# Southern Great Basin strontium isotope, pollen, ostracod, lake level and magnetic susceptibility data from the late Pleistocene and Holocene #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # 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 '#' followed by a space # Data lines have no '#' # # NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/38781 # 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-lake-38781.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Paleolimnology # # Dataset_DOI: # # Science_Keywords: Hydrology, Earth Surface Conditions Reconstruction, Other Reconstruction, Last Interglacial, Interglacial #--------------------------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/california/lowenstein2024/lowenstein2024-dv-93-1_ostracods.txt # Data_Download_Description: NOAA Template File; DV-93-1 Ostracods Data # #--------------------------------------- # Contribution_Date # Date: 2024-06-18 #--------------------------------------- # File_Last_Modified_Date # Date: 2024-06-26 #--------------------------------------- # Title # Study_Name: Southern Great Basin strontium isotope, pollen, ostracod, lake level and magnetic susceptibility data from the late Pleistocene and Holocene #--------------------------------------- # Investigators # Investigators: Lowenstein, Tim (https://orcid.org/0000-0003-2828-7341); Olson, Kristian (https://orcid.org/0000-0003-4745-1688); Stewart, Brian; McGee, David (https://orcid.org/0000-0002-7329-3428); Stroup, Justin (https://orcid.org/0000-0002-0506-3479); Hudson, Adam (https://orcid.org/0000-0002-3387-9838); Wendt, Kathleen; Peaple, Mark (https://orcid.org/0000-0002-4208-0104); Feakins, Sarah (https://orcid.org/0000-0003-3434-2423); Spencer, Ronald; Bhattacharya, Tripti (https://orcid.org/0000-0002-5528-3760); Lund, Steve (https://orcid.org/0000-0002-1215-5478) #--------------------------------------- # Description_Notes_and_Keywords # Description: # Provided Keywords: strontium isotopes, pollen, ostracods, lake level, magnetic susceptibility #--------------------------------------- # Publication # Authors: Tim K. Lowenstein, Kristian J. Olson, Brian W. Stewart, David McGee, Justin S. Stroup, Adam M. Hudson, Kathleen A. Wendt, Mark D. Peaple, Sarah J. Feakins, Ronald J. Spencer, Tripti Bhattacharya, Steve Lund # Published_Date_or_Year: 2024 # Published_Title: Unified 200 kyr paleohydrologic history of the Southern Great Basin: Death Valley, Searles Valley, Owens Valley and the Devils Hole cave # Journal_Name: Quaternary Science Reviews # Volume: 336 # Edition: # Issue: # Pages: # Report_Number: # DOI: 10.1016/j.quascirev.2024.108751 # Online_Resource: # Full_Citation: # Abstract: We present a hydroclimate synthesis of the southern Great Basin over the last two glacial-interglacial cycles focused on paleolakes in Death Valley (core DV-93-1), Searles Lake (core SLAPP-SRLS17), Owens Lake (core OL92), and the Devils Hole Cave. There is close agreement between the occurrence of lakes in Death Valley and the height of the water table in the Devils Hole (50 km to the northeast) during the last 200 kyr. Death Valley and Devils Hole have adjacent, partly overlapping, drainage areas and most likely did over the last 200 kyr. When the water table in the Devils Hole was above the threshold level of ~5 m higher than the modern, permanent lakes existed in Death Valley. At water table elevations less than 5 m above the modern, ephemeral lakes, saline pans, and mudflats occurred in Death Valley. The close temporal agreement between inferred paleoenvironments from the