# Tasman Sea DSDP site 593 Benthic foraminifera B/Ca and Sr/Ca data for the last 1 million years #----------------------------------------------------------------------- # 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/38819 # 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-ocean-38819.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Paleoceanography # # Dataset_DOI: 10.25921/jg1r-rd46 # # Science_Keywords: Last Interglacial, Last Glacial Maximum, Milankovitch, biogeochemical cycles, carbon cycle #--------------------------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/paleocean/pacific/elmore2024/elmore2024-dsdp593.txt # Data_Download_Description: NOAA Template File; DSDP 593 B/Ca, Sr/Ca Data # #--------------------------------------- # Contribution_Date # Date: 2023-12-18 #--------------------------------------- # File_Last_Modified_Date # Date: 2025-04-21 #--------------------------------------- # Title # Study_Name: Tasman Sea DSDP site 593 Benthic foraminifera B/Ca and Sr/Ca data for the last 1 million years #--------------------------------------- # Investigators # Investigators: Elmore, A.C. (https://orcid.org/0000-0002-4977-3771); McClymont, E.L. (https://orcid.org/0000-0003-1562-8768); Kender, S. (https://orcid.org/0000-0003-4216-3214); Greaves, M. (https://orcid.org/0000-0001-8014-8627); Elderfield, H. #--------------------------------------- # Description_Notes_and_Keywords # Description: Reconstruction of intermediate water properties is important for understanding feedbacks within the ocean-climate system. Here we presenttrace metal analyses from the epifaunal benthic foraninifera Planulina wuellerstorfi. B/Ca data is previously published (Elmore et al., 2015 and https://doi.org/10.25921/rt7q-nh82) and compared to Sr/Ca for an assessment of the controls over both ratios (Lawson et al. submitted). # Provided Keywords: Antarctic Intermediate Water, Deep Sea Drilling Program site 593, benthic foraminifera, stable isotopes, Mg/Ca, B/Ca #--------------------------------------- # Publication # Authors: Lawson, Vera J., Yair Rosenthal, Samantha C. Bova, Jonathan Lambert, Braddock K. Linsley, Kaixuan Bu, Vincent J. Clementi, Aurora Elmore, Erin L. McClymont # Published_Date_or_Year: 2024 # Published_Title: Controls on Sr/Ca, S/Ca and Mg/Ca in benthic foraminifera: Implications for the carbonate chemistry of the Pacific Ocean over the last 350 ky # Journal_Name: Geochemistry, Geophysics, Geosystems # Volume: 25 # Edition: # Issue: 8 # Pages: # Report_Number: e2024GC011508 # DOI: 10.1029/2024GC011508 # Online_Resource: # Full_Citation: # Abstract: Boron to calcium (B/Ca) records in benthic foraminifera, used for reconstructing the carbonate ion saturation state (ΔCO3) of the deep ocean, suggest that carbon sequestration in the Southern Pacific contributed to lowering atmospheric CO2 during the last glacial interval. However, the spatial and temporal extent of this storage is debated due to limited ΔCO3 records. To increase available ΔCO3 records, we explored using strontium and sulfur to calcium (Sr/Ca, S/Ca) in Planulina wuellerstorfi as additional proxies for ΔCO3 based on comparison with paired B/Ca down-core records from Pacific Sites U1486 (1,332 m depth) and U1487 (874 m depth) cored during the International Ocean Discovery Program Expedition 363. The Sr/Ca and S/Ca records from P. wuellerstorfi closely covary with the B/Ca-derived ΔCO3 records. Temperature, reconstructed using Uvigerina peregrina magnesium to calcium (Mg/Ca), has no discernible effect on Sr/Ca, whereas S/Ca also varies with Mg/Ca in both U. peregrina and P. wuellerstorfi, suggesting