# NOAA Paleoclimatology Program - Paleocean Site Data # 74kl-tab.txt # Complete Data # File Created: 18-Jan-2005 # #********************************************************************************* # Please cite the contributor and the original publications when using these data #********************************************************************************* # # Missing Values indicated by '-999' # # PI: Frank Sirocko # Core/Site: 74KL # Latitude: 14.19.16N ( 14.32111) # Longitude: 57.20.49E ( 57.34694) # Water Depth(m): 3212 # # Publications: # Sirocko, F., M. Sarnthein, H. Erlenkeuser, H. Lange, M. Arnold, and J.-C. Duplessy. # 1993. Century-Scale events in monsoonal climate over the past 24,000 years. Nature # 364:322-324. #------------------ # # Description & Notes: # Arabian Sea monsoon during the past 24,000 years. # The CaCO3 data from the "Coulomat" are slightly lower than the "Carmhograph" # data for core 74KL (Fig. 19), because the "Carmhograph" method is based on use # of hot phosphoric acid (conc.) to dissolve all carbonates, whereas the "Coulomat" # method uses a weak phosphoric acid at room temperature. Accordingly, dolomites # are dissolved using the "Carmhograph", whereas the "Coulomat" only dissolves # CaCO3. The "Carmhograph" data are used to calculate the element concentrations # for core 74KL on a carbonate-and-opal-free-basis, whereas "Coulomat" data are # used for the time-slice samples. Determination of biogenic opal contentThe biogenic # opal concentrations were determined after a single extraction of silica into # 2M Na2CO3 solution at 85oC for 5 hours at the Lamont-Doherty-Earth Observatory, # using the method of Mortlock & Froelich (1989).Determination of trace elements # by ICP-MS (Inductively Coupled Plasma-Mass Spectrometry)250 mg of the bulk sample # were weighed into "Savillex" teflon beakers. The sample was moistened with 1 # ml H2O, 2 ml HNO3 (conc.) were added to the sample, heated for 2 hours at 100oC # and taken to dryness to dissolve carbonate and attack organics. 4 ml HF (conc., # p.a. grade) and 1 ml HNO3 (conc., p.a. grade) were added and heated for 24 hours # in closed vials at 160oC. The solution was taken to dryness; 1 ml HNO3 and 10 # drops HClO4 (conc., p.a. grade) were added to the residue, heated for 24 hours # at 160oC and taken to complete dryness at 220oC. The residue was dissolved in # 2 ml HNO3 and this solution was increased to a volume of 50 ml with deionized # water.The analyses were run on a VG PlasmaQuad PQ 1 in the ICP-MS laboratory # at the "Geologisch-Paläontologische Institut, Universität Kiel", according to # the procedure as outlined by Garbe-Schönberg (1993).Garbe-Schönberg, C.