# Lake Keilambete, SE Australia Holocene Sediment Data and Lake Level #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. # If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/22430 # Description: NOAA Landing Page # Online_Resource: https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/australia/keilambete2013ost.txt # Description: NOAA location of the template # # Original_Source_URL: # Description: # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Paleolimnology # # Dataset DOI: # # Parameter_Keywords: lake level, population abundance, geochemistry, reconstruction, physical property, oxygen isotopes #-------------------- # Contribution_Date # Date: 2017-07-10 #-------------------- # File_Last_Modified_Date # Date: 2017-07-10 #-------------------- # Title # Study_Name: Lake Keilambete, SE Australia Holocene Sediment Data and Lake Level #-------------------- # Investigators # Investigators: Wilkins, D.; Gouramanis, C.; De Deckker, P.; Fifeld, L. K.; Olley, J. #--------------------------------------- # Description_Notes_and_Keywords # Description: Multiproxy Holocene sediment data and lake level reconstructions from Lake Keilambete, southwestern Victoria, Australia # Provided Keywords: delta O-18, maar lake, Modern Analogue Technique, ostracod, precipitation/evaporation, Sr/Ca, western Victoria, southeastern Australia, climate-change, southern Australia, maar lakes, variability, sediments, history, core #--------------------------------------- # Publication # Authors: Daniel Wilkins, Chris Gouramanis, Patrick De Deckker, L. Keith Fifield, Jon Olley # Published_Date_or_Year: 2013-02-06 # Published_Title: Holocene lake-level fluctuations in Lakes Keilambete and Gnotuk, southwestern Victoria, Australia # Journal_Name: Holocene # Volume: 23 # Edition: # Issue: 6 # Pages: 784-795 # Report Number: # DOI: 10.1177/0959683612471983 # Online_Resource: http://journals.sagepub.com/doi/10.1177/0959683612471983 # Full_Citation: # 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 (d18O 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 ~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 dD 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: Daniel Wilkins, Patrick De Deckker, L. Keith Fifield, Chris Gouramanis, Jon Olley # Published_Date_or_Year: 2012-06-01 # Published_Title: Comparative optical and radiocarbon dating of laminated Holocene sediments in two maar lakes: Lake Keilambete and Lake Gnotuk, south-western Victoria, Australia # Journal_Name: Quaternary Geochronology # Volume: 9 # Edition: # Issue: # Pages: 3-15 # Report Number: # DOI: 