# Eastern Subpolar North Atlantic Stable Isotope, Mg/Ca and SST Data During the Last Deglaciation #----------------------------------------------------------------------- # World Data Center for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # NOTE: Please cite original publication, online resource and date accessed when using this data. # If there is no publication information, please cite Investigator, title, online resource and date accessed. # # Online_Resource: http://www.hurricane.ncdc.noaa.gov/pls/paleox/f?p=519:1:::::P1_STUDY_ID: # Online Resource: ftp://ftp.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/benway2010/benway2010.txt # # Archive: Paleoceanography # #-------------------------------- # Contribution_Date # Date: 2013-05-15 #-------------------------------- # Title: Eastern Subpolar North Atlantic Stable Isotope, Mg/Ca and SST Data During the Last Deglaciation #-------------------------------- # Investigators: Benway, H.M.; McManus, J.F.; Oppo, D.W.; Cullen, J.L. #-------------------- # Description and Notes: # Description: The chronology for ODP Site 980 is based on 35 monospecific foraminifera accelerator mass spectrometry (AMS) 14C dates # (Globigerina bulloides, N. pachyderma (d), N. pachyderma (s)) spanning from the LGM to the late Holocene (Table 1). The Calib (Stuiver # and Reimer, 1993) program (version 6.0, Marine09 calibration data set of Reimer et al., 2009) was used to convert 14C ages to calendar ages. # The resulting age model suggests an average sedimentation rate of ~23 cm/ky throughout the deglacial interval. Calendar age # differences between N. pachyderma (s) and N. pachyderma (d) at the same depths (Table 1) are mostly on the order of 100-200 years, # except for a ~900-year difference just prior to the onset of the BA, which may reflect age differences in polar vs. subpolar water masses. # These age discrepancies are taken into account by applying slightly different age models for N. pachyderma (s) vs. N. pachyderma # (d) records (based on dual ages obtained at the four depth intervals listed in Table 1). Paired geochemical measurements of two planktonic foraminifer species, Neogloboquadrina pachyderma (dextral (d), or right-coiling) and N. pachyderma (sinistral (s), or left-coiling), constrain changes in upper ocean temperature and salinity and their relationship to global climate and deep ocean circulation. The oxygen isotope composition of foraminiferal calcite (d18Oc) reflects both ambient calcification temperature and seawater isotopic composition (d18Osw). Independent estimates of calcification temperature from Mg/Ca measurements differentiate temperature and d18Osw influences on d18Oc. # #-------------------- # Publication # Authors: Benway, H.M., J.F. McManus, D.W. Oppo, and J.L. Cullen # Journal_Name: Quaternary Science Reviews # Published_Title: Hydrographic changes in the eastern subpolar North Atlantic during the last deglaciation # Published_Date_or_Year: 2010 # Volume: 29 # Pages: 3336-3345 # DOI: 10.1016/j.quascirev.2010.08.013 # Abstract: Millennial-scale climate fluctuations of the last deglaciation have been tied to abrupt changes in the Atlantic Meridional Overturning Circulation (MOC). A key to understanding mechanisms of MOC collapse and recovery is the documentation of upper ocean hydrographic changes in the vicinity of North Atlantic deep convection sites. Here we present new high-resolution ocean temperature and d18Osw records spanning the last deglaciation from an eastern subpolar North Atlantic site that lies along the flow path of the North Atlantic Current, approaching deep convection sites in the Labrador and Greenland-Iceland-Norwegian (GIN) Seas. High-resolution temperature and d18Osw records from subpolar Site 980 help track the movement of the subpolar/subtropical front associated with temperature and Atlantic MOC changes throughout the last deglaciation. Distinct d18Osw minima during Heinrich 1 (H1) and the Younger Dryas (YD) correspond with peaks in ice-rafted debris and periods of reduced Atlantic MOC, indicating the presence of melt water in this region that could have contributed to MOC reductions during these intervals. Increased tropical and subtropical d18Osw during these periods of apparent freshening in the subpolar North Atlantic suggest a buildup of salt at low latitudes that served as a negative feedback on reduced Atlantic MOC. #-------------------------------- # Site Information: # Site_Name: ODP980 # Location: North Atlantic Ocean # Northernmost_Latitude: 55.48 # Southernmost_Latitude: 55.48 # Easternmost_Longitude: -14.7 # Westernmost_Longitude: -14.7 # Elevation: -2179 #-------------------------------- # Data Collection # Collection_Name: ODP980-Benway10 # Oldest_Year: 22000 # Most_Recent_Year: 10000 # Time_Unit: cal yr BP # Notes: IRD and Benthic d13C data was first published in: McManus, J. F., Oppo, D. W., Cullen, J. L., 1999. A 0.5-million-year record of millennial-scale climate variability in the North Atlantic. Science 283, 971-975. #-------------------------------- # Chronology: # 980 AGE CONTROL* - 14C AMS DATES FROM NATIONAL OCEAN SCIENCES ACCELERATOR MASS SPECTROMETRY FACILITY (NOSAMS) # Leg Site Hole Core T Sec Top (cm) Bot (cm) Depth (mcd) Species 14C Age (Yrs BP) 14C Error (Yrs) # 162 980 B 1 H 1 0 1 0.00 G. bulloides 1060 25 # 162 980 B 1 H 1 0 2 0.00 N. pachyderma (dex) 1190 35 # 162 980 B 1 H 1 35 