# Garrison Basin, Gulf of Mexico d18O and Mg/Ca in three multicores and stacked SST/d18Osw/SSS reconstructions spanning the past 4.4 kyrs #----------------------------------------------------------------------- # 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/23373 # Description: NOAA Landing Page # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/by_contributor/thirumalai2018/thirumalai2018-stack.txt # Description: NOAA location of the template # # Archive: Paleoceanography # # Dataset_DOI: # # Parameter_Keywords: oxygen isotopes, trace metals in carbonates, age control, geochemistry #--------------------------------------- # Contribution_Date # Date: 2018-02-05 #--------------------------------------- # File_Last_Modified_Date # Date: 2018-02-05 #--------------------------------------- # Title # Study_Name: Garrison Basin, Gulf of Mexico d18O and Mg/Ca in three multicores and stacked SST/d18Osw/SSS reconstructions spanning the past 4.4 kyrs #--------------------------------------- # Investigators # Investigators: Thirumalai, Kaustubh; Quinn, Terrence M.; Okumura, Yuko; Richey, Julie N.; Partin, Judson W.; Poore, Richard Z.; Moreno-Chamarro, Eduardo; #--------------------------------------- # Description_Notes_and_Keywords # Description: Sea-surface temperature, d18Osw, and sea-surface salinity reconstructions from the northern Gulf of Mexico generated from paired Mg/Ca-dą8O measurements in G. ruber (White) from three Garrison Basin sediment cores spanning the last 4,400 years # Provided Keywords: Gulf of Mexico, sea-surface temperature, sea-surface salinity, G. ruber, foraminifera, late Holocene #--------------------------------------- # Publication # Authors: Thirumalai, K., T.M. Quinn, Y. Okumura, J.N. Richey, J.W. Partin, R.Z. Poore, and E. Moreno-Chamarro # Published_Date_or_Year: 2018 # Published_Title: Pronounced centennial-scale Atlantic Ocean climate variability correlated with Western Hemisphere hydroclimate # Journal_Name: Nature Communications # Volume: 9 # Edition: # Issue: 1 # Pages: 1-11 # Report Number: 392 # DOI: 10.1038/s41467-018-02846-4 # Online_Resource: # Full_Citation: # Abstract: Surface-ocean circulation in the northern Atlantic Ocean influences Northern Hemisphere climate. Century-scale circulation variability in the Atlantic Ocean, however, is poorly con- strained due to insufficiently-resolved paleoceanographic records. Here we present a repli- cated reconstruction of sea-surface temperature and