# 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-davies8-metals.txt # Data_Download_Description: NOAA Template File; Davies8 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: Davies Reef # Location: Great Barrier Reef, Australia # Northernmost_Latitude: -18.8 # Southernmost_Latitude: -18.8 # Easternmost_Longitude: 147.7 # Westernmost_Longitude: 147.7 # Elevation_m: -6.8 #--------------------------------------- # Data_Collection # Collection_Name: Davies8 trace metals Fallon2003 # First_Year: 1990 # Last_Year: 1993 # Time_Unit: year Common Era # Core_Length_m: 0.15 # Parameter_Keywords: trace metals # Notes: Porites lutea #--------------------------------------- # 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 lutea,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## Mg/Ca Magnesium/Calcium,Porites lutea,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## Sr/Ca Strontium/Calcium,Porites lutea,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## Ba/Ca Barium/Calcium,Porites lutea,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## U/Ca Uranium/Calcium,Porites lutea,,mole per mole,,corals and sclerosponges,,inductively-coupled plasma mass spectrometry,N,laser ablation inductively-coupled mass spectrometry ## Mn Manganese,Porites lutea,,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 0.13612380 1993.769000 0.0004735469 0.0044056350 0.0091516249 0.0000391813 0.0000009897 0.3016764870 0.47643331 1993.732118 0.0004680479 0.0042067278 0.0093223169 0.0000468454 0.0000010667 0.2235945290 0.81674282 1993.693294 0.0004641790 0.0039467154 0.0091338995 0.0000262038 0.0000010986 0.1363329200 1.15705232 1993.654471 0.0005245723 0.0044752212 0.0090468462 0.0000185430 0.0000009478 0.1026924720 1.49736183 1993.615647 0.0005091176 0.0043828167 0.0089385388 0.0000251276 0.0000009383 0.0924298450 1.83767133 1993.576824 0.0004994766 0.0038047031 0.0089781876 0.0000175801 0.0000010645 0.0783334160 2.17798084 1993.538000 0.0005164993 0.0039632963 0.0091353790 0.0000223914 0.0000010348 0.0866451030 2.51829035 1993.518778 0.0005097760 0.0038209716 0.0090585015 0.0000184109 0.0000010665 0.0893815990 2.85859985 1993.499555 0.0005112183 0.0038419616 0.0090142593 0.0000212919 0.0000010351 0.0753460140 3.19890936 1993.480333 0.0004919086 0.0036489773 0.0090814317 0.0000180731 0.0000010452 0.0654889040 3.53921887 1993.461111 0.0004990665 0.0037758097 0.0090270469 0.0000124645 0.0000010013 0.0731804930 3.87952837 1993.441889 0.0004897635 0.0040820502 0.0090724677 0.0000251403 0.0000010119 0.1021762510 4.21983788 1993.422666 0.0004715825 0.0041856442 0.0089326248 0.0000165790 0.0000009416 0.1031260330 4.56014738 1993.403444 0.0004590075 0.0041228146 0.0090394843 0.0000169919 0.0000010146 0.1120411040 4.90045689 1993.384222 0.0004380053 0.0040872248 0.0089519736 0.0000115704 0.0000009850 0.1085139480 5.24076640 1993.365000 0.0004217541 0.0042196327 0.0089160092 0.0000105424 0.0000009886 0.1062016410 5.58107590 1993.345778 0.0004243670 0.0044920512 0.0090085475 0.0000176637 0.0000009539 0.1564318090 5.92138541 1993.326556 0.0004199793 0.0045572688 0.0089320608 0.0000114398 0.0000009377 0.1222389800 6.26169492 1993.307334 0.0004012476 0.0044442732 0.0088548728 0.0000118159 0.0000009491 0.1365925420 6.60200442 1993.288111 0.0004164632 0.0042855986 0.0089070411 0.0000114026 0.0000009780 0.1660254910 6.94231393 1993.268889 0.0004033639 0.0045127440 0.0088230002 0.0000094532 0.0000009473 0.1485124760 7.28262343 1993.249667 0.0003783849 0.0044543283 0.0088377257 0.0000072244 0.0000009349 0.1246904200 