-D. (1993). # Simultanous determination of thirty seven trace elements in twenty-eigth international # rock standards by ICP-MS. Geostandard Newsletters, 17(1), 81-97. Concentration # values of all trace elements in rock standards of the USGS (United States Geological # Survey) were determined routinely every day for the "BR" or "BHVO-1" standard. # Certified concentration values for trace elements, their long-term average concentration # reproduced with the ICP-MS at Kiel, respective data from the day when the samples # of core 74KL were measured, standard deviation (n=2; i.e., the 74KL sample batch # and the long-term avarage for the ICP-MS at Kiel) and relative error are listed # in Tab. 4. Accordingly, except for Tl, the relative error of the analytical precision # is less than 5%, below 1,2 % for the elements used for the reconstruction of # the monsoon history (Zn, Zr, Rb, see chapter C.4., D.3.). Minor discrepancies # between the concentration values for core 74KL and the respective values of core # 74KL in the four time-slice maps may occur, because downcore values represent # 1 cm thick samples, and time-slice values represent 4 cm thick samples, averaging # over a longer sediment section. Accordingly, the time-slice samples are more # likely to include proportions from microenvironments like scattered pyrite crystals, # micro Mn nodules, single fish bones etc..The total relative error, encountered # for the concentration values of an element, is the relative error of the analytical # precision (Tab. 4), plus a maximum error of 4% from the calculation of concentration # values on a carbonate-and-opal-free-basis (1% from the CaCO3 analyis, 1% for # neglecting organic carbon content, and 2% for the presence of pore water salt).Determination # of Cd by graphite furnace ETAAS (electrothermal atomic absorption spectrometry)Cd # was measured on a Perkin Elmer, Zeeman 5000, ETAAS at "Geologisch-Paläontologische # Institut, Universität Kiel" from the same solution as the ICP-MS samples. 20 # ml of a matrix modifier (mixture of equal parts of Pd-nitrate, Mg-nitrate, HNO3) # was added to 1000 ml of solution. Determination of Al, Fe and Mg by ICP (electrothermal # atomic absorption spectrometry)These three elements were measured on a Perkin # Elmer ICP/6000 ("Geologisch-Paläontologische Institut, Univ. Kiel") from the # same solution than the ICP-MS samples. Determination of carbon and nitrogen contentTotal # C and total N of the bulk sediment was measured on an Carlo Erba CN-analyser # on a 100 mg aliqout from the bulk sample. The data were measured at the "Zentrum # für Meeres- und Klimaforschung, Universität Hamburg".Determination of organic # carbon contentCorg was determined by subtraction of carbonate-C from total-C.Determination # of sulfur contentS was measured on a LECO CS 125 analyzer at "GEOMAR" Kiel. The # analysis was repeated three times on aliqouts of 50 mg of the bulk sample, and # average values have been calculated. Determination of d18O, d13C of Globigerinoides # ruber, Cibicides wuellerstorfi, and the total CaCO3 fractionIsotopic measurements # of the d18O, d13C composition of planktonic foraminifera (G.ruber), benthic foraminifera # (C.wuellerstorfi) and of the total carbonate fraction, were made with a Finnigan # MAT 251 mass spectrometer at the C-14 Laboratory of the "Institut für Kernphysik, # Universität Kiel". The MAT is coupled on-line to a Carbo-Kiel automated CO2 preparation # from carbonate samples. The system measures with an accuracy of ±0.07‰ for oxygen # and ±0.04‰ for carbon isotopes. Calibration was done to the NBS 20, 19 and 18 # standard. All values are reported on the Pee Dee belemnite (PDB) scale. # # Variables: # depth Depth (cm) # yrBP Sirocko et al,(1993) radiocarbon years B.P. (Libby half-life; B.P. = 1950) # Al% Aluminum percent # Ba ppm Barium ppm # carb%1 Calcium Carbonate percent, method 1 # carb%2 Calcium Carbonate percent, method 2 # carb%3 Calcium Carbonate percent, method 3 # Cd ppm Cadmium ppm # Ce ppm Cerium ppm # Co ppm Cobalt ppm # corg1% Organic Carbon percent # Cr ppm Chromium ppm # Cs ppm Cesium ppm # Cu ppm Copper ppm # d13Cg.rub delta C13 PDB (Globigerinoides ruber) # d18Og.rub delta O18 PDB (Globigerinoides ruber) # dolofrac Dolomite fraction, impulse counter # Dy ppm Dysprosium ppm # Er ppm Erbium ppm # Eu ppm Europium ppm # Fe% Iron percent # Ga ppm Gallium ppm # Gd ppm Gadolinium ppm # Hf ppm Hafnium ppm # Ho ppm Holium ppm # K% Potassium percent # La ppm Lanthanum ppm # Li ppm Lithium ppm # Lu ppm Lutetium ppm # Mg% Magnesium percent # Mn% Manganese percent # Mo ppm Molybdenum ppm # N% Nitrogen percent # Na% Sodium percent # Nb ppm Niobium ppm # Nd ppm Neodymium ppm # Ni ppm Nickel ppm # opal% Opal percent # Pb ppm Lead ppm # Pr ppm Praseodymium ppm # quartzi Quartz in silt impulse # Rb ppm Rubidium ppm # S% Sulphur percent # Sc ppm Scandium ppm # Sm ppm Samarium ppm # Sr ppm Strontium ppm # Ta ppm Tantalum ppm # Tb ppm Terbium ppm # Tl ppm Thallium ppm # Tm ppm Thulium ppm # U ppm Uranium ppm # Y ppm Yyttrium ppm # Yb ppm Ytterbium ppm # Zn ppm Zinc ppm # Zr ppm Zirconium ppm # # CORE: 74KL depth yrBP Siro Al% Ba ppm carb%1 carb%2 carb%3 Cd ppm Ce ppm Co ppm corg1% Cr ppm Cs ppm Cu ppm d13Cg.rub d18Og.rub