Respiration and ammonium excretion by open ocean gelatinous zooplankton1

Warm‐water species of siphonophores, medusae, ctenophores, heteropods, pseudothecosomatous pteropods, salps, and doliolids were individually collected in jars by SCUBA divers in the western North Atlantic Ocean. In situ rates of oxygen consumption and ammonium excretion were estimated by difference...

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Bibliographic Details
Published in:Limnology and Oceanography
Main Author: Biggs, Douglas C.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1977
Subjects:
Online Access:http://dx.doi.org/10.4319/lo.1977.22.1.0108
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1977.22.1.0108
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1977.22.1.0108
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Summary:Warm‐water species of siphonophores, medusae, ctenophores, heteropods, pseudothecosomatous pteropods, salps, and doliolids were individually collected in jars by SCUBA divers in the western North Atlantic Ocean. In situ rates of oxygen consumption and ammonium excretion were estimated by difference from control jars of seawater enclosed simultaneously. The cystonect siphonophores Rhizophysa filiformis and Bathyphysa sibogae had low respiration and excretion rates [4–7 µ l O 2 (mg protein‐h) −1 and 0.3–0.5 NH 4 + (mg protein‐h) −1 ], while several calycophore siphonophores, heteropods, and salps had high rates [19–192 µ l O 2 (mg protein‐h) −1 and 1.0–3.1 µ g NH 4 + (mg protein‐h) −1 ]. Most O: NH 4 + ratios ranged from 16–38 and suggest that both protein and lipid are important metabolites in tropical and subtropical gelatinous zooplankton. Many physonect siphonophores, scyphomedusae, heteropods, and salps excreted ammonium at rates exceeding 0.3 µ g‐atom NH 4 + ‐N h −1 and may play an important role in recycling nitrogen in the upper mixed layer of oligotrophic ocean regions.