Traditionally, fresh water carbonate research has focused on the sedimentology and
palaeontology of ancient lacustrine deposits. Lithofacies in such low‐energy deposits are …

Non-marine carbonate rocks including cave, spring, stream, calcrete and lacustrine-
palustrine sediments, are susceptible to early diagenetic processes. These can profoundly …

Conventional carbonate–water oxygen isotope thermometry and the more recently
developed clumped isotope thermometer have been widely used for the reconstruction of …

Carbonate build-ups in lakes, hydrothermal and fluvial settings are characterized by
distinctive geometry, spatial distribution, fabrics and geochemical signature but also by …

In this paper we present the first detailed geochemical study of the world-famous actively
forming Pamukkale and Karahayit travertines (Denizli Basin, SW-Turkey) and associated …

Abstract In the Denizli Basin (Turkey), located in the western Anatolian extensional province,
travertine and tufa deposition has been an ongoing process for at least 600,000 years …

This study presents new stable carbon and oxygen isotope data from Lower Cretaceous
lacustrine carbonate rock samples recovered from a well drilled in the Santos Basin …

The 18O content of carbonates (expressed as δ18O) is widely used in paleothermometry,
yet it is clear from comparison of experimental results and natural carbonate samples that …

Biofilms are mucilaginous-organic layers produced by microbial activity including viruses.
Growing biofilms form microbial mats which enhance sediment stability by binding particles …

Abstract The Denizli Basin in the West Anatolian Extensional Province in western Turkey is
well‐known for its numerous travertine occurrences. A combined sedimentological …