# Central Equatorial Pacific Isotope and Amino Acid Data During the Late 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/38820 # 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-coral-38820.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Corals and Sclerosponges # # Dataset_DOI: 10.25921/3nzr-yg28 # # Science_Keywords: Tropics, Biogeochemical cycles, ENSO, Decadal resolution #--------------------------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/coral/central_pacific/guilderson2024/guilderson2024-kingman-k2-iso.txt # Data_Download_Description: NOAA Template File; Kingman Reef Sample K2 d15N, d13C Data # #--------------------------------------- # Contribution_Date # Date: 2023-12-20 #--------------------------------------- # File_Last_Modified_Date # Date: 2025-04-17 #--------------------------------------- # Title # Study_Name: Central Equatorial Pacific Isotope and Amino Acid Data During the Late Holocene #--------------------------------------- # Investigators # Investigators: Guilderson, Thomas (https://orcid.org/0000-0001-9371-7059); Glynn, Danielle; McCarthy, Matthew #--------------------------------------- # Description_Notes_and_Keywords # Description: water depth approx 400m. #--------------------------------------- # Publication # Authors: Guilderson, T.P., D.S. Glynn, and M.D. McCarthy # Published_Date_or_Year: 2024 # Published_Title: Tropical Decadal Variability in nutrient supply and phytoplankton community in the Central Equatorial Pacific During the Late Holocene. # Journal_Name: Nature Scientific Reports # Volume: 14 # Edition: # Issue: # Pages: # Report_Number: 4161 # DOI: 10.1038/s41598-024-54635-3 # Online_Resource: # Full_Citation: # Abstract: We have reconstructed baseline d15N and d13C of export production at Kingman Reef in the Central Equatorial Pacific (CEP) at sub-decadal resolution, nearly continuously over the last 2000 years. The changes in d15N reflects the strength of the North Equatorial Counter Current (NECC) relative to the South Equatorial Current (SEC), and to a lesser extent, the North Equatorial Current (NEC). Seasonal to multi-decadal variation in the strength of these currents, through the redistribution of heat, have global climate impacts and influence marine and terrestrial ecosystems. We use modern El Niño-La Nina dynamics and Tropical Pacific Decadal Variability (TPDV), which is defined in the CEP, as a framework for analyzing isotopic data. The CEP d15N and d13C records exhibit consistent multi-decadal (50-60 year) TPDV variability. A large multi-centennial feature in the CEP d15N data, within age-model uncertainties, is consistent with one of the prolonged dry-pluvial sequences in the American west at the end of the Medieval Climate Anomaly, where low TPDV is correlated with drier conditions. This unique record shows that the strength of the NECC, as reflected in baseline d15N and d13C, has at quasi-predictable intervals throughout the late Holocene, toggled the phytoplankton community between prokaryotes and picoplankton versus eukaryotes. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: NOAA/National Undersea Research Program # Grant: University of Hawaii's Hawaii Undersea Research Laboratory (HURL) #--------------------------------------- # Funding_Agency # Funding_Agency_Name: National Geographic Society # Grant: CRE 7717-04 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: GRFP 1339067, OCE-0551481 #--------------------------------------- # Site_Information # Site_Name: Kingman Reef # Location: Line Islands, Central Equatorial Pacific # Northernmost_Latitude: 6.38 # Southernmost_Latitude: 6.38 # Easternmost_Longitude: -162.42 # Westernmost_Longitude: -162.42 # Elevation_m: -400 #--------------------------------------- # Data_Collection # Collection_Name: Kingman K2 isotope Guilderson2024 # First_Year: 13 # Last_Year: 922 # Time_Unit: year Common Era # Core_Length_m: # Parameter_Keywords: carbon isotopes, age control, chemistry # Notes: #--------------------------------------- # Chronology_Information # Chronology: Radiocarbon # Chronology_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/templates/noaa-wds-paleo-14c-terms.csv # Chronology_Download_Description: Radiocarbon terms and definitions. # Chronology_Notes: Radiocarbon analyses on acid-pretreated skeletal material at the Center for Accelerator Mass Spectrometry. Fraction modern as per Stuiver and Polach (1977) is equivalent to F14C of Reimer et al. (2004). # Rejection_Rationale: # Reservoir_Method: DELTA_R relative to Marine20 using Zaunbracher et al. (2010) surface coral data # Calibration_Method: Marine20 (Heaton et al. 2020) # Age_Model_Method: Bacon # Missing_Values: # Chronology_Table: # samp_id lab_code frac_mod frac_mod_1s age_14C_BP1950 age_14C_1s_yr depth_mm calib_curve delta_R_yr delta_R_uncert_yr # PV655_GERL_001 CAMS-166975 0.8176 0.0033 1615 35 0.1 Marine20 -134 25 # PV655_GERL_039 CAMS-166976 0.8196 0.0031 1600 35 3.9 Marine20 -134 25 # PV655_GERL_076 CAMS-166977 0.7896 0.0037 1900 40 7.6 Marine20 -134 25 # PV655_GERL_114 CAMS-166978 0.7834 0.0035 1960 40 11.4 Marine20 -134 25 # PV655_GERL_172 CAMS-166979 0.762 0.0028 2195 30 17.2 Marine20 -134 25 # PV655_GERL_210 CAMS-166980 0.7568 0.0033 2240 35 21.0 Marine20 -134 25 #--------------------------------------- # 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) # ## SampleID sample identification,,,,,corals and sclerosponges,,,C, ## depth_mm depth,,,millimeter,,corals and sclerosponges,,,N,Radial distance edge; computerized micromill ## year_CE age,,,year Common Era,,corals and sclerosponges,,,N,Common Era Age estimate; BACON output ## year_BP age,,,calendar year before present,,corals and sclerosponges,,,N,Years BP Age