/* DATA DESCRIPTION: Citation: Schulz, Hartmut (1995): Age model of sediment core SO90-111KL. PANGAEA, https://doi.org/10.1594/PANGAEA.55229, In supplement to: Schulz, H (1995): Meeresoberflächentemperaturen vor 10.000 Jahren - Auswirkungen des frühholozänen Insolationsmaximums = Sea-surface temperatures 10,000 years B.P. - consequences of the early Holocene insolation maximum. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 73, 156 pp, https://doi.org/10.2312/reports-gpi.1995.73 Related to: Schulz, Hartmut; von Rad, Ulrich; Erlenkeuser, Helmut (1998): Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years. Nature, 393(6680), 54-57, https://doi.org/10.1038/31750 Coverage: LATITUDE: 23.096000 * LONGITUDE: 66.483000 DATE/TIME START: 1993-09-19T00:00:00 * DATE/TIME END: 1993-09-19T00:00:00 MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 14.30 m Event(s): SO90_111KL * LATITUDE: 23.096000 * LONGITUDE: 66.483000 * DATE/TIME: 1993-09-19T00:00:00 * ELEVATION: -775.0 m * Recovery: 14.45 m * LOCATION: Arabian Sea * CAMPAIGN: SO90 (PAKOMIN) (URI: https://doi.org/10.2312/cr_so90) * BASIS: Sonne (URI: https://en.wikipedia.org/wiki/RV_Sonne) * METHOD/DEVICE: Piston corer (BGR type) (KL) * COMMENT: GPS, Parameter(s): DEPTH, sediment/rock [m] (Depth sed) * GEOCODE Age model [ka] (Age model) * PI: Schulz, Hartmut (hartmut.schulz@uni-tuebingen.de, https://www.uni-tuebingen.de/en/faculties/faculty-of-science/departments/geosciences/arbeitsgruppen/palaeobiology/research-area/micropaleontology/working-group/members/hartmut-schulz.html) * METHOD/DEVICE: Age model, SPECMAP chronology, Imbrie et al. (1984) (URI: hdl:10013/epic.48655.d001) * COMMENT: calendar years License: Creative Commons Attribution 3.0 Unported (CC-BY-3.0) (URI: https://creativecommons.org/licenses/by/3.0/) Size: 35 data points */ Depth sed [m] Age model [ka] 0.00 2.00 0.70 9.70 0.95 11.45 1.40 12.60 1.90 12.90 2.20 14.50 2.40 16.10 3.40 17.20 3.80 19.20 5.02 23.30 5.30 24.00 5.50 24.70 5.72 25.50 6.32 27.70 6.68 28.90 7.18 30.10 7.55 30.70 7.82 32.10 8.15 33.50 8.52 35.10 9.55 38.20 10.00 39.30 10.42 40.10 10.68 41.10 11.05 42.50 11.50 43.30 11.72 45.30 11.92 45.90 12.60 46.90 13.05 51.60 13.35 53.50 13.58 56.20 13.72 57.50 14.00 60.80 14.30 61.90