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Spratt, Rachel M; Lisiecki, Lorraine E (2025): A Late Pleistocene sea level stack, version 2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.979830

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Published: 2025-03-20DOI registered: 2025-03-20

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Abstract:
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). When we compare the sea level stack with the d18O of benthic foraminifera, we find that sea level change accounts for about ~40 % 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.
Supplement to:
Spratt, Rachel M; Lisiecki, Lorraine E (2016): A Late Pleistocene sea level stack. Climate of the Past, 12(4), 1079-1092, https://doi.org/10.5194/cp-12-1079-2016
Source:
Spratt, Rachel M; Lisiecki, Lorraine E (2016): NOAA/WDS Paleoclimatology - Global Sea Level Reconstruction using Stacked Records from 0-800 ka [dataset]. NOAA National Centers for Environmental Information, https://doi.org/10.25921/RD66-5820
Comment:
This version presents the data of the published paper and replaces doi:10.1594/PANGAEA.854045 which presented the data of the discussion paper.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1AGEAgeka BPSpratt, Rachel MGeocode
2Sea levelSea levelm NNSpratt, Rachel MSeaLev_shortPC1: Scaled first principal component of seven sea level reconstructions (0-430 ka), meters above modern sea level
3Sea level, standard deviationSea level std dev±Spratt, Rachel MSeaLev_shortPC1_err_sig: Scaled first principal component of seven sea level reconstructions (0-430 ka), meters above modern sea level, standard deviation from bootstrap
4Confidence interval lower limitCI lowSpratt, Rachel MSeaLev_shortPC1_err_lo: Scaled first principal component of seven sea level reconstructions (0-430 ka), meters above modern sea level, 95% confidence interval lower bound
5Confidence interval upper limitCI upSpratt, Rachel MSeaLev_shortPC1_err_up: Scaled first principal component of seven sea level reconstructions (0-430 ka), meters above modern sea level, 95% confidence interval upper bound
6Sea levelSea levelm NNSpratt, Rachel MSeaLev_longPC1: Scaled first principal component of five sea level reconstructions (0-798 ka), meters above modern sea level
7Sea level, standard deviationSea level std dev±Spratt, Rachel MSeaLev_longPC1_err_sig: Scaled first principal component of five sea level reconstructions (0-798 ka), meters above modern sea level, standard deviation from bootstrap
8Confidence interval lower limitCI lowSpratt, Rachel MSeaLev_longPC1_err_lo: Scaled first principal component of five sea level reconstructions (0-798 ka), meters above modern sea level, 95% confidence interval lower bound
9Confidence interval upper limitCI upSpratt, Rachel MSeaLev_longPC1_err_up: Scaled first principal component of five sea level reconstructions (0-798 ka), meters above modern sea level, 95% confidence interval upper bound
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
6392 data points

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