Agulhas Retroflection 30KYr Stratigraphic Data ----------------------------------------------------------------------- World Data Center for Paleoclimatology, Boulder and NOAA Paleoclimatology Program ----------------------------------------------------------------------- NOTE: PLEASE CITE ORIGINAL REFERENCE WHEN USING THIS DATA!!!!! NAME OF DATA SET: Agulhas Retroflection 30KYr Stratigraphic Data LAST UPDATE: 5/2009 (Original receipt by WDC Paleo) CONTRIBUTOR: Allison M. Franzese, Rutgers, the State University of New Jersey. IGBP PAGES/WDCA CONTRIBUTION SERIES NUMBER: 2009-047 WDC PALEO CONTRIBUTION SERIES CITATION: Franzese, A.M., et al. 2009. Agulhas Retroflection 30KYr Stratigraphic Data. IGBP PAGES/World Data Center for Paleoclimatology Data Contribution Series # 2009-047. NOAA/NCDC Paleoclimatology Program, Boulder CO, USA. ORIGINAL REFERENCE: Franzese, A.M., S.R. Hemming, and S.L. Goldstein. 2009. Strontium isotopes in detrital sediments constrain the glacial position of the Agulhas Retroflection. Paleoceanography, 2008PA001706, in press. doi:10.1029/2008PA001706 ABSTRACT: The Agulhas Leakage represents a significant portion of the warm, surface return flow of the global overturning circulation, and thus may be an important feedback in the ocean-climate system. Models indicate that reduced Leakage could be caused by a stronger Agulhas Current and/or a more upstream (eastward) Agulhas Retroflection, while a weaker Agulhas Current would result in a more westward Retroflection and increased Leakage. However, data for the last glacial maximum support both a weaker Agulhas Current and less Leakage, implying a possible displacement of the Retroflection. We present new 87Sr/86Sr results for modern sediments within this region, confirming that the modern pathway of the Agulhas Current, Retroflection and Leakage can be traced by terrigenous sediment provenance using Sr isotopes. New 87Sr/86Sr data from sediments deposited during the last glacial maximum suggest that the glacial Agulhas Current and Retroflection followed nearly their modern trajectory. The provenance data appear to rule out both a stronger Agulhas Current and a more upstream Agulhas Retroflection. We conclude that the reduced glacial Leakage was caused by the weakened Agulhas Current, with no significant change in the Retroflection position. This is inconsistent with the model predictions and thus emphasizes the need for further work in this region. ADDITIONAL REFERENCES: Franzese, A.M. 2008. Paleoceanography of the Agulhas Current and Retroflection. Ph.D. Thesis, Columbia University, New York, USA. Danzeglocke, U., O. Jöris, and B. Weninger. 2007 CalPal-2007online, edited. Hughen, K., J. Southon, S. Lehman, C. Bertrand, and J. Turnbull. 2006. Marine-derived 14C calibration and activity record for the past 50,000 years updated from the Cariaco Basin. Quaternary Science Reviews, 25, 3216. Hughen, K.A., M.G.L. Baillie, E. Bard, J.W. Beck, C.J.H. Bertrand, P.G. Blackwell, C.E. Buck, G.S. Burr, K.B. Cutler, P.E. Damon, R.L. Edwards, R.G. Fairbanks, M. Friedrich, T.P. Guilderson, B. Kromer, G. McCormac, S. Manning, C.B. Ramsey, P.J. Reimer, R.W. Reimer, S. Remmele, J.R. Southon, M. Stuiver, S. Talamo, F.W. Taylor, J. van der Plicht, and C.E. Weyhenmeyer. 2004. Marine04 Marine Radiocarbon Age Calibration, 0-26 Cal Kyr BP. Radiocarbon, 46, 1059-1086. Mortlock, R.A., and P.N. Froelich. 1989. A simple method for the rapid determination of biogenic opal in pelagic marine sediments. Deep-Sea Res., 36, 1415-1426. Southon, J., M. Kashgarian, M. Fontugne, B. Metivier, and W.W.S. Yim. 2002. Marine reservoir corrections for the Indian Ocean and southeast Asia. Radiocarbon, 44, 167-180. Stuiver, M., and P.J. Reimer. 1993. Extended 14C database and revised CALIB radiocarbon calibration program (version 5.0). Radiocarbon, 35, 215-230. GEOGRAPHIC REGION: Agulhas Retroflection (Southeast Atlantic/Western Indian Ocean) PERIOD OF RECORD: Last Glacial Maximum/Holocene, ~25KYrBP - present FUNDING SOURCES: US National Science Foundation grants OCE 98-09253 and OCE 00-96427 to S.L.G. and S.R.H. NSF Graduate Research Fellowship to A.M.F. And a grants/cooperative agreement from the National Oceanic and Atmospheric Administration. DESCRIPTION: Stratigraphic and related data for cores beneath the Agulhas Retroflection. Auxiliary Material for Franzese, et al. 2009. The cores are from Agulhas Retroflection (Southeast Atlantic/Western Indian Ocean) and the samples span the last ~30kyr This dataset includes 26 data tables relevant to the stratigraphy of cores in the Agulhas Current and Retroflection region. The data were collected over the period from 2001-2008 at the Lamont-Doherty Earth Observatory of Columbia University. The data include radiocarbon ages, percent carbonate, magnetic susceptibility, lithic grains per gram and percent opal. Ship Codes: RC=Robert Conrad, VM=Vema Core Locations: Core ID Lat° Long° Water Depth (m) RC11-84 -39.27 12.58 4898 RC11-86 -35.78 18.45 2829 RC11-87 -38.95 19.15 4996 RC12-304 -33.22 29.18 3290 RC14-3 -35.48 28.95 4471 RC14-4 -32.62 31.13 3660 RC17-55 -40.42 24.17 4159 VM14-65 -41.06 7.78 4825 VM16-53 -36.83 21.3 1500 VM16-56 -41.35 26.63 2961 VM18-184 -36.92 23.4 5053 VM19-224 -35.5 29.95 4572 VM19-225 -35.92 27.75 4658 VM20-201 -36.32 25.28 3847 VM24-216 -37.32 21.57 3632 VM29-84 -43.85 27.6 5451 VM29-89 -45.73 25.65 5945 VM29-90 -43.7 25.73 5148 VM29-94 -35.92 25.25 4751 VM34-153 -39.37 24.5 3517 VM34-155 -42.17 26.73 4000 VM34-156 -42.07 26.63 3819 VM34-157 -41.95 26.42 3636 VM34-158 -41.25 25.78 2994 VM34-159 -41.08 25.48 2892 DATA: 1. Age Data 1a. NOSAMS 14C ages Results of radiocarbon analyses for samples from cores performed at the National Ocean Sciences Accelerator Mass Spectrometry Facility (NOSAMS) at Woods Hole Oceanographic Institute (WHOI) and their corresponding calendar ages. Most of the 14C ages were converted to calendar ages using the radiocarbon calibration program CALIB05 [Stuiver and Reimer, 1993] using the calibration dataset Marine04 [Hughen, et al., 2004] with a regional reservoir correction ?R = 219 ± 6 years [Southon, et al., 2002]. Those with ages outside of the calibration range of this dataset (0-26 ka) were converted to calendar ages using the new 0-50 ka dataset from the Cariaco Basin [Hughen, et al., 2006] with the online calibration program CalPal-2007 [Danzeglocke, et al., 2007], using the same reservoir correction of ?R = 219 ± 6 years [Southon, et al., 2002]. Size = minimum shell size, sieve size in microns. err. = 2 sigma error as reported by NOSAMS Ship/Cruise/Core Lat. Long. WaterDepth Top Bot. Material Size 14Cage err. CalAge RC 11 86 -35.78 18.45 2829 35 36 G. Inflata 150 10900 60 12040 RC 11 86 -35.78 18.45 2829 45 45 G. Bulloides 150 18650 150 21390 RC 11 86 -35.78 18.45 2829 55 56 G. Inflata 150 21100 