# Central Great Barrier Reef, Porites spp. trace metals 1983-1998 CE #----------------------------------------------------------------------- # 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/39021 # 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-39021.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/p7g3-qc81 # # Science_Keywords: #--------------------------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/coral/west_pacific/great_barrier/fallon2003/fallon2003-orpheus-metals.txt # Data_Download_Description: NOAA Template File; Orpheus Trace Metals Data # #--------------------------------------- # Contribution_Date # Date: 2024-02-12 #--------------------------------------- # File_Last_Modified_Date # Date: 2025-06-30 #--------------------------------------- # Title # Study_Name: Central Great Barrier Reef, Porites spp. trace metals 1983-1998 CE #--------------------------------------- # Investigators # Investigators: Fallon, S.J. (https://orcid.org/0000-0002-8064-5903); McCulloch, M.T. (https://orcid.org/0000-0003-1538-1558); Alibert, C. (https://orcid.org/0000-0002-9113-7365) #--------------------------------------- # Description_Notes_and_Keywords # Description: Contributed as part of the Great Barrier Reef Coral Skeletal Records Database (GBRCD). # Provided Keywords: Great Barrier Reef, Coral Geochemistry, Sea Surface Temperature, LA-ICP-MS #--------------------------------------- # Publication # Authors: Fallon, S.J., McCulloch, M.T., Alibert, C. # Published_Date_or_Year: 2003 # Published_Title: Examining water temperature proxies in Porites corals from the Great Barrier Reef: a cross-shelf comparison # Journal_Name: Coral Reefs # Volume: 22 # Edition: # Issue: 4 # Pages: 389–404 # Report_Number: # DOI: 10.1007/s00338-003-0322-5 # Online_Resource: # Full_Citation: # Abstract: Cores from colonies of the coral species Porites sp. were collected from inshore, mid-shelf, and outer reef localities (central Great Barrier Reef) to test the robustness of the major elemental sea surface temperature (SST) proxies (B/Ca, Mg/Ca, Sr/Ca, U/Ca) to the influence of inshore processes. Time series analyses of Sr/Ca, U/Ca, B/Ca, and Mg/Ca are compared to sea surface temperature (SST) in order to provide calibrations for these elements. This study shows that there are significant variations between the corals with respect to some of the proxies. In some cases, variations of ~6 °C are observed for a single U/Ca value. This magnitude of variation is also seen in the Mg/Ca proxy and, to a smaller extent, in the B/Ca–SST relationship. In two of the corals, both Mg/Ca and U/Ca do not follow a seasonal signal. The Mg/Ca and U/Ca ratios for two inshore corals are significantly different than the offshore corals (lower and higher, respectively). The other two proxies (B/Ca and Sr/Ca) do not display any inshore vs. offshore variations except for one inshore site that did not have a clear seasonal signal for either of these proxies. The Sr/Ca–SST relationship is the most robust, with a temperature variation of ~2 °C for a single Sr/Ca value, which is within error for this technique. #--------------------------------------- # Publication # Authors: Fallon, S.J. # Published_Date_or_Year: 2000 # Published_Title: Environmental Records from Corals and Coralline Sponges # Journal_Name: # Volume: # Edition: # Issue: # Pages: # Report_Number: # DOI: 10.25911/5d778a502c764 # Online_Resource: # Full_Citation: Fallon, S.J. (2000), ‘Environmental Records from Corals and Coralline Sponges’, PhD Thesis, Australian National University, https://doi.org/10.25911/5d778a502c764. # Abstract: This research centers on the