Cosmogenic nuclide dating relies on the constancy of production and incorporation of
radionuclides in geological archives. Anomalous deviations from constancy during the …

Today's marine calcifiers (coccolithophore algae, Foraminifera [protists], Mollusca,
Crustacea, Anthozoa [corals], Echinodermata) remove carbon dioxide (CO 2) from the …

The Atlantic is the only ocean basin almost entirely surrounded by passive margins, and a
major global long‐term sink of carbonate carbon that has evaded subduction. Quantifying …

The marine biological pump is crucial for removing excess carbon dioxide from the
atmosphere to the ocean interior and seafloor sediments. The Late Miocene Biogenic Bloom …

We are all familiar with the episodes in the deep time history of Earth that enabled life to
emerge in such abundance. Episodes like the formation of a Moon large enough and near …

We reconstructed the orbital-scale variability of deep-water mass properties in the equatorial
Indian Ocean during the late early to late Miocene (17.9 to 8.2 Ma) using benthic …

We give a plain language guide to the Earth's carbon cycle by briefly summarising the
observations and origins of increased levels of greenhouse gases, mainly CO2 but including …

Deep-sea sediments record the geological and climate history of the Earth. The seismic
properties of these sediments, namely the P-and S-wave velocities, depend on their …

Carbonate dissolution and deposition in the deep ocean is a critical component of carbon
cycle, but detailed pictures of carbonate dynamics below the Carbonate Compensation …

Abstract The Miocene Epoch (23.3–5.3 Ma) represents a remarkable time in the Earth's
geological history with significant palaeoclimatic and palaeoenvironmental relevance. In this …