7.62293294 1993.230445 0.0003893986 0.0046521163 0.0088392879 0.0000073601 0.0000009094 0.1453456370 7.96324245 1993.211222 0.0003872408 0.0049113977 0.0087356710 0.0000056407 0.0000008814 0.1117202680 8.30355195 1993.192000 0.0003678217 0.0047541331 0.0087241547 0.0000045022 0.0000008638 0.0987289160 8.64386146 1993.174214 0.0003745330 0.0046015316 0.0087932305 0.0000049895 0.0000009388 0.1082071410 8.98417097 1993.156428 0.0003700544 0.0044131227 0.0087576768 0.0000055476 0.0000009200 0.1019014450 9.32448047 1993.138643 0.0003857355 0.0046473099 0.0088377278 0.0000036277 0.0000009178 0.0937715580 9.66478998 1993.120857 0.0003836760 0.0047764389 0.0087635742 0.0000033673 0.0000008782 0.1084826810 10.00509948 1993.103071 0.0003711169 0.0049394729 0.0087536724 0.0000044129 0.0000008498 0.1221172500 10.34540899 1993.085285 0.0003773597 0.0045914268 0.0087612828 0.0000031369 0.0000008939 0.1042220020 10.68571850 1993.067500 0.0003722377 0.0043647442 0.0086969916 0.0000026873 0.0000009211 0.0885056930 11.02602800 1993.049714 0.0003807429 0.0043268124 0.0088546749 0.0000038320 0.0000009333 0.1110317040 11.36633751 1993.031928 0.0003911288 0.0046690375 0.0088203298 0.0000039129 0.0000009154 0.1092769660 11.70664702 1993.014142 0.0003712031 0.0043463986 0.0087838886 0.0000028676 0.0000009269 0.0900699400 12.04695652 1992.996357 0.0003605094 0.0041265764 0.0087686832 0.0000030831 0.0000009483 0.0866240790 12.38726603 1992.978571 0.0003613325 0.0044367706 0.0088243061 0.0000029148 0.0000009310 0.1023834730 12.72757553 1992.960786 0.0003884158 0.0048030559 0.0088558711 0.0000038718 0.0000008732 0.1233511490 13.06788504 1992.943000 0.0003726795 0.0044550394 0.0086958409 0.0000029218 0.0000008882 0.0950135790 13.40819455 1992.920143 0.0003824125 0.0045975571 0.0087992708 0.0000032512 0.0000008844 0.0874229950 13.74850405 1992.897286 0.0004140387 0.0043921085 0.0089039066 0.0000029473 0.0000009779 0.0892623370 14.08881356 1992.874429 0.0004180091 0.0044365000 0.0088559822 0.0000039264 0.0000009066 0.0996950360 14.42912307 1992.851571 0.0004248249 0.0043140683 0.0088675954 0.0000039053 0.0000009394 0.0929182170 14.76943257 1992.828714 0.0004272073 0.0042940570 0.0088822899 0.0000035170 0.0000009816 0.1005057930 15.10974208 1992.805857 0.0004198359 0.0040556792 0.0088933643 0.0000034853 0.0000009672 0.0952177010 15.45005158 1992.783000 0.0004315146 0.0040009336 0.0089460229 0.0000041380 0.0000010284 0.1018359790 15.79036109 1992.760143 0.0004336247 0.0037926492 0.0089349720 0.0000030132 0.0000010760 0.0922157340 16.13067060 1992.737286 0.0004359697 0.0037800518 0.0089324654 0.0000034448 0.0000010853 0.0908320030 16.47098010 1992.714429 0.0004420209 0.0037830029 0.0090343025 0.0000033721 0.0000010203 0.0881453300 16.81128961 1992.691571 0.0004774506 0.0039042294 0.0090285247 0.0000030628 0.0000010536 0.0802955790 17.15159912 1992.668714 0.0004891829 0.0038599064 0.0090792497 0.0000033076 0.0000010525 0.0785104790 17.49190862 1992.645857 0.0004923012 0.0041208098 0.0090436198 0.0000035469 0.0000009875 0.0790906270 17.83221813 1992.623000 0.0004779975 0.0040716733 0.0091263056 0.0000042541 0.0000010181 0.0806244690 18.17252763 1992.581400 0.0004667554 0.0039318721 0.0089932933 0.0000034528 0.0000010270 0.0857154850 18.51283714 1992.539800 0.0004770491 0.0039300366 0.0090313190 0.0000030376 0.0000010235 0.0735848050 18.85314665 1992.498199 0.0005082180 0.0039899345 0.0090385526 0.0000033407 0.0000010341 0.0763926530 19.19345615 1992.456599 0.0004774202 0.0039935327 0.0089490223 0.0000037398 0.0000010236 0.0876199220 