salinity from a site sensitive to North Atlantic circulation in the Gulf of Mexico which reveals pronounced centennial-scale varia- bility over the late Holocene. We find significant correlations on these timescales between salinity changes in the Atlantic, a diagnostic parameter of circulation, and widespread pre- cipitation anomalies using three approaches: multiproxy synthesis, observational datasets, and a transient simulation. Our results demonstrate links between centennial changes in northern Atlantic surface-circulation and hydroclimate changes in the adjacent continents over the late Holocene. Notably, our findings reveal that weakened surface-circulation in the Atlantic Ocean was concomitant with well-documented rainfall anomalies in the Western Hemisphere during the Little Ice Age. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: # Grant: #--------------------------------------- # Site Information # Site_Name: Garrison Basin # Location: Gulf of Mexico # Country: USA # Northernmost_Latitude: 26.66 # Southernmost_Latitude: 26.66 # Easternmost_Longitude: -93.92 # Westernmost_Longitude: -93.92 # Elevation: -1776 #--------------------------------------- # Data_Collection # Collection_Name: Garrison Stack Thirumalai2018 # First_Year: -2403 # Last_Year: 1999 # Time_Unit: AD # Core_Length: 0.6 # Notes: Most recent year is -49 yr BP and oldest is 4353 yr BP #--------------------------------------- # Chronology_Information # Chronology: # # core ID name of multicore dated # core.sample Interval of sampling in core # depth_top Top depth of sample interval (cm) # depth_bottom Bottom depth of sample interval (cm) # depth_mid Middle depth of sampled interval (cm) # mat.dated Material dated # 14C.raw Conventional radiocarbon age, years before 1950AD # 14C.raw_err Radiocarbon age, standard error # # core core.sample depth_bottom depth_top depth_mid mat.dated 14C.raw 14C.raw_err # 2010-GB2-MCA 2010-GB2-MCA 0.0-0.5 0.5 0 0.25 Mixed Planktics >Modern 30 # 2010-GB2-MCA 2010-GB2-MCA 9.5-10.0 10 9.5 9.75 Mixed Planktics 855 30 # 2010-GB2-MCA 2010-GB2-MCA 19.5-20.0 20 19.5 19.75 Mixed Planktics 1450 30 # 2010-GB2-MCA 2010-GB2-MCA 34.5-35 35 34.5 34.75 Mixed Planktics 2405 30 # 2010-GB2-MCA 2010-GB2-MCA 49.5-50 50 49.5 49.75 Mixed Planktics 3560 35 # 2010-GB2-MCA 2010-GB2-MCA 59.5-60 60 59.5 59.75 Mixed Planktics 4250 30 # 2010-GB2-MCB 2010-GB2-MCB 0-0.25 0.25 0 0.125 Mixed Planktics >Modern 30 # 2010-GB2-MCB 2010-GB2-MCB 11-11.25 11.25 11 11.125 