37 0.35 N. pachyderma (dex) 1710 55 # 162 980 B 1 H 1 65 67 0.65 N. pachyderma (dex) 2910 35 # 162 980 B 1 H 1 74 75 0.74 G. bulloides 3290 35 # 162 980 B 1 H 1 85 87 0.86 N. pachyderma (dex) 3670 40 # 162 980 B 1 H 1 104 105 1.04 G. bulloides 4490 25 # 162 980 B 1 H 1 115 117 1.15 G. bulloides 4880 50 # 162 980 B 1 H 1 135 137 1.35 N. pachyderma (dex) 6240 65 # 162 980 B 1 H 2 11 12 1.61 G. bulloides 7230 70 # 162 980 B 1 H 2 20 22 1.70 N. pachyderma (dex) 7580 50 # 162 980 B 1 H 2 45 47 1.95 G. bulloides 8830 45 # 162 980 B 1 H 2 80 82 2.30 N. pachyderma (dex) 9620 50 # 162 980 B 1 H 2 99 100 2.49 G. bulloides 9780 70 # 162 980 B 1 H 2 145 147 2.95 G. bulloides 10900 55 # 162 980 B 1 H 3 0 2 3.00 N. pachyderma (sin) 11050 50 # 162 980 B 1 H 3 15 17 3.15 N. pachyderma (sin) 12050 75 # 162 980 B 1 H 3 15 17 3.15 N. pachyderma (dex) 12100 60 # 162 980 B 1 H 3 31 32 3.31 N. pachyderma (sin) 12200 55 # 162 980 B 1 H 3 31 32 3.31 N. pachyderma (dex) 12450 60 # 162 980 B 1 H 3 40 42 3.40 N. pachyderma (sin) 12550 50 # 162 980 B 1 H 3 45 47 3.45 N. pachyderma (sin) 12800 70 # 162 980 B 1 H 3 55 57 3.55 N. pachyderma (sin) 13100 55 # 162 980 B 1 H 3 55 57 3.55 N. pachyderma (dex) 12700 90 # 162 980 B 1 H 3 65 67 3.65 N. pachyderma (sin) 13250 55 # 162 980 B 1 H 3 65 67 3.65 N. pachyderma (dex) 13050 100 # 162 980 B 1 H 3 80 82 3.80 N. pachyderma (sin) 15300 80 # 162 980 C 2 H 1 45 46 4.02 N. pachyderma (sin) 15350 80 # 162 980 C 2 H 1 55 56 4.12 N. pachyderma (sin) 15450 55 # 162 980 C 2 H 1 70 71 4.27 N. pachyderma (sin) 16000 75 # 162 980 C 2 H 1 74 76 4.31 N. pachyderma (sin) 16450 75 # 162 980 C 2 H 1 84 86 4.41 N. pachyderma (sin) 16650 95 # 162 980 C 2 H 1 94 96 4.51 N. pachyderma (sin) 17200 85 # 162 980 C 2 H 1 114 116 4.71 N. pachyderma (sin) 17750 80 # 162 980 C 2 H 1 134 136 4.91 N. pachyderma (sin) 18500 65 # # *Details of age model available in: Benway, H.M., J.F. McManus, D.W. Oppo, and J.L. Cullen. 2010. Hydrographic changes in the eastern subpolar North Atlantic during the last deglaciation. Quaternary Science Reviews 29, 3336-3345. #-------------------------------- # Variables # # Data variables follow (have no #) # Variables list, one per line, shortname-tab Var components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Char or Numeric data) ## depth_m Depth,,,m,,,,,N ## age_calkaBP age,,,calendar kiloyears before 1950 AD,,,,,N ## age_calkaBP-np.d age,from Neogloboquadrina pachyderma right coiling 14C dates,,calendar kiloyears before 1950 AD,,paleoceanography,,,N ## d18On.pachy-l.VPDB delta 18O,Neogloboquadrina pachyderma left coiling,,per mil VPDB,,paleoceanography,,,N ## d18On.pachy-r.VPDB delta 18O,Neogloboquadrina pachyderma right coiling,,per