Carbonate minerals contain stable isotopes of carbon and oxygen with different masses
whose abundances and bond arrangement are governed by thermodynamics. The clumped …

Since the discovery of dolomite, numerous attempts have been made to understand its
precipitation mechanism at Earth's surface conditions. One such mechanism relies on a …

The carbon isotopic (δ13C) composition of shallow-water carbonates often is interpreted to
reflect the δ13C of the global ocean and is used as a proxy for changes in the global carbon …

The measured carbon isotopic compositions of carbonate sediments (δ13Ccarb) on modern
platforms are commonly 13C‐enriched compared to predicted values for minerals forming in …

Clumped isotope thermometry is an effective tool which allows to understand the post-
depositional alteration, including recrystallization and solid-state reordering, of carbonate …

Triple oxygen isotope measurements are an emerging tool in paleoclimate reconstructions.
In this contribution we develop the application of triple oxygen isotope measurements to …

Abstract The North American Newark Canyon Formation (NCF;∼ 113–98 Ma) presents an
opportunity to examine how terrestrial carbonate facies reflect different aspects of …

Dissolved organic matter (DOM) is the largest carbon pool and directly affects the
biogeochemistry in lakes. In the current study, fourier transform ion cyclotron mass …

The elevation history of the Tibetan Plateau promises insight into the mechanisms and
dynamics that develop and sustain high topography over tens of millions of years, as well as …

The gas hydrate‐bearing structure—mud volcano Kedr‐1 (Lake Baikal, southern basin)—is
located near the coal‐bearing sediments of the Tankhoy formation of Oligocene–Miocene …