India's northward flight and collision with Asia was a major driver of global tectonics in the
Cenozoic and, we argue, of atmospheric CO2 concentration (p CO2) and thus global …

The small reservoir of carbon dioxide in the atmosphere (pCO 2) that modulates climate
through the greenhouse effect reflects a delicate balance between large fluxes of sources …

ABSTRACT A simple model that tracks global land area and its average latitude to specify
C02 levels and consequent surface temperatures has been used to infer paleotemperatures …

The middle Miocene represents a major change in state in Cenozoic climatic evolution,
following the climax of Neogene warmth in the late early Miocene at∼ 16 Ma. The early …

Combining magnetostratigraphic and carbon isotopic data for the late Miocene can provide
a temporal framework for an isotopic shift first documented in soil carbonate nodules of …

Previous studies have suggested that during the late Pleistocene ice ages, surface-deep
exchange was somehow weakened in the Southern Ocean's Antarctic Zone, which reduced …

Climate change is known to occur for the past several hundreds of million years. Geological
records of these changes are seen in various continental and marine settings. Several …

Steep topography, a tropical climate, and mafic lithologies contribute to efficient chemical
weathering and carbon sequestration in the Southeast Asian islands. Ongoing arc–continent …

It is generally accepted that progressive cooling of global climate since the Late Cretaceous
results from decreasing partial pressure of atmospheric CO2 (pCO2). However, details on …

Cenozoic era was the turning point in the geological history of the Indian subcontinent when
India experienced maximum isolation before it collided with Asia and there occurred a great …