Mixed Planktics 910 30 # 2010-GB2-MCB 2010 GB2 MCB 34-34.25 34.25 34 34.125 Mixed Planktics 2280 30 # 2010-GB2-MCC 2010 GB2 MCC 0-0.5 0.5 0 0.25 Mixed Planktics >Modern 30 # 2010-GB2-MCC 2010 GB2 MCC 9.5-10 10 9.5 9.75 Mixed Planktics 950 30 # 2010-GB2-MCC 2010 GB2 MCC 29.5-30 30 29.5 29.75 Mixed Planktics 2065 30 # #--------------------------------------- # 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) ## age age,,,calendar year before present,,,,,N, ## stack_sst sea surface temperature,Globigerinoides ruber white,,degree Celsius,annual,climate reconstruction;paleoceanography,,,N,See Thirumalai et al. 2018 for inversion equations and details; stacked record ## e32_sst sea surface temperature,Globigerinoides ruber white,percentile,degree Celsius,annual,climate reconstruction;paleoceanography,,,N,32nd percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e68_sst sea surface temperature,Globigerinoides ruber white,percentile,degree Celsius,annual,climate reconstruction;paleoceanography,,,N,68th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e5_sst sea surface temperature,Globigerinoides ruber white,percentile,degree Celsius,annual,climate reconstruction;paleoceanography,,,N,5th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e95_sst sea surface temperature,Globigerinoides ruber white,percentile,degree Celsius,annual,climate reconstruction;paleoceanography,,,N,95th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## stack_d18O-sw seawater delta 18O,Globigerinoides ruber white,,per mil VSMOW,annual,climate reconstruction;paleoceanography,,,N,See Thirumalai et al. 2018 for inversion equations and details; stacked record ## e32_d18O-sw seawater delta 18O,Globigerinoides ruber white,percentile,per mil VSMOW,annual,climate reconstruction;paleoceanography,,,N,32nd percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e68_d18O-sw seawater delta 18O,Globigerinoides ruber white,percentile,per mil VSMOW,annual,climate reconstruction;paleoceanography,,,N,68th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e5_d18O-sw seawater delta 18O,Globigerinoides ruber white,percentile,per mil VSMOW,annual,climate reconstruction;paleoceanography,,,N,5th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e95_d18O-sw seawater delta 18O,Globigerinoides ruber white,percentile,per mil VSMOW,annual,climate reconstruction;paleoceanography,,,N,95th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## stack_sss sea surface