BACKGROUND Radiocarbon (14C) has long been recognized as providing an essential
dating method covering the past 55,000 years. However, the further role of 14C as a …

Radiocarbon is an extremely useful carbon cycle tracer and radiometric dating tool. Here,
we review the main principles and challenges involved in the use of radiocarbon in …

Radiocarbon is a tracer that provides unique insights into the ocean's ability to sequester CO
2 from the atmosphere. While spatial patterns of radiocarbon in the ocean interior can …

Cosmogenic isotopes are produced by cosmic rays mostly in the middle‐low atmosphere
and then take part in the complicated processes of atmospheric transport and deposition that …

Abstract The Indian Ocean accounts for over 20% of the global ocean volume, nearly at par
with the Atlantic, and possesses a unique hydrography characterized by turn-over entirely …

Understanding climate variability from millennial to glacial–interglacial time scales remains
challenging due to the complex and nonlinear feedbacks between ice, ocean, sediments …

Cosmogenic radionuclide records from polar ice cores provide unique insights into past
cosmic ray flux variations. They allow reconstructions of past solar activity, space weather …

The ocean carbon reservoir controls atmospheric carbon dioxide (CO2) on millennial
timescales. Radiocarbon (14C) anomalies in eastern North Pacific sediments suggest a …

The geomagnetic dipole moment (GDM) modulates the production rates of cosmogenic
radionuclides via the shielding of galactic cosmic rays. Therefore, it is possible to use this …

Abstract The Middle to Late Holocene transition was associated with a notable episode of
aridity throughout many parts of the world known as the 4.2 ka event. Indian summer …