sediments in the Death Valley core and the paleowater table elevation in Devils Hole suggests a common forcing and provides insight into climate variability in the southwestern United States over the last two glacial cycles. Owens Lake and Searles Lake, which derived inflow waters from the Sierra Nevada via the Owens River, contain paleohydrologic records which match those from Death Valley and the Devils Hole in terms of timing and direction of water availability over the last two glacial- interglacial cycles, indicating a similar paleohydrologic history for the entire southern Great Basin region. Near the end of the penultimate glacial, ~140 ka - 130 ka (Termination II), Lake Manly in Death Valley became shallow and hypersaline, and ultimately dried up at 127.1 ka ± 4.3 ka. The transition from glacial to interglacial vegetation, which involves loss of Juniperus pollen and increase in oak pollen)Quercus (oak) pollen, occurs in Death Valley core DV93-1 at 131.3 ka ± 4 ka. Following the glacial to interglacial pollen shift, an anomalous large alkaline lake formed in Death Valley. Similarly unusual conditions (freshwater, high productivity, and a mixed, deeply oxygenated water column indicated by biomarkers) existed in Searles Lake between 135.3 +2.7 / -2.9 ka and 130.1 +2.7 / -2.6 ka, also following the juniper-oak pollen transition. Sr isotopes in calcite and sulfate minerals (gypsum, glauberite, thenardite), and the rare occurrence of the sodium carbonate mineral northupite with a low 87 Sr/ 86 Sr ratio in core DV93-1, together with organic geochemical proxies from Searles core SLAPP-SRLS17, all suggest that at this time, late glacial Lake Manly received alkaline water via spillover from Searles Lake into Death Valley through Panamint Valley. The hydrologic connection between Searles Lake, Panamint Lake, and Death Valley during Termination II is documented here for this system of pluvial lakes for the first time. The Devils Hole water table decreased to +6.5 m at 140.8 ka ± 3.2 ka, rose briefly to +8 m at 137.6 ka ± 0.5 ka, and then dropped 8 m by 120.36 ka ± 0.45 ka, when it reached an elevation similar to the modern. The unusual lakes in Death Valley and Searles Valley may have coincided with the rise of the Devils Hole water table at ~ 137.6 ka ± 0.5 ka years ago, although the age models for core DV93-1 and Searles Lake core SLAPP-SLRS17 during the end of the penultimate glacial carry large uncertainties. #--------------------------------------- # Publication # Authors: Mark D. Peaple, Tripti Bhattacharya, Tim K. Lowenstein, David McGee, Kristian J. Olson, Justin S. Stroup, Jessica E. Tierney, Sarah J. Feakins # Published_Date_or_Year: 2022 # Published_Title: Biomarker and Pollen Evidence for Late Pleistocene Pluvials in the Mojave Desert # Journal_Name: Paleoceanography and Paleoclimatology # Volume: 37 # Edition: 10 # Issue: e2022PA004471 # Pages: # Report_Number: # DOI: 10.1029/2022PA004471 # Online_Resource: # Full_Citation: # Abstract: The climate of the southwestern North America has experienced profound changes between wet and dry phases over the past 200 Kyr. To better constrain the timing, magnitude, and paleoenvironmental impacts of these changes in hydroclimate, we conducted a multiproxy biomarker study from samples collected from a new 77 m sediment core (SLAPP-SRLS17) drilled in Searles Lake, California. Here, we use biomarkers and pollen to reconstruct vegetation, lake conditions, and climate. We find that dD values of long chain n-alkanes are dominated by glacial to interglacial changes that match nearby