Silicate weathering is critical to global carbon cycle and climate change, and has attracted
considerable attention in Earth science studies. Chemical weathering intensity evaluation …

Abstract The Bay of Bengal (BoB) is a semi-enclosed basin located in the north-eastern
Indian Ocean which receives enormous fluvial sediment input primarily from the Himalayan …

While the peninsular Indian rivers deliver considerable loads of detrital sediments to the Bay
of Bengal, changes in their depositional patterns with time are relatively less constrained …

Climate change has been a key driver throughout human history and has frequently been
associated with the rise and fall of civilizations. Holocene settlement changes or population …

Downcore geochemical composition of sediment core retrieved from the central Andaman
Sea were measured to help understanding the potential connection between chemical …

This paper reports centennial-scale variations in the Indian summer monsoon (ISM) that
induced stratification and resultant productivity changes in the southern Andaman Sea. The …

Chemical weathering of silicate rocks on continents is thought to have played an important
role in the evolution of past atmospheric carbon dioxide over geologic timescales. However …

Mineral magnetic and geochemical investigations were carried out on a short sediment core
collected from the eastern Southwest Indian Ridge (ESWIR) to study the variations in the …

We present major oxides, trace element compositions, rare earth elements (REEs), clay
mineral assemblages, and magnetic mineral parameters data for the siliciclastic fraction …

Lithogenic grain-size, geochemical elements of core sediments from the central Bay of
Bengal (BoB) were analyzed to identify sediment provenance and explore the regional …