mil VPDB,,paleoceanography,,,N ## Mg/Ca-n.pachy-l Magnesium/Calcium,Neogloboquadrina pachyderma left coiling,,mmol/mol,,paleoceanography,,,N ## Mg/Ca-n.pachy-r Magnesium/Calcium,Neogloboquadrina pachyderma right coiling,,mmol/mol,,paleoceanography,,,N ## sst-cold.MAT sea surface temperature,,,degrees C,,paleoceanography,cold season,modern analog technique,N ## sst-warm.MAT sea surface temperature,,,degrees C,,paleoceanography,warm season,modern analog technique,N ## N.pachy-l% Neogloboquadrina pachyderma left coiling,,,percent,,paleoceanography,,,N ## IRD Ice rafted debris,,,lithics/g,,paleoceanography,,,N ## d13C-benth.VPDB delta 18O,benthic foraminifers,,per mil VPDB,,paleoceanography,,,N # Data: # Missing Values: NA depth_m age_calkaBP age_calkaBP-np.d d18On.pachy-l.VPDB d18On.pachy-r.VPDB Mg/Ca-n.pachy-l Mg/Ca-n.pachy-r sst-cold.MAT sst-warm.MAT N.pachy-l% IRD d13C-benth.VPDB notes 2.45 10.581 NA NA NA NA NA NA NA 0.651 7.13 1.000 162 980B 1-H-2 95-97 2.48 10.597 NA NA NA NA NA NA NA 0.585 NA NA 162 980B 1-H-2 98-100 2.50 10.636 NA NA 1.590 NA 1.676 9.170 13.000 0.421 NA NA 162 980B 1-H-2 100-102 2.53 10.695 NA NA 1.872 NA 1.572 NA NA NA NA NA 162 980B 1-H-2 103-104 2.54 10.707 NA NA NA NA NA 9.280 13.180 0.631 NA NA 162 980B 1-H-2 104-105 2.55 10.754 NA NA 1.822 NA 1.473 8.670 12.340 0.309 0.000 NA 162 980B 1-H-2 105-107 2.58 10.813 NA NA 1.772 NA 1.339 NA NA NA NA NA 162 980B 1-H-2 108-109 2.59 10.837 NA NA NA NA NA 9.170 13.000 0.554 NA NA 162 980B 1-H-2 109-110 2.60 10.860 NA NA NA NA 1.310 NA NA NA NA NA 162 980B 1-H-2 110-111 2.61 10.872 NA NA NA NA NA 9.160 13.000 1.425 NA NA 162 980B 1-H-2 111-112 2.63 10.931 NA NA NA NA 1.479 NA NA NA NA NA 162 980B 1-H-2 113-114 2.64 10.943 NA NA NA NA NA 9.200 13.070 1.047 NA NA 162 980B 1-H-2 114-115 2.65 10.990 NA 2.206 1.574 NA 1.290 8.920 12.740 2.525 14.090 NA 162 980B 1-H-2 115-117 2.68 11.050 NA 2.849 1.716 NA 1.363 NA NA NA NA NA 162 980B 1-H-2 118-119 2.69 11.061 NA NA NA NA NA 9.160 13.000 2.231 NA NA 162 980B 1-H-2 119-120 2.70 11.109 NA NA 1.655 NA 1.366 8.860 12.740 2.120 NA NA 162 980B 1-H-2 120-122 2.74 11.180 NA NA NA NA NA 8.880 12.670 1.070 NA NA 162 980B 1-H-2 124-125 2.75 11.227 NA NA 1.852 NA 1.279 8.640 12.420 1.003 4.740 NA 162 980B 1-H-2 125-127 2.78 11.286 NA 3.068 NA NA 1.184 NA NA NA NA NA 162 980B 1-H-2 128-129 2.79 11.298 NA NA NA NA NA 9.160 13.000 2.410 NA NA 162 980B 1-H-2 129-130 2.80 11.333 NA NA 2.041 NA 1.451 NA NA NA NA NA 162 980B 1-H-2 130-131 2.81 11.345 NA NA NA NA NA 9.070 13.100 1.871 NA NA 162 980B 1-H-2 131-132 2.83 11.404 NA 3.125 2.050 NA 1.585 NA NA NA NA NA 162 980B 1-H-2 133-134 2.84 11.416 NA NA NA NA NA 8.620 12.360 3.383 NA NA 162 980B 1-H-2 134-135 