Dataset - B2FIND

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...

Data compilation of bio-SiO2 MAR from 21 sites

The table includes complicated bio-SiO2 MAR from 21 sites in the global ocean during the late Miocene. We also use Geologic Time Scale 2020 timescale (Gradstein et al., 2020;...

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...

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....

Multi-proxy reconstructions of productivity during the late Miocene

The Late Miocene Biogenic Bloom (LMBB), marked by notable increases in biogenic components in marine sediments, provides insights into the response of the biological pump to...

Oxygenated bottom water conditions on Broken Ridge (central Indian Ocean) in ...

The late Miocene and early Pliocene were marked by widespread oxygen depletion in the Pacific and Indian Oceans in conjunction with the so-called "Late Miocene Biogenic Bloom"...

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...

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...

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...

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...

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...

Compositional results from the Late Miocene and Pliocene of Sites U1514 and U...

Late Miocene and Pliocene marine sediments were cored at Sites U1514 and U1516 in the Mentelle Basin offshore Western Australia, as part of the International Ocean Discovery...

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...

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...