# Galapagos Islands and Great Barrier Reef coral and geochemical data from 1729-2010 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.ncdc.noaa.gov/access/paleo-search/study/35193 # 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-35193.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/y68n-1x24 # # Science_Keywords: ocean acidification #--------------------------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/coral/east_pacific/thompson2021/galapagosfossilrawdata-thompson2021.txt # Data_Download_Description: NOAA Template File; Galapagos Fossil Raw Data # #--------------------------------------- # Contribution_Date # Date: 2022-01-06 #--------------------------------------- # File_Last_Modified_Date # Date: 2022-04-07 #--------------------------------------- # Title # Study_Name: Galapagos Islands and Great Barrier Reef coral and geochemical data from 1729-2010 CE #--------------------------------------- # Investigators # Investigators: Thompson, Diane M.; McCulloch, Malcolm; Cole, Julia E.; Reed, Emma V.; D'Olivo, Juan P.; Dyez, Kelsey; Lofverstrom, Marcus; Lough, Janice; Cantin, Neal; Tudhope, Alexander W.; Cheung, Anson, H., Vetter, Lael; Edwards, R. Lawrence #--------------------------------------- # Description_Notes_and_Keywords # Description: We leverage geochemical tracers of coral biomineralization–skeletal B/Ca ([CO3-]), d11B (pHcf), and U/Ca ([CO3-])–that constrain the calcifying fluid chemistry, including the aragonite saturation that governs calcification rate (DeCarlo et al., 2018, 2015). We combine these with paleo-environmental tracers that primarily reflect factors external to the coral calcification environment: Sr/Ca (Beck et al., 1992; Corrège et al., 2000), Li/Mg (Hathorne, Felis, et al., 2013; Montagna et al., 2014), and d18O (Weber & Woodhead, 1972; McConnaughey, 1989) (all primarily controlled by SST); Ba/Ca (upwelling, Lea et al., 1989; Shen et al., 1992); and d13C (upwelling, metabolic carbon / photosynthesis, respiration, and reproduction, G. T. Shen et al., 1992). These new recent (1976-2010) and fossil (1729-1733) Galápagos records (Wolf Island, 1o23.15’N, 91o49.90’W) significantly extend the multi-tracer data coverage prior to the industrial era, which allows us to assess the capacity of corals to buffer against changing environmental conditions. We compare our new Galápagos results with published data from the Great Barrier Reef (McCulloch et al., 2017) to contextualize results from the marginal Galápagos reef environment–a comparatively cold, low-saturation, and highly variable environment. # Provided Keywords: boron isotopes, trace elemental geochemistry, ocean acidification, heat stress, ENSO #--------------------------------------- # Publication # Authors: Thompson, Diane M.; McCulloch, Malcolm; Cole, Julia E.; Reed, Emma V.; D'Olivo, Juan P.; Dyez, Kelsey; Lofverstrom, Marcus; Lough, Janice; Cantin, Neal; Tudhope, Alexander W.; Cheung, Anson, H., Vetter, Lael; Edwards, R. Lawrence # Published_Date_or_Year: 2022-02-01 # Published_Title: Marginal reefs under stress: physiological limits render Galápagos corals susceptible to ocean acidification and thermal stress # Journal_Name: AGU Advances # Volume: 3 # Edition: # Issue: 1 # Pages: # Report_Number: e2021AV000509 # DOI: 10.1029/2021AV000509 # Online_Resource: # Full_Citation: # Abstract: Ocean acidification and thermal stress may undermine corals’ ability to calcify and support diverse reef communities, particularly in marginal environments. Coral calcification depends on aragonite supersaturation (Ω>>1) of the calcifying fluid (cf) from which the skeleton precipitates. Corals actively upregulate pHcf relative to seawater to buffer against changes in temperature and dissolved inorganic carbon (DICcf), which together control Ωcf. Here we assess the buffering capacity in modern and fossil corals from the