estimate; BACON output ## year_BP-95%CI age,,95% confidence interval margin of error,calendar year before present,,corals and sclerosponges,,,N,Age estimate uncertainty 95% Confidence Interval; BACON output ## C/N carbon/nitrogen,Kulamanamana sp.,,atomic ratio,,corals and sclerosponges,,elemental analysis; isotope ratio mass spectrometry,N,precision: 0.2 ## d15N-Kula.sp delta 15N,Kulamanamana sp.,,per mil AIR,,corals and sclerosponges,,elemental analysis; isotope ratio mass spectrometry,N,Bulk skeletal nitrogen isotope data; precision <0.1 per mil ## d13C-Kula.sp delta 13C,Kulamanamana sp.,,per mil VPDB,,corals and sclerosponges,,elemental analysis; isotope ratio mass spectrometry,N,Bulk skeletal carbon isotope data; precision <0.1 per mil #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: NA SampleID depth_mm year_CE year_BP year_BP-95%CI C/N d15N-Kula.sp d13C-Kula.sp PV 655 GERL 1 0.1 922 1028 126 3.30 17.01 -14.65 PV 655 GERL 2 0.2 917 1033 125 3.03 17.70 -14.49 PV 655 GERL 3 0.3 913 1037 124 3.00 17.70 -14.69 PV 655 GERL 4 0.4 909 1041 123 2.99 17.41 -14.73 PV 655 GERL 5 0.5 904 1046 123 3.06 17.37 -14.94 PV 655 GERL 6 0.6 900 1050 123 3.00 17.71 -14.84 PV 655 GERL 7 0.7 896 1054 122 2.95 17.78 -14.94 PV 655 GERL 8 0.8 891 1059 121 3.02 17.75 -14.91 PV 655 GERL 9 0.9 887 1063 120 2.96 17.92 -14.87 PV 655 GERL 10 1 883 1067 120 2.95 17.69 -15.16 PV 655 GERL 11 1.1 879 1071 120 2.88 17.63 -15.21 PV 655 GERL 12 1.2 875 1075 119 2.91 17.49 -15.05 PV 655 GERL 13 1.3 870 1080 118 2.90 17.63 -15.11 PV 655 GERL 14 1.4 866 1084 118 2.92 17.73 -15.17 PV 655 GERL 15 1.5 862 1088 119 2.93 17.66 -15.18 PV 655 GERL 16 1.6 858 1092 119 2.89 17.87 -15.35 PV 655 GERL 17 1.7 854 1096 117 2.93 NA NA PV 655 GERL 18 1.8 849 1101 117 2.89 18.01 -15.25 PV 655 GERL 19 1.9 845 1105 116 2.88 18.04 -15.12 PV 655 GERL 20 2 841 1109 116 2.90 18.01 -15.22 PV 655 GERL 21 2.1 837 1113 117 2.86 17.90 -15.50 PV 655 GERL 22 2.2 832 1118 115 2.91 17.78 -15.34 PV 655 GERL 23 2.3 828 1122 114 2.90 17.83 -15.37 PV 655 GERL 24 2.4 824 1126 114 2.89 17.85 -15.69 PV 655 GERL 25 2.5 819 1131 114 2.92 17.81 -15.64 PV 655 GERL 26 2.6 815 1135 114 2.88 17.81 -15.48 PV 655 GERL 27 2.7 811 1139 112 2.86 17.80 -15.56 PV 655 GERL 28 2.8 807 1143 111 2.85 17.71 -15.59 PV 655 GERL 29 2.9 802 1148 111 2.87 17.58 -15.60 PV 655 GERL 30 3 798 1152 111 2.91 17.73 -15.44 PV 655 GERL 31 3.1 794 1156 112 2.88 17.41 -15.31 PV 655 GERL 32 3.2 790 1160 110 2.89 17.27 -15.44 PV 655 GERL 33 3.3 785 1165 109 2.90 17.18 -15.35 PV 655 GERL 34 3.4 781 1169 108 2.92 17.61 -15.38 PV 655 GERL 35 3.5 777 1173 108 2.83 17.18 -15.52 PV 655 GERL 36 3.6 773 1177 108 2.88 18.10 -15.55 PV 655 GERL 37 3.7 768 1182 106 2.97 17.98 -15.24 PV 655 GERL 38 3.8 764 1186 105 2.91 18.26 -15.16 PV 655 GERL 39 3.9 760 1190 105 2.90 17.78 -15.29 PV 655 GERL 40 4 755 1195 105 2.91 NA NA PV 655 GERL 