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Benthic foraminifera relative abundance and enhanced benthic foraminifera oxy...
Relative abundance of benthic foraminifera genera from IODP Site U1488, western equatorial Pacific Ocean. The dataset spans the Late Miocene-Early Pliocene interval, from 8.7 to... -
Standardized and compiled marine paleoproductivity records across the late Mi...
This dataset represents a compilation of globally distributed paleoproductivity proxy records, mainly derived from low latitudes. It includes standardized and compiled records... -
XRF core scanning data from IODP Hole 371-U1506A
This dataset has no description
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Semi-quantitative calcareous nannofossils counts 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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Carbonate mass accumulation rates from IODP Hole 371-U1506A
This dataset has no description
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Accumulation rates of benthic foraminifera 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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Relative group abundance of benthic foraminifera from IODP Hole 371-U1506A
This dataset has no description
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Relative cluster abundance of benthic foraminifera from IODP Hole 371-U1506A
This dataset has no description
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Age model, geochemistry, XRF core scanning elemental data and benthic foramin...
The Late Miocene-Early Pliocene Biogenic Bloom (~9–3.5 Ma) was a paleoceanographic phenomenon defined by anomalously high accumulations of biological components at multiple open... -
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... -
Mg/Ca ratios measured on planktic foraminifera species and reconstructed Sea ...
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... -
Major element composition of IODP Site U1501 in the South China Sea from 5.2 ...
IODP Site U1501 (18°53.09′N, 115°45.95′E, water depth: 2846 m) is situated on the west side of Pearl River Canyon. The length for hole C at IODP Site U1501 is up to 461.8 m,... -
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...