110 24530 RC 11 86 -35.78 18.45 2829 75 76 G. Inflata 150 25500 150 30480 RC 12 304 -33.22 29.18 3290 80 80 G. Inflata 150 13000 70 14420 RC 14 3 -35.48 28.95 4471 3.5 4.5 Mixed planktonic 150 11150 55 12480 RC 14 3 -35.48 28.95 4471 18 19 Mixed planktonic 150 24500 110 28970 RC 14 4 -35.48 28.95 4471 53 55 G. Inflata 150 11950 55 13200 RC 17 55 -40.42 24.17 4159 0 2 Mixed planktonic 250 27900 140 32950 VM 16 53 -36.83 21.3 1500 99 100 Mixed planktonic 150 23500 400 27870 VM 19 224 -35.5 29.95 4572 51 53 Mixed planktonic 150 19350 90 22290 VM 19 225 -35.92 27.75 4658 0 2 Mixed planktonic 150 10500 120 11360 VM 20 201 -36.32 25.28 3847 40 43 Mixed planktonic 150 13400 55 15080 VM 20 201 -36.32 25.28 3847 46 47 Mixed planktonic 150 25600 110 30490 VM 20 201 -36.32 25.28 3847 60 61 Mixed planktonic 250 30400 180 35520 VM 34 153 -39.37 24.5 3517 4 5 Mixed planktonic 150 12950 170 14370 VM 34 153 -39.37 24.5 3517 30 31 Mixed planktonic 150 39000 490 43600 VM 34 155 -42.17 26.73 4000 60 61 G. Bulloides 150 17900 70 20400 VM 34 156 -42.07 26.63 3819 100 101 G. Bulloides 150 21400 120 24990 VM 34 157 -41.95 26.42 3636 15 16 G. Inflata 150 4110 40 3870 VM 34 157 -41.95 26.42 3636 65 66 G. Inflata 150 16350 80 18960 VM 34 157 -41.95 26.42 3636 70 71 G. Bulloides 150 19600 170 22520 VM 34 157 -41.95 26.42 3636 95 96 G. Inflata 150 28100 170 33150 VM 34 157 -41.95 26.42 3636 125 125 G. Inflata 150 33000 240 38100 VM 34 158 -41.25 25.78 2994 2 4 Mixed planktonic 300 4710 35 4670 VM 34 158 -41.25 25.78 2994 49 50 Mixed planktonic 300 17100 80 19660 1b. Stratigraphic reversals ages Radiocarbon analyses performed at the National Ocean Sciences Accelerator Mass Spectrometry Facility (NOSAMS) at Woods Hole Oceanographic Institute (WHOI) for cores with apparent stratigraphic reversals (VM16-56, VM29-94 and VM34-159). Ship RC=Robert Conrad, VM=Vema Top, Bottom sample depth in cm. Ship/Cruise/Core Lat. Long. WaterDepth Top Bot. Material Size 14Cage Error 2 sigma VM 16 56 -41.35 26.63 2961 6 8 Mixed planktonic 63 8350 55 VM 16 56 -41.35 26.63 2961 6 8 Bulk sediment 63 14600 70 VM 16 56 -41.35 26.63 2961 12 14 Mixed planktonic 250 45600 720 VM 16 56 -41.35 26.63 2961 69 70 Mixed planktonic 250 21100 85 VM 16 56 -41.35 26.63 2961 70 72 Mixed planktonic 150 18450 85 VM 16 56 -41.35 26.63 2961 70 72 G. Inflata 150 5960 35 VM 29 94 -35.92 25.25 4751 160 160 Mixed planktonic 250 43200 310 VM 29 94 -35.92 25.25 4751 354 357 Mixed planktonic 150 39800 250 VM 34 159 -41.08 25.48 2892 0 3 Mixed planktonic 150 22600 130 VM 34 159 -41.08 25.48 2892 9 11 Mixed planktonic 150 45000 1200 VM 34 159 -41.08 25.48 2892 18 20 Mixed planktonic 150 36600 310 VM 34 159 -41.08 25.48 2892 30 30 Mixed planktonic 150 32900 190 VM 34 159 -41.08 25.48 2892 30 30 Bulk sediment 63 43600 490 1c. Inter-species 14C Results of radiocarbon analyses performed at the National Ocean Sciences Accelerator Mass Spectrometry Facility (NOSAMS) at Woods Hole Oceanographic Institute (WHOI) for stratigraphically concurrent samples of different species. Columns 10-19 give the radiocarbon age and 2 sigma error of samples of various species. Top and Bottom sample depths in cm Minimum shell size(microns), Sieve size in microns. Radiocarbon age measured on samples of G. inflata, G. bulloides, G. sacculifer, mixed planktonic species, and bulk sediment, plus 2 sigma errors, as reported by NOSAMS Ship/Cruise/Core Lat. Long. WaterDepth Top Bot. Size G.inf err. G.bul err. G.sac err. Plank. err. Bulk err. VM 16 56 -41.35 26.63 2961 6 8 63 null null null null null null 8350 55 14600 70 VM 16 56 -41.35 26.63 2961 70 72 150 5960 35 null null null null 18450 85 null null VM 20 201 -36.32 25.28 3847 40 43 150 11850 45 null null null null 13400 55 null null VM 34 155 -42.17 26.73 4000 60 61 150 null null 17900 70 19150 75 null null null null VM 34 158 -41.25 25.78 2994 2 4 300 4140 35 6500 45 null null 4710 35 null null VM 34 158 -41.25 25.78 2994 49 50 300 14200 60 18400 75 null null 17100 80 null null VM 34 159 -41.08 25.48 2892 30 30 150 null null null null null null 32900 190 43600 490 1d. Old Core Top Ages Measured or extrapolated ages of core tops older than 5000 years Ship/Cruise/Core Lat. Long. WaterDepth CoreTopAgeYrs RC 14 3 -35.48 28.95 4471 7950 RC 17 55 -40.42 24.17 4159 32950 VM 19 225 -35.92 27.75 4658 11360 VM 34 153 -39.37 24.5 3517 9380 1e. VM14-65 Age Model Tie points determined by correlating %CaCO3 record with that of RC11-83. Depth Age ka 40 3.5 110 13.25 120 14.07 130 14.87 140 15.62 150 16.35 160 17.06 170 17.74 260 24.09 270 24.67 280 25.19 290 25.82 330 28.13 480 35.82 650 45.69 2. Core Top and Last Glacial Maximum Ages and Sedimentation Rates Measured or extrapolated ages of the core top, the depth of the 20 ka (LGM) horizon, and the average sedimentation rate Core top age in kiloyears. Depth of the 20 ka interval in centimeters. Sedimentation rate in cm/ka. Column 10 lists the tools used for the stratigraphic determinations. Ship/Cruise/Core/Type Lat. Long. WaterDepth CoreTopka 20kaInt SedRate Tool(s), Reference(s) RC 11 87 P -38.95 19.15 4996 26 null 29 Magnetic susceptibility, %CaCO3, lithic grains RC 12 304 P -33.22 29.18 3290 0 111 5.6 Radiocarbon RC 14 3 P -35.48 28.95 4471 8 10.5 0.9 d18O [Ninnemann], Radiocarbon RC 14 4 P -32.62 31.13 3660 0 82 4.1 Core description, Radiocarbon RC 17 55 TW -40.42 24.17 4159 32.2 null null %CaCO3, Radiocarbon VM 14 65 P -41.07 7.78 4825 0 200 null Correlation of %CaCO3 [Burckle] to RC11-83 VM 16 53 P -36.83 21.3 1500 0 71 3.6 Magnetic susceptibility, Radiocarbon VM 18 184 P -36.92 23.4 5053 0.2 84 4.2 Magnetic susceptibility VM 19 224 P -35.5 29.95 4572 0 46 2.3 Magnetic susceptibility, Radiocarbon VM 19 225 TW -35.92 27.75 4658 11.4 null null %CaCO3, Radiocarbon VM 20 201 P -36.32 25.28 3847 0 44 2.2 Magnetic susceptibility, Radiocarbon VM 24 216 P -37.32 21.57 3632 0 53 2.7 Magnetic susceptibility VM 29 84 P -43.85 27.6 5451 0 120 6 C. davisiana counts [Hays et al 1976] VM 29 89 P -45.73 25.65 5945 0 120 6 C. davisiana counts [Hays et al 1976] VM 29 90 P -43.7 25.73 5148 0 60 3 C. davisiana counts [Hays et al 1976] VM 34 153 P -39.37 24.5 3517 9.4 9 0.9 %CaCO3, Radiocarbon VM 34 155 P -42.17 26.73 4000 0 60 3 Radiocarbon VM 34 156 P -42.07 26.63 3819 0 100 4 Radiocarbon VM 34 158 P -41.25 25.78 2994 3.7 50 3.2 Radiocarbon 3. Table 1: New Strontium Isotope Data for the Holocene and LGM *a Errors are reported as 2sigma*10-5 *b The abbreviations for stratigraphic tools are as follows: 14C = Radiocarbon analyses performed by NOSAMS; 14C(ext) = extrapolation between 14C tie points; MS = magnetic susceptibility (this study); CaCO3 = %CaCO3 (* indicates the record was provided by Lloyd Burckle); MP = Micropaleontology (shipboard analysis of foraminiferal assemblages [Hall and Zahn, 2004]); Color = Color changes correlated to those