extraction of environmental information stored in the calcium carbonate skeletons of corals (Porites) and coralline sponges (Astrosclera willeyana). Elemental variations are measured in these samples using laser ablation inductively coupled plasma mass spectrometry. During this project, techniques were refined and developed to quantitatively measure major (B, Mg, Sr, Ba, U) and minor (Mn, Zn, Pb, REE’s) elemental abundances in corals and coralline sponges. This method was used to extract seasonal records from a high latitude coral living at its limits of cold-water tolerance in Japan. Seasonal cycles of major elements (B, Mg, Sr, U) were calibrated against in situ instrumental temperature monitors. Calibrations were in good agreement with other published reports. This coral also recorded wind-induced upwelling (both annual and El Nin~o related) by increases in the Ba/Ca ratio. The trace element annual patterns and slow growth rate also indicated that this coral had very slow/no extension during the cold winter months when water temperature was below 18 oC. Cores from Porites sp. coral colonies were also collected from inshore, mid-shelf and outer reef localities (central Great Barrier Reef) to test the robustness of the major elemental SST and runoff proxies (B/Ca, Mg/Ca, Sr/Ca, Ba/Ca, U/Ca). The inshore reefs selected for this study are heavily influenced by river runoff whereas the mid-reef and outer-reef locations are not. It is shown that Ba/Ca provides an excellent proxy for river runoff. Time series analyses of Sr/Ca, U/Ca, B/Ca and Mg/Ca are compared to in situ sea surface temperature (SST) and/or IGOSS NMC weekly satellite SST to provide calibrations for these elements. Previous workers have noted differences in the calibration of Sr/Ca vs. SST; this LA-ICP-MS dataset shows a slight variation between different corals. This suggests small-scale intra- coral variability. Both the U/Ca and Mg/Ca have calibrations within error for mid-shelf and outer reef corals but the calibrations differ for the inshore corals. Sr/Ca and B/Ca appear to be the most robust of the elemental temperature proxies in terms of recording water temperature. Measurements of coral manganese suggest a seasonal cycle closely linked to solar radiation and wind. Increased solar radiation may increase the dissolved seawater Mn that result in corals having elevated concentrations of Mn during the summer. The use of corals as recorders of marine pollution was examined on the island of Misima in Papua New Guinea where open-cut gold mining commenced in 1989. This mining caused increased sedimentation affecting the nearby fringing coral reef to varying degrees, causing coral mortality (complete suffocation) in some areas. This sediment is made up of completely weathered quartz feldspar, greenstone and schist. These rocks have distinct chemical constituents (rare earth elements [REE], zinc and lead etc.), which are entering the near-shore environment in considerably higher than normal concentrations. Eight coral colonies (2 from high sedimentation, 2 transitional, 2 minor and 2 unaffected control sites) were analyzed for Mn, Y, La, Ce, Zn and Pb. All sites show low steady “background” levels prior to the commencement of mining. After mine construction began in 1988, all sites aside from the control show dramatic increases of Mn, Y, La, and Ce associated with the increased sedimentation. Zn and Pb increase after 1989 when ore processing began. The concentration of these elements in these corals decreases as the distance from the mine increases. Rare earth elements (REE) measured in two corals suggest a pattern different from “normal” seawater. When