Galápagos Islands that have been exposed to sub-optimal conditions, extreme thermal stress, and ocean acidification. We demonstrate a significant decline in pHcf and Ωcf since the pre-industrial era, trends which are exacerbated during extreme warm years. These results suggest that there are likely physiological limits to corals’ pH buffering capacity, and that these constraints render marginal reefs particularly susceptible to ocean acidification. #--------------------------------------- # Publication # Authors: McCulloch, M.T.; D’Olivo, J. P.; Falter, J.; Holcomb, M.; & Trotter, J. A. # Published_Date_or_Year: 2017 # Published_Title: Coral calcification in a changing world and the interactive dynamics of pH and DIC upregulation.  # Journal_Name: Nature Communications # Volume: 8 # Edition: # Issue: # Pages: # Report_Number: 15686 # DOI: 10.1038/ncomms15686 # Online_Resource: # Full_Citation: # Abstract: Coral calcification is dependent on the mutualistic partnership between endosymbiotic zooxanthellae and the coral host. Here, using newly developed geochemical proxies (d11B and B/Ca), we show that Porites corals from natural reef environments exhibit a close (r2 ~0.9) antithetic relationship between dissolved inorganic carbon (DIC) and pH of the corals’ calcifying fluid (cf). The highest DICcf (~ × 3.2 seawater) is found during summer, consistent with thermal/light enhancement of metabolically (zooxanthellae) derived carbon, while the highest pHcf (~8.5) occurs in winter during periods of low DICcf (~ × 2 seawater). These opposing changes in DICcf and pHcf are shown to maintain oversaturated but stable levels of carbonate saturation (Ocf ~ × 5 seawater), the key parameter controlling coral calcification. These findings are in marked contrast to artificial experiments and show that pHcf upregulation occurs largely independent of changes in seawater carbonate chemistry, and hence ocean acidification, but is highly vulnerable to thermally induced stress from global warming. #--------------------------------------- # Publication # Authors: Reed, E.V.; Thompson, D.M.; Cole, J.E.; Lough, J.M; Cantin, N.E.; Cheung, A.H., Tudhope, A.; Vetter, L., Jimenez, G.; and Edward, R.L. # Published_Date_or_Year: 2021-04-01 # Published_Title: Impacts of coral growth on geochemistry: Lessons from the Galapagos Islands # Journal_Name: Paleoceanography and Paleoclimatology # Volume: 36 # Edition: # Issue: 4 # Pages: # Report_Number: e2020PA004051 # DOI: 10.1029/2020PA004051 # Online_Resource: # Full_Citation: # Abstract: Coral geochemical climate reconstructions can extend our knowledge of global climate variability and trends over timescales longer than those of instrumental data. However, such reconstructions can be biased by coral growth and skeletal architecture, such as growth troughs, off-axis corallite orientation, and changing growth direction. This study quantifies the impact of skeletal architecture and growth on geochemistry using measurements of coral skeletal density, extension rate, and calcification rate, and uses these metrics to improve paleoclimate reconstructions. We present paired geochemistry-density records at Wolf Island, Galápagos, from three Porites lobata corals: two new paired density and geochemistry records from one fossil coral, and new density data from two previously published modern geochemistry records. We categorize each sampling transect used in this record by the quality of its orientation with respect to skeletal architecture. We observe relationships between geochemistry and density that are not detected using extension or calcification rate alone. These density-geochemistry relationships likely reflect both the response of coral growth to environmental conditions and the non-climatic impact of skeletal architecture on geochemistry in sub-optimal sampling transects. Correlations of density