Abstract The late Paleozoic Ice Age (LPIA) was one of Earth's most important Phanerozoic
climatic events lasting for over 100 Mys. Despite its importance, its history is controversial …

Glacial to interglacial changes in atmospheric CO 2 are an intriguing part of carbon
reorganization in the climate system and are estimated by investigating deep-water …

Although detailed age models exist for some marine sediment records of the last glacial
cycle (0–150 ka), age models for many cores rely on the stratigraphic correlation of benthic …

Stable isotopes from a U/Th dated aragonite stalagmite from the Central Kumaun Himalaya
provide evidence of variation in climatic conditions in the last∼ 1800 years. The δ 18 O and …

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 …

Oxygen isotopes of surface, thermocline and bottom dwelling foraminifera were analysed
from two well-dated Andaman Sea cores and combined with nine previously published …

This paper presents the first stable isotope (δ18O and δ13C) data of a∼ 400 years (1590–
2006 AD) long annual to decadal-resolution speleothem record collected from the Indian …

The spatial domain of the Asian monsoon has been defined by the intensity, seasonal
concentration, and annual range of precipitation. Monsoon subdomains, such as the Indian …

Palaeoclimate data hold the unique promise of providing a long-term perspective on climate
change and as such can serve as an important benchmark for climate models. However …

The mineralogical and stable isotopic composition of authigenic carbonates from the
Krishna–Godavari (KG) and Mahanadi Basin provide a deeper insight into the processes …