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- W2023162861 abstract "The biogeography of phytoplankton sampled along 92°W and between 45 and 36°S in conjunction with a detailed XBT section corroborates the physical evidence of a counterflow to the West Wind Drift. Distinct communities exist to either side of an east-west tending front that separates the low-salinity surface water tongue off Chile from subantarctic waters to the south. A plankton group dominated by Ceratium trichoceros and other dinoflagellates exists south of the front in the subantarctic waters, while a distinct group dominated by Rhizosolenia bergonii and other diatoms occupies the low-salinity tongue; the northern limit of the lower salinity surface water is the Subtropical Convergence where a third, distinct plankton community is also dominated by dinoflagellates, mainly C. furca and C. gibberum. Factor analyses support the existence of the distinct groups; it also provides some evidence for the origin of the low-salinity surface water as a mixture of subantarctic surface and coastal runoff by identifying a unique factor axis for Nitzshcia longissima, a pennate diatom generally associated with shallow coastal waters and which comprises a major fraction of the phytoplankton assemblage near the frontal zone but within the low-salinity tongue." @default.
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- W2023162861 date "1982-10-01" @default.
- W2023162861 modified "2023-09-27" @default.
- W2023162861 title "Phytoplankton community composition across the West Wind Drift off South America" @default.
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- W2023162861 doi "https://doi.org/10.1016/0198-0149(82)90092-9" @default.
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