In pelagic carbonate sediments, the degree to which the δ13C values of inorganic and
organic fractions co‐vary has been used to interpret rates of production, burial and …

We investigated the seasonal and geographical variation in the stable carbon isotope ratios
of total dissolved inorganic carbon (δ 13 c dic) and suspended matter (δ 13 C POC) in the …

Abstract δ 13 C values of oceanic inorganic carbon from six stations in the North and South
Atlantic vary between− 1 and+ 2%. relative to the PDB standard. A correlation between the …

The reconstruction of ocean history employs a large variety of methods with origins in the
biological, chemical, and physical sciences, and uses modern statistical techniques for the …

The concentration and carbon isotopic composition (δ 13 C) of sedimentary organic carbon
(C org), N/C ratios, and terrigenous and marine δ 13 C org endmembers form a basis from …

Origins and fates of organic carbon in estuarine and nearshore marine food webs of Hood
Canal, a fjord extension of Puget Sound, Washington (USA), were evaluated seasonally …

The carbon isotope record of carbonate sediments deposited on the ocean floor during the
past 108 years may be intepreted in terms of changes in the global organic carbon reservoir …

Samples for stable isotope studies of possible chemosynthesis in anoxic basins were
collected in 1986 in the Cariaco Trench and May 1988 in the Black Sea. POM (particulate …

The type and flux of organic carbon (OC) delivered from the continents to the sea can both
influence, and be influenced by, climate change on regional and global scales. In order to …

The effects of nonconservative sources (inputs) and sinks (outputs) of carbon are indicated
by the behavior of Δ14C and δ13C of the total dissolved inorganic carbon (ΣCO2) in San …