dolofrac Dy ppm Er ppm Eu ppm Fe% Ga ppm Gd ppm Hf ppm Ho ppm K% La ppm Li ppm Lu ppm Mg% Mn% Mo ppm N% Na% Nb ppm Nd ppm Ni ppm opal% Pb ppm Pr ppm quartzi Rb ppm S% Sc ppm Sm ppm Sr ppm Ta ppm Tb ppm Tl ppm Tm ppm U ppm Y ppm Yb ppm Zn ppm Zr ppm 2.5 610 1.78 1389 60.6 55 55.5 0.97 15.7 12.1 1.26 39.8 1.55 46 1.32 -1.62 1.21 1.95 1.25 0.38 1.21 5.43 2.02 0.94 0.42 0.67 9.21 12.01 0.2 1.35 0.061 0.83 0.16 2.1 4.02 8.83 79.7 8.6 7.83 2.19 16.8 20.1 0.223 8.64 1.91 967 0.27 0.31 0.32 0.18 3.56 14.2 1.24 104.1 37.9 5 950 1.81 1391 58.8 56.4 55.4 1.1 15.9 11 1.26 39.5 1.5 46.7 1.43 -1.73 1 1.99 1.3 0.39 1.22 5.45 2.05 0.93 0.43 0.69 9.34 11.89 0.2 1.37 0.058 0.63 0.18 1.73 3.96 8.99 78.1 8.2 8.06 2.22 17.05 20.8 0.23 7.72 1.93 960 0.27 0.32 0.32 0.19 3.24 14.4 1.28 104.2 36.1 7.5 1170 1.67 1321 60.4 57.8 58 0.74 15.3 14.1 1.28 39.3 1.45 48 1.49 -1.66 1.35 1.93 1.26 0.4 1.18 5.44 2.18 0.83 0.42 0.69 9.15 10.29 0.2 1.32 0.043 0.68 0.18 1.89 3.81 8.77 78.3 8 7.9 2.2 16.85 21.4 0.225 8.23 1.91 931 0.25 0.32 0.31 0.18 5.12 14 1.25 99.1 34.7 10 1390 1.79 1450 62.3 58.3 58 0.7 16.3 9.6 1.21 38.3 1.57 48 1.56 -1.74 -999 2.04 1.3 0.39 1.21 5.59 2.05 0.89 0.43 0.68 9.68 12.31 0.2 1.28 0.038 0.47 0.19 1.27 3.97 9.13 73.3 7.7 7.94 2.28 -999 21.6 0.206 7.65 1.93 989 0.26 0.32 0.28 0.19 4.52 14.8 1.29 100.9 37.3 12.5 1620 1.73 1350 62.1 58.5 58.6 1 15.2 12.4 1.16 36.9 1.41 48.1 1.09 -1.79 0.95 1.94 1.26 0.4 1.18 5.2 2.17 0.81 0.42 0.68 9.1 10.28 0.2 1.39 0.041 0.62 0.18 1.79 3.56 8.75 77.9 7.4 7.52 2.17 16.9 20.2 0.243 7.06 1.86 915 0.24 0.31 0.3 0.18 4.98 13.7 1.27 101.2 34 15 1840 1.75 1451 60.7 58.5 58.6 0.84 15.3 16.5 1.26 40.7 1.57 52.9 1.06 -1.94 0.85 1.93 1.27 0.39 1.19 5.5 2.11 0.87 0.43 0.67 9.29 10.63 0.2 1.38 0.047 0.91 0.18 1.83 3.84 8.55 87.6 7.6 7.6 2.17 17.4 20.9 0.251 8.16 1.91 1011 0.24 0.32 0.39 0.19 5.72 14.8 1.28 122.3 36 17.5 2070 1.64 1330 60.8 57.1 58.4 0.84 14.5 14 1.17 36.8 1.36 41.6 1.29 -1.71 2.95 1.87 1.22 0.38 1.12 4.98 2.07 0.88 0.41 0.7 8.75 10.06 0.2 1.34 0.06 1.21 0.17 2.07 3.5 8.41 87 7.5 7.8 2.1 18.55 19.3 0.232 6.74 1.84 913 0.24 0.31 0.49 0.18 5.55 13.4 1.24 96.5 34.4 20 2290 1.64 1300 62.3 59.6 61.2 0.41 13.8 9.3 1.11 31.8 1.32 36 1.13 -1.65 0.8 1.76 1.16 0.39 1.09 4.69 1.85 0.75 0.38 0.66 8.39 10.95 0.17 1.33 0.048 0.86 0.16 1.87 3.21 7.93 66.3 7.5 6.38 1.98 16.95 18.4 0.229 6.23 1.71 920 0.22 0.28 0.29 0.17 4.32 12.6 1.14 77.8 31.8 22.5 2510 1.56 1288 64.5 60.8 61 0.71 14 13.5 0.95 34.1 1.31 44.6 1.34 -1.82 2.5 1.77 1.16 0.37 1.06 4.61 2.02 0.75 0.38 0.67 8.41 9.66 0.18 1.29 0.057 1.24 0.13 1.9 3.15 8.25 82.4 6.6 7.31 2.03 20.5 18.1 0.224 8.9 1.78 1004 0.22 0.29 0.48 0.17 5.56 