# Sulu Sea Core MD97-2141 Globoratalia tumida d18O and Mg/Ca Data Spanning Marine Isotope Stages 3-5 #----------------------------------------------------------------------- # 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/36695 # 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-36695.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/b285-4433 # # Science_Keywords: Sea Level Reconstruction, Tropics, Sea Surface Temperature Reconstruction #--------------------------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/paleocean/pacific/weiss2022/weiss2022-2141-ruber.txt # Data_Download_Description: NOAA Template File; MD97-2141 G. ruber Data # #--------------------------------------- # Contribution_Date # Date: 2022-07-26 #--------------------------------------- # File_Last_Modified_Date # Date: 2025-05-27 #--------------------------------------- # Title # Study_Name: Sulu Sea Core MD97-2141 Globoratalia tumida d18O and Mg/Ca Data Spanning Marine Isotope Stages 3-5 #--------------------------------------- # Investigators # Investigators: Weiss, Thomas L.; Linsley, Braddock K.; Gordon, Arnold, L.; Rosenthal, Yair; Dannenmann-Di Palma, Stefanie #--------------------------------------- # Description_Notes_and_Keywords # Description: All G. tumida data were published in Weiss et al. 2022. G. ruber Mg/Ca and d18Ow data were also published in Weiss et al. 2022. All G. ruber d18O data and G. ruber Mg/Ca and d18Ow data from 31.43-70.80 ka were published in Dannenmann et al. 2003 and Oppo et al. 2003 using the original age model from de Garidel-Thoron et al. 2001. G. tumida and and G. ruber data are presented here on the updated age model from Weiss et al. 2021 that is based on recalibration of the tie points from de Garidel-Thoron et al. 2001. # Provided Keywords: oxygen isotopes, thermocline, Mg/Ca based temperture #--------------------------------------- # Publication # Authors: Weiss, Thomas L.; Linsley, Braddock K.; Gordon, Arnold, L.; Rosenthal, Yair; Dannenmann-Di Palma, Stefanie # Published_Date_or_Year: 2022-09-01 # Published_Title: Constraints on Marine Isotope Stage 3 and 5 Sea Level from the Flooding History of the Karimata Strit in Indonesia # Journal_Name: Paleoceanography and Paleoclimatology # Volume: 37 # Edition: # Issue: 9 # Pages: # Report_Number: e2021PA004361 # DOI: 10.1029/2021PA004361 # Online_Resource: # Full_Citation: # Abstract: Global mean sea level (GMSL) during intermediate interglacial Marine Isotope Stage 3 (MIS 3) (60-26 ka) has proven difficult to constrain. Paleo-sea level estimates based on ice margin, modeling, and paleo-shoreline reconstructions indicate that MIS 3 GMSL was substantially higher than reconstructed from deep-ocean benthic foraminifera oxygen isotope (d18O) and coral records, implying much smaller ice sheets during MIS 3. Here we use the d18O and Mg/Ca chemistry of surface and thermocline dwelling foraminifera in the Sulu Sea in the western Pacific margins to estimate relative changes of the influx of South China Sea surface flow through the Sulu Sea over the last 140 ka. We show that this South China Sea throughflow is controlled in-part by changes in GMSL modulating the depth of the 36 m deep Karimata Strait at the southern