in CD154-06-6PK; Lithics = Counts of lithic grains >63 um (this study); d18O = d18O measured on benthic forams (provided by Ulysses Ninnemann); C. davisiana = Stratigraphy based on radiolarian abundances [Hays, et al., 1976] Time-slice, Region and Core name Lat. Lon. WaterDepth CoreDepth 87Sr/86Sr +/- *a Stratigraphic Tools *b Holocene Agulhas Current CD154-02-1P -29.07 32.75 1613 Core Top 0.73031 1.3 CD154-02-3K -29.06 32.77 1626 Core Top 0.73597 1.2 MP CD154-03-3PK -29.13 32.89 1745 Core Top 0.73448 0.9 CD154-03-5K -29.12 32.89 1747 Core Top 0.73569 1.3 CD154-04-4PK -29.61 33.45 2533 Core Top 0.7268 0.9 MP CD154-04-6K -29.59 33.42 2469 Core Top 0.72868 1.2 CD154-05-5PK -29.92 32.79 1784 Core Top 0.72275 1.4 CD154-05-7K -29.93 32.81 1850 Core Top 0.72703 1 CD154-06-4P -30.51 32.51 2998 Core Top 0.72609 1 CD154-06-6PK -30.6 32.48 3015 Core Top 0.7219 0.9 MP CD154-07-7PK -30.13 31.7 1017 Core Top 0.72084 1.2 MP CD154-09-9K -30.85 31.75 2986 Core Top 0.72664 0.9 Color CD154-11-7PT -31.15 31.87 3072 Core Top 0.72722 1 CD154-13-10PK -34.05 27.96 3596 Core Top 0.72137 1.2 MP CD154-15-12PK -33.69 28.25 3152 38 0.72105 1.6 Color CD154-15-14K -33.73 28.2 3236 Core Top 0.72323 1.4 MP, Color CD154-15-9P -33.71 28.19 3182 Core Top 0.72106 1.3 MP CD154-16-10P -33.69 28.25 3173 Core Top 0.72112 1.4 CD154-16-13PK -33.73 28.22 3215 Core Top 0.72109 1.7 CD154-16-15K -33.7 28.24 3166 Core Top 0.7233 1.2 MP, Color CD154-17-11P -33.27 29.12 3333 Core Top 0.72197 1.4 CD154-17-11P -33.27 29.12 3333 Near Top 0.72032 1.2 CD154-17-17K -33.27 29.12 3333 Core Top 0.72296 1.3 CD154-18-13P -33.31 28.85 3090 Core Top 0.72333 1.3 CD154-18-13P -33.31 28.85 3090 Core Top 0.72234 1.4 CD154-18-18K -33.31 28.85 3037 Core Top 0.72325 1 CD154-19-14P -34.41 27.22 3572 Core Top 0.72325 1.2 CD154-19-19K -34.4 27.21 3544 Core Top 0.72449 1.4 CD154-20-15P -34.46 27.14 3583 Core Top 0.72029 1.6 CD154-20-20K -34.45 27.15 3512 Core Top 0.72493 1.4 CD154-20-21K -34.45 27.14 3561 Core Top 0.72256 1.3 RC14-4 -32.62 31.13 3660 9.5-10.5 0.72516 1.3 14C(ext) Retroflection CD154-23-16P -36.81 22 3189 Core Top 0.72592 1 MP CD154-23-24K -36.8 22.01 3173 Core Top 0.72934 0.9 MP CD154-24-17-P -36.96 21.55 3429 Core Top 0.72488 1 CD154-24-25K -36.96 21.55 3429 Core Top 0.7245 1 MP CD154-25-19P -37.41 20.05 3691 Core Top 0.72105 1.4 MP CD154-25-20P -37.41 20.05 3692 Core Top 0.72437 1.6 MP CD154-25-20P -37.41 20.05 3692 Near Top 0.72319 1 MP VM20-201 -36.32 25.28 3847 10-Aug 0.72292 0.9 MS, 14C(ext) Agulhas Plateau VM34-155 -42.17 26.73 4000 6-May 0.72453 1.7 CaCO3*, 14C(ext) VM34-156 -42.07 26.63 3819 3-Jan 0.72507 2.6 CaCO3*, 14C(ext) VM34-158 -41.25 25.78 2994 4-Feb 0.72492 1 CaCO3*, 14C LGM (19-26ka) Agulhas Current CD154-02-3K -29.06 32.77 1626 145 0.73075 1.2 MP CD154-06-6PK -30.61 32.48 3015 44 0.72476 1 MP CD154-09-9PK -30.82 31.73 2987 55 0.72258 1.2 MP, Color CD154-13-12K -34.09 27.89 3612 41 0.72054 1.3 Color CD154-15-12PK -33.69 28.25 3152 41 0.71893 1.6 Color CD154-15-13K -33.71 28.24 3145 40 0.71632 1.6 Color CD154-15-14K -33.73 28.2 3236 53 0.71592 1 MP, Color CD154-16-15K -33.7 28.24 3166 30 0.7182 1 MP, Color Transkei Basin RC14-3 -35.48 28.95 4471 11-Oct 0.71668 1.3 d18O, 14C(ext) VM19-224 -35.5 29.95 4572 51-53 0.71696 1 MS, 14C Retroflection RC11-87 -38.95 19.15 4996 <10 0.71614 1 MS, CaCO3, Lithics VM16-53 -36.83 21.3 1500 71-72 0.71853 0.9 MS, 14C(ext) VM20-201 -36.32 25.28 3847 43-44 0.71923 2.2 MS, 14C(ext) Agulhas Plateau VM34-153 -39.37 24.5 3517 12-Nov 0.7183 1.1 CaCO3, 14C(ext) VM34-155 -42.17 26.73 4000 60-61 0.71888 2.6 CaCO3*, 14C VM34-156 -42.07 26.63 3819 100-101 0.7189 0.9 CaCO3*, 14C VM34-158 -41.25 25.78 2994 49-50 0.7188 1.6 CaCO3*, 14C Southern VM29-89 -45.73 25.65 5945 117-120 0.71238 1.4 C. davisiana VM29-90 -43.7 25.73 5148 57-59 0.71389 1.1 C. davisiana 4. Lithic Grains Counts of lithic grains >63 microns per gram of sediment for cores RC11-84 and RC11-87. Column 1: Sample depth in centimeters Column 2: Lithic grains >63 microns per gram of bulk sediment RC11-84 Depth Lithic grains per gram 10 198 25 155 50 236 75 388 120 194 180 221 RC11-87 Depth Lithic grains per gram 10 922 70 876 180 350 290 501 410 332 5. Calcium Carbonate and Opal Data Percent carbonate measured by coulometry at the Lamont-Doherty Earth Observatory (LDEO) of Columbia University. Sample depths in centimeters Percent carbonate measured by coulometry Percent opal measured by the method of [Mortlock and Froelich, 1989] V34-153 DepthTop DepthBot. %CaCO3 %OPAL 11 12 51.62 4.02 20 21 51.29 3.76 30 31 50.39 3.57 40 41 50.73 2.96 49 50 56.4 4.45 59 60 55.41 4 70 71 53.39 3.88 80 81 57.18 4.25 90 91 51.53 3.96 V22-175tw Depth %CaCO3 0 86.66 5 84.94 10 80.32 15 83.26 20 87.19 25 81.36 V22-175 Depth %CaCO3 10 93.11 20 89.14 30 90.91 40 91.01 50 92.81 60 83.89 70 89.5 80 84.78 90 86.44 100 87.66 V19-225tw Depth %CaCO3 0 25.61 5 24.74 10 34.44 15 36.05 20 35.03 24 39.25 RC17-55tw Depth %CaCO3 5 62.11 10 68.37 20 73.13 30 72.95 40 67.5 50 68.95 60 67.24 65 69.61 RC17-55 Depth %CaCO3 10 67.19 20 67.79 30 67.67 40 71.93 50 74.92 60 70.05 70 73.61 80 72.82 90 77.62 100 76.08 RC11-84 Depth/ Interval %CaCO3 0 41.22 5 49.11 10 55.96 15 48.91 20 52.98 25 51.64 30 53.6 35 46.87 40 47.36 45 53.23 50 54.08 55 50.27 60 55.66 65 56.78 70 56.77 75 40.47 80 43.52 85 43.28 90 42.18 95 44.01 100 39.22 105 32.39 110 36.67 115 36.43 120 32.17 125 34.17 130 39.15 135 24 140 29.22 145 9.26 150 19.7 155 2.03 160 4.73 165 9.62 170 16.55 175 18.78 180 20.17 185 19.56 190 24.02 195 23.06 200 25.25 205 31.05 210 35.44 215 41.56 220 41.88 225 42.49 230 51.12 235 49.59 240 44.9 245 56.15 250 50.44 255 49.43 260 45.25 265 33.49 270 29.46 275 25.54 280 19.1 285 3.23 290 35.84 295 41.97 300 56.51 310 47.24 315 40.38 320 45.98 325 43.01 330 44.43 335 36.67 340 29.06 345 7.93 350 7.81 355 21.13 360 15.14 365 13.62 370 5.42 375 3.97 380 2.1 385 0.31 390 0.14 395 1.17 400 0.78 405 1.22 410 0.9 415 1.19 420 3.81 425 6.98 430 7.61 435 9.56 440 4.39 445 1.31 450 1.4 455 0.95 460 0.28 465 0.15 470 0.85 475 0.12 480 0.11 485 0.13 490 0.2 495 2.62 500 9.31 505 11.29 510 12.48 515 10.02 520 15.18 525 13.48 530 12.8 535 9.44 540 26.64 545 32.53 550 37.49 555 37.47 560 33.94 565 33.61 570 32.26 575 41.4 580 44.35 585 45.04 590 41.55 595 37.49 600 28.67 605 13.18 610 22.73 615 8.54 620 9.27 625 4.4 630 4.25 635 1.8 640 0.73 645 0.35 650 4.02 655 20.28 660 17.05 665 15.98 670 19.54 675 20.86 680 29.05 685 32.23 690 29.11 695 32.56 700 26.56 705 21.1 710 21.76 715 12.06 720 0.82 725 0.23 730 0.39 735 1.74 6. Magnetic Susceptibility Magnetic susceptibility measured using a hand-held magnetometer at the Lamont-Doherty Earth Observatory (LDEO) of Columbia University. Sample depth in centimeters Magnetic susceptibility in SI units Age in kiloyears Missing values = null RC11-84 Depth Magnetic Susceptibility (SI units) 