289.2 577 434.1 434.5 0 0 0 0 0 0 0 NA NA 19.5 0.595544 289.2 577 434.1 434.5 22 21 21.5 465 329.1 630.6 479.9 481.4 0 0 0 0 0 1 0 4.7709 0.133782 21.5 0.644092 329.1 630.6 479.9 481.4 24 23 23.5 514 372.8 685.3 528.3 529.5 0 0 0 0 0 0 1 4.3397 0.113579 23.5 0.69264 372.8 685.3 528.3 529.5 26 25 25.5 564 416.8 737 576 577.5 0 0 0 0 0 0 0 NA NA 25.5 0.741188 416.8 737 576 577.5 50 49 49.5 1157 915.1 1312.4 1113.9 1114.7 0 0 0 0 0 0 0 NA NA 49.5 1.323764 915.1 1312.4 1113.9 1114.7 51.8 51 51.4 1204 955.5 1354.8 1156.2 1157.1 0 1 0 0 0 0 0 4.84834 0.0925756 0.004809577 0.021891568 51.4 1.3698846 955.5 1354.8 1156.2 1157.1 1.78 1.78 52.3 51.8 52.05 1220 970.5 1371.9 1170.3 1171.8 0 1 0 0 0 0 0 4.84834 0.0925756 0.004617348 0.021016604 52.05 1.3856627 970.5 1371.9 1170.3 1171.8 3.51 3.51 52.9 52.3 52.6 1233 982.4 1384 1182.8 1184.4 0 1 0 0 0 0 0 4.84834 0.0925756 0.002842443 0.012937839 52.6 1.3990134 982.4 1384 1182.8 1184.4 3.94 3.94 53.8 53.3 53.55 1257 1000.2 1408.7 1205.5 1206 0 1 0 0 0 0 0 4.84834 0.0925756 0.003893348 0.0177212 53.55 1.4220737 1000.2 1408.7 1205.5 1206 2.79 2.79 55.1 54.3 54.7 1285 1025.5 1437.2 1231.8 1232.3 0 1 0 0 0 0 0 4.84834 0.0925756 0.001758413 0.0080037 54.7 1.4499888 1025.5 1437.2 1231.8 1232.3 2.75 2.75 57 56 56.5 1330 1066 1481.1 1274 1274.6 0 1 0 0 0 0 0 4.84834 0.0925756 0.00391805 0.017833637 56.5 1.493682 1066 1481.1 1274 1274.6 2.52 2.52 59 58 58.5 1379 1107.7 1529.7 1320.6 1320.8 0 1 0 0 0 0 0 4.84834 0.0925756 0.00599259 0.027276241 58.5 1.54223 1107.7 1529.7 1320.6 1320.8 2.26 2.26 61 60 60.5 1428 1152 1581.2 1366.3 1366.8 1 1 0 0 0 0 0 4.78675 0.0625538 0.005162666 0.023498707 60.5 1.590778 1152 1581.2 1366.3 1366.8 2.58 2.58 63 62 62.5 1478 1194.9 1628.8 1411.7 1413.2 1 1 0 0 0 0 0 4.78675 0.0625538 0.006663383 0.030329464 62.5 1.639326 1194.9 1628.8 1411.7 1413.2 2.43 2.43 65 64 64.5 1527 1240.1 1677 1456.8 1458.8 1 1 0 0 0 0 0 4.78675 0.0625539 0.005892252 0.026819537 64.5 1.687874 1240.1 1677 1456.8 1458.8 2.16 2.16 67 66 66.5 1577 1284.7 1725.6 1503.4 1505.4 1 1 0 0 0 0 0 4.78675 0.0625539 0.008750052 0.039827271 66.5 1.736422 1284.7 1725.6 1503.4 1505.4 2.3 2.3 69 68 68.5 1626 1328.5 1773.4 1548.5 1551.2 0 1 0 0 0 0 0 4.84834 0.0925756 0.008107137 0.036900944 68.5 1.78497 1328.5 1773.4 1548.5 1551.2 2.17 2.17 71 70 70.5 1675 1372.4 1822.3 1594.6 1597.9 0 1 0 0 0 0 0 4.84834 0.0925756 0.00619848 0.028213381 70.5 1.833518 1372.4 1822.3 1594.6 1597.9 2.96 2.96 73 72 72.5 1725 1417.5 1873.9 1641.5 1645.3 0 1 0 0 0 0 0 4.84834 0.0925756 0.004222173 0.019217903 72.5 1.882066 1417.5 1873.9 1641.5 1645.3 2.65 2.65 75 74 74.5 1774 1464.1 1921.4 1689.3 1692.5 0 1 0 0 0 0 0 4.84834 0.0925756 0.00687014 0.031270549 74.5 1.930614 1464.1 1921.4 1689.3 1692.5 2.23 2.23 77 76 76.5 1824 1509.8 1966.8 1736.1 1738.1 0 1 0 0 0 0 0 4.84834 0.0925756 0.011297774 0.051423641 76.5 1.979162 1509.8 1966.8 1736.1 1738.1 1.97 1.97 79 78 78.5 1873 1551.6 2015.5 1783.5 1784.2 0 1 0 0 0 0 0 4.84834 0.0925756 0.014705431 0.066934144 78.5 2.02771 1551.6 2015.5 1783.5 1784.2 2.28 2.28 81 80 80.5 1922 1601.2 2064.5 1830.4 1833 0 1 0 0 0 0 1 4.33646 0.196183 0.013997572 0.063712205 80.5 2.076258 1601.2 2064.5 1830.4 1833 2.5 2.5 83 82 82.5 1972 1648.9 2116.1 1878.5 