an additional temperature effect. Mg/Ca records from P. wuellerstorfi are affected by both temperature and ΔCO3. We assess calibrations of Sr/Ca to ΔCO3 for the Atlantic, Pacific, and Indian Oceans and recommend using the down-core rather than core-top calibrations as they yield consistent sensitivity, though with offsets, in all ocean basins. Reconstructing Pacific ΔCO3 records from sites U1486, U1487, and DSDP 593, we demonstrate the benefit of using Sr/Ca as an additional ΔCO3 proxy to assess the contribution of the Southern Pacific to the increase of atmospheric CO2 at glacial terminations. #--------------------------------------- # Publication # Authors: Elmore, Aurora C., Erin L. McClymont, Henry Elderfield, Sev Kender, Michael R. Cook, Melanie J. Leng, Mervyn Greaves, and Sambuddha Misra # Published_Date_or_Year: 2015 # Published_Title: Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera # Journal_Name: Earth and Planetary Science Letters # Volume: 428 # Edition: # Issue: # Pages: 193-203 # Report_Number: # DOI: 10.1016/j.epsl.2015.07.013 # Online_Resource: https://doi.org/10.1016/j.epsl.2015.07.013 # Full_Citation: # Abstract: Reconstruction of intermediate water properties is important for understanding feedbacks within the ocean-climate system, particularly since these water masses are capable of driving high–low latitude teleconnections. Nevertheless, information about intermediate water mass evolution through the late Pleistocene remains limited. This paper examines changes in Antarctic Intermediate Water (AAIW), the most extensive intermediate water mass in the modern ocean through the last 400 kyr using the stable isotopic composition (δ18O and δ13C) and trace element concentration (Mg/Ca and B/Ca) of two benthic foraminiferal species from the same samples: epifaunal Planulina wuellerstorfi and infaunal Uvigerina peregrina. Our results confirm that the most reasonable estimates of AAIW temperature and Δ[CO2−3] are generated by Mg/CaU. peregrina and B/CaP. wuellerstorfi, respectively. We present a 400 kyr record of intermediate water temperature and Δ[CO2−3] from a sediment core from the Southwest Pacific (DSDP site 593; 40°30′S, 167°41′E, 1068 m water depth), which lies within the core of modern AAIW. Our results suggest that a combination of geochemical analyses on both infaunal and epifaunal benthic foraminiferal species yields important information about this critical water mass through the late Pleistocene. When combined with two nearby records of water properties from deeper depths, our data demonstrate that during interglacial stages of the late Pleistocene, AAIW and Circumpolar Deep Water (CPDW) have more similar water mass properties (temperature and δ13C), while glacial stages are typified by dissimilar properties between AAIW and CPDW in the Southwest Pacific. Our new Δ[CO2−3] record shows short time-scale variations, but a lack of coherent glacial–interglacial variability indicating that large quantities of carbon were not stored in intermediate waters during recent glacial periods. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Natural Environment Research Council (NERC) # Grant: NE/I027703/1, NE/I024372/1 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: European Research Council # Grant: 2010-NEWLOG ADG-267931 #--------------------------------------- # Site_Information # Site_Name: DSDP 593 # Location: Tasman Sea # Northernmost_Latitude: -40.507833 # Southernmost_Latitude: -40.507833 # Easternmost_Longitude: 167.6745 # Westernmost_Longitude: 167.6745 # Elevation_m: -1068 #--------------------------------------- # Data_Collection # Collection_Name: DSDP593 B/Ca, Sr/Ca Elmore2024 # First_Year: 1053900 # Last_Year: 0 # Time_Unit: calendar year before present # Core_Length_m: 23.04 # Parameter_Keywords: trace metals in carbonates # Notes: #--------------------------------------- # Chronology_Information # Chronology: # Chronology_Notes: Chronology as published in McClymont et al. (2016; doi:10.1002/2016PA002954) and as stated in https://www.ncdc.noaa.gov/paleo/study/18918. Tie points include radiocarbon analysis (14C AMS), alignment to the LR04 oxygen isotope stratigraphy (Lisiecki and Raymo, 2005), or an independently dated New Zealand tephra. # Rejection_Rationale: # Age_Model_Method: # Missing_Values: # Chronology_Table: # depth_end_m age_kaBP1950 date_type reference citation # 0.31 15.9 14C (AMS) Dudley and Nelson (1989) Dudley, W. C., and C. S. Nelson (1989), Quaternary surface-water stable isotope signal from calcareous nannofossils at DSDP Site 593, Southern Tasman Sea, Mar. Micropaleontol., 13, 353–373 # 0.81 88 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 1.8 123 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 2.31 138 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 3.18 186 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 3.86 237 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 4.89 252 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 5.28 295 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 5.6 332 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 5.8 341 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 7.61 370 LR04 Elmore et al. (2015) Elmore, A. C., E. L. McClymont, H. Elderfield, S. Kender, M. R. Cook, M. J. Leng, M. Greaves, and S. Misra (2015), Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera, Earth Planet. Sci. Lett., 428, 193–203. # 8.07 421 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 9.81 491 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 10.31 513 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 10.51 530 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 11.01 584 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 11.12 600 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 12 650 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 12.26 695 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 12.81 706 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 14.9 718 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 15.1 735 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 15.67 766 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 15.88 790 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 16.8 809 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 17.17 831 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 17.7 858 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 18.1 874 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 18.35 907 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 18.56 920 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 19.59 954 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 21.2 987 LR04 Kender et al. (2016) Kender, S., E. L. McClymont, A. C. Elmore, D. Emanuele, M. J. Leng, and H. Elderfield (2016), Mid-Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution, Nat. Commun., 7, 11970, doi:10.1038/ncomms11970 # 21.5 1000 Potaka tephra Shane (1994) Shane, P. A. R. (1994), A widespread, early Pleistocene tephra (Potaka tephra, 1 Ma) in New Zealand: Character, distribution, and implications,N. Z. J. Geol. Geophys., 37(1), 25–35 # 23.5 1070 Base of Jaramillo Cooke et al. (2004) Cooke, P. J., C. S. Nelson, M. P. Crundwell, B. D. Field, E. S. Elkington, and