10 5 12 8 14 3 16 2 18 3 20 4 22 4 24 3 28 6 30 7 32 5 36 8 38 6 40 10 42 7 46 5 48 6 50 6 52 5 54 6 58 4 60 6 62 5 66 4 68 8 70 8 74 10 76 10 78 4 82 6 84 8 86 11 88 3 90 6 94 8 96 5 98 8 100 9 102 11 104 23 106 11 108 7 110 8 112 13 118 12 120 11 122 6 124 11 128 10 130 15 132 11 134 12 138 14 140 10 142 13 144 13 146 12 148 12 150 13 154 15 156 12 158 13 160 10 164 13 166 13 168 18 172 15 174 17 176 14 180 14 182 15 184 12 188 15 190 17 192 12 194 10 198 10 200 12 202 10 204 8 208 10 210 11 214 6 216 6 218 7 220 6 222 8 224 7 226 6 228 9 230 6 232 8 234 10 236 10 238 9 240 11 242 13 244 12 246 13 248 8 250 9 252 16 254 13 256 13 258 9 260 8 262 13 264 11 266 11 268 10 270 11 272 10 274 7 278 10 280 11 282 10 286 10 288 10 290 10 292 8 294 11 296 13 298 12 300 12 302 11 304 13 306 13 308 16 310 15 314 18 316 19 318 14 320 11 322 13 324 11 326 10 330 10 332 12 334 17 336 14 342 14 344 13 346 14 348 14 350 18 352 13 356 13 358 16 360 14 362 15 364 12 368 6 370 12 372 9 376 11 378 10 380 13 382 14 384 10 386 8 388 11 390 7 392 7 394 6 396 13 398 13 400 14 404 13 406 15 408 15 410 13 414 11 416 11 420 7 422 10 424 16 426 12 430 10 432 11 434 13 436 11 438 10 440 10 442 12 444 12 448 13 450 16 452 15 454 7 456 7 458 6 460 5 462 3 464 4 466 4 468 5 470 4 472 5 474 5 476 7 478 3 480 3 482 6 484 7 486 5 490 5 494 3 502 3 504 3 506 4 508 4 510 4 512 4 514 3 516 2 518 4 520 2 522 2 524 2 526 2 528 3 530 2 532 3 534 3 536 4 538 3 540 4 542 5 544 3 548 6 550 6 552 5 554 6 556 6 558 6 560 6 562 8 564 5 566 6 568 6 570 6 572 6 574 5 576 6 578 7 580 6 582 5 584 7 586 2 588 4 590 5 592 5 596 5 598 5 600 5 602 4 604 4 606 4 608 5 610 5 612 5 614 5 616 4 618 5 620 4 622 4 624 5 626 4 628 5 630 4 632 5 634 5 636 5 638 6 640 6 642 7 644 7 646 8 648 6 650 6 652 6 654 6 656 5 658 4 660 4 662 9 664 8 666 8 668 6 670 6 672 5 674 4 676 4 678 5 680 4 682 4 684 4 686 4 688 4 690 4 692 3 694 3 696 4 698 4 700 6 702 4 704 7 706 5 708 5 710 5 712 5 714 4 716 3 720 3 722 4 724 3 726 3 728 4 730 6 734 7 736 4 738 4 740 3 742 5 744 5 746 4 748 5 750 5 752 4 754 4 756 4 758 3 760 3 762 4 764 5 766 4 768 4 770 5 772 7 774 5 776 4 778 5 780 6 782 5 784 6 786 5 788 5 790 6 792 7 794 7 796 6 798 6 800 8 802 7 804 7 806 6 808 7 810 8 812 10 814 5 816 7 818 5 820 5 822 5 824 4 826 5 828 4 830 6 832 9 834 10 836 8 838 9 840 8 842 9 844 8 846 7 848 8 850 7 852 7 854 6 858 6 860 6 862 5 864 5 866 5 868 5 870 6 872 5 874 4 876 4 878 7 880 6 882 5 884 7 886 5 888 7 890 10 892 8 894 9 896 7 898 8 900 6 902 6 904 5 906 6 908 7 910 6 912 6 914 8 916 8 918 8 920 9 922 9 924 7 926 8 928 10 930 7 932 7 934 6 936 5 938 5 940 5 942 6 944 4 946 4 948 4 950 5 952 5 954 5 956 4 960 4 962 5 964 5 966 6 968 5 970 6 972 8 974 8 976 5 978 8 980 6 982 6 984 5 986 6 988 6 990 5 992 6 994 6 996 7 998 7 1000 8 1002 8 1004 8 1006 9 1008 7 1010 8 1012 8 1014 6 1016 8 1018 7 1020 6 1022 5 1024 4 1026 6 1028 7 1030 7 1032 8 1034 8 1036 7 1038 7 1040 6 1042 6 1044 5 1046 5 1048 4 1050 5 1052 6 1054 5 1056 4 1058 4 1060 5 1062 4 1064 4 1066 4 1068 5 1070 4 1072 7 1074 4 1076 4 1078 3 1080 3 1082 4 1084 5 1086 4 1088 6 1090 5 1092 6 1094 6 1096 5 1098 5 1100 6 1102 5 1104 6 1106 5 1108 5 1110 8 1112 7 1114 7 1116 6 1118 8 1120 8 1122 8 1124 9 1126 6 1128 9 1130 8 1132 6 1134 5 1136 4 1138 5 1140 8 1142 6 1144 4 1146 6 1148 6 1150 4 1152 5 1154 7 1156 8 1158 6 1160 7 1162 7 1164 6 1166 4 1172 6 1174 3 1176 6 1178 7 1182 4 1184 4 1186 4 1190 4 1192 3 1194 3 1196 3 1198 4 1200 4 1202 3 1204 3 1206 5 1208 4 1210 4 1212 3 1214 4 1216 4 1218 3 1220 4 1222 4 1224 3 1226 3 1228 4 1230 5 1234 6 1236 4 RC11-86 Depth Age Magnetic Susceptibility 10 5.3 2 12 5.9 2 14 6.5 2 16 7.1 2 18 7.6 2 20 8.2 2 22 8.8 1 24 9.3 2 26 9.9 1 28 10.5 1 30 11.1 1 32 11.6 2 34 12.2 2 36 13 2 38 14.3 2 40 15.5 3 42 16.8 2 44 18 2 46 19.3 1 48 20.5 1 50 21.8 1 52 23 1 54 24.3 1 56 25.2 5 58 25.7 8 60 26.3 3 62 26.8 3 64 27.3 1 66 27.9 1 68 28.4 1 70 29 1 72 29.5 2 74 30.1 1 76 30.8 1 78 31.4 1 80 31.9 1 82 32.5 1 84 33.1 1 86 34.5 1 88 35.3 1 90 36.1 1 92 37 1 94 37.8 1 96 38.6 1 98 39.5 1 100 40.3 1 102 41.2 1 104 42 1 106 42.9 1 108 43.7 1 110 44.6 2 112 45.4 2 114 46.3 3 116 47.1 2 118 48 1 120 48.8 2 122 49.7 1 124 50.6 1 126 51.4 1 128 52.3 2 130 53.1 1 132 54 1 134 54.9 1 136 55.7 4 138 56.6 3 140 57.4 2 142 58.3 3 144 59.2 1 146 60 3 148 60.9 2 150 61.8 2 152 62.6 5 154 63.5 7 156 64.3 2 158 65.2 3 160 66.1 1 162 66.9 1 164 67.8 1 166 68.6 5 168 69.5 2 172 71.2 2 174 72.1 5 176 73 3 178 73.8 3 180 74.7 4 182 75.6 6 184 76.4 5 186 77.3 4 188 78.2 9 190 79 10 192 79.9 2 194 80.8 4 196 81.6 5 198 82.5 3 200 83.4 3 202 84.3 5 204 85.1 3 206 86 2 208 86.9 1 210 87.8 2 212 88.7 3 214 89.6 3 216 90.5 3 218 91.4 2 220 92.3 3 222 93.2 4 224 94.1 4 226 95 2 228 95.9 3 230 96.8 3 232 97.7 1 234 98.7 1 236 99.6 1 238 101 1 240 102 1 242 102 1 244 103 1 246 104 1 248 105 1 250 106 1 252 107 1 254 108 1 256 109 1 258 110 1 260 111 1 262 112 1 264 113 3 266 114 2 268 116 2 270 117 2 272 118 1 274 119 1 276 120 1 278 121 1 280 122 1 282 123 1 284 124 2 286 126 2 288 127 1 290 128 1 292 129 2 294 130 4 296 132 6 298 133 5 300 134 7 302 135 8 304 136 4 306 137 8 308 138 5 310 140 1 312 141 1 314 142 1 316 143 1 318 144 1 320 145 1 322 146 1 324 147 1 326 149 1 328 150 1 330 151 1 332 152 1 334 153 3 336 154 3 338 155 8 340 157 7 342 158 3 344 159 4 346 160 3 348 161 1 350 162 1 352 163 1 354 164 1 356 166 1 358 167 1 360 168 1 362 169 1 364 170 1 366 171 1 368 172 1 370 174 1 372 175 1 374 176 1 376 177 1 378 178 1 380 179 2 382 180 1 384 181 1 386 183 1 388 184 1 390 185 1 392 186 1 394 187 2 396 188 1 398 189 3 400 190 3 402 192 3 404 193 4 406 194 4 408 195 1 410 196 1 412 197 2 414 198 1 416 200 1 418 201 2 420 202 1 422 203 1 424 204 2 426 205 1 428 206 1 430 207 3 432 209 4 434 210 2 436 211 2 438 212 1 440 213 2 442 214 1 444 215 2 446 216 1 448 218 3 450 219 2 452 220 2 454 221 3 456 222 3 458 223 2 460 224 4 462 226 1 464 227 1 466 228 1 468 229 1 470 230 1 472 231 1 474 232 1 476 233 1 478 235 1 480 236 1 482 237 1 484 238 1 486 239 1 488 240 2 490 241 1 492 243 1 494 244 1 496 245 1 498 246 1 500 247 2 502 248 1 504 249 2 506 250 1 508 252 2 510 253 1 512 254 1 514 255 2 516 256 1 518 257 1 520 258 1 522 259 1 524 261 1 526 262 1 528 263 1 530 264 2 532 265 3 534 266 5 536 267 4 538 269 3 540 270 3 542 271 3 544 272 1 546 273 3 548 274 1 550 275 2 552 276 2 554 278 1 556 279 1 558 280 2 560 281 5 562 282 6 564 283 2 566 284 1 568 285 1 570 287 1 572 288 2 574 289 2 576 290 1 578 291 1 580 292 1 582 293 1 584 295 1 586 296 1 588 297 1 590 298 1 592 299 1 594 300 1 596 301 1 598 302 4 600 304 3 602 305 2 604 306 1 606 307 1 608 308 1 610 309 1 612 310 1 614 312 1 616 313 1 618 314 1 620 315 2 622 316 1 624 317 1 626 318 1 628 319 1 630 321 1 632 322 1 634 323 1 636 324 1 638 325 1 640 326 1 642 327 1 644 328 1 646 