Search results for "SO147"

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(Table 1) Sea surface temperature reconstruction for eastern equatorial Pacific surface sediment samples

2012

Significant uncertainties persist in the reconstruction of past sea surface temperatures in the eastern equatorial Pacific, especially regarding the amplitude of the glacial cooling and the details of the post-glacial warming. Here we present the first regional calibration of alkenone unsaturation in surface sediments versus mean annual sea surface temperatures (maSST). Based on 81 new and 48 previously published data points, it is shown that open ocean samples conform to established global regressions of Uk'37 versus maSST and that there is no systematic bias from seasonality in the production or export of alkenones, or from surface ocean nutrient concentrations or salinity. The flattening…

Reference sourceRC23RR9702ASea surface temperatureannual meaninterpolatedV21Roger A RevellePiston corer (BGR type)ME0005Aunsaturation index UK 37VemaKNR182 91988RC18Marion Dufresne (1995)Hakuho MaruKH-03-1MultiCorerTemperaturePiston corer BGR typeAMPHITRITEsediment rockRoger A. RevelleKH 03 1Earth System ResearchLeg138Robert ConradCoreWecomaCalculated from UK 37 Prahl et alPiston corerMoana WaveLongitude of eventHakuho-MaruAlkenone unsaturation index UK'37Thomas WashingtonW7706differenceKNR176-2KNR195-5Leg201DEPTH sediment/rockVNTR01SO147PLDS 3Sea surface temperature annual meanPLDS-3Giant piston corerMW8708MelvilleMD126Marion Dufresne 1995KnorrRC11RC13Event labelJoides ResolutionYALOC69Calculated from UK'37 (Prahl et al. 1988)V19ArgoSonneKNR176 2KNR195 5DEPTHYaquinaKNR182-9Gravity corerTemperature differenceBox corerAlkenoneComposite CoreSCANReference/source
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(Table 1) Age determination of sediment core SO147_106KL

2005

Here we present a high-resolution marine sediment record from the El Niño region off the coast of Peru spanning the last 20,000 years. Sea surface temperature, photosynthetic pigments, and a lithic proxy for El Niño flood events on the continent are used as paleo-El Niño-Southern Oscillation proxy data. The onset of stronger El Niño activity in Peru started around 17,000 calibrated years before the present, which is later than modeling experiments show but contemporaneous with the Heinrich event 1. Maximum El Niño activity occurred during the early and late Holocene, especially during the second and third millennium B.P. The recurrence period of very strong El Niño events is 60-80 years. El…

Age datedPiston corer (BGR type)SonneAge maximum/oldAge minimum/youngLaboratory code/labelAge dated error to youngerAge dated error to olderAge 14C calibratedDEPTH sediment/rockSO147Age 14C AMSAge model
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