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Alkenone-based sea surface temperature during the last 8 Ma from IODP Site 38...
This dataset presents a sea surface temperature (SST) record based on the alkenone UK'37 index from IODP Site 383-U1543 and PS97/114-2 in the Southeast Pacific. The SST record... -
C37 alkenones in Miocene sediments from ODP Site 188-1165 in the polar Southe...
We measured the concentrations of C37 alkenones in sediment samples from Ocean Drilling Program (ODP) Site 118-1165. From these concentrations, we calculated the unsaturation... -
Opal contents at IODP U1417 (Gulf of Alaska) during Late Miocne to Early Plei...
International Ocean Discovery Program Site U1417 in the Surveyor (Gulf of Alaska) preserves the hemi-pelagic sediments influenced by the glacial and fluvi-al depositional from... -
Semi-quantitative calcareous nannofossils counts from IODP Hole 371-U1506A
This dataset has no description
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Carbonate mass accumulation rates from IODP Hole 371-U1506A
This dataset has no description
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Stable isotope (δ¹³C) of Trilobatus sacculifer from IODP Hole 371-U1506A
This dataset has no description
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Stable isotope (δ¹³C, δ¹⁸O) of Cibicides mundulus from IODP Hole 371-U1506A
This dataset has no description
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XRF core scanning data from IODP Hole 371-U1506A
This dataset has no description
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Age model form IODP Hole 371-U1506A
This dataset has no description
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Late Miocene radiogenic Sr, Nd, and Pb isotope data of the detrital clay frac...
Data from Enhanced late Miocene chemical weathering and altered precipitation patterns in the watersheds of the Bay of Bengal recorded by detrital clay radiogenic isotopes in... -
Accumulation rates of biogenic components of ODP Hole 154-926B
The multi-proxies (BAR, bio-SiO2 MAR, and CaCO3 MAR) of productivity in Ocean Drilling Program (ODP) Leg 154 Site 926 Hole B (3°43'N, 42°54'W) during the late Miocene. Based on... -
Accumulation rates of biogenic components of ODP Hole 121-758A
The multi-proxies (BAR, bio-SiO2 MAR, and CaCO3 MAR) of productivity in Ocean Drilling Program (ODP) Leg 121 Site 758 Hole A (5°23.05'N, 90°21.67'E) during the late Miocene.... -
Laser driffaction grain-size fractions for IODP Hole 369-U1516A (Table S3)
Hole U1516A laser diffraction grain-size fractions. Dx (10) - 10% percentile size; Dx (50) - 50% percentile size; Dx (90) - 90% percentile size. -
Compositional results from discrete x-ray fluorescence measurements for IODP ...
Compositional results (%) from discrete x-ray fluorescence measurements (WD-XRF) for Site U1514. Excess silica is calculated from the linear relationship between terrigenous... -
Compositional results from discrete x-ray fluorescence measurements for IODP ...
Compositional results (%) from discrete x-ray fluorescence measurements (WD-XRF) for Site U1516. Excess silica is calculated from the linear relationship between terrigenous... -
Late Pleistocene δ¹¹B based carbon dioxide levels from ODP Site 154-926
Earth's climate cooled markedly during the Late Miocene from 12 to 5 million years ago, with far-reaching consequences for global ecosystems. However, the driving forces of... -
Climatic simulation from the equatorial Indian Ocean
During the late Miocene, global cooling occurred alongside the establishment of near-modern terrestrial and marine ecosystems. Significant (3 to 5 °C) sea surface cooling from... -
Late Miocene model boundary condtions
Here we present Late Miocene (~11-7 Ma) model boundary conditions used by Knorr et al. [2011] in two files (Paleogeography.nc and Surface_conditions.nc). These boundary...