Devils Hole calcite d18O variability, suggesting both archives predominantly reflect precipitation isotopes. However, precipitation isotopes do not simply covary with evidence for wet-dry changes in vegetation and lake conditions, indicating a partial disconnect between large scale atmospheric circulation tracked by precipitation isotopes and landscape moisture availability. Increased crenarchaeol production and decreased evidence for methane cycling reveal a 10 Kyr interval of a fresh, productive, and well-mixed lake during Termination II, corroborating evidence for a paleolake highstand from shorelines and spillover deposits in downstream Panamint Basin and Death Valley during the end of the penultimate (Tahoe) glacial (140–130 ka). At the same time brGDGTs yield the lowest temperature estimates (mean months above freezing = 9°C ± 3°C) of the 200 Kyr record. These limnological conditions are not replicated elsewhere in the 200 Kyr record, suggesting that the Heinrich stadial 11 highstand was wetter than the last glacial maximum and Heinrich 1 (18–15 ka). #--------------------------------------- # Publication # Authors: Richard M. Forester, Tim K. Lowenstein, Ronald J. Spencer # Published_Date_or_Year: 2005 # Published_Title: An ostracode based paleolimnologic and paleohydrologic history of Death Valley: 200 to 0 ka # Journal_Name: Geological Society of America Bulletin # Volume: 117 # Edition: # Issue: # Pages: 1379-1386 # Report_Number: # DOI: 10.1130/B25637.1 # Online_Resource: # Full_Citation: # Abstract: Death Valley, a complex tectonic and hydrologic basin, was cored from its lowest surface elevation to a depth of 186 m. The sediments range from bedded primary halite to black muds. Continental ostracodes found in the black muds indicate that those sediments were deposited in a variety of hydrologic settings ranging from deep, relatively fresh water to shallow saline lakes to spring discharge supported wetlands. The alkaline-enriched, calcium-depleted paleolake waters indicate extrabasinal streamflow and basin-margin spring discharge. The alkaline-depleted, calcium-enriched paleowetland waters indicate intrabasinal spring discharge. During Marine Isotope Stage 6 (MIS 6, ca. 180-140 ka) the hydrologic settings were highly variable, implying that complex relations existed between climate and basin hydrology. Termination II (MIS 6 to MIS 5E) was a complex multicyclic sequence of paleoenvironments, implying that climates oscillated between high and low effective moisture. MIS 4 (ca. 73-61 ka) was a spring discharge supported wetland complex. During MIS 2 (ca. 20-12 ka) the hydrologic settings were variable, although they are not fully understood because some black muds deposited during that time were lost during coring. #--------------------------------------- # Publication # Authors: Tim K. Lowenstein; Jianren Li; Christopher Brown; Sheila M. Roberts; Teh-Lung Ku; Shangde Luo; Wenbo Yang # Published_Date_or_Year: 1999 # Published_Title: 200 k.y. paleoclimate record from Death Valley salt core # Journal_Name: Geology # Volume: 27 # Edition: # Issue: # Pages: 3-6 # Report_Number: # DOI: 10.1130/0091-7613(1999)027<0003:KYPRFD>2.3.CO;2 # Online_Resource: # Full_Citation: # Abstract: A 186-m-long core (DV93-1) from Death Valley, California, composed of interbedded salts and muds contains a 200 k.y. record of closed-basin environments and paleoclimates, interpreted on the basis of sedimentology, ostracodes, homogenization temperatures of fluid inclusions in halite, and correlation with shoreline tufa. The 200 k.y. paleoclimate