10.1016/j.quageo.2012.01.008 # Online_Resource: http://www.sciencedirect.com/science/article/pii/S1871101412000106 # Full_Citation: # Abstract: Sediment core chronologies of optical dates on single-grains/very small aliquots of sand-sized quartz are compared with Accelerator Mass Spectrometry (AMS) radiocarbon (14C) 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 14C dating were taken from the same Mackereth cores, allowing a direct comparison of the two techniques from two laminated sedimentary sequences. Additional AMS 14C 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 14C 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 14C reservoir in Lake Gnotuk during the Holocene. The chronology presented here supports the premise that previously published bulk conventional 14C 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 (De), 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 14C dating is unsuitable or an alternative chronometer is required. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Australian Research Council # Grant: DP034493 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Commonwealth Scientific and Industrial Research Organisation (CSIRO) # Grant: Land and Water scholarship #--------------------------------------- # Site Information # Site_Name: Lake Keilambete # Location: Australia/New Zealand>Australia # Country: Australia # Northernmost_Latitude: -38.207 # Southernmost_Latitude: -38.207 # Easternmost_Longitude: 142.878 # Westernmost_Longitude: 142.878 # Elevation: 120 m #--------------------------------------- # Data_Collection # Collection_Name: Keil02ost # First_Year: 9480 # Last_Year: -53 # Time_Unit: cal. yr BP # Core_Length: 389cm # Notes: Ostracod census and Sr/Ca data from Lake Keilambete core Keil02 #--------------------------------------- # Chronology_Information # Chronology: # # 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 (cm) 17 52.3 78 101 129 145 164 208 258 295 337 363 388 # depth_top (cm) modern 16 51.8 77 99 128 143 163 207 257 294 336 362 386 # age (bp) # age14C (bp) 750 1755 1815 2940 3730 4000 4200 5470 5300 6460 7310 8720 9370 # age_error (years) 170 170 175 190 175 170 180 180 270 210 185 185 175 # calibrated age (cal BP) # 2-sigma error of cal age (years) # cal_age_range_old (bp) 160 1100 1185 2380 3380 3725 3975 5705 5490 7510 7625 9100 9920 # cal_age_range_young (2_s) -4 765 895 1945 2960 3325 3550 5280 4890 7150 7300 8600 9470 # 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 # # OSL Dates # Core depth_top_cm depth_bot_cm Age (YBP) small error*a large error*b # KEIL02 2 4 240 0.06 0.07 # KEIL02 6 8 