end of the South China Sea. We constrain maximum allowable GMSL at the beginning and end of MIS 3 to -22±6 m and -29±5 m respectively and minimum allowable GMSL during interglacial stages MIS 5c and 5a (117-72 ka) to range from -3±8 to -8±8 m and -11±7 to -12±7 m respectively. Our results constrain MIS 3 GMSL, but do not rule out higher MIS 3 ice margin, modeling, and paleo-shoreline-based MIS 3 GMSL estimates or lower coral and seawater d18O-based estimates. Our results favor the highest MIS 5a and 5c GMSL estimates and confirm that the Sunda Shelf served as a land-bridge for human and megafauna migration during MIS 3 when humans first arrived in Borneo. #--------------------------------------- # Publication # Authors: de Garidel-Thoron, Thibault; Beaufort, Luc # Published_Date_or_Year: 2001-10-01 # Published_Title: Millenial-scale dynamics of the East Asian winter monsson during the last 200,000 years # Journal_Name: Paleoceanography # Volume: 16 # Edition: 5 # Issue: # Pages: 491-502 # Report_Number: # DOI: 10.1029/2000PA000557 # Online_Resource: # Full_Citation: # Abstract: The primary productivity dynamics of the last 200,000 years in the Sulu Sea was reconstructed using abundance of the coccolithophore Florisphaera profunda in the IMAGES MD97-2141 core. We find that primary productivity was enhanced during glacial periods, which we suggest is due to a stronger East Asian winter monsoon. During the last 80 kyr, eight significant increases in primary productivity (PP) in the Sulu Sea are similar to East Asian winter monsson changes recorded in Chinese Loess. The PP maxima are not linked with Heinrich events (HE) in the North Atlantic, although four PP peaks are synchronous with HE. The PP oscillations have frequencies near those of the Dansgaard-Oeschger cycles in Northen Hemisphere ice records and indicate a teleconnection of the East Asian winter monsoon with Greenland climate. In this Sulu Se recod the East Asian winter monsoon oscillates with periodicities of ~6, 4.2-3.4, 2.3, and 1.5 kyr. In particular, the 1.5 kyr cycle exhibits a strong and pervasive signal from stage 6 to the Holocene without any ice volume modulation. This stationarity suggests that the 1.5 kyr cycle is not driven by some high-latitude forcing. #--------------------------------------- # Publication # Authors: Dannenmann, S., Linsley, B. K., Oppo, D. W., Rosenthal, Y., & Beaufort, L. # Published_Date_or_Year: 2003-01-01 # Published_Title: East Asian monsoon forcing of suborbital variability in the Sulu Sea during Marine Isotope Stage 3: Link to Northern Hemisphere climate. # Journal_Name: Geochemistry, Geophysics, Geosystems # Volume: 4 # Edition: 1 # Issue: # Pages: 1-13 # Report_Number: # DOI: 10.1029/2002GC000390 # Online_Resource: # Full_Citation: # Abstract: We have generated a new high-resolution record of variations in planktonic foraminiferal oxygen isotopes (δ18O) and Mg/Ca from a sediment core (IMAGES 97-2141) in the Sulu Sea located in the Philippine archipelago of western tropical Pacific. This record reveals distinct, suborbital-scale δ18O changes, most notably during Marine Isotope Stage 3 (MIS3) (∼30,000 to 60,000 years B.P.). The amplitudes of these δ18O fluctuations (0.4 to 0.7‰) exceed