12.7 1.15 99.5 29.3 25 2740 1.49 1230 64.1 59.8 62.1 0.73 13.2 13.8 0.96 35 1.25 43 1.34 -1.7 1.6 1.72 1.12 0.35 1.03 4.58 1.92 0.77 0.37 0.63 8.02 9.04 0.18 1.24 0.046 1.06 0.13 1.71 3.19 7.73 80.3 7.4 6.95 1.93 18.9 17.5 0.246 7.11 1.69 1001 0.21 0.28 0.37 0.16 6.89 12.5 1.12 95.6 30.3 27.5 2960 1.46 1310 66.2 63 62.5 0.78 13.2 12.9 0.83 35.6 1.33 43.7 1.48 -1.79 2.5 1.69 1.11 0.33 0.98 4.68 1.82 0.75 0.37 0.63 8.16 9.95 0.18 1.18 0.046 0.99 0.12 1.69 3.23 7.52 75.6 7 6.37 1.9 19.05 17.5 0.231 5.96 1.61 1088 0.21 0.27 0.37 0.16 5.34 13 1.11 100 31.2 30 3180 1.5 1262 66.8 60.3 64 0.62 13.5 15.4 0.81 36 1.36 44.5 1.51 -1.82 2.25 1.69 1.12 0.34 0.99 4.67 1.92 0.77 0.37 0.63 8.16 10.02 0.18 1.18 0.053 1.24 0.12 1.54 3.32 7.44 81.8 7.8 6.58 1.92 19.45 17.2 0.193 5.95 1.64 1100 0.21 0.27 0.43 0.17 5.52 13.2 1.12 89.9 31.6 32.5 3410 1.34 1083 62.3 58.9 58.6 0.67 11.5 16.7 0.88 30.5 1.1 38 1.42 -1.71 1.2 1.52 0.98 0.32 0.84 3.99 1.67 0.69 0.33 0.63 7 8.42 0.16 1.17 0.056 1.75 0.13 2.65 2.68 6.86 97.8 9.4 6.15 1.69 14.85 15.6 0.244 6.45 1.47 939 0.19 0.24 0.47 0.14 5.53 11 1 82.8 27.1 35 3630 1.35 1143 64.2 60.4 59.7 0.58 12 17.7 0.92 28.7 1.22 41.1 1.33 -2.11 1.2 1.51 0.98 0.32 0.9 4.11 1.71 0.63 0.33 0.59 7.31 8.69 0.16 1.14 0.053 1.19 0.15 1.91 2.87 6.7 87.7 9.1 5.81 1.72 14.75 15.1 0.225 7.35 1.5 1050 0.18 0.25 0.41 0.15 4.86 11.8 1 84.8 26.8 37.5 3970 1.38 1165 64.3 64.2 61.3 0.74 12.2 11 0.81 36.5 1.24 38.8 1.41 -1.72 1.1 1.56 1.01 0.29 0.91 4.32 1.61 0.67 0.34 0.65 7.3 10.24 0.16 1.2 0.057 1.59 0.12 2.26 2.94 7.1 87.2 7.2 6.37 1.74 19.45 16.7 0.253 9.46 1.53 1036 0.2 0.25 0.46 0.15 4.16 11.4 1.01 84.8 26.6 40 4300 1.38 1216 69.8 63.3 62.7 0.76 11.9 11.3 0.56 31.7 1.21 41 1.36 -1.77 1.95 1.54 1.03 0.29 0.91 4.17 1.63 0.72 0.33 0.61 7.21 9.5 0.16 1.07 0.055 1.25 0.1 1.58 2.89 6.91 83.4 7.4 6.08 1.71 18.1 15.9 0.195 5.37 1.49 1067 0.19 0.25 0.42 0.15 4.76 11.5 1.03 92.7 28.4 42.5 4640 1.37 1214 65.1 61.7 62.3 0.62 12 9.2 0.64 31.4 1.22 40.6 1.49 -1.82 2.95 1.57 1.05 0.29 0.94 4.2 1.63 0.73 0.34 0.66 7.22 9.77 0.16 1.19 0.049 1.52 0.11 2.38 2.92 6.92 71 7 6.04 1.72 17.85 15.9 0.239 7.03 1.49 1045 0.19 0.25 0.43 0.15 4.11 11.6 1.04 80.5 29 45 4980 1.29 1201 66.3 64.1 64.3 0.68 11 9.6 0.64 29.7 1.14 40.3 1.32 -1.67 2.8 1.44 0.97 0.27 0.91 4.02 1.49 0.65 0.31 0.58 6.76 9.39 0.15 1.08 0.042 1.1 0.1 1.8 2.72 6.49 67.4 6.6 5.4 1.58 20.15 15 0.234 5.96 1.4 1028 0.18 0.23 0.34 0.14 4.29 11 0.98 85.7 26.4 47.5 5310 1.25 1186 66.2 66.1 66.1 0.93 10.8 7.7 0.66 25.6 1.11 41.9 1.39 -1.77 3.35 1.43 0.94 0.26 0.83 3.77 1.46 0.57 0.31 0.6 6.6 9.78 0.14 1.18 0.048 1.69 0.1 2.65 2.48 6.24 62.9 6.9 6.1 1.56 19.45 14.4 0.286 7.59 