record is dominated by two dry and/or warm and wet and cold cycles that occurred on a 100 k.y. time scale. These cycles begin with mud-flat deposits (192 ka to bottom of core, and 60 ka to 120 ka). Wetter and/or colder conditions produced greater effective moisture; saline pan and shallow saline lake evaporites overlie mud-flat sediments (186 ka to 192 ka and 35 ka to 60 ka). Eventually, enough water entered Death Valley to sustain perennial lakes that had fluctuating water levels and salinities (120 ka to 186 ka and 10 ka to 35 ka). When more arid conditions returned, mud-flat deposits accumulated on top of the perennial lake sediments, completing the cycle (120 ka and 10 ka). Of particular significance are the major lacustrine phases, 10 ka to 35 ka and 120 ka to 186 ka (oxygen isotope stages 2 and 5e–6), which represent markedly colder and wetter conditions than those of modern Death Valley. Of the two major lake periods, the penultimate glacial lakes were deeper and far longer lasting than those of the last glacial. #--------------------------------------- # Publication # Authors: Nicholas E. Bader # Published_Date_or_Year: 2000 # Published_Title: Pollen Analysis of Death Valley Sediments Deposited Between 166 and 114 ka # Journal_Name: Palynology # Volume: 24 # Edition: # Issue: # Pages: 49-61 # Report_Number: # DOI: # Online_Resource: # Full_Citation: # Abstract: Salt Core DV93-1, from Badwater Basin in California’s Death Valley, is a nearly complete sedimentary record of mud and evaporite deposits spanning the past 192 ka. Fossil palynomorph assemblages from core depths of 151.8 m (ca. 166 ka) to 103.5 m (ca. 114 ka) have been analyzed as part of a larger study which will eventually include all of core DV93-1. The palynological analysis discussed here reveals four pollen zones between 151.8 m and 103.5 m. Zone 1, the “Cheno–Am” zone (151.8 m to 143.5 m depth, 166–154 ka), has high percentages of Chenopodiaceae/Amaranthus (Cheno–Am) pollen, and is correlative with the end of marine Oxygen Isotope Stage (OIS) 7. Zone 2, the juniper zone (143.5 m to 117.3 m, 154–124 ka), correlates with OIS 6, as evidenced by high percentages of juniper (Cupressaceae) pollen and low percentages of Ambrosia pollen. Equivalent pollen assemblages are found at higher elevations in Death Valley today, where temperatures are 11° C cooler and rainfall is eight times greater. At the top of Zone 2 (124 ka), a simultaneous drop in juniper and increase in oak (Quercus) pollen occurs, followed by a replacement of Artemisia with Ambrosia in Zone 3, the oak zone. This event corresponds to warming associated with Termination II. The estimated age of this warming event is in agreement with the Termination II event visible in the pollen record from nearby Owens Lake (Litwin et al., 1997). Zone 4, the Asteraceae zone (108.8 m to 103.5 m, 119–115 ka), contains higher percentages of Asteraceae and Cheno–Am pollen, indicating further warming during this time. #--------------------------------------- # Publication # Authors: Kathleen A Wendt, Yuri V Dublyansky, Gina E Moseley, R Lawrence Edwards, Hai Cheng, Christoph Spötl # Published_Date_or_Year: 2018 # Published_Title: Moisture availability in the southwest United States over the last three glacial-interglacial cycles # Journal_Name: Science Advances # Volume: 4 # Edition: eaau1375 # Issue: 10 # Pages: # Report_Number: # DOI: 10.1126/sciadv.aau1375 # Online_Resource: # Full_Citation: # Abstract: The projected long-term drying of the southwest (SW) United States in response to climate warming raises