370 0.17 0.24 # KEIL02 24 26 800 0.14 0.19 # KEIL02 73 75 1880 0.37 0.38 # KEIL02 119 121 2610 0.31 0.33 # KEIL02 142 144 3380 0.43 0.52 # KEIL02 166 168 4190 0.46 0.51 # KEIL02 192 194 5320 0.5 0.58 # KEIL02 211 213 5480 0.51 0.59 # KEIL02 230 232 6280 0.57 0.66 # KEIL02 249 251 6290 0.56 0.66 # KEIL02 291 293 7850 0.75 0.94 # KEIL02 336 338 7750 0.63 0.75 # KEIL02 386 388 9690 1.56 2.12 # # *a small error incorporates random uncertainty and 2.5% uncertainty associated with equivalent dose measurement # *b large error incorporates all systematic and random uncertainties # #--------------------------------------- # 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 depth, , , cm, , , Top Depth of Sample, ,N, ## depth_bot_cm depth, , , cm, , , Bottom Depth of Sample, ,N, ## depth_cm depth, , , cm, , , Midpoint Depth of Sample, ,N, ## age_calBP age, , , calendar years before present, , , Best rounded to whole year, based on accuracy of age model,N, ## A.rob Australocypris robusta Ostracod tests,microfossil,,count,,paleolimnology,,,N, ## D.comp Diacypris compacta Ostracod tests,microfossil,,count,,paleolimnology,,,N, ## D.diet Diacypris dietzi Ostracod tests,microfossil,,count,,paleolimnology,,,N, ## R.clav Reticypris clava Ostracod tests,microfossil,,count,,paleolimnology,,,N, ## R.herb Reticypris herbstii Ostracod tests,microfossil,,count,,paleolimnology,,,N, ## P.bau Platycypris baueri Ostracod tests,microfossil,,count,,paleolimnology,,,N, ## M.pra Mytilocypris praenuncia Ostracod tests,microfossil,,count,,paleolimnology,,,N, ## log10(TDS) salinity,NA,Root Mean Square Error of MAT=0.3 R2=0.85,mg/L,,paleolimnology,,Modern Analogue Technique based on 491 modern salinity measurements,N, ## salSE Salinity Standard Error,NA,,mg/L,,,,Modern Analogue Technique based on 491 modern salinity measurements,N, ## Sr/CaA.rob Sr/Ca ratio in Australocypris robusta ostracod valve,Calcite,,mmol/mol,,paleolimnology,,Inductively Coupled Plasma Mass Spectrometry,N, ## Sr/CaD.comp Sr/Ca ratio in Diacypris compacta ostracod valve,Calcite,,mmol/mol,,paleolimnology,,Inductively Coupled Plasma Mass Spectrometry,N, ## Sr/CaM.pra Sr/Ca ratio in Mytilocypris praenuncia ostracod valve,Calcite,,mmol/mol,,paleolimnology,,Inductively Coupled Plasma Mass Spectrometry,N, ## Sr/CaR.sp. Sr/Ca ratio in Reticypris sp. ostracod valve,Calcite,,mmol/mol,,paleolimnology,,Inductively Coupled Plasma Mass Spectrometry,N, ## Sr/CaWA.rob Calculated Sr/Ca ratio of water from measured Sr/Ca of Australocypris robusta ostracod test,NA,,mmol/mol,,paleolimnology,,reconstructed using partition coefficients of Gouramanis