19.53376566 1992.415000 0.0004520511 0.0038147116 0.0090188959 0.0000038542 0.0000010568 0.0916485710 19.87407517 1992.396250 0.0004385668 0.0039771390 0.0089232733 0.0000034408 0.0000010015 0.0825873330 20.21438467 1992.377500 0.0004249443 0.0045524995 0.0088511407 0.0000036917 0.0000009131 0.1054803520 20.55469418 1992.358750 0.0004110856 0.0044676363 0.0088871451 0.0000034432 0.0000009176 0.0928051250 20.89500368 1992.340000 0.0003964756 0.0045689859 0.0087872019 0.0000032517 0.0000009199 0.1025152970 21.23531319 1992.321000 0.0004071358 0.0045399307 0.0088435997 0.0000031190 0.0000009226 0.0980080130 21.57562270 1992.302000 0.0003962185 0.0043420392 0.0088176487 0.0000035132 0.0000009481 0.1079342410 21.91593220 1992.283000 0.0003839088 0.0043565511 0.0088710554 0.0000035959 0.0000009545 0.1153462250 22.25624171 1992.264000 0.0003880900 0.0044196532 0.0087363703 0.0000031261 0.0000009328 0.0973651230 22.59655122 1992.245000 0.0003739231 0.0043396830 0.0088639016 0.0000034336 0.0000009425 0.0895756600 22.93686072 1992.226000 0.0003562692 0.0042137581 0.0086499212 0.0000035660 0.0000009186 0.0821783790 23.27717023 1992.207143 0.0003508870 0.0041609296 0.0087987610 0.0000034697 0.0000009361 0.0871819120 23.61747973 1992.188286 0.0003448521 0.0041949139 0.0087272929 0.0000028428 0.0000009177 0.0878593040 23.95778924 1992.169428 0.0003491723 0.0041204737 0.0087262661 0.0000026111 0.0000009090 0.0963469540 24.29809875 1992.150571 0.0003608025 0.0039720956 0.0087810323 0.0000028029 0.0000009291 0.0997075780 24.63840825 1992.131714 0.0003701397 0.0041356164 0.0086951129 0.0000033181 0.0000008878 0.0991560420 24.97871776 1992.112857 0.0003625077 0.0040795162 0.0087989836 0.0000029677 0.0000008862 0.1106433370 25.31902727 1992.094000 0.0003812550 0.0041890254 0.0087585684 0.0000028280 0.0000009237 0.1236253570 25.65933677 1992.075143 0.0003838932 0.0042989843 0.0088616562 0.0000026528 0.0000009009 0.1216671400 25.99964628 1992.056285 0.0003784324 0.0040963381 0.0087102673 0.0000027878 0.0000009124 0.1183994280 26.33995578 1992.037429 0.0003909730 0.0044322783 0.0087128258 0.0000033273 0.0000009109 0.1233888260 26.68026529 1992.018572 0.0003879757 0.0048962468 0.0087685513 0.0000031561 0.0000008422 0.1312238650 27.02057480 1991.999714 0.0003845986 0.0048841704 0.0087393621 0.0000029653 0.0000008239 0.1116726580 27.36088430 1991.980857 0.0003893030 0.0046516101 0.0087597472 0.0000034121 0.0000008633 0.1411580480 27.70119381 1991.962000 0.0003931137 0.0045372066 0.0087019716 0.0000026448 0.0000008927 0.1085318040 28.04150332 1991.925667 0.0003652692 0.0043472912 0.0088064157 0.0000032868 0.0000008869 0.1036203510 28.38181282 1991.889333 0.0003659413 0.0043623736 0.0087595921 0.0000022447 0.0000008857 0.0925747690 28.72212233 1991.853000 0.0003882278 0.0041944353 0.0088440310 0.0000022936 0.0000009289 0.0877981380 29.06243183 1991.816667 0.0004042428 0.0041009963 0.0089123931 0.0000025182 0.0000009924 0.0845200000 29.40274134 1991.780333 0.0004225623 0.0041145427 0.0088876372 0.0000021136 0.0000009985 0.0844202590 29.74305085 1991.744000 0.0004135430 0.0040187038 0.0089875118 0.0000025805 0.0000009948 0.0846888560 30.08336035 1991.707667 0.0004216271 0.0035612809 0.0090455397 0.0000022402 0.0000010936 0.0751018340 30.42366986 1991.671333 0.0004493160 0.0037138867 0.0091044188 0.0000029547 0.0000011626 0.0953926040 30.76397937 1991.635000 0.0004624255 0.0036267482 0.0091258390 0.0000027529 0.0000012049 0.0824590810 31.10428887 1991.577333 0.0004861844 0.0038031072 0.0090738092 0.0000023375 0.0000011181 