# Makassar Strait 14KYr Foraminiferal Mg/Ca SST and d18Osw #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # 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 # # Data lines have no # # # NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/10420 # Landing_Page_Description: NOAA Landing Page of this file's parent study, which includes all study metadata. # # Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-ocean-10420.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Paleoceanography # # Dataset_DOI: 10.25921/1v6g-2z72 # # Science_Keywords: Other Hydroclimate Reconstruction, Sea Surface Temperature Reconstruction, Warm Pool #-------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/contributions_by_author/linsley2010/linsley2010-wpwp-SST-comp-noaa.txt # Data_Download_Description: NOAA Template File; Composite of Sea Surface Temperature in 200-Year Bins # #-------------------- # Contribution_Date # Date: 2010-08-02 #-------------------- # File_Last_Modified_Date # Date: 2024-02-26 #-------------------- # Title # Study_Name: Makassar Strait 14KYr Foraminiferal Mg/Ca SST and d18Osw #-------------------- # Investigators # Investigators: Linsley, B.K.; Rosenthal, Y.; Oppo, D.W. #-------------------- # Description_Notes_and_Keywords # Description: Planktonic foraminiferal Mg/Ca records of mixed-layer temperatures in the western Pacific warm pool. Included are new Globigerinoides ruber Mg/Ca data from the southern Makassar Strait, cores 13GGC, 70GGC and 10GGC, and regional average composite sediment core SST and d18Osw reconstructions utilizing these and previously published data. LAST UPDATE: 10/2010 - Addition of raw d18O and Mg/Ca by depth for cores 13GGC, 70GGC and 10GGC, plus 14C age table. Original receipt by WDC Paleo 8/2010. #-------------------- # Publication # Authors: Linsley, B.K., Y. Rosenthal, and D.W. Oppo # Published_Date_or_Year: 2010-08-01 # Published_Title: Holocene evolution of the Indonesian throughflow and the western Pacific warm pool # Journal_Name: Nature Geoscience # Volume: 3 # Edition: # Issue: # Pages: 578-583 # Report_Number: # DOI: 10.1038/ngeo920 # Publication_Place: # Publisher: # ISBN: # Online_Resource: # Other_Reference_Details: # Full_Citation: # Abstract: High sea surface temperatures in the western Pacific warm pool fuel atmospheric convection and influence tropical climate. This region also hosts the Indonesian throughflow, the network of currents through which surface and thermocline waters are transported from the western equatorial Pacific Ocean into the Indian Ocean. Here we show, using records of the δ18O and Mg/Ca of planktonic foraminifera from eight sediment cores, that from about 10,000 to 7,000 years ago, sea surface temperatures in the western sector of the western Pacific warm pool were about 0.5°C higher than during pre-industrial times. We also find that about 9,500 years ago, when the South China and Indonesian seas were connected by rising sea level, surface waters in the Makassar Strait became relatively fresher. We suggest that the permanent reduction of surface salinity initiated the enhanced flow at lower, thermocline depths seen in the modern Indonesian throughflow. However, the uniformly warm sea surface temperatures found upstream and downstream of the Indonesian throughflow indicate that the early Holocene warmth in this region was not directly related to reduced heat transport by the throughflow that may have resulted from surface freshening of the Makassar Strait. Instead, we propose that the elevated temperatures were the result of a westward shift or expansion of the boundaries of the western Pacific warm pool. #-------------------- # Publication # Authors: Levi, Camille; Labeyrie, Laurent; Bassinot, Franck; Guichard, Fran̤ois; Cortijo, Elsa; Waelbroeck, Claire; Caillon, Nicolas; Duprat, Josette; de Garidel-Thoron, Thibault; Elderfield, Harry # Published_Date_or_Year: 2007 # Published_Title: Low-latitude hydrological cycle and rapid climate changes during the last deglaciation # Journal_Name: Geochemistry, Geophysics, Geosystems # Volume: 8 # Edition: # Issue: 5 # Pages: # Report_Number: Q05N12 # DOI: 10.1029/2006GC001514 # Publication_Place: # Publisher: # ISBN: # Online_Resource: # Other_Reference_Details: # Full_Citation: # Abstract: Sea surface temperature and oxygen isotopic records from two well-dated Indian Ocean cores covering the last deglaciation show the occurrence of two periods of increased salinity along the route of warm surface water transport from the Indian to the Atlantic Ocean, one between 18 and 14.5 ka and the other during the Younger Dryas. Our results imply that during these periods, salt accumulated in the tropical Atlantic, creating favorable conditions for an abrupt resumption of the thermohaline circulation and abrupt northern hemisphere warming. Furthermore, we suggest that the observed pattern of millennial climate variability during the last glacial and deglaciation resulted from the interaction between the relatively slow rhythm of expansion and decay of the northern hemisphere ice sheets, and El Niño–Southern Oscillation variability, through changes in the position of the Intertropical Convergence Zone. This interaction generated an oscillator with millennial time response that operated at times of sufficient northern hemisphere ice sheets extent. #-------------------- # Publication # Authors: Visser, K., Thunell, R. and Stott, L. # Published_Date_or_Year: 2003-01-09 # Published_Title: Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation # Journal_Name: Nature # Volume: 42 # Edition: # Issue: # Pages: 152-155 # Report_Number: # DOI: 10.1038/nature01297 # Publication_Place: # Publisher: # ISBN: # Online_Resource: # Other_Reference_Details: # Full_Citation: # Abstract: Ocean–atmosphere interactions in the tropical Pacific region have a strong influence on global heat and water vapour transport and thus constitute an important component of the climate system. Changes in sea surface temperatures and convection in the tropical Indo-Pacific region are thought to be responsible for the interannual to decadal climate variability observed in extra-tropical regions, but the role of the tropics in climate changes on millennial and orbital timescales is less clear. Here we analyse oxygen isotopes and Mg/Ca ratios of foraminiferal shells from the Makassar strait in the heart of the Indo-Pacific warm pool, to obtain synchronous estimates of sea surface temperatures and ice volume. We find that sea surface temperatures increased by 3.5–4.0°C during the last two glacial—interglacial transitions, synchronous with the global increase in atmospheric CO2 and Antarctic warming, but the temperature increase occurred 2,000–3,000 years before the Northern Hemisphere ice sheets melted. Our observations suggest that the tropical Pacific region plays an important role in driving glacial—interglacial cycles, possibly through a system similar to how El Niño/Southern Oscillation regulates the poleward flux of heat and water vapour. #-------------------- # Publication # Authors: Rosenthal, Y., Oppo, D.W. and Linsley, B.K. # Published_Date_or_Year: 2003-04-01 # Published_Title: The amplitude and phasing of climate change during the last deglaciation in the Sulu Sea, western equatorial Pacific # Journal_Name: Geophysical Research Letters # Volume: 30 # Edition: # Issue: 8 # Pages: # Report_Number: 1428 # DOI: 10.1029/2002GL016612 # Publication_Place: # Publisher: # ISBN: # Online_Resource: # Other_Reference_Details: # Full_Citation: # Abstract: Variations in tropical sea surface temperature patterns and the phasing relative to climate change in higher-latitudes provide insight into the mechanisms of climate change on both orbital and shorter time-scales. Here, we present well-dated, high-resolution records of planktonic foraminiferal δ18O and Mg/Ca-based SST spanning the last deglaciation from the Sulu Sea, located in the western equatorial Pacific. The results indicate that the last glacial maximum was 2.3 ± 0.5°C cooler than present in the Sulu Sea with a concomitant decrease in sea surface salinity. The similarity between variations in surface salinity in the Sulu Sea, the western and eastern equatorial Pacific, and the Greenland ice-core record suggests that the observed changes in salinity reflect large-scale rearrangement of atmospheric patterns, which were coherent and synchronous throughout the Northern Hemisphere. The results suggest that the glacial equatorial Pacific climate was strongly influenced by both tropical, and extra-tropical forcing, although it is not clear whether interannual (ENSO) variability is a good analogue of glacial-interglacial climate change. #-------------------- # Publication # Authors: Steinke, S., M. Kienast, J. Groeneveld, L.-C. Lin, M.-T. Chen, and R. Rendle-Bühring # Published_Date_or_Year: 2008-04-01 # Published_Title: Proxy dependence of the temporal pattern of deglacial warming in the tropical South China Sea: Toward resolving seasonality # Journal_Name: Quaternary Science Reviews # Volume: 27 # Edition: # Issue: 7-8 # Pages: 688-700 # Report_Number: # DOI: 10.1016/j.quascirev.2007.12.003 # Publication_Place: # Publisher: # ISBN: # Online_Resource: # Other_Reference_Details: # Full_Citation: # Abstract: Sea surface temperatures (SSTs), reconstructed from two Globigerinoides ruber (white) morphotypes (G. ruber sensu stricto, (s.s.); G. ruber sensu lato, (s.l.)) Mg/Ca and alkenones (UK'37) from core MD01-2390 from the tropical South China Sea (SCS) during the last deglaciation reveal a proxy-dependent discrepancy in the temporal pattern of the deglacial warming. Alkenone data suggest that the deglacial warming is punctuated by a decrease in temperature between ~17 and 15 ka BP, corroborating previously published alkenone UK'37 SST records from the southern SCS. Within dating uncertainties, this cooling is coeval with the Heinrich Event 1 (H1) time interval in the North Atlantic region, underscoring the imprints of northern hemisphere forcing on tropical SCS ocean temperatures. The deglacial UK'37 SST minimum is also paralleled by a maximum in G. ruber morphotype-specific d18O. G. ruber Mg/Ca SST estimates suggest a morphotype-specific record of SSTs during the time interval of H1. Whereas G. ruber s.s. imply a continuous warming starting around 18 ka BP without any marked response to H1, G. ruber s.l.-based Mg/Ca SST estimates reveal a cooling around ~17–15 ka BP similar to the H1 interval cooling seen in the alkenone SST record. Similar proxy-dependent differences in deglacial surface water warming have been recorded in the eastern equatorial Pacific, implying a common pattern on both sides of the tropical Pacific Ocean. We submit that this discrepancy could be due to differences in seasonality of planktonic foraminifera G. ruber morphotypes and alkenone-producing algae. #-------------------- # Publication # Authors: Stott, L.D., K.G. Cannariato, R.C. Thunell, G.H. Haug, A. Koutavas, and S.P. Lund # Published_Date_or_Year: 2004-09-02 # Published_Title: Decline of surface temperature and salinity in the western tropical Pacific Ocean during the Holocene Epoch # Journal_Name: Nature # Volume: 431 # Edition: # Issue: # Pages: 56-59 # Report_Number: # DOI: 10.1038/nature02903 # Publication_Place: # Publisher: # ISBN: # Online_Resource: # Other_Reference_Details: # Full_Citation: # Abstract: In the present-day climate, surface water salinities are low in the western tropical Pacific Ocean and increase towards the eastern part of the basin. The salinity of surface waters in the tropical Pacific Ocean is thought to be controlled by a combination of atmospheric convection, precipitation, evaporation and ocean dynamics, and on interannual timescales significant variability is associated with the El Niņo/Southern Oscillation cycles. However, little is known about the variability of the coupled ocean-atmosphere system on timescales of centuries to millennia. Here we combine oxygen isotope and Mg/Ca data from foraminifers retrieved from three sediment cores in the western tropical Pacific Ocean to reconstruct Holocene sea surface temperatures and salinities in the region. We find a decrease in sea surface temperatures of ~0.5 °C over the past 10,000 yr, whereas sea surface salinities decreased by ~1.5 practical salinity units. Our data imply either that the Pacific basin as a whole has become progressively less salty or that the present salinity gradient along the Equator has developed relatively recently. #-------------------- # Publication # Authors: Xu, J., Holbourn, A., Kuhnt, W., Jian, Z. and Kawamura, H. # Published_Date_or_Year: 2008-08-30 # Published_Title: Changes in the thermocline structure of the Indonesian outflow during Terminations I and II # Journal_Name: Earth and Planetary Science Letters # Volume: 273 # Edition: # Issue: 1-2 # Pages: 152-162 # Report_Number: # DOI: 10.1016/j.epsl.2008.06.029 # Publication_Place: # Publisher: # ISBN: # Online_Resource: # Other_Reference_Details: # Full_Citation: # Abstract: We present centennial records of sea surface and upper thermocline temperatures in Core MD01-2378 from the Timor Sea, which provide new insights into the variability of the Indonesian outflow across the last two glacial terminations. Mg/Ca in Globigerinoides ruber (white s. s.) indicates an overall increase of 3.2 °C in sea surface temperature (SST) over Termination I. Following an early Holocene plateau at 11.3–6.4 ka, SSTs cooled by 0.6 °C during the middle to late Holocene (6.4–0.7 ka). The early Holocene warming occurred in phase with increasing northern hemisphere summer insolation, coinciding with northward displacement of the Intertropical Convergence Zone, enhanced boreal summer monsoon and expansion of the Indo-Pacific Warm Pool. Thermocline temperatures (Pulleniatina obliquiloculata Mg/Ca) gradually decreased from 24.5 to 21.5 °C since 10.3 ka, reflecting intensification of a cool thermocline throughflow. The vertical structure of the upper ocean in the Timor Sea evolved in similar fashion during the Holocene and MIS5e, although the duration of SST plateaux differed (11.3 to 6.4 ka in Termination I and from 129 to 119 ka in Termination II), which was probably due to the more intense northern hemisphere summer insolation during MIS 5e. During both terminations, SST increased simultaneously in the southern high latitudes and the tropical eastern Indian Ocean, suggesting virtually instantaneous atmospheric climate feedbacks between the high and low latitudes. #-------------------- # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: #-------------------- # Site_Information # Site_Name: Cores 10GGC, 70GGC, MD62, MD65, MD41, MD81, MD76, MD78 # Location: Western Pacific Ocean # Northernmost_Latitude: 8.783 # Southernmost_Latitude: -13.083 # Easternmost_Longitude: 133.433 # Westernmost_Longitude: 115.2 # Elevation_m: #-------------------- # Data_Collection # Collection_Name: WPWP_sst_comp # Earliest_Year: 25900 # Most_Recent_Year: 100 # Time_Unit: cal yr BP # Core_Length_m: # Parameter_Keywords: sea surface temperature # Notes: Black curve in Figure 2b in Linsley et al. 2010 #-------------------- # Chronology_Information # Chronology: # #-------------------- # Variables # # PaST_Thesaurus_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/PaST-thesaurus/SKOS/past-thesaurus-v1.0.rdf # PaST_Thesaurus_Download_Description: Paleoenvironmental Standard Terms (PaST) Thesaurus terms, definitions, and relationships in SKOS format. # # Variables format: Short_name what,material,error,units,seasonality,data_type,detail,method,data_format,additional_information # ## age_calBP age,,,calendar year before present,,paleoceanography;climate reconstructions,,,N, ## compSST_anom sea surface temperature,magnesium/calcium,,degree Celsius,,paleoceanography;climate reconstructions,anomalized;composited,,N,composite of 8 cores (13GGC; 70GGC; MD62; MD65; MD78; MD41; MD81; MD76) in 200 year non-overlapping bins; anomalized relative to the average of the last 2k ## num_meas number of samples,,,count,,paleoceanography;climate reconstructions,,,N,number of samples per bin ## SST_SE sea surface temperature,magnesium/calcium,one standard error,degree Celsius,,paleoceanography;climate reconstructions,,N,composite of 8 cores (13GGC; 70GGC; MD62; MD65; MD78; MD41; MD81; MD76) in 200 year non-overlapping bins ## SSTanom+SE sea surface temperature,magnesium/calcium,one standard error upper bound,degree Celsius,,paleoceanography;climate reconstructions,anomalized;composited,,N,composite of 8 cores (13GGC; 70GGC; MD62; MD65; MD78; MD41; MD81; MD76) in 200 year non-overlapping bins; anomalized relative to the average of the last 2k ## SSTanom-SE sea surface temperature,magnesium/calcium,one standard error lower bound,degree Celsius,,paleoceanography;climate reconstructions,anomalized;composited,,N,composite of 8 cores (13GGC; 70GGC; MD62; MD65; MD78; MD41; MD81; MD76) in 200 year non-overlapping bins; anomalized relative to the average of the last 2k # #-------------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: age_calBP compSST_anom num_meas SST_SE SSTanom+SE SSTanom-SE 100 -0.2410 23 0.1217 -0.1193 -0.3627 300 -0.2285 24 0.1018 -0.1266 -0.3303 500 0.2021 18 0.1672 0.3694 0.0349 700 0.1076 16 0.0846 0.1923 0.0230 900 0.3333 18 0.1551 0.4884 0.1781 1100 0.1990 19 0.0990 0.2980 0.1000 1300 0.1377 20 0.0922 0.2299 0.0454 1500 -0.0069 17 0.1123 0.1054 -0.1192 1700 -0.2305 18 0.1133 -0.1171 -0.3438 1900 -0.0977 16 0.1303 0.0327 -0.2280 2100 -0.1021 17 0.1149 0.0128 -0.2169 2300 -0.1170 18 0.1008 -0.0162 -0.2177 2500 0.0872 16 0.1310 0.2182 -0.0437 2700 0.0682 19 0.1110 0.1791 -0.0428 2900 0.0701 17 0.1540 0.2241 -0.0838 3100 0.3056 14 0.0901 0.3957 0.2155 3300 0.1583 16 0.1084 0.2667 0.0499 3500 0.1210 14 0.1292 0.2502 -0.0082 3700 0.1037 16 0.0999 0.2035 0.0038 3900 0.1257 17 0.0821 0.2077 0.0436 4100 -0.0617 16 0.0737 0.0121 -0.1354 4300 0.1200 16 0.1370 0.2570 -0.0169 4500 0.0722 18 0.0716 0.1438 0.0006 4700 0.2146 17 0.1136 0.3283 0.1010 4900 0.1797 18 0.1316 0.3113 0.0480 5100 0.3634 16 0.1317 0.4951 0.2317 5300 0.2435 17 0.1321 0.3757 0.1114 5500 0.0563 17 0.1074 0.1637 -0.0511 5700 0.2571 19 0.1234 0.3806 0.1337 5900 0.3497 19 0.1165 0.4662 0.2332 6100 0.4122 18 0.1519 0.5641 0.2603 6300 0.3271 21 0.0765 0.4036 0.2505 6500 0.3743 21 0.1285 0.5028 0.2458 6700 0.3997 16 0.1417 0.5414 0.2580 6900 0.2294 