2.85 11.463 NA NA 1.670 NA 1.153 8.360 12.150 5.330 28.160 0.950 162 980B 1-H-2 135-137 2.88 11.523 NA NA 2.029 0.982 1.074 NA NA NA NA 0.930 162 980B 1-H-2 138-139 2.89 11.534 NA NA NA NA NA 8.560 12.400 6.452 NA NA 162 980B 1-H-2 139-140 2.90 11.582 NA NA 1.835 NA 0.858 6.290 10.990 16.390 NA NA 162 980B 1-H-2 140-142 2.93 11.641 NA 3.188 1.949 0.821 1.137 NA NA NA NA NA 162 980B 1-H-2 143-144 2.94 11.665 NA 3.040 1.733 0.791 1.212 7.590 11.730 13.348 NA NA 162 980B 1-H-2 144-145 2.95 11.700 NA NA NA NA NA 5.650 10.460 48.797 113.850 0.610 162 980B 1-H-2 145-147 2.97 11.778 11.831 3.001 1.910 NA 0.886 NA NA NA NA NA 162 980B 1-H-2 147-148 2.98 11.830 NA 3.114 NA 0.848 NA NA NA NA NA NA 162 980B 1-H-2 148-149 2.99 11.882 12.006 3.058 2.062 0.780 NA 4.940 9.780 70.732 NA NA 162 980B 1-H-2 149-150 3.00 11.960 NA NA NA NA NA 4.200 9.560 70.038 523.500 0.940 162 980B 1-H-3 0-2 3.02 12.120 12.269 3.128 2.471 0.787 0.941 NA NA NA NA NA 162 980B 1-H-3 2-3 3.03 12.227 12.356 3.177 1.742 0.860 NA NA NA NA 73.500 NA 162 980B 1-H-3 3-4 3.04 12.280 NA NA NA NA NA 6.820 11.160 23.491 NA NA 162 980B 1-H-3 4-5 3.05 12.493 12.575 2.950 2.293 0.822 1.239 6.070 10.600 26.000 20.760 0.770 162 980B 1-H-3 5-7 3.08 12.760 12.794 3.097 2.489 0.810 1.172 NA NA NA NA NA 162 980B 1-H-3 8-9 3.09 12.813 NA NA NA NA NA NA NA NA 263.113 NA 162 980B 1-H-3 9-10 3.10 NA 12.969 NA 2.500 NA 0.938 NA NA NA NA NA 162 980B 1-H-3 10-11 3.11 13.027 NA NA NA NA NA NA NA NA 33.489 NA 162 980B 1-H-3 11-12 3.13 13.293 13.231 NA 2.606 0.830 1.016 NA NA NA NA NA 162 980B 1-H-3 13-14 3.14 13.347 NA NA NA NA NA NA NA NA 1.336 NA 162 980B 1-H-3 14-15 3.15 13.560 13.450 3.204 2.256 0.778 NA NA NA NA 34.670 0.960 162 980B 1-H-3 15-17 3.18 13.613 13.487 NA 2.487 0.888 1.171 NA NA NA NA NA 162 980B 1-H-3 18-19 3.19 13.624 NA NA NA NA NA NA NA NA 5.553 NA 162 980B 1-H-3 19-20 3.20 13.667 13.524 NA 2.434 0.832 1.329 NA NA NA NA NA 162 980B 1-H-3 20-22 3.23 13.720 13.561 3.073 2.411 0.890 1.048 NA NA NA NA NA 162 980B 1-H-3 23-24 3.24 13.730 NA NA NA NA NA NA NA NA 15.057 NA 162 980B 1-H-3 24-25 3.25 13.773 NA NA NA NA NA 8.560 12.440 3.323 6.200 0.770 162 980B 1-H-3 25-27 3.27 13.805 13.621 2.911 2.305 NA 1.153 NA NA NA NA NA 162 980B 1-H-3 27-28 3.29 13.837 NA NA NA NA NA NA NA NA 10.394 NA 162 980B 1-H-3 29-30 3.30 13.869 13.665 3.258 2.535 0.893 1.098 NA NA NA NA NA 162 980B 1-H-3 30-31 3.31 13.879 NA NA NA NA NA NA NA NA 4.674 NA 162 980B 1-H-3 31-32 3.33 13.909 13.717 3.315 2.417 0.817 1.424 NA NA NA NA NA 162 980B 1-H-3 33-34 3.34 13.914 NA NA NA NA NA NA NA NA 6.681 NA 162 980B 1-H-3 34-35 3.35 13.933 13.763 3.123 2.678 0.872 1.229 NA NA NA 11.420 0.940 162 980B 1-H-3 35-37 3.38 13.956 13.809 3.205 2.611 