noaa-ocean-19982 Global Sea Level Reconstruction using Stacked Records from 0-800 ka Spratt, R.M.; Lisiecki, L.E. Global Sea Level Reconstruction using Stacked Records from 0-800 ka 2016-04-11 NCDC-Paleoclimatology ONLINE Files Pending https://www.ncdc.noaa.gov/paleo/study/19982 Investigator R.M. Spratt Investigator L.E. Lisiecki earth science paleoclimate climate reconstructions|paleoceanography sea level,delta 18O,null,meter,null,climate reconstructions|paleoceanography,null,null,N,Scaled first principal component of five sea level reconstructions (0-798 ka); meters above modern sea level earth science paleoclimate climate reconstructions|paleoceanography sea level,delta 18O,95% confidence interval lower bound,meter,null,climate reconstructions|paleoceanography,null,null,N,Scaled first principal component of five sea level reconstructions (0-798 ka) earth science paleoclimate paleoceanography age,null,null,calendar kiloyear before present,null,paleoceanography,null,null,N,null earth science paleoclimate climate reconstructions|paleoceanography sea level,delta 18O,95% confidence interval upper bound,meter,null,climate reconstructions|paleoceanography,null,null,N,Scaled first principal component of seven sea level reconstructions (0-430 ka) earth science paleoclimate climate reconstructions|paleoceanography sea level,delta 18O,95% confidence interval upper bound,meter,null,climate reconstructions|paleoceanography,null,null,N,Scaled first principal component of five sea level reconstructions (0-798 ka) earth science paleoclimate climate reconstructions|paleoceanography sea level,delta 18O,one standard deviation,meter,null,climate reconstructions|paleoceanography,null,null,N,Scaled first principal component of seven sea level reconstructions (0-430 ka) earth science paleoclimate climate reconstructions|paleoceanography sea level,delta 18O,95% confidence interval lower bound,meter,null,climate reconstructions|paleoceanography,null,null,N,Scaled first principal component of seven sea level reconstructions (0-430 ka) earth science paleoclimate climate reconstructions|paleoceanography sea level,delta 18O,one standard deviation,meter,null,climate reconstructions|paleoceanography,null,null,N,Scaled first principal component of five sea level reconstructions (0-798 ka) earth science paleoclimate climate reconstructions|paleoceanography sea level,delta 18O,null,meter,null,climate reconstructions|paleoceanography,null,null,N,Scaled first principal component of seven sea level reconstructions (0-430 ka); standard deviation from bootstrap; meters above modern sea level earth science paleoclimate paleocean reconstruction geoscientificInformation Sea Level Reconstruction -798000 cal yr BP 0 cal yr BP Complete -40.937 61.425 -180 180 Geographic Region Global Global 61.5N to 41S>LATITUDE >LONGITUDE None Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site. English DOC/NOAA/NESDIS/NCEI National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce https://www.ncdc.noaa.gov/data-access/paleoclimatology-data DATA Center Contact Bruce Bauer bruce.a.bauer@noaa.gov paleo@noaa.gov 303-497-6280 303-497-6513

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Boulder CO 80305-3328 USA online ASCII Rachel M. Spratt and Lorraine E. Lisiecki 2016 Climate of the Past 12 1079-1092 10.5194/cp-12-1-2016 https://www.clim-past.net/12/1079/2016/

Late Pleistocene sea level has been reconstructed from ocean sediment core data using a wide variety of proxies and models. However, the accuracy of individual reconstructions is limited by measurement error, local variations in salinity and temperature, and assumptions particular to each technique. Here we present a sea level stack (average) which increases the signal-to-noise ratio of individual reconstructions. Specifically, we perform principal component analysis (PCA) on seven records from 0-430 ka and five records from 0-798 ka. The first principal component, which we use as the stack, describes ~80% of the variance in the data and is similar using either five or seven records. After scaling the stack based on Holocene and Last Glacial Maximum (LGM) sea level estimates, the stack agrees to within 5 m with isostatically adjusted coral sea level estimates for Marine Isotope Stages 5e and 11 (125 and 400 ka, respectively). Bootstrapping and random sampling yield mean uncertainty estimates of 9-12 m (1s) for the scaled stack. Sea level change accounts for about 45% of the total orbital-band variance in benthic d18O, compared to a 65% contribution during the LGM-to-Holocene transition. Additionally, the second and third principal components of our analyses reflect differences between proxy records associated with spatial variations in the d18O of seawater. STUDY NOTES: Late Pleistocene sea level stack based on marine sediment core data (foraminiferal carbonate d18O) as estimated by several different techniques in seven different studies. Sea level stack is a compilation data from the following published sea level reconstructions: Bintanja, R., Roderik, S.W., van de Wal, O. J.: Modeled atmospheric temperatures and global sea levels over the past million years, Nature, 437, 125-128 doi:10.1038/nature03975, 2005. ; Elderfield, H., Ferretti, P., Greaves, M., Crowhurst, S. J., McCave, I.N., Hodell, D. A., Piotrowski, A. M.: Evolution of ocean temperature and ice volume through the Mid-Pleistocene Climate Transition, Science, 337,6095, 704-709, doi:10.1126/science.1221294, 2012.; Rohling, E.J., Grant, K., Bolshaw, M., Roberts, A.P., Siddall, M., Hemleben, C., Kucera, M.: Antarctic temperature and global sea level closely coupled over the past five glacial cycles. Nat. Geosci., 2, 500–504, 2009.; Rohling, E. J., Grant, K.M., Bolshaw, M., Roberts, A. P., Siddall, M., Hemleben C. Kucera, M., Foster, G.L., Marino, G., Roberts, A.P., Tamisiea, M.E., and Williams, F.: Sea-level and deep-sea-temperature variability over the past 5.3 million years, Nature, 508, 477–482, 2014.; Shakun, J. D., Lea, D. W., Lisiecki, L. E., Raymo, M. E.: An 800-kyr record of global surface ocean d18O and implications for ice volume-temperature coupling, Earth. Planet. Sc. Lett., 426, 58–68, 2015.; Sosdian S., Rosenthal Y.: Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions, Science, 17, 325, 5938, 306-310, doi: 10.1126/science.1169938, 2009.; Waelbroeck, C., Labeyrie, L., Michel, E., Duplessy J.C., McManus J.: Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records, Quaternary Sci. Rev., 21, 295–305, 2002. Provided Keywords: sea level, Pleistocene

GET DATA https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/spratt2016/spratt2016.txt Formatted Text File; Sea Level Stack data USA/NOAA DIF Version 9.8.4 2018-12-11 2018-12-11