with Sr/Ca, Ba/Ca, and Mg/Ca are consistent with the Rayleigh fractionation model of trace element incorporation into coral skeletons. Removing transects with sub-optimal skeletal architecture increases mean reconstructed SST closer to instrumental mean SST, and lowers errors of reconstruction by up to 20%. These results demonstrate the usefulness of coral density data for assessing skeletal architecture and growth when generating coral paleoclimate records. #--------------------------------------- # Publication # Authors: Jimenez, G.; Cole, J.E.; Thompson, D.M.; and Tudhope, A.W. # Published_Date_or_Year: 2018 # Published_Title: Northern Galápagos Corals Reveal Twentieth Century Warming in the Eastern Tropical Pacific # Journal_Name: Geophysical Research Letters # Volume: 45 # Edition: # Issue: # Pages: 1981-1988 # Report_Number: # DOI: 10.1002/2017GL075323 # Online_Resource: # Full_Citation: # Abstract: Models and observations disagree regarding sea surface temperature (SST) trends in the eastern tropical Pacific. We present a new Sr/Ca-SST record that spans 1940–2010 from two Wolf Island corals (northern Gala´pagos). Trend analysis of the Wolf record shows significant warming on multiple timescales, which is also present in several other records and gridded instrumental products. Together, these data sets suggest that most of the eastern tropical Pacific has warmed over the twentieth century. In contrast, recent decades have been characterized by warming during boreal spring and summer (especially north of the equator), and subtropical cooling during boreal fall and winter (especially south of the equator). These SST trends are consistent with the effects of radiative forcing, mitigated by cooling due to wind forcing during boreal winter, as well as intensified upwelling and a strengthened Equatorial Undercurrent. #--------------------------------------- # Publication # Authors: Cheung, A.H.; Cole, J.E.; Thompson, D.M.; Vetter, L., Jimenez, G.; and Tudhope, A.W. # Published_Date_or_Year: 2021-12-01 # Published_Title: Fidelity of the Coral Sr/Ca Paleothermometer Following Heat Stress in the Northern Galápagos # Journal_Name: Paleoceanography and Paleoclimatology # Volume: 36 # Edition: # Issue: 12 # Pages: # Report_Number: e2021PA004323 # DOI: 10.1029/2021PA004323 # Online_Resource: # Full_Citation: # Abstract: Coral Sr/Ca records have been widely used to reconstruct and understand past sea surface temperature (SST) variability in the tropical Pacific. However, in the eastern equatorial Pacific, coral growth conditions are marginal, and strong El Niño events have led to high mortality, limiting opportunities for coral Sr/Ca-based SST reconstructions. In this study, we present two ~25-year Sr/Ca and Mg/Ca records measured on modern Porites lobata from Wolf and Darwin Islands in the northern Galápagos. In these records, we confirm the well-established relationship between Sr/Ca and SST and investigate the impact of heat stress on this relationship. We demonstrate a weakened relationship between Sr/Ca and SST after a major (Degree Heating Months 9°C-months) heat stress event during the 1997–1998 El Niño, with a larger response in the Wolf core. However, removing data that covers the 1997–1998 El Niño from calibration does not improve reconstruction statistics. Nevertheless, we find that excluding data after the 1997–1998 El Niño event from the calibration reduces the SST reconstruction error slightly. These results confirm that coral Sr/Ca is a reliable SST proxy in this region, although it can respond adversely to unusual heat stress. We suggest that noise in Sr/Ca-SST calibrations may be reduced by removing data immediately following large heat extremes. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: NSF # Grant: 1401326/1829613 and 0957881 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: UK Natural Environment Research Council # Grant: NE/H009957/1 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: ARC Centre of Excellence # Grant: CE140100020 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Boston University # Grant: Startup funds #--------------------------------------- # Site_Information # Site_Name: Wolf Island # Location: Galápagos Islands # Northernmost_Latitude: 1.385833 # Southernmost_Latitude: 1.385833 # Easternmost_Longitude: -91.831667 # Westernmost_Longitude: -91.831667 # Elevation_m: #--------------------------------------- # Data_Collection # Collection_Name: GalapagosFossilRawData-Thompson2021 # First_Year: # Last_Year: # Time_Unit: # Core_Length_m: # Parameter_Keywords: trace metals, oxygen isotopes # Notes: #--------------------------------------- # Chronology_Information # Chronology: Uranium-Thorium # Chronology_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/templates/noaa-wds-paleo-uth-terms.csv # Chronology_Download_Description: Uranium-Thorium terms and definitions. # Chronology_Notes: # 238U_Decay_Constant: # 234U_Decay_Constant: # 230Th_Decay_Constant: # Initial_230Th/232Th: 4.4 ppm +/- 2.2 ppm # Initial_230Th/232Th_Method: Estimated using the values for a material at secular equilibrium, with the bulk earth 232Th/238U value of 3.8. The errors are arbitrarily assumed to be 50%. # Missing_Values: NaN # Chronology_Table: # samp_id depth_mm 238U_ppb 238U_2s_ppb 232Th_ppt 232Th_2s_ppt 230Th_232Th_atom_10e-6 230Th_232Th_atom_2s_10e-6 d234U_meas_permil d234U_meas_2s_permil 230Th_238U_act 230Th_238U_act_2s age_uncorr_BM age_uncorr_2s_yr age_corr_BM age_corr_2s_yr d234U_init_permil d234U_init_2s_permil age_corr_BP1950 age_corr_2s_yr # W-4 NaN 2566.84917681749 5.72443343974862 35.8041042314164 2.92776874095001 3478.63508026779 297.85521223493 144.577284957514 2.8556001649249 2.94290108750308E-03 7.50197704690843E-05 280.720230599114 7.19917459825138 280.365377984808 7.20341665105339 144.691720937881 2.85786194653303 218.365377984808 7.20341665105339 218.365377984808 # W-5 NaN 2314.6041590957 2.77942756246694 74.2917436034908 2.31041056540306 1481.88184390906 53.9616301244951 147.164872803928 1.85676691268719 2.88477357145561E-03 5.47562128084923E-05 274.547136536471 5.2364643785168 273.732766998169 5.26785956847738 147.278600182713 1.85820309143345 211.732766998169 5.26785956847738 #--------------------------------------- # Variables # PaST_Thesaurus_Download_Resource: https://www.ncdc.noaa.gov/paleo/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) # ## Core_depth depth,,,millimeter,,corals and sclerosponges,,,N,core depth ## Lab_ID sample identification,,,,,corals and sclerosponges,,,C,Lab ID ## d13C delta 13C,Porites lobata,,per mil,,corals and sclerosponges,averaged,dual-inlet isotope ratio mass spectrometry,N, ## d18O delta 18O,Porites lobata,,per mil,,corals and sclerosponges,averaged,dual-inlet isotope ratio mass spectrometry,N, ## Sample_Name sample identification,,,,,corals and sclerosponges,,,C,Sample Name ## Latitude latitude,,,degree north,,corals and sclerosponges,,,N, ## Longitude longitude,,,degree east,,corals and sclerosponges,,,N, ## Depth collection water depth,,,meter,,corals and sclerosponges,,,N ## d11B delta 11B,Porites lobata,,per mil SRM 951,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N,error reported as 2 sigma of JCP-1 standard; error detail: 0.22 ## pHcf pH,calcifying fluid;delta 11B,,dimensionless,,corals and sclerosponges; climate reconstructions,corrected,,N, ## pHcf_press_corr pH,calcifying fluid;delta 11B,,dimensionless,,corals and sclerosponges; climate reconstructions,corrected,,N,pressure corrected ## DICcf dissolved inorganic carbon,calcifying fluid,,micromole per kilogram,,corals and sclerosponges; climate reconstructions,corrected,,N, ## Wcf aragonite saturation state,calcifying fluid,,dimensionless,,corals