/* DATA DESCRIPTION: Citation: Rühlemann, Carsten (2004): Paleoproductivity as carbon of sediment core GeoB1523-1. PANGAEA, https://doi.org/10.1594/PANGAEA.55909 Related to: Rühlemann, Carsten; Frank, Martin; Hale, Walter; Mangini, Augusto; Mulitza, Stefan; Müller, Peter J; Wefer, Gerold (1996): Late Quaternary productivity changes in the western equatorial Atlantic: Evidence from 230Th-normalized carbonate and organic carbon accumulation rates. Marine Geology, 135(1-4), 127-152, https://doi.org/10.1016/S0025-3227(96)00048-5 Project(s): Geosciences, University of Bremen (GeoB) (URI: https://www.geo.uni-bremen.de/page.php?langid=EN) Coverage: LATITUDE: 3.831667 * LONGITUDE: -41.621667 DATE/TIME START: 1991-05-17T00:00:00 * DATE/TIME END: 1991-05-17T00:00:00 MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 4.48 m Event(s): GeoB1523-1 * LATITUDE: 3.831667 * LONGITUDE: -41.621667 * DATE/TIME: 1991-05-17T00:00:00 * ELEVATION: -3292.0 m * Recovery: 6.65 m * LOCATION: Amazon Fan * CAMPAIGN: M16/2 (URI: https://doi.org/10.2312/cr_m16) * BASIS: Meteor (1986) (URI: https://en.wikipedia.org/wiki/RV_Meteor_(1986)) * METHOD/DEVICE: Gravity corer (Kiel type) (SL) Parameter(s): DEPTH, sediment/rock [m] (Depth sed) * GEOCODE Paleoproductivity as carbon [g/m**2/a] (PP C) * PI: Rühlemann, Carsten (c.ruehlemann@bgr.de) * METHOD/DEVICE: Calculated, see reference(s) * COMMENT: based on empirical relationship after Müller & Suess (1979) and on sedimentation rates obtained by normalizing to 230Th (excess) (see Rühlemann et al, 1996) Paleoproductivity as carbon [g/m**2/a] (PP C) * PI: Rühlemann, Carsten (c.ruehlemann@bgr.de) * METHOD/DEVICE: Calculated, see reference(s) * COMMENT: based on empirical relationship after Sarnthein et al (1992) and on sedimentation rates obtained by normalizing to 230Th (excess) (see Rühlemann et al, 1996) Paleoproductivity as carbon [g/m**2/a] (PP C) * PI: Rühlemann, Carsten (c.ruehlemann@bgr.de) * METHOD/DEVICE: Calculated, see reference(s) * COMMENT: based on empirical relationship after Stein (1986) and on sedimentation rates obtained by normalizing to 230Th (excess) (see Rühlemann et al, 1996) Paleoproductivity as carbon [g/m**2/a] (PP C) * PI: Rühlemann, Carsten (c.ruehlemann@bgr.de) * METHOD/DEVICE: Calculated, see reference(s) * COMMENT: based on empirical relationship after Van Kreveld et al (1996) and on sedimentation rates obtained by normalizing to 230Th (excess) (see Rühlemann et al, 1996) License: Creative Commons Attribution 3.0 Unported (CC-BY-3.0) (URI: https://creativecommons.org/licenses/by/3.0/) Size: 364 data points */ Depth sed [m] PP C [g/m**2/a] (based on empirical relationsh...) PP C [g/m**2/a] (based on empirical relationsh...) PP C [g/m**2/a] (based on empirical relationsh...) PP C [g/m**2/a] (based on empirical relationsh...) 0.00 59 96 76 60 0.03 63 94 77 58 0.08 46 84 60 57 0.13 40 82 54 58 0.18 35 83 52 63 0.23 31 83 49 55 0.28 26 81 44 49 0.33 28 82 46 38 0.38 31 82 48 39 0.43 31 82 48 39 0.48 33 84 51 37 0.53 33 83 50 34 0.58 33 80 49 33 0.63 34 80 49 36 0.68 32 80 48 38 0.73 36 84 53 43 0.78 36 87 55 48 0.83 39 90 59 52 0.88 40 92 61 54 0.93 36 88 56 50 0.98 40 88 58 45 1.03 39 87 57 45 1.08 42 92 63 49 1.13 37 88 56 48 1.18 40 86 57 44 1.23 37 84 54 42 1.28 46 89 63 46 1.33 40 86 57 51 1.38 38 87 56 51 1.43 40 88 58 49 1.48 37 85 54 46 1.53 35 84 53 43 1.58 30 83 48 40 1.63 32 83 50 33 1.68 30 81 47 27 1.73 35 84 52 28 1.78 35 87 55 30 1.83 33 86 52 34 1.88 39 92 60 34 1.93 36 88 56 41 1.98 36 86 54 38 2.03 38 84 54 41 2.08 34 82 50 49 2.13 30 78 46 44 2.18 29 77 44 40 2.23 27 77 42 30 2.28 28 78 44 34 2.33 28 79 44 44 2.38 28 83 47 55 2.43 27 82 45 56 2.48 31 81 48 49 2.53 33 80 49 47 2.58 33 78 47 47 2.63 30 76 44 47 2.68 31 76 45 43 2.73 28 77 43 42 2.78 24 79 41 39 2.83 23 81 42 35 2.88 24 79 41 39 2.93 24 79 41 43 2.98 30 85 49 56 3.03 28 79 44 55 3.08 34 76 46 48 3.13 31 74 44 50 3.18 25 73 39 51 3.23 22 72 36 50 3.28 20 72 34 47 3.33 20 74 36 41 3.38 23 76 39 38 3.43 26 76 41 43 3.48 28 77 43 40 3.53 28 77 43 36 3.58 27 77 43 34 3.63 36 81 51 32 3.68 36 80 51 30 3.73 40 82 54 29 3.78 41 83 56 29 3.83 37 82 53 29 3.88 35 82 51 29 3.93 35 86 54 33 3.98 29 89 51 49 4.03 35 91 57 48 4.08 30 81 47 38 4.13 32 83 49 36 4.18 36 89 57 41 4.23 39 90 59 52 4.28 42 89 60 53 4.33 36 88 56 57 4.38 30 90 53 69 4.43 30 90 52 63 4.48 23 81 42 52