Numerous methods have been proposed to estimate the pre-nuclear-detonation 14 C
content of dissolved inorganic carbon (DIC) recharged to groundwater that has been …

A better understanding of the relative roles of internal climate variability and external
contributions, from both natural (solar, volcanic) and anthropogenic greenhouse gas forcing …

A number of studies proposed a close link between the climate changes in the Asian
summer monsoon (ASM), the Southern Hemisphere (SH), and high latitudes of the Northern …

The climatic controls on the stable carbon isotopic composition (δ 13 C) of speleothem
carbonate are less often discussed in the scientific literature in contrast to the frequently …

Understanding the relationships between speleothem stable isotopes (δ13C δ18O) and in
situ cave forcing mechanisms is important to interpreting ancient stalagmite paleoclimate …

Surface temperature is a fundamental parameter of Earth's climate. Its evolution through time
is commonly reconstructed using the oxygen isotope and the clumped isotope compositions …

Two speleothem stable isotope records from East-Central Europe demonstrate that
Greenland Stadial 12 (GS12) and GS10—at 44.3–43.3 and 40.8–40.2 ka—were prominent …

Paleoclimate observations constitute the only constraint on climate behavior prior to the
instrumental era. However, such observations only provide indirect (proxy) constraints on …

Many fields of Earth sciences benefit from the knowledge of mineral formation temperatures.
For example, carbonates are extensively used for reconstruction of the Earth's past climatic …

We report the first high resolution stalagmite record from Indian Central Himalaya by using a
combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the …