and De Deckker (2010),N, ## Sr/CaWD.comp Calculated Sr/Ca ratio of water from measured Sr/Ca of Diacypris compacta ostracod test,NA,,mmol/mol,,paleolimnology,,reconstructed using partition coefficients of Gouramanis and De Deckker (2010),N, ## Sr/CaWM.pra Calculated Sr/Ca ratio of water from measured Sr/Ca of Mytilocypris praenuncia ostracod test,NA,,mmol/mol,,paleolimnology,,reconstructed using partition coefficients of Gouramanis and De Deckker (2010),N, ## Sr/CaWR.sp. Calculated Sr/Ca ratio of water from measured Sr/Ca of Reticypris sp. ostracod test,NA,,mmol/mol,,paleolimnology,,reconstructed using partition coefficients of Gouramanis and De Deckker (2010),N, # #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: NA # 0 depth samples live collected at time of coring depth_top_cm depth_bot_cm depth_cm age_calBP A.rob D.comp D.diet R.clav R.herb P.bau M.pra log10(TDS) salSE Sr/CaA.rob Sr/CaD.comp Sr/CaM.pra Sr/CaR.sp. Sr/CaWA.rob Sr/CaWD.comp Sr/CaWM.pra Sr/CaWR.sp. 0 0 0 -51 1 0 0 0 0 0 0 NA NA 0.01018 0.06118 1 0 0.5 -54 1 1 0 0 0 1 0 4.8742 0.0812 0.01882 0.08567 2 1 1.5 -29 0 1 0 0 0 0 0 4.8483 0.0926 4 2 3 8 0 0 0 1 0 0 0 4.6231 0.1668 5 4 4.5 45 0 0 0 0 0 0 1 4.3397 0.1136 6 5 5.5 70 0 0 0 1 0 1 1 4.1009 0.1438 8 7 7.5 119 0 1 0 0 0 1 1 4.5792 0.2058 10 9 9.5 169 0 0 0 0 0 1 1 3.9804 0.1784 12 11 11.5 218 0 0 0 0 0 1 1 3.9804 0.1784 14 13 13.5 267 0 0 0 0 0 0 0 NA NA 16 15 15.5 317 0 0 0 0 0 0 0 NA NA 18 17 17.5 366 0 0 0 0 0 0 1 4.3397 0.1136 19 18 18.5 391 0 0 0 0 0 0 0 NA NA 20 19 19.5 416 0 0 0 0 0 0 0 NA NA 22 21 21.5 465 0 0 0 0 0 1 0 4.7709 0.1338 24 23 23.5 514 0 0 0 0 0 0 1 4.3397 0.1136 26 25 25.5 564 0 0 0 0 0 0 0 NA NA 50 49 49.5 1157 0 0 0 0 0 0 0 NA NA 51.8 51 51.4 1204 0 1 0 0 0 0 0 4.8483 0.0926 0.00481 0.02189 52.3 51.8 52.05 1220 0 1 0 0 0 0 0 4.8483 0.0926 0.00462 0.02102 52.9 52.3 52.6 1233 0 1 0 0 0 0 0 4.8483 0.0926 0.00284 0.01294 53.8 53.3 53.55 1257 0 1 0 0 0 0 0 4.8483 0.0926 0.00389 0.01772 55.1 54.3 54.7 1285 0 1 0 0 0 0 0 4.8483 0.0926 0.00176 0.00800 57 56 56.5 1330 0 1 0 0 0 0 0 4.8483 0.0926 0.00392 0.01783 59 58 58.5 1379 0 1 0 0 0 0 0 4.8483 0.0926 0.00599 0.02728 61 60 60.5 1428 1 1 0 0 0 0 0 4.7868 0.0626 0.00516 0.02350 63 62 62.5 1478 1 1 0 0 0 0 0 4.7868 0.0626 0.00666 0.03033 65 64 64.5 1527 1 1 0 0 0 0 0 4.7868 0.0626 0.00589 0.02682 67 66 66.5 1577 1 1 0 0 0 0 0 4.7868 0.0626 0.00875 0.03983 69 68 68.5 1626 0 1 0 0 0 0 0 4.8483 0.0926 0.00811 0.03690 71 70 70.5 1675 0 1 0 0 0 0 0 4.8483 0.0926 0.00620 0.02821 73 72 72.5 1725 0 1 0 0 0 0 0 4.8483 0.0926 0.00422 0.01922 75 74 74.5 1774 0 1 0 0 0 0 0 4.8483 0.0926 0.00687 