Surface sediment samples (depth 0–160cm) and a paleosol (depth 10–15m), both part of a
sediment profile exposed in a cliff section of Narmada River, Western India were analyzed …

We report the late-Holocene climate and vegetation of the Lower Narmada valley, Gujarat,
western India as inferred from the stable carbon and oxygen isotopic composition (δ13C and …

Stable-isotopic, clay-mineralogic, and bulk-chemical analyses were conducted on paleosols
of the Neogene Siwalik sections in northern Pakistan in order to reconstruct floodplain …

This study incorporates micromorphology, geochemistry, and stable carbon and nitrogen
isotope compositions of soil organic matter (δ 13 C and δ 15 N) in a radiocarbon-dated …

Carbon isotope ratio of early diagenetic carbonate cement (EDCC) from sandstones was
measured from Mohand Rao (age: 9 to 4.5 Ma) and Haripur Khol (6 to 1.8 Ma) sections of …

Stable carbon isotope analyses of pedogenic carbonates were conducted on two Siwalik
sections, Jammu–Nandni and Purmandal–Uttarbehani, covering a lateral stretch of∼ 25 km …

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 …

The presence of a series of humus-rich layers, identified as paleosols in the loess sediments
in the Kashmir basin in northwestern India indicate phases of climatic amelioration in the …

Pedogenic carbonates in a 19m-thick dune section (16R) at Didwana, and several shorter
profiles from the eastern margin of the Thar Desert, Rajasthan, were studied for their stable …

Investigations into the most plausible causes which triggered the Late Miocene global
expansion of C 4 grasslands have reached no consensus and are still being debated. The …