Unchanged nitrogen isotopic composition of organic matter in the South China Sea during the last climatic cycle: Global implications
- 1 April 2000
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 15 (2) , 244-253
- https://doi.org/10.1029/1999pa000407
Abstract
No abstract availableKeywords
This publication has 90 references indexed in Scilit:
- Nitrogen isotopic fractionation during a simulated diatom spring bloom:importance of N-starvation in controlling fractionationMarine Ecology Progress Series, 1999
- Glacial/interglacial variations in production and nitrogen fixation in the Cariaco Basin during the last 580 kyrPaleoceanography and Paleoclimatology, 1998
- The sequence of events surrounding Termination II and their implications for the cause of glacial‐interglacial CO2 changesPaleoceanography and Paleoclimatology, 1998
- Surface ocean and monsoon climate variability in the South China Sea since the last glaciationMarine Micropaleontology, 1997
- Reconstruction of past nutrient utilization in the Eastern Angola Basin based on sedimentary 15N/14N ratiosPaleoceanography and Paleoclimatology, 1997
- Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilizationGlobal Biogeochemical Cycles, 1994
- The distribution of radiocarbon in the glacial oceanGlobal Biogeochemical Cycles, 1990
- Global variations of surface ocean productivity in low and mid latitudes: Influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 yearsPaleoceanography and Paleoclimatology, 1988
- Biogeochemical studies on the transport of organic matter along the Otsuchi River watershed, JapanEstuarine, Coastal and Shelf Science, 1987
- Limits on the ventilation rate for the deep ocean over the last 12000 yearsClimate Dynamics, 1986