The presence of arsenic in the groundwater of the densely-populated Bengal Basin evolved
as a mass-poisoning agent and is a reason for the misery of millions of people living here …

Determining the rates, mechanisms, and geographic variability of relative sea-level (RSL)
change following the Last Glacial Maximum (LGM) provides insight into the sensitivity of ice …

The evolution of past global ice sheets is highly uncertain. One example is the missing ice
problem during the Last Glacial Maximum (LGM, 26 000-19 000 years before present)–an …

" Sometime before 15,000 years ago, a band of hunter-gatherers arrived in Northeast Asia.
They continued east, becoming the first people to set foot in the Americas. They soon found …

The most rapid global sea-level rise event of the last deglaciation, Meltwater Pulse 1A (MWP-
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …

Sea level and deep-sea temperature variations are key indicators of global climate changes.
For continuous records over millions of years, deep-sea carbonate microfossil–based δ18O …

Global ice volume (sea level) and deep‐sea temperature are key measures of Earth's
climatic state. We synthesize evidence for multi‐centennial to millennial ice‐volume and …

We assembled a database of Holocene relative sea-level index points (n= 213) and marine
(n= 211) and terrestrial (n= 122) limiting points for the broader South and Southeast Asian …

Large benthic foraminifera are major carbonate components in tropical carbonate platforms,
important carbonate producers, stratigraphic tools and powerful bioindicators (proxies) of …

Palaeoshorelines and associated palaeo-coastal features are studied to reconstruct past
sea level, climate, and depositional environments. Their identification typically depends on …