0.844 1.045 NA NA NA NA NA 162 980B 1-H-3 38-39 3.39 13.961 NA NA NA NA NA NA NA NA 34.660 NA 162 980B 1-H-3 39-40 3.40 13.980 13.855 3.210 2.280 0.875 1.072 NA NA NA NA NA 162 980B 1-H-3 40-42 3.43 14.190 13.900 3.165 2.549 0.917 1.138 NA NA NA NA NA 162 980B 1-H-3 43-44 3.44 14.232 NA NA NA NA NA NA NA NA 24.216 NA 162 980B 1-H-3 44-45 3.45 14.400 13.946 3.396 2.492 0.814 1.116 5.780 10.800 30.675 12.000 0.880 162 980B 1-H-3 45-47 3.48 14.563 13.992 NA 2.840 0.832 1.159 NA NA NA NA NA 162 980B 1-H-3 48-49 3.49 14.595 NA NA NA NA NA NA NA NA 30.126 NA 162 980B 1-H-3 49-50 3.50 14.693 14.029 NA 2.429 0.747 NA NA NA NA NA NA 162 980B 1-H-3 50-51 3.51 14.725 NA NA NA NA NA NA NA NA 21.255 NA 162 980B 1-H-3 51-52 3.53 14.888 14.084 2.599 2.320 NA 1.205 NA NA NA NA NA 162 980B 1-H-3 53-54 3.54 14.920 NA NA NA NA NA NA NA NA 8.172 NA 162 980B 1-H-3 54-55 3.55 15.050 14.130 3.256 2.265 NA 1.209 NA NA NA 15.850 0.570 162 980B 1-H-3 55-57 3.58 15.088 14.348 NA 2.458 0.843 1.608 NA NA NA NA NA 162 980B 1-H-3 58-59 3.59 15.095 NA NA NA NA NA NA NA NA 62.107 NA 162 980B 1-H-3 59-60 3.60 15.125 14.565 2.832 2.213 NA NA NA NA NA NA NA 162 980B 1-H-3 60-62 3.63 15.163 14.783 NA 2.336 0.850 1.894 NA NA NA NA NA 162 980B 1-H-3 63-64 3.64 15.170 NA NA NA NA NA NA NA NA 22.086 NA 162 980B 1-H-3 64-65 3.65 15.200 15.000 3.268 2.515 0.745 1.314 8.140 12.260 6.707 47.100 0.400 162 980B 1-H-3 65-67 3.68 15.417 15.250 3.205 2.442 0.748 1.271 NA NA NA NA NA 162 980B 1-H-3 68-69 3.69 15.460 NA NA NA NA NA NA NA NA 70.797 NA 162 980B 1-H-3 69-70 3.70 15.590 15.450 3.657 2.389 0.727 1.196 NA NA NA NA NA 162 980B 1-H-3 70-71 3.71 15.633 NA NA NA NA NA NA NA NA 42.973 NA 162 980B 1-H-3 71-72 3.73 15.850 15.750 3.129 2.057 0.792 NA NA NA NA NA NA 162 980B 1-H-3 73-74 3.74 15.893 NA NA NA NA NA NA NA NA 355.996 NA 162 980B 1-H-3 74-75 3.75 16.067 16.000 3.250 2.524 NA 1.252 NA NA NA 170.320 0.210 162 980B 1-H-3 75-77 3.78 16.283 16.250 3.230 NA 0.832 1.247 NA NA NA NA NA 162 980B 1-H-3 78-79 3.79 16.327 NA NA NA NA NA NA NA NA 504.796 NA 162 980B 1-H-3 79-80 3.80 16.500 NA 2.868 2.104 NA 1.305 NA NA NA NA NA 162 980B 1-H-3 80-82 3.83 16.688 NA 3.341 1.949 0.879 1.430 NA NA NA NA NA 162 980B 1-H-3 83-84 3.84 16.726 NA NA NA NA NA NA NA NA 173.819 NA 162 980B 1-H-3 84-85 3.85 16.876 NA 3.024 1.678 0.779 1.269 5.900 10.610 42.414 296.510 0.350 162 980B 1-H-3 85-87 3.88 17.064 NA 2.978 2.810 0.837 NA NA NA NA NA NA 162 980B 1-H-3 88-89 3.89 17.102 NA NA NA NA NA NA NA NA 818.799 NA 162 980B 1-H-3 89-90 3.90 17.215 NA 3.427 2.805 0.739 NA NA NA NA NA NA 162 980B 1-H-3 90-91 3.91 17.252 NA NA NA NA NA NA NA NA 508.968 NA 162 980B 1-H-3 91-92 3.92 17.328 NA NA NA NA NA NA NA NA 543.340 0.360 162 