that which can be attributed to sea level changes and must be due to changes in sea surface conditions. In the same interval, variations in planktonic foraminifera Mg/Ca suggest that suborbital surface ocean temperature variations of 1 to 1.5°C in the Sulu Sea were not in phase with δ18O. Combined, this evidence indicates that the MIS3 millennial δ18O events in the Sulu Sea were primarily the result of changes in surface water salinity, which today is directly related to the East Asian Monsoon (EAM) and its influence on the balance between surface water contributions from the South China Sea and Western Pacific Warm Pool (WPWP). Within dating uncertainties the MIS3 Sulu Sea δ18O suborbital variability indicates that times of fresher surface conditions in the Sulu Sea coincide with similar conditions in the WPWP [Stott et al., 2002] and also with intensifications of the summer EAM as recorded in the U-Th dated Chinese (Hulu Cave) speleothem δ18O record [Wang et al., 2001] and thus by inference with interstadials in the Greenland Ice core records. Combined, these results indicate that pronounced suborbital variability in the summer EAM and Intertropical Convergence Zone (ITCZ) during MIS3 was tightly coupled with climate conditions in the northern high latitudes. #--------------------------------------- # Publication # Authors: Oppo, D. W., Linsley, B. K., Rosenthal, Y., Dannenmann, S., & Beaufort, L. # Published_Date_or_Year: 2003-01-01 # Published_Title: Orbital and suborbital climate variability in the Sulu Sea, western tropical Pacific. # Journal_Name: Geochemistry, Geophysics, Geosystems # Volume: 4 # Edition: 1 # Issue: # Pages: 1-20 # Report_Number: # DOI: 10.1029/2001GC000260 # Online_Resource: # Full_Citation: # Abstract: A detailed record of planktic δ18O from a sediment core in the Sulu Sea, located between the South China Sea and the western Pacific warm pool, reveals that for the past 400 kyr (1 kyr = 1000 years), δ18O variability on orbital timescales is similar to that caused by changes in ice volume alone. This result indicates that in the Sulu Sea, temperature-driven changes in planktic δ18O on orbital times scales were generally compensated for by the effects of sea level and changes in seasonal monsoon intensity on the local freshwater budget, as well as by other changes in the tropical hydrologic cycle and their attendant effects on surface water δ18O. Increased freshening of the western tropical Pacific warm pool is reminiscent of La Niña conditions. However, we argue that the mean tropical climate state was not more La Niña-like than today on broader spatial scales. Suborbital variability occurred in the Sulu Sea throughout the past 400 kyr, suggesting little sensitivity to ice volume or to glacial-interglacial changes in tropical hydrology. Variations on 4–10 kyr timescales appear to be linked to those in the North Atlantic region, suggesting a common forcing of that variability. We suggest that Sulu Sea salinity variations were a response to suborbital climate variability in the North Atlantic region, transmitted via changes in the intensity of the East Asian summer monsoon. We suggest that a North Atlantic origin of that tropical suborbital variability can be reconciled with weak glacial amplification in the tropics if the tropical response is nonlinear. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: OCE-1736602, OCE-9710156, OCE-9987060 #--------------------------------------- # Funding_Agency # Funding_Agency_Name: Lamont-Doherty Earth Observatory # Grant: Climate Center #--------------------------------------- # Site_Information # Site_Name: MD97-2141 # Location: Sulu Sea # Northernmost_Latitude: 8.78 # Southernmost_Latitude: 8.78 # Easternmost_Longitude: 121.28 # Westernmost_Longitude: 121.28 # Elevation_m: -3633 #--------------------------------------- # Data_Collection # Collection_Name: MD97-2141 G.ruber Weiss2022 # First_Year: 127750 # Last_Year: 31430 # Time_Unit: calendar year before present # Core_Length_m: 36 # Parameter_Keywords: oxygen isotopes, trace metals in carbonates, reconstruction # Notes: #--------------------------------------- # Chronology_Information # Chronology: Radiocarbon # Chronology_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/templates/noaa-wds-paleo-14c-terms.csv # Chronology_Download_Description: Radiocarbon terms and definitions. # Chronology_Notes: Age model radiocarbon tie points newly updated in Weiss et al. 2022. The age model is based on orbital tuning older than the oldest radiocarbon tie point and was originally published in de Garidel-Thoron et al. 2001 # Rejection_Rationale: # Reservoir_Method: default CALIB 7.04 time-dependent reservoir correction of ∼400 years # Calibration_Method: Marine13 calibration curve from CALIB 7.04 # Age_Model_Method: # Missing_Values: # Chronology_Table: # depth_cm age_14C_BP1950 age_14C_1s_yr age_calib_BP1950 age_calib_neg1s_BP1950 age_calib_pos1s_BP1950 date_used material_dated lab_code calib_curve # 440 28000 130 31360 31244 31366 yes sacculifer (w/out sac) OS-17882 Marine13 # 487 30900 260 34458 34215 34691 yes ruber (white) OS-17912 Marine13 # 506.5 33000 310 36561 36117 36934 no sacculifer (w/out sac) OS-17917 Marine13 # 543 33600 590 37398 36655 38202 no sacculifer (w/out sac) OS-17911 Marine13 # 553 34300 390 38308 37803 38831 yes sacculifer (w/out sac) OS-17915 Marine13 # 594 36900 460 41087 40664 41566 yes sacculifer (w/out sac) OS-17918 Marine13 #--------------------------------------- # 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) # ## depth_cm depth,,,centimeter,,paleoceanography; climate reconstructions,,,N, ## age_ka age,,,calendar kiloyear before present,,paleoceanography; climate reconstructions,,,N, ## d18O delta 18O,Globigerinoides ruber,,per mil VPDB,,paleoceanography,,,N, ## Mg/Ca magnesium/calcium,Globigerinoides ruber,,millimole per mole,,paleoceanography,,,N, ## temperature sea water temperature,magnesium/calcium,,degree celsius,,paleoceanography; climate reconstructions,,,N,Seawater temperature calculated from Globigerinoides ruber magnesium/calcium ## d18Ow delta 18O,sea water; magnesium/calcium; delta 18O,,per mil VSMOW,,paleoceanography; climate reconstructions,,,N,calculated from Globigerinoides ruber magnesium/calcium and d18O #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: -999 depth_cm age_ka d18O Mg/Ca temperature d18Ow 441 31.43 -1.88 3.49 26.62 0.50 442 31.49 -2.04 -999 -999 -999 443 31.56 -1.70 3.53 26.75 0.71 444 31.62 -1.88 -999 -999 -999 445 31.69 -1.88 3.62 27.00 0.57 446 31.76 -1.92 -999 -999 -999 447 31.82 -2.02 3.47 26.54 0.34 448 31.89 -2.05 -999 -999 -999 449 31.95 -1.91 3.39 26.29 0.40 450 32.02 -1.94 3.47 26.54 0.43 451 32.09 -2.16 3.25 25.86 0.06 452 32.15 -1.88 -999 -999 -999 453 32.22 -2.22 3.50 26.64 0.17 454 32.28 -2.02 -999 -999 -999 455 32.35 -2.13 3.47 26.55 0.23 456 32.42 -2.12 -999 -999 -999 457 32.48 -2.17 3.57 26.86 0.25 458 32.55 -2.08 -999 -999 -999 459 32.61 -1.86 3.43 26.44 0.48 460 32.68 -1.99 -999 -999 -999 461 32.74 -2.22 3.35 26.19 0.07 462 32.81 -2.23 -999 -999 -999 463 32.88 -2.03 3.28 25.95 0.21 464 32.94 -2.33 3.70 27.22 0.17 465 33.01 -2.07 -999 -999 -999 466 33.07 -2.08 -999 -999 -999 467 33.14 -1.78 3.80 27.50 0.78 468 33.21 -2.04 -999 -999 -999 469 33.27 -2.06 3.79 27.49 0.50 470 33.34 -1.94 -999 -999 -999 471 33.40 -2.19 3.56 26.81 0.23 472 33.47 -2.02 -999 -999 -999 473 33.54 -2.04 -999 -999 -999 474 33.60 -1.98 3.67 27.14 0.51 475 33.67 -2.00 -999 -999 -999 476 33.73 -1.86 -999 -999 -999 477 33.80 -1.86 3.68 27.18 0.64 478 33.87 -2.02 -999 -999 -999 479 33.93 -2.17 3.83 27.60 0.41 480 34.00 -1.86 -999 -999 -999 481 34.06 -1.85 3.69 27.19 0.65 482 34.13 -1.93 -999 -999 -999 483 34.19 -1.92 -999 -999 -999 484 34.26 -2.13 3.71 27.25 0.38 485 34.33 -2.03 -999 -999 -999 486 34.39 -1.92 3.64 27.06 0.55 487 34.46 -2.02 -999 -999 -999 488 34.52 -2.08 -999 -999 -999 489 34.58 -2.22 3.84 27.62 0.37 490 34.63 -1.88 -999 -999 -999 491 34.69 -2.01 -999 -999 -999 492 34.75 -2.14 3.56 26.81 0.27 493 34.81 -2.04 -999 -999 -999 494 34.87 -2.02 3.78 27.45 0.53 495 34.93 -1.94 -999 -999 -999 496 34.98 -2.21 3.62 27.00 0.25 497 35.04 -2.03 -999 -999 -999 498 35.10 -1.90 3.80 27.51 0.67 499 35.16 -2.07 -999 -999 -999 500 35.22 -1.81 3.67 27.14 0.67 501 35.28 -1.78 -999 -999 -999 502 35.33 -2.04 -999 -999 -999 503 35.39 -1.89 -999 -999 -999 504 35.45 -2.08 -999 -999 -999 505 35.51 -2.07 3.83 27.60 0.51 506 35.57 -2.20 -999 -999 -999 507 35.63 -2.29 -999 -999 -999 508 35.68 -2.18 3.84 27.63 0.41 509 35.74 -1.92 -999 -999 -999 510 35.80 -1.88 3.81 27.54 0.68 511 35.86 -2.00 3.85 27.65 0.59 512 35.92 -2.21 3.70 27.22 0.30 513 35.98 -2.01 -999 -999 -999 514 36.03 -1.88 3.82 27.55 0.69 515 36.09 -2.08 3.59 26.90 0.35 516 36.15 -1.91 -999 -999 -999 517 36.21 -1.95 -999 -999 -999 518 36.27 -1.80 3.67 27.13 0.68 519 36.33 -1.88 -999 -999 -999 520 36.38 -1.96 3.83 27.59 0.62 521 36.44 -1.71 -999 -999 -999 522 36.50 -1.71 3.80 27.50 0.85 523 36.56 -1.80 -999 -999 -999 524 36.62 -1.81 -999 -999 -999 525 36.68 -1.84 3.62 26.99 0.61 526 36.73 -1.48 -999 -999 -999 527 36.79 -1.64 3.69 27.19 0.86 528 36.85 -1.74 -999 -999 -999 529 36.91 -1.48 3.61 26.96 0.97 530 36.97 -1.81 -999 -999 -999 531 37.03 -1.51 3.63 27.03 0.95 532 37.08 -1.52 -999 -999 -999 533 37.14 -1.74 3.80 27.52 0.83 534 37.20 -1.54 -999 -999 -999 535 37.26 -1.64 3.60 26.93 0.81 536 37.32 -1.55 -999 -999 -999 537 37.38 -1.74 -999 -999 -999 538 37.43 -1.45 -999 -999 -999 539 37.49 -1.49 -999 -999 -999 540 37.55 -1.63 3.86 27.68 0.97 541 37.61 -1.71 3.45 26.48 0.64 542 37.67 -1.47 -999 -999 -999 543 37.73 -1.47 -999 -999 -999 544 37.78 -1.49 3.58 26.87 0.94 545 37.84 -1.62 3.59 26.90 0.82 546 37.90 -1.68 3.57 26.86 0.75 547 37.96 -1.91 3.86 27.66 0.68 548 38.02 -1.64 -999 -999 -999 549 38.08 -1.77 -999 -999 -999 550 38.13 -1.82 3.67 27.13 0.66 551 38.19 -1.81 -999 -999 -999 552 38.25 -1.99 3.61 26.97 0.46 553 38.31 -2.15 -999 -999 -999 554 38.38 -1.91 -999 -999 -999 555 38.44 -1.89 3.63 27.03 0.58 556 38.51 -2.02 3.57 26.85 0.41 557 38.58 -1.84 3.74 27.33 0.68 558 38.65 -2.06 -999 -999 -999 559 38.72 -1.98 -999 -999 -999 560 38.78 -2.09 3.85 27.65 0.51 561 38.85 -1.83 -999 -999 -999 562 38.92 -1.96 -999 -999 -999 563 38.99 -1.90 3.60 26.95 0.55 564 39.05 -1.92 -999 -999 -999 565 39.12 -1.90 -999 -999 -999 566 39.19 -1.86 3.54 26.76 0.54 567 39.26 -1.86 -999 -999 -999 568 39.33 -1.92 3.39 26.31 0.39 569 39.39 -1.98 -999 -999 -999 570 39.46 -2.20 3.68 27.16 0.29 571 39.53 -1.90 -999 -999 -999 572 39.60 -1.90 -999 -999 -999 573 39.66 -1.98 -999 -999 -999 574 39.73 -1.76 -999 -999 -999 575 39.80 -1.95 3.56 26.82 0.47 576 39.87 -1.98 -999 -999 -999 577 39.94 -1.96 -999 -999 -999 578 40.00 -2.10 -999 -999 -999 579 40.07 -2.15 3.82 27.57 0.43 580 40.14 -1.99 -999 -999 -999 581 40.21 -1.88 3.58 26.87 0.55 582 40.27 -1.99 -999 -999 -999 583 40.34 -1.81 -999 -999 -999 584 40.41 -1.94 -999 -999 -999 585 40.48 -1.92 -999 -999 -999 586 40.55 -1.90 3.53 26.72 0.50 587 40.61 -2.09 -999 -999 -999 588 40.68 -2.03 3.53 26.74 0.37 589 40.75 -1.90 -999 -999 -999 590 40.82 -1.87 3.74 27.33 0.65 591 40.88 -2.03 3.74 27.34 0.50 592 40.95 -1.90 -999 -999 -999 593 41.02 -1.82 3.51 26.68 0.57 594 41.13 -1.72 -999 -999 -999 595 41.19 -1.88 -999 -999 -999 596 41.24 -2.04 -999 -999 -999 597 41.30 -2.03 3.85 27.64 0.56 598 41.36 -1.67 -999 -999 -999 599 41.42 -2.26 -999 -999 -999 600 41.47 -1.95 3.90 27.79 0.67 601 41.53 -2.08 -999 -999 -999 602 41.59 -2.15 3.89 27.76 0.47 603 41.65 -2.02 -999 -999 -999 604 41.70 -2.00 3.95 27.90 0.64 605 41.76 -2.03 -999 -999 -999 606 41.82 -2.23 -999 -999 -999 607 41.88 -1.92 -999 -999 -999 608 41.93 -1.89 -999 -999 -999 609 41.99 -2.04 -999 -999 -999 610 42.05 -1.94 3.85 27.66 0.65 611 42.11 -2.06 -999 -999 -999 612 42.16 -2.08 -999 -999 -999 613 42.22 -2.17 -999 -999 -999 614 42.28 -2.30 3.84 27.62 0.28 615 42.34 -2.06 -999 -999 -999 616 42.39 -2.08 3.74 27.33 0.45 617 42.45 -1.86 -999 -999 -999 618 42.51 -2.06 3.78 27.44 0.49 619 42.57 -1.98 -999 -999 -999 620 42.62 -1.99 3.96 27.94 0.66 621 42.68 -1.79 -999 -999 -999 622 42.74 -1.93 3.67 27.14 0.55 623 42.80 -1.90 -999 -999 -999 624 42.85 -2.02 3.77 27.41 0.52 625 42.91 -2.00 -999 -999 -999 626 42.97 -1.89 -999 -999 -999 627 43.03 -1.79 -999 -999 -999 628 43.08 -1.73 3.47 26.54 0.63 629 43.14 -1.76 -999 -999 -999 630 43.20 -1.81 -999 -999 -999 631 43.26 -1.99 -999 -999 -999 632 43.31 -1.80 -999 -999 -999 633 43.37 -1.94 -999 -999 -999 634 43.43 -1.89 -999 -999 -999 635 43.49 -2.03 -999 -999 -999 636 43.54 -1.94 3.46 26.53 0.42 637 43.60 -1.99 -999 -999 -999 638 43.66 -1.86 -999 -999 -999 639 43.72 -1.95 -999 -999 -999 640 43.77 -1.93 3.74 27.34 0.59 641 43.83 -1.94 -999 -999 -999 642 43.89 -2.00 -999 -999 -999 643 43.95 -1.95 -999 -999 -999 644 44.00 -1.96 3.58 26.89 0.47 645 44.06 -1.92 -999 -999 -999 646 44.12 -2.26 -999 -999 -999 647 44.18 -2.03 -999 -999 -999 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