330 1 648 331 1 650 332 1 652 333 1 654 334 1 656 335 1 658 336 1 660 338 1 662 339 2 664 340 1 666 341 1 668 342 1 670 343 1 672 344 1 674 345 1 676 347 1 678 348 1 680 349 1 682 350 1 684 351 1 686 352 1 688 353 1 690 354 1 692 356 1 694 357 3 696 358 2 698 359 2 700 360 4 702 361 2 704 362 2 706 364 3 708 365 5 710 366 4 712 367 3 714 368 2 716 369 3 718 370 3 720 371 3 722 373 2 724 374 3 726 375 3 728 376 3 730 377 2 732 378 2 734 379 2 736 381 2 738 382 2 740 383 1 742 384 2 744 385 2 746 386 1 748 387 1 750 388 2 752 390 1 754 391 2 756 392 2 758 393 2 760 394 1 762 395 2 764 396 1 766 397 4 768 399 1 770 400 2 772 401 1 774 402 2 776 403 1 778 404 1 780 405 1 782 407 1 784 408 2 786 409 1 788 410 2 790 411 1 792 412 1 794 413 1 796 414 1 798 416 1 800 417 1 802 418 1 804 419 1 806 420 1 808 421 1 810 422 1 812 423 1 814 425 1 816 426 1 818 427 1 820 428 1 822 429 1 824 430 2 826 431 1 828 433 1 830 434 1 832 435 1 834 436 1 836 437 1 838 438 2 840 439 2 842 440 2 844 442 2 846 443 2 848 444 1 850 445 1 852 446 1 854 447 1 856 448 1 858 450 1 860 451 2 862 452 1 864 453 1 866 454 2 868 455 1 870 456 1 872 457 2 874 459 1 876 460 1 878 461 1 880 462 1 882 463 2 884 464 2 886 465 1 888 466 1 890 468 1 892 469 1 894 470 1 896 471 1 898 472 1 900 473 1 902 474 1 904 476 1 906 477 2 908 478 2 910 479 2 912 480 3 914 481 1 916 482 1 918 483 1 920 485 1 922 486 2 924 487 3 926 488 5 RC11-87 Depth Magnetic Susceptibility 0 17 2 12 4 11 6 8 8 9 10 9 12 8 14 8 16 7 18 6 20 6 22 7 24 6 26 5 28 5 30 6 32 6 34 5 36 5 38 4 40 4 42 4 44 4 46 3 48 3 50 3 52 3 54 3 56 5 58 5 60 5 62 4 64 5 66 4 68 4 70 4 72 5 74 4 76 5 78 5 80 6 82 7 84 7 86 5 88 6 90 6 92 5 94 4 96 4 98 4 100 3 102 4 104 3 106 3 108 3 110 2 112 4 114 4 116 4 118 4 120 5 122 5 124 4 126 4 128 5 130 5 132 7 134 8 136 7 138 6 140 6 142 6 144 5 146 4 148 5 150 6 152 6 154 6 156 7 158 6 160 7 162 6 164 5 166 5 168 6 170 6 172 6 174 5 176 5 178 7 180 7 182 7 184 6 186 5 188 6 190 7 192 6 194 5 196 5 198 5 200 5 202 6 204 6 206 7 208 6 210 7 212 6 214 5 216 5 218 4 220 6 222 5 224 6 226 5 228 4 230 5 232 4 234 5 236 5 238 6 240 7 242 6 244 8 246 7 248 7 250 7 252 7 254 7 256 7 258 6 260 6 262 7 264 5 266 5 268 6 270 7 272 8 274 8 276 7 278 8 280 8 282 6 284 7 286 6 288 5 290 6 292 6 294 8 296 6 298 6 300 7 302 8 304 8 306 9 308 9 310 12 312 11 314 14 316 11 318 15 320 16 322 15 324 16 326 16 328 14 330 12 332 11 334 14 336 15 338 14 340 15 342 13 344 21 346 11 350 12 352 15 354 15 356 15 358 15 360 17 362 15 364 14 366 15 368 14 370 17 372 14 374 15 376 14 378 15 380 14 382 14 384 12 386 14 388 14 390 12 392 12 394 13 396 13 398 9 400 13 402 13 404 9 406 8 408 10 410 9 412 8 414 6 RC17-69 Depth Age Magnetic Susceptibility 0 4.28 24 2 4.47 16 4 4.96 18 6 5.46 15 8 5.96 17 10 6.45 18 12 6.95 17 14 7.45 18 16 7.94 20 18 8.44 20 20 8.94 19 22 9.44 22 24 9.93 24 26 10.4 21 28 10.9 18 30 11.4 19 32 11.9 19 34 12.4 18 36 12.9 18 38 13.4 17 40 13.9 14 42 14.4 17 44 14.9 18 46 15.4 18 48 15.9 20 50 16 18 52 17.6 16 54 19.2 19 56 20.8 19 58 22.4 11 60 24 14 62 25.6 9 64 27.2 12 66 28.8 12 68 30.4 15 70 32 15 72 32.6 17 74 33.4 13 76 34.2 13 78 35.1 15 80 35.9 14 82 36.8 11 84 37.6 16 86 38.5 15 88 39.3 18 90 40.1 14 92 41 16 94 41.8 17 96 42.7 18 98 43.5 15 100 44.4 19 102 45.2 12 104 46 14 106 46.9 15 108 47.7 13 110 48.6 15 112 49.4 14 114 50.3 19 116 51.1 20 118 51.9 19 120 52.8 20 122 53.6 23 124 54.5 23 126 55.3 22 128 56.2 25 130 57 22 132 57.8 22 134 58.7 20 136 59.5 20 138 60.4 19 140 61.2 18 142 62.1 16 144 62.9 15 146 63.7 14 148 64.6 14 150 65.4 16 152 66.3 14 154 67.1 19 156 68 14 158 68.8 18 160 69.6 13 162 70.5 15 164 71.3 15 166 72.2 16 168 73 17 170 73.9 19 172 74.7 14 174 75.5 13 176 76.4 12 178 77.2 14 180 78.1 9 182 78.9 8 184 79.8 11 186 80.6 11 188 81.4 15 190 82.3 12 192 83.1 14 194 84 15 196 84.8 17 198 85.7 18 200 86.4 19 202 87.2 18 204 88.1 17 206 89 16 208 89.8 15 210 90.7 16 212 91.6 21 214 92.4 24 216 93.3 20 218 94.1 25 220 95 20 222 95.9 14 224 96.7 22 226 97.6 22 228 98.5 23 230 99.3 21 232 100 19 234 101 19 236 102 19 238 103 19 240 104 16 242 105 20 244 105 19 246 106 24 248 107 23 250 108 22 252 109 22 254 110 22 256 111 19 258 111 18 260 112 19 262 113 19 264 114 17 266 115 17 268 116 15 270 117 14 272 117 13 274 118 17 276 119 17 278 120 19 280 121 17 282 122 13 284 123 21 286 124 22 288 124 21 290 125 22 292 126 13 294 127 20 296 128 23 298 129 23 300 130 22 302 130 18 304 131 17 306 132 15 308 133 14 310 134 16 312 135 13 314 136 12 316 136 13 318 137 14 320 138 10 322 139 7 324 140 7 326 141 9 328 142 8 330 143 14 332 143 21 334 144 24 336 145 23 338 146 21 340 147 21 342 148 21 344 149 20 346 149 20 348 150 24 350 151 26 352 152 27 354 153 23 356 154 20 358 155 26 360 155 23 362 156 25 364 157 21 366 158 20 368 159 19 370 160 8 372 161 18 374 161 10 376 162 13 378 163 14 380 164 17 382 165 17 384 166 16 386 167 15 388 168 16 390 168 15 392 169 14 394 170 20 396 171 14 398 172 16 400 173 16 402 174 20 404 174 18 406 175 16 408 176 19 410 177 12 412 178 18 414 179 21 416 180 18 418 180 19 420 181 11 422 182 12 424 183 14 426 184 10 428 185 13 430 186 17 432 187 14 434 187 14 436 188 14 438 189 17 440 190 9 442 191 13 444 192 9 446 193 9 448 193 9 450 194 7 452 195 8 454 196 9 456 197 10 458 198 8 460 199 7 462 199 8 464 200 11 466 201 8 468 202 7 470 203 10 472 204 9 474 205 9 476 206 11 478 206 4 480 207 14 482 208 12 484 209 12 486 210 17 488 211 11 490 212 12 492 212 14 494 213 12 496 214 2 498 215 10 500 216 10 502 217 13 504 218 12 506 218 10 508 219 10 510 220 7 512 221 7 514 222 6 516 223 7 518 224 8 520 225 8 522 225 7 524 226 3 526 227 3 528 228 7 530 229 6 532 230 6 534 231 6 536 231 6 538 232 6 540 233 8 542 234 9 544 235 10 546 236 9 548 237 13 550 237 12 552 238 9 554 239 8 556 240 13 558 241 11 560 242 11 562 243 10 564 244 11 566 244 9 568 245 10 570 246 9 572 247 7 574 248 6 576 249 8 578 250 9 580 250 10 582 251 12 584 252 11 586 253 13 588 254 15 590 255 15 592 256 17 594 256 14 596 257 15 598 258 15 600 259 13 602 260 12 604 261 13 606 262 13 608 263 12 610 263 11 612 264 11 614 265 9 616 266 11 618 267 10 620 268 12 622 269 14 624 269 13 626 270 12 628 271 13 630 272 12 632 273 12 634 274 14 636 275 15 638 275 13 640 276 2 642 277 10 644 278 8 646 279 8 648 280 6 650 281 4 652 282 4 654 282 4 656 283 6 658 284 5 660 285 2 662 286 4 664 287 5 666 288 5 668 288 8 670 289 10 672 290 9 674 291 10 676 292 10 678 293 11 680 294 11 682 294 9 684 295 10 686 296 13 688 297 4 690 298 13 692 299 14 694 300 16 696 301 16 698 301 15 700 302 17 702 303 16 704 304 16 706 305 17 708 306 15 710 307 14 712 307 13 714 308 12 716 309 12 718 310 10 720 311 11 722 312 11 724 313 11 726 313 12 728 314 12 730 315 12 732 316 13 734 317 10 736 318 11 738 319 8 740 319 9 742 320 9 744 321 9 746 322 9 748 323 6 750 324 6 752 325 4 754 326 