H. H. Stone (2004), Textural variations in Neogene pelagic carbonate ooze at DSDP Site 593, southern Tasman Sea, and their paleoceanographic implications, N. Z. J. Geol. Geophys., 47(4), 787–807. #--------------------------------------- # 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) # ## Top_Depth_MBSF depth at sample end,,,meter,,paleoceanography,,,N,depth at top of sample ## Age_ka age,,,calendar kiloyear before present,,paleoceanography,,,N, ## B/Ca_P.wuell boron/calcium,Cibicidoides wuellerstorfi,,micromole per mole,,paleoceanography,,inductively-coupled plasma mass spectrometry,N,B/Ca data are blank-corrected. We use Planulina wuellerstorfi as the identifer in the associated publications ## Sr/Ca_P.wuell strontium/calcium,Cibicidoides wuellerstorfi,,micromole per mole,,paleoceanography,,inductively-coupled plasma mass spectrometry,N,We use Planulina wuellerstorfi as the identifer in the associated publications ## DSDP_sampleID sample identification,,,,,paleoceanography,,,C,DSDP descriptor for sample (Site&Hole-core number&Section-Coresection; top depth in section. All samples were 2 cm in thickness. #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: NA Top_Depth_MBSF Age_ka B/Ca_P.wuell Sr/Ca_P.wuell DSDP_sampleID 0.07 0 200.1105 1.482772 U0593Z-1H-1 W, 7.0 0.12 3.975 201.8981 1.47142 U0593Z-1H-1 W, 12.0 0.17 7.95 200.9838 1.48648 U0593Z-1H-1 W, 17.0 0.24 11.925 210.9345 1.534558 U0593Z-1H-1 W, 24.0 0.31 15.9 210.023 1.498817 U0593Z-1H-1 W, 31.0 0.34 16.34286 NA 1.516147 U0593Z-1H-1 W, 34.0 0.38 16.78571 211.6057 1.494725 U0593Z-1H-1 W, 38.0 0.42 17.22857 204.9019 1.493573 U0593Z-1H-1 W, 42.0 0.5 18.11429 206.7179 1.492243 U0593Z-1H-1 W, 50.0 0.53 18.55714 201.9063 1.453567 U0593Z-1H-1 W, 53.0 0.59 23 190.299 1.463012 U0593Z-1H-1 W, 59.0 0.62 27 190.9366 1.462498 U0593Z-1H-1 W, 62.0 0.65 31 198.9161 1.478388 U0593Z-1H-1 W, 65.0 0.68 35 199.7427 1.449244 U0593Z-1H-1 W, 68.0 0.71 39 188.4297 1.478197 U0593Z-1H-1 W, 71.0 0.74 43 200.7157 1.487633 U0593Z-1H-1 W, 74.0 0.77 47 187.7341 1.45313 U0593Z-1H-1 W, 77.0 0.81 51 192.8004 1.43619 U0593Z-1H-1 W, 81.0 0.83 55 187.4458 1.455446 U0593Z-1H-1 W, 83.0 0.86 59 198.0563 1.468153 U0593Z-1H-1 W, 86.0 0.9 63 195.8109 1.465123 U0593Z-1H-1 W, 90.0 0.94 67 188.0764 1.446196 U0593Z-1H-1 W, 94.0 0.98 71 191.116 1.471644 U0593Z-1H-1 W, 98.0 1.13 79 200.6751 1.487165 U0593Z-1H-1 W, 113.0 1.24 85 198.6271 1.44966 U0593Z-1H-1 W, 124.0 1.29 87 196.3271 1.466251 U0593Z-1H-1 W, 129.0 1.4 91 188.9967 1.437603 U0593Z-1H-1 W, 140.0 1.55 93 189.2828 1.433799 U0593Z-1H-2 W, 5.0 1.61 95 188.5768 1.423571 U0593Z-1H-2 W, 11.0 1.67 103 188.5345 1.443767 U0593Z-1H-2 W, 17.0 1.78 106 185.754 1.421326 U0593Z-1H-2 W, 28.0 1.89 114 195.9504 1.44848 U0593Z-1H-2 W, 39.0 1.98 120 194.4421 1.443378 U0593Z-1H-2 W, 48.0 2.14 125 184.2409 1.448665 U0593Z-1H-2 W, 64.0 2.22 130 202.321 1.499046 U0593Z-1H-2 W, 72.0 2.38 135 180.3148 1.452282 U0593Z-1H-2 W, 88.0 2.51 143.166 188.9381 1.498526 U0593Z-1H-2 W, 101.0 2.64 151.332 185.9554 1.467474 U0593Z-1H-2 W, 114.0 2.79 159.498 191.2521 1.477407 U0593Z-1H-2 W, 129.0 2.85 167.664 189.8224 1.498988 U0593Z-1H-2 W, 135.0 2.91 174 191.3786 1.46041 U0593Z-1H-2 W, 141.0 3.03 178.8462 182.5949 1.452003 U0593Z-1H-3 W, 3.0 3.1 183.6923 198.0576 1.448896 U0593Z-1H-3 W, 10.0 3.18 188.5385 185.7393 1.425164 U0593Z-1H-3 W, 18.0 3.24 193.3846 189.0998 1.458886 U0593Z-1H-3 W, 24.0 3.27 198.2308 191.6775 1.472986 U0593Z-1H-3W, 27.0 3.31 203.0769 187.3527 1.470177 U0593Z-1H-3 W, 31.0 3.41 207.9231 195.3583 1.489178 U0593Z-1H-3 W, 41.0 3.46 212.7692 198.4501 1.448395 U0593Z-1H-3 W, 46.0 3.51 