Abstract Interglacials of the Quaternary Period are currently the focus of a great deal of
attention within the scientific community. This is primarily because they play a vital role in …

The short-term variability in the Indian monsoon is well documented through instrumental
records and paleoclimatic studies of the recent geological past. However, the effect of mid …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

Several independent trajectories of subsistence intensification, often leading to agriculture,
began during the Holocene. No plant-rich intensifications are known from the Pleistocene …

Western Eurasia yielded a rich Middle (MP) and Late Pleistocene (LP) fossil record
documenting the evolution of the Neandertals that can be analyzed in light of recently …

Stable isotope and ice-rafted debris records from three core sites in the mid-latitude North
Atlantic (IODP Site U1313, MD01-2446, MD03-2699) are combined with records of ODP …

The modern Great Barrier Reef (GBR) is part of the world's largest and best known mixed
terrigenous-carbonate continental margin. The GBR shelf contains three shore-parallel …

Pleistocene interglacials are often considered to be possible geological analogs for the
climatic development of the Holocene epoch. Marine isotope stage 11 (MIS 11), a prominent …

The global ocean overturning circulation is a major means of distributing heat around the
Earth, and an important trigger or amplifier of climate change. This study presents a 1.5-Myr …

The Marine Isotope Stage 11 interglacial, centred at∼ 400ka, appears to be the best
candidate for understanding climatic changes in the context of low insolation forcing such as …