4 756 326 3 758 327 5 760 328 5 762 329 5 764 330 4 766 331 3 768 332 2 770 332 4 772 333 5 774 334 4 776 335 3 778 336 4 780 337 6 782 338 6 784 338 null 786 339 6 788 340 4 790 341 5 792 342 6 794 343 6 796 344 6 798 345 5 800 345 4 802 346 6 804 347 6 806 348 5 808 349 5 810 350 4 812 351 5 814 351 4 816 352 7 818 353 6 820 354 8 822 355 8 824 356 10 826 357 10 828 357 10 830 358 8 832 359 6 834 360 6 836 361 7 838 362 8 840 363 8 842 364 6 844 364 6 846 365 9 848 366 7 850 367 8 852 368 11 854 369 11 856 370 12 858 370 11 860 371 7 862 372 7 864 373 6 866 374 5 868 375 5 870 376 6 872 376 7 874 377 8 876 378 6 878 379 4 880 380 4 882 381 5 884 382 9 886 383 9 888 383 9 890 384 11 892 385 12 894 386 11 896 387 12 898 388 11 900 389 13 902 389 11 904 390 11 906 391 11 908 392 14 910 393 12 912 394 13 914 395 14 VM14-65 Depth Age Magnetic Susceptibility 0 0.96 18 2 1.21 21 4 1.45 20 6 1.7 23 8 1.94 21 10 2.18 17 12 2.43 21 14 2.67 24 16 2.9 21 18 3.14 20 20 3.38 16 22 3.61 20 24 3.84 19 26 4.08 18 28 4.31 17 30 4.54 19 32 4.76 19 34 4.99 18 36 5.21 18 38 5.44 16 40 5.66 15 42 5.88 15 44 6.1 13 46 6.32 15 48 6.54 14 50 6.76 13 52 6.97 13 54 7.19 11 56 7.4 9 58 7.61 9 60 7.82 7 62 8.03 5 64 8.24 6 66 8.44 8 68 8.65 5 70 8.86 7 72 9.06 6 74 9.26 6 76 9.46 6 78 9.66 6 80 9.86 6 82 10.1 6 84 10.3 6 86 10.5 5 88 10.6 5 90 10.8 6 92 11 5 94 11.2 6 96 11.4 6 98 11.6 5 100 11.8 8 102 12 6 104 12.2 7 106 12.3 7 108 12.5 7 110 12.7 7 112 12.9 5 114 13.1 5 116 13.3 7 118 13.4 6 120 13.6 7 122 13.8 5 124 14 7 126 14.1 6 128 14.3 4 130 14.5 5 132 14.7 5 134 14.8 7 136 15 6 138 15.2 6 140 15.3 4 142 15.5 5 144 15.7 6 146 15.8 6 148 16 6 150 16.2 6 152 16.3 6 154 16.5 5 156 16.7 7 158 16.8 9 160 17 8 162 17.1 8 164 17.3 7 166 17.5 8 168 17.6 9 170 17.8 9 172 17.9 9 174 18.1 9 176 18.2 8 178 18.4 10 180 18.5 9 182 18.7 11 184 18.8 9 186 19 11 188 19.1 10 190 19.3 12 192 19.4 10 194 19.6 12 196 19.7 9 198 19.9 13 200 20 13 202 20.1 11 204 20.3 12 206 20.4 12 208 20.6 11 210 20.7 12 212 20.9 11 214 21 11 216 21.1 11 218 21.3 12 220 21.4 11 222 21.5 12 224 21.7 13 226 21.8 13 228 21.9 11 230 22.1 12 232 22.2 11 234 22.3 11 236 22.5 7 238 22.6 14 240 22.7 14 242 22.9 13 244 23 13 246 23.1 12 248 23.3 11 250 23.4 10 252 23.5 12 254 23.6 10 256 23.8 11 258 23.9 9 260 24 11 262 24.1 12 264 24.3 12 266 24.4 12 268 24.5 12 270 24.6 10 272 24.8 11 274 24.9 10 276 25 9 278 25.1 11 280 25.3 12 282 25.4 11 284 25.5 11 286 25.6 10 288 25.7 9 290 25.8 12 292 26 11 294 26.1 9 296 26.2 8 298 26.3 7 300 26.4 9 302 26.5 7 304 26.7 8 306 26.8 8 308 26.9 8 310 27 7 312 27.1 6 314 27.2 8 316 27.3 6 318 27.5 5 320 27.6 6 322 27.7 7 324 27.8 6 326 27.9 6 328 28 5 330 28.1 6 332 28.2 5 334 28.3 4 336 28.5 6 338 28.6 7 340 28.7 6 342 28.8 5 344 28.9 5 346 29 4 348 29.1 7 350 29.2 6 352 29.3 5 354 29.4 6 356 29.5 7 358 29.6 6 360 29.7 7 362 29.9 7 364 30 6 366 30.1 8 368 30.2 5 370 30.3 6 372 30.4 8 374 30.5 7 376 30.6 7 378 30.7 5 380 30.8 6 382 30.9 6 384 31 6 386 31.1 6 388 31.2 7 390 31.3 5 392 31.4 8 394 31.5 6 396 31.6 7 398 31.7 8 400 31.8 8 402 31.9 7 404 32 9 406 32.1 8 408 32.2 8 410 32.3 6 412 32.4 8 414 32.5 7 416 32.6 6 418 32.7 7 420 32.8 6 422 32.9 7 424 33 8 426 33.1 8 428 33.2 8 430 33.3 9 432 33.4 9 434 33.5 10 436 33.6 10 438 33.8 9 440 33.9 9 442 34 9 444 34.1 8 446 34.2 7 448 34.3 7 450 34.4 8 452 34.5 6 454 34.6 7 456 34.7 7 458 34.8 6 460 34.9 6 462 35 6 464 35.1 6 466 35.2 6 468 35.3 6 470 35.4 7 472 35.5 5 474 35.6 5 476 35.7 4 478 35.8 4 480 35.9 5 482 36 3 484 36.1 4 486 36.2 3 488 36.3 4 490 36.4 3 492 36.5 3 494 36.6 4 496 36.7 4 498 36.8 5 500 36.9 4 502 37 4 504 37.1 2 506 37.2 3 508 37.3 3 510 37.4 2 512 37.5 3 514 37.6 3 516 37.7 4 518 37.8 5 520 37.9 5 522 38 8 524 38.1 9 526 38.2 11 528 38.3 11 530 38.4 5 532 38.5 5 534 38.6 4 536 38.7 3 538 38.8 2 540 38.9 3 542 39 4 VM18-184 Depth Magnetic Susceptibility 8 15 10 20 12 15 14 18 16 16 18 12 20 12 22 13 24 12 26 15 28 20 30 14 32 7 34 6 36 7 38 7 40 7 42 9 44 10 46 10 48 12 50 11 52 6 54 7 56 9 58 5 60 8 62 8 64 8 66 10 68 11 70 13 72 9 74 10 76 10 78 11 80 11 82 15 84 18 86 12 88 14 90 18 92 10 94 9 96 9 98 15 100 14 102 14 104 13 106 12 108 15 110 18 112 13 114 10 116 9 118 11 120 8 122 6 124 14 126 10 128 9 130 11 132 11 134 10 136 13 138 12 140 11 142 15 144 12 146 11 148 11 150 10 152 10 154 14 156 10 158 15 160 17 162 14 164 7 166 6 168 9 170 13 172 11 174 8 176 8 178 11 180 8 182 13 184 9 186 16 188 9 190 7 192 6 194 9 196 7 198 6 200 9 202 8 204 13 206 11 208 9 210 9 212 8 214 8 216 6 218 7 220 7 222 7 224 7 226 7 228 7 230 6 232 8 234 9 236 11 238 12 240 10 242 10 244 9 246 9 248 8 250 9 252 8 254 11 256 8 258 7 260 7 262 7 264 6 266 6 268 6 270 9 272 7 274 7 276 8 278 9 280 11 282 11 284 7 286 11 288 15 290 15 292 9 294 8 296 7 298 7 300 8 302 10 304 17 306 null 308 17 310 13 312 9 314 9 316 11 318 13 320 13 322 12 324 10 326 14 328 15 330 15 332 null 334 null 336 null 338 null 340 null 342 null 344 null 346 null 348 null 350 null 352 null 354 null 356 null 358 null 360 null 362 null 364 null 366 null 368 null 370 null 372 null 374 null 376 null 378 null 380 null 382 null 384 null 386 null 388 null 390 null 392 null 394 null 396 null 398 null 400 null 402 6 404 10 406 10 408 10 410 8 412 8 414 9 416 7 418 7 420 8 422 6 424 7 426 null 428 7 430 6 432 6 434 6 436 6 438 4 440 3 442 3 444 3 446 4 448 4 450 4 452 4 454 4 456 4 458 5 460 5 462 6 464 8 466 8 468 6 470 5 472 5 474 5 476 4 478 4 480 4 482 5 484 5 486 7 488 6 490 6 492 6 494 6 496 6 498 5 500 4 502 4 504 4 506 5 508 5 510 5 512 5 514 6 516 6 518 8 520 10 522 10 524 10 526 8 528 6 530 6 532 5 534 4 536 4 538 4 540 4 542 4 544 4 546 6 548 5 550 5 552 5 554 5 556 5 558 6 560 5 562 6 564 4 566 4 568 5 570 5 572 5 574 6 576 7 578 7 580 6 582 5 584 6 586 4 588 4 590 5 592 6 594 6 596 5 598 5 600 5 602 5 604 4 606 5 608 6 610 7 612 4 614 4 616 4 618 3 620 3 622 3 624 3 626 3 628 3 630 3 632 3 634 3 636 3 638 3 640 3 642 4 644 4 646 4 648 3 650 3 652 4 654 6 656 8 658 10 660 10 662 5 VM19-224 Depth Magnetic Susceptibility 0 11 2 14 4 13 6 16 8 20 10 12 12 14 14 11 16 14 18 13 20 14 22 11 24 11 26 10 28 9 30 10 32 10 34 10 36 11 38 10 40 11 42 12 44 11 46 16 48 16 50 16 52 16 54 19 56 14 58 16 60 15 62 13 64 16 66 14 68 11 70 12 72 14 74 21 76 11 78 8 80 10 82 11 84 14 86 16 88 21 90 14 92 12 94 14 96 21 98 16 100 22 102 18 104 19 106 16 108 12 110 12 112 16 114 18 116 20 118 8 120 null 122 null 124 null 126 null 128 null 130 null 132 null 134 null 136 null 138 null 140 5 142 6 144 7 146 10 148 9 150 6 152 5 154 6 156 8 158 6 160 6 162 6 164 9 166 11 168 9 170 9 172 11 174 12 176 12 178 15 180 16 182 16 184 18 186 20 188 20 190 20 192 26 194 17 196 15 198 16 200 21 202 15 204 12 206 14 208 14 210 15 212 16 214 14 216 11 218 13 220 14 222 16 224 13 226 15 228 18 230 20 232 17 234 18 236 18 238 14 240 13 242 15 244 