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

It has been known for some time that viable palaeoclimatic information should be recorded
in groundwater-fed riverine tufas, particularly barrage, paludal or spring-line deposits. Stable …

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

Actively forming travertine and tufa sites are widespread in temperate and warm climates,
such as the Mediterranean region, but also develop in other climatic regimes from the Arctic …

Spring systems encompass a tremendous range of environmental niches where calcareous
deposits commonly form. Although active springs have been classified according to their …

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 …

Abstract Abiotic, Bioinduced and Biocontrolled carbonates are process-based sediment
categories. They successively reflect increasing levels of biotic control over carbonate …

Fluvial and associated carbonate deposits are common nowadays and in the Quaternary
record, but are less abundant further back in time. At present, they develop under climate …

During deposition of the Upper Jurassic Morrison Formation, water that originated as
precipitation in uplands to the west of the Western Interior depositional basin infiltrated …

The formation of carbonate sediments in continental environments is subject to numerous
environmental controls, of which climate is one of the foremost. Consequently, calcareous …