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Sarnthein, Michael; Balmer, Sven; Grootes, Pieter Meiert; Mudelsee, Manfred (2014): (Table 2i) Planktic and benthic 14C and 14C reservoir ages of sediment core MD02-2489 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.837488, In supplement to: Sarnthein, M et al. (2015): Planktic and benthic 14C reservoir ages for three ocean basins, calibrated by a suite of 14C plateaus in the glacial-to-deglacial Suigetsu atmospheric 14C record. Radiocarbon, 57(1), 129-151, https://doi.org/10.2458/azu_rc.57.17916

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Related to:
Gebhardt, Holger; Sarnthein, Michael; Grootes, Pieter Meiert; Kiefer, Thorsten; Kühn, Hartmut; Schmieder, Frank; Röhl, Ursula (2008): Paleonutrient and productivity records from the subarctic North Pacific for Pleistocene glacial terminations I to V. Paleoceanography, 23(4), PA4212, https://doi.org/10.1029/2007PA001513 (original 14C age publication)
Gebhardt, Holger; Sarnthein, Michael; Grootes, Pieter Meiert; Kiefer, Thorsten; Kühn, Hartmut; Schmieder, Frank; Röhl, Ursula (2008): Radiocarbon ages of sediment core MD02-2489 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.708672 (original 14C age publication)
Coverage:
Latitude: 54.390700 * Longitude: -148.921300
Date/Time Start: 2002-05-23T00:00:00 * Date/Time End: 2002-05-23T00:00:00
Minimum DEPTH, sediment/rock: 0.5900 m * Maximum DEPTH, sediment/rock: 6.8400 m
Event(s):
MD02-2489 (MD022489) * Latitude: 54.390700 * Longitude: -148.921300 * Date/Time: 2002-05-23T00:00:00 * Elevation: -3640.0 m * Recovery: 29.8 m * Campaign: MD122 (IMAGES VII - WEPAMA) * Basis: Marion Dufresne (1995) * Method/Device: Giant piston corer (GPC) * Comment: Originally the site and core belonged to the cruise IMAGES VII WEPAMA but was postponed due to tight schedule. The core was then taken in 2002, during transit, preliminary to cruise IMAGES VIII MONA.
Comment:
All 14C dates are rounded to decades. Planktic plateau boundaries were either defined at or in between single 14C ages of the records. For reasons of specimen availability paired benthic 14C ages were partly analyzed at core depths without any paired planktic correlative 14C age immediately corresponding. Here the planktic-benthic age difference was derived from interpolated neighbor planktic dates
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Laboratory code/labelLab labelSarnthein, Michael
2DEPTH, sediment/rockDepth sedmGeocode
3Age, dated materialDated materialSarnthein, Michael
4Age, datedAge datedkaSarnthein, MichaelAge, 14C AMSraw planktic/benthic 14C date
5Age, dated, error to olderAge e +ka +Sarnthein, MichaelAge, 14C AMSraw planktic/benthic 14C date, 1 sigma
6Age, dated, error to youngerAge e -ka -Sarnthein, MichaelAge, 14C AMSraw planktic/benthic 14C date, 1 sigma
7Age, commentCommSarnthein, MichaelSUIGETSU Plateau No.
8Reservoir ageRes agekaSarnthein, Michaelapp. plankt. res. age vs. Suigetsu (14C)
9Calendar ageCal ageka BPSarnthein, MichaelAge, 14C calibratedtuned to Suigetsu varve counts
10CommentCommentSarnthein, Michael
11Age, differenceAge diffkaSarnthein, Michaelbenthic-planktic
12Reservoir ageRes agekaSarnthein, Michaelbenthic res. age vs. Suigetsu (14C)
Size:
453 data points

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