0.03127 77 76 76.5 1824 0 1 0 0 0 0 0 4.8483 0.0926 0.01130 0.05142 79 78 78.5 1873 0 1 0 0 0 0 0 4.8483 0.0926 0.01471 0.06693 81 80 80.5 1922 0 1 0 0 0 0 1 4.3365 0.1962 0.01400 0.06371 83 82 82.5 1972 0 1 0 0 0 0 1 4.3365 0.1962 0.00898 0.04086 85 84 84.5 2021 0 1 0 0 0 0 1 4.3365 0.1962 0.00836 0.03807 87 86 86.5 2071 0 1 0 0 0 0 1 4.3365 0.1962 0.01250 0.05689 89 88 88.5 2120 0 1 0 0 0 0 1 4.3365 0.1962 0.01013 0.04613 91 90 90.5 2169 0 1 0 0 0 0 1 4.3365 0.1962 0.00932 0.04244 93 92 92.5 2219 0 1 0 0 0 0 1 4.3365 0.1962 0.01255 0.05713 95 94 94.5 2268 0 1 0 0 0 0 1 4.3365 0.1962 0.01397 0.06360 96 95 95.5 2293 0 1 0 0 0 0 0 4.8483 0.0926 0.00862 0.03926 97 96 96.5 2318 0 1 0 0 0 0 1 4.3365 0.1962 99 98 98.5 2367 0 1 0 0 0 0 1 4.3365 0.1962 0.00677 0.03081 100 99 99.5 2392 0 1 0 0 0 0 1 4.3365 0.1962 0.00526 0.02392 101 100 100.5 2416 0 1 0 0 0 0 1 4.3365 0.1962 103 102 102.5 2466 0 1 0 0 0 0 1 4.3365 0.1962 105 104 104.5 2515 0 1 0 0 0 0 1 4.3365 0.1962 107 106 106.5 2565 1 1 0 0 0 0 1 4.7600 0.0568 109 108 108.5 2614 0 1 0 0 0 0 1 4.3365 0.1962 0.00518 0.02358 111 110 110.5 2663 1 1 0 0 0 0 1 4.7600 0.0568 0.00796 0.03625 113 112 112.5 2713 0 1 0 0 0 0 1 4.3365 0.1962 0.01113 0.05067 115 114 114.5 2762 0 1 0 0 0 0 0 4.8483 0.0926 0.00808 0.03677 117 116 116.5 2812 1 1 0 0 0 0 1 4.7600 0.0568 0.00998 0.04545 123 122 122.5 2960 0 1 0 0 0 0 0 4.8483 0.0926 0.00896 0.04077 125 124 124.5 3009 1 1 0 0 0 0 1 4.7600 0.0568 0.00701 0.04160 127 126 126.5 3059 0 1 0 0 0 0 1 4.3365 0.1962 0.00453 0.02689 129 128 128.5 3108 1 0 0 0 0 0 1 4.6185 0.1145 0.00731 0.04336 131 130 130.5 3157 1 1 0 0 0 0 1 4.7600 0.0568 0.00796 0.04722 133 132 132.5 3207 1 0 0 0 0 0 0 4.8448 0.0644 0.00791 0.04690 135 134 134.5 3256 0 0 0 0 0 0 1 4.3397 0.1136 0.00528 0.03134 137 136 136.5 3306 0 1 0 0 0 0 1 4.3365 0.1962 139 138 138.5 3355 0 0 0 0 0 0 1 4.3397 0.1136 141 140 140.5 3404 0 1 0 0 0 0 1 4.3365 0.1962 143 142 142.5 3454 0 1 0 0 0 0 0 4.8483 0.0926 0.00836 0.03805 144 143 143.5 3478 0 1 0 0 0 0 0 4.8483 0.0926 0.01004 0.04570 145 144 144.5 3503 0 1 0 0 0 0 0 4.8483 0.0926 0.01023 0.04658 146 145 145.5 3528 0 1 0 0 0 0 1 4.3365 0.1962 0.01033 0.04700 147 146 146.5 3553 0 0 0 0 0 0 1 4.3397 0.1136 0.00860 0.05170 149 148 148.5 3602 0 0 0 0 0 0 1 4.3397 0.1136 0.00780 0.04686 151 150 150.5 3651 0 1 0 0 0 0 0 4.8483 0.0926 0.00826 0.04964 153 152 152.5 3701 1 0 0 0 0 0 0 4.8448 0.0644 0.00779 0.04681 155 154 154.5 3750 1 1 0 0 0 0 0 4.7868 0.0626 0.00755 0.04535 157 156 156.5 3800 1 0 0 0 0 0 0 4.8448 0.0644 0.00822 0.04938 159 158 158.5 3849 1 1 0 0 0 0 0 4.7868 0.0626 161 160 160.5 3898 1 0 