In situ twilight grazing rhythm during diel vertical migrations of a scattering layer of Calanus finmarchicus 1
A scattering layer of Calanus finmarchicus was sampled every 90 min during 48 h in the lower St. Lawrence estuary. Grazing activity (phytoplankton pigments in the gut) and the percentage of recently and nonrecently fed copepods (from observation of food in the gut) were monitored in two strata (0–30...
Published in: | Limnology and Oceanography |
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Language: | English |
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Wiley
1985
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crwiley:10.4319/lo.1985.30.3.0598 2023-12-03T10:20:38+01:00 In situ twilight grazing rhythm during diel vertical migrations of a scattering layer of Calanus finmarchicus 1 Simard, Yvan Lacroix, Guy Legendre, Louis 1985 http://dx.doi.org/10.4319/lo.1985.30.3.0598 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1985.30.3.0598 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1985.30.3.0598 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 30, issue 3, page 598-606 ISSN 0024-3590 1939-5590 Aquatic Science Oceanography journal-article 1985 crwiley https://doi.org/10.4319/lo.1985.30.3.0598 2023-11-09T14:01:19Z A scattering layer of Calanus finmarchicus was sampled every 90 min during 48 h in the lower St. Lawrence estuary. Grazing activity (phytoplankton pigments in the gut) and the percentage of recently and nonrecently fed copepods (from observation of food in the gut) were monitored in two strata (0–30 m and 30–100 m). Phytoplankton was restricted to the upper stratum. A bimodal twilight grazing rhythm was observed: the first feeding period, in the upper stratum, begins after sunset; it is followed by the “midnight sinking” in the deeper stratum (2–3 h), during which the gut content is evacuated; after this, the animals return to the upper stratum for a second meal, before the dawn descent. In both migrations, there was a dynamic interchange of individuals between the two strata, which masked the fact that all the copepods migrated to the upper stratum and that a dawn rise actually happened. The feeding time in the warmer surface water was very short. Feeding ceased rapidly even if phytoplankton concentration was low. A large increase in the number of migrants did not change the feeding patterns. Results support the hypothesis that the behavior of C. finmarchicus during the central phase of vertical migrations in late summer is closely linked to an in situ grazing rhythm. Article in Journal/Newspaper Calanus finmarchicus Copepods Wiley Online Library (via Crossref) Limnology and Oceanography 30 3 598 606 |
institution |
Open Polar |
collection |
Wiley Online Library (via Crossref) |
op_collection_id |
crwiley |
language |
English |
topic |
Aquatic Science Oceanography |
spellingShingle |
Aquatic Science Oceanography Simard, Yvan Lacroix, Guy Legendre, Louis In situ twilight grazing rhythm during diel vertical migrations of a scattering layer of Calanus finmarchicus 1 |
topic_facet |
Aquatic Science Oceanography |
description |
A scattering layer of Calanus finmarchicus was sampled every 90 min during 48 h in the lower St. Lawrence estuary. Grazing activity (phytoplankton pigments in the gut) and the percentage of recently and nonrecently fed copepods (from observation of food in the gut) were monitored in two strata (0–30 m and 30–100 m). Phytoplankton was restricted to the upper stratum. A bimodal twilight grazing rhythm was observed: the first feeding period, in the upper stratum, begins after sunset; it is followed by the “midnight sinking” in the deeper stratum (2–3 h), during which the gut content is evacuated; after this, the animals return to the upper stratum for a second meal, before the dawn descent. In both migrations, there was a dynamic interchange of individuals between the two strata, which masked the fact that all the copepods migrated to the upper stratum and that a dawn rise actually happened. The feeding time in the warmer surface water was very short. Feeding ceased rapidly even if phytoplankton concentration was low. A large increase in the number of migrants did not change the feeding patterns. Results support the hypothesis that the behavior of C. finmarchicus during the central phase of vertical migrations in late summer is closely linked to an in situ grazing rhythm. |
format |
Article in Journal/Newspaper |
author |
Simard, Yvan Lacroix, Guy Legendre, Louis |
author_facet |
Simard, Yvan Lacroix, Guy Legendre, Louis |
author_sort |
Simard, Yvan |
title |
In situ twilight grazing rhythm during diel vertical migrations of a scattering layer of Calanus finmarchicus 1 |
title_short |
In situ twilight grazing rhythm during diel vertical migrations of a scattering layer of Calanus finmarchicus 1 |
title_full |
In situ twilight grazing rhythm during diel vertical migrations of a scattering layer of Calanus finmarchicus 1 |
title_fullStr |
In situ twilight grazing rhythm during diel vertical migrations of a scattering layer of Calanus finmarchicus 1 |
title_full_unstemmed |
In situ twilight grazing rhythm during diel vertical migrations of a scattering layer of Calanus finmarchicus 1 |
title_sort |
in situ twilight grazing rhythm during diel vertical migrations of a scattering layer of calanus finmarchicus 1 |
publisher |
Wiley |
publishDate |
1985 |
url |
http://dx.doi.org/10.4319/lo.1985.30.3.0598 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.1985.30.3.0598 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.1985.30.3.0598 |
genre |
Calanus finmarchicus Copepods |
genre_facet |
Calanus finmarchicus Copepods |
op_source |
Limnology and Oceanography volume 30, issue 3, page 598-606 ISSN 0024-3590 1939-5590 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.4319/lo.1985.30.3.0598 |
container_title |
Limnology and Oceanography |
container_volume |
30 |
container_issue |
3 |
container_start_page |
598 |
op_container_end_page |
606 |
_version_ |
1784268099915087872 |