Blooms of the pelagic tunicate, <I>Dolioletta gegenbauri:</I> Are they associated with Gulf Stream frontal eddies?
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ID: 294763
1985
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Abstract
On observe une pullulation de D.g. a 60 km au nord-ouest du front thermique du Gulf Stream. La pullulation apparait entre deux fronts, l'un de temperature et de salinite a l'isobathe 20-m, l'autre de temperature a l'isobathe 40-m. La presence de ces masses de tuniciers est une reponse biologique a des forces physiques conductrices; ce n'est pas seulement un cas de concentration par un seul mecanisme physique
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| Reference Key |
openalex_W2077172008
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|---|---|
| Authors | Don Deibel |
| Journal | journal of marine research |
| Year | 1985 |
| DOI |
10.1357/002224085788437307
|
| URL | |
| Keywords | Keywords not found |
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