Dataset - B2FIND

(Figure 2) Monthly interpolated coral δ¹⁸O and d18Oseawater record from Bonai...

Fossil coral U/Th Age: 120.5 ± 1.1 kyr before the year of measurement (which is AD 2014) / Time period: 14 years around 120.5 ka / Internal chronology starts at base (oldest...

(Figure 2) Monthly interpolated coral δ¹⁸O and d18Oseawater record from Bonai...

Fossil coral U/Th Age: 125.8 ± 1.6 kyr before the year of measurement (which is AD 2014) / Time period: 10 years around 125.8 ka / Internal chronology starts at base (oldest...

(Figure 2) Monthly interpolated coral δ¹⁸O and d18Oseawater record from Bonai...

Fossil coral U/Th Age: 123.9 ± 1.3 kyr before the year of measurement (which is AD 2014) / Time period: 37 years around 123.9 ka / Internal chronology starts at base (oldest...

(Figure 2) Monthly interpolated coral δ¹⁸O and d18Oseawater record from Bonai...

Fossil coral U/Th Age: 125.5 ± 2.4 kyr before the year of measurement (which is AD 2014) / Time period: 5 years around 125.5 ka/ Internal chronology starts at base (oldest...

(Figure 2) Monthly interpolated coral δ¹⁸O and d18Oseawater record from Bonai...

Fossil coral U/Th Age: 124.9 ± 1.9 kyr before the year of measurement (which is AD 2014) / Time period: 3 years around 124.9 ka / Internal chronology starts at base (oldest...

(Figure 2) Monthly interpolated coral δ¹⁸O and d18Oseawater record from Bonai...

Fossil coral U/Th Age: 123.3 ± 3.1 kyr before the year of measurement (which is AD 2014) / Time period: 6 years around 123.3 ka / Internal chronology starts at base (oldest...

(Figure 2) Monthly interpolated coral δ¹⁸O and d18Oseawater record from Bonai...

Fossil coral U/Th Age: 129.7 ± 1.7 kyr before the year of measurement (which is AD 2014) / Time period: 10 years around 129.7 ka / Internal chronology starts at base (oldest...

Geochemistry on Holocene sediments from the Mediterranean

The enhanced accumulation of organic matter in Eastern Mediterranean sapropels and their unusually low d15N values have been attributed to either enhanced nutrient availability...

Mineral dust deposition in interglacial and glacial climate conditions: model...

The global aerosol/climate model ECHAM5-HAM is used in order to investigate the dust cycle for four interglacial and one glacial climate conditions. The 20-year time-slices are...