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Table 1 Control points for the age model for core MD972151
Accelerator mass spectrometry (AMS) C-14 ages were obtained for nine samples using calcareous tests of single species of the planktonic foraminifer G. sacculifer. Marine isotope... -
Alkenone-derived Holocene Sea Surface Temperature database
see dating methoda: Correlation with GISP2 oxygen isotope record (Grootes and Stuiver, 1997).b: The age model of the core AD91-17 is based on AMS 14C, planktonic isotopic record... -
Sea surface temperature reconstruction from sediment core MD97-2151 using alk...
This dataset has no description
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Sea surface temperature reconstruction from sediment core MD97-2121 using alk...
This dataset has no description
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Sea surface temperature reconstruction from sediment core MD97-2120 using alk...
This dataset has no description
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Sea surface temperature reconstruction from sediment core MD97-2141 using Mg/...
This dataset has no description
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Sea surface temperature reconstruction from sediment core MD97-2125 using Mg/...
This dataset has no description
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Sea surface temperature reconstruction from sediment core MD97-2120 using Mg/...
This dataset has no description
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Mg/Ca-derived Holocene Sea Surface Temperature database
Dating method:(a) radiocarbon + correlation with nearby MD98-2176(b) AMS 14C on ME-43JC; ODP1242 is correlated with ME43-JC through comparison of d18O. Mg/Ca and sediment... -
Summary of sea surface temperature trends reconstructed from alkenones for th...
Trend >0 means a warming over the time period, trend <0 means a cooling over the time period. -
Summary of sea surface temperature trends reconstructed from Mg/Ca ratios for...
Trend >0 means a warming over the time period, trend <0 means a cooling over the time period. -
Table 3: Extent of amino acid racemisation (total acid hydrolysate) in marine...
This dataset has no description
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Table 2: AMS radiocarbon ages from carbonate microfossils of sediment core MD...
The ages are initially presented in conventional radiocarbon years (5730 a half-life), corrected for isotopic fractionation, and without reservoir correction. Samples with d13C... -
Table 2: AMS radiocarbon ages from carbonate microfossils of sediment core MD...
The ages are initially presented in conventional radiocarbon years (5730 a half-life), corrected for isotopic fractionation, and without reservoir correction. Samples with d13C... -
Table 2: AMS radiocarbon ages from carbonate microfossils of sediment core MD...
The ages are initially presented in conventional radiocarbon years (5730 a half-life), corrected for isotopic fractionation, and without reservoir correction. Samples with d13C... -
Table 2: AMS radiocarbon ages from carbonate microfossils of sediment core MD...
The ages are initially presented in conventional radiocarbon years (5730 a half-life), corrected for isotopic fractionation, and without reservoir correction. Samples with d13C... -
Table 2: AMS radiocarbon ages from carbonate microfossils of sediment core MD...
The ages are initially presented in conventional radiocarbon years (5730 a half-life), corrected for isotopic fractionation, and without reservoir correction. Samples with d13C... -
Age model of sediment core MD97-2120
This dataset has no description
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Stable oxygen isotopes (δ¹⁸O) of sediment core MD97-2120
This dataset has no description
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(Figure 2) Paleointensity of sediment core MD97-2140 (1654-1724cm)
This dataset has no description