a sobering alarm for this already water-limited region, yet the climatic controls on moisture availability over longer time scales remain a topic of debate. Here, we present a 350,000-year record of past water table fluctuations in Devils Hole 2 cave that are driven by variations in recharge amount to the local groundwater flow system. Because of the unprecedented length and precision of our record, we can observe variations in regional moisture availability over the last three glacial-interglacial cycles at a millennial-scale resolution. The timing of past water table rises and falls (>9 m in amplitude) closely coincides with the expansion and reduction of Northern Hemisphere ice volume, which in turn influences the position and intensity of westerly winter storms on orbital time scales. Superimposed on this long-term trend are millennial-scale highstands recorded during the last glaciation that coincide with North Atlantic Heinrich events. Earlier millennial-scale highstands provide the first evidence of multiple short-lived wet periods in the SW United States linked to coeval cooling intervals in the North Atlantic during marine isotope stages 6 and 8. The Devils Hole 2 water table record is currently the longest independently dated paleomoisture record in the SW United States and thus provides a critical testbed to examine the controls on regional moisture availability over larger time scales. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: National Science Foundation # Grant: 1903519, 1903659, 1903544, 1903665 #--------------------------------------- # Site_Information # Site_Name: Death Valley (DV-93-1) # Location: California # Northernmost_Latitude: 36.2295 # Southernmost_Latitude: 36.2295 # Easternmost_Longitude: -116.7679 # Westernmost_Longitude: -116.7679 # Elevation_m: -86 #--------------------------------------- # Data_Collection # Collection_Name: DV-93-1_ostracods # First_Year: 216 # Last_Year: 2 # Time_Unit: calendar year before present # Core_Length_m: 190 # Parameter_Keywords: population abundance # Notes: #--------------------------------------- # Chronology_Information # Chronology: # DV-93-1 # ID depth_m 238U 238U_err 232Th 232Th_err d234U d234U_err 230Th/238U 230Th/238U_err 230Th/232Th 230Th/232Th_err Age_ya_uncorr Age_ya_uncorr_err Age_ya_corr Age_ya_corr_err d234U_initial d234U_initial_err 230Th/232Th 230Th/232Th_err 232Th/238U 232Th/238U_err 234U/238U 234U/238U_err # KO1 7.7 15.9 0.3 45500 900 486.2 1.2 0.864 0.017 4.79 0.1 89500 2600 10000 80000 500 120 0.888222130187116 1.77290460191539E-02 0.973291029236004 2.14752943116226E-03 1.48618478081336 1.21537889840751E-03 # KO2 60 4.9 0.1 9860 200 519.6 2 1.024 0.013 8.08 0.1 112000 2300 70000 30000 630 50 1.49813995442895 1.86902862002518E-02 0.683558912772396 8.66781874205963E-04 1.51955724677742 1.98901302360213E-03 # KO3 86.5 152 3 81100 1600 424.6 0.7 0.932 0.004 27.75 0.12 107900 700 97000 6000 558 9 5.14306610180765 2.24802866429729E-02 0.181241839563264 2.44251489353179E-04 1.4245729680715 6.74084784568404E-04 # KO4 125.3 73.9 1.5 84400 1700 585.2 0.8 1.362 0.009 18.94 0.14 173800 2400 154000 11000 900 30 3.51043864465018 2.62090285908118E-02 0.387967483633884 9.11649629573891E-04 1.58524101577744 7.81777198285997E-04 # KO5 161.7 144 3 42700 900 616.4 0.7 1.495 0.007 80.3 0.5 205000 2300 200600 3200 1086 10 14.8924431909416 9.03802192068581E-02 0.100415519992298 2.43221571417079E-04 1.61642246506931 6.78434271314738E-04 # KO6 182.8 13.5 0.3 21900 400 243.9 1.9 1.136 0.01 11.14 0.1 222400 6100 180000 30000 410 30 2.06557525778172 