14 246 13 248 12 250 11 252 13 254 16 256 13 258 7 260 8 262 6 264 null 266 null 268 null 270 null 272 null 274 null 276 null 278 null 280 4 282 7 284 4 286 4 288 4 290 4 292 4 294 4 296 4 298 5 300 5 302 8 304 10 306 11 308 11 310 10 312 10 314 9 316 10 318 12 320 12 322 11 324 10 326 8 328 8 330 9 332 8 334 8 336 8 338 8 340 null 342 null 344 7 346 9 348 10 350 11 352 14 354 15 356 14 358 13 360 12 362 13 364 12 366 10 368 11 370 10 372 13 374 14 376 12 378 12 380 10 382 12 384 12 386 14 388 17 390 19 392 21 394 19 396 17 398 16 400 14 402 14 404 13 406 13 408 11 410 13 412 14 414 13 416 16 418 14 420 15 422 18 424 17 426 15 428 19 430 16 432 14 434 11 436 11 438 11 440 12 442 11 444 12 446 12 448 11 450 11 452 9 454 15 456 13 458 13 460 13 462 13 464 11 466 9 468 11 470 14 472 12 474 12 476 11 478 10 480 8 482 6 484 6 486 9 488 7 490 9 492 9 494 9 496 10 498 9 500 9 502 6 504 6 506 5 508 5 510 5 512 7 514 8 516 10 518 10 520 7 522 6 524 6 526 9 528 11 530 10 532 9 534 9 536 9 538 8 540 11 542 14 544 14 546 11 548 7 550 8 552 8 554 7 556 7 558 6 560 5 562 5 564 5 566 5 568 6 570 7 572 8 574 7 576 8 578 9 580 9 582 10 584 11 586 12 588 9 590 8 592 11 VM20-201 Depth Magnetic Susceptibility 8 7 10 7 12 7 14 7 16 7 18 7 20 7 22 9 24 9 26 9 28 8 30 9 32 9 34 9 36 8 38 11 40 10 42 9 44 11 46 11 48 10 50 10 52 11 54 9 56 8 58 9 60 9 62 10 64 10 66 10 68 9 70 9 72 7 74 10 76 9 78 8 80 8 82 8 84 8 86 9 88 7 90 6 92 6 94 6 96 6 98 4 100 7 102 9 104 8 106 8 108 6 110 7 112 7 114 8 116 7 118 6 120 7 122 7 124 7 126 6 128 6 130 8 132 10 134 10 136 7 138 5 140 4 142 4 144 3 146 null 148 7 150 7 152 7 154 8 156 9 158 8 160 9 162 8 164 8 166 6 168 4 170 7 172 7 174 7 176 7 178 7 180 6 182 6 184 6 186 7 188 7 190 7 192 7 194 7 196 7 198 7 200 7 202 9 204 9 206 8 208 7 210 8 212 8 214 9 216 8 218 8 220 8 222 9 224 8 226 9 228 7 230 8 232 7 234 7 236 6 238 5 240 7 242 9 244 9 246 8 248 8 250 8 252 9 254 6 256 5 258 4 260 5 262 5 264 5 266 5 268 6 270 6 272 5 274 6 276 5 278 6 280 5 282 5 284 4 286 4 288 4 290 5 292 5 294 5 296 5 298 4 300 4 302 4 304 4 306 5 308 5 310 4 312 4 314 4 316 4 318 4 320 6 322 7 324 7 326 7 328 6 330 6 332 5 334 4 336 4 338 4 340 4 342 5 344 5 346 5 348 6 350 6 352 6 354 5 356 5 358 6 360 6 362 5 364 5 366 5 368 5 370 4 372 4 374 4 376 5 378 4 380 5 382 5 384 5 386 5 388 5 390 5 392 4 394 4 396 4 398 4 400 4 402 4 404 4 406 4 408 4 410 4 412 4 414 4 416 4 418 4 420 5 422 5 424 3 426 5 428 5 430 5 432 4 434 4 436 4 438 4 440 4 442 4 444 5 446 4 448 5 450 6 452 6 454 6 456 6 458 6 460 5 462 5 464 4 466 5 468 5 470 5 472 5 474 4 476 4 478 4 480 5 482 5 484 5 486 5 488 5 490 5 492 5 494 5 496 5 498 5 500 5 502 5 504 5 506 6 508 6 510 7 512 6 514 5 516 5 518 5 520 4 522 5 524 5 526 5 528 4 530 5 532 4 534 4 536 4 538 4 540 3 542 4 544 4 546 4 548 5 550 6 552 5 554 5 556 5 558 5 560 5 562 5 564 6 566 4 568 4 570 5 572 3 574 4 576 3 578 4 580 4 582 4 584 4 586 3 588 4 590 4 592 3 594 3 596 3 598 3 600 4 602 4 604 4 606 5 608 4 610 4 612 4 614 4 616 4 618 4 620 4 622 5 624 5 626 5 628 4 630 5 632 4 634 4 636 4 638 4 640 4 642 4 644 3 646 3 648 3 650 4 652 4 654 4 656 4 658 5 660 5 662 5 664 4 666 4 668 6 670 5 672 5 674 5 676 5 678 5 680 5 682 5 684 4 686 4 688 5 690 5 692 5 694 6 696 5 698 6 700 6 702 5 704 5 706 4 708 4 710 4 712 4 714 4 716 3 718 3 720 3 722 3 724 3 726 3 728 3 730 3 732 2 734 3 736 3 738 2 740 3 742 2 744 2 746 2 748 2 750 2 752 2 754 3 756 3 758 2 760 2 762 2 764 2 766 3 768 3 770 3 772 3 774 3 776 3 778 3 780 2 782 4 784 4 786 4 788 3 790 4 792 3 794 3 796 3 798 3 800 3 802 3 804 3 806 3 808 3 810 4 812 4 814 3 816 3 818 3 820 2 822 3 824 3 826 3 828 3 830 3 832 3 834 3 836 3 838 3 840 3 842 4 844 4 846 4 848 3 850 4 852 4 854 5 856 4 858 4 860 4 862 4 864 4 866 3 868 3 870 4 872 4 874 4 876 3 878 3 880 3 882 3 884 3 886 3 888 3 890 3 892 3 894 3 896 4 898 5 900 4 902 4 904 5 906 5 908 4 910 5 912 5 914 5 916 5 918 6 920 6 922 6 924 6 926 6 928 6 930 6 932 6 934 6 936 6 938 5 940 5 942 5 944 5 946 5 948 5 950 5 952 4 VM24-216 Depth Magnetic Susceptibility 10 18 12 16 14 15 16 15 18 21 20 16 22 15 24 16 26 13 28 15 30 14 32 13 34 13 36 11 38 17 40 18 42 19 44 10 46 18 48 20 50 20 52 22 54 20 56 15 58 18 60 11 62 19 64 12 66 null 68 6 70 8 72 17 74 11 76 11 78 8 80 11 82 15 84 11 86 19 88 11 90 20 92 20 94 14 96 17 98 13 100 14 102 20 104 22 106 null 108 18 110 25 112 17 114 16 116 17 118 18 120 13 122 10 124 10 126 10 128 15 130 17 132 18 134 13 136 21 138 22 140 21 142 11 144 11 146 25 148 19 150 22 152 14 154 11 156 9 158 15 160 11 162 22 164 18 166 19 168 null 170 null 172 16 174 14 176 10 178 19 180 null 182 14 184 11 186 16 188 18 190 15 192 16 194 16 196 13 198 11 200 9 202 9 204 9 206 11 208 13 210 11 212 11 214 12 216 12 218 12 220 14 222 null 224 9 226 10 228 10 230 11 232 11 234 9 236 8 238 9 240 8 VM29-94 Depth Magnetic Susceptibility 8 11 10 11 12 11 14 11 16 11 18 11 20 13 22 13 24 12 26 12 28 12 30 12 32 11 34 12 36 13 38 15 40 16 42 15 44 15 46 14 48 13 50 11 52 12 54 13 56 13 58 11 60 12 62 11 64 10 66 11 68 12 70 11 72 11 74 7 76 9 78 10 80 11 82 13 84 13 86 11 88 11 90 11 92 10 94 9 96 10 98 10 100 10 102 7 104 5 106 6 108 8 110 11 112 10 114 8 116 8 118 4 120 3 122 2 124 3 126 3 128 4 130 5 132 5 134 6 136 7 138 6 140 5 142 5 144 5 146 5 148 5 150 5 152 4 154 null 156 null 158 null 160 null 162 null 164 null 166 null 168 5 170 5 172 5 174 7 176 6 178 6 180 5 182 4 184 5 186 6 188 6 190 7 192 8 194 8 196 8 198 6 200 6 202 5 204 8 206 7 208 8 210 10 212 10 214 9 216 8 218 6 220 8 222 9 224 7 226 10 228 11 230 11 232 11 234 11 236 11 238 12 240 12 242 9 244 11 246 10 248 12 250 12 252 12 254 11 256 12 258 12 260 14 262 15 264 13 266 14 268 15 270 14 272 12 274 11 276 13 278 12 280 12 282 14 284 13 286 14 288 11 290 14 292 12 294 13 296 13 298 13 300 14 302 15 304 18 306 17 308 17 310 15 312 16 314 17 316 16 318 15 320 14 322 14 324 14 326 17 328 18 330 17 332 21 334 22 336 22 338 22 340 17 342 17 344 16 346 18 348 21 350 23 352 19 354 20 356 20 358 20 360 18 362 17 364 16 366 15 368 14 370 16 372 21 374 22 376 20 378 22 380 21 382 19 384 16 386 14 388 15 390 14 392 16 394 19 396 17 398 14 400 13 402 13 404 12 406 13 408 11 410 10 412 9 414 8 416 9 418 9 420 7 422 8 424 7 426 6 428 6 430 6 432 6 434 6 436 6 438 5 440 5 442 5 444 6 446 6 448 5 450 5 452 5 454 4 456 5 458 4 460 4 462 4 464 4 466 4 468 4 470 3 472 3 474 3 476 3 478 4 480 4 482 4 484 5 486 6 488 5 490 7 492 6 494 7 496 6 498 6 500 8 502 9 504 8 506 8 508 8 510 7 512 6 514 7 516 6 518 7 520 7 522 7 524 7 526 8 528 8 530 8 532 8 534 7 536 7 538 8 540 9 542 7 544 8 546 7 548 7 550 7 552 8 554 8 556 7 558 7 560 7 562 8 564 8 566 9 568 8 570 7 572 8 574 8 576 8 578 8 580 9 582 8 584 9 586 9 588 8 590 8 592 8 594 7 596 6 598 5 600 null 602 null 604 null 606 null 608 null 610 null 612 null 614 null 616 null 618 null 