salinity,Globigerinoides ruber white,,practical salinity unit,annual,climate reconstruction;paleoceanography,,,N,See Thirumalai et al. 2018 for inversion equations and details; stacked record ## e32_sss sea surface salinity,Globigerinoides ruber white,percentile,practical salinity unit,annual,climate reconstruction;paleoceanography,,,N,32nd percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e68_sss sea surface salinity,Globigerinoides ruber white,percentile,practical salinity unit,annual,climate reconstruction;paleoceanography,,,N,68th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e5_sss sea surface salinity,Globigerinoides ruber white,percentile,practical salinity unit,annual,climate reconstruction;paleoceanography,,,N,5th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) ## e95_sss sea surface salinity,Globigerinoides ruber white,percentile,practical salinity unit,annual,climate reconstruction;paleoceanography,,,N,95th percentile; See Thirumalai et al. 2018 for error details (uncertainty accounts for analytical, sampling, and dating uncertainty) #------------------------ # Data # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Value: NA age stack_sst e32_sst e68_sst e5_sst e95_sst stack_d18O-sw e32_d18O-sw e68_d18O-sw e5_d18O-sw e95_d18O-sw stack_sss e32_sss e68_sss e5_sss e95_sss -49 26.6 0.06 0.13 0.31 0.36 1.06 0.03 0.03 0.11 0.11 36.42 0.06 0.06 0.21 0.20 -14 26.0 0.1 0.1 0.3 0.3 1.34 0.04 0.02 0.13 0.10 36.9 0.1 0.0 0.2 0.2 21 26.0 0.1 0.1 0.4 0.3 1.10 0.07 0.00 0.16 0.08 36.5 0.1 0.0 0.3 0.1 55 25.5 0.1 0.0 0.3 0.3 1.09 0.04 0.01 0.12 0.08 36.4 0.1 0.0 0.2 0.2 88 25.7 0.2 0.0 0.5 0.2 1.06 0.02 0.04 0.11 0.13 36.5 0.1 0.0 0.2 0.2 121 25.4 0.2 0.1 0.5 0.2 1.08 0.03 0.02 0.11 0.10 36.5 0.1 0.0 0.2 0.2 153 25.1 0.1 0.1 0.4 0.4 0.98 0.03 0.04 0.11 0.12 36.3 0.0 0.1 0.2 0.2 184 25.0 0.1 0.0 0.4 0.3 0.92 0.03 0.03 0.10 0.10 36.2 0.1 0.1 0.2 0.2 216 25.3 0.1 0.1 0.3 0.3 0.97 0.03 0.03 0.10 0.10 36.3 0.0 0.1 0.2 0.2 246 25.7 0.2 0.0 0.4 0.2 1.00 0.03 0.02 0.09 0.09 36.3 0.1 0.0 0.2 0.2 276 25.0 0.1 0.0 0.3 0.3 0.91 0.04 0.02 0.11 0.10 36.2 0.1 0.0 0.2 0.2 306 24.8 0.0 0.1 0.3 0.3 0.85 0.03 0.02 0.10 0.09 36.1 0.1 0.0 0.2 0.2 335 25.1 0.1 0.0 0.4 0.3 0.88 0.01 0.05 0.08 0.13 36.3 0.0 0.1 0.2 0.2 364 25.7 0.2 0.1 0.4 0.1 0.91 0.02 0.03 0.09 0.09 36.1 0.1 0.0 0.2 0.1 392 25.3 0.1 0.1 0.3 0.3 0.85 0.04 0.01 0.11 0.08 36.1 0.1 0.0 0.2 0.1 420 25.4 0.1 0.1 0.4 0.3 0.90 0.03 0.03 0.10 0.10 36.1 0.1 0.1 0.2 0.2 448 24.2 0.1 0.1 0.4 0.3 