Proxy reconstructions from deep ocean sediments have helped to shape our understanding
of the role of the global overturning circulation in past climate change. Neodymium (Nd) …

Abstract Approximately 1,250,000 to 700,000 years ago, the pacing of glacial-interglacial
cycles changed from 41,000 years to∼ 100,000 years, a shift known as the 'Mid-Pleistocene …

Nepheloid layers and turbidity currents transport large quantities of detrital sediments to
deep-sea basins. Locally they may control seawater–detrital particle interactions and modify …

The role of suspended particulate matter in the biogeochemical cycling of neodymium (Nd)
in the ocean is not well understood. This study reports the measurement of dissolved Nd …

The global overturning ocean circulation plays a key role in global climate by distributing
heat around the Earth and by triggering or amplifying major climate changes. Neodymium …

Mangroves are essential tropical ecosystems nurturing a wide range of marine biodiversity
and counteracting global warming by sequestering atmospheric carbon dioxide. Hence, the …

Neodymium (Nd) isotopes have been utilized as a tracer of water mass source in the
modern ocean and in palaeoceanographic studies, though the oceanic cycling of Nd is not …

The neodymium (Nd) isotopic composition of seawater is a widely used ocean circulation
tracer. However, uncertainty in quantifying the global ocean Nd budget, particularly …

To improve our understanding and guide future studies and applications, we review the
biogeochemistry of the rare earth elements (REE). The REEs, which form a chemically …

Neodymium isotopic compositions (εNd) in the marginal sea is influenced by the ocean
circulations as well as the lithogenic input from continents, but their relative contributions …