We use the carbon and oxygen isotopic compositions of fossil tooth enamel and paleosols to
reconstruct the late Cenozoic history of vegetation and environmental change in the Linxia …

The results of a carbon isotope study from a hitherto unexplored marine sediments from the
Birmania basin, Northwestern India are reported, which documents significant isotope …

Organic carbon isotope and geochemical changes across a continental interior Permo–
Triassic boundary section from the Raniganj Basin, India, indicate a∼ 9‰ drop in organic …

The oxygen isotope compositions of the pedogenic carbonates formed on the sediments of
the Lameta Formation of Central India during the Upper Cretaceous range from− 6.7 to …

This study aims at reconstructing paleovegetation history in the northeast Himalaya during
the past 2700 yrs using a 100 cm long sedimentary section selected near Anini village …

Stable isotopic data of calcareous nannofossil, monogeneric and monospecific planktic and
benthic foraminifera from five Indian Ocean DSDP sites (212, 217, 220, 237, and 253), leads …

Three cycles of δ13C occurred in Oligocene to Miocene benthic and planktonic foraminifera
at western North Atlantic Sites 558 and 563. Intervals of high δ13C occurred at about 35–33 …

The early Cenozoic was a time of climatic and oceanographic transition from the Cretaceous
“Greenhouse” world to the “Icehouse” world of the Neogene. δ 18 O measurements shed …

The Vindhyan sedimentary succession in central India spans a wide time bracket from the
Paleoproterozoic to the Neoproterozoic period. Chronostratigraphic significance of stable …

One of the largest and most abrupt climatic warming events documented in the geologic
record occurred at the end of the Paleocene epoch. Oceanic deep waters warmed to 10° C …