the coral REE pattern is compared to seawater an enrichment of the light and middle REE’s appear. The heavy REE’s are depleted relative to the seawater pattern. This suggests the nearshore seawater REE’s are influenced by island weathering. Coralline sponges have been proposed as a new source of tropical paleoclimatic information. Profiles of d13C in coralline sponges have documented (better and more accurately than corals) the atmospheric increase of Due to their very slow growth rates ~0.2 mm yr-1 sponges are better suited to recording and providing long-term environmental information rather than annual information. These sponges appear to smooth the record stored in their skeleton by adding secondary aragonite near the base of the living tissue layer. This smoothing limits their use as annual environmental recorders but still enables their use for decadal or longer environmental fluctuations. Smoothed records of Sr/Ca from five sponges around the Southwest Pacific C associated with increased fossil fuel consumption. suggest that these sponges are able to capture 5 yr. and longer seawater temperature anomalies over the past 50-200 years. The temperature sensitivity of Sr/Ca in sponges is 7 to 12 times larger than corals with ~0.7-0.9 mmol/mol DSr/Ca per oC for sponges compared to ~0.07 mmol/mol DSr/Ca per oC for corals. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Australian National University # Grant: #--------------------------------------- # Site_Information # Site_Name: Orpheus Island # Location: Great Barrier Reef, Australia # Northernmost_Latitude: -18.65 # Southernmost_Latitude: -18.65 # Easternmost_Longitude: 146.49 # Westernmost_Longitude: 146.49 # Elevation_m: -2.5 #--------------------------------------- # Data_Collection # Collection_Name: Orpheus trace metals Fallon2003 # First_Year: 1988 # Last_Year: 1992 # Time_Unit: year Common Era # Core_Length_m: # Parameter_Keywords: trace metals # Notes: Porites sp. #--------------------------------------- # Chronology_Information # Chronology: #--------------------------------------- # 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) # ## Distance depth,,,millimeter,,corals and sclerosponges,,,N,Distance from top of coral ## age_CE age,,,year Common Era,,corals and sclerosponges,,,N, ## B/Ca Boron/Calcium,Porites sp.,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## Mg/Ca Magnesium/Calcium,Porites sp.,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## Sr/Ca Strontium/Calcium,Porites sp.,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## Ba/Ca Barium/Calcium,Porites sp.,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## U/Ca Uranium/Calcium,Porites sp.,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## Mn Manganese,Porites sp.,,microgram per gram,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: NA Distance age_CE B/Ca Mg/Ca Sr/Ca Ba/Ca U/Ca Mn 0.00 1992.43 0.0003750 0.003756 0.009061 0.000005763 0.0000012520 0.346 0.30 1992.38 0.0003946 0.004563 0.008846 0.000005199 0.0000010070 0.347 0.59 1992.35 0.0003984 0.004475 0.008739 0.000005052 0.0000010580 0.312 0.89 1992.33 0.0004049 0.004020 0.008935 0.000004740 0.0000011200 0.326 1.18 1992.31 0.0004062 0.003867 0.008867 0.000004307 0.0000011190 0.279 1.48 1992.29 0.0003990 0.004211 0.008938 0.000005162 0.0000010800 0.303 1.77 1992.27 0.0003989 0.004150 0.008898 0.000006197 0.0000010600 0.313 2.07 1992.24 0.0003919 0.004395 0.008907 0.000007892 0.0000010350 0.324 2.36 1992.22 0.0003973 0.004207 0.008846 0.000005814 0.0000010900 0.326 2.66 1992.2 0.0003889 0.004299 0.008802 0.000004833 0.0000010580 0.368 2.95 1992.18 0.0003778 0.003902 0.008819 0.000005072 