Why does a component of Calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes?

During the overwintering period Calanus finmarchicus is known to reside in deeper waters in high-latitude environments. More recent data indicate that the overwintering stages of this species are also found in surface water during the winter period. The present article documents that overwintering s...

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Published in:ICES Journal of Marine Science
Main Authors: Pedersen, G., Tande, K., Ottesen, G. O.
Format: Text
Language:English
Published: Oxford University Press 1995
Subjects:
Online Access:http://icesjms.oxfordjournals.org/cgi/content/short/52/3-4/523
https://doi.org/10.1016/1054-3139(95)80066-2
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spelling fthighwire:oai:open-archive.highwire.org:icesjms:52/3-4/523 2023-05-15T15:38:46+02:00 Why does a component of Calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes? Pedersen, G. Tande, K. Ottesen, G. O. 1995-06-01 00:00:00.0 text/html http://icesjms.oxfordjournals.org/cgi/content/short/52/3-4/523 https://doi.org/10.1016/1054-3139(95)80066-2 en eng Oxford University Press http://icesjms.oxfordjournals.org/cgi/content/short/52/3-4/523 http://dx.doi.org/10.1016/1054-3139(95)80066-2 Copyright (C) 1995, International Council for the Exploration of the Sea/Conseil International pour l'Exploration de la Mer Articles TEXT 1995 fthighwire https://doi.org/10.1016/1054-3139(95)80066-2 2016-11-16T19:02:33Z During the overwintering period Calanus finmarchicus is known to reside in deeper waters in high-latitude environments. More recent data indicate that the overwintering stages of this species are also found in surface water during the winter period. The present article documents that overwintering stages CIV and CV are abundant in the uppermost 100 m at selected sites in the western part of the Barents Sea, and in coastal-and fjord areas in North Norway. The moulting cycle of the surface and deep-water dwelling population components was studied by using a method for monitoring the formation of the opal teeth on the mandibular gnathobase. Although only a limited number of specimens were examined, no moulting indices were found out of approximately 300 specimens examined from November to January. The overall daytime vertical distribution pattern in Grøtsund appeared to have a fairly large component of the population in the uppermost 100 m of depth during the entire winter period, differing from the Barents Sea, where a higher degree of variability in the vertical distribution of C. finmarchicus was found. Physical conditions and trade-offs due to differences in the degree of diapause might account for this vertical distribution pattern. In Grøtsund, the apolysis in stages CIV and CV was found at the beginning of February, prior to the onset of ecdysis. The present study indicated that apolysis in overwintering generations is more closely coupled to ecdysis than shown earlier in C. finmarchicus from the Gulf of Maine. Text Barents Sea Calanus finmarchicus North Norway HighWire Press (Stanford University) Barents Sea Norway ICES Journal of Marine Science 52 3-4 523 531
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Pedersen, G.
Tande, K.
Ottesen, G. O.
Why does a component of Calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes?
topic_facet Articles
description During the overwintering period Calanus finmarchicus is known to reside in deeper waters in high-latitude environments. More recent data indicate that the overwintering stages of this species are also found in surface water during the winter period. The present article documents that overwintering stages CIV and CV are abundant in the uppermost 100 m at selected sites in the western part of the Barents Sea, and in coastal-and fjord areas in North Norway. The moulting cycle of the surface and deep-water dwelling population components was studied by using a method for monitoring the formation of the opal teeth on the mandibular gnathobase. Although only a limited number of specimens were examined, no moulting indices were found out of approximately 300 specimens examined from November to January. The overall daytime vertical distribution pattern in Grøtsund appeared to have a fairly large component of the population in the uppermost 100 m of depth during the entire winter period, differing from the Barents Sea, where a higher degree of variability in the vertical distribution of C. finmarchicus was found. Physical conditions and trade-offs due to differences in the degree of diapause might account for this vertical distribution pattern. In Grøtsund, the apolysis in stages CIV and CV was found at the beginning of February, prior to the onset of ecdysis. The present study indicated that apolysis in overwintering generations is more closely coupled to ecdysis than shown earlier in C. finmarchicus from the Gulf of Maine.
format Text
author Pedersen, G.
Tande, K.
Ottesen, G. O.
author_facet Pedersen, G.
Tande, K.
Ottesen, G. O.
author_sort Pedersen, G.
title Why does a component of Calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes?
title_short Why does a component of Calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes?
title_full Why does a component of Calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes?
title_fullStr Why does a component of Calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes?
title_full_unstemmed Why does a component of Calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes?
title_sort why does a component of calanus finmarchicus stay in the surface waters during the overwintering period in high latitudes?
publisher Oxford University Press
publishDate 1995
url http://icesjms.oxfordjournals.org/cgi/content/short/52/3-4/523
https://doi.org/10.1016/1054-3139(95)80066-2
geographic Barents Sea
Norway
geographic_facet Barents Sea
Norway
genre Barents Sea
Calanus finmarchicus
North Norway
genre_facet Barents Sea
Calanus finmarchicus
North Norway
op_relation http://icesjms.oxfordjournals.org/cgi/content/short/52/3-4/523
http://dx.doi.org/10.1016/1054-3139(95)80066-2
op_rights Copyright (C) 1995, International Council for the Exploration of the Sea/Conseil International pour l'Exploration de la Mer
op_doi https://doi.org/10.1016/1054-3139(95)80066-2
container_title ICES Journal of Marine Science
container_volume 52
container_issue 3-4
container_start_page 523
op_container_end_page 531
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