1.86956046326965E-02 0.550160023111497 6.83703386430939E-04 1.24388094659288 1.85403012499842E-03 # KO7 16.1 34.4 0.7 31200 600 881.9 1.3 0.568 0.006 9.95 0.1 38100 500 23000 8000 940 20 1.84356201840579 1.88472129117852E-02 0.308075607557102 4.50282566781698E-04 1.88191461938922 1.28445879588868E-03 # KO8 56.8 13.5 0.3 3310 70 856.7 0.9 0.924 0.004 59.9 0.3 70700 400 67000 1900 1035 6 11.094103387945 4.97298371809851E-02 8.33061199312826E-02 1.08686368210817E-04 1.85670250326953 9.34287604882082E-04 # KO9 76.8 17.9 0.4 16600 300 492.2 1.6 1.047 0.007 17.91 0.13 120200 1400 102000 10000 656 19 3.31897562824516 2.46405633450295E-02 0.315548229063567 6.43701089942267E-04 1.49220228705797 1.59250403024423E-03 # KO10 109.7 97.1 1.9 41400 800 461.9 0.9 1.095 0.005 40.8 0.2 135100 1200 127100 4300 661 8 7.55674517167928 4.11103379240729E-02 0.144854655363869 2.62946812792292E-04 1.46193132745194 8.95765116752378E-04 # KO11 138.9 229 5 242000 5000 608.4 0.6 1.584 0.01 23.72 0.17 243000 4000 228000 10000 1160 30 4.39657729681393 3.12413719656602E-02 0.360340190128824 7.95868224912882E-04 1.60839058329659 6.16426377255764E-04 # KO12 148.5 68.9 1.4 135000 3000 477.7 1.1 1.547 0.013 12.55 0.11 321000 12000 290000 20000 1080 70 2.32602557565238 2.03113777786924E-02 0.66520769932935 1.12167855296466E-03 1.47770949582783 1.07672132194239E-03 # #--------------------------------------- # Variables # PaST_Thesaurus_Download_Resource: https://www.ncei.noaa.gov/access/paleo-search/skos/past-thesaurus.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_m depth,sediment,,meter,,Paleolimnology,,,N, ## age_calkyrBP age,sediment,,calendar kiloyear before present,,Paleolimnology,,,N,Mean; central estimate of the age model. ## L_staplini identified ostracod,sediment,,count,,Paleolimnology,,microscopy,N,1=species present; 0=specieis not present ## C_rawsoni identified ostracod,sediment,,count,,Paleolimnology,,microscopy,N,1=species present; 0=specieis not present ## L_sappaensis identified ostracod,sediment,,count,,Paleolimnology,,microscopy,N,1=species present; 0=specieis not present ## L_cenotuberosa identified ostracod,sediment,,count,,Paleolimnology,,microscopy,N,1=species present; 0=specieis not present ## C_caudata identified ostracod,sediment,,count,,Paleolimnology,,microscopy,N,1=species present; 0=specieis not present #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: -999999 depth_m age_calkyrBP L_staplini C_rawsoni L_sappaensis L_cenotuberosa C_caudata 1.57 1.789 0 0 0 0 0 2.11 2.404 0 0 0 0 0 2.36 2.686 0 0 0 0 0 3.33 3.784 0 0 0 0 0 4.19 4.762 0 0 0 0 0 4.47 5.083 0 0 0 0 0 4.72 5.369 0 0 0 0 0 5.64 6.42 0 0 0 0 0 6.73 7.667 0 0 0 0 0 7.11 8.033 0 0 0 0 0 8.69 10.079 1 0 0 0 0 10.41 14.031 1 1 0 0 0 10.82 14.976 0 0 0 0 0 13.74 21.642 0 0 0 0 0 14.02 22.277 0 0 0 0 0 14.3 22.918 1 0 0 1 0 14.59 23.583 0 0 0 0 0 14.96 24.43 1 0 0 0 0 15.6 25.882 1 1 0 0 0 16 26.788 1 0 0 0 0 16.09 26.957 1 0 1 0 0 16.57 27.859 0 0 0 0 0 16.87 28.422 1 0 0 0 0 16.98 28.629 1 0 0 0 0 17.67 29.311 0 0 0 0 1 18.01 29.638 0 0 0 0 0 18.18 29.798 1 0 0 0 0 60.71 69.105 0 0 0 0 0 92.05 105.992 0 0 0 0 0 92.47 106.534 0 0 0 0 0 94.35 108.961 0 0 0 0 0 96.425 #N/A 0 1 0 0 0 98.15 113.873 0 0 0 0 0 100 116.25 0 0 0 0 0 101 117.543 0 0 0 0 0 102 118.83 0 0 0 0 0 104 121.411 0 0 0 0 0 107.1 125.414 0 0 0 0 0 108 126.575 0 0 0 0 0 108.96 127.374 0 1 0 0 0 109.65 127.702 0 0 0 0 0 113.35 129.4 1 0 0 1 0 115.6 130.437 0 1 0 1 0 115.8 130.529 1 1 1 1 0 116 130.621 1 0 0 0 0 116.7 130.944 0 0 0 0 0 117.05 131.105 0 0 0 0 0 117.4 131.266 0 0 0 0 0 118 131.541 1 0 0 0 0 118.4 