620 null 622 null 624 null 626 null 628 null 630 null 632 null 634 null 636 null 638 null 640 null 642 null 644 null 646 null 648 null 650 null 652 null 654 null 656 null 658 null 660 5 662 6 664 6 666 5 668 6 670 5 672 7 674 5 676 7 678 7 680 7 682 7 684 7 686 7 688 null 690 null 692 null 694 null 696 7 698 7 700 7 702 7 704 7 706 6 708 5 710 7 712 7 714 6 716 6 718 7 720 7 722 8 724 8 726 8 728 8 730 8 732 9 734 9 736 10 738 9 740 9 742 10 744 9 746 8 748 8 750 8 752 7 754 8 756 8 758 8 760 8 762 9 764 9 766 9 768 9 770 10 772 9 774 8 776 8 778 8 780 8 782 8 784 7 786 8 788 8 790 8 792 8 794 9 796 11 798 10 800 9 802 10 804 12 806 13 808 12 810 11 812 13 814 13 816 12 818 9 820 9 822 10 824 9 826 9 828 10 830 10 832 14 834 14 836 14 838 14 840 14 842 16 844 18 846 16 848 16 850 15 852 15 854 16 856 15 858 15 860 15 862 16 864 16 866 13 868 12 870 12 872 12 874 11 876 11 878 11 880 11 882 10 884 10 886 9 888 9 890 7 892 7 894 6 896 8 898 7 900 6 902 6 904 8 906 6 908 7 910 7 912 7 914 6 916 6 918 6 920 6 922 5 VM34-157 Depth Age Magnetic Susceptibility 10 3.54 2 12 3.74 1 14 3.97 1 16 4.22 1 18 4.51 1 20 4.82 3 22 5.17 3 24 5.54 3 26 5.95 3 28 6.38 2 30 6.85 2 32 7.34 2 34 7.86 2 36 8.41 2 38 9 1 40 9.61 2 42 10.2 1 44 10.9 2 46 11.6 3 48 12.4 3 50 13.1 4 52 13.9 3 54 14.7 4 56 15.6 3 58 16.4 2 60 17.4 1 62 18.3 2 64 19.3 1 66 20.3 1 68 21.4 2 70 22.8 1 72 24.1 1 74 25.3 2 76 26.4 2 78 27.4 2 80 28.3 1 82 29.1 2 84 29.9 1 86 30.6 1 88 31.2 1 90 31.8 1 92 32.4 1 94 32.8 1 96 33.3 1 98 33.7 1 100 34.1 1 102 34.5 1 104 34.8 1 106 35.1 1 108 35.5 1 110 35.8 1 112 36.1 1 114 36.4 2 116 36.7 2 118 37.1 1 120 37.5 1 122 37.9 2 124 38.3 2 126 38.8 1 128 39.3 1 130 39.9 1 132 40.5 1 134 41.2 1 136 41.9 1 138 42.7 1 140 43.6 1 142 44.3 1 144 44.9 1 146 45.6 1 148 46.2 1 150 46.8 1 152 47.4 1 154 48 1 156 48.7 1 158 49.3 1 160 49.9 1 162 50.5 1 164 51.2 1 166 51.8 1 168 52.4 2 170 53 3 172 53.7 2 174 54.3 2 176 54.9 3 178 55.5 4 180 56.2 3 182 56.8 2 184 57.4 1 186 58 1 188 58.7 1 190 59.3 2 192 59.9 1 194 60.5 1 196 61.2 1 198 61.8 1 200 62.4 1 202 63 1 204 63.6 2 206 64.3 1 208 64.9 1 210 65.5 3 212 66.1 2 214 66.8 1 216 67.4 1 218 68 1 220 68.6 1 222 69.3 2 224 69.9 1 226 70.5 1 228 71.1 1 230 71.8 1 232 72.4 1 234 73 0 236 73.6 1 238 74.3 0 240 74.9 1 242 75.5 1 244 76.1 1 246 76.8 1 248 77.4 1 250 78 2 252 78.6 2 254 79.2 2 256 79.9 2 258 80.5 2 260 81.1 2 262 81.7 3 264 82.4 3 266 83 3 268 83.6 4 270 84.2 6 272 84.9 5 274 85.5 4 276 86.1 3 278 86.7 4 280 87.4 4 282 88 4 284 88.6 4 286 89.2 1 288 89.9 1 290 90.5 1 292 91.1 1 294 91.7 1 296 92.4 1 298 93 2 300 93.6 1 302 94.2 2 304 94.8 1 306 95.5 1 308 96.1 2 310 96.7 2 312 97.3 1 314 98 1 316 98.6 1 318 99.2 1 320 99.8 1 322 100 1 324 101 1 326 102 1 328 102 2 330 103 2 332 104 1 334 104 1 336 105 1 338 105 1 340 106 1 342 107 1 344 107 1 346 108 1 348 109 1 350 109 1 352 110 2 354 110 1 356 111 2 358 112 2 360 112 2 362 113 2 364 114 2 366 114 2 368 115 2 370 115 2 372 116 2 374 117 2 376 117 2 378 118 2 380 119 2 382 119 2 384 119 2 386 120 2 388 121 2 390 121 2 392 122 2 394 123 2 396 123 2 398 124 2 400 125 2 402 126 2 404 126 2 406 127 2 408 128 2 410 128 1 412 129 1 414 130 1 416 130 1 418 131 1 420 132 1 422 132 1 424 133 1 426 134 1 428 134 1 430 135 1 432 136 1 434 136 1 436 137 1 438 138 1 440 138 1 442 139 1 444 140 1 446 140 1 448 141 1 450 142 1 452 142 1 454 143 1 456 143 1 458 144 1 460 145 1 462 145 1 464 146 2 466 146 1 468 147 1 470 148 1 472 148 1 474 149 1 476 149 1 478 150 1 480 151 1 482 151 1 484 152 1 486 152 1 488 153 2 490 153 1 492 154 2 494 155 2 496 155 1 498 156 1 500 156 1 502 157 1 504 157 2 506 158 2 508 158 1 510 159 1 512 159 2 514 160 1 516 161 1 518 161 1 520 162 1 522 162 1 524 163 1 526 163 2 528 164 2 530 164 1 532 165 1 534 165 1 536 166 2 538 166 12 540 167 2 542 167 1 544 168 1 546 168 1 548 169 1 552 170 2 554 170 2 556 171 2 558 171 1 560 172 1 562 172 1 564 173 1 566 173 2 568 173 2 570 174 2 572 174 2 574 175 1 576 175 1 578 176 1 580 176 1 582 177 1 584 177 1 586 178 1 588 178 1 590 179 1 592 179 1 594 180 1 596 180 1 598 181 1 600 181 1 602 182 1 604 182 1 606 183 1 608 183 1 610 184 1 612 184 2 614 184 2 616 185 2 618 185 1 620 186 1 622 186 1 624 187 1 626 187 1 628 188 2 630 188 1 632 189 1 634 189 1 636 190 1 638 190 3 640 191 2 642 191 2 644 192 1 646 192 1 648 193 1 650 194 1 652 194 2 654 195 1 656 195 1 658 196 1 660 196 1 662 197 1 664 197 2 666 198 2 668 198 1 670 199 1 672 199 1 674 200 1 676 201 1 678 201 1 680 202 1 682 202 1 684 203 1 686 203 1 688 204 1 690 205 1 692 205 1 694 206 2 696 206 1 698 207 1 700 208 1 702 208 1 704 209 1 706 209 1 708 210 1 710 211 1 712 211 1 714 212 2 716 213 1 718 213 1 720 214 1 722 214 1 724 215 1 726 216 1 728 216 1 730 217 1 732 218 1 734 218 1 736 219 1 738 220 1 740 220 1 742 221 0 744 222 1 746 222 1 748 223 2 750 224 1 752 224 1 754 225 1 756 226 1 758 227 1 760 227 2 762 228 2 764 229 2 766 229 1 768 230 2 770 231 2 772 232 1 774 232 1 776 233 1 778 234 1 780 234 1 782 235 2 784 236 3 786 237 2 788 237 3 790 238 2 792 239 3 794 239 2 796 240 2 798 241 2 800 242 2 802 242 1 804 243 1 806 244 1 808 244 1 810 245 1 812 246 1 814 247 1 816 247 1 818 248 2 820 249 1 822 249 1 824 250 2 826 251 2 828 251 2 830 252 1 832 253 2 834 253 1 836 254 1 838 255 2 840 255 1 842 256 2 844 257 1 846 257 2 848 258 1 850 259 2 852 259 2 854 260 2 856 260 1 858 261 1 860 262 1 862 262 1 864 263 2 866 263 1 868 264 1 870 264 1 872 265 1 874 265 1 876 266 1 878 266 1 880 267 1 882 267 1 884 267 1 886 268 1 888 268 1 890 269 1 892 269 1 894 269 1 896 270 1 898 270 1 900 270 1 902 271 2 904 271 1 906 271 1 908 271 1 910 271 1 912 272 1 914 272 1 916 272 1 918 272 2 920 272 1 922 272 1 924 272 1 926 272 1 928 272 1 930 null 1 932 null 1 934 null 1 936 null 1 938 null 1 940 null 1 942 null 1 944 null 1 946 null 1 948 null 1 950 null 2 952 null 1 954 null 1 956 null 1 958 null 1 960 null 1 962 null 1 964 null 1 966 null 1 968 null 1 970 null 1 972 null 1 974 null 1 976 null 1 978 null 2 980 null 1 982 null 1 984 null 1 986 null 1 988 null 1 990 null 1 992 null 1 994 null 1 996 null 1 998 null 1 1000 null 1 1002 null 1 1004 null 1 1006 null 2 1008 null 1 1010 null 1 1012 null 1 1014 null 1 1016 null 1 1018 null 1 1020 null 1 1022 null 1 1024 null 1 1026 null 1 1028 null 1 1030 null 1 1032 null 1 1034 null 1 1036 null 1 1038 null 1 1040 null 1 1042 null 1 1044 null 1 1046 null 2 1048 null 1 1050 null 1 1052 null 1 1054 null 2 1056 null 1 1058 null 1 1060 null 1 1062 null 1 1064 null 1 1066 null 1 1068 null 1 1070 null 1 1072 null 1 1074 null 1 1076 null 2 1078 null 2 1080 null 1 1082 null 1 1084 null 1 1086 null 1 1088 null 1 1090 null 2 1092 null 1 1094 null 1 1096 null 1 1098 null 1 1100 null 1 1102 null 1 1104 null 1 1106 null 1 1108 null 1 1110 null 1 1112 null 1 1114 null 1 1116 null 1