and sclerosponges; climate reconstructions,corrected,,N, ## [Ca] calcium,Porites lobata,,parts per million,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N, ## Mg/Ca magnesium/calcium,Porites lobata,,millimole per mole,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N,error reported as 1 sigma of JCP-1 standard; error detail: 0.024 ## Sr/Ca strontium/calcium,Porites lobata,,millimole per mole,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N,error reported as 1 sigma of JCP-1 standard; error detail: 0.0194 ## Ba/Ca barium/calcium,Porites lobata,,micromole per mole,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N,error reported as 1 sigma of JCP-1 standard; error detail: 0.242 ## U/Ca uranium/calcium,Porites lobata,,micromole per mole,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N,error reported as 1 sigma of JCP-1 standard; error detail: 0.0092 ## Li/Mg lithium/magnesium,Porites lobata,,millimole per mole,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N,error reported as 1 sigma of JCP-1 standard; error detail: 0.0325 ## B/Mg boron/magnesium,Porites lobata,,millimole per mole,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N,error reported as 1 sigma of JCP-1 standard; error detail: 2.74 ## B/Ca boron/calcium,Porites lobata,,micromole per mole,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N,error reported as 1 sigma of JCP-1 standard; error detail: 11.79 ## U/Sr uranium/strontium,Porites lobata,,millimole per mole,,corals and sclerosponges,raw,inductively-coupled plasma mass spectrometry,N, Calculated from U/Ca and Sr/Ca; error calculated from propagating uncertainty of U/Ca and Sr/Ca ## Sr/Ca-SST sea surface temperature,strontium/calcium,,degree Celsius,,corals and sclerosponges; climate reconstructions,,,N,Sr/Ca-SST calculated using the Jimenez et al. 2018 composite slope (from cores WLF10-10 and WLF10-3) ## Li/Mg-SST sea surface temperature,lithium/magnesium,,degree Celsius,,corals and sclerosponges; climate reconstructions,,,N, #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: NaN Core_depth Lab_ID d13C d18O Sample_Name Latitude Longitude Depth d11B pHcf pHcf_press_corr DICcf Wcf [Ca] Mg/Ca Sr/Ca Ba/Ca U/Ca Li/Mg B/Mg B/Ca U/Sr Sr/Ca-SST Li/Mg-SST 588 M151 -2.414725201 -4.263806895 GW10-4D-B587 1.385783 -91.831667 10 24.55026 8.56148682 8.56101776 4181.496 17.13248 11.45897 4.378741 9.151806 3.980615 1.139421 1.418749 111.564 491.8533 7.886251 26.42445 27.31579 590 M152 -2.446127876 -5.08212324 GW10-4D-B589 1.385783 -91.831667 10 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 592 M153 -2.37303347 -4.825364682 GW10-4D-B591 1.385783 -91.831667 10 25.06983 8.56899069 8.5685253 3948.688 17.56003 11.37646 4.427629 9.05084 3.124023 1.102566 1.383485 113.8634 505.1899 7.82622 28.1958 27.82945 594 M154 -2.375036056 -4.84254931 GW10-4D-B593 1.385783 -91.831667 10 25.23267 8.59550336 8.59503568 3894.335 17.32315 11.92079 4.425937 9.115212 2.957051 1.101591 1.398189 115.7571 516.7029 7.891675 27.06645 27.6137 596 M155 -2.207820086 -4.823342961 GW10-4D-B595 1.385783 -91.831667 10 25.4729 8.60488965 8.60442268 3728.645 17.10703 11.57112 4.408484 9.092254 2.819029 1.107881 1.41739 120.0843 534.4759 7.86173 27.46923 27.33534 598 M156 -2.326973981 -4.874896845 GW10-4D-B597 1.385783 -91.831667 10 25.78528 8.63873345 8.63826447 3664.392 17.11547 11.66783 4.373352 9.148134 2.650031 1.112758 1.429634 123.4057 545.5578 7.912194 26.48887 27.15981 600 M157 -2.40407356 -4.873885984 GW10-4D-B599 1.385783 -91.831667 10 25.25733 8.59277311 8.59230613 3843.069 17.21477 11.40531 4.489427 9.098218 2.760554 1.093988 1.372324 115.7389 521.6343 7.883126 27.36459 27.99476 602 M158 -2.54325332 -4.903200938 GW10-4D-B601 1.385783 -91.831667 10 24.56154 8.54086282 8.54039701 4090.156 17.1556 11.609 4.567866 9.067287 3.044835 1.070793 1.347876 107.3538 494.4472 7.877957 27.90725 