1.34 1022 0.17 0.23 0.48 0.13 4.49 10.5 0.93 84.5 24.9 50 5650 1.22 1265 69.6 68.4 68.3 0.91 11 8.7 0.78 28 1.14 43.4 1.36 -1.67 2.8 1.45 0.96 0.27 0.87 3.99 1.48 0.62 0.31 0.58 6.67 9.47 0.15 1.04 0.046 1.04 0.1 1.47 2.64 6.43 67.1 6.4 5.95 1.57 19 14.5 0.187 5.73 1.39 1146 0.17 0.23 0.39 0.14 5.01 10.3 0.95 89.7 25.3 52.5 5980 1.25 1239 68.4 66.4 65.6 1 11.5 9 0.84 30.3 1.14 42.3 1.41 -1.8 2.95 1.47 0.99 0.28 0.85 4.1 1.55 0.65 0.32 0.61 6.96 9.49 0.15 1.11 0.052 1.19 0.12 1.77 2.77 6.37 64.4 6.2 6.03 1.63 17.55 14.6 0.209 4.7 1.39 1111 0.18 0.23 0.43 0.15 4.62 11.7 0.99 94.6 28.1 55 6320 1.21 1247 70.4 67.6 67.6 1.1 11 9.3 0.72 29.3 1.13 41.1 1.31 -1.84 3.55 1.44 0.95 0.26 0.89 3.92 1.46 0.64 0.31 0.59 6.65 10.22 0.15 1.12 0.049 1.01 0.09 1.55 2.56 6.37 64.6 6.2 6.62 1.57 19 14.2 0.174 4.73 1.35 1130 0.18 0.23 0.38 0.14 5.26 8.9 0.92 91.4 25.6 57.5 6710 1.28 1213 67.5 68.6 68.4 0.76 10.9 13 -999 31.4 1.16 45.8 1.19 -1.8 4.45 1.4 0.95 0.27 0.86 4.13 1.56 0.62 0.31 0.56 6.69 9.73 0.15 1.03 0.058 1.06 0.1 1.25 2.69 6.07 78.7 6.5 5.91 1.54 17.8 14.9 0.195 4.9 1.35 1110 0.18 0.22 0.39 0.14 4.92 10.3 0.92 96 26.7 60 7090 1.23 1264 69.8 66.7 66.3 1.01 11.5 12.7 0.7 29.6 1.15 45.6 1.29 -1.69 2.25 1.53 1.01 0.28 0.9 3.98 1.54 0.67 0.33 0.57 6.86 11.15 0.16 1.14 0.06 1.55 0.1 1.5 2.57 6.59 82 7.7 6.65 1.64 17.7 14.6 0.221 5.83 1.4 1112 0.17 0.24 0.53 0.14 4.77 10.9 1.01 94.3 26.2 62.5 7480 1.3 1243 70.4 65.2 66.5 1 11.5 15.1 0.64 30.5 1.17 47.5 1.35 -1.79 5 1.51 0.99 0.3 0.85 4.18 1.71 0.67 0.33 0.59 6.91 9.52 0.15 1.14 0.066 1.28 0.1 1.5 2.73 6.63 90.3 6.7 6.76 1.65 16.95 15.4 0.209 6.57 1.46 1129 0.19 0.24 0.45 0.14 5.16 9.7 0.98 95.2 26.3 65 7860 1.29 1094 67.9 65.9 65.6 0.78 11 14.9 0.8 32.7 1.08 46.3 1.32 -1.91 5.1 1.48 0.97 0.29 0.93 4.06 1.6 0.67 0.32 0.59 6.46 8.96 0.15 1.18 0.056 1.37 0.1 1.54 2.66 6.39 82.1 7.2 6.32 1.58 17.5 15.2 0.184 4.99 1.39 1033 0.18 0.23 0.45 0.14 4.84 11.1 0.97 93 27.3 67.5 8250 1.33 1115 66.8 63.2 64.4 0.86 11.4 11.6 0.83 32.8 1.14 43.1 1.14 -1.62 1.7 1.49 1.01 0.3 0.94 3.94 1.64 0.71 0.32 0.63 6.79 9.88 0.16 1.21 0.069 1.78 0.11 2.1 2.6 6.55 81.5 6.7 6.46 1.62 22.15 15.4 0.256 5.84 1.4 1009 0.19 0.24 0.54 0.15 5.13 10.6 1 81.1 28.3 70 8630 1.27 1158 68.7 67.3 66.2 0.56 11.4 10.7 0.81 32.6 1.17 42.2 0.99 -1.58 -0.15 1.41 0.94 0.26 0.9 4.05 1.45 0.66 0.31 0.59 6.51 10.48 0.15 1.16 0.059 1.37 0.11 1.37 2.68 6.33 67.8 7.1 6.21 1.58 22.4 15.1 0.32 4.88 1.4 1101 0.18 0.22 0.39 0.14 4.78 9.5 0.9 70.2 26.3 72.5 8860 1.23 1098 66.5 65.4 64.1 0.75 11.1 9.5 0.91 30.5 1.12 42.7 -999 -999 0.01 1.38 0.93 0.25 0.81 3.9 1.37 0.6 0.3 0.61 6.31 9.89 0.14 1.12 0.057 1.84 0.11 2.02 2.61 6.04 68.6 