41 4.1 751 1199 105 2.93 17.58 -15.52 PV 655 GERL 42 4.2 746 1204 105 2.95 17.39 -15.29 PV 655 GERL 43 4.3 741 1209 105 2.99 17.25 -15.32 PV 655 GERL 44 4.4 737 1213 104 2.88 17.38 -15.35 PV 655 GERL 45 4.5 732 1218 105 2.88 17.33 -15.27 PV 655 GERL 46 4.6 728 1222 106 2.92 NA NA PV 655 GERL 47 4.7 723 1227 105 2.88 NA NA PV 655 GERL 48 4.8 718 1232 105 2.93 17.44 -15.15 PV 655 GERL 49 4.9 714 1236 105 2.96 17.51 -15.25 PV 655 GERL 50 5 709 1241 106 2.93 17.42 -15.28 PV 655 GERL 51 5.1 704 1246 107 2.87 17.03 -15.19 PV 655 GERL 52 5.2 700 1250 106 2.87 17.29 -15.33 PV 655 GERL 53 5.3 695 1255 105 2.87 17.16 -15.26 PV 655 GERL 54 5.4 690 1260 105 2.86 17.39 -15.35 PV 655 GERL 55 5.5 686 1264 105 2.87 17.30 -15.40 PV 655 GERL 56 5.6 681 1269 106 2.81 17.58 -15.49 PV 655 GERL 57 5.7 676 1274 104 2.89 17.78 -15.24 PV 655 GERL 58 5.8 672 1278 104 2.87 17.41 -15.23 PV 655 GERL 59 5.9 667 1283 103 2.85 17.71 -15.29 PV 655 GERL 60 6 662 1288 103 2.86 17.69 -15.10 PV 655 GERL 61 6.1 658 1292 105 2.86 17.86 -15.29 PV 655 GERL 62 6.2 653 1297 103 2.85 17.88 -15.33 PV 655 GERL 63 6.3 649 1301 102 2.84 17.74 -15.42 PV 655 GERL 64 6.4 644 1306 102 2.82 17.58 -15.42 PV 655 GERL 65 6.5 639 1311 102 2.82 17.75 -15.55 PV 655 GERL 66 6.6 635 1315 103 2.82 17.47 -15.60 PV 655 GERL 67 6.7 630 1320 102 2.81 17.15 -15.40 PV 655 GERL 68 6.8 626 1324 101 2.83 17.55 -15.59 PV 655 GERL 69 6.9 621 1329 100 2.83 17.68 -15.53 PV 655 GERL 70 7 616 1334 101 2.85 17.69 -15.60 PV 655 GERL 71 7.1 612 1338 101 2.84 17.38 -15.45 PV 655 GERL 72 7.2 607 1343 100 2.85 17.49 -15.34 PV 655 GERL 73 7.3 602 1348 98 2.83 17.26 -15.50 PV 655 GERL 74 7.4 598 1352 97 2.81 17.02 -15.54 PV 655 GERL 75 7.5 593 1357 98 2.82 16.96 -15.68 PV 655 GERL 76 7.6 588 1362 98 2.85 16.96 -15.52 PV 655 GERL 77 7.7 584 1366 98 2.85 16.67 -15.62 PV 655 GERL 78 7.8 580 1370 98 2.86 16.80 -15.65 PV 655 GERL 79 7.9 576 1374 98 2.85 16.57 -15.56 PV 655 GERL 80 8 571 1379 99 2.85 16.77 -15.59 PV 655 GERL 81 8.1 567 1383 100 2.79 16.73 -15.48 PV 655 GERL 82 8.2 563 1387 100 2.83 16.98 -15.57 PV 655 GERL 83 8.3 559 1391 100 2.80 17.11 -15.49 PV 655 GERL 84 8.4 555 1395 100 2.84 17.41 -15.45 PV 655 GERL 85 8.5 551 1399 101 2.80 17.29 -15.45 PV 655 GERL 86 8.6 546 1404 103 2.79 17.13 -15.41 PV 655 GERL 87 8.7 542 1408 102 2.83 17.29 -15.58 PV 655 GERL 88 8.8 538 1412 101 2.81 17.42 -15.73 PV 655 GERL 89 8.9 534 1416 101 2.82 17.29 -15.58 PV 655 GERL 90 9 530 1420 101 2.86 17.48 -15.61 PV 655 GERL 91 9.1 526 1424 103 2.84 17.10 -15.79 PV 655 GERL 92 9.2 522 1428 102 2.83 17.15 -15.72 PV 655 GERL 93 9.3 518 1432 101 2.84 16.96 -15.70 PV 655 GERL 94 9.4 514 1436 102 2.82 17.37 -15.73 PV 655 GERL 95 9.5 509 1441 103 2.80 17.29 -15.57 PV 655 GERL 96 9.6 505 1445 104 2.82 17.09 -15.48 PV 655 GERL 97 9.7 501 1449 103 2.84 17.30 -15.62 PV 655 GERL 98 9.8 497 1453 104 2.80 17.18 -15.56 PV 655 GERL 99 