0.0801435670 31.44459838 1991.519667 0.0004930113 0.0036614230 0.0091720211 0.0000052790 0.0000011441 0.0934411860 31.78490789 1991.462000 0.0004936753 0.0035242923 0.0091602890 0.0000065490 0.0000010875 0.0663699210 32.12521739 1991.417000 0.0005020739 0.0036939289 0.0089660973 0.0000029294 0.0000010174 0.0759473620 32.46552690 1991.372000 0.0004975608 0.0038166494 0.0089745030 0.0000032158 0.0000010238 0.0824287590 32.80583640 1991.327000 0.0004751180 0.0039205961 0.0089173148 0.0000023935 0.0000009565 0.0683295440 33.14614591 1991.307800 0.0004820227 0.0037939263 0.0090741439 0.0000023205 0.0000010084 0.0744846440 33.48645542 1991.288600 0.0004407879 0.0037827442 0.0089147521 0.0000027100 0.0000010368 0.0910065650 33.82676492 1991.269400 0.0004166642 0.0039101800 0.0088980787 0.0000028440 0.0000010013 0.0893938820 34.16707443 1991.250200 0.0004008819 0.0038940647 0.0088939780 0.0000028387 0.0000009888 0.0871933670 34.50738394 1991.231000 0.0003876252 0.0037059047 0.0087894450 0.0000029483 0.0000010458 0.0898616560 34.84769344 1991.215789 0.0004045216 0.0041252028 0.0088500107 0.0000027538 0.0000009446 0.1034540230 35.18800295 1991.200579 0.0003905731 0.0039083793 0.0089564588 0.0000031647 0.0000009929 0.1027984850 35.52831245 1991.185368 0.0003963833 0.0040798441 0.0088042177 0.0000030010 0.0000010048 0.1103819240 35.86862196 1991.170158 0.0004046738 0.0040652302 0.0089545490 0.0000029636 0.0000010060 0.1384949740 36.20893147 1991.154947 0.0003798050 0.0041739379 0.0086808574 0.0000031023 0.0000009201 0.1575910480 36.54924097 1991.139737 0.0003610061 0.0039198134 0.0087985569 0.0000053214 0.0000009868 0.1602181640 36.88955048 1991.124526 0.0003683224 0.0039387406 0.0088784691 0.0000031641 0.0000009978 0.1427196790 37.22985999 1991.109316 0.0003949292 0.0038557231 0.0088056867 0.0000025260 0.0000010046 0.1324645410 37.57016949 1991.094105 0.0004027771 0.0037722924 0.0088357141 0.0000024620 0.0000010224 0.1446119480 37.91047900 1991.078895 0.0003952429 0.0042932282 0.0086919496 0.0000026792 0.0000008999 0.1509647990 38.25078850 1991.063684 0.0004138461 0.0044213805 0.0087448160 0.0000026523 0.0000008865 0.1360586550 38.59109801 1991.048474 0.0004132930 0.0040211135 0.0088651454 0.0000024685 0.0000009451 0.1091477740 38.93140752 1991.033263 0.0004051096 0.0044876319 0.0087695235 0.0000027690 0.0000008674 0.1179076250 39.27171702 1991.018053 0.0003968294 0.0043578314 0.0088430232 0.0000026850 0.0000009397 0.1030783210 39.61202653 1991.002842 0.0003914273 0.0037343590 0.0088955124 0.0000026526 0.0000010423 0.0971895520 39.95233604 1990.987632 0.0004101578 0.0038265906 0.0089489955 0.0000031340 0.0000009876 0.1105848480 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0.0000010921 0.0742957670 43.69574060 1990.658308 0.0005051660 0.0037411751 0.0092221701 0.0000029591 0.0000011619 0.0694372490 44.03605011 1990.622846 0.0004948549 0.0035669699 0.0090849910 0.0000037014 0.0000011468 0.0857060870 44.37635962 1990.587385 0.0005416384 0.0036793957 0.0090992962 0.0000032798 0.0000011875 0.0867722720 44.71666912 1990.551923 0.0005014240 0.0034238840 0.0091961103 0.0000035388 0.0000012285 0.0779699840 45.05697863 1990.516461 0.0004867659 0.0035850154 0.0090480324 0.0000031170 0.0000011572 0.0958681350 45.39728814 1990.481000 0.0004493105 0.0037514787 0.0091321708 0.0000029504 0.0000011292 0.1006186590 45.73759764 1990.445538 0.0004475888 0.0039889103 0.0089671749 0.0000031344 0.0000010264 0.1294912980 46.06089167 1990.410077 0.0004196974 0.0035494517 0.0088350935 0.0000037299 0.0000009851 0.1562969750