Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's
oceans through time have been documented through stratigraphic study of marine …

Abstract The Smithian-Spathian boundary (SSB) was an interval characterized by a major
global carbon cycle perturbation, climatic cooling from a middle/late Smithian boundary …

We construct a time scale for the 840–544Ma Neoproterozoic interval from isotopic variation
of δ13Ccarbonate and δ13Corganic, 87Sr/86Sr, and δ34Ssulfate in seawater measured …

Vertical gradients in the δ13C of seawater dissolved inorganic carbon (Δδ13CDIC) can be
estimated for paleomarine systems based on δ13Ccarb data from sections representing a …

In the Athabasca Basin Proterozoic sandstones unconformably overlie Archean and
Aphebian rocks. Multiple fluid events, involving isotopically-and chemically-distinct fluids …

Carbon isotope data from Upper Cambrian sections in three Laurentian basins in northern
Utah, central Iowa, and western Newfoundland record a large positive δ13C excursion …

The cause of the late Paleozoic (ca. 355–255 Ma) ice age remains uncertain. A lowering of
atmospheric carbon dioxide levels near the beginning of this time period occurred in …

The primary variability of the composition and properties of seawater is much greater in the
shallow coastal zones than in the main body of ocean water. An inadequate understanding …

Critical assessment of dolomite abundance throughout the Phanerozoic suggests that most
large-scale dolomite has had an origin related to salinity-elevated seawaters. The …

A combined study of trace elements, carbon and oxygen isotopes was carried out for
Carboniferous marine limestones from the Lower Yangtze platform in South China. The …