Document généré le 13/05/2026 depuis l'adresse: https://www.documentation.eauetbiodiversite.fr/fr/notice/aspartate-transcarbamylase-du-mesozooplancton-et-prerecrutement-de-la-sole-les-conditions-d-une-approche-systemique-en-manche
Aspartate transcarbamylase du mesozooplancton et prerecrutement de la sole: les conditions d’une approche systémique en Manche
Titre alternatif
Producteur
Contributeur(s)
Éditeur(s)
Gauthier-villars/editions Elsevier
Identifiant documentaire
9-18303
Identifiant OAI
oai:archimer.ifremer.fr:18303
Auteur(s):
Bergeron, Jean-pierre
Mots clés
ASPARTATE TRANSCARBAMYLASE
ENGLISH CHANNEL
RECRUITMENT
DOVER SOLE
ZOOPLANKTON
Date de publication
01/01/1993
Date de création
Date de modification
Date d'acceptation du document
Date de dépôt légal
Langue
fre
Thème
Type de ressource
Source
Oceanologica Acta (0399-1784) (Gauthier-villars/editions Elsevier), 1993 , Vol. 16 , N. 5-6 , P. 677-686
Droits de réutilisation
1993 Gauthier-villars/editions Elsevier
Région
Département
Commune
Description
In temperate neritic areas, meteorological conditions prevailing during winter and the following spring play a major role on the main features of the spring development pattern of pelagic ecosystems. Interannual fluctuations of this environment lead to qualitative and quantitative variations of secondary production which may strongly influence processes regulating the recruitment of many species. A method for assessing pelagic secondary production is based on measurement of the activity of an enzyme, aspartate transcarbamylase, and has been carried out during spring periods for six years in succession, in the southwestern part of the English Channel. These works have permitted the establishment of a close correlation between the quantitative variations of this enzyme activity and changes in biomass with time of the mesozooplankton community. For the same years, other authors have performed, in the eastern English Channel, the assessment of sole pre-recruitment, which shows striking analogies with interannual variations of the secondary production index. Therefore, from a macroscale point of view, more or less favourable years appear in quite agreement for both estimates. The general oceanographical features, the spatio-temporal scales of involved processes are presented and allow to explain why, and within what limits, such results can be successfully achieved for some fish populations and especially sole in the English Channel.
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