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Seasonal and interannual variability of zooplankton community in waters off Mallorca island (Balearic Sea, Western Mediterranean): 1994–1999
During 1994–1999, the mesozooplankton community was sampled monthly in the upper sea layer (up to 100 m) along a cross-shelf transect of three stations in waters off Mallorca island. Copepods formed the most abundant group (54%) followed by appendicularians (17%), cladocerans and meroplankton larvae...
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Published in: | Oceanologica acta 2003, Vol.26 (5), p.673-686 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | During 1994–1999, the mesozooplankton community was sampled monthly in the upper sea layer (up to 100 m) along a cross-shelf transect of three stations in waters off Mallorca island. Copepods formed the most abundant group (54%) followed by appendicularians (17%), cladocerans and meroplankton larvae (13%). The abundance of all these groups decreased in the offshore direction but it was not the case for other zooplankton groups. A clear seasonal cycle was evident consisting of a general decrease of the abundance from the beginning to the end of the year. In addition to the general increase during late winter and spring, an absolute maximum was detected in May, particularly important at the neritic station and a relative maximum in March and October. During this annual cycle, the community structure was almost maintained. An interannual trend was also present, characterized by an overall decrease in the total zooplankton abundance from 1994 to 1999. Concurrent measurements of water and air temperature show that this trend was correlated with a warming of coastal waters of atmospherical origin. In particular, a marked minimum in zooplankton abundance was recorded during 1998, which was the warmest year registered. During 1997–1998, the warming was also associated with the presence of fresh, nutrient-poor southern waters of Atlantic origin.
De 1994 à 1999, la communauté superficielle du mésozooplancton des cent premiers mètres a été échantillonnée le long d'une radiale de trois stations au large de Majorque. Les copépodes représentent le groupe le plus abondant (54 %) suivi des appendiculaires (17 %), des cladocères et des larves de méroplancton (13 %). L'abondance de ces groupes décroît au fur et à mesure que l'on s'éloigne de la côte, ce qui n'est pas le cas pour les autres groupes de zooplancton. Le cycle saisonnier est très marqué, avec une diminution générale de l'abondance entre le début et la fin de l'année. L'augmentation pendant la première moitié de l'année est marqué par un maximum détecté au printemps, particulièrement important au niveau de la station néritique, et un maximum relatif pendant l'hiver et l'automne. Cet écart s'amoindrit cependant au large. On remarque une tendance interannuelle caractérisée par une diminution générale de l'abondance totale du zooplancton entre 1994 et 1999. Des mesures de la température de l'eau et de l'air démontrent que cette tendance est liée à un réchauffement d'origine atmosphérique des eaux du plateau continen |
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ISSN: | 0399-1784 |
DOI: | 10.1016/j.oceact.2003.07.001 |