9.9 493 1457 104 2.78 17.29 -15.76 PV 655 GERL 100 10 489 1461 104 2.78 17.42 -15.51 PV 655 GERL 101 10.1 485 1465 105 2.79 17.26 -15.68 PV 655 GERL 102 10.2 481 1469 105 2.78 17.02 -15.76 PV 655 GERL 103 10.3 477 1473 105 2.79 17.24 -15.65 PV 655 GERL 104 10.4 473 1477 105 2.80 17.07 -15.78 PV 655 GERL 105 10.5 469 1481 105 2.77 17.05 -15.74 PV 655 GERL 106 10.6 464 1486 106 2.80 16.90 -15.98 PV 655 GERL 107 10.7 460 1490 105 2.80 16.93 -15.77 PV 655 GERL 108 10.8 456 1494 104 2.81 16.83 -15.67 PV 655 GERL 109 10.9 452 1498 103 2.81 17.00 -15.88 PV 655 GERL 110 11 448 1502 104 2.83 17.06 -15.62 PV 655 GERL 111 11.1 443 1507 105 2.83 16.99 -15.89 PV 655 GERL 112 11.2 439 1511 104 2.84 16.74 -15.89 PV 655 GERL 113 11.3 435 1515 104 2.86 16.85 -15.88 PV 655 GERL 114 11.4 431 1519 104 2.81 16.68 -15.95 PV 655 GERL 115 11.5 426 1524 105 2.81 16.78 -15.92 PV 655 GERL 116 11.6 422 1528 105 2.84 16.70 -15.85 PV 655 GERL 117 11.7 418 1532 105 2.78 16.71 -15.96 PV 655 GERL 118 11.8 414 1536 106 2.78 16.70 -15.98 PV 655 GERL 119 11.9 409 1541 106 2.93 16.83 -16.11 PV 655 GERL 120 12 405 1545 107 2.92 16.67 -15.97 PV 655 GERL 121 12.1 401 1549 107 2.90 16.65 -16.03 PV 655 GERL 122 12.2 396 1554 107 2.85 16.61 -16.13 PV 655 GERL 123 12.3 392 1558 107 2.92 16.70 -15.96 PV 655 GERL 124 12.4 388 1562 108 2.93 16.73 -16.02 PV 655 GERL 125 12.5 383 1567 108 2.92 16.85 -15.86 PV 655 GERL 126 12.6 379 1571 110 2.93 16.91 -16.02 PV 655 GERL 127 12.7 375 1575 110 2.95 16.70 -15.93 PV 655 GERL 128 12.8 370 1580 110 2.92 16.96 -15.89 PV 655 GERL 129 12.9 366 1584 110 2.94 17.09 NA PV 655 GERL 130 13 362 1588 110 2.93 NA NA PV 655 GERL 131 13.1 357 1593 111 2.94 17.23 -15.82 PV 655 GERL 132 13.2 353 1597 111 2.92 17.03 -16.06 PV 655 GERL 133 13.3 349 1601 111 2.99 17.01 -15.97 PV 655 GERL 134 13.4 345 1605 111 2.91 17.24 -15.96 PV 655 GERL 135 13.5 340 1610 112 2.90 17.15 -15.86 PV 655 GERL 136 13.6 336 1614 113 2.85 17.05 -15.92 PV 655 GERL 137 13.7 332 1618 112 2.83 16.97 -15.95 PV 655 GERL 138 13.8 327 1623 111 2.88 17.02 -16.04 PV 655 GERL 139 13.9 323 1627 111 2.89 16.79 -16.03 PV 655 GERL 140 14 319 1631 112 2.87 16.83 -16.07 PV 655 GERL 141 14.1 314 1636 113 2.86 16.75 -16.13 PV 655 GERL 142 14.2 310 1640 113 2.90 16.74 -15.84 PV 655 GERL 143 14.3 306 1644 113 2.88 16.98 -16.06 PV 655 GERL 144 14.4 301 1649 113 2.91 16.82 -15.93 PV 655 GERL 145 14.5 297 1653 114 2.92 16.84 -15.99 PV 655 GERL 146 14.6 293 1657 116 2.90 16.95 -15.81 PV 655 GERL 147 14.7 288 1662 115 2.90 16.79 -16.04 PV 655 GERL 148 14.8 284 1666 114 2.87 16.83 -15.88 PV 655 GERL 149 14.9 280 1670 114 2.87 16.67 -15.94 PV 655 GERL 150 15 275 1675 115 2.85 16.77 -15.95 PV 655 GERL 151 15.1 271 1679 115 2.86 16.38 -15.92 PV 655 GERL 152 15.2 266 1684 115 2.85 16.52 -16.17 PV 655 GERL 153 15.3 262 1688 115 2.86 16.71 -16.14 PV 655 GERL 154 15.4 258 1692 115 2.86 17.08 -16.17 