J.-C. Duplessy

Bio: J.-C. Duplessy is an academic researcher. The author has contributed to research in topics: Foraminifera & North Atlantic Deep Water. The author has an hindex of 6, co-authored 7 publications receiving 1664 citations.

Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation

Abstract: The degree of similarity of the ∂13C records of the planktonic foraminiferal species N. pachyderma and of the benthic foraminiferal genus Cibicides in the high-latitude basins of the world ocean is used as an indicator of the presence of deepwater sources during the last climatic cycle. Whereas continuous formation of deep water is recognized in the southern ocean, the Norwegian Sea stopped acting as a sink for surface water during isotope stage 4 and the remainder of the last glaciation. However, deep water formed in the north Atlantic south of the Norwegian Sea during the last climatic cycle as early as isotope substage 5d, and this area was also the only active northern source during stages 4–2. A detailed reconstruction of the geographic distribution of ∂13C in benthic foraminifera in the Atlantic Ocean during the last glacial maximum shows that the most important deepwater mass originated from the southern ocean, whereas the Glacial North Atlantic Deep Water cannot be traced south of 40°N. At shallower depth an oxygenated 13C rich Intermediate Water mass extended from 45°N to 15°S. In the Pacific Ocean a ventilation higher than the modern one was also found in open ocean in the depth range 700–2600 m and is best explained by stronger formation of Intermediate Water in high northern latitudes.

δ13C Measurements as Indicators of Carbon Flow in Marine and Freshwater Ecosystems

Abstract: Stable isotope ratios provide clues about the origins and transformations of organic matter. A few key reactions control the isotopic composition of most organic matter. Isotopic variations introduced by these reactions are often passed on with little change so that isotopic measurements can indicate natural pathways and flows “downstream” from these key reactions. When chemical and metabolic processes scramble the information content of molecules, isotopic compositions are often preserved. This realization has prompted increasing use of stable isotope analyses as a tool for understanding complex ecological processes.

Fractionation and turnover of stable carbon isotopes in animal tissues: Implications for δ13C analysis of diet

Abstract: The use of stable carbon isotopes as a means of studying energy flow is increasing in ecology and paleo- ecology. However, secondary fractionation and turnover of stable isotopes in animals are poorly understood pro- cesses. This study shows that tissues of the gerbil (Meriones unguienlatus) have different 613C values when equilibrated on corn (C4) or wheat (C~) diets with constant 13c/1ac contents. Lipids were depleted 3.0%o and hair was enriched 1.0%o relative to the C4 diet. Tissue 6t3C values were ranked hair > brain > muscle > liver > fat. After changing the gerbils to a wheat (C3) diet, isotope ratios of the tissues shifted in the direction of the 6a3C value of the new diet. The rate at which carbon derived from the corn diet was replaced by carbon derived from the wheat diet was ade- quately described by a negative exponential decay model for all tissues examined. More metabolically active tissues such as liver and fat had more rapid turnover rates than less metabolically active tissues such as hair. The half-life for carbon ranged from 6.4 days in liver to 47.5 days in hair. The results of this study have important implications for the use of 6~3C values as indicators of animal diet. Both fractionation and turnover of stable carbon isotopes in animal tissues may obscure the relative contributions of isotopically distinct dietary components (such as C3 vs. C,, or marine vs. terrestrial) if an animal's diet varies through time. These complications deserve attention in any study using stable isotope ratios of animal tissue as dietary indicators and might be minimized by analysis of several tissues or products covering a range of turnover times.

Glacial/interglacial variations in atmospheric carbon dioxide

Abstract: Twenty years ago, measurements on ice cores showed that the concentration of carbon dioxide in the atmosphere was lower during ice ages than it is today. As yet, there is no broadly accepted explanation for this difference. Current investigations focus on the ocean's 'biological pump', the sequestration of carbon in the ocean interior by the rain of organic carbon out of the surface ocean, and its effect on the burial of calcium carbonate in marine sediments. Some researchers surmise that the whole-ocean reservoir of algal nutrients was larger during glacial times, strengthening the biological pump at low latitudes, where these nutrients are currently limiting. Others propose that the biological pump was more efficient during glacial times because of more complete utilization of nutrients at high latitudes, where much of the nutrient supply currently goes unused. We present a version of the latter hypothesis that focuses on the open ocean surrounding Antarctica, involving both the biology and physics of that region.