1882.2 0 1 0 0 0 0 1 4.33646 0.196183 0.008977681 0.040863365 82.5 2.124806 1648.9 2116.1 1878.5 1882.2 2.39 2.39 85 84 84.5 2021 1697 2169.3 1928 1931.9 0 1 0 0 0 0 1 4.33647 0.196183 0.008364408 0.038071951 84.5 2.173354 1697 2169.3 1928 1931.9 2.94 2.94 87 86 86.5 2071 1744.9 2223.4 1976.1 1981 0 1 0 0 0 0 1 4.33647 0.196183 0.012498554 0.056889185 86.5 2.221902 1744.9 2223.4 1976.1 1981 1.64 1.64 89 88 88.5 2120 1795.6 2273.4 2025.6 2030.3 0 1 0 0 0 0 1 4.33647 0.196183 0.010134129 0.046127123 88.5 2.27045 1795.6 2273.4 2025.6 2030.3 2.64 2.64 91 90 90.5 2169 1844.4 2325.1 2074.3 2079 0 1 0 0 0 0 1 4.33647 0.196183 0.009323484 0.04243734 90.5 2.318998 1844.4 2325.1 2074.3 2079 2.6 2.6 93 92 92.5 2219 1889.9 2374.9 2123.7 2128.1 0 1 0 0 0 0 1 4.33647 0.196182 0.012551092 0.057128323 92.5 2.367546 1889.9 2374.9 2123.7 2128.1 1.79 1.79 95 94 94.5 2268 1939.8 2424.4 2172 2176.9 0 1 0 0 0 0 1 4.33647 0.196182 0.013973592 0.063603057 94.5 2.416094 1939.8 2424.4 2172 2176.9 2.6 2.6 96 95 95.5 2293 1966 2450.4 2196.3 2201.3 0 1 0 0 0 0 0 4.84834 0.0925756 0.008624425 0.039255463 95.5 2.440368 1966 2450.4 2196.3 2201.3 97 96 96.5 2318 1990.8 2475.7 2221.8 2226.2 0 1 0 0 0 0 1 4.33648 0.196182 96.5 2.464642 1990.8 2475.7 2221.8 2226.2 2.48 2.48 99 98 98.5 2367 2040.3 2526.2 2267.6 2274 0 1 0 0 0 0 1 4.33648 0.196182 0.006769999 0.030814744 98.5 2.51319 2040.3 2526.2 2267.6 2274 2.69 2.69 100 99 99.5 2392 2064.9 2550.7 2291.4 2298 0 1 0 0 0 0 1 4.33648 0.196182 0.005255166 0.023919738 99.5 2.537464 2064.9 2550.7 2291.4 2298 3.02 3.02 101 100 100.5 2416 2089 2574.8 2315.9 2322.3 0 1 0 0 0 0 1 4.33648 0.196182 100.5 2.561738 2089 2574.8 2315.9 2322.3 3.87 3.87 103 102 102.5 2466 2138.3 2629.3 2364.8 2372.2 0 1 0 0 0 0 1 4.33648 0.196182 102.5 2.610286 2138.3 2629.3 2364.8 2372.2 3.73 3.73 105 104 104.5 2515 2187.7 2675.9 2415.9 2422.4 0 1 0 0 0 0 1 4.33648 0.196182 104.5 2.658834 2187.7 2675.9 2415.9 2422.4 3.81 3.81 107 106 106.5 2565 2234.1 2726.9 2465.9 2472.1 1 1 0 0 0 0 1 4.76004 0.056801 106.5 2.707382 2234.1 2726.9 2465.9 2472.1 4 4 109 108 108.5 2614 2283.3 2775 2515.7 2521.5 0 1 0 0 0 0 1 4.33648 0.196182 0.005179576 0.023575678 108.5 2.75593 2283.3 2775 2515.7 2521.5 3.16 3.16 111 110 110.5 2663 2331 2822.5 2565.4 2570.9 1 1 0 0 0 0 1 4.76004 0.056801 0.007963885 0.036248906 110.5 2.804478 2331 2822.5 2565.4 2570.9 3.13 3.13 113 112 112.5 2713 2379.2 2869.9 2614.9 2620.9 0 1 0 0 0 0 1 4.33648 0.196181 0.011132206 0.05067003 112.5 2.853026 2379.2 2869.9 2614.9 2620.9 115 114 114.5 2762 2431.1 2919.3 2664.4 2670.2 0 1 0 0 0 0 0 4.84834 0.0925756 0.008079237 0.03677395 114.5 2.901574 2431.1 2919.3 2664.4 2670.2 2.72 2.72 117 116 116.5 2812 2479.5 2968.2 2714.4 2719.4 1 1 0 0 0 0 1 4.76004 0.056801 0.009984396 0.045445588 116.5 2.950122 2479.5 2968.2 2714.4 2719.4 3.21 3.21 123 122 122.5 2960 2632.2 3113.2 2867.4 2870.3 0 1 0 0 0 0 0 4.84834 0.0925756 0.008956473 0.040766833 122.5 3.095766 2632.2 3113.2 2867.4 2870.3 3.82 3.82 125 124 124.5 3009 2683.4 3163.7 2917.5 2920.9 1 1 0 0 0 0 1 4.76004 0.056801 0.007013095 0.041596056 124.5 3.144314 2683.4 3163.7 2917.5 2920.9 4.68 4.68 127 126 126.5 3059 2734.5 3215.6 2968.5 2971.7 0 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