-
Raw counts of sporomorphs in the Eocene interval of IODP Hole 318-U1356A
This dataset has no description
-
(Table S1) Pollen and spores of IODP Hole 318-U1356A
Sediment depth is given in mbsf. All samples are from the work half of the sediment core. -
Quantitative analysis of the Eocene record from IODP Hole 318-U1356A
Sediment depth is given in mbsf. Only samples with 100 and more individuals are presented. -
R-code of sporomorph analyses of IODP Hole 318-U1356A
This dataset has no description
-
(Table S6) Calculated annual mean air temperature of IODP Hole 318-U1356A
Sediment depth is given in mbsf. All samples are from the work half of the sediment core. -
(Table S5) Taxa defining the upper and lower limits in the application of the...
Temperate rainforest biome, samples with counts >= 90, nearest living relatives (NLR) >= 5. Sediment depth is given in mbsf. -
(Table S4) Taxa defining the upper and lower limits in the application of the...
Paratropical rainforest biome, samples with counts >= 90, nearest living relatives (NLR) >= 5. Sediment depth is given in mbsf. -
(Table S3) Bioclimatic analysis for IODP Hole 318-U1356A based on Mosbrugger ...
Ts not available for some taxa. Sediment depth is given in mbsf. -
(Table S2) Bioclimatic analysis for IODP Hole 318-U1356A based on Greenwood e...
T sum not available for some taxa. Sediment depth is given in mbsf. -
Sporomorphs and quantitative analysis of the Eocene record from IODP Hole 318...
The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was characterized by an expansion of near-tropical vegetation belts into the... -
Pollen and spores, calculated temperature and precipitation of IODP Hole 318-...
The warmest global climates of the past 65 million years occurred during the early Eocene epoch (about 55 to 48 million years ago), when the Equator-to-pole temperature...
