Tintinnids (Ciliophora) and other net microzooplankton (>30 µm) in southwestern Atlantic Shelf Break waters

THOMPSON GUSTAVO; ALDER VIVIANA; BOLTOVSKOY DEMETRIO

MARINE ECOLOGY-PUBBLICAZIONI DELLA STAZIONE ZOOLOGICA DI NAPOLI I

Blackwell Wissenschafts-Verlag

Lugar: Berlin; Año: 2001 vol. 22 p. 343 - 355

0173-9565

Proportions of foraminifers, tintinnids, polycystine radiolarians, pteropods and crustacean larval stages were estimated in a collection of 76 vertically stratified (0‑100 m) 30 µm net microplankton samples from 16 stations located following roughly the Argentine shelf‑slope (around 200 m isobath ‑ between 40 and 56°S), covered on 13‑18 November 1996. Tintinnids were identified to species. Relative abundances of the microzooplankton assessed and chlorophyll a values allow to define two contrasting groups of stations: ?deep? and ?shallow?. The former, located in pelagic, purely subantarctic Malvinas Current waters, hosted higher proportions of foraminifers and lower proportions of tintinnids, as well as less chlorophyll a (all differences were significant at the 0.1% level). ?Shallow? stations were located in the area of the thermohaline front where the Patagonian Current comes in contact with the Malvinas Current, and were generally characterized by higher chlorophyll a levels (up to 3.7 µg Chl a l‑1). The distribution of tintinnid species, on the other hand, did not allow discriminating between these two areas, although some of the dominant forms showed much higher relative abundances in one of the two groups of stations. Twenty‑six tintinnid taxa were recorded, yet only 6 accounted for 95% of the specimens identified. Tintinnid taxocoenoses were characterized by a few abundant species and many rare ones. Numbers of tintinnid species present and specific diversity did not differ noticeably with depth and latitude. Cape Horn Current waters were detected in the area by the presence of expatriated organisms presumably originating at mid‑latitudes in the South Pacific Ocean.