0.70 0.07 0.01 0.14 0.07 35.8 0.1 0.0 0.3 0.1 475 24.2 0.1 0.1 0.4 0.3 0.69 0.04 0.10 0.04 0.18 35.8 0.1 0.2 0.1 0.3 502 23.7 0.1 0.1 0.4 0.4 0.55 0.04 0.02 0.12 0.10 35.5 0.1 0.0 0.2 0.2 529 24.1 0.2 0.0 0.4 0.3 0.70 0.03 0.03 0.11 0.11 35.8 0.1 0.1 0.2 0.2 556 23.9 0.1 0.1 0.3 0.3 0.69 0.05 0.00 0.12 0.07 35.8 0.1 0.0 0.2 0.1 582 24.6 0.1 0.1 0.4 0.3 0.83 0.06 0.00 0.14 0.08 36.0 0.1 0.0 0.3 0.1 608 24.7 0.1 0.1 0.3 0.3 0.80 0.02 0.03 0.09 0.10 36.0 0.0 0.1 0.2 0.2 634 23.9 0.2 0.3 0.1 0.6 0.64 0.03 0.02 0.10 0.10 35.7 0.0 0.0 0.2 0.2 659 23.9 0.0 0.2 0.2 0.4 1.07 0.08 0.03 0.15 0.04 36.4 0.1 0.0 0.2 0.1 685 24.5 0.1 0.1 0.3 0.3 0.95 0.02 0.07 0.05 0.14 36.4 0.1 0.0 0.2 0.2 710 25.1 0.1 0.1 0.3 0.3 0.94 0.02 0.03 0.08 0.09 36.2 0.0 0.0 0.2 0.2 736 25.4 0.2 0.0 0.4 0.2 0.76 0.01 0.04 0.09 0.12 35.9 0.0 0.1 0.2 0.2 761 24.8 0.1 0.1 0.3 0.3 0.87 0.03 0.03 0.10 0.11 36.1 0.0 0.1 0.2 0.2 786 25.3 0.1 0.1 0.3 0.3 0.94 0.02 0.04 0.10 0.11 36.2 0.0 0.1 0.2 0.2 811 24.4 0.1 0.1 0.4 0.3 0.87 0.05 0.01 0.13 0.08 36.1 0.1 0.0 0.2 0.2 836 25.7 0.4 0.2 0.6 0.1 0.85 0.03 0.03 0.12 0.11 36.0 0.1 0.1 0.2 0.2 861 23.4 0.1 0.3 0.3 0.6 0.66 0.05 0.03 0.14 0.12 35.7 0.1 0.1 0.2 0.2 887 24.9 0.2 0.0 0.4 0.2 0.88 0.03 0.03 0.11 0.10 36.1 0.1 0.0 0.2 0.2 912 23.8 0.2 0.1 0.5 0.5 0.88 0.04 0.04 0.16 0.15 36.1 0.1 0.1 0.3 0.3 937 25.3 0.1 0.1 0.5 0.4 1.05 0.04 0.04 0.15 0.14 36.4 0.1 0.1 0.3 0.2 963 25.2 0.1 0.1 0.5 0.4 1.03 0.04 0.04 0.15 0.14 36.4 0.1 0.1 0.3 0.3 989 26.1 0.1 0.1 0.4 0.4 1.31 0.04 0.04 0.14 0.14 36.9 0.1 0.1 0.3 0.3 1014 25.7 0.1 0.1 0.4 0.4 1.19 0.04 0.04 0.15 0.14 36.7 0.1 0.1 0.3 0.3 1040 25.0 0.1 0.1 0.5 0.4 0.98 0.05 0.04 0.15 0.14 36.3 0.1 0.1 0.3 0.3 1067 25.4 0.2 0.1 0.5 0.4 1.00 0.04 0.04 0.15 0.14 36.3 0.1 0.1 0.3 0.3 1093 24.8 0.2 0.1 0.6 0.4 0.96 0.05 0.04 0.15 0.14 36.2 0.1 0.1 0.3 0.3 1119 24.6 0.1 0.1 0.5 0.5 0.87 0.04 0.04 0.15 0.15 36.1 0.1 0.1 0.3 0.3 1146 23.4 0.2 0.1 0.6 0.5 0.74 0.05 0.04 0.16 0.15 35.9 0.1 0.1 0.3 0.3 1173 24.9 0.1 0.1 0.5 0.4 0.93 0.04 0.04 0.15 0.14 36.2 0.1 0.1 0.3 0.3 1201 24.9 0.1 0.1 0.5 0.5 0.89 0.04 0.04 0.15 0.15 36.1 0.1 0.1 0.3 0.3 1229 25.9 0.1 0.1 0.4 0.4 1.13 0.04 0.04 0.14 0.14 36.6 0.1 0.1 0.3 0.2 1257 25.3 0.1 0.1 0.5 0.4 1.07 0.04 0.04 0.14 0.14 36.5 0.1 0.1 0.3 0.2 1286 24.4 0.1 0.1 0.5 0.5 0.75 0.04 0.04 0.16 0.14 35.9 0.1 0.1 0.3 0.3 1315 24.3 0.1 0.1 0.5 0.5 0.83 0.04 0.04 0.15 0.15 36.0 0.1 0.1 0.3 0.3 1344 24.6 0.1 0.1 0.5 0.5 0.88 0.04 0.04 0.15 0.15 36.1 0.1 0.1 0.3 0.3 1374 