Glacial to interglacial surface nutrient variations of Bering Deep Basins recorded by δ13C and δ15N of sedimentary organic matter
- 1 December 1995
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 10 (6) , 1047-1061
- https://doi.org/10.1029/95pa02644
Abstract
No abstract availableThis publication has 70 references indexed in Scilit:
- Climate-related variations in denitrification in the Arabian Sea from sediment 15N/14N ratiosNature, 1995
- Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilizationGlobal Biogeochemical Cycles, 1994
- Evidence from nitrogen isotope ratios for enhanced productivity during formation of eastern Mediterranean sapropelsNature, 1992
- Seasonal and depth-related changes in the source of sinking particles in the North AtlanticNature, 1991
- Variations in nitrogen isotopic composition between sinking and suspended particles: implications for nitrogen cycling and particle transformation in the open oceanDeep Sea Research Part A. Oceanographic Research Papers, 1988
- Depletion of 13C in lignin and its implications for stable carbon isotope studiesNature, 1987
- Vostok ice core provides 160,000-year record of atmospheric CO2Nature, 1987
- Mechanism of Carbon Isotope Fractionation Associated with Lipid SynthesisScience, 1977
- Metabolic fractionation of carbon isotopes in marine plankton—II. Data on samples collected off the coasts of Peru and EcuadorDeep Sea Research and Oceanographic Abstracts, 1968
- UPTAKE OF NEW AND REGENERATED FORMS OF NITROGEN IN PRIMARY PRODUCTIVITY1Limnology and Oceanography, 1967