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 …

Stable Nd isotope ratio is a potentially useful tool to provide new constraints on the
geological reservoir formation processes, complementing information from the radiogenic …

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 mid-Pleistocene transition (MPT)[~ 1.25 to 0.85 million years ago (Ma)] marks a shift in
the character of glacial-interglacial climate (,). One prevailing hypothesis for the origin of the …

The isotope composition of dissolved neodymium (Nd) in seawater, expressed as ε Nd,
serves as a valuable geochemical tracer for the provenance and mixing of water masses in …

Eastern Mediterranean deep-intermediate convection was highly sensitive to varying inputs
of fresh water fluxes associated with increased rainfall during the African Humid period (15-6 …

Spatially distant sources of neodymium (Nd) to the ocean that carry different isotopic
signatures (ε Nd) have been shown to trace out major water masses and have thus been …

Abstract The Mid-Pleistocene Transition (MPT), occurring between~ 1250 to 700 Ka (1.25 to
0.7 Ma) marks a fundamental change in Earth's climate system when the glacial cyclicity of …

The deep Southern Ocean circulation is of major significance for our understanding of the
ocean's impact on Earth's climate as uptake and release of CO2 strongly depend on the …

抄録 Neodymium (Nd) isotopic compositions of ferromanganese (Fe–Mn) crusts, bulk
sediment leachates, foraminiferal Fe–Mn hydroxides, biogenic apatite, and deep-sea corals …