7 6.42 1.51 21 15.3 0.171 6.67 1.33 1034 0.17 0.21 0.48 0.13 4.22 10.3 0.91 74.7 25 75 9090 1.28 1028 68.5 64.5 64.9 0.66 10.6 11 0.86 25.1 1.07 37 1.19 -1.6 -0.2 1.31 0.89 0.31 0.83 3.67 1.4 0.53 0.29 0.57 6.16 9.35 0.13 1.11 0.057 1.62 0.12 1.52 2.47 5.86 73.5 8.3 5.94 1.44 18.75 15.1 0.251 3.91 1.28 951 0.16 0.21 0.47 0.12 4.18 9.6 0.88 69.1 24.1 77.5 9320 1.32 1125 66.8 61 59.9 0.7 11.6 15.4 0.93 33.2 1.15 45.2 1.18 -1.69 0.15 1.41 0.96 0.27 0.84 3.96 1.47 0.67 0.31 0.62 6.61 9.98 0.15 1.15 0.058 1.77 0.12 1.81 2.63 6.58 94.4 8 6.8 1.6 19.2 15.6 0.201 5.41 1.45 1089 0.17 0.22 0.47 0.14 4.67 10.2 0.95 79.3 26.2 80 9550 1.27 1082 69.8 66.7 66.1 0.91 11.5 12.2 0.75 33.8 1.18 43.4 1.09 -1.79 -0.1 1.4 0.92 0.27 0.85 3.94 1.4 0.65 0.3 0.59 6.56 10.15 0.14 1.13 0.056 1.57 0.11 1.35 2.7 6.29 78.5 8.2 6.68 1.57 21.75 15.7 0.222 4.82 1.37 1098 0.18 0.22 0.42 0.13 5.23 9.6 0.89 85.8 26.4 82.5 9880 1.2 1087 68.9 65.1 65.6 0.81 11.6 15.3 0.83 32.8 1.2 43.3 1.1 -1.41 0.02 1.41 0.94 0.27 0.84 3.97 1.45 0.7 0.31 0.61 6.58 10.32 0.14 1.23 0.06 1.81 0.12 1.56 2.75 6.39 92.2 7.6 6.48 1.59 21 15.6 0.222 5.02 1.4 1118 0.18 0.22 0.43 0.14 4.44 9.8 0.9 82.7 26.6 85 10220 1.35 939 69.6 65.5 64.7 0.53 11.6 9.4 0.67 31.4 1.23 37.1 1.05 -1.38 -0.05 1.41 0.9 0.28 0.93 3.95 1.45 0.67 0.3 0.63 6.63 10.55 0.14 1.18 0.055 1.42 0.09 1.44 2.84 6.42 62.6 6.4 6.16 1.6 23.3 16.8 0.259 6.01 1.42 1028 0.19 0.22 0.35 0.13 4.82 10.1 0.89 73.3 25.7 87.5 10550 1.34 853 67.8 65.1 66.1 0.48 11.2 10.6 -999 31.1 1.2 37.9 1.01 -1.45 0.85 1.31 0.85 0.27 0.95 3.81 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0.5 52.7 1.83 27.5 0.54 -0.79 1.05 1.59 0.98 0.37 1.34 4.76 1.8 0.93 0.33 0.84 8.13 14.47 0.14 1.68 0.055 0.91 0.08 1.26 4.42 7.53 63.5 3.2 5.99 1.96 34 23.3 0.231 6.31 1.67 1002 0.28 0.26 0.35 0.14 3.15 11.6 0.92 58.9 34.6 127.5 16060 2.22 333 62.2 57.1 56.7 0.42 16 10.7 0.34 56.8 2.01 24.3 0.7 -0.34 0.8 1.66 1.03 0.4 1.65 5.05 1.78 0.94 0.35 0.97 8.41 17.03 0.14 1.97 0.049 0.9 0.06 1.54 4.6 8.36 63.9 3.1 6.31 2.1 33.4 27.3 0.185 6.79 1.79 839 0.31 0.27 0.3 0.15 3.05 11.2 0.96 57.9 34.3 130 16330 2.42 279 60.4 58 58.4 0.3 17.7 11.5 0.27 61.5 2.22 24 0.67 -0.15 -999 1.8 1.08 0.44 1.58 5.43 1.9 1.09 0.37 1.03 9.28 20.12 0.15 2.1 0.051 0.72 0.05 1.3 4.97 9.02 68 3.2 6.32 2.29 -999 30 0.181 7.32 1.92 778 0.34 0.29 0.27 0.15 3.04 11.7 1.02 52.7 37.9 132.5 16610 2.62 271 58.8 51 51.9 0.54 18.8 11 0.23 65.9 2.37 27.1 0.56 -0.39 9.5 1.89 1.15 0.47 1.7 5.82 2.07 1.18 0.38 1.12 9.75 20.05 0.16 2.24 0.048 0.9 0.07 1.49 5.53 9.64 69.6 3.2 7.1 2.4 30.5 32.1 0.27 8.11 2.05 755 0.38 0.31 0.32 0.16 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