28.36162 604 M159 -2.427103304 -4.986091496 GW10-4D-B603 1.385783 -91.831667 10 24.50649 8.54849674 8.54802937 4164.887 17.16339 12.00444 4.516319 9.111494 3.372557 1.089087 1.358118 107.8225 490.3619 7.901845 27.13169 28.20713 606 M160 -2.457142101 -4.910276961 GW10-4D-B605 1.385783 -91.831667 10 24.48189 8.54331386 8.54284702 4209.438 17.36617 11.7495 4.612294 9.097167 3.780527 1.088989 1.347768 104.3377 484.0496 7.887627 27.38303 28.36325 608 M161 -2.405074853 -4.959809124 GW10-4D-B607 1.385783 -91.831667 10 25.12553 8.58144565 8.58097918 4027.071 17.84662 11.747 4.48861 9.08635 3.106387 1.087684 1.349184 111.3807 498.116 7.878259 27.57281 28.34182 610 M162 -2.210823966 -4.786951984 GW10-4D-B609 1.385783 -91.831667 10 25.50533 8.61919856 8.61872979 3833.345 17.42841 11.88325 4.305563 9.140777 2.739944 1.124363 1.438384 121.7907 524.2097 7.891947 26.61795 27.03528 612 M163 -2.330979154 -4.513008798 GW10-4D-B611 1.385783 -91.831667 10 25.5059 8.64172038 8.64124801 3763.547 16.73724 11.40235 4.154097 9.229097 2.769448 1.182115 1.521819 130.7085 542.7918 7.916122 25.06848 25.88455 614 M164 -2.192800688 -4.361379728 GW10-4D-B613 1.385783 -91.831667 10 25.4006 8.65274327 8.65226789 3705.057 16.02471 11.69187 4.015886 9.297865 2.655605 1.209958 1.601659 138.4099 559.935 7.953965 23.86202 24.841 616 M165 -2.566283064 -4.23502217 GW10-4D-B615 1.385783 -91.831667 10 24.94612 8.63444254 8.63396541 3817.321 15.57855 11.83689 4.004897 9.338244 3.242434 1.234479 1.641472 138.811 553.722 7.967108 23.15362 24.33991 618 M166 -2.625359365 -4.178413984 GW10-4D-B617 1.385783 -91.831667 10 23.68171 8.56021925 8.5597413 4187.674 14.75599 11.94034 4.162744 9.363741 4.616721 1.235599 1.626732 125.32 522.1801 7.991361 22.70629 24.524 620 M167 -2.192105613 -4.745425389 GW10-4D-B619 1.385783 -91.831667 10 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 622 M168 -1.907432116 -5.238806612 GW10-4D-B621 1.385783 -91.831667 10 24.36828 8.52296651 8.52250145 4229.76 17.4767 11.65333 4.739864 9.045081 2.955356 1.061216 1.35304 101.7102 477.88 7.866388 28.29682 28.28358 624 M169 -1.999551094 -5.01641731 GW10-4D-B623 1.385783 -91.831667 10 24.56595 8.53965548 8.53918989 4207.334 17.68335 11.81512 4.691527 9.061365 2.788863 1.073512 1.345314 102.987 480.0762 7.869015 28.01114 28.40045 626 M170 -1.935468327 -4.86377738 GW10-4D-B625 1.385783 -91.831667 10 24.41388 8.54735456 8.54688627 4129.774 16.76483 11.97368 4.45952 9.13033 2.845922 1.123646 1.416076 111.2607 497.3247 7.882297 26.80123 27.35428 628 M171 -1.93646962 -4.542323752 GW10-4D-B627 1.385783 -91.831667 10 24.76546 8.58902182 8.58855008 3860.068 15.96314 11.78697 4.185491 9.206255 2.77504 1.183607 1.547268 127.0515 536.0043 7.891623 25.46921 25.54609 630 M172 -1.861372628 -4.665648728 GW10-4D-B629 1.385783 -91.831667 10 25.35669 8.61393081 8.61346127 3771.67 16.81544 11.60753 4.345902 9.157029 2.705321 1.14937 1.473946 122.7309 536.228 7.880424 26.33283 26.53685 632 M173 -1.90242565 -4.752582728 GW10-4D-B631 1.385783 -91.831667 10 25.14888 8.58572627 8.58525925 3778.916 16.73942 11.67559 4.481937 9.097473 2.689584 1.117579 1.388232 117.2193 531.6783 7.856178 27.37766 27.75955 634 M174 -2.24286535 -5.073025496 GW10-4D-B633 1.385783 -91.831667 10 23.70275 8.46843807 8.46797489 4593.922 17.85945 11.64929 4.728191 8.998012 4.957404 1.062601 1.263258 92.88679 441.2647 7.817781 29.1226 29.68479 636 M175 -2.152748959 -5.183209287 GW10-4D-B635 1.385783 -91.831667 10 23.57359 8.45232161 8.45185955 4742.32 18.32643 12.00315 4.904476 8.966941 7.243846 1.043501 1.235592 87.13507 425.6735 7.807925 29.6677 30.13672 638 M176 -1.709176056 -4.900168356 GW10-4D-B637 1.385783 -91.831667 10 24.95217 8.58282347 8.58235491 4057.853 17.4337 11.86572 4.34463 9.135277 3.494397 1.134357 1.43503 114.7805 500.8638 7.875347 26.71444 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24.79343 8.58599155 