25.2 0.1 0.1 0.5 0.4 0.96 0.04 0.04 0.15 0.14 36.3 0.1 0.1 0.3 0.3 1404 24.9 0.1 0.1 0.5 0.4 0.96 0.04 0.04 0.15 0.15 36.3 0.1 0.1 0.3 0.3 1435 25.6 0.1 0.1 0.4 0.4 1.13 0.04 0.04 0.14 0.13 36.6 0.1 0.1 0.3 0.3 1465 24.4 0.1 0.1 0.5 0.5 1.18 0.04 0.04 0.15 0.15 36.7 0.1 0.1 0.3 0.3 1497 24.7 0.1 0.1 0.5 0.4 1.42 0.00 0.00 0.00 0.00 37.1 0.0 0.0 0.0 0.0 1529 24.6 0.1 0.1 0.5 0.4 1.12 0.04 0.04 0.15 0.14 36.6 0.1 0.1 0.3 0.3 1561 24.4 0.0 0.0 0.0 0.0 0.97 0.04 0.04 0.15 0.15 36.3 0.1 0.1 0.3 0.3 1594 24.9 0.1 0.1 0.5 0.4 1.01 0.04 0.04 0.15 0.15 36.3 0.1 0.1 0.3 0.3 1627 25.3 0.1 0.1 0.5 0.4 1.07 0.04 0.04 0.14 0.14 36.5 0.1 0.1 0.3 0.3 1661 24.9 0.1 0.1 0.5 0.4 0.90 0.05 0.04 0.15 0.14 36.1 0.1 0.1 0.3 0.3 1695 25.0 0.1 0.1 0.5 0.4 0.94 0.04 0.04 0.15 0.15 36.2 0.1 0.1 0.3 0.3 1730 25.3 0.1 0.1 0.5 0.4 0.82 0.05 0.04 0.15 0.14 36.0 0.1 0.1 0.3 0.3 1765 25.1 0.2 0.1 0.5 0.4 1.01 0.05 0.04 0.15 0.14 36.3 0.1 0.1 0.3 0.3 1801 24.7 0.1 0.1 0.5 0.5 0.80 0.04 0.04 0.14 0.15 36.0 0.1 0.1 0.3 0.3 1837 24.9 0.1 0.1 0.5 0.4 0.91 0.04 0.04 0.15 0.14 36.2 0.1 0.1 0.3 0.3 1873 24.5 0.1 0.1 0.5 0.5 0.98 0.04 0.04 0.14 0.15 36.3 0.1 0.1 0.3 0.3 1911 25.1 0.1 0.1 0.5 0.5 0.87 0.04 0.04 0.15 0.14 36.1 0.1 0.1 0.3 0.3 1948 24.8 0.1 0.1 0.5 0.4 1.11 0.04 0.04 0.15 0.14 36.5 0.1 0.1 0.3 0.3 1987 25.2 0.1 0.1 0.5 0.5 0.76 0.04 0.04 0.14 0.14 35.9 0.1 0.1 0.3 0.3 2026 24.5 0.1 0.1 0.5 0.5 0.98 0.04 0.04 0.15 0.15 36.3 0.1 0.1 0.3 0.3 2066 24.3 0.2 0.1 0.5 0.5 0.78 0.05 0.04 0.15 0.15 35.9 0.1 0.1 0.3 0.3 2106 24.8 0.1 0.1 0.5 0.5 0.88 0.04 0.04 0.14 0.15 36.1 0.1 0.1 0.3 0.3 2147 23.5 0.2 0.1 0.5 0.5 0.52 0.04 0.04 0.16 0.16 35.5 0.1 0.1 0.3 0.3 2189 24.4 0.2 0.1 0.5 0.5 0.48 0.04 0.04 0.15 0.15 35.4 0.1 0.1 0.3 0.3 2231 25.0 0.1 0.1 0.5 0.4 0.73 0.04 0.04 0.15 0.14 35.8 0.1 0.1 0.3 0.3 2274 24.8 0.1 0.1 0.5 0.5 0.94 0.04 0.04 0.15 0.15 36.2 0.1 0.1 0.3 0.3 2317 25.3 0.1 0.1 0.5 0.4 0.96 0.04 0.04 0.14 0.14 36.3 0.1 0.1 0.3 0.3 2361 25.1 0.1 0.1 0.5 0.5 0.79 0.04 0.04 0.15 0.14 35.9 0.1 0.1 0.3 0.3 2405 25.5 0.1 0.1 0.4 0.4 0.89 0.04 0.04 0.14 0.15 36.1 0.1 0.1 0.3 0.3 2450 25.5 0.1 0.1 0.5 0.4 0.97 0.04 0.04 0.15 0.15 36.3 0.1 0.1 0.3 0.3 2495 25.5 0.1 0.1 0.4 0.4 1.12 0.04 0.04 0.14 0.15 36.5 0.1 0.1 0.3 0.3 2540 25.9 0.1 0.1 0.4 0.4 1.08 0.04 0.02 0.13 0.10 36.4 0.1 0.1 0.3 0.3 2586 25.7 0.1 0.1 0.4 0.4 0.90 0.04 0.04 0.15 0.15 36.4 0.1 0.0 0.3 0.2 2632 25.4 0.1 0.1 0.3 0.4 0.88 0.04 0.04 0.14 0.14 36.1 0.1 0.1 0.3 0.3 2679 25.6 0.1 0.1 0.5 0.4 0.86 0.05 0.04 