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(Table 3) Sea surface temperature calculated from sediment core RC09-126
This dataset has no description
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(Table 3) Sea surface temperature calculated from sediment core RC09-124
This dataset has no description
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Bioclimate data for the surface transect from the New Mongolian-Siberian Data...
This dataset has no description
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Precipitation pollen-based climate reconstruction of a sediment core from Lak...
This dataset has no description
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Holocene sea-surface reconstructions in the Canadian Arctic, core 2004-804-009
This dataset has no description
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Holocene sea-surface reconstructions in the Canadian Arctic, cor 2005-804-006
This dataset has no description
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Holocene sea-surface reconstructions in the Canadian Arctic, cor 2005-804-004
This dataset has no description
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Holocene temperature reconstructions for northeastern North America and the n...
This dataset has no description
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Holocene temperature reconstructions for northeastern North America and the n...
This dataset has no description
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Holocene temperature reconstructions for northeastern North America and the n...
This dataset has no description
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Holocene temperature reconstructions for northeastern North America and the n...
This dataset has no description
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Mean monthly air temperature for the Pole of Cold of the Northen Hemisphere (...
This dataset has no description
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(Appendix A) Sea surface temperture reconstruction for ODP Hole 117-723A
This dataset has no description
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(Figure 5) Foraminifera abundance and sea-surface temperature of sediment cor...
AGE (Ka BP) is BP(1950). -
Diatom percentage abundances and sea surface temperature reconstruction for c...
Here, we present datasets of diatom abundance and a diatom-based sea surface temperature reconstruction from the Iceland Basin. The 419.5 cm long marine sediment core... -
Diatom percentage abundances and sea surface temperature reconstruction for c...
Due to the shortness of available records, the longterm patterns of climate variability in the Labrador Sea and Newfoundland region are not clear. Here, a diatom-based... -
Deglacial diatom-based august sea surface temperatures in Baffin Bay
The transition from the last ice age to the present-day interglacial was interrupted by the Younger Dryas (YD) cold period. While many studies exist on this climate event, only...
