Interglacials, including the present (Holocene) period, are warm, low land ice extent (high
sea level), end‐members of glacial cycles. Based on a sea level definition, we identify …

Abstract The Iberian Margin is a sensitive area to track high and low latitude processes, and
is a key location to understand major past climatic and oceanographic changes. Here we …

Abrupt cooling is observed at the end of interglacials in many paleoclimate records, but the
mechanism responsible remains unclear. Using model simulations, we demonstrate that …

Abundant evidence from marine, ice-core and terrestrial records demonstrates that Earth's
climate has experienced co-evolution of orbital-and millennial-scale variability through the …

Pulse-like carbon dioxide release to the atmosphere on centennial time scales has only
been identified for the most recent glacial and deglacial periods and is thought to be absent …

Paleotemperature proxy data form the cornerstone of paleoclimate research and are integral
to understanding the evolution of the Earth system across the Phanerozoic Eon. Here, we …

Radiometric dating of glacial terminations over the past 640,000 years suggests pacing by
Earth's climatic precession, with each glacial-interglacial period spanning four or five cycles …

The contourite depositional system (CDS) along the southwestern Iberian Margin (SIM),
within the Gulf of Cadiz and offshore areas of western Portugal bear the unmistakable signal …

Prediction of breast cancer response to Neoadjuvant Chemotherapy (NACT) is an urgent
need to promptly direct non-responder patients to alternative therapies. Infiltrating T …

We present a 3.2 Myr record of stable isotopes and physical properties at IODP Site U1308
(reoccupation of DSDP Site 609) located within the ice-rafted detritus (IRD) belt of the North …