Multiple Stable Isotopes Used to Trace the Flow of Organic Matter in Estuarine Food Webs

The use of a combination of the stable isotopes of sulfur, carbon, and nitrogen allows the flow of organic matter and trophic relations in salt marshes and estuaries to be traced while eliminating many ambiguities that accompany the use of a single isotopic tracer. Salt-marsh grasses take up the iso...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 1985-03, Vol.227 (4692), p.1361-1363
Hauptverfasser: Peterson, Bruce J., Howarth, Robert W., Garritt, Robert H.
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container_issue 4692
container_start_page 1361
container_title Science (American Association for the Advancement of Science)
container_volume 227
creator Peterson, Bruce J.
Howarth, Robert W.
Garritt, Robert H.
description The use of a combination of the stable isotopes of sulfur, carbon, and nitrogen allows the flow of organic matter and trophic relations in salt marshes and estuaries to be traced while eliminating many ambiguities that accompany the use of a single isotopic tracer. Salt-marsh grasses take up the isotopically light sulfides formed during sulfate reduction, and the transfer of this light sulfur through the marsh food web is illustrated with data on the ribbed mussel (Geukensia demissa) from various locations in a New England marsh. The multiple isotope approach shows that this filter feeder consumes both marsh grass (Spartina) detritus and plankton, with the relative proportions of each determined by the location of the mussels in the marsh.
doi_str_mv 10.1126/science.227.4692.1361
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source Jstor Complete Legacy; Science Magazine
subjects Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Brackish water ecosystems
Cord grass
Diet
Estuaries
Food
Food webs
Fundamental and applied biological sciences. Psychology
Highlands
Isotopes
Marshes
Mussels
Plankton
Salt marsh ecology
Spartina
Spartina alterniflora
Sulfur
Synecology
Tidal marsh ecology
title Multiple Stable Isotopes Used to Trace the Flow of Organic Matter in Estuarine Food Webs
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