0 0 0 0 0 4.8448 0.0644 163 162 162.5 3948 1 0 0 0 0 0 0 4.8448 0.0644 0.00454 0.02729 165 164 164.5 3997 1 0 0 0 0 0 0 4.8448 0.0644 167 166 166.5 4047 1 0 0 0 0 0 0 4.8448 0.0644 169 168 168.5 4096 1 0 0 0 0 0 0 4.8448 0.0644 171 170 170.5 4145 1 0 0 0 0 0 0 4.8448 0.0644 173 172 172.5 4195 0 0 0 0 0 0 0 NA NA 175 174 174.5 4244 1 0 0 0 0 0 0 4.8448 0.0644 177 176 176.5 4294 0 0 0 0 0 0 0 NA NA 179 178 178.5 4343 0 0 0 0 0 0 0 NA NA 181 180 180.5 4392 0 0 0 0 0 0 1 4.3397 0.1136 183 182 182.5 4442 0 0 0 0 0 0 1 4.3397 0.1136 185 184 184.5 4491 0 0 0 0 0 0 0 NA NA 187 186 186.5 4541 0 0 0 0 0 0 0 NA NA 189 188 188.5 4590 0 1 0 0 0 0 0 4.8483 0.0926 191 190 190.5 4639 0 1 0 0 0 0 1 4.3365 0.1962 193 192 192.5 4689 0 1 0 0 0 0 0 4.8483 0.0926 195 194 194.5 4738 0 0 0 0 0 0 1 4.3397 0.1136 197 196 196.5 4788 0 0 0 0 0 0 1 4.3397 0.1136 199 198 198.5 4837 0 0 0 0 0 0 0 NA NA 203 202 202.5 4936 0 0 0 0 0 0 0 NA NA 205 204 204.5 4985 0 0 0 0 0 0 1 4.3397 0.1136 207 206 206.5 5035 0 0 0 0 0 0 0 NA NA 209 208 208.5 5084 0 0 0 0 0 0 0 NA NA 211 210 210.5 5133 0 0 0 0 0 0 0 NA NA 213 212 212.5 5183 0 0 0 0 0 0 0 NA NA 215 214 214.5 5232 0 0 0 0 0 0 0 NA NA 217 216 216.5 5282 0 0 0 0 0 0 0 NA NA 219 218 218.5 5331 0 0 0 0 0 0 0 NA NA 221 220 220.5 5380 0 0 0 0 0 0 0 NA NA 223 222 222.5 5430 0 0 0 0 0 0 0 NA NA 225 224 224.5 5479 0 0 0 0 0 0 0 NA NA 227 226 226.5 5529 0 0 0 0 0 0 0 NA NA 229 228 228.5 5578 0 0 0 0 0 0 0 NA NA 231 230 230.5 5627 0 0 0 0 0 0 0 NA NA 233 232 232.5 5677 0 0 0 0 0 0 0 NA NA 235 234 234.5 5726 0 0 0 0 0 0 0 NA NA 237 236 236.5 5776 0 0 0 0 0 0 0 NA NA 239 238 238.5 5825 0 0 0 0 0 0 0 NA NA 241 240 240.5 5874 0 0 0 0 0 0 0 NA NA 243 242 242.5 5924 0 0 0 0 0 0 0 NA NA 245 244 244.5 5973 0 0 0 0 0 0 0 NA NA 247 246 246.5 6023 0 0 0 0 0 0 0 NA NA 249 248 248.5 6072 0 0 0 0 0 0 0 NA NA 251 250 250.5 6121 0 0 0 0 0 0 0 NA NA 253 252 252.5 6171 0 0 0 0 0 0 0 NA NA 255 254 254.5 6220 0 0 0 0 0 0 0 NA NA 257 256 256.5 6270 0 0 0 0 0 0 0 NA NA 259 258 258.5 6319 0 0 0 0 0 0 0 NA NA 261 260 260.5 6368 0 0 0 0 0 0 0 NA NA 263 262 262.5 6418 0 0 0 0 0 0 0 NA NA 265 264 264.5 6467 0 0 0 0 0 0 0 NA NA 267 266 266.5 6517 0 0 0 0 0 0 0 NA NA 269 268 268.5 6566 0 0 0 0 0 0 0 NA NA 271 270 270.5 6615 0 0 0 0 0 0 0 NA NA 273 272 272.5 6665 0 0 0 0 0 0 0 NA NA 275 274 274.5 6714 0 0 0 0 0 0 0 NA NA 277 276 276.5 6764 0 0 0 0 0 0 0 NA NA 279 278 278.5 6813 0 0 0 0 0 0 0 NA NA 281 280 280.5 6862 0 0 0 0 0 0 0 NA NA 283 282 282.5 6912 0 0 0 0 0 0 0 NA NA 285 284 284.5 6961 0 0 0 0 0 0 0 NA NA 287 286 286.5 7011 0 0 0 0 0 0 0 NA NA 289 288 288.5 7060 0 0 0 0 0 0 0 NA NA 291 290 