0.0000011080 0.400 3.25 1992.15 0.0003951 0.004123 0.008872 0.000005486 0.0000010660 0.373 3.54 1992.13 0.0004104 0.004361 0.008734 0.000004108 0.0000009223 0.318 3.84 1992.1 0.0004457 0.004270 0.008784 0.000005452 0.0000009956 0.378 4.13 1992.08 0.0004302 0.004022 0.008719 0.000006222 0.0000009903 0.374 4.43 1992.05 0.0004582 0.004160 0.008869 0.000006913 0.0000009893 0.300 4.72 1992.02 0.0004679 0.004527 0.008750 0.000008166 0.0000009457 0.286 5.02 1991.99 0.0004512 0.004529 0.008779 0.000007055 0.0000009583 0.285 5.32 1991.96 0.0004536 0.004485 0.008817 0.000006674 0.0000010100 0.273 5.61 1991.94 0.0004281 0.004230 0.008746 0.000006139 0.0000010350 0.269 5.91 1991.91 0.0004100 0.004033 0.008867 0.000006353 0.0000010550 0.245 6.20 1991.88 0.0004100 0.003996 0.008678 0.000005128 0.0000010720 0.216 6.50 1991.85 0.0004119 0.003937 0.008757 0.000004944 0.0000010930 0.219 6.79 1991.82 0.0004152 0.003873 0.008811 0.000005152 0.0000011060 0.232 7.09 1991.8 0.0004331 0.003609 0.008848 0.000004895 0.0000011700 0.310 7.38 1991.77 0.0004438 0.003629 0.008895 0.000004632 0.0000011770 0.353 7.68 1991.74 0.0004551 0.003668 0.008988 0.000004172 0.0000011600 0.218 7.97 1991.71 0.0004665 0.003676 0.008962 0.000003785 0.0000012020 0.210 8.27 1991.68 0.0004563 0.003771 0.008925 0.000003163 0.0000011360 0.216 8.56 1991.65 0.0004668 0.003849 0.008881 0.000002877 0.0000011150 0.220 8.86 1991.62 0.0004701 0.003687 0.008992 0.000002897 0.0000011900 0.197 9.15 1991.59 0.0004813 0.003748 0.008965 0.000003191 0.0000011940 0.190 9.45 1991.56 0.0004825 0.003766 0.008932 0.000003227 0.0000011620 0.174 9.75 1991.52 0.0004661 0.003803 0.008908 0.000003497 0.0000011150 0.176 10.04 1991.49 0.0004562 0.003756 0.008982 0.000003999 0.0000011780 0.183 10.34 1991.46 0.0004632 0.003681 0.008979 0.000004106 0.0000012020 0.200 10.63 1991.44 0.0004603 0.003601 0.008946 0.000004045 0.0000011640 0.223 10.93 1991.42 0.0004640 0.003615 0.009005 0.000003208 0.0000011760 0.221 11.22 1991.4 0.0004684 0.003699 0.008921 0.000003244 0.0000011600 0.208 11.52 1991.38 0.0004678 0.003728 0.008984 0.000003627 0.0000011470 0.209 11.81 1991.36 0.0004581 0.003673 0.008963 0.000003636 0.0000011440 0.208 12.11 1991.34 0.0004649 0.003776 0.009028 0.000003733 0.0000011260 0.184 12.40 1991.32 0.0004717 0.003951 0.008885 0.000004031 0.0000010860 0.197 12.70 1991.3 0.0004589 0.004031 0.008908 0.000004400 0.0000011010 0.209 12.99 1991.28 0.0004658 0.003995 0.008897 0.000004507 0.0000010740 0.200 13.29 1991.26 0.0004420 0.003977 0.008882 0.000004643 0.0000010680 0.199 13.58 1991.24 0.0004403 0.004245 0.008840 0.000005889 0.0000010210 0.202 13.88 1991.22 0.0004337 0.004230 0.008839 0.000007173 0.0000010000 0.238 14.17 1991.2 0.0004356 0.004263 0.008849 0.000005964 0.0000010000 0.279 14.47 1991.18 0.0004183 0.004497 0.008691 0.000005310 0.0000009647 0.301 14.77 1991.16 0.0004283 0.004352 0.008823 0.000005519 0.0000010030 0.287 15.06 1991.14 0.0004427 0.004220 0.008804 0.000006507 0.0000009862 0.249 15.36 1991.12 0.0004187 0.004267 0.008717 0.000008235 0.0000009134 0.307 15.65 1991.1 0.0003906 0.004178 0.008577 0.000008657 0.0000009370 0.364 15.95 1991.08 0.0004131 0.004249 0.008624 0.000006616 0.0000009483 0.426 16.83 1991.04 0.0004212 0.003883 0.008631 0.000009275 0.0000010020 0.504 17.13 1991.02 0.0003970 0.004174 0.008748 0.000006249 0.0000009945 0.381 17.42 1991.01 0.0003985 0.004462 0.008665 0.000007654 0.0000009729 0.339 17.72 1990.99 0.0004363 0.004481 0.008766 0.000009095 0.0000009686 0.319 18.01 1990.98 0.0004150 0.004611 0.008704 0.000010910 0.0000009590 0.315 18.31 1990.96 0.0004135 0.004791 0.008561 0.000010250 0.0000008978 0.312 18.60 1990.94 0.0004356 