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Metadata for a compilation of 127 benthic δ¹³C time series (20-6 ka)
Abbreviations for ocean and sea regionsINA: intermediate North Atlantic OceanUDNA: upper deep North Atlantic OceanLDNA: lower deep North Atlantic OceanISA: intermediate South... -
Full Brazilian margin (Brazil Current and North Brazil Current) sea surface t...
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Raw SST data for the full BR SST stack
Comment to Sea surface temperature, standard deviation from Core GL1090:2sd[-] =Q0.025;1sd[-] =Q0.16;1sd[+] =Q0.84;2sd[+] =Q0.975 -
GGC90 benthic 14C dates and calculated calendar ages, which strenthen the age...
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Planktonic 14C dates and calculated calendar ages in core GGC90 (Supplementar...
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Intermediate water reconstructions in core GGC90 (Supplementary Table 6)
Averaged [PO43-] and T are Umling et al. (2019), and averaged [CO32-] data are from Lacerra et al (2019). S and [CO32-]as are from this study. See Methods for calculation details. -
Age model controlling dates used for core GGC90 (Supplementary Table 9)
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Cibicides spp. oxygen isotopes of sediment core JPC-17
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MAT-derived sea surface temperature of sediment core JPC-17
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Planktonic foraminifera assemblage of sediment core JPC-17
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(Table S2) Epsilon-Nd data of planktic foraminifera of sediment core KNR159-36
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(Table S4c) Age control points used for calculation of sedimentation rates of...
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(Table S3c) 14C ages measured on Globigerinoides ruber of sediment core KNR15...
*Came et al.. 2003; #Sortor and Lund. 2011.14C ages, 14C plateaus, and age conversion into calendar ages in three sediment cores from the tropical and subtropical South... -
(Table S1 c) Definition of planktic 14C plateaus for sediment core KNR159-5-3...
Plateau No. YD - 5a: Two suites of 14C outliers with approximately uniform 14C age each are ascribed to two events of Zoophycos burrowing (Fig.2). Below Plateau 5a a 14C jump of... -
Stable isotope ratios of Cibicidoides of sediment core KNR159-36
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Cd/Ca ratios of Uvigerina spp. of sediment core KNR159-36
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Seawater Cd estimates for sediment core KNR159-36
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(Table 2) Holocene Cd reconstruction for Brazil Margin sediment cores
d13C results are not from the same samples in which Cd was measured (and in some cases are from different cores within 77 m water depth). -
(Table 1) LGM Cd reconstruction for Brazil Margin sediment cores
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World Ocean 14C plateau tuning
On the basis of minor time scale adjustments including the synchronization on IntCal20 the Suigetsu-based atmospheric 14C plateau structures are shown to be authentic. Their...