290.5 7109 0 0 0 0 0 0 0 NA NA 293 292 292.5 7159 0 0 0 0 0 0 0 NA NA 295 294 294.5 7208 0 0 0 0 0 0 0 NA NA 297 296 296.5 7258 0 0 0 0 0 0 0 NA NA 299 298 298.5 7307 0 0 0 0 0 0 0 NA NA 301 300 300.5 7356 0 0 0 0 0 0 0 NA NA 303 302 302.5 7406 0 0 0 0 0 0 0 NA NA 305 304 304.5 7455 0 0 0 0 0 0 0 NA NA 307 306 306.5 7505 0 0 0 0 0 0 0 NA NA 309 308 308.5 7554 0 0 0 0 0 0 0 NA NA 311 310 310.5 7603 0 0 0 0 0 0 0 NA NA 313 312 312.5 7653 0 0 0 0 0 0 0 NA NA 315 314 314.5 7702 0 0 0 0 0 0 0 NA NA 317 316 316.5 7752 0 0 0 0 0 0 0 NA NA 319 318 318.5 7801 0 0 0 0 0 0 0 NA NA 321 320 320.5 7850 0 0 0 0 0 0 0 NA NA 323 322 322.5 7900 0 0 0 0 0 0 0 NA NA 325 324 324.5 7949 0 0 0 0 0 0 0 NA NA 327 326 326.5 7999 0 0 0 0 0 0 0 NA NA 329 328 328.5 8048 0 0 0 0 0 0 0 NA NA 331 330 330.5 8097 0 1 0 0 0 0 0 4.8483 0.0926 333 332 332.5 8147 0 1 0 0 0 0 0 4.8483 0.0926 335 334 334.5 8196 0 1 1 0 0 0 0 4.7245 0.0884 0.00332 0.01509 336.8 336 336.4 8243 0 1 1 0 0 0 0 4.7245 0.0884 0.00233 0.01058 339.3 338 338.65 8299 0 1 1 0 0 0 0 4.7245 0.0884 0.00209 0.00949 341.3 340.3 340.8 8352 0 1 1 0 0 0 0 4.7245 0.0884 0.00173 0.00787 342.8 341.3 342.05 8383 0 1 1 0 0 0 0 4.7245 0.0884 0.00186 0.00848 345 343.8 344.4 8441 0 1 1 0 0 0 0 4.7245 0.0884 0.00227 0.01033 347 346 346.5 8493 0 1 0 0 0 0 0 4.8483 0.0926 349 348 348.5 8542 0 1 1 0 0 0 0 4.7245 0.0884 0.00268 0.01219 353 352 352.5 8641 0 0 0 0 1 0 0 4.8411 0.0836 0.00503 0.02118 354 354.5 354.25 8684 1 0 1 0 1 0 0 4.6900 0.0842 0.00544 0.01782 355 355.8 355.4 8712 0 0 1 0 1 0 0 4.7773 0.0737 0.00457 0.01924 358.5 356.8 357.65 8768 0 0 1 0 1 0 0 4.7773 0.0737 0.00436 0.01837 360.7 359.6 360.05 8827 0 1 1 0 1 0 0 4.6636 0.0682 0.00380 0.01729 363 361.8 362.4 8885 1 0 0 0 0 0 0 4.8448 0.0644 364.9 363.9 364.4 8935 0 0 1 0 0 0 0 4.7324 0.1133 0.01201 0.03935 368.3 367.3 367.8 9019 1 0 0 0 1 0 0 4.8501 0.0600 0.00559 0.02353 370.3 369.3 369.8 9068 1 0 0 0 1 0 0 4.8501 0.0600 0.00599 0.02521 372.3 371.3 371.8 9117 1 0 0 0 1 0 0 4.8501 0.0600 0.00779 0.03282 375 373.3 374.15 9176 1 0 0 0 1 0 0 4.8501 0.0600 0.00859 0.03617 377.4 376.4 376.9 9243 1 0 0 0 1 0 0 4.8501 0.0600 0.01084 0.03553 379.7 378.4 379.05 9297 1 0 1 0 1 0 0 4.6900 0.0842 0.00848 0.03572 381.7 380.7 381.2 9350 1 0 1 0 1 0 0 4.6900 0.0842 0.01043 0.03417 383.8 382.7 383.25 9400 1 0 1 0 1 0 0 4.6900 0.0842 0.00986 0.03232 385.8 384.8 385.3 9451 1 0 1 0 1 0 0 4.6900 0.0842 0.00763 0.03214 386.8 385.8 386.3 9476 1 0 1 0 1 0 0 4.6900 0.0842 0.00891 0.02921 387.8 386.8 387.3 9500 1 0 1 0 1 0 0 4.6900 0.0842 0.01001 0.03279 389 387.8 388.4 9527 0 0 1 0 1 0 0 4.7773 0.0737 0.00569 0.02395