980B 1-H-3 92-93 3.94 17.516 NA 3.471 3.430 0.668 NA NA NA NA 772.093 NA 162 980C 2-H-1 37-38 3.95 17.553 NA NA NA NA NA NA NA NA 909.240 NA 162 980C 2-H-1 38-39 3.96 17.629 NA NA NA NA NA NA NA NA 609.660 0.400 162 980C 2-H-1 39-40 3.97 17.741 NA 4.035 3.355 0.676 NA NA NA NA NA NA 162 980C 2-H-1 40-41 3.98 17.779 NA NA NA NA NA NA NA NA 671.927 NA 162 980C 2-H-1 41-42 4.00 17.967 NA 4.048 3.762 0.717 NA NA NA NA NA NA 162 980C 2-H-1 43-44 4.01 18.005 NA NA NA NA NA NA NA NA 287.198 NA 162 980C 2-H-1 44-45 4.02 18.080 NA NA NA NA NA NA NA NA 243.390 0.800 162 980C 2-H-1 45-46 4.04 18.098 NA 4.219 3.947 0.686 NA NA NA NA NA NA 162 980C 2-H-1 47-48 4.05 18.101 NA NA NA NA NA 0.530 5.750 92.340 109.499 0.780 162 980C 2-H-1 48-50 4.06 18.108 NA NA NA NA NA NA NA NA 196.940 NA 162 980C 2-H-1 49-50 4.10 18.140 NA 4.163 4.192 0.601 NA NA NA NA NA NA 162 980C 2-H-1 53-54 4.12 18.143 NA NA NA NA NA NA NA NA 300.667 NA 162 980C 2-H-1 55-56 4.14 18.247 NA 4.074 4.199 0.660 NA NA NA NA NA NA 162 980C 2-H-1 57-58 4.15 18.266 NA NA NA NA NA NA NA NA 359.927 NA 162 980C 2-H-1 58-59 4.17 18.363 NA 4.178 NA 0.725 NA NA NA NA NA NA 162 980C 2-H-1 60-61 4.18 18.382 NA NA NA NA NA NA NA NA 378.588 NA 162 980C 2-H-1 61-62 4.20 18.479 NA NA NA NA NA NA NA NA NA 0.850 162 980C 2-H-1 63-64 4.21 18.498 NA 4.185 NA 0.657 NA -0.170 4.760 92.611 308.450 NA 162 980C 2-H-1 64-66 4.22 18.537 NA NA NA NA NA NA NA NA 634.211 NA 162 980C 2-H-1 65-66 4.24 18.634 NA 4.140 4.261 0.599 NA NA NA NA NA NA 162 980C 2-H-1 67-68 4.25 18.653 NA NA NA NA NA NA NA NA 635.853 NA 162 980C 2-H-1 68-69 4.30 19.157 NA 4.202 NA 0.641 NA NA NA NA NA NA 162 980C 2-H-1 73-74 4.31 19.224 NA NA NA NA NA NA NA NA 74.972 NA 162 980C 2-H-1 74-76 4.34 19.378 NA 4.442 4.194 0.587 NA NA NA NA NA NA 162 980C 2-H-1 77-78 4.35 19.381 NA NA NA NA NA NA NA NA 126.972 NA 162 980C 2-H-1 78-79 4.37 19.399 NA 4.413 3.882 0.603 NA NA NA NA NA NA 162 980C 2-H-1 80-81 4.38 19.402 NA NA NA NA NA NA NA NA 171.216 NA 162 980C 2-H-1 81-82 4.40 19.420 NA 4.189 4.093 0.630 NA NA NA NA NA NA 162 980C 2-H-1 83-84 4.41 19.423 NA NA NA NA NA 1.610 6.310 92.580 215.420 NA 162 980C 2-H-1 84-86 4.42 19.430 NA NA NA NA NA NA NA NA 120.000 0.820 162 980C 2-H-1 85-86 4.44 19.593 NA 4.205 3.961 0.626 NA NA NA NA NA NA 162 980C 2-H-1 87-88 4.45 19.625 NA NA NA NA NA NA NA NA 96.134 NA 162 980C 2-H-1 88-89 4.47 19.788 NA 4.402 4.310 0.659 NA NA NA NA NA NA 162 980C 2-H-1 90-91 4.48 19.820 NA NA NA NA NA NA NA NA 130.367 NA 162 980C 2-H-1 91-92 4.50 19.983 NA 4.016 4.069 0.621 NA NA NA NA NA NA 162 980C 2-H-1 93-94 4.51 20.015 NA 4.174 4.056 0.555 NA NA NA NA NA NA 162 980C 2-H-1 94-96 4.52 20.080 NA NA NA NA NA NA NA NA 194.071 NA 162 980C 2-H-1 95-96 