8.58552108 4009.592 16.71145 11.55504 4.426736 9.187403 3.854919 1.165823 1.450005 116.7847 513.81 7.892524 25.79995 26.87107 660 M187 -1.73821356 -4.866809961 GW10-4D-B659 1.385783 -91.831667 10 23.91072 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 662 M188 -1.915442462 -4.88601631 GW10-4D-B661 1.385783 -91.831667 10 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 664 M189 -1.634079064 -4.830418984 GW10-4D-B663 1.385783 -91.831667 10 23.35948 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 666 M190 -1.795287274 -5.061906031 GW10-4D-B665 1.385783 -91.831667 10 24.84921 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 2 M192 -1.539333261 -4.245074661 GW10-5E-B3 1.385783 -91.831667 10 25.83328 8.67082115 8.67034793 4020.826 18.34937 11.22 4.365 9.262 3.229 1.136 1.470707 114.9894 507.0968 8.000245 24.49123 26.58176 4 M193 -1.616055786 -4.292641217 GW10-5E-B5 1.385783 -91.831667 10 26.08531 8.69599788 8.69552301 3930.304 18.24718 11.34 4.228 9.298 2.599 1.151 1.528042 122.3689 518.8727 8.019584 23.85965 25.80127 6 M194 -1.372135435 -4.285507043 GW10-5E-B7 1.385783 -91.831667 10 25.66953 8.67725795 8.67678162 3938.985 17.40025 11.36 4.127 9.327 2.493 1.174 1.588544 127.4292 526.0265 8.023038 23.35088 25.0088 8 M195 -1.812309259 -4.243109054 GW10-5E-B9 1.385783 -91.831667 10 25.13085 8.65726787 8.65678943 4065.604 16.75175 10.96 4.159 9.381 2.901 1.214 1.609926 124.7974 521.8278 8.03261 22.40351 24.73593 10 M196 -1.791282101 -4.109675472 GW10-5E-B11 1.385783 -91.831667 10 25.09911 8.62110822 8.62063546 4222.165 17.90191 11.06 4.427 9.249 2.942 1.139 1.469905 109.4854 490.3472 7.983913 24.7193 26.59288 12 M197 -1.966508417 -4.486726426 GW10-5E-B13 1.385783 -91.831667 10 25.35207 8.61413897 8.61366975 4139.717 18.43819 10.88 4.516 9.159 2.431 1.091 1.399641 106.8081 488.7865 7.947226 26.29825 27.59252 14 M198 -1.951489019 -4.707094007 GW10-5E-B15 1.385783 -91.831667 10 25.27827 8.61201487 8.61154514 4027.754 17.75642 11.11 4.523 9.169 2.321 1.093 1.432697 110.9487 504.1712 7.955005 26.12281 27.11613 16 M199 -1.983530402 -4.654529263 GW10-5E-B17 1.385783 -91.831667 10 25.10625 8.61336674 8.61289527 4194.401 17.94031 11.36 4.562 9.217 2.395 1.099 1.442165 107.1317 490.5043 7.996341 25.2807 26.98171 18 M200 -1.746223906 -4.621170868 GW10-5E-B19 1.385783 -91.831667 10 24.82862 8.5967973 8.59632556 4191.862 17.38848 11.05 4.585 9.221 2.487 1.105 1.463972 107.534 494.2945 7.993677 25.21053 26.67542 20 M201 -1.732561887 -4.466441952 GW10-5E-B21 1.385783 -91.831667 10 25.29633 8.60909434 8.60862537 4134.299 18.33504 11.36 4.66 9.153 2.366 1.083 1.391834 104.2032 489.4961 7.950112 26.40351 27.70666 22 M202 -1.523936808 -4.729332938 GW10-5E-B23 1.385783 -91.831667 10 24.7697 8.57295244 8.57248371 4214.214 17.7253 11.43 4.653 9.142 2.326 1.075 1.422898 102.8316 484.8218 7.947998 26.59649 27.25619 24 M203 -1.711178643 -4.428096519 GW10-5E-B25 1.385783 -91.831667 10 24.39129 8.54937474 8.54890638 4531.03 18.28287 11.25 4.723 9.144 2.44 1.06 1.317146 95.89009 454.7251 7.966658 26.5614 28.83228 26 M204 -1.675494365 -4.942533251 GW10-5E-B27 1.385783 -91.831667 10 24.23521 8.53332747 8.53285955 4404.444 17.58057 11.1 4.6 9.12 2.401 1.068 1.41252 100.7101 467.0533 7.933772 26.98246 27.40559 28 M205 -1.866720622 -4.823257724 GW10-5E-B29 1.385783 -91.831667 10 24.61489 8.56818702 8.56771744 4332.083 17.82713 11.02 4.399 9.162 2.353 1.118 1.449744 107.2872 475.0522 7.920237 26.24561 26.87474 30 M206 -1.642455274 -4.602901242 GW10-5E-B31 1.385783 -91.831667 10 24.78559 8.59867337 8.59820033 4087.215 16.79976 11.17 4.285 9.239 2.317 1.147 1.568778 117.9494 509.2197 7.965027 24.89474 25.26433 32 M207 -1.64208941 -4.644420659 GW10-5E-B33 1.385783 -91.831667 10 25.23451 8.64047573 8.64000089 3997.359 17.01711 11.08 4.229 9.291 2.351 1.173 1.560184 122.1476 520.4094 7.988149 23.98246 25.37644 34 M208 -1.564989831 -4.281521751 GW10-5E-B35 1.385783 -91.831667 10 25.18922 8.64950973 8.64903314 3939.617 16.50617 11.16 4.215 9.337 2.76 1.195 1.5745 124.8757 533.2562 8.009714 23.17544 25.19002 36 M209 -1.73821356 -4.152131612 GW10-5E-B37 1.385783 -91.831667 10 24.51003 8.57961391 8.57914183 4336.94 17.32714 11.22 4.545 9.233 2.986 1.134 1.450355 105.0927 482.29 7.973466 25 26.86613 38 M210 -1.571188779 -4.348715661 GW10-5E-B39 1.385783 -91.831667 10 23.92202 8.49384432 8.49337956 4660.755 18.34309 11.3 4.882 9.043 2.518 1.029 1.282747 88.46014 437.217 7.90009 28.33333 29.37236 40 M211 -1.641454089 -4.94657649 GW10-5E-B41 1.385783 -91.831667 10 23.63959 8.48969512 8.48922818 4578.119 17.19074 10.88 4.631 9.099 2.545 1.087 1.358775 96.59619 452.61 7.891669 27.35088 28.19725 42 M212 -1.641088116 -4.82132124 GW10-5E-B43 1.385783 -91.831667 10 24.26658 8.54597467 8.54550513 4438.278 17.58224 11.34 4.513 9.162 2.693 1.14 1.443024 103.1521 467.1011 7.895802 26.24561 26.96956 44 M213 -1.393768688 -4.597921077 GW10-5E-B45 1.385783 -91.831667 10 24.06716 8.55002259 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8.48316803 5289.683 17.30942 11.11 4.159 9.275 3.436 1.26 1.516333 98.51213 412.4853 7.875518 24.26316 25.95825 56 M219 -1.380751876 -4.640377217 GW10-5E-B57 1.385783 -91.831667 10 22.84635 8.50615049 8.50567254 5148.123 16.42751 11.13 4.106 9.366 2.947 1.296 1.616722 104.9074 432.3503 7.926533 22.66667 24.64997 58 M220 -1.326080944 -4.509906763 GW10-5E-B59 1.385783 -91.831667 10 23.31186 8.52741222 8.52693557 4871.237 16.5811 11.28 4.092 9.33 2.968 1.302 1.616163 108.9654 449.2387 7.883869 23.29825 24.65702 60 M221 -0.991248808 -4.47358524 GW10-5E-B61 1.385783 -91.831667 10 24.75331 8.61774141 8.6172652 4292.981 17.23055 11.18 4.108 9.321 2.781 1.274 1.602112 119.8828 492.9764 7.905968 23.45614 24.83524 62 M222 -1.024291485 -4.363401449 GW10-5E-B63 1.385783 -91.831667 10 24.95082 8.62613262 8.62565736 4175.197 17.18591 11.32 4.227 9.305 2.709 1.211 1.548798 118.812 502.9708 7.959942 23.73684 25.52592 64 M223 -1.631075184 -4.348238542 GW10-5E-B65 1.385783 -91.831667 10 24.88347 8.623414 8.62293882 4171.18 17.0205 11.56 4.314 9.311 2.745 1.171 1.503509 116.3897 504.8406 8.01037 23.63158 26.13158 66 M224 -1.792283395 -4.437194263 GW10-5E-B67 1.385783 -91.831667 10 24.30411 8.55549497 8.55502477 4466.282 17.63802 11.48 4.567 9.19 3.413 1.096 1.376944 101.2726 466.4084 7.972673 25.75439 27.92617 68 M225 -2.110008477 -4.510917573 GW10-5E-B69 1.385783 -91.831667 10 23.68498 8.48759402 8.48712802 4832.087 18.33693 10.99 4.807 9.079 4.164 1.048 1.28311 87.65481 426.6973 7.914986 27.70175 29.36658 70 M226 -2.359015365 -4.80009317 GW10-5E-B71 1.385783 -91.831667 10 23.24852 8.45743953 8.45697388 5266.179 19.04298 11.4 4.993 9.072 5.281 1.027 1.224935 78.41181 394.0074 7.931311 27.82456 30.3135 72 M227 -2.320966222 -4.948689659 GW10-5E-B73 1.385783 -91.831667 10 24.01529 8.51090166 8.51043541 4917.102 19.32346 11.09 4.749 9.087 4.05 1.055 1.267459 87.06134 417.3974 7.915212 27.5614 29.61704 74 M228 -1.944479966 -5.046743124 GW10-5E-B75 1.385783 -91.831667 10 24.35135 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23.753 8.55632148 8.55584598 5117.593 18.32928 11.24 4.246 9.331 5.445 1.136 1.43632 99.63014 423.776 8.069245 23.2807 27.06459 86 M234 -1.07535744 -4.762691333 GW10-5E-B87 1.385783 -91.831667 10 25.3537 8.65265641 8.65218163 4511.426 19.36409 11.22 4.26 9.309 3.955 1.118 1.447926 107.8813 461.3456 8.067237 23.66667 26.90034 88 M235 -0.90513759 -4.732365519 GW10-5E-B89 1.385783 -91.831667 10 26.0022 8.70058516 8.70010901 4155.646 18.95903 11.24 4.133 9.336 3.244 1.155 1.515656 119.1746 495.1914 8.053142 23.19298 25.96736 90 M236 -1.058335455 -4.436183403 GW10-5E-B91 1.385783 -91.831667 10 25.97826 8.71208969 8.71161142 4067.402 18.29667 11.43 4.077 9.386 3.136 1.174 1.56118 124.5725 510.8773 8.082038 22.31579 25.36341