131.727 0 0 1 0 0 119.1 132.051 0 0 0 0 0 119.6 132.283 1 0 0 0 0 120 132.468 0 0 1 0 0 120.3 132.606 1 0 1 0 0 120.6 132.744 1 0 1 0 0 120.8 132.837 0 0 1 0 0 121.2 133.021 0 1 0 0 0 121.6 133.204 1 1 0 0 0 122.6 133.666 0 0 0 0 0 123.25 133.966 0 0 0 0 0 124.95 134.75 0 0 1 0 0 125 134.773 1 0 1 0 0 125.15 134.843 1 1 1 1 0 125.45 134.982 1 1 1 0 0 125.65 135.076 1 0 1 0 0 125.85 135.169 0 0 1 0 0 126 135.239 1 1 1 1 0 126.1 135.285 1 0 1 0 0 126.5 135.471 0 1 1 0 0 126.7 135.564 1 0 1 0 0 126.9 135.657 1 0 1 0 0 127 135.703 0 0 0 0 0 127.1 135.728 0 0 1 0 0 127.3 135.778 0 0 1 0 0 127.5 135.828 1 0 1 0 0 127.75 135.893 1 0 1 0 0 127.95 135.939 0 0 1 0 0 128 135.95 0 0 1 0 0 130.8 140.668 1 0 0 0 0 131 141.005 1 0 0 0 0 131.2 141.341 0 0 0 0 0 131.4 141.677 1 0 0 0 0 131.6 142.012 0 0 0 0 0 131.8 142.348 0 0 1 0 0 131.88 142.483 0 0 1 0 0 133 144.356 0 0 1 0 0 133.2 144.691 1 0 0 0 0 133.4 145.026 1 0 1 0 0 133.6 145.361 1 0 0 0 0 133.8 145.696 1 0 0 0 0 134 146.031 0 0 0 0 0 134.2 146.368 1 0 0 0 0 134.4 146.705 1 0 0 0 0 134.6 147.042 1 0 0 0 0 134.8 147.379 0 0 0 0 0 135 147.715 1 1 0 0 0 135.2 148.05 1 0 0 0 0 135.4 148.385 0 1 0 0 0 135.6 148.72 1 1 1 0 0 135.8 149.055 1 0 0 0 0 135.9 149.223 1 0 0 0 0 136 149.39 1 0 0 0 0 136.15 149.642 0 0 1 0 0 137.1 151.24 1 1 0 0 0 137.3 151.574 1 0 0 0 0 138.5 153.71 0 0 0 1 0 138.6 153.903 0 1 0 1 0 138.8 154.288 0 0 0 1 0 139 154.674 0 1 1 1 0 139.2 155.079 0 1 1 0 0 139.4 155.484 0 0 0 0 0 140 156.7 0 0 0 1 0 140.2 157.101 0 1 0 1 0 140.4 157.502 0 0 0 1 0 140.6 157.903 0 0 0 1 0 140.8 158.304 0 0 0 0 0 141 158.705 0 0 0 0 0 141.2 159.107 0 0 1 1 0 141.4 159.51 0 0 0 0 0 141.6 159.912 0 0 1 0 0 141.8 160.314 0 1 1 0 0 141.95 160.616 0 0 0 0 0 143 162.733 0 0 0 0 0 143.2 163.133 0 0 0 0 1 143.4 163.533 0 0 0 0 0 143.6 163.932 0 0 0 0 0 143.8 164.332 0 0 0 0 0 144 164.731 0 0 0 0 0 144.23 165.196 0 0 0 0 0 144.4 165.54 0 0 0 0 0 144.6 165.944 0 0 0 0 0 144.8 166.348 0 0 0 0 0 145.1 166.954 0 0 1 0 0 145.2 167.156 0 0 0 0 0 145.4 167.559 0 1 0 0 0 145.6 167.963 0 0 0 0 0 145.8 168.366 0 1 0 0 0 146 168.77 0 0 0 0 0 146.2 169.175 0 0 0 0 0 146.4 169.58 0 1 0 0 0 146.6 169.985 0 0 0 0 0 146.76 170.309 0 0 0 0 0 147.85 172.498 0 0 0 0 0 148 172.798 0 0 0 0 0 148.2 173.2 0 0 0 0 0 148.4 173.602 0 0 0 0 0 151 178.827 0 0 0 0 0 151.2 179.235 0 0 0 0 0 151.4 179.642 0 0 0 0 0 151.6 180.05 0 0 1 0 0 151.8 180.458 0 0 0 0 0 152 180.866 0 0 0 0 0 152.2 181.295 0 0 0 0 0 152.4 181.724 0 0 0 0 0 152.6 182.152 0 0 0 0 0 152.8 182.581 0 0 0 0 0 153 183.01 0 0 0 0 0 153.2 183.441 0 0 1 0 0 153.4 183.872 0 0 0 0 0 154 185.165 0 0 0 0 0 154.2 185.594 0 0 0 0 0 155.2 187.742 1 1 1 0 0 155.5 188.386 0 0 0 0 0 155.7 188.815 0 0 1 0 0 156.8 191.192 1 0 0 0 0 157 191.626 1 0 0 0 0 157.2 192.053 0 0 0 0 0 157.35 192.374 0 0 0 0 0 157.71 193.144 1 0 1 1 0 158 193.763 0 0 0 0 0 158.2 194.191 0 0 0 0 0 158.4 194.619 0 0 0 0 0 158.6 195.046 0 0 0 0 0 159 195.901 0 0 0 0 0 159.2 196.332 0 0 0 0 0 159.4 196.762 1 0 0 0 0 159.6 197.193 0 0 1 0 0 159.8 197.623 0 0 0 0 0 160 198.054 0 0 0 0 0 160.1 198.157 0 0 0 0 0 160.8 198.877 0 0 0 0 0 160.9 198.98 0 0 0 0 0 161.25 199.334 0 0 0 0 0 161.57 199.656 0 0 0 0 0 162.15 200.224 0 1 0 0 0 172.2 209.423 0 0 0 0 0 173.7 210.802 0 0 0 0 0 173.7 210.802 0 0 0 0 0 173.96 211.041 0 0 0 0 0 174 211.078 0 0 0 0 0 174.73 211.744 0 0 0 0 0 175 211.99 0 0 0 0 0 175.05 212.036 0 0 0 0 0 175.73 212.657 0 0 0 0 0 176 212.904 0 0 0 0 0 176.77 213.611 0 0 0 0 0 177 213.822 1 0 0 0 0 177.56 214.335 0 0 0 0 0 177.95 214.692 0 0 0 0 0 178 214.737 0 0 0 0 0 179 215.645 0 0 0 0 0