22 0.0710 0.3004 0.1583 7100 0.4388 21 0.1217 0.5605 0.3171 7300 0.1714 22 0.1055 0.2769 0.0659 7500 0.5001 18 0.1049 0.6050 0.3952 7700 0.4112 18 0.0993 0.5105 0.3119 7900 0.5170 18 0.1053 0.6223 0.4117 8100 0.5295 17 0.1460 0.6754 0.3835 8300 0.5834 18 0.1189 0.7022 0.4645 8500 0.3042 18 0.0882 0.3925 0.2160 8700 0.4079 17 0.0928 0.5008 0.3151 8900 0.4777 17 0.0842 0.5619 0.3935 9100 0.4055 19 0.1040 0.5095 0.3015 9300 0.2951 18 0.0857 0.3808 0.2094 9500 0.3669 17 0.1154 0.4823 0.2516 9700 0.4897 18 0.1328 0.6225 0.3569 9900 0.2361 17 0.1257 0.3617 0.1104 10100 0.1933 19 0.1060 0.2993 0.0873 10300 0.3907 19 0.1151 0.5058 0.2757 10500 0.2746 18 0.1345 0.4091 0.1401 10700 0.1254 14 0.1248 0.2502 0.0006 10900 0.2075 13 0.1131 0.3206 0.0944 11100 0.2811 15 0.1052 0.3864 0.1759 11300 0.1691 15 0.1286 0.2977 0.0405 11500 -0.0238 12 0.2107 0.1869 -0.2346 11700 0.0506 14 0.1546 0.2052 -0.1040 11900 0.0291 9 0.1341 0.1632 -0.1050 12100 -0.4324 10 0.1729 -0.2595 -0.6053 12300 -0.5826 14 0.1808 -0.4018 -0.7634 12500 -0.5520 13 0.2293 -0.3226 -0.7813 12700 -0.5475 15 0.2144 -0.3331 -0.7619 12900 -0.9091 12 0.2266 -0.6825 -1.1357 13100 -1.0973 13 0.1970 -0.9002 -1.2943 13300 -0.8615 13 0.2466 -0.6149 -1.1080 13500 -0.9944 12 0.2086 -0.7857 -1.2030 13700 -0.9695 13 0.2352 -0.7342 -1.2047 13900 -1.3416 12 0.2483 -1.0933 -1.5899 14100 -1.0851 16 0.2401 -0.8449 -1.3252 14300 -1.3308 15 0.2091 -1.1218 -1.5399 14500 -1.4480 13 0.1482 -1.2998 -1.5962 14700 -1.5397 13 0.1494 -1.3902 -1.6891 14900 -1.3599 10 0.2218 -1.1381 -1.5816 15100 -1.2811 10 0.1703 -1.1108 -1.4515 15300 -1.1257 9 0.2332 -0.8925 -1.3589 15500 -1.4403 10 0.2252 -1.2151 -1.6655 15700 -1.5550 9 0.1280 -1.4270 -1.6830 15900 -1.8400 9 0.1718 -1.6681 -2.0118 16100 -2.1556 11 0.1818 -1.9738 -2.3374 16300 -1.8107 10 0.1923 -1.6184 -2.0031 16500 -1.7963 8 0.2602 -1.5362 -2.0565 16700 -2.2971 10 0.2100 -2.0872 -2.5071 16900 -2.4559 8 0.1994 -2.2564 -2.6553 17100 -2.5203 11 0.1208 -2.3996 -2.6411 17300 -2.3459 12 0.2098 -2.1361 -2.5557 17500 -2.2777 10 0.2317 -2.0460 -2.5094 17700 -2.7700 13 0.1924 -2.5777 -2.9624 17900 -3.0834 12 0.2710 -2.8124 -3.3544 18100 -2.6855 13 0.1838 -2.5017 -2.8693 18300 -2.9698 11 0.1958 -2.7740 -3.1656 18500 -3.1334 13 0.1738 -2.9597 -3.3072 18700 -2.9352 9 0.3016 -2.6337 -3.2368 18900 -2.6173 8 0.1730 -2.4444 -2.7903 19100 -2.9356 8 0.1947 -2.7408 -3.1303 19300 -3.0792 12 0.1487 -2.9305 -3.2278 19500 -2.9827 11 0.1322 -2.8505 -3.1150 19700 -2.8219 8 0.1721 -2.6499 -2.9940 19900 -2.7459 8 0.3120 -2.4340 -3.0579 20100 -3.0150 9 0.1724 -2.8426 -3.1874 20300 -2.6747 8 0.1112 -2.5635 -2.7859 20500 -2.5741 8 0.1632 -2.4110 -2.7373 20700 -2.6438 8 0.2295 -2.4144 -2.8733 20900 -2.6657 8 0.1362 -2.5295 -2.8019 21100 -3.1159 8 0.1289 -2.9870 -3.2448 21300 -2.7992 7 0.0991 -2.7001 -2.8983 21500 -2.8408 8 0.2028 -2.6380 -3.0436 21700 -2.6925 7 0.1440 -2.5484 -2.8365 21900 -2.9358 5 0.2530 -2.6828 -3.1888 22100 -2.7636 3 0.0489 -2.7148 -2.8125 22300 -3.0549 3 0.3656 -2.6894 -3.4205 22500 -2.6858 4 0.4491 -2.2367 -3.1349 22700 -2.8765 3 0.2998 -2.5767 -3.1763 22900 -2.2117 2 0.1817 -2.0300 -2.3935 23100 -2.9473 3 0.3638 -2.5835 -3.3111 23300 -1.9217 1 0.0000 -1.9217 -1.9217 23500 -1.7329 3 0.3796 -1.3533 -2.1125 23700 -1.9057 1 0.0000 -1.9057 -1.9057 23900 -1.4026 2 0.6326 -0.7700 -2.0352 24100 -2.7915 3 0.7279 -2.0636 -3.5194 24300 -2.6100 3 0.4104 -2.1995 -3.0204 24500 -1.8860 1 0.0000 -1.8860 -1.8860 24700 -2.4010 2 0.5490 -1.8520 -2.9500 24900 -2.1904 2 0.3796 -1.8108 -2.5700 25100 -2.3814 4 0.3579 -2.0234 -2.7393 25300 -1.7738 3 0.8610 -0.9128 -2.6348 25500 -2.1342 3 0.4165 -1.7177 -2.5507 25700 -2.5755 2 0.2455 -2.3300 -2.8209 25900 -2.3620 1 0.0000 -2.3620 -2.3620