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CLAM age model and pollen profile of sediment core 133-820
This dataset has no description
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CLAM age model and pollen profile of sediment core Lynchs_Crater
This dataset has no description
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CLAM age model and pollen profile of sediment core Lake_Consuelo_CON1
This dataset has no description
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CLAM age model and pollen profile of sediment core GeoB3104-1
This dataset has no description
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CLAM age model and pollen profile of sediment core Fuquene
This dataset has no description
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CLAM age model and pollen profile of sediment core 133-820
This dataset has no description
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CLAM age model and pollen profile of sediment core Lake_Wangoom
This dataset has no description
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CLAM age model and pollen profile of sediment core Caledonia_Fen
This dataset has no description
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Pollen record from sediment core M77/2_056-3 (Bay of Guayaquil, Peru)
We analyzed the pollen content of a marine core located near the bay of Guayaquil in Ecuador to document the link between sea surface temperatures (SST) and changes in rainfall... -
Abundance of terrestrial palynomorphs of sediment core CRP-1
Sparse pollen and spores from the lower Miocene section of CRP-1 derive from at least three sources. A low-diversity but persitent angiosperm-moss-liverwort assemblage may... -
(Appendix 1) Pollen and spores abundance in surface sediment of Liaodong Bay ...
A minimum of 200 pollen grains (excluding spores) were counted for each sample. All of the pollen percentages (i.e. relative abundances) were calculated on the basis of the... -
(Appendix 1) Pollen and spores percentage in surface sediment of Liaodong Bay...
A minimum of 200 pollen grains (excluding spores) were counted for each sample. All of the pollen percentages (i.e. relative abundances) were calculated on the basis of the... -
Pollen profile of sediment core FR1/94-GC3 from the East Tasman Plateau, Aust...
Long, well-dated records of climate change in Australia are rare because most of the continent is prone to deflation and sediments are difficult to date beyond 40,000 years.... -
Pollen and spores of ODP Hole 175-1081A, Miocene-Pliocene, Walvis Ridge
Aridification is an important component of Late Neogene climate change in south-western Africa probably caused by modifications in the atmospheric circulation in relation to the... -
Table 2. Percentage of palynomorphs found in each sample through Longling sec...
The Longling Coal Mine (W. Yunnan) is situated in an area of substantial geotectonic activity. Its Late Pliocene palynoflora is of considerable interest, since the area... -
Relative abundances of AP and NAP pollen in the Toushe Basin (Fig2B)
This dataset has no description
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REVEALS reconstruction of past vegetation cover with optimized RPP values for...
This data set presents the reconstructed vegetation cover for 155 African sites based on harmonized pollen data from the data set LegacyPollen 2.0... -
REVEALS reconstruction of past vegetation cover with optimized RPP values for...
This data set presents the reconstructed vegetation cover for 173 South American sites based on harmonized pollen data from the data set LegacyPollen 2.0... -
REVEALS reconstruction of past vegetation cover with optimized RPP values for...
This data set presents the reconstructed vegetation cover for 1115 North American sites based on harmonized pollen data from the data set LegacyPollen 2.0... -
REVEALS reconstruction of past vegetation cover with optimized RPP values for...
This data set presents the reconstructed vegetation cover for 80 Indopacific sites based on harmonized pollen data from the data set LegacyPollen 2.0...