0.15 0.14 36.1 0.1 0.1 0.3 0.3 2726 25.2 0.1 0.1 0.5 0.4 0.95 0.04 0.04 0.15 0.14 36.2 0.1 0.1 0.3 0.3 2773 25.5 0.1 0.1 0.4 0.4 0.79 0.04 0.05 0.15 0.15 36.0 0.1 0.1 0.3 0.3 2821 25.0 0.1 0.1 0.5 0.4 0.78 0.04 0.04 0.15 0.14 35.9 0.1 0.1 0.3 0.3 2869 25.6 0.1 0.1 0.5 0.4 0.70 0.05 0.04 0.15 0.14 35.8 0.1 0.1 0.3 0.3 2917 24.7 0.1 0.1 0.5 0.5 0.58 0.04 0.04 0.15 0.15 35.6 0.1 0.1 0.3 0.3 2965 24.6 0.1 0.1 0.5 0.5 0.78 0.04 0.04 0.15 0.14 35.9 0.1 0.1 0.3 0.3 3014 24.5 0.1 0.1 0.5 0.4 1.08 0.04 0.04 0.15 0.15 36.5 0.1 0.1 0.3 0.3 3062 24.3 0.2 0.1 0.5 0.4 0.70 0.05 0.04 0.15 0.15 35.8 0.1 0.1 0.3 0.3 3112 25.7 0.1 0.1 0.5 0.4 0.98 0.04 0.04 0.14 0.14 36.3 0.1 0.1 0.3 0.3 3161 24.8 0.1 0.1 0.5 0.4 1.01 0.04 0.04 0.15 0.14 36.3 0.1 0.1 0.3 0.3 3210 24.7 0.1 0.1 0.5 0.5 0.84 0.04 0.04 0.15 0.14 36.0 0.1 0.1 0.3 0.3 3259 24.0 0.1 0.1 0.5 0.5 0.77 0.04 0.04 0.15 0.16 35.9 0.1 0.1 0.3 0.3 3309 24.5 0.2 0.1 0.5 0.4 1.04 0.05 0.03 0.16 0.14 36.4 0.1 0.1 0.3 0.2 3359 24.7 0.1 0.1 0.5 0.5 1.08 0.04 0.04 0.16 0.14 36.5 0.1 0.1 0.3 0.3 3410 24.1 0.2 0.1 0.6 0.5 0.75 0.05 0.04 0.16 0.15 35.9 0.1 0.1 0.3 0.3 3460 23.5 0.2 0.1 0.6 0.5 0.78 0.05 0.04 0.16 0.15 35.9 0.1 0.1 0.3 0.3 3510 23.9 0.2 0.1 0.5 0.5 0.73 0.04 0.04 0.15 0.16 35.8 0.1 0.1 0.3 0.3 3561 25.3 0.1 0.1 0.5 0.4 0.88 0.05 0.04 0.15 0.14 36.1 0.1 0.1 0.3 0.3 3611 24.2 0.2 0.1 0.6 0.4 0.76 0.05 0.04 0.16 0.15 35.9 0.1 0.1 0.3 0.3 3661 24.2 0.2 0.1 0.5 0.5 0.66 0.00 0.00 0.00 0.00 35.7 0.1 0.1 0.3 0.3 3712 24.2 0.0 0.0 0.0 0.0 0.75 0.04 0.04 0.15 0.16 36.0 0.0 0.0 0.0 0.0 3762 24.2 0.1 0.1 0.5 0.5 1.13 0.04 0.04 0.15 0.14 36.6 0.1 0.1 0.3 0.3 3812 23.7 0.2 0.1 0.5 0.5 0.62 0.04 0.04 0.15 0.15 35.6 0.1 0.1 0.3 0.3 3862 24.3 0.1 0.1 0.5 0.5 0.93 0.04 0.04 0.15 0.15 36.2 0.1 0.1 0.3 0.3 3912 25.3 0.1 0.1 0.5 0.4 1.16 0.04 0.04 0.14 0.14 36.6 0.1 0.1 0.3 0.3 3962 25.0 0.1 0.1 0.5 0.4 0.95 0.04 0.04 0.14 0.15 36.2 0.1 0.1 0.3 0.3 4011 24.9 0.1 0.1 0.5 0.5 0.93 0.04 0.04 0.14 0.15 36.2 0.1 0.1 0.3 0.3 4061 25.6 0.1 0.1 0.4 0.4 1.06 0.04 0.04 0.14 0.14 36.4 0.1 0.1 0.3 0.3 4110 24.5 0.1 0.1 0.5 0.5 0.85 0.04 0.04 0.15 0.15 36.1 0.1 0.1 0.3 0.3 4159 24.4 0.2 0.1 0.5 0.5 1.01 0.04 0.04 0.15 0.15 36.3 0.1 0.1 0.3 0.3 4209 26.4 0.4 0.4 0.6 0.6 1.19 0.10 0.10 0.18 0.18 36.7 0.2 0.2 0.3 0.3 4258 25.2 0.4 0.4 0.6 0.6 1.10 0.10 0.10 0.18 0.18 36.5 0.2 0.2 0.3 0.3 4305 25.1 0.4 0.4 0.6 0.6 0.93 0.10 0.10 0.18 0.18 36.2 0.2 0.2 0.3 0.3 4353 25.5 0.4 0.4 0.6 0.6 1.11 0.10 0.10 0.18 0.18 36.5 0.2 0.2 0.3 0.3