0.004973 0.008707 0.000010270 0.0000009026 0.315 18.90 1990.91 0.0004104 0.004810 0.008534 0.000010390 0.0000009340 0.305 19.19 1990.89 0.0004115 0.004360 0.008633 0.000011070 0.0000009819 0.320 19.49 1990.87 0.0004070 0.004176 0.008683 0.000011450 0.0000010320 0.316 19.79 1990.84 0.0004111 0.004030 0.008874 0.000009078 0.0000010490 0.281 20.08 1990.82 0.0004058 0.004083 0.008651 0.000005865 0.0000010070 0.282 20.38 1990.79 0.0004136 0.004178 0.008810 0.000004944 0.0000010640 0.279 20.67 1990.77 0.0004104 0.004038 0.008729 0.000004513 0.0000010420 0.282 20.97 1990.75 0.0004114 0.003918 0.008817 0.000004792 0.0000010840 0.269 21.26 1990.72 0.0004155 0.003744 0.008966 0.000004716 0.0000011450 0.233 21.56 1990.7 0.0004284 0.003705 0.008966 0.000004397 0.0000011490 0.243 21.85 1990.67 0.0004607 0.003800 0.008987 0.000003481 0.0000011330 0.272 22.15 1990.65 0.0004702 0.003827 0.008947 0.000003210 0.0000011320 0.262 22.44 1990.63 0.0004760 0.003831 0.009049 0.000003341 0.0000011700 0.269 22.74 1990.6 0.0004924 0.003798 0.009011 0.000003369 0.0000011680 0.255 23.03 1990.58 0.0004866 0.003740 0.008883 0.000003450 0.0000011650 0.260 23.33 1990.55 0.0004978 0.003377 0.009148 0.000003136 0.0000012680 0.227 23.62 1990.53 0.0004929 0.003503 0.009054 0.000002801 0.0000012480 0.185 23.92 1990.51 0.0005109 0.003431 0.009104 0.000002839 0.0000012670 0.192 24.22 1990.48 0.0005192 0.003323 0.009294 0.000003178 0.0000012830 0.318 24.51 1990.47 0.0005311 0.003487 0.009169 0.000003783 0.0000012590 0.283 24.81 1990.45 0.0005403 0.003524 0.009113 0.000003879 0.0000012310 0.195 25.10 1990.44 0.0005319 0.003493 0.009052 0.000004266 0.0000011860 0.177 25.40 1990.42 0.0005225 0.003538 0.009049 0.000004558 0.0000011780 0.170 25.69 1990.41 0.0005034 0.003557 0.009135 0.000004198 0.0000011490 0.195 25.99 1990.39 0.0004952 0.003792 0.009031 0.000003930 0.0000011480 0.212 26.28 1990.38 0.0004858 0.004154 0.008887 0.000004033 0.0000010610 0.205 26.58 1990.36 0.0004629 0.004151 0.008996 0.000004346 0.0000010480 0.185 26.87 1990.34 0.0004695 0.004087 0.008916 0.000004559 0.0000010390 0.191 27.17 1990.33 0.0004550 0.004119 0.008900 0.000004400 0.0000010580 0.234 27.46 1990.31 0.0004398 0.004186 0.008767 0.000003850 0.0000010540 0.272 27.76 1990.3 0.0004328 0.004023 0.008901 0.000004366 0.0000011050 0.242 28.05 1990.28 0.0004177 0.003935 0.008863 0.000004689 0.0000010670 0.232 28.35 1990.27 0.0004241 0.004075 0.008850 0.000004341 0.0000010350 0.294 28.64 1990.26 0.0004196 0.004119 0.008734 0.000004229 0.0000010360 0.310 28.94 1990.25 0.0004128 0.004146 0.008846 0.000004312 0.0000010620 0.343 29.24 1990.24 0.0004173 0.003828 0.008846 0.000004219 0.0000010960 0.321 29.53 1990.23 0.0004339 0.003738 0.008898 0.000005223 0.0000011520 0.298 29.83 1990.21 0.0004317 0.003727 0.008817 0.000006938 0.0000011360 0.270 30.12 1990.2 0.0004107 0.003950 0.008798 0.000007442 0.0000010460 0.283 30.42 1990.19 0.0003800 0.004365 0.008818 0.000006293 0.0000009877 0.330 30.71 1990.17 0.0003996 0.004277 0.008818 0.000004972 0.0000010330 0.364 31.01 1990.15 0.0004080 0.004295 0.008890 0.000004408 0.0000010150 0.374 31.30 1990.12 0.0004126 0.004254 0.008803 0.000004765 0.0000010130 0.368 31.60 1990.1 0.0004201 0.004264 0.008641 0.000005283 0.0000010040 0.354 31.89 1990.08 0.0004150 0.004202 0.008713 0.000007444 0.0000009686 0.370 32.19 1990.06 0.0004154 0.004271 0.008742 0.000007077 0.0000009625 0.336 32.48 1990.04 0.0004131 0.004288 0.008796 0.000005760 0.0000009820 0.295 32.78 1990.01 0.0004200 0.004263 0.008751 0.000005849 0.0000009708 0.280 33.07 1989.99 0.0004073 0.004433 0.008674 0.000006722 0.0000009392 0.270 33.37 1989.97 0.0004086 0.004220 0.008745 0.000008010 