217.6154 180.6003 1.419222 U0593Z-1H-3 W, 51.0 3.57 222.4615 189.7996 1.446883 U0593Z-1H-3 W, 57.0 3.64 227.6 191.2866 1.475952 U0593Z-1H-3 W, 64.0 3.72 232.2 185.0362 1.440729 U0593Z-1H-3 W, 72.0 3.81 239 175.6495 1.414564 U0593Z-1H-3 W, 81.0 4.04 245.3 176.6224 1.437346 U0593Z-1H-3 W, 104.0 4.28 247.6 191.4947 1.467592 U0593Z-1H-3 W, 128.0 4.67 249 188.9938 1.50372 U0593Z-1H-4 W, 17.0 4.86 251 189.4785 1.481415 U0593Z-1H-4 W, 36.0 4.92 259.25 194.7101 1.490615 U0593Z-1H-4 W, 42.0 5.07 275.75 NA 1.495977 U0593Z-1H-4 W, 57.0 5.1 284 184.8703 1.408157 U0593Z-2H-1 W, 0.0 5.2 289.125 187.3606 1.429413 U0593Z-2H-1 W, 10.0 5.28 299.375 190.5888 1.402447 U0593Z-2H-1 W, 18.0 5.33 304.5 178.0182 1.386652 U0593Z-2H-1 W, 23.0 5.38 309.625 186.9891 1.428229 U0593Z-2H-1 W, 28.0 5.5 319.875 195.7412 1.442264 U0593Z-2H-1 W, 40.0 5.55 325 184.0132 1.421552 U0593Z-2H-1 W, 45.0 5.7 334.2941 188.5958 1.429666 U0593Z-2H-1 W, 60.0 5.91 343.5882 NA 1.415433 U0593Z-2H-1 W, 81.0 6.11 352.8824 188.7441 1.438599 U0593Z-2H-1 W, 101.0 6.26 357.5294 NA 1.4067 U0593Z-2H-1 W, 116.0 6.71 366.8235 185.0513 1.41474 U0593Z-2H-2 W, 11.0 6.77 371.4706 NA 1.435951 U0593Z-2H-2 W, 17.0 7.01 376.1176 NA 1.446874 U0593Z-2H-2 W, 41.0 14.74 715 206.4388 1.492785 U0593Z-3H-1, 4.0 cm 14.9 719.13 193.7344 1.470185 U0593Z-3H-1, 10.0 cm 15.01 727.79 196.2449 1.453735 U0593Z-3H-1, 25.0 cm 15.1 734.86 216.3275 1.456438 U0593Z-3H-1, 31.0 cm 15.16 738.73 189.7444 1.440055 U0593Z-3H-1 W, 43.0- 15.22 741.74 203.8166 1.415765 U0593Z-3H-1 W, 49.0- 15.33 747.27 197.5019 1.441673 U0593Z-3H-1, 58.0 cm 15.45 753.67 202.9932 1.45053 U0593Z-3H-1, 69.0 cm 15.57 761.62 201.6003 1.44723 U0593Z-3H-1, 81.0 cm 15.68 764 216.4962 1.448783 U0593Z-3H-1, 87.0 cm 15.83 776 197.9601 1.486527 U0593Z-3H-1, 108.0 cm 15.93 784 198.6401 1.465048 U0593Z-3H-1, 118.0 cm 15.98 788 208.9617 1.448021 U0593Z-3H-1 W, 123.0 16.04 791.5 191.8933 1.45067 U0593Z-3H-1 W, 131.0 16.09 793 212.5546 1.490081 U0593Z-3H-1, 134.0 cm 16.24 797 201.9488 1.481365 U0593Z-3H-1, 140.0 cm 16.35 801 219.3904 1.438233 U0593Z-3H-2, 10.0 cm 16.4 803 217.8786 1.472705 U0593Z-3H-2 W, 15.0- 16.7 809 196.289 1.457923 U0593Z-3H-2, 40.0 cm 17 818 207.634 1.416552 U0593Z-3H-2, 70.0 cm 17.09 821 194.5561 1.427026 U0593Z-3H-2, 80.0 cm 17.38 842.18 206.7667 1.440361 U0593Z-3H-2, 106.0 cm 17.59 852.64 201.3208 1.461077 U0593Z-3H-2, 130.0 cm 17.68 856.75 204.4769 1.462248 U0593Z-3H-2 W, 139.0 17.8 862.23 199.6872 1.470248 U0593Z-3H-2, 148.0 cm 17.98 869.19 215.5116 1.479927 U0593Z-3H-3, 20.0 cm 18.12 876.57 209.3419 1.490292 U0593Z-3H-3, 36.0 cm 18.17 882.72 196.7398 1.455873 U0593Z-3H-3 W, 45.0- 18.35 904.86 216.4382 1.461414 U0593Z-3H-3, 60.0 cm 18.4 910.55 190.6733 1.463596 U0593Z-3H-3, 65.0 cm 18.46 913.77 203.3761 1.445227 U0593Z-3H-3, 70.0 cm 18.51 916.46 200.0832 1.431799 U0593Z-3H-3, 76.0 cm 18.61 921.82 211.8075 1.423387 U0593Z-3H-3, 86.0 cm 18.78 929.23 203.8052 1.427539 U0593Z-3H-3, 97.0 cm 18.97 935.8 NA 1.423936 U0593Z-3H-3, 118.0 cm 19.18 942.16 214.4392 1.434759 U0593Z-3H-3, 136.0 cm 19.4 948.58 189.8714 1.403641 U0593Z-3H-4, 11.0 cm 19.59 953.97 203.697 1.428255 U0593Z-3H-4, 30.0 cm 19.76 958.24 182.4945 1.371633 U0593Z-3H-4 W, 48.0- 19.9 961.63 198.1 1.407069 U0593Z-3H-4, 56.0 cm 20.11 965.72 197.4716 1.38295 U0593Z-3H-4 W, 81.0- 20.2 967.38 195.8635 1.411105 U0593Z-3H-4, 91.0 cm 20.6 973.59 196.5365 1.404623 U0593Z-3H-4, 128.0 cm 21.39 995.2 210.9977 1.417536 U0593Z-3H-5, 64.0 cm 21.97 1016.5 218.9596 1.501865 U0593Z-3H-5, 69.0 cm 22.5 1035.1 205.5121 1.416634 U0593Z-3H-5, 127.0 cm 22.66 1040.7 198.1389 1.412729 U0593Z-3H-6, 46.0 cm 23.04 1053.9 188.4648 1.384452 U0593Z-3H-6, 84.0 cm