4.54 20.129 NA 4.191 4.188 0.649 NA NA NA NA NA NA 162 980C 2-H-1 97-98 4.55 20.139 NA NA NA NA NA NA NA NA 215.115 NA 162 980C 2-H-1 98-99 4.57 20.187 NA 4.094 4.062 0.730 NA NA NA NA NA NA 162 980C 2-H-1 100-101 4.58 20.197 NA NA NA NA NA NA NA NA 210.959 NA 162 980C 2-H-1 101-102 4.60 20.246 NA 4.074 3.995 0.537 NA NA NA NA NA NA 162 980C 2-H-1 103-104 4.61 20.256 NA NA NA NA NA 0.890 5.720 89.123 511.495 NA 162 980C 2-H-1 104-106 4.62 20.275 NA NA NA NA NA NA NA NA 131.130 0.890 162 980C 2-H-1 105-106 4.64 20.324 NA 4.213 4.042 0.552 NA NA NA NA NA NA 162 980C 2-H-1 107-108 4.65 20.334 NA NA NA NA NA NA NA NA 332.871 NA 162 980C 2-H-1 108-109 4.67 20.382 NA 4.183 4.172 NA NA NA NA NA NA NA 162 980C 2-H-1 110-111 4.68 20.392 NA NA NA NA NA NA NA NA 803.520 NA 162 980C 2-H-1 111-112 4.70 20.441 NA 4.081 4.195 0.583 NA NA NA NA NA NA 162 980C 2-H-1 113-114 4.71 20.470 NA 4.040 4.130 0.577 NA NA NA NA 592.079 NA 162 980C 2-H-1 114-116 4.74 20.600 NA 4.159 4.051 0.574 NA NA NA NA NA NA 162 980C 2-H-1 117-118 4.75 20.626 NA NA NA NA NA NA NA NA 413.144 NA 162 980C 2-H-1 118-119 4.77 20.756 NA 4.108 4.109 0.583 NA NA NA NA NA NA 162 980C 2-H-1 120-121 4.78 20.782 NA NA NA NA NA NA NA NA 536.162 NA 162 980C 2-H-1 121-122 4.80 20.912 NA 4.139 3.853 0.574 NA NA NA NA NA NA 162 980C 2-H-1 123-124 4.81 20.938 NA NA NA NA NA -0.030 5.830 93.624 572.522 NA 162 980C 2-H-1 124-126 4.82 20.990 NA NA NA NA NA NA NA NA 453.070 0.820 162 980C 2-H-1 125-126 4.84 21.120 NA 4.035 4.224 0.604 NA NA NA NA NA NA 162 980C 2-H-1 127-128 4.85 21.146 NA NA NA NA NA NA NA NA 224.975 NA 162 980C 2-H-1 128-129 4.87 21.276 NA 4.069 4.194 0.627 NA NA NA NA NA NA 162 980C 2-H-1 130-131 4.88 21.302 NA NA NA NA NA NA NA NA 412.233 NA 162 980C 2-H-1 131-132 4.90 21.432 NA 4.036 4.273 0.507 NA NA NA NA NA NA 162 980C 2-H-1 133-134 4.91 21.458 NA 4.142 4.297 0.573 NA NA NA NA NA NA 162 980C 2-H-1 134-136 4.92 21.510 NA NA NA NA NA NA NA NA 428.284 NA 162 980C 2-H-1 135-136 4.94 21.640 NA 4.148 4.190 0.520 NA NA NA NA NA NA 162 980C 2-H-1 137-138 4.95 21.666 NA NA NA NA NA NA NA NA 644.190 NA 162 980C 2-H-1 138-139 4.97 21.796 NA 4.108 3.857 0.607 NA NA NA NA NA NA 162 980C 2-H-1 140-141 4.98 21.822 NA NA NA NA NA NA NA NA 197.229 NA 162 980C 2-H-1 141-142 5.00 21.952 NA 3.970 3.942 NA NA NA NA NA NA NA 162 980C 2-H-1 143-144 5.01 22.030 NA NA NA NA NA -0.220 4.680 93.974 205.630 0.740 162 980C 2-H-1 144-146 5.04 22.160 NA 3.996 3.702 0.750 NA NA NA NA NA NA 162 980C 2-H-1 147-148 5.12 22.550 NA NA NA NA NA 0.890 5.510 95.650 198.770 NA 162 980C 2-H-2 5-6 5.32 23.590 NA NA NA NA NA NA NA 44.980 9.450 0.630 162 980C 2-H-2 25-26 5.52 24.630 NA NA NA NA NA NA NA NA 344.050 NA 162 980C 2-H-2 45-46