0.0000009950 0.273 33.66 1989.95 0.0004111 0.004035 0.008668 0.000008215 0.0000009829 0.246 33.96 1989.92 0.0004175 0.004289 0.008649 0.000008879 0.0000009096 0.240 34.26 1989.9 0.0004436 0.004408 0.008599 0.000009325 0.0000009431 0.219 34.55 1989.88 0.0004633 0.004231 0.008842 0.000008545 0.0000009995 0.255 34.85 1989.87 0.0004645 0.004207 0.008778 0.000007905 0.0000009752 0.296 35.14 1989.85 0.0004479 0.004255 0.008774 0.000007724 0.0000009735 0.324 35.44 1989.83 0.0004299 0.004361 0.008680 0.000007857 0.0000009843 0.317 35.73 1989.81 0.0004310 0.004163 0.008810 0.000006713 0.0000010100 0.303 36.03 1989.79 0.0003996 0.004151 0.008784 0.000006164 0.0000010300 0.301 36.32 1989.77 0.0004035 0.003993 0.008804 0.000006206 0.0000010510 0.263 36.62 1989.75 0.0004153 0.003905 0.008819 0.000005759 0.0000010780 0.264 36.91 1989.73 0.0004108 0.003657 0.008896 0.000005128 0.0000011400 0.318 37.21 1989.71 0.0004316 0.003734 0.008931 0.000004739 0.0000011600 0.317 37.50 1989.69 0.0004396 0.003776 0.008904 0.000004013 0.0000011850 0.303 37.80 1989.67 0.0004611 0.003572 0.008988 0.000003695 0.0000012230 0.308 38.09 1989.65 0.0004769 0.003535 0.009085 0.000003669 0.0000012060 0.280 38.39 1989.64 0.0004905 0.003462 0.009077 0.000002998 0.0000012670 0.262 38.69 1989.61 0.0004934 0.003441 0.009163 0.000003023 0.0000012730 0.230 38.98 1989.59 0.0005070 0.003406 0.009089 0.000002826 0.0000012520 0.207 39.28 1989.57 0.0005155 0.003298 0.009174 0.000002964 0.0000012690 0.207 39.57 1989.55 0.0005192 0.003426 0.009155 0.000003269 0.0000012820 0.190 39.87 1989.53 0.0005185 0.003263 0.009184 0.000003087 0.0000012500 0.173 40.16 1989.51 0.0005088 0.003391 0.009071 0.000003092 0.0000012280 0.190 40.46 1989.49 0.0005116 0.003521 0.009180 0.000003085 0.0000012440 0.186 40.75 1989.47 0.0005015 0.003608 0.009060 0.000003259 0.0000011910 0.199 41.05 1989.45 0.0005025 0.003721 0.009025 0.000003538 0.0000011750 0.194 41.34 1989.43 0.0004798 0.003553 0.008959 0.000003420 0.0000012060 0.185 41.64 1989.41 0.0004644 0.003586 0.009020 0.000003649 0.0000011990 0.202 41.93 1989.39 0.0004560 0.003681 0.009016 0.000003896 0.0000011380 0.207 42.23 1989.37 0.0004538 0.003798 0.008917 0.000004430 0.0000011260 0.218 42.52 1989.35 0.0004362 0.003595 0.008899 0.000004521 0.0000011900 0.208 42.82 1989.33 0.0004263 0.003566 0.009055 0.000004546 0.0000011790 0.204 43.11 1989.31 0.0004171 0.003703 0.008915 0.000004834 0.0000011300 0.226 43.41 1989.29 0.0004107 0.004102 0.008883 0.000005257 0.0000010850 0.250 43.71 1989.27 0.0004030 0.003790 0.008866 0.000004670 0.0000011230 0.257 44.00 1989.24 0.0003989 0.003971 0.008844 0.000005264 0.0000010660 0.250 44.30 1989.22 0.0004177 0.004156 0.008837 0.000005281 0.0000010310 0.254 44.59 1989.2 0.0003803 0.004170 0.008835 0.000005404 0.0000010710 0.269 44.89 1989.18 0.0003782 0.004161 0.008748 0.000004894 0.0000010350 0.287 45.18 1989.16 0.0003887 0.004009 0.008794 0.000004555 0.0000010650 0.300 45.48 1989.14 0.0003847 0.004119 0.008915 0.000004820 0.0000010660 0.268 45.77 1989.12 0.0003833 0.003889 0.008865 0.000005197 0.0000011090 0.238 46.07 1989.1 0.0003909 0.004024 0.008795 0.000006422 0.0000010570 0.230 46.36 1989.08 0.0003968 0.004256 0.008700 0.000005404 0.0000010050 0.257 46.66 1989.06 0.0003853 0.003951 0.008789 0.000005192 0.0000010350 0.250 46.95 1989.04 0.0003739 0.004164 0.008717 0.000005634 0.0000010130 0.293 47.25 1989.02 0.0003745 0.004127 0.008755 0.000005030 0.0000009788 0.314 47.54 1988.99 0.0003900 0.004058 0.008822 0.000004464 0.0000009994 0.301 47.84 1988.96 0.0003954 0.004039 0.008777 0.000004986 0.0000010240 0.341 48.14 1988.92 0.0003957 0.003732 0.008809 0.000004706 0.0000010970 0.319