PV 655 GERL 155 15.5 254 1696 115 2.86 16.76 -16.12 PV 655 GERL 156 15.6 249 1701 116 2.86 17.03 -16.14 PV 655 GERL 157 15.7 245 1705 116 2.81 17.06 -16.11 PV 655 GERL 158 15.8 241 1709 116 2.86 16.98 -16.14 PV 655 GERL 159 15.9 237 1713 117 2.86 16.74 -16.04 PV 655 GERL 160 16 232 1718 117 2.84 16.84 -16.13 PV 655 GERL 161 16.1 228 1722 118 2.86 16.50 -16.04 PV 655 GERL 162 16.2 224 1726 117 2.84 16.55 -16.16 PV 655 GERL 163 16.3 219 1731 117 2.84 16.36 -15.96 PV 655 GERL 164 16.4 215 1735 118 2.86 16.22 -16.18 PV 655 GERL 165 16.5 210 1740 118 2.84 16.16 -16.28 PV 655 GERL 166 16.6 206 1744 120 2.82 16.50 -16.14 PV 655 GERL 167 16.7 202 1748 119 2.83 16.53 -16.26 PV 655 GERL 168 16.8 197 1753 119 2.84 16.39 -16.34 PV 655 GERL 169 16.9 193 1757 119 2.83 NA NA PV 655 GERL 170 17 189 1761 119 2.83 16.33 -16.35 PV 655 GERL 171 17.1 184 1766 120 2.85 16.68 -16.33 PV 655 GERL 172 17.2 180 1770 120 2.85 16.49 -16.35 PV 655 GERL 173 17.3 176 1774 120 2.84 16.37 NA PV 655 GERL 174 17.4 171 1779 120 2.83 16.59 -15.94 PV 655 GERL 175 17.5 167 1783 121 2.83 16.53 -16.23 PV 655 GERL 176 17.6 163 1787 122 2.83 16.34 -16.10 PV 655 GERL 177 17.7 158 1792 122 2.80 16.45 -16.31 PV 655 GERL 178 17.8 154 1796 122 2.64 16.89 -16.37 PV 655 GERL 179 17.9 150 1800 123 2.80 16.64 -16.32 PV 655 GERL 180 18 145 1805 124 2.82 16.56 -16.27 PV 655 GERL 181 18.1 141 1809 124 2.79 16.76 -16.30 PV 655 GERL 182 18.2 137 1813 125 2.66 16.66 -16.33 PV 655 GERL 183 18.3 132 1818 125 2.75 16.69 -16.22 PV 655 GERL 184 18.4 128 1822 125 2.72 16.62 -16.31 PV 655 GERL 185 18.5 124 1826 126 2.75 16.52 -16.32 PV 655 GERL 186 18.6 119 1831 128 2.75 16.40 -16.32 PV 655 GERL 187 18.7 115 1835 128 2.73 16.61 -16.32 PV 655 GERL 188 18.8 110 1840 129 2.74 16.63 -16.39 PV 655 GERL 189 18.9 106 1844 129 2.74 16.61 -16.31 PV 655 GERL 190 19 102 1848 129 2.74 16.57 -16.27 PV 655 GERL 191 19.1 97 1853 131 2.74 16.52 -16.26 PV 655 GERL 192 19.2 93 1857 130 2.76 16.49 -16.34 PV 655 GERL 193 19.3 88 1862 131 2.75 16.31 -16.25 PV 655 GERL 194 19.4 84 1866 131 2.75 16.31 -16.28 PV 655 GERL 195 19.5 79 1871 132 2.73 16.15 -16.26 PV 655 GERL 196 19.6 75 1875 133 2.76 15.79 -16.21 PV 655 GERL 197 19.7 71 1879 133 2.73 15.93 -16.08 PV 655 GERL 198 19.8 66 1884 133 2.72 15.86 -16.06 PV 655 GERL 199 19.9 62 1888 134 2.72 16.25 -16.20 PV 655 GERL 200 20 58 1892 134 2.71 16.49 -16.28 PV 655 GERL 201 20.1 53 1897 135 2.75 16.41 -16.34 PV 655 GERL 202 20.2 49 1901 134 2.72 16.34 -16.21 PV 655 GERL 203 20.3 44 1906 135 2.73 16.55 -16.26 PV 655 GERL 204 20.4 40 1910 135 2.72 16.20 -16.15 PV 655 GERL 205 20.5 36 1914 137 2.72 16.73 -16.19 PV 655 GERL 206 20.6 31 1919 138 2.71 16.62 -16.24 PV 655 GERL 207 20.7 27 1923 138 2.69 16.56 -16.20 PV 655 GERL 208 20.8 22 1928 138 2.70 16.47 -16.16 PV 655 GERL 